Articles | Volume 10, issue 3
https://doi.org/10.5194/essd-10-1687-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/essd-10-1687-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
14 Sep 2018
| 14 Sep 2018
The SISAL database: a global resource to document oxygen and carbon isotope records from speleothems
Kamolphat Atsawawaranunt
Centre for Past Climate Change and School of Archaeology, Geography &
Environmental Sciences, Reading University, Whiteknights, Reading, RG6 6AH,
UK
Laia Comas-Bru
CORRESPONDING AUTHOR
School of Earth Sciences, University College Dublin, Belfield, Dublin 4,
Ireland
Sahar Amirnezhad Mozhdehi
School of Earth Sciences, University College Dublin, Belfield, Dublin 4,
Ireland
Michael Deininger
School of Earth Sciences, University College Dublin, Belfield, Dublin 4,
Ireland
Institute of Geosciences, Johannes-Gutenberg-University Mainz,
Johann-Joachim-Becher-Weg 21, 55128 Mainz, Germany
Sandy P. Harrison
Centre for Past Climate Change and School of Archaeology, Geography &
Environmental Sciences, Reading University, Whiteknights, Reading, RG6 6AH,
UK
Andy Baker
School of Biological, Earth and Environmental Sciences, University of New
South Wales, Kensington 2052, Australia
Meighan Boyd
Department of Earth Sciences, Royal Holloway University of London, Egham,
Surrey, TW20 0EX, UK
Nikita Kaushal
Department of Earth Sciences, University of Oxford, South Parks Road,
Oxford, OX1 3AN, UK
Syed Masood Ahmad
CSIR – National Geophysical Research Institute, Uppal Road, 500 007
Hyderabad, India
Department of Geography, Faculty of Natural Sciences, Jamia Millia Islamia, New Delhi 110025,
India
Yassine Ait Brahim
Institute of Global Environmental Change, Xi'an Jiaotong University,
Xi'an, Shaanxi, China
Monica Arienzo
Division of Hydrologic Sciences, Desert Research Institute, 2215 Raggio
Parkway, 89512 Reno, NV, USA
Petra Bajo
School of Geography, The University of Melbourne, 3010 Victoria, Australia
Kerstin Braun
Institute of Human Origins, Arizona State University, P.O. Box 874101,
85287 Tempe, AZ, USA
Yuval Burstyn
Institute of Sciences, Hebrew University of Jerusalem,
Edmond J. Safra Campus, Givat Ram, 91904 Jerusalem, Israel
Geological Survey of Israel, 30 Malkhe Israel, 95501 Jerusalem, Israel
Sakonvan Chawchai
MESA Research Unit, Department of Geology, the Faculty of Science, Chulalongkorn University, 10330 Bangkok, Thailand
Wuhui Duan
Institute of Geology and Geophysics, Chinese Academy of Sciences,
University of Chinese Academy of Sciences, No. 19 Beitucheng West Road,
Chaoyang District, Beijing, China
István Gábor Hatvani
Institute for Geological and Geochemical Research, Research Centre for
Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi
út 45, 1112 Budapest, Hungary
Department of Earth Sciences, University of Southern California, 3651
Trousdale Parkway, 90089 Los Angeles, CA, USA
Zoltán Kern
Institute for Geological and Geochemical Research, Research Centre for
Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi
út 45, 1112 Budapest, Hungary
Inga Labuhn
Institute of Geography, University of Bremen, Bremen, Germany
Matthew Lachniet
Dept. of Geoscience, University of Nevada, Box 4010, 89154 Las Vegas,
NV, USA
Franziska A. Lechleitner
Department of Earth Sciences, University of Oxford, South Parks Road,
Oxford, OX1 3AN, UK
Andrew Lorrey
Climate, Atmosphere and Hazards Centre, National Institute of Water &
Atmospheric Research, 41 Market Place, Central Business District, Auckland,
New Zealand
Carlos Pérez-Mejías
Department of Geoenvironmental Processes and Global Change, Pyrenean
Institute of Ecology (IPE-CSIC), Avda. Montañana 1005, 50059 Zaragoza,
Spain
Robyn Pickering
Department of Geological Sciences, Human Evolutionary Research
Institute, University of Cape Town, 7701 Rondebosch, Cape Town, South Africa
Nick Scroxton
Department of Geosciences, University of Massachusetts Amherst, 611
North Pleasant Street, 01003-9297 Amherst, MA, USA
SISAL Working Group Members
A full list of authors and their affiliations appears at the end of the paper.
Related authors
Laia Comas-Bru, Kira Rehfeld, Carla Roesch, Sahar Amirnezhad-Mozhdehi, Sandy P. Harrison, Kamolphat Atsawawaranunt, Syed Masood Ahmad, Yassine Ait Brahim, Andy Baker, Matthew Bosomworth, Sebastian F. M. Breitenbach, Yuval Burstyn, Andrea Columbu, Michael Deininger, Attila Demény, Bronwyn Dixon, Jens Fohlmeister, István Gábor Hatvani, Jun Hu, Nikita Kaushal, Zoltán Kern, Inga Labuhn, Franziska A. Lechleitner, Andrew Lorrey, Belen Martrat, Valdir Felipe Novello, Jessica Oster, Carlos Pérez-Mejías, Denis Scholz, Nick Scroxton, Nitesh Sinha, Brittany Marie Ward, Sophie Warken, Haiwei Zhang, and SISAL Working Group members
Earth Syst. Sci. Data, 12, 2579–2606, https://doi.org/10.5194/essd-12-2579-2020, https://doi.org/10.5194/essd-12-2579-2020, 2020
Short summary
Short summary
This paper presents an updated version of the SISAL (Speleothem Isotope Synthesis and Analysis) database. This new version contains isotopic data from 691 speleothem records from 294 cave sites and new age–depth models, including their uncertainties, for 512 speleothems.
Marco M. Lehmann, Josie Geris, Ilja van Meerveld, Daniele Penna, Youri Rothfuss, Matteo Verdone, Pertti Ala-Aho, Matyas Arvai, Alise Babre, Philippe Balandier, Fabian Bernhard, Lukrecija Butorac, Simon Damien Carrière, Natalie C. Ceperley, Zuosinan Chen, Alicia Correa, Haoyu Diao, David Dubbert, Maren Dubbert, Fabio Ercoli, Marius G. Floriancic, Teresa E. Gimeno, Damien Gounelle, Frank Hagedorn, Christophe Hissler, Frédéric Huneau, Alberto Iraheta, Tamara Jakovljević, Nerantzis Kazakis, Zoltan Kern, Karl Knaebel, Johannes Kobler, Jiří Kocum, Charlotte Koeber, Gerbrand Koren, Angelika Kübert, Dawid Kupka, Samuel Le Gall, Aleksi Lehtonen, Thomas Leydier, Philippe Malagoli, Francesca Sofia Manca di Villahermosa, Chiara Marchina, Núria Martínez-Carreras, Nicolas Martin-StPaul, Hannu Marttila, Aline Meyer Oliveira, Gaël Monvoisin, Natalie Orlowski, Kadi Palmik-Das, Aurel Persoiu, Andrei Popa, Egor Prikaziuk, Cécile Quantin, Katja T. Rinne-Garmston, Clara Rohde, Martin Sanda, Matthias Saurer, Daniel Schulz, Michael Paul Stockinger, Christine Stumpp, Jean-Stéphane Venisse, Lukas Vlcek, Stylianos Voudouris, Björn Weeser, Mark E. Wilkinson, Giulia Zuecco, and Katrin Meusburger
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2024-409, https://doi.org/10.5194/essd-2024-409, 2024
Preprint under review for ESSD
Short summary
Short summary
This study describes a unique large-scale isotope dataset to study water dynamics in European forests. Researchers collected data from 40 beech and spruce forest sites in spring and summer 2023, using a standardized method to ensure consistency. The results show that water sources for trees change between seasons and vary by tree species. This large dataset offers valuable information for understanding plant water use, improving ecohydrological models, and mapping water cycles across Europe.
Kieran M. R. Hunt and Sandy P. Harrison
EGUsphere, https://doi.org/10.5194/egusphere-2024-2128, https://doi.org/10.5194/egusphere-2024-2128, 2024
Short summary
Short summary
In this study, we train machine learning models on tree rings, speleothems, and instrumental rainfall to estimate seasonal monsoon rainfall over India over the last 500 years. Our models highlight multidecadal droughts in the mid-seventeenth and nineteenth centuries, and we link these to historical famines. Using techniques from explainable AI, we show our models use known relationships between local hydroclimate and the monsoon circulation.
Sina Panitz, Michael Rogerson, Jack Longman, Nick Scroxton, Tim J. Lawson, Tim C. Atkinson, Vasile Ersek, James Baldini, Lisa Baldini, Stuart Umbo, Mahjoor A. Lone, Gideon M. Henderson, and Sebastian F. M. Breitenbach
Clim. Past Discuss., https://doi.org/10.5194/cp-2024-48, https://doi.org/10.5194/cp-2024-48, 2024
Preprint under review for CP
Short summary
Short summary
Reconstructions of past glaciations tell us about how ice sheets grow and retreat. In this study, we use speleothems (cave deposits, e.g., stalagmites) in the British Isles to help constrain the extent of past glaciations both in time and space. Speleothems require liquid water to grow, and therefore, their presence indicates the absence of ice above the cave. By dating these speleothems we can improve existing reconstructions of past ice sheets.
Stuart Umbo, Franziska Lechleitner, Thomas Opel, Sevasti Modestou, Tobias Braun, Anton Vaks, Gideon Henderson, Pete Scott, Alexander Osintzev, Alexandr Kononov, Irina Adrian, Yuri Dublyansky, Alena Giesche, and Sebastian Breitenbach
EGUsphere, https://doi.org/10.5194/egusphere-2024-1691, https://doi.org/10.5194/egusphere-2024-1691, 2024
Short summary
Short summary
We use cave rocks to reconstruct northern Siberian climate 8.68 ± 0.09 million years ago. We show that when global average temperature was about 4.5 °C warmer than today (similar to what’s expected in the coming decades should carbon emissions continue unabated), Arctic temperature increased by more than 18 °C. Similar levels of Arctic warming in the future would see huge areas of permafrost (permanently frozen ground) thaw and release greenhouse gases to the atmosphere.
Jade Margerum, Julia Homann, Stuart Umbo, Gernot Nehrke, Thorsten Hoffmann, Anton Vaks, Aleksandr Kononov, Alexander Osintsev, Alena Giesche, Andrew Mason, Franziska A. Lechleitner, Gideon M. Henderson, Ola Kwiecien, and Sebastian F. M. Breitenbach
EGUsphere, https://doi.org/10.5194/egusphere-2024-1707, https://doi.org/10.5194/egusphere-2024-1707, 2024
Short summary
Short summary
We analyse a southern Siberian stalagmite to reconstruct soil respiration, wildfire, and vegetation trends, during the last interglacial (LIG) (124.1 – 118.8 ka BP) and Holocene (10 – 0 ka BP). We show that wildfires were greater during the LIG than the Holocene and were supported by fire prone-species, low soil respiration, and a greater difference between summer and winter temperature. We show that vegetation type and summer/winter temperature contrast are strong drivers of Siberian wildfires.
Luke Fionn Sweeney, Sandy P. Harrison, and Marc Vander Linden
EGUsphere, https://doi.org/10.5194/egusphere-2024-1523, https://doi.org/10.5194/egusphere-2024-1523, 2024
Short summary
Short summary
Changes in tree cover across Europe during the Holocene are reconstructed from fossil pollen data using a model developed with modern observations of tree cover and modern pollen assemblages. There is a rapid increase in tree cover after the last glacial with maximum cover during the mid-Holocene and a decline thereafter; the timing of the maximum and the speed of the increase and subsequent decrease vary regionally likely reflecting differences in climate trajectories and human influence.
Nikita Kaushal, Carlos Perez-Mejias, and Heather M. Stoll
Clim. Past Discuss., https://doi.org/10.5194/cp-2024-37, https://doi.org/10.5194/cp-2024-37, 2024
Preprint under review for CP
Short summary
Short summary
Terminations are large magnitude rapid events triggered in the North Atlantic region that manifest across the global climate system. They provide key examples of climatic teleconnections and dynamics. In this study, we use the SISAL global speleothem database and find that there are sufficient climatic records from key locations to make speleothems a valuable archive for studying Terminations and provide instances for more targeted work on speleothem research.
Fang Li, Xiang Song, Sandy P. Harrison, Jennifer R. Marlon, Zhongda Lin, L. Ruby Leung, Jörg Schwinger, Virginie Marécal, Shiyu Wang, Daniel S. Ward, Xiao Dong, Hanna Lee, Lars Nieradzik, Sam S. Rabin, and Roland Séférian
Geosci. Model Dev. Discuss., https://doi.org/10.5194/gmd-2024-85, https://doi.org/10.5194/gmd-2024-85, 2024
Revised manuscript accepted for GMD
Short summary
Short summary
This study provides the first comprehensive assessment of historical fire simulations from 19 CMIP6 ESMs. Most models reproduce global total, spatial pattern, seasonality, and regional historical changes well, but fail to simulate the recent decline in global burned area and underestimate the fire sensitivity to wet-dry conditions. They addressed three critical issues in CMIP5. We present targeted guidance for fire scheme development and methodologies to generate reliable fire projections.
Andy Baker, Margaret Shanafield, Wendy Timms, Martin Sogaard Andersen, Stacey Priestley, and Marilu Melo Zurita
Geosci. Instrum. Method. Data Syst., 13, 117–129, https://doi.org/10.5194/gi-13-117-2024, https://doi.org/10.5194/gi-13-117-2024, 2024
Short summary
Short summary
Much of the world relies on groundwater as a water resource, yet it is hard to know when and where rainfall replenishes our groundwater aquifers. Caves, mines, and tunnels that are situated above the groundwater table are unique observatories of water transiting from the land surface to the aquifer. This paper will show how networks of loggers deployed in these underground spaces across Australia have helped understand when, where, and how much rainfall is needed to replenish the groundwater.
Nikita Kaushal, Franziska A. Lechleitner, Micah Wilhelm, Khalil Azennoud, Janica C. Bühler, Kerstin Braun, Yassine Ait Brahim, Andy Baker, Yuval Burstyn, Laia Comas-Bru, Jens Fohlmeister, Yonaton Goldsmith, Sandy P. Harrison, István G. Hatvani, Kira Rehfeld, Magdalena Ritzau, Vanessa Skiba, Heather M. Stoll, József G. Szűcs, Péter Tanos, Pauline C. Treble, Vitor Azevedo, Jonathan L. Baker, Andrea Borsato, Sakonvan Chawchai, Andrea Columbu, Laura Endres, Jun Hu, Zoltán Kern, Alena Kimbrough, Koray Koç, Monika Markowska, Belen Martrat, Syed Masood Ahmad, Carole Nehme, Valdir Felipe Novello, Carlos Pérez-Mejías, Jiaoyang Ruan, Natasha Sekhon, Nitesh Sinha, Carol V. Tadros, Benjamin H. Tiger, Sophie Warken, Annabel Wolf, Haiwei Zhang, and SISAL Working Group members
Earth Syst. Sci. Data, 16, 1933–1963, https://doi.org/10.5194/essd-16-1933-2024, https://doi.org/10.5194/essd-16-1933-2024, 2024
Short summary
Short summary
Speleothems are a popular, multi-proxy climate archive that provide regional to global insights into past hydroclimate trends with precise chronologies. We present an update to the SISAL (Speleothem Isotopes
Synthesis and AnaLysis) database, SISALv3, which, for the first time, contains speleothem trace element records, in addition to an update to the stable isotope records available in previous versions of the database, cumulatively providing data from 365 globally distributed sites.
Synthesis and AnaLysis) database, SISALv3, which, for the first time, contains speleothem trace element records, in addition to an update to the stable isotope records available in previous versions of the database, cumulatively providing data from 365 globally distributed sites.
Mengmeng Liu, Iain Colin Prentice, and Sandy P. Harrison
Clim. Past Discuss., https://doi.org/10.5194/cp-2024-12, https://doi.org/10.5194/cp-2024-12, 2024
Preprint under review for CP
Short summary
Short summary
Dansgaard-Oeschger events were large and rapid warming events that occurred multiple times during the last ice age. We show that changes in the northern extratropics and the southern extratropics were anti-phased, with warming over most of the north and cooling in the south. The reconstructions do not provide evidence for a change in seasonality in temperature. However, they do indicate that warming was generally accompanied by wetter conditions and cooling by drier conditions.
Adrien Deroubaix, Marco Vountas, Benjamin Gaubert, Maria Dolores Andrés Hernández, Stephan Borrmann, Guy Brasseur, Bruna Holanda, Yugo Kanaya, Katharina Kaiser, Flora Kluge, Ovid Oktavian Krüger, Inga Labuhn, Michael Lichtenstern, Klaus Pfeilsticker, Mira Pöhlker, Hans Schlager, Johannes Schneider, Guillaume Siour, Basudev Swain, Paolo Tuccella, Kameswara S. Vinjamuri, Mihalis Vrekoussis, Benjamin Weyland, and John P. Burrows
EGUsphere, https://doi.org/10.5194/egusphere-2024-516, https://doi.org/10.5194/egusphere-2024-516, 2024
Short summary
Short summary
This study assesses atmospheric composition using air quality models during aircraft campaigns in Europe and Asia, focusing on carbonaceous aerosols and trace gases. While carbon monoxide is well modeled, other pollutants have moderate to weak agreement with observations. Wind speed modeling is reliable for identifying pollution plumes, where models tend to overestimate concentrations. This highlights challenges in accurately modeling aerosol and trace gas composition, particularly in cities.
Adrien Deroubaix, Marco Vountas, Benjamin Gaubert, Maria Dolores Andrés Hernández, Stephan Borrmann, Guy Brasseur, Bruna Holanda, Yugo Kanaya, Katharina Kaiser, Flora Kluge, Ovid Oktavian Krüger, Inga Labuhn, Michael Lichtenstern, Klaus Pfeilsticker, Mira Pöhlker, Hans Schlager, Johannes Schneider, Guillaume Siour, Basudev Swain, Paolo Tuccella, Kameswara S. Vinjamuri, Mihalis Vrekoussis, Benjamin Weyland, and John P. Burrows
EGUsphere, https://doi.org/10.5194/egusphere-2024-521, https://doi.org/10.5194/egusphere-2024-521, 2024
Short summary
Short summary
This study explores the proportional relationships between carbonaceous aerosols (black and organic carbon) and trace gases using airborne measurements from two campaigns in Europe and East Asia. Differences between regions were found, but air quality models struggled to reproduce them accurately. We show that these proportional relationships can help to constrain models and can be used to infer aerosol concentrations from satellite observations of trace gases, especially in urban areas.
Heather M. Stoll, Chris Day, Franziska Lechleitner, Oliver Kost, Laura Endres, Jakub Sliwinski, Carlos Pérez-Mejías, Hai Cheng, and Denis Scholz
Clim. Past, 19, 2423–2444, https://doi.org/10.5194/cp-19-2423-2023, https://doi.org/10.5194/cp-19-2423-2023, 2023
Short summary
Short summary
Stalagmites formed in caves provide valuable information about past changes in climate and vegetation conditions. In this contribution, we present a new method to better estimate past changes in soil and vegetation productivity using carbon isotopes and trace elements measured in stalagmites. Applying this method to other stalagmites should provide a better indication of past vegetation feedbacks to climate change.
Huiying Xu, Han Wang, Iain Colin Prentice, and Sandy P. Harrison
Biogeosciences, 20, 4511–4525, https://doi.org/10.5194/bg-20-4511-2023, https://doi.org/10.5194/bg-20-4511-2023, 2023
Short summary
Short summary
Leaf carbon (C) and nitrogen (N) are crucial elements in leaf construction and physiological processes. This study reconciled the roles of phylogeny, species identity, and climate in stoichiometric traits at individual and community levels. The variations in community-level leaf N and C : N ratio were captured by optimality-based models using climate data. Our results provide an approach to improve the representation of leaf stoichiometry in vegetation models to better couple N with C cycling.
Esmeralda Cruz-Silva, Sandy P. Harrison, I. Colin Prentice, Elena Marinova, Patrick J. Bartlein, Hans Renssen, and Yurui Zhang
Clim. Past, 19, 2093–2108, https://doi.org/10.5194/cp-19-2093-2023, https://doi.org/10.5194/cp-19-2093-2023, 2023
Short summary
Short summary
We examined 71 pollen records (12.3 ka to present) in the eastern Mediterranean, reconstructing climate changes. Over 9000 years, winters gradually warmed due to orbital factors. Summer temperatures peaked at 4.5–5 ka, likely declining because of ice sheets. Moisture increased post-11 kyr, remaining high from 10–6 kyr before a slow decrease. Climate models face challenges in replicating moisture transport.
Jonathan Obrist-Farner, Andreas Eckert, Peter M. J. Douglas, Liseth Perez, Alex Correa-Metrio, Bronwen L. Konecky, Thorsten Bauersachs, Susan Zimmerman, Stephanie Scheidt, Mark Brenner, Steffen Kutterolf, Jeremy Maurer, Omar Flores, Caroline M. Burberry, Anders Noren, Amy Myrbo, Matthew Lachniet, Nigel Wattrus, Derek Gibson, and the LIBRE scientific team
Sci. Dril., 32, 85–100, https://doi.org/10.5194/sd-32-85-2023, https://doi.org/10.5194/sd-32-85-2023, 2023
Short summary
Short summary
In August 2022, 65 scientists from 13 countries gathered in Antigua, Guatemala, for a workshop, co-funded by the US National Science Foundation and the International Continental Scientific Drilling Program. This workshop considered the potential of establishing a continental scientific drilling program in the Lake Izabal Basin, eastern Guatemala, with the goals of establishing a borehole observatory and investigating one of the longest continental records from the northern Neotropics.
Olivia Haas, Iain Colin Prentice, and Sandy P. Harrison
Biogeosciences, 20, 3981–3995, https://doi.org/10.5194/bg-20-3981-2023, https://doi.org/10.5194/bg-20-3981-2023, 2023
Short summary
Short summary
We quantify the impact of CO2 and climate on global patterns of burnt area, fire size, and intensity under Last Glacial Maximum (LGM) conditions using three climate scenarios. Climate change alone did not produce the observed LGM reduction in burnt area, but low CO2 did through reducing vegetation productivity. Fire intensity was sensitive to CO2 but strongly affected by changes in atmospheric dryness. Low CO2 caused smaller fires; climate had the opposite effect except in the driest scenario.
Giulia Mengoli, Sandy P. Harrison, and I. Colin Prentice
EGUsphere, https://doi.org/10.5194/egusphere-2023-1261, https://doi.org/10.5194/egusphere-2023-1261, 2023
Preprint archived
Short summary
Short summary
Soil water availability affects plant carbon uptake by reducing leaf area and/or by closing stomata, which reduces its efficiency. We present a new formulation of how climatic dryness reduces both maximum carbon uptake and the soil-moisture threshold below which it declines further. This formulation illustrates how plants adapt their water conservation strategy to thrive in dry climates, and is step towards a better representation of soil-moisture effects in climate models.
Mengmeng Liu, Yicheng Shen, Penelope González-Sampériz, Graciela Gil-Romera, Cajo J. F. ter Braak, Iain Colin Prentice, and Sandy P. Harrison
Clim. Past, 19, 803–834, https://doi.org/10.5194/cp-19-803-2023, https://doi.org/10.5194/cp-19-803-2023, 2023
Short summary
Short summary
We reconstructed the Holocene climates in the Iberian Peninsula using a large pollen data set and found that the west–east moisture gradient was much flatter than today. We also found that the winter was much colder, which can be expected from the low winter insolation during the Holocene. However, summer temperature did not follow the trend of summer insolation, instead, it was strongly correlated with moisture.
Janica C. Bühler, Josefine Axelsson, Franziska A. Lechleitner, Jens Fohlmeister, Allegra N. LeGrande, Madhavan Midhun, Jesper Sjolte, Martin Werner, Kei Yoshimura, and Kira Rehfeld
Clim. Past, 18, 1625–1654, https://doi.org/10.5194/cp-18-1625-2022, https://doi.org/10.5194/cp-18-1625-2022, 2022
Short summary
Short summary
We collected and standardized the output of five isotope-enabled simulations for the last millennium and assess differences and similarities to records from a global speleothem database. Modeled isotope variations mostly arise from temperature differences. While lower-resolution speleothems do not capture extreme changes to the extent of models, they show higher variability on multi-decadal timescales. As no model excels in all comparisons, we advise a multi-model approach where possible.
Inga Labuhn, Franziska Tell, Ulrich von Grafenstein, Dan Hammarlund, Henning Kuhnert, and Bénédicte Minster
Biogeosciences, 19, 2759–2777, https://doi.org/10.5194/bg-19-2759-2022, https://doi.org/10.5194/bg-19-2759-2022, 2022
Short summary
Short summary
This study presents the isotopic composition of recent biogenic carbonates from several lacustrine species which calcify during different times of the year. The authors demonstrate that when biological offsets are corrected, the dominant cause of differences between species is the seasonal variation in temperature-dependent fractionation of oxygen isotopes. Consequently, such carbonates from lake sediments can provide proxy records of seasonal water temperature changes in the past.
Yicheng Shen, Luke Sweeney, Mengmeng Liu, Jose Antonio Lopez Saez, Sebastián Pérez-Díaz, Reyes Luelmo-Lautenschlaeger, Graciela Gil-Romera, Dana Hoefer, Gonzalo Jiménez-Moreno, Heike Schneider, I. Colin Prentice, and Sandy P. Harrison
Clim. Past, 18, 1189–1201, https://doi.org/10.5194/cp-18-1189-2022, https://doi.org/10.5194/cp-18-1189-2022, 2022
Short summary
Short summary
We present a method to reconstruct burnt area using a relationship between pollen and charcoal abundances and the calibration of charcoal abundance using modern observations of burnt area. We use this method to reconstruct changes in burnt area over the past 12 000 years from sites in Iberia. We show that regional changes in burnt area reflect known changes in climate, with a high burnt area during warming intervals and low burnt area when the climate was cooler and/or wetter than today.
Sandy P. Harrison, Roberto Villegas-Diaz, Esmeralda Cruz-Silva, Daniel Gallagher, David Kesner, Paul Lincoln, Yicheng Shen, Luke Sweeney, Daniele Colombaroli, Adam Ali, Chéïma Barhoumi, Yves Bergeron, Tatiana Blyakharchuk, Přemysl Bobek, Richard Bradshaw, Jennifer L. Clear, Sambor Czerwiński, Anne-Laure Daniau, John Dodson, Kevin J. Edwards, Mary E. Edwards, Angelica Feurdean, David Foster, Konrad Gajewski, Mariusz Gałka, Michelle Garneau, Thomas Giesecke, Graciela Gil Romera, Martin P. Girardin, Dana Hoefer, Kangyou Huang, Jun Inoue, Eva Jamrichová, Nauris Jasiunas, Wenying Jiang, Gonzalo Jiménez-Moreno, Monika Karpińska-Kołaczek, Piotr Kołaczek, Niina Kuosmanen, Mariusz Lamentowicz, Martin Lavoie, Fang Li, Jianyong Li, Olga Lisitsyna, José Antonio López-Sáez, Reyes Luelmo-Lautenschlaeger, Gabriel Magnan, Eniko Katalin Magyari, Alekss Maksims, Katarzyna Marcisz, Elena Marinova, Jenn Marlon, Scott Mensing, Joanna Miroslaw-Grabowska, Wyatt Oswald, Sebastián Pérez-Díaz, Ramón Pérez-Obiol, Sanna Piilo, Anneli Poska, Xiaoguang Qin, Cécile C. Remy, Pierre J. H. Richard, Sakari Salonen, Naoko Sasaki, Hieke Schneider, William Shotyk, Migle Stancikaite, Dace Šteinberga, Normunds Stivrins, Hikaru Takahara, Zhihai Tan, Liva Trasune, Charles E. Umbanhowar, Minna Väliranta, Jüri Vassiljev, Xiayun Xiao, Qinghai Xu, Xin Xu, Edyta Zawisza, Yan Zhao, Zheng Zhou, and Jordan Paillard
Earth Syst. Sci. Data, 14, 1109–1124, https://doi.org/10.5194/essd-14-1109-2022, https://doi.org/10.5194/essd-14-1109-2022, 2022
Short summary
Short summary
We provide a new global data set of charcoal preserved in sediments that can be used to examine how fire regimes have changed during past millennia and to investigate what caused these changes. The individual records have been standardised, and new age models have been constructed to allow better comparison across sites. The data set contains 1681 records from 1477 sites worldwide.
Franziska A. Lechleitner, Christopher C. Day, Oliver Kost, Micah Wilhelm, Negar Haghipour, Gideon M. Henderson, and Heather M. Stoll
Clim. Past, 17, 1903–1918, https://doi.org/10.5194/cp-17-1903-2021, https://doi.org/10.5194/cp-17-1903-2021, 2021
Short summary
Short summary
Soil respiration is a critical but poorly constrained component of the global carbon cycle. We analyse the effect of changing soil respiration rates on the stable carbon isotope ratio of speleothems from northern Spain covering the last deglaciation. Using geochemical analysis and forward modelling we quantify the processes affecting speleothem stable carbon isotope ratios and extract a signature of increasing soil respiration synchronous with deglacial warming.
Ashley N. Martin, Karina Meredith, Andy Baker, Marc D. Norman, and Eliza Bryan
Hydrol. Earth Syst. Sci., 25, 3837–3853, https://doi.org/10.5194/hess-25-3837-2021, https://doi.org/10.5194/hess-25-3837-2021, 2021
Short summary
Short summary
We measured the silicon isotopic composition of groundwater from Rottnest Island, Western Australia, to investigate water–rock interactions in a coastal aquifer. Silicon isotopic ratios varied spatially across the island and were related to secondary mineral formation and vertical mixing within the aquifer. We find that silicate dissolution occurs in the freshwater–seawater transition zone, supporting the recent recognition of submarine groundwater discharge in the oceanic silicon isotope cycle.
Alexander Kuhn-Régnier, Apostolos Voulgarakis, Peer Nowack, Matthias Forkel, I. Colin Prentice, and Sandy P. Harrison
Biogeosciences, 18, 3861–3879, https://doi.org/10.5194/bg-18-3861-2021, https://doi.org/10.5194/bg-18-3861-2021, 2021
Short summary
Short summary
Along with current climate, vegetation, and human influences, long-term accumulation of biomass affects fires. Here, we find that including the influence of antecedent vegetation and moisture improves our ability to predict global burnt area. Additionally, the length of the preceding period which needs to be considered for accurate predictions varies across regions.
Sarah E. Parker, Sandy P. Harrison, Laia Comas-Bru, Nikita Kaushal, Allegra N. LeGrande, and Martin Werner
Clim. Past, 17, 1119–1138, https://doi.org/10.5194/cp-17-1119-2021, https://doi.org/10.5194/cp-17-1119-2021, 2021
Short summary
Short summary
Regional trends in the oxygen isotope (δ18O) composition of stalagmites reflect several climate processes. We compare stalagmite δ18O records from monsoon regions and model simulations to identify the causes of δ18O variability over the last 12 000 years, and between glacial and interglacial states. Precipitation changes explain the glacial–interglacial δ18O changes in all monsoon regions; Holocene trends are due to a combination of precipitation, atmospheric circulation and temperature changes.
Masa Kageyama, Sandy P. Harrison, Marie-L. Kapsch, Marcus Lofverstrom, Juan M. Lora, Uwe Mikolajewicz, Sam Sherriff-Tadano, Tristan Vadsaria, Ayako Abe-Ouchi, Nathaelle Bouttes, Deepak Chandan, Lauren J. Gregoire, Ruza F. Ivanovic, Kenji Izumi, Allegra N. LeGrande, Fanny Lhardy, Gerrit Lohmann, Polina A. Morozova, Rumi Ohgaito, André Paul, W. Richard Peltier, Christopher J. Poulsen, Aurélien Quiquet, Didier M. Roche, Xiaoxu Shi, Jessica E. Tierney, Paul J. Valdes, Evgeny Volodin, and Jiang Zhu
Clim. Past, 17, 1065–1089, https://doi.org/10.5194/cp-17-1065-2021, https://doi.org/10.5194/cp-17-1065-2021, 2021
Short summary
Short summary
The Last Glacial Maximum (LGM; ~21 000 years ago) is a major focus for evaluating how well climate models simulate climate changes as large as those expected in the future. Here, we compare the latest climate model (CMIP6-PMIP4) to the previous one (CMIP5-PMIP3) and to reconstructions. Large-scale climate features (e.g. land–sea contrast, polar amplification) are well captured by all models, while regional changes (e.g. winter extratropical cooling, precipitations) are still poorly represented.
Cody C. Routson, Darrell S. Kaufman, Nicholas P. McKay, Michael P. Erb, Stéphanie H. Arcusa, Kendrick J. Brown, Matthew E. Kirby, Jeremiah P. Marsicek, R. Scott Anderson, Gonzalo Jiménez-Moreno, Jessica R. Rodysill, Matthew S. Lachniet, Sherilyn C. Fritz, Joseph R. Bennett, Michelle F. Goman, Sarah E. Metcalfe, Jennifer M. Galloway, Gerrit Schoups, David B. Wahl, Jesse L. Morris, Francisca Staines-Urías, Andria Dawson, Bryan N. Shuman, Daniel G. Gavin, Jeffrey S. Munroe, and Brian F. Cumming
Earth Syst. Sci. Data, 13, 1613–1632, https://doi.org/10.5194/essd-13-1613-2021, https://doi.org/10.5194/essd-13-1613-2021, 2021
Short summary
Short summary
We present a curated database of western North American Holocene paleoclimate records, which have been screened on length, resolution, and geochronology. The database gathers paleoclimate time series that reflect temperature, hydroclimate, or circulation features from terrestrial and marine sites, spanning a region from Mexico to Alaska. This publicly accessible collection will facilitate a broad range of paleoclimate inquiry.
Nick Scroxton, Stephen J. Burns, David McGee, Laurie R. Godfrey, Lovasoa Ranivoharimanana, and Peterson Faina
Clim. Past Discuss., https://doi.org/10.5194/cp-2020-138, https://doi.org/10.5194/cp-2020-138, 2020
Revised manuscript not accepted
Short summary
Short summary
The end of the Harappan civilization in the Indus Valley around 4,200 years ago has been attributed to monsoon failure associated with a global megadrought. Using a suite of high resolution paleoclimate records from around the Indian Ocean basin we find that two consecutive droughts contributed to the end of the Harappa. A winter drought starting 4,200 years ago was followed by monsoon failure at 3,900 years ago. The double hit caused civilization decline first, and abandonment later.
Nick Scroxton, Stephen J. Burns, David McGee, Laurie R. Godfrey, Lovasoa Ranivoharimanana, and Peterson Faina
Clim. Past Discuss., https://doi.org/10.5194/cp-2020-137, https://doi.org/10.5194/cp-2020-137, 2020
Revised manuscript not accepted
Short summary
Short summary
The 4.2 kyr climatic event caused drought in the Mediterranean and Middle East and the collapse of the Akkadian Civilization. Outside of this region the global footprint of this event, be it drought or flood conditions, is poorly understood. This study uses a stalagmite from Madagascar to determine how the 4.2 kyr event influenced the South-East African Monsoon. We find drought in Madagascar and around Lake Malawi but wet conditions elsewhere, a pattern that resembles modern climate variability.
Laia Comas-Bru, Kira Rehfeld, Carla Roesch, Sahar Amirnezhad-Mozhdehi, Sandy P. Harrison, Kamolphat Atsawawaranunt, Syed Masood Ahmad, Yassine Ait Brahim, Andy Baker, Matthew Bosomworth, Sebastian F. M. Breitenbach, Yuval Burstyn, Andrea Columbu, Michael Deininger, Attila Demény, Bronwyn Dixon, Jens Fohlmeister, István Gábor Hatvani, Jun Hu, Nikita Kaushal, Zoltán Kern, Inga Labuhn, Franziska A. Lechleitner, Andrew Lorrey, Belen Martrat, Valdir Felipe Novello, Jessica Oster, Carlos Pérez-Mejías, Denis Scholz, Nick Scroxton, Nitesh Sinha, Brittany Marie Ward, Sophie Warken, Haiwei Zhang, and SISAL Working Group members
Earth Syst. Sci. Data, 12, 2579–2606, https://doi.org/10.5194/essd-12-2579-2020, https://doi.org/10.5194/essd-12-2579-2020, 2020
Short summary
Short summary
This paper presents an updated version of the SISAL (Speleothem Isotope Synthesis and Analysis) database. This new version contains isotopic data from 691 speleothem records from 294 cave sites and new age–depth models, including their uncertainties, for 512 speleothems.
Chris M. Brierley, Anni Zhao, Sandy P. Harrison, Pascale Braconnot, Charles J. R. Williams, David J. R. Thornalley, Xiaoxu Shi, Jean-Yves Peterschmitt, Rumi Ohgaito, Darrell S. Kaufman, Masa Kageyama, Julia C. Hargreaves, Michael P. Erb, Julien Emile-Geay, Roberta D'Agostino, Deepak Chandan, Matthieu Carré, Partrick J. Bartlein, Weipeng Zheng, Zhongshi Zhang, Qiong Zhang, Hu Yang, Evgeny M. Volodin, Robert A. Tomas, Cody Routson, W. Richard Peltier, Bette Otto-Bliesner, Polina A. Morozova, Nicholas P. McKay, Gerrit Lohmann, Allegra N. Legrande, Chuncheng Guo, Jian Cao, Esther Brady, James D. Annan, and Ayako Abe-Ouchi
Clim. Past, 16, 1847–1872, https://doi.org/10.5194/cp-16-1847-2020, https://doi.org/10.5194/cp-16-1847-2020, 2020
Short summary
Short summary
This paper provides an initial exploration and comparison to climate reconstructions of the new climate model simulations of the mid-Holocene (6000 years ago). These use state-of-the-art models developed for CMIP6 and apply the same experimental set-up. The models capture several key aspects of the climate, but some persistent issues remain.
Bronwen L. Konecky, Nicholas P. McKay, Olga V. Churakova (Sidorova), Laia Comas-Bru, Emilie P. Dassié, Kristine L. DeLong, Georgina M. Falster, Matt J. Fischer, Matthew D. Jones, Lukas Jonkers, Darrell S. Kaufman, Guillaume Leduc, Shreyas R. Managave, Belen Martrat, Thomas Opel, Anais J. Orsi, Judson W. Partin, Hussein R. Sayani, Elizabeth K. Thomas, Diane M. Thompson, Jonathan J. Tyler, Nerilie J. Abram, Alyssa R. Atwood, Olivier Cartapanis, Jessica L. Conroy, Mark A. Curran, Sylvia G. Dee, Michael Deininger, Dmitry V. Divine, Zoltán Kern, Trevor J. Porter, Samantha L. Stevenson, Lucien von Gunten, and Iso2k Project Members
Earth Syst. Sci. Data, 12, 2261–2288, https://doi.org/10.5194/essd-12-2261-2020, https://doi.org/10.5194/essd-12-2261-2020, 2020
Zoltán Kern, Dániel Erdélyi, Polona Vreča, Ines Krajcar Bronić, István Fórizs, Tjaša Kanduč, Marko Štrok, László Palcsu, Miklós Süveges, György Czuppon, Balázs Kohán, and István Gábor Hatvani
Earth Syst. Sci. Data, 12, 2061–2073, https://doi.org/10.5194/essd-12-2061-2020, https://doi.org/10.5194/essd-12-2061-2020, 2020
Short summary
Short summary
Here we present the spatially continuous gridded database for amount-weighted annual mean tritium activity in precipitation for the period 1976 to 2017 for the Adriatic–Pannonian region, with a special focus on the years after 2010, which are not represented by existing global models. This AP3H database is capable of providing reliable spatiotemporal input for hydrogeological applications at any place within Slovenia, Hungary, and their surroundings.
Stijn Hantson, Douglas I. Kelley, Almut Arneth, Sandy P. Harrison, Sally Archibald, Dominique Bachelet, Matthew Forrest, Thomas Hickler, Gitta Lasslop, Fang Li, Stephane Mangeon, Joe R. Melton, Lars Nieradzik, Sam S. Rabin, I. Colin Prentice, Tim Sheehan, Stephen Sitch, Lina Teckentrup, Apostolos Voulgarakis, and Chao Yue
Geosci. Model Dev., 13, 3299–3318, https://doi.org/10.5194/gmd-13-3299-2020, https://doi.org/10.5194/gmd-13-3299-2020, 2020
Short summary
Short summary
Global fire–vegetation models are widely used, but there has been limited evaluation of how well they represent various aspects of fire regimes. Here we perform a systematic evaluation of simulations made by nine FireMIP models in order to quantify their ability to reproduce a range of fire and vegetation benchmarks. While some FireMIP models are better at representing certain aspects of the fire regime, no model clearly outperforms all other models across the full range of variables assessed.
Karina T. Meredith, Andy Baker, Martin S. Andersen, Denis M. O'Carroll, Helen Rutlidge, Liza K. McDonough, Phetdala Oudone, Eliza Bryan, and Nur Syahiza Zainuddin
Hydrol. Earth Syst. Sci., 24, 2167–2178, https://doi.org/10.5194/hess-24-2167-2020, https://doi.org/10.5194/hess-24-2167-2020, 2020
Short summary
Short summary
Dissolved organic carbon within groundwater and processes controlling it remain largely unknown. The average groundwater concentration at this coastal site was 5 times higher than the global median, doubling with depth, but with no change in chromatographic character. The lack of oxygen limited the rate of organic matter processing, leading to enhanced preservation. Changes in coastal hydrology could lead to the flux of unreacted organic carbon.
Sean F. Cleator, Sandy P. Harrison, Nancy K. Nichols, I. Colin Prentice, and Ian Roulstone
Clim. Past, 16, 699–712, https://doi.org/10.5194/cp-16-699-2020, https://doi.org/10.5194/cp-16-699-2020, 2020
Short summary
Short summary
We present geographically explicit reconstructions of seasonal temperature and annual moisture variables at the Last Glacial Maximum (LGM), 21 000 years ago. The reconstructions use existing site-based estimates of climate, interpolated in space and time in a physically consistent way using climate model simulations. The reconstructions give a much better picture of the LGM climate and will provide a robust evaluation of how well state-of-the-art climate models simulate large climate changes.
Benjamin D. Stocker, Han Wang, Nicholas G. Smith, Sandy P. Harrison, Trevor F. Keenan, David Sandoval, Tyler Davis, and I. Colin Prentice
Geosci. Model Dev., 13, 1545–1581, https://doi.org/10.5194/gmd-13-1545-2020, https://doi.org/10.5194/gmd-13-1545-2020, 2020
Short summary
Short summary
Estimating terrestrial photosynthesis relies on satellite data of vegetation cover and models simulating the efficiency by which light absorbed by vegetation is used for CO2 assimilation. This paper presents the P-model, a light use efficiency model derived from a carbon–water optimality principle, and evaluates its predictions of ecosystem-level photosynthesis against globally distributed observations. The model is implemented and openly accessible as an R package (rpmodel).
Sandy P. Harrison, Marie-José Gaillard, Benjamin D. Stocker, Marc Vander Linden, Kees Klein Goldewijk, Oliver Boles, Pascale Braconnot, Andria Dawson, Etienne Fluet-Chouinard, Jed O. Kaplan, Thomas Kastner, Francesco S. R. Pausata, Erick Robinson, Nicki J. Whitehouse, Marco Madella, and Kathleen D. Morrison
Geosci. Model Dev., 13, 805–824, https://doi.org/10.5194/gmd-13-805-2020, https://doi.org/10.5194/gmd-13-805-2020, 2020
Short summary
Short summary
The Past Global Changes LandCover6k initiative will use archaeological records to refine scenarios of land use and land cover change through the Holocene to reduce the uncertainties about the impacts of human-induced changes before widespread industrialization. We describe how archaeological data are used to map land use change and how the maps can be evaluated using independent palaeoenvironmental data. We propose simulations to test land use and land cover change impacts on past climates.
Romane Berthelin, Michael Rinderer, Bartolomé Andreo, Andy Baker, Daniela Kilian, Gabriele Leonhardt, Annette Lotz, Kurt Lichtenwoehrer, Matías Mudarra, Ingrid Y. Padilla, Fernando Pantoja Agreda, Rafael Rosolem, Abel Vale, and Andreas Hartmann
Geosci. Instrum. Method. Data Syst., 9, 11–23, https://doi.org/10.5194/gi-9-11-2020, https://doi.org/10.5194/gi-9-11-2020, 2020
Short summary
Short summary
We present the setup of a soil moisture monitoring network, which is implemented at five karstic sites with different climates across the globe. More than 400 soil moisture probes operating at a high spatio-temporal resolution will improve the understanding of groundwater recharge and evapotranspiration processes in karstic areas.
Lina Teckentrup, Sandy P. Harrison, Stijn Hantson, Angelika Heil, Joe R. Melton, Matthew Forrest, Fang Li, Chao Yue, Almut Arneth, Thomas Hickler, Stephen Sitch, and Gitta Lasslop
Biogeosciences, 16, 3883–3910, https://doi.org/10.5194/bg-16-3883-2019, https://doi.org/10.5194/bg-16-3883-2019, 2019
Short summary
Short summary
This study compares simulated burned area of seven global vegetation models provided by the Fire Model Intercomparison Project (FireMIP) since 1900. We investigate the influence of five forcing factors: atmospheric CO2, population density, land–use change, lightning and climate.
We find that the anthropogenic factors lead to the largest spread between models. Trends due to climate are mostly not significant but climate strongly influences the inter-annual variability of burned area.
Laia Comas-Bru, Sandy P. Harrison, Martin Werner, Kira Rehfeld, Nick Scroxton, Cristina Veiga-Pires, and SISAL working group members
Clim. Past, 15, 1557–1579, https://doi.org/10.5194/cp-15-1557-2019, https://doi.org/10.5194/cp-15-1557-2019, 2019
Short summary
Short summary
We use an updated version of the Speleothem Isotopes Synthesis and Analysis (SISAL) database and palaeoclimate simulations generated using the ECHAM5-wiso isotope-enabled climate model to provide a protocol for using speleothem isotopic data for model evaluation, including screening the observations and the optimum period for the modern observational baseline. We also illustrate techniques through which the absolute isotopic values during any time period could be used for model evaluation.
Guangqi Li, Sandy P. Harrison, and I. Colin Prentice
Biogeosciences Discuss., https://doi.org/10.5194/bg-2019-63, https://doi.org/10.5194/bg-2019-63, 2019
Publication in BG not foreseen
Short summary
Short summary
Current methods of removing age effect from tree-ring are influenced by sampling biases – older trees are more abundantly sampled for recent decades, when the strongest environmental change happens. New technique of extracting environment-driven signals from tree ring is specifically designed to overcome this bias, drawing on theoretical tree growth. It removes sampling-bias effectively and shows consistent relationships between growth and climates through time and across two conifer species.
Dongyang Wei, Penélope González-Sampériz, Graciela Gil-Romera, Sandy P. Harrison, and I. Colin Prentice
Clim. Past Discuss., https://doi.org/10.5194/cp-2019-16, https://doi.org/10.5194/cp-2019-16, 2019
Revised manuscript not accepted
Short summary
Short summary
El Cañizar de Villarquemado provides a pollen record from semi-arid Spain since before the last interglacial. We use modern pollen–climate relationships to reconstruct changes in seasonal temperature and moisture, accounting for CO2 effects on plants, and show coherent climate changes on glacial–interglacial and orbital timescales. The low glacial CO2 means moisture changes are less extreme than suggested by the vegetation shifts, and driven by evapotranspiration rather than rainfall changes.
Ilaria Isola, Giovanni Zanchetta, Russell N. Drysdale, Eleonora Regattieri, Monica Bini, Petra Bajo, John C. Hellstrom, Ilaria Baneschi, Piero Lionello, Jon Woodhead, and Alan Greig
Clim. Past, 15, 135–151, https://doi.org/10.5194/cp-15-135-2019, https://doi.org/10.5194/cp-15-135-2019, 2019
Short summary
Short summary
To understand the natural variability in the climate system, the hydrological aspect (dry and wet conditions) is particularly important for its impact on our societies. The reconstruction of past precipitation regimes can provide a useful tool for forecasting future climate changes. We use multi-proxy time series (oxygen and carbon isotopes, trace elements) from a speleothem to investigate circulation pattern variations and seasonality effects during the dry 4.2 ka event in central Italy.
Matthias Forkel, Niels Andela, Sandy P. Harrison, Gitta Lasslop, Margreet van Marle, Emilio Chuvieco, Wouter Dorigo, Matthew Forrest, Stijn Hantson, Angelika Heil, Fang Li, Joe Melton, Stephen Sitch, Chao Yue, and Almut Arneth
Biogeosciences, 16, 57–76, https://doi.org/10.5194/bg-16-57-2019, https://doi.org/10.5194/bg-16-57-2019, 2019
Short summary
Short summary
Weather, humans, and vegetation control the occurrence of fires. In this study we find that global fire–vegetation models underestimate the strong increase of burned area with higher previous-season plant productivity in comparison to satellite-derived relationships.
Laia Comas-Bru and Armand Hernández
Earth Syst. Sci. Data, 10, 2329–2344, https://doi.org/10.5194/essd-10-2329-2018, https://doi.org/10.5194/essd-10-2329-2018, 2018
Short summary
Short summary
This review presents new EOF-based monthly indices of the east Atlantic and the Scandinavian patterns covering the period from 1851 to present. The paper also includes a comparison with their analogous instrumental indices, provides insights into the reasons why different sources of data may give slightly different time series and demonstrates that using these patterns to explain climate variability beyond the winter season needs to be done carefully due to their non-stationary behaviour.
Anthony Dosseto, Holly L. Taylor, Juraj Farkaš, Grant M. Cox, Andrew Kingston, Andrew Lorrey, Alexander J. Corrick, and Bing Shen
Clim. Past Discuss., https://doi.org/10.5194/cp-2018-119, https://doi.org/10.5194/cp-2018-119, 2018
Revised manuscript not accepted
Short summary
Short summary
Life experienced a big boost in complexity ~ 600 million years ago. This step forward in evolution happened not long after the largest glaciations experienced in Earth's history. This study shows that following the last major
Snowball Earth, the planet's surface rapidly recovered and the first animals emerged in an environment maybe not that different from our modern oceans.
Sandy P. Harrison, Patrick J. Bartlein, Victor Brovkin, Sander Houweling, Silvia Kloster, and I. Colin Prentice
Earth Syst. Dynam., 9, 663–677, https://doi.org/10.5194/esd-9-663-2018, https://doi.org/10.5194/esd-9-663-2018, 2018
Short summary
Short summary
Temperature affects fire occurrence and severity. Warming will increase fire-related carbon emissions and thus atmospheric CO2. The size of this feedback is not known. We use charcoal records to estimate pre-industrial fire emissions and a simple land–biosphere model to quantify the feedback. We infer a feedback strength of 5.6 3.2 ppm CO2 per degree of warming and a gain of 0.09 ± 0.05 for a climate sensitivity of 2.8 K. Thus, fire feedback is a large part of the climate–carbon-cycle feedback.
Masa Kageyama, Pascale Braconnot, Sandy P. Harrison, Alan M. Haywood, Johann H. Jungclaus, Bette L. Otto-Bliesner, Jean-Yves Peterschmitt, Ayako Abe-Ouchi, Samuel Albani, Patrick J. Bartlein, Chris Brierley, Michel Crucifix, Aisling Dolan, Laura Fernandez-Donado, Hubertus Fischer, Peter O. Hopcroft, Ruza F. Ivanovic, Fabrice Lambert, Daniel J. Lunt, Natalie M. Mahowald, W. Richard Peltier, Steven J. Phipps, Didier M. Roche, Gavin A. Schmidt, Lev Tarasov, Paul J. Valdes, Qiong Zhang, and Tianjun Zhou
Geosci. Model Dev., 11, 1033–1057, https://doi.org/10.5194/gmd-11-1033-2018, https://doi.org/10.5194/gmd-11-1033-2018, 2018
Short summary
Short summary
The Paleoclimate Modelling Intercomparison Project (PMIP) takes advantage of the existence of past climate states radically different from the recent past to test climate models used for climate projections and to better understand these climates. This paper describes the PMIP contribution to CMIP6 (Coupled Model Intercomparison Project, 6th phase) and possible analyses based on PMIP results, as well as on other CMIP6 projects.
Katalin Takács, Zoltán Kern, and László Pásztor
Earth Syst. Sci. Data, 10, 391–404, https://doi.org/10.5194/essd-10-391-2018, https://doi.org/10.5194/essd-10-391-2018, 2018
Short summary
Short summary
Annual ice phenology was compiled for the largest river (Danube) and lake (Balaton) in eastern–central Europe back to AD 1774 and AD 1885, respectively. The dates of the first appearance of ice and freeze-up have shifted to later. Break-up and ice-off have shifted to earlier, except break-up on Lake Balaton. The derived centennial records of freshwater cryophenology for the Danube and Balaton are readily available for detailed analysis of the temporal trends or other climatological purposes.
Kashif Mahmud, Gregoire Mariethoz, Andy Baker, and Pauline C. Treble
Hydrol. Earth Syst. Sci., 22, 977–988, https://doi.org/10.5194/hess-22-977-2018, https://doi.org/10.5194/hess-22-977-2018, 2018
Short summary
Short summary
This study explores the relationship between drip water and rainfall in a SW Australian karst, where both intra- and interannual hydrological variations are strongly controlled by seasonal variations in recharge. The hydrological behavior of cave drips is examined at daily resolution with respect to mean discharge and the flow variation. We demonstrate that the analysis of the time series produced by cave drip loggers generates useful hydrogeological information that can be applied generally.
István Gábor Hatvani, Zoltán Kern, Szabolcs Leél-Őssy, and Attila Demény
Earth Syst. Sci. Data, 10, 139–149, https://doi.org/10.5194/essd-10-139-2018, https://doi.org/10.5194/essd-10-139-2018, 2018
Short summary
Short summary
Evenly spaced carbon and oxygen stable isotope records were produced from central European stalagmites. To mitigate the potential bias of interpolation, the variance spectra were carefully evaluated. The derived data are ready to use with conventional uni- and multivariate statistics, which are usually not prepared to handle the general characteristic of sedimentary paleoclimate records derived from geological sequences unevenly sampled in time.
Bette L. Otto-Bliesner, Pascale Braconnot, Sandy P. Harrison, Daniel J. Lunt, Ayako Abe-Ouchi, Samuel Albani, Patrick J. Bartlein, Emilie Capron, Anders E. Carlson, Andrea Dutton, Hubertus Fischer, Heiko Goelzer, Aline Govin, Alan Haywood, Fortunat Joos, Allegra N. LeGrande, William H. Lipscomb, Gerrit Lohmann, Natalie Mahowald, Christoph Nehrbass-Ahles, Francesco S. R. Pausata, Jean-Yves Peterschmitt, Steven J. Phipps, Hans Renssen, and Qiong Zhang
Geosci. Model Dev., 10, 3979–4003, https://doi.org/10.5194/gmd-10-3979-2017, https://doi.org/10.5194/gmd-10-3979-2017, 2017
Short summary
Short summary
The PMIP4 and CMIP6 mid-Holocene and Last Interglacial simulations provide an opportunity to examine the impact of two different changes in insolation forcing on climate at times when other forcings were relatively similar to present. This will allow exploration of the role of feedbacks relevant to future projections. Evaluating these simulations using paleoenvironmental data will provide direct out-of-sample tests of the reliability of state-of-the-art models to simulate climate changes.
Masa Kageyama, Samuel Albani, Pascale Braconnot, Sandy P. Harrison, Peter O. Hopcroft, Ruza F. Ivanovic, Fabrice Lambert, Olivier Marti, W. Richard Peltier, Jean-Yves Peterschmitt, Didier M. Roche, Lev Tarasov, Xu Zhang, Esther C. Brady, Alan M. Haywood, Allegra N. LeGrande, Daniel J. Lunt, Natalie M. Mahowald, Uwe Mikolajewicz, Kerim H. Nisancioglu, Bette L. Otto-Bliesner, Hans Renssen, Robert A. Tomas, Qiong Zhang, Ayako Abe-Ouchi, Patrick J. Bartlein, Jian Cao, Qiang Li, Gerrit Lohmann, Rumi Ohgaito, Xiaoxu Shi, Evgeny Volodin, Kohei Yoshida, Xiao Zhang, and Weipeng Zheng
Geosci. Model Dev., 10, 4035–4055, https://doi.org/10.5194/gmd-10-4035-2017, https://doi.org/10.5194/gmd-10-4035-2017, 2017
Short summary
Short summary
The Last Glacial Maximum (LGM, 21000 years ago) is an interval when global ice volume was at a maximum, eustatic sea level close to a minimum, greenhouse gas concentrations were lower, atmospheric aerosol loadings were higher than today, and vegetation and land-surface characteristics were different from today. This paper describes the implementation of the LGM numerical experiment for the PMIP4-CMIP6 modelling intercomparison projects and the associated sensitivity experiments.
Bronwyn C. Dixon, Jonathan J. Tyler, Andrew M. Lorrey, Ian D. Goodwin, Joëlle Gergis, and Russell N. Drysdale
Clim. Past, 13, 1403–1433, https://doi.org/10.5194/cp-13-1403-2017, https://doi.org/10.5194/cp-13-1403-2017, 2017
Short summary
Short summary
Existing sedimentary palaeoclimate records in Australasia were assessed for suitability for examining the last 2 millennia. A small number of high-quality records were identified, and new Bayesian age models were constructed for each record. Findings suggest that Australasian record chronologies and confidence in proxy–climate relationships are the main factors limiting appropriate data for examining Common Era climate variability. Recommendations for improving data accessibility are provided.
María Fernanda Sánchez Goñi, Stéphanie Desprat, Anne-Laure Daniau, Frank C. Bassinot, Josué M. Polanco-Martínez, Sandy P. Harrison, Judy R. M. Allen, R. Scott Anderson, Hermann Behling, Raymonde Bonnefille, Francesc Burjachs, José S. Carrión, Rachid Cheddadi, James S. Clark, Nathalie Combourieu-Nebout, Colin. J. Courtney Mustaphi, Georg H. Debusk, Lydie M. Dupont, Jemma M. Finch, William J. Fletcher, Marco Giardini, Catalina González, William D. Gosling, Laurie D. Grigg, Eric C. Grimm, Ryoma Hayashi, Karin Helmens, Linda E. Heusser, Trevor Hill, Geoffrey Hope, Brian Huntley, Yaeko Igarashi, Tomohisa Irino, Bonnie Jacobs, Gonzalo Jiménez-Moreno, Sayuri Kawai, A. Peter Kershaw, Fujio Kumon, Ian T. Lawson, Marie-Pierre Ledru, Anne-Marie Lézine, Ping Mei Liew, Donatella Magri, Robert Marchant, Vasiliki Margari, Francis E. Mayle, G. Merna McKenzie, Patrick Moss, Stefanie Müller, Ulrich C. Müller, Filipa Naughton, Rewi M. Newnham, Tadamichi Oba, Ramón Pérez-Obiol, Roberta Pini, Cesare Ravazzi, Katy H. Roucoux, Stephen M. Rucina, Louis Scott, Hikaru Takahara, Polichronis C. Tzedakis, Dunia H. Urrego, Bas van Geel, B. Guido Valencia, Marcus J. Vandergoes, Annie Vincens, Cathy L. Whitlock, Debra A. Willard, and Masanobu Yamamoto
Earth Syst. Sci. Data, 9, 679–695, https://doi.org/10.5194/essd-9-679-2017, https://doi.org/10.5194/essd-9-679-2017, 2017
Short summary
Short summary
The ACER (Abrupt Climate Changes and Environmental Responses) global database includes 93 pollen records from the last glacial period (73–15 ka) plotted against a common chronology; 32 also provide charcoal records. The database allows for the reconstruction of the regional expression, vegetation and fire of past abrupt climate changes that are comparable to those expected in the 21st century. This work is a major contribution to understanding the processes behind rapid climate change.
Pauline C. Treble, Andy Baker, Linda K. Ayliffe, Timothy J. Cohen, John C. Hellstrom, Michael K. Gagan, Silvia Frisia, Russell N. Drysdale, Alan D. Griffiths, and Andrea Borsato
Clim. Past, 13, 667–687, https://doi.org/10.5194/cp-13-667-2017, https://doi.org/10.5194/cp-13-667-2017, 2017
Short summary
Short summary
Little is known about the climate of southern Australia during the Last Glacial Maximum and deglaciation owing to sparse records for this region. We present the first high-resolution data, derived from speleothems that grew 23–5 ka. It appears that recharge to the Flinders Ranges was higher than today, particularly during 18.9–15.8 ka, argued to be due to the enhanced availability of tropical moisture. An abrupt shift to aridity is recorded at 15.8 ka, associated with restored westerly airflow.
Michael Deininger, Martin Werner, and Frank McDermott
Clim. Past, 12, 2127–2143, https://doi.org/10.5194/cp-12-2127-2016, https://doi.org/10.5194/cp-12-2127-2016, 2016
Short summary
Short summary
This study investigates the NAO (Northern Atlantic Oscillation)-related mechanisms that control winter precipitation stable oxygen and hydrogen isotope gradients across Europe. The results show that past longitudinal stable oxygen and hydrogen isotope gradients in European rainfall stored in palaeoclimate archives (e.g. speleothems) can be used to infer the past winter NAO modes from its variations.
Carol V. Tadros, Pauline C. Treble, Andy Baker, Ian Fairchild, Stuart Hankin, Regina Roach, Monika Markowska, and Janece McDonald
Hydrol. Earth Syst. Sci., 20, 4625–4640, https://doi.org/10.5194/hess-20-4625-2016, https://doi.org/10.5194/hess-20-4625-2016, 2016
Short summary
Short summary
We investigated the potential use of trace element and stable oxygen-isotope variations in cave drip water as palaeorainfall proxies in an Australian alpine karst site. Using 7 years of cave monitoring data, we constrained the hydrological processes impacting the drip-water composition and identified a robust ENSO–drip water hydrochemical relationship. These findings are fundamental for reconstructing past ENSO variability from speleothems (cave deposits) regionally and globally.
Katie Coleborn, Gabriel C. Rau, Mark O. Cuthbert, Andy Baker, and Owen Navarre
Hydrol. Earth Syst. Sci., 20, 4439–4455, https://doi.org/10.5194/hess-20-4439-2016, https://doi.org/10.5194/hess-20-4439-2016, 2016
Short summary
Short summary
This is the first observation of tree water use in cave drip water. Our novel time series analysis using the synchrosqueeze transform identified daily and sub-daily oscillations in drip rate. The only hypothesis consistent with hydrologic theory and the data was that the oscillations were caused by solar driven pumping by trees above the cave. We propose a new protocol for inferring karst architecture and our findings support research on the impact trees on speleothem paleoclimate proxies.
Michel Legrand, Joseph McConnell, Hubertus Fischer, Eric W. Wolff, Susanne Preunkert, Monica Arienzo, Nathan Chellman, Daiana Leuenberger, Olivia Maselli, Philip Place, Michael Sigl, Simon Schüpbach, and Mike Flannigan
Clim. Past, 12, 2033–2059, https://doi.org/10.5194/cp-12-2033-2016, https://doi.org/10.5194/cp-12-2033-2016, 2016
Short summary
Short summary
Here, we review previous attempts made to reconstruct past forest fire using chemical signals recorded in Greenland ice. We showed that the Greenland ice records of ammonium, found to be a good fire proxy, consistently indicate changing fire activity in Canada in response to past climatic conditions that occurred since the last 15 000 years, including the Little Ice Age and the last large climatic transition.
Bette L. Otto-Bliesner, Pascale Braconnot, Sandy P. Harrison, Daniel J. Lunt, Ayako Abe-Ouchi, Samuel Albani, Patrick J. Bartlein, Emilie Capron, Anders E. Carlson, Andrea Dutton, Hubertus Fischer, Heiko Goelzer, Aline Govin, Alan Haywood, Fortunat Joos, Allegra N. Legrande, William H. Lipscomb, Gerrit Lohmann, Natalie Mahowald, Christoph Nehrbass-Ahles, Jean-Yves Peterschmidt, Francesco S.-R. Pausata, Steven Phipps, and Hans Renssen
Clim. Past Discuss., https://doi.org/10.5194/cp-2016-106, https://doi.org/10.5194/cp-2016-106, 2016
Preprint retracted
Gurinder Nagra, Pauline C. Treble, Martin S. Andersen, Ian J. Fairchild, Katie Coleborn, and Andy Baker
Hydrol. Earth Syst. Sci., 20, 2745–2758, https://doi.org/10.5194/hess-20-2745-2016, https://doi.org/10.5194/hess-20-2745-2016, 2016
Short summary
Short summary
Our current understanding of wildfires on Earth is filled with knowledge gaps. One reason for this is our poor record of fire in natural archives. We open the possibility for speleothems to be "a missing piece to the fire-puzzle". We find by effecting surface evaporation and transpiration rates, wildfires can have a multi-year impact on speleothem, forming dripwater hydrology and chemistry. We open a new avenue for speleothems as potential palaeo-fire archives.
Stijn Hantson, Almut Arneth, Sandy P. Harrison, Douglas I. Kelley, I. Colin Prentice, Sam S. Rabin, Sally Archibald, Florent Mouillot, Steve R. Arnold, Paulo Artaxo, Dominique Bachelet, Philippe Ciais, Matthew Forrest, Pierre Friedlingstein, Thomas Hickler, Jed O. Kaplan, Silvia Kloster, Wolfgang Knorr, Gitta Lasslop, Fang Li, Stephane Mangeon, Joe R. Melton, Andrea Meyn, Stephen Sitch, Allan Spessa, Guido R. van der Werf, Apostolos Voulgarakis, and Chao Yue
Biogeosciences, 13, 3359–3375, https://doi.org/10.5194/bg-13-3359-2016, https://doi.org/10.5194/bg-13-3359-2016, 2016
Short summary
Short summary
Our ability to predict the magnitude and geographic pattern of past and future fire impacts rests on our ability to model fire regimes. A large variety of models exist, and it is unclear which type of model or degree of complexity is required to model fire adequately at regional to global scales. In this paper we summarize the current state of the art in fire-regime modelling and model evaluation, and outline what lessons may be learned from the Fire Model Intercomparison Project – FireMIP.
Inga Labuhn, Valérie Daux, Olivier Girardclos, Michel Stievenard, Monique Pierre, and Valérie Masson-Delmotte
Clim. Past, 12, 1101–1117, https://doi.org/10.5194/cp-12-1101-2016, https://doi.org/10.5194/cp-12-1101-2016, 2016
Short summary
Short summary
This article presents a reconstruction of summer droughts in France for the last 680 years, based on oxygen isotope ratios in tree ring cellulose from living trees and building timbers at two sites, Fontainebleau and Angoulême. Both sites show coherent drought patterns during the 19th and 20th century, and are characterized by increasing drought in recent decades. A decoupling between sites points to a more heterogeneous climate in France during earlier centuries.
A. V. Gallego-Sala, D. J. Charman, S. P. Harrison, G. Li, and I. C. Prentice
Clim. Past, 12, 129–136, https://doi.org/10.5194/cp-12-129-2016, https://doi.org/10.5194/cp-12-129-2016, 2016
Short summary
Short summary
It has become a well-established paradigm that blanket bog landscapes in the British Isles are a result of forest clearance by early human populations. We provide a novel test of this hypothesis using results from bioclimatic modelling driven by cimate reconstructions compared with a database of peat initiation dates. Both results show similar patterns of peat initiation over time and space. This suggests that climate was the main driver of blanket bog inception and not human disturbance.
K. Mahmud, G. Mariethoz, A. Baker, P. C. Treble, M. Markowska, and E. McGuire
Hydrol. Earth Syst. Sci., 20, 359–373, https://doi.org/10.5194/hess-20-359-2016, https://doi.org/10.5194/hess-20-359-2016, 2016
Short summary
Short summary
Caves offer a natural inception point to observe both the long-term groundwater recharge and the preferential movement of water through the unsaturated zone of such limestone. In this study, we develop a method that combines automated drip rate logging systems and remote sensing techniques to quantify the infiltration processes within a cave.
B. A. A. Hoogakker, R. S. Smith, J. S. Singarayer, R. Marchant, I. C. Prentice, J. R. M. Allen, R. S. Anderson, S. A. Bhagwat, H. Behling, O. Borisova, M. Bush, A. Correa-Metrio, A. de Vernal, J. M. Finch, B. Fréchette, S. Lozano-Garcia, W. D. Gosling, W. Granoszewski, E. C. Grimm, E. Grüger, J. Hanselman, S. P. Harrison, T. R. Hill, B. Huntley, G. Jiménez-Moreno, P. Kershaw, M.-P. Ledru, D. Magri, M. McKenzie, U. Müller, T. Nakagawa, E. Novenko, D. Penny, L. Sadori, L. Scott, J. Stevenson, P. J. Valdes, M. Vandergoes, A. Velichko, C. Whitlock, and C. Tzedakis
Clim. Past, 12, 51–73, https://doi.org/10.5194/cp-12-51-2016, https://doi.org/10.5194/cp-12-51-2016, 2016
Short summary
Short summary
In this paper we use two climate models to test how Earth’s vegetation responded to changes in climate over the last 120 000 years, looking at warm interglacial climates like today, cold ice-age glacial climates, and intermediate climates. The models agree well with observations from pollen, showing smaller forested areas and larger desert areas during cold periods. Forests store most terrestrial carbon; the terrestrial carbon lost during cold climates was most likely relocated to the oceans.
T.-T. Meng, H. Wang, S. P. Harrison, I. C. Prentice, J. Ni, and G. Wang
Biogeosciences, 12, 5339–5352, https://doi.org/10.5194/bg-12-5339-2015, https://doi.org/10.5194/bg-12-5339-2015, 2015
Short summary
Short summary
By analysing the quantitative leaf-traits along extensive temperature and moisture gradients with generalized linear models, we found that metabolism-related traits are universally acclimated to environmental conditions, rather than being fixed within plant functional types. The results strongly support a move towards Dynamic Global Vegetation Models in which continuous, adaptive trait variation provides the fundamental mechanism for changes in ecosystem properties along environmental gradients.
G. Li, S. P. Harrison, and I. C. Prentice
Biogeosciences Discuss., https://doi.org/10.5194/bgd-12-4769-2015, https://doi.org/10.5194/bgd-12-4769-2015, 2015
Revised manuscript has not been submitted
M. Pacton, S. F. M. Breitenbach, F. A. Lechleitner, A. Vaks, C. Rollion-Bard, O. S. Gutareva, A. V. Osintcev, and C. Vasconcelos
Biogeosciences, 10, 6115–6130, https://doi.org/10.5194/bg-10-6115-2013, https://doi.org/10.5194/bg-10-6115-2013, 2013
Related subject area
Palaeooceanography, palaeoclimatology
Coral skeletal proxy records database for the Great Barrier Reef, Australia
A revised marine fossil record of the Mediterranean before and after the Messinian salinity crisis
Seeing the wood for the trees: active human–environmental interactions in arid northwestern China
SISALv3: a global speleothem stable isotope and trace element database
DINOSTRAT version 2.1-GTS2020
Paleo±Dust: quantifying uncertainty in paleo-dust deposition across archive types
An 800 kyr planktonic δ18O stack for the Western Pacific Warm Pool
Tephra data from varved lakes of the Last Glacial–Interglacial Transition: towards a global inventory and better chronologies on the Varved Sediments Database (VARDA)
A modern pollen dataset from lake surface sediments on the central and western Tibetan Plateau
Last Glacial loess in Europe: luminescence database and chronology of deposition
The CoralHydro2k database: a global, actively curated compilation of coral δ18O and Sr ∕ Ca proxy records of tropical ocean hydrology and temperature for the Common Era
BENFEP: a quantitative database of benthic foraminifera from surface sediments of the eastern Pacific
The World Atlas of Last Interglacial Shorelines (version 1.0)
A dataset of standard precipitation index reconstructed from multi-proxies over Asia for the past 300 years
Artemisia pollen dataset for exploring the potential ecological indicators in deep time
Volcanic stratospheric sulfur injections and aerosol optical depth during the Holocene (past 11 500 years) from a bipolar ice-core array
Last Interglacial sea-level data points from Northwest Europe
World Atlas of late Quaternary Foraminiferal Oxygen and Carbon Isotope Ratios
Compilation of Last Interglacial (Marine Isotope Stage 5e) sea-level indicators in the Bahamas, Turks and Caicos, and the east coast of Florida, USA
Compilation of a database of Holocene nearshore marine mollusk shell geochemistry from the California Current System
Last interglacial sea-level proxies in the glaciated Northern Hemisphere
Harmonized chronologies of a global late Quaternary pollen dataset (LegacyAge 1.0)
High-resolution aerosol concentration data from the Greenland NorthGRIP and NEEM deep ice cores
DINOSTRAT: a global database of the stratigraphic and paleolatitudinal distribution of Mesozoic–Cenozoic organic-walled dinoflagellate cysts
The Southern Ocean Radiolarian (SO-RAD) dataset: a new compilation of modern radiolarian census data
Lake surface sediment pollen dataset for the alpine meadow vegetation type from the eastern Tibetan Plateau and its potential in past climate reconstructions
A global compilation of U-series-dated fossil coral sea-level indicators for the Last Interglacial period (Marine Isotope Stage 5e)
A standardized database of Marine Isotopic Stage 5e sea-level proxies on tropical Pacific islands
Last interglacial sea-level history from speleothems: a global standardized database
Last interglacial sea-level proxies in East Africa and the Western Indian Ocean
A multiproxy database of western North American Holocene paleoclimate records
A review of MIS 5e sea-level proxies around Japan
Last interglacial (MIS 5e) sea-level proxies in southeastern South America
Compilation of relative pollen productivity (RPP) estimates and taxonomically harmonised RPP datasets for single continents and Northern Hemisphere extratropics
A global mean sea surface temperature dataset for the Last Interglacial (129–116 ka) and contribution of thermal expansion to sea level change
SISALv2: a comprehensive speleothem isotope database with multiple age–depth models
The Eurasian Modern Pollen Database (EMPD), version 2
VARDA (VARved sediments DAtabase) – providing and connecting proxy data from annually laminated lake sediments
The Iso2k database: a global compilation of paleo-δ18O and δ2H records to aid understanding of Common Era climate
Integrating palaeoclimate time series with rich metadata for uncertainty modelling: strategy and documentation of the PalMod 130k marine palaeoclimate data synthesis
Simple noise estimates and pseudoproxies for the last 21 000 years
Speleothem stable isotope records for east-central Europe: resampling sedimentary proxy records to obtain evenly spaced time series with spectral guidance
A database of paleoceanographic sediment cores from the North Pacific, 1951–2016
The ACER pollen and charcoal database: a global resource to document vegetation and fire response to abrupt climate changes during the last glacial period
A 156 kyr smoothed history of the atmospheric greenhouse gases CO2, CH4, and N2O and their radiative forcing
Ariella K. Arzey, Helen V. McGregor, Tara R. Clark, Jody M. Webster, Stephen E. Lewis, Jennie Mallela, Nicholas P. McKay, Hugo W. Fahey, Supriyo Chakraborty, Tries B. Razak, and Matt J. Fischer
Earth Syst. Sci. Data, 16, 4869–4930, https://doi.org/10.5194/essd-16-4869-2024, https://doi.org/10.5194/essd-16-4869-2024, 2024
Short summary
Short summary
Coral skeletal records from the Great Barrier Reef (GBR) provide vital data on climate and environmental change. Presented here is the Great Barrier Reef Coral Skeletal Records Database, an extensive compilation of GBR coral records. The database includes key metadata, primary data, and access instructions, and it enhances research on past, present, and future climate and environmental variability of the GBR. The database will assist with contextualising present-day threats to reefs globally.
Konstantina Agiadi, Niklas Hohmann, Elsa Gliozzi, Danae Thivaiou, Francesca R. Bosellini, Marco Taviani, Giovanni Bianucci, Alberto Collareta, Laurent Londeix, Costanza Faranda, Francesca Bulian, Efterpi Koskeridou, Francesca Lozar, Alan Maria Mancini, Stefano Dominici, Pierre Moissette, Ildefonso Bajo Campos, Enrico Borghi, George Iliopoulos, Assimina Antonarakou, George Kontakiotis, Evangelia Besiou, Stergios D. Zarkogiannis, Mathias Harzhauser, Francisco Javier Sierro, Angelo Camerlenghi, and Daniel García-Castellanos
Earth Syst. Sci. Data, 16, 4767–4775, https://doi.org/10.5194/essd-16-4767-2024, https://doi.org/10.5194/essd-16-4767-2024, 2024
Short summary
Short summary
We present a dataset of 23032 fossil occurrences of marine organisms from the Late Miocene to the Early Pliocene (~11 to 3.6 million years ago) from the Mediterranean Sea. This dataset will allow us, for the first time, to quantify the biodiversity impact of the Messinian salinity crisis, a major geological event that possibly changed global and regional climate and biota.
Hui Shen, Robert N. Spengler, Xinying Zhou, Alison Betts, Peter Weiming Jia, Keliang Zhao, and Xiaoqiang Li
Earth Syst. Sci. Data, 16, 2483–2499, https://doi.org/10.5194/essd-16-2483-2024, https://doi.org/10.5194/essd-16-2483-2024, 2024
Short summary
Short summary
Understanding how early farmers adapted to their environments is important regarding how we respond to the changing climate. Here, we present wood charcoal records from northwestern China to explore human–environmental interactions. Our data suggest that people started managing chestnut trees around 4600 BP and cultivating fruit trees and transporting conifers from 3500 BP. From 2500 BP, people established horticultural systems, showing that they actively adapted to the environment.
Nikita Kaushal, Franziska A. Lechleitner, Micah Wilhelm, Khalil Azennoud, Janica C. Bühler, Kerstin Braun, Yassine Ait Brahim, Andy Baker, Yuval Burstyn, Laia Comas-Bru, Jens Fohlmeister, Yonaton Goldsmith, Sandy P. Harrison, István G. Hatvani, Kira Rehfeld, Magdalena Ritzau, Vanessa Skiba, Heather M. Stoll, József G. Szűcs, Péter Tanos, Pauline C. Treble, Vitor Azevedo, Jonathan L. Baker, Andrea Borsato, Sakonvan Chawchai, Andrea Columbu, Laura Endres, Jun Hu, Zoltán Kern, Alena Kimbrough, Koray Koç, Monika Markowska, Belen Martrat, Syed Masood Ahmad, Carole Nehme, Valdir Felipe Novello, Carlos Pérez-Mejías, Jiaoyang Ruan, Natasha Sekhon, Nitesh Sinha, Carol V. Tadros, Benjamin H. Tiger, Sophie Warken, Annabel Wolf, Haiwei Zhang, and SISAL Working Group members
Earth Syst. Sci. Data, 16, 1933–1963, https://doi.org/10.5194/essd-16-1933-2024, https://doi.org/10.5194/essd-16-1933-2024, 2024
Short summary
Short summary
Speleothems are a popular, multi-proxy climate archive that provide regional to global insights into past hydroclimate trends with precise chronologies. We present an update to the SISAL (Speleothem Isotopes
Synthesis and AnaLysis) database, SISALv3, which, for the first time, contains speleothem trace element records, in addition to an update to the stable isotope records available in previous versions of the database, cumulatively providing data from 365 globally distributed sites.
Synthesis and AnaLysis) database, SISALv3, which, for the first time, contains speleothem trace element records, in addition to an update to the stable isotope records available in previous versions of the database, cumulatively providing data from 365 globally distributed sites.
Peter K. Bijl
Earth Syst. Sci. Data, 16, 1447–1452, https://doi.org/10.5194/essd-16-1447-2024, https://doi.org/10.5194/essd-16-1447-2024, 2024
Short summary
Short summary
This new version release of DINOSTRAT, version 2.1, aligns stratigraphic ranges of dinoflagellate cysts (dinocysts), a microfossil group, to the latest Geologic Time Scale. In this release I present the evolution of dinocyst subfamilies from the Middle Triassic to the modern period.
Nicolás J. Cosentino, Gabriela Torre, Fabrice Lambert, Samuel Albani, François De Vleeschouwer, and Aloys J.-M. Bory
Earth Syst. Sci. Data, 16, 941–959, https://doi.org/10.5194/essd-16-941-2024, https://doi.org/10.5194/essd-16-941-2024, 2024
Short summary
Short summary
One of the main uncertainties related to future climate change has to do with how aerosols interact with climate. Dust is the most abundant aerosol in the atmosphere by mass. In order to better understand the links between dust and climate, we can turn to geological archives of ancient dust. Paleo±Dust is a compilation of measured values of the paleo-dust deposition rate. We can use this compilation to guide climate models so that they better represent dust–climate interactions.
Christen L. Bowman, Devin S. Rand, Lorraine E. Lisiecki, and Samantha C. Bova
Earth Syst. Sci. Data, 16, 701–713, https://doi.org/10.5194/essd-16-701-2024, https://doi.org/10.5194/essd-16-701-2024, 2024
Short summary
Short summary
We estimate an average (stack) of Western Pacific Warm Pool (WPWP) sea surface climate records over the last 800 kyr from 10 ocean sediment cores. To better understand glacial–interglacial differences between the tropical WPWP and high-latitude climate change, we compare our WPWP stack to global and North Atlantic deep-ocean stacks. Although we see similar timing in glacial–interglacial change between the stacks, the WPWP exhibits less amplitude of change.
Anna Beckett, Cecile Blanchet, Alexander Brauser, Rebecca Kearney, Celia Martin-Puertas, Ian Matthews, Konstantin Mittelbach, Adrian Palmer, Arne Ramisch, and Achim Brauer
Earth Syst. Sci. Data, 16, 595–604, https://doi.org/10.5194/essd-16-595-2024, https://doi.org/10.5194/essd-16-595-2024, 2024
Short summary
Short summary
This paper focuses on volcanic ash (tephra) in European annually laminated (varve) lake records from the period 25 to 8 ka. Tephra enables the synchronisation of these lake records and their proxy reconstructions to absolute timescales. The data incorporate geochemical data from tephra layers across 19 varve lake records. We highlight the potential for synchronising multiple records using tephra layers across continental scales whilst supporting reproducibility through accessible data.
Qingfeng Ma, Liping Zhu, Jianting Ju, Junbo Wang, Yong Wang, Lei Huang, and Torsten Haberzettl
Earth Syst. Sci. Data, 16, 311–320, https://doi.org/10.5194/essd-16-311-2024, https://doi.org/10.5194/essd-16-311-2024, 2024
Short summary
Short summary
Modern pollen datasets are essential for pollen-based quantitative paleoclimate reconstructions. Here we present a modern pollen dataset from lake surface sediments on the central and western Tibetan Plateau. This dataset can be used not only for quantitative precipitation reconstructions on the central and western Tibetan Plateau, but can also be combined with other pollen datasets to improve the reliability of quantitative climate reconstructions across the entire Tibetan Plateau.
Mathieu Bosq, Sebastian Kreutzer, Pascal Bertran, Philippe Lanos, Philippe Dufresne, and Christoph Schmidt
Earth Syst. Sci. Data, 15, 4689–4711, https://doi.org/10.5194/essd-15-4689-2023, https://doi.org/10.5194/essd-15-4689-2023, 2023
Short summary
Short summary
During the last glacial period, cold conditions associated with changes in atmospheric circulation resulted in the deposition of widespread loess. It seems that the phases of loess accumulation were not strictly synchronous. To test this hypothesis, the chronology of loess deposition in different regions of Europe was studied by recalculating 1423 luminescence ages in a database. Our study discusses the link between the main loess sedimentation phases and the maximal advance of glaciers.
Rachel M. Walter, Hussein R. Sayani, Thomas Felis, Kim M. Cobb, Nerilie J. Abram, Ariella K. Arzey, Alyssa R. Atwood, Logan D. Brenner, Émilie P. Dassié, Kristine L. DeLong, Bethany Ellis, Julien Emile-Geay, Matthew J. Fischer, Nathalie F. Goodkin, Jessica A. Hargreaves, K. Halimeda Kilbourne, Hedwig Krawczyk, Nicholas P. McKay, Andrea L. Moore, Sujata A. Murty, Maria Rosabelle Ong, Riovie D. Ramos, Emma V. Reed, Dhrubajyoti Samanta, Sara C. Sanchez, Jens Zinke, and the PAGES CoralHydro2k Project Members
Earth Syst. Sci. Data, 15, 2081–2116, https://doi.org/10.5194/essd-15-2081-2023, https://doi.org/10.5194/essd-15-2081-2023, 2023
Short summary
Short summary
Accurately quantifying how the global hydrological cycle will change in the future remains challenging due to the limited availability of historical climate data from the tropics. Here we present the CoralHydro2k database – a new compilation of peer-reviewed coral-based climate records from the last 2000 years. This paper details the records included in the database and where the database can be accessed and demonstrates how the database can investigate past tropical climate variability.
Paula Diz, Víctor González-Guitián, Rita González-Villanueva, Aida Ovejero, and Iván Hernández-Almeida
Earth Syst. Sci. Data, 15, 697–722, https://doi.org/10.5194/essd-15-697-2023, https://doi.org/10.5194/essd-15-697-2023, 2023
Short summary
Short summary
Benthic foraminifera are key components of the ocean benthos and marine sediments. Determining their geographic distribution is highly relevant for improving our understanding of the recent and past ocean benthic ecosystem and establishing adequate conservation strategies. Here, we contribute to this knowledge by generating an open-access database of previously documented quantitative data of benthic foraminifera species from surface sediments of the eastern Pacific (BENFEP).
Alessio Rovere, Deirdre D. Ryan, Matteo Vacchi, Andrea Dutton, Alexander R. Simms, and Colin V. Murray-Wallace
Earth Syst. Sci. Data, 15, 1–23, https://doi.org/10.5194/essd-15-1-2023, https://doi.org/10.5194/essd-15-1-2023, 2023
Short summary
Short summary
In this work, we describe WALIS, the World Atlas of Last Interglacial Shorelines. WALIS is a sea-level database that includes sea-level proxies and samples dated to marine isotope stage 5 (~ 80 to 130 ka). The database was built through topical data compilations included in a special issue in this journal.
Yang Liu, Jingyun Zheng, Zhixin Hao, and Quansheng Ge
Earth Syst. Sci. Data, 14, 5717–5735, https://doi.org/10.5194/essd-14-5717-2022, https://doi.org/10.5194/essd-14-5717-2022, 2022
Short summary
Short summary
Proxy-based precipitation reconstruction is essential to study the inter-annual to decadal variability and underlying mechanisms beyond the instrumental period that is critical for climate modeling, prediction and attribution. We present a set of standard precipitation index reconstructions for the whole year and wet seasons over the whole of Asia since 1700, with the spatial resolution of 2.5°, based on 2912 annually resolved proxy series mainly derived from tree rings and historical documents.
Li-Li Lu, Bo-Han Jiao, Feng Qin, Gan Xie, Kai-Qing Lu, Jin-Feng Li, Bin Sun, Min Li, David K. Ferguson, Tian-Gang Gao, Yi-Feng Yao, and Yu-Fei Wang
Earth Syst. Sci. Data, 14, 3961–3995, https://doi.org/10.5194/essd-14-3961-2022, https://doi.org/10.5194/essd-14-3961-2022, 2022
Short summary
Short summary
Artemisia is one of the dominant plant elements in the arid and semi-arid regions. We attempt to decipher the underlying causes of the long-standing disagreement on the correlation between Artemisia pollen and aridity by using the dataset to recognize the different ecological implications of Artemisia pollen types. Our findings improve the resolution of palaeoenvironmental assessment and change the traditional concept of Artemisia being restricted to arid and semi-arid environments.
Michael Sigl, Matthew Toohey, Joseph R. McConnell, Jihong Cole-Dai, and Mirko Severi
Earth Syst. Sci. Data, 14, 3167–3196, https://doi.org/10.5194/essd-14-3167-2022, https://doi.org/10.5194/essd-14-3167-2022, 2022
Short summary
Short summary
Volcanism is a key driver of climate. Based on ice cores from Greenland and Antarctica, we reconstruct its climate impact potential over the Holocene. By aligning records on a well-dated chronology from Antarctica, we resolve long-standing inconsistencies in the dating of past volcanic eruptions. We reconstruct 850 eruptions (which, in total, injected 7410 Tg of sulfur in the stratosphere) and estimate how they changed the opacity of the atmosphere, a prerequisite for climate model simulations.
Kim M. Cohen, Víctor Cartelle, Robert Barnett, Freek S. Busschers, and Natasha L. M. Barlow
Earth Syst. Sci. Data, 14, 2895–2937, https://doi.org/10.5194/essd-14-2895-2022, https://doi.org/10.5194/essd-14-2895-2022, 2022
Short summary
Short summary
We describe a geological sea-level dataset for the Last Interglacial period (peaking ~125 000 years ago). From 80 known sites in and around the North Sea and English Channel (from below coastal plains, from along terraced parts of coastlines, from offshore), we provide and document 146 data points (35 entries in the Netherlands, 10 in Belgium, 23 in Germany, 17 in Denmark, 36 in Britain and the Channel Isles, 25 in France) that are also viewable at https://warmcoasts.eu/world-atlas.html.
Stefan Mulitza, Torsten Bickert, Helen C. Bostock, Cristiano M. Chiessi, Barbara Donner, Aline Govin, Naomi Harada, Enqing Huang, Heather Johnstone, Henning Kuhnert, Michael Langner, Frank Lamy, Lester Lembke-Jene, Lorraine Lisiecki, Jean Lynch-Stieglitz, Lars Max, Mahyar Mohtadi, Gesine Mollenhauer, Juan Muglia, Dirk Nürnberg, André Paul, Carsten Rühlemann, Janne Repschläger, Rajeev Saraswat, Andreas Schmittner, Elisabeth L. Sikes, Robert F. Spielhagen, and Ralf Tiedemann
Earth Syst. Sci. Data, 14, 2553–2611, https://doi.org/10.5194/essd-14-2553-2022, https://doi.org/10.5194/essd-14-2553-2022, 2022
Short summary
Short summary
Stable isotope ratios of foraminiferal shells from deep-sea sediments preserve key information on the variability of ocean circulation and ice volume. We present the first global atlas of harmonized raw downcore oxygen and carbon isotope ratios of various planktonic and benthic foraminiferal species. The atlas is a foundation for the analyses of the history of Earth system components, for finding future coring sites, and for teaching marine stratigraphy and paleoceanography.
Andrea Dutton, Alexandra Villa, and Peter M. Chutcharavan
Earth Syst. Sci. Data, 14, 2385–2399, https://doi.org/10.5194/essd-14-2385-2022, https://doi.org/10.5194/essd-14-2385-2022, 2022
Short summary
Short summary
This paper includes data that have been compiled to identify the position of sea level during a warm period about 125 000 years ago that is known as the Last Interglacial. Here, we have focused on compiling data for the region of the Bahamas, Turks and Caicos, and the east coast of Florida. These data were compiled and placed within a standardized format prescribed by a new database known as WALIS, which stands for World Atlas of Last Interglacial Shorelines Database.
Hannah M. Palmer, Veronica Padilla Vriesman, Roxanne M. W. Banker, and Jessica R. Bean
Earth Syst. Sci. Data, 14, 1695–1705, https://doi.org/10.5194/essd-14-1695-2022, https://doi.org/10.5194/essd-14-1695-2022, 2022
Short summary
Short summary
Shells of coastal marine organisms can serve as archives of past ocean and climate change. Here, we compiled a database of all available oxygen and carbon isotope values of nearshore marine molluscs from the northeast Pacific coast of North America through the Holocene including both modern collected shells and shells analyzed from midden sites. This first-of-its-kind database can be used to answer archaeological and oceanographic questions in future research.
April S. Dalton, Evan J. Gowan, Jan Mangerud, Per Möller, Juha P. Lunkka, and Valery Astakhov
Earth Syst. Sci. Data, 14, 1447–1492, https://doi.org/10.5194/essd-14-1447-2022, https://doi.org/10.5194/essd-14-1447-2022, 2022
Short summary
Short summary
The last interglacial (LIG; 130 to 115 ka) is a useful analogue for improving predictions of future changes to sea level. Here, we describe the location and characteristics of 82 LIG marine sites from the glaciated Northern Hemisphere (Russia, northern Europe, Greenland and North America). Sites are located in a variety of settings, including boreholes, riverbank exposures and along coastal cliffs.
Chenzhi Li, Alexander K. Postl, Thomas Böhmer, Xianyong Cao, Andrew M. Dolman, and Ulrike Herzschuh
Earth Syst. Sci. Data, 14, 1331–1343, https://doi.org/10.5194/essd-14-1331-2022, https://doi.org/10.5194/essd-14-1331-2022, 2022
Short summary
Short summary
Here we present a global chronology framework of 2831 palynological records, including globally harmonized chronologies covering up to 273 000 years. A comparison with the original chronologies reveals a major improvement according to our assessment. Our chronology framework and revised chronologies will interest a broad geoscientific community, as it provides the opportunity to make use in synthesis studies of, for example, pollen-based vegetation and climate change.
Tobias Erhardt, Matthias Bigler, Urs Federer, Gideon Gfeller, Daiana Leuenberger, Olivia Stowasser, Regine Röthlisberger, Simon Schüpbach, Urs Ruth, Birthe Twarloh, Anna Wegner, Kumiko Goto-Azuma, Takayuki Kuramoto, Helle A. Kjær, Paul T. Vallelonga, Marie-Louise Siggaard-Andersen, Margareta E. Hansson, Ailsa K. Benton, Louise G. Fleet, Rob Mulvaney, Elizabeth R. Thomas, Nerilie Abram, Thomas F. Stocker, and Hubertus Fischer
Earth Syst. Sci. Data, 14, 1215–1231, https://doi.org/10.5194/essd-14-1215-2022, https://doi.org/10.5194/essd-14-1215-2022, 2022
Short summary
Short summary
The datasets presented alongside this manuscript contain high-resolution concentration measurements of chemical impurities in deep ice cores, NGRIP and NEEM, from the Greenland ice sheet. The impurities originate from the deposition of aerosols to the surface of the ice sheet and are influenced by source, transport and deposition processes. Together, these records contain detailed, multi-parameter records of past climate variability over the last glacial period.
Peter K. Bijl
Earth Syst. Sci. Data, 14, 579–617, https://doi.org/10.5194/essd-14-579-2022, https://doi.org/10.5194/essd-14-579-2022, 2022
Short summary
Short summary
Using microfossils to gauge the age of rocks and sediments requires an accurate age of their first (origination) and last (extinction) appearances. But how do you know such ages can then be applied worldwide? And what causes regional differences? This paper investigates the regional consistency of ranges of species of a specific microfossil group, organic-walled dinoflagellate cysts. This overview helps in identifying regional differences in the stratigraphic ranges of species and their causes.
Kelly-Anne Lawler, Giuseppe Cortese, Matthieu Civel-Mazens, Helen Bostock, Xavier Crosta, Amy Leventer, Vikki Lowe, John Rogers, and Leanne K. Armand
Earth Syst. Sci. Data, 13, 5441–5453, https://doi.org/10.5194/essd-13-5441-2021, https://doi.org/10.5194/essd-13-5441-2021, 2021
Short summary
Short summary
Radiolarians found in marine sediments are used to reconstruct past Southern Ocean environments. This requires a comprehensive modern dataset. The Southern Ocean Radiolarian (SO-RAD) dataset includes radiolarian counts from sites in the Southern Ocean. It can be used for palaeoceanographic reconstructions or to study modern species diversity and abundance. We describe the data collection and include recommendations for users unfamiliar with procedures typically used by the radiolarian community.
Xianyong Cao, Fang Tian, Kai Li, Jian Ni, Xiaoshan Yu, Lina Liu, and Nannan Wang
Earth Syst. Sci. Data, 13, 3525–3537, https://doi.org/10.5194/essd-13-3525-2021, https://doi.org/10.5194/essd-13-3525-2021, 2021
Short summary
Short summary
The Tibetan Plateau is quite remote, and it is difficult to collect samples on it; the previous modern pollen data are located on a nearby road, and there is a large geographic gap in the eastern and central Tibetan Plateau. Our novel pollen data can fill the gap and will be valuable in establishing a complete dataset covering the entire Tibetan Plateau, thus helping us to get a comprehensive understanding. In addition, the dataset can also be used to investigate plant species distribution.
Peter M. Chutcharavan and Andrea Dutton
Earth Syst. Sci. Data, 13, 3155–3178, https://doi.org/10.5194/essd-13-3155-2021, https://doi.org/10.5194/essd-13-3155-2021, 2021
Short summary
Short summary
This paper summarizes a global database of fossil coral U-series ages for the Last Interglacial period and was compiled as a contribution to the World Atlas of Last Interglacial Shorelines. Each entry contains relevant age, elevation and sample metadata, and all ages and isotope activity ratios have been normalized and recalculated using the same decay constant values. We also provide two example geochemical screening criteria to help users assess sample age quality.
Nadine Hallmann, Gilbert Camoin, Jody M. Webster, and Marc Humblet
Earth Syst. Sci. Data, 13, 2651–2699, https://doi.org/10.5194/essd-13-2651-2021, https://doi.org/10.5194/essd-13-2651-2021, 2021
Short summary
Short summary
The last interglacial (Marine Isotope Stage 5e – MIS 5e) occurred between 128 and 116 ka when sea level was about 6–8 m above its present level; sea-level changes during this period are still debated. MIS 5e represents a potential future warm-climate analogue. This paper presents an open-access database based on the review of MIS 5e coral reef records from many tropical Pacific islands. Overall, the database contains 318 age data points and 94 relative sea-level data points from 38 studies.
Oana A. Dumitru, Victor J. Polyak, Yemane Asmerom, and Bogdan P. Onac
Earth Syst. Sci. Data, 13, 2077–2094, https://doi.org/10.5194/essd-13-2077-2021, https://doi.org/10.5194/essd-13-2077-2021, 2021
Short summary
Short summary
Here we describe a global database that summarizes the current knowledge of MIS 5 sea level as captured by speleothems. We used the framework of the WALIS database to provide a standardized format which will facilitate the sea-level research community to utilize this worldwide database. This is the first speleothem database and contains all the information needed to assess former paleo relative sea levels and their chronological constraints.
Patrick Boyden, Jennifer Weil-Accardo, Pierre Deschamps, Davide Oppo, and Alessio Rovere
Earth Syst. Sci. Data, 13, 1633–1651, https://doi.org/10.5194/essd-13-1633-2021, https://doi.org/10.5194/essd-13-1633-2021, 2021
Short summary
Short summary
Sea levels during the last interglacial (130 to 73 ka) are seen as possible process analogs for future sea-level-rise scenarios as our world warms. To this end we catalog previously published ancient shoreline elevations and chronologies in a standardized data format for East Africa and the Western Indian Ocean region. These entries were then contributed to the greater World Atlas of Last Interglacial Shorelines database.
Cody C. Routson, Darrell S. Kaufman, Nicholas P. McKay, Michael P. Erb, Stéphanie H. Arcusa, Kendrick J. Brown, Matthew E. Kirby, Jeremiah P. Marsicek, R. Scott Anderson, Gonzalo Jiménez-Moreno, Jessica R. Rodysill, Matthew S. Lachniet, Sherilyn C. Fritz, Joseph R. Bennett, Michelle F. Goman, Sarah E. Metcalfe, Jennifer M. Galloway, Gerrit Schoups, David B. Wahl, Jesse L. Morris, Francisca Staines-Urías, Andria Dawson, Bryan N. Shuman, Daniel G. Gavin, Jeffrey S. Munroe, and Brian F. Cumming
Earth Syst. Sci. Data, 13, 1613–1632, https://doi.org/10.5194/essd-13-1613-2021, https://doi.org/10.5194/essd-13-1613-2021, 2021
Short summary
Short summary
We present a curated database of western North American Holocene paleoclimate records, which have been screened on length, resolution, and geochronology. The database gathers paleoclimate time series that reflect temperature, hydroclimate, or circulation features from terrestrial and marine sites, spanning a region from Mexico to Alaska. This publicly accessible collection will facilitate a broad range of paleoclimate inquiry.
Evan Tam and Yusuke Yokoyama
Earth Syst. Sci. Data, 13, 1477–1497, https://doi.org/10.5194/essd-13-1477-2021, https://doi.org/10.5194/essd-13-1477-2021, 2021
Short summary
Short summary
Changes in sea level during Marine Isotope Stage (MIS) 5e are comparable to modern sea levels in our global climate. Contributing to the World Atlas of Last Interglacial Shorelines (WALIS), this paper reviewed data from over 70 studies detailing sea-level markers for MIS 5e around Japan. Most sea-level markers were found as marine terraces and are often dated by comparison to dated volcanic ash or sediment layers, which has connected Japan’s landforms to global patterns of sea-level change.
Evan J. Gowan, Alessio Rovere, Deirdre D. Ryan, Sebastian Richiano, Alejandro Montes, Marta Pappalardo, and Marina L. Aguirre
Earth Syst. Sci. Data, 13, 171–197, https://doi.org/10.5194/essd-13-171-2021, https://doi.org/10.5194/essd-13-171-2021, 2021
Short summary
Short summary
During the last interglacial (130 to 115 ka), global sea level was higher than present. The World Atlas of Last Interglacial Shorelines (WALIS) has been created to document this. In this paper, we have compiled data for southeastern South America. There are landforms that indicate that sea level was 5 to 25 m higher than present during this time period. However, the quality of these data is hampered by limitations on elevation measurements, chronology, and geological descriptions.
Mareike Wieczorek and Ulrike Herzschuh
Earth Syst. Sci. Data, 12, 3515–3528, https://doi.org/10.5194/essd-12-3515-2020, https://doi.org/10.5194/essd-12-3515-2020, 2020
Short summary
Short summary
Relative pollen productivity (RPP) estimates are used to estimate vegetation cover from pollen records. This study provides (i) a compilation of northern hemispheric RPP studies, allowing researchers to identify suitable sets for their study region and to identify data gaps for future research, and (ii) taxonomically harmonized, unified RPP sets for China, Europe, North America, and the whole Northern Hemisphere, generated from the available studies.
Chris S. M. Turney, Richard T. Jones, Nicholas P. McKay, Erik van Sebille, Zoë A. Thomas, Claus-Dieter Hillenbrand, and Christopher J. Fogwill
Earth Syst. Sci. Data, 12, 3341–3356, https://doi.org/10.5194/essd-12-3341-2020, https://doi.org/10.5194/essd-12-3341-2020, 2020
Short summary
Short summary
The Last Interglacial (129–116 ka) experienced global temperatures and sea levels higher than today. The direct contribution of warmer conditions to global sea level (thermosteric) are uncertain. We report a global network of sea surface temperatures. We find mean global annual temperature anomalies of 0.2 ± 0.1˚C and an early maximum peak of 0.9 ± 0.1˚C. Our reconstruction suggests warmer waters contributed on average 0.08 ± 0.1 m and a peak contribution of 0.39 ± 0.1 m to global sea level.
Laia Comas-Bru, Kira Rehfeld, Carla Roesch, Sahar Amirnezhad-Mozhdehi, Sandy P. Harrison, Kamolphat Atsawawaranunt, Syed Masood Ahmad, Yassine Ait Brahim, Andy Baker, Matthew Bosomworth, Sebastian F. M. Breitenbach, Yuval Burstyn, Andrea Columbu, Michael Deininger, Attila Demény, Bronwyn Dixon, Jens Fohlmeister, István Gábor Hatvani, Jun Hu, Nikita Kaushal, Zoltán Kern, Inga Labuhn, Franziska A. Lechleitner, Andrew Lorrey, Belen Martrat, Valdir Felipe Novello, Jessica Oster, Carlos Pérez-Mejías, Denis Scholz, Nick Scroxton, Nitesh Sinha, Brittany Marie Ward, Sophie Warken, Haiwei Zhang, and SISAL Working Group members
Earth Syst. Sci. Data, 12, 2579–2606, https://doi.org/10.5194/essd-12-2579-2020, https://doi.org/10.5194/essd-12-2579-2020, 2020
Short summary
Short summary
This paper presents an updated version of the SISAL (Speleothem Isotope Synthesis and Analysis) database. This new version contains isotopic data from 691 speleothem records from 294 cave sites and new age–depth models, including their uncertainties, for 512 speleothems.
Basil A. S. Davis, Manuel Chevalier, Philipp Sommer, Vachel A. Carter, Walter Finsinger, Achille Mauri, Leanne N. Phelps, Marco Zanon, Roman Abegglen, Christine M. Åkesson, Francisca Alba-Sánchez, R. Scott Anderson, Tatiana G. Antipina, Juliana R. Atanassova, Ruth Beer, Nina I. Belyanina, Tatiana A. Blyakharchuk, Olga K. Borisova, Elissaveta Bozilova, Galina Bukreeva, M. Jane Bunting, Eleonora Clò, Daniele Colombaroli, Nathalie Combourieu-Nebout, Stéphanie Desprat, Federico Di Rita, Morteza Djamali, Kevin J. Edwards, Patricia L. Fall, Angelica Feurdean, William Fletcher, Assunta Florenzano, Giulia Furlanetto, Emna Gaceur, Arsenii T. Galimov, Mariusz Gałka, Iria García-Moreiras, Thomas Giesecke, Roxana Grindean, Maria A. Guido, Irina G. Gvozdeva, Ulrike Herzschuh, Kari L. Hjelle, Sergey Ivanov, Susanne Jahns, Vlasta Jankovska, Gonzalo Jiménez-Moreno, Monika Karpińska-Kołaczek, Ikuko Kitaba, Piotr Kołaczek, Elena G. Lapteva, Małgorzata Latałowa, Vincent Lebreton, Suzanne Leroy, Michelle Leydet, Darya A. Lopatina, José Antonio López-Sáez, André F. Lotter, Donatella Magri, Elena Marinova, Isabelle Matthias, Anastasia Mavridou, Anna Maria Mercuri, Jose Manuel Mesa-Fernández, Yuri A. Mikishin, Krystyna Milecka, Carlo Montanari, César Morales-Molino, Almut Mrotzek, Castor Muñoz Sobrino, Olga D. Naidina, Takeshi Nakagawa, Anne Birgitte Nielsen, Elena Y. Novenko, Sampson Panajiotidis, Nata K. Panova, Maria Papadopoulou, Heather S. Pardoe, Anna Pędziszewska, Tatiana I. Petrenko, María J. Ramos-Román, Cesare Ravazzi, Manfred Rösch, Natalia Ryabogina, Silvia Sabariego Ruiz, J. Sakari Salonen, Tatyana V. Sapelko, James E. Schofield, Heikki Seppä, Lyudmila Shumilovskikh, Normunds Stivrins, Philipp Stojakowits, Helena Svobodova Svitavska, Joanna Święta-Musznicka, Ioan Tantau, Willy Tinner, Kazimierz Tobolski, Spassimir Tonkov, Margarita Tsakiridou, Verushka Valsecchi, Oksana G. Zanina, and Marcelina Zimny
Earth Syst. Sci. Data, 12, 2423–2445, https://doi.org/10.5194/essd-12-2423-2020, https://doi.org/10.5194/essd-12-2423-2020, 2020
Short summary
Short summary
The Eurasian Modern Pollen Database (EMPD) contains pollen counts and associated metadata for 8134 modern pollen samples from across the Eurasian region. The EMPD is part of, and complementary to, the European Pollen Database (EPD) which contains data on fossil pollen found in Late Quaternary sedimentary archives. The purpose of the EMPD is to provide calibration datasets and other data to support palaeoecological research on past climates and vegetation cover over the Quaternary period.
Arne Ramisch, Alexander Brauser, Mario Dorn, Cecile Blanchet, Brian Brademann, Matthias Köppl, Jens Mingram, Ina Neugebauer, Norbert Nowaczyk, Florian Ott, Sylvia Pinkerneil, Birgit Plessen, Markus J. Schwab, Rik Tjallingii, and Achim Brauer
Earth Syst. Sci. Data, 12, 2311–2332, https://doi.org/10.5194/essd-12-2311-2020, https://doi.org/10.5194/essd-12-2311-2020, 2020
Short summary
Short summary
Annually laminated lake sediments (varves) record past climate change at seasonal resolution. The VARved sediments DAtabase (VARDA) is created to utilize the full potential of varves for climate reconstructions. VARDA offers free access to a compilation and synchronization of standardized climate-proxy data, with applications ranging from reconstructing regional patterns of past climate change to validating simulations of climate models. VARDA is freely accessible at https://varve.gfz-potsdam.de
Bronwen L. Konecky, Nicholas P. McKay, Olga V. Churakova (Sidorova), Laia Comas-Bru, Emilie P. Dassié, Kristine L. DeLong, Georgina M. Falster, Matt J. Fischer, Matthew D. Jones, Lukas Jonkers, Darrell S. Kaufman, Guillaume Leduc, Shreyas R. Managave, Belen Martrat, Thomas Opel, Anais J. Orsi, Judson W. Partin, Hussein R. Sayani, Elizabeth K. Thomas, Diane M. Thompson, Jonathan J. Tyler, Nerilie J. Abram, Alyssa R. Atwood, Olivier Cartapanis, Jessica L. Conroy, Mark A. Curran, Sylvia G. Dee, Michael Deininger, Dmitry V. Divine, Zoltán Kern, Trevor J. Porter, Samantha L. Stevenson, Lucien von Gunten, and Iso2k Project Members
Earth Syst. Sci. Data, 12, 2261–2288, https://doi.org/10.5194/essd-12-2261-2020, https://doi.org/10.5194/essd-12-2261-2020, 2020
Lukas Jonkers, Olivier Cartapanis, Michael Langner, Nick McKay, Stefan Mulitza, Anne Strack, and Michal Kucera
Earth Syst. Sci. Data, 12, 1053–1081, https://doi.org/10.5194/essd-12-1053-2020, https://doi.org/10.5194/essd-12-1053-2020, 2020
Oliver Bothe, Sebastian Wagner, and Eduardo Zorita
Earth Syst. Sci. Data, 11, 1129–1152, https://doi.org/10.5194/essd-11-1129-2019, https://doi.org/10.5194/essd-11-1129-2019, 2019
Short summary
Short summary
Reconstructions try to extract a climate signal from paleo-observations. It is essential to understand their uncertainties. Similarly, comparing climate simulations and paleo-observations requires approaches to address their uncertainties. We describe a simple but flexible noise model for climate proxies for temperature on millennial timescales, which can assist these goals.
István Gábor Hatvani, Zoltán Kern, Szabolcs Leél-Őssy, and Attila Demény
Earth Syst. Sci. Data, 10, 139–149, https://doi.org/10.5194/essd-10-139-2018, https://doi.org/10.5194/essd-10-139-2018, 2018
Short summary
Short summary
Evenly spaced carbon and oxygen stable isotope records were produced from central European stalagmites. To mitigate the potential bias of interpolation, the variance spectra were carefully evaluated. The derived data are ready to use with conventional uni- and multivariate statistics, which are usually not prepared to handle the general characteristic of sedimentary paleoclimate records derived from geological sequences unevenly sampled in time.
Marisa Borreggine, Sarah E. Myhre, K. Allison S. Mislan, Curtis Deutsch, and Catherine V. Davis
Earth Syst. Sci. Data, 9, 739–749, https://doi.org/10.5194/essd-9-739-2017, https://doi.org/10.5194/essd-9-739-2017, 2017
Short summary
Short summary
We created a database of 2134 marine sediment cores above 30° N in the North Pacific from 1951 to 2016 to facilitate paleoceanographic and paleoclimate research. This database allows for accessibility to sedimentary sequences, age models, and proxies produced in the North Pacific. We found community-wide shifts towards multiproxy investigation and increased age model generation. The database consolidates the research efforts of an entire community into an efficient tool for future investigations.
María Fernanda Sánchez Goñi, Stéphanie Desprat, Anne-Laure Daniau, Frank C. Bassinot, Josué M. Polanco-Martínez, Sandy P. Harrison, Judy R. M. Allen, R. Scott Anderson, Hermann Behling, Raymonde Bonnefille, Francesc Burjachs, José S. Carrión, Rachid Cheddadi, James S. Clark, Nathalie Combourieu-Nebout, Colin. J. Courtney Mustaphi, Georg H. Debusk, Lydie M. Dupont, Jemma M. Finch, William J. Fletcher, Marco Giardini, Catalina González, William D. Gosling, Laurie D. Grigg, Eric C. Grimm, Ryoma Hayashi, Karin Helmens, Linda E. Heusser, Trevor Hill, Geoffrey Hope, Brian Huntley, Yaeko Igarashi, Tomohisa Irino, Bonnie Jacobs, Gonzalo Jiménez-Moreno, Sayuri Kawai, A. Peter Kershaw, Fujio Kumon, Ian T. Lawson, Marie-Pierre Ledru, Anne-Marie Lézine, Ping Mei Liew, Donatella Magri, Robert Marchant, Vasiliki Margari, Francis E. Mayle, G. Merna McKenzie, Patrick Moss, Stefanie Müller, Ulrich C. Müller, Filipa Naughton, Rewi M. Newnham, Tadamichi Oba, Ramón Pérez-Obiol, Roberta Pini, Cesare Ravazzi, Katy H. Roucoux, Stephen M. Rucina, Louis Scott, Hikaru Takahara, Polichronis C. Tzedakis, Dunia H. Urrego, Bas van Geel, B. Guido Valencia, Marcus J. Vandergoes, Annie Vincens, Cathy L. Whitlock, Debra A. Willard, and Masanobu Yamamoto
Earth Syst. Sci. Data, 9, 679–695, https://doi.org/10.5194/essd-9-679-2017, https://doi.org/10.5194/essd-9-679-2017, 2017
Short summary
Short summary
The ACER (Abrupt Climate Changes and Environmental Responses) global database includes 93 pollen records from the last glacial period (73–15 ka) plotted against a common chronology; 32 also provide charcoal records. The database allows for the reconstruction of the regional expression, vegetation and fire of past abrupt climate changes that are comparable to those expected in the 21st century. This work is a major contribution to understanding the processes behind rapid climate change.
Peter Köhler, Christoph Nehrbass-Ahles, Jochen Schmitt, Thomas F. Stocker, and Hubertus Fischer
Earth Syst. Sci. Data, 9, 363–387, https://doi.org/10.5194/essd-9-363-2017, https://doi.org/10.5194/essd-9-363-2017, 2017
Short summary
Short summary
We document our best available data compilation of published ice core records of the greenhouse gases CO2, CH4, and N2O and recent measurements on firn air and atmospheric samples covering the time window from 156 000 years BP to the beginning of the year 2016 CE. A smoothing spline method is applied to translate the discrete and irregularly spaced data points into continuous time series. The radiative forcing for each greenhouse gas is computed using well-established, simple formulations.
Cited articles
Affek, H. P., Matthews, A., Ayalon, A., Bar-Matthews, M., Burstyn, Y.,
Zaarur, S., and Zilberman, T.: Accounting for kinetic isotope effects in
Soreq Cave (Israel) speleothems, Geochim. Cosmochim. Acta, 143, 303–318,
https://doi.org/10.1016/j.gca.2014.08.008, 2014.
Aharon, P., Aldridge, D., and Hellstrom, J.: Rainfall Variability and the
Rise and Collapse of the Mississippian Chiefdoms: Evidence From a Desoto
Caverns Stalagmite, in: Climates, Landscapes, and Civilizations,
American Geophysical Union, 35–42, 2013.
Ait Brahim, Y., Cheng, H., Sifeddine, A., Wassenburg, J. A., Cruz, F. W.,
Khodri, M., Sha, L., Pérez-Zanón, N., Beraaouz, E. H.,
Apaéstegui, J., Guyot, J.-L., Jochum, K. P., and Bouchaou, L.: Speleothem
records decadal to multidecadal hydroclimate variations in southwestern
Morocco during the last millennium, Earth Planet. Sci. Lett., 476, 1–10,
https://doi.org/10.1016/j.epsl.2017.07.045, 2017.
Akers, P. D., Brook, G. A., Railsback, L. B., Liang, F., Iannone, G.,
Webster, J. W., Reeder, P. P., Cheng, H., and Edwards, R. L.: An extended and
higher-resolution record of climate and land use from stalagmite MC01 from
Macal Chasm, Belize, revealing connections between major dry events, overall
climate variability, and Maya sociopolitical changes, Palaeogeogr.
Palaeocl., 459, 268–288,
https://doi.org/10.1016/j.palaeo.2016.07.007, 2016.
Apaéstegui, J., Cruz, F. W., Sifeddine, A., Vuille, M., Espinoza, J. C.,
Guyot, J. L., Khodri, M., Strikis, N., Santos, R. V., Cheng, H., Edwards, L.,
Carvalho, E., and Santini, W.: Hydroclimate variability of the northwestern
Amazon Basin near the Andean foothills of Peru related to the South American
Monsoon System during the last 1600 years, Clim. Past, 10, 1967–1981,
https://doi.org/10.5194/cp-10-1967-2014, 2014.
Arienzo, M. M., Swart, P. K., Pourmand, A., Broad, K., Clement, A. C.,
Murphy, L. N., Vonhof, H. B., and Kakuk, B.: Bahamian speleothem reveals
temperature decrease associated with Heinrich stadials, Earth Planet. Sci.
Lett., 430, 377–386, https://doi.org/10.1016/j.epsl.2015.08.035, 2015.
Arienzo, M. M., Swart, P. K., Broad, K., Clement, A. C., Pourmand, A. and
Kakuk, B.: Multi-proxy evidence of millennial climate variability from
multiple Bahamian speleothems, Quaternary Sci. Rev., 161, 18–29,
https://doi.org/10.1016/j.quascirev.2017.02.004, 2017.
Asmerom, Y., Polyak, V. J., and Burns, S. J.: Variable winter moisture in the
southwestern United States linked to rapid glacial climate shifts, Nat.
Geosci., 3, 114–117, https://doi.org/10.1038/ngeo754, 2010.
Asrat, A., Baker, A., Mohammed, M. U., Leng, M. J., Van Calsteren, P., and
Smith, C.: A high-resolution multi-proxy stalagmite record from Mechara,
Southeastern Ethiopia: palaeohydrological implications for speleothem
palaeoclimate reconstruction, J. Quaternary Sci., 22, 53–63,
https://doi.org/10.1002/jqs.1013, 2006.
Asrat, A., Baker, A., Leng, M., Gunn, J., and Umer, M.: Environmental
monitoring in the Mechara caves, Southeastern Ethiopia: implications for
speleothem palaeoclimate studies, Int. J. Speleol., 37, 207–220,
https://doi.org/10.5038/1827-806x.37.3.5, 2008.
Atkinson, T. C. and Hopley, P. J.: Speleothems and Palaeoclimates, chap. 5, in: Caves and Karst of the Yorkshire
Dales, esite by: Waltham, T. and Lowe, D., British Cave Research Association, Buxton, 181–186,
2013.
Atsawawaranunt, K., Harrison, S. P., and Comas-Bru, L.: SISAL (Speleothem Isotopes
Synthesis and AnaLysis Working Group) database Version 1.0, University of Reading, Dataset,
https://doi.org/10.17864/1947.147, last access: 4 September 2018.
Ayliffe, L. K., Marianelli, P. C., Moriarty, K. C., Wells, R. T., McCulloch,
M. T., Mortimer, G. E., and Hellstrom, J. C.: 500 ka precipitation record
from southeastern Australia: Evidence for interglacial relative aridity,
Geology, 26, 147–150, https://doi.org/10.1130/0091-7613(1998)026<0147:KPRFSA>2.3.CO;2,
1998.
Ayliffe, L. K., Gagan, M. K., Zhao, J., Drysdale, R. N., Hellstrom, J. C.,
Hantoro, W. S., Griffiths, M. L., Scott-Gagan, H., Pierre, E. S., Cowley, J.
A., and Suwargadi, B. W.: Rapid interhemispheric climate links via the
Australasian monsoon during the last deglaciation, Nat. Commun., 4, 2908,
https://doi.org/10.1038/ncomms3908, 2013.
Bajo, P., Hellstrom, J., Frisia, S., Drysdale, R., Black, J., Woodhead, J.,
Borsato, A., Zanchetta, G., Wallace, M. W., Regattieri, E., and Haese, R.:
“Cryptic” diagenesis and its implications for speleothem geochronologies,
Quaternary Sci. Rev., 148, 17–28, https://doi.org/10.1016/j.quascirev.2016.06.020, 2016.
Baker, A., Ito, E., Smart, P. L., and McEwan, R. F.: Elevated and variable
values of 13C in speleothems in a British cave system, Chem. Geol., 136,
263–270, https://doi.org/10.1016/S0009-2541(96)00129-5, 1997.
Baker, A., Asrat, A., Fairchild, I. J., Leng, M. J., Wynn, P. M., Bryant, C.,
Genty, D., and Umer, M.: Analysis of the climate signal contained within
δ18O and growth rate parameters in two Ethiopian stalagmites,
Geochim. Cosmochim. Acta, 71, 2975–2988, https://doi.org/10.1016/j.gca.2007.03.029,
2007.
Baker, A., Asrat, A., Fairchild, I. J., Leng, M. J., Thomas, L., Widmann, M.,
Jex, C. N., Dong, B., van Calsteren, P., and Bryant, C.: Decadal-scale
rainfall variability in Ethiopia recorded in an annually laminated,
Holocene-age, stalagmite, The Holocene, 20, 827–836,
https://doi.org/10.1177/0959683610365934, 2010.
Baker, A., Wilson, R., Fairchild, I. J., Franke, J., Spötl, C., Mattey,
D., Trouet, V., and Fuller, L.: High resolution δ18O and δ13C records from an annually laminated Scottish stalagmite and
relationship with last millennium climate, Global Planet. Change, 79,
303–311, https://doi.org/10.1016/j.gloplacha.2010.12.007, 2011.
Baker, A., Bradley, C., Phipps, S. J., Fischer, M., Fairchild, I. J., Fuller,
L., Spötl, C., and Azcurra, C.: Millennial-length forward models and
pseudoproxies of stalagmite δ18O: an example from NW Scotland,
Clim. Past, 8, 1153–1167, https://doi.org/10.5194/cp-8-1153-2012, 2012.
Baker, J. L., Lachniet, M. S., Chervyatsova, O., Asmerom, Y., and Polyak, V.
J.: Holocene warming in western continental Eurasia driven by glacial retreat
and greenhouse forcing, Nat. Geosci., 10, 430–435, https://doi.org/10.1038/ngeo2953,
2017.
Baldini, J., McDermott, F., Baker, A., Baldini, L., Mattey, D., and
Railsback, L.: Biomass effects on stalagmite growth and isotope ratios: A
20th century analogue from Wiltshire, England, Earth Planet. Sci. Lett., 240,
486–494, https://doi.org/10.1016/j.epsl.2005.09.022, 2005.
Baldini, J. U. L.: Morphologic and dimensional linkage between recently
deposited speleothems and drip water from Browns Folly Mine, Wiltshire,
England, J. Cave Karst Stud., 63, 83–90, available at:
https://caves.org/pub/journal/PDF/V63/cave_63-03-fullr.pdf (last access: 30 May 2018), 2001.
Baldini, J. U. L., McDermott, F., Hoffmann, D. L., Richards, D. A., and
Clipson, N.: Very high-frequency and seasonal cave atmosphere P
Bar-Matthews, M., Ayalon, A., Kaufman, A. and Wasserburg, G. J.: The Eastern
Mediterranean paleoclimate as a reflection of regional events: Soreq cave,
Israel, Earth Planet. Sci. Lett., 166, 85–95,
https://doi.org/10.1016/S0012-821X(98)00275-1, 1999.
Bartolomé, M., Moreno, A., Sancho, C., Stoll, H. M., Cacho, I.,
Spötl, C., Belmonte, Á., Edwards, R. L., Cheng, H., and Hellstrom, J.
C.: Hydrological change in Southern Europe responding to increasing North
Atlantic overturning during Greenland Stadial 1, P. Natl. Acad. Sci. USA,
112, 6568–6572, https://doi.org/10.1073/pnas.1503990112, 2015.
Berkelhammer, M., Sinha, A., Mudelsee, M., Cheng, H., Edwards, R. L., and
Cannariato, K.: Persistent multidecadal power of the Indian Summer Monsoon,
Earth Planet. Sci. Lett., 290, 166–172, https://doi.org/10.1016/j.epsl.2009.12.017,
2010.
Berkelhammer, M., Sinha, A., Stott, L., Cheng, H., Pausata, F. S. R., and
Yoshimura, K.: An Abrupt Shift in the Indian Monsoon 4000 Years Ago, in:
Climates, Landscapes, and Civilizations, American Geophysical Union, 75–88,
2013.
Bernal, J. P., Lachniet, M., McCulloch, M., Mortimer, G., Morales, P., and
Cienfuegos, E.: A speleothem record of Holocene climate variability from
southwestern Mexico, Quaternary Res., 75, 104–113,
https://doi.org/10.1016/j.yqres.2010.09.002, 2011.
Bernal, J. P., Cruz, F. W., Stríkis, N. M., Wang, X., Deininger, M.,
Catunda, M. C. A., Ortega-Obregón, C., Cheng, H., Edwards, R. L., and
Auler, A. S.: High-resolution Holocene South American monsoon history
recorded by a speleothem from Botuverá Cave, Brazil, Earth Planet. Sci.
Lett., 450, 186–196, https://doi.org/10.1016/j.epsl.2016.06.008, 2016.
Boch, R. and Spötl, C.: Reconstructing palaeoprecipitation from an active
cave flowstone, J. Quaternary Sci., 26, 675–687, https://doi.org/10.1002/jqs.1490, 2011.
Boch, R., Spötl, C., and Kramers, J.: High-resolution isotope records of
early Holocene rapid climate change from two coeval stalagmites of Katerloch
Cave, Austria, Quaternary Sci. Rev., 28, 2527–2538,
https://doi.org/10.1016/j.quascirev.2009.05.015, 2009.
Boch, R., Cheng, H., Spötl, C., Edwards, R. L., Wang, X., and
Häuselmann, Ph.: NALPS: a precisely dated European climate record
120–60 ka, Clim. Past, 7, 1247–1259,
https://doi.org/10.5194/cp-7-1247-2011, 2011.
Bolliet, T., Brockmann, P., Masson-Delmotte, V., Bassinot, F., Daux, V.,
Genty, D., Landais, A., Lavrieux, M., Michel, E., Ortega, P., Risi, C.,
Roche, D. M., Vimeux, F., and Waelbroeck, C.: Water and carbon stable isotope
records from natural archives: a new database and interactive online platform
for data browsing, visualizing and downloading, Clim. Past, 12, 1693–1719,
https://doi.org/10.5194/cp-12-1693-2016, 2016.
Bowen, G. J. and Wilkinson, B.: Spatial distribution of δ18O in
meteoric precipitation, Geology, 30, 315–318,
https://doi.org/10.1130/0091-7613(2002)030<0315:SDOOIM>2.0.CO;2, 2002.
Bradley, R. S.: Paleoclimatology: Reconstructing Climates of the Quaternary,
3rd edn., Academic Press, https://doi.org/10.1016/C2009-0-18310-1, 2015.
Breitenbach, S. F. M., Rehfeld, K., Goswami, B., Baldini, J. U. L., Ridley,
H. E., Kennett, D. J., Prufer, K. M., Aquino, V. V., Asmerom, Y., Polyak, V.
J., Cheng, H., Kurths, J., and Marwan, N.: COnstructing Proxy Records from
Age models (COPRA), Clim. Past, 8, 1765–1779,
https://doi.org/10.5194/cp-8-1765-2012, 2012.
Breitenbach, S. F. M., Lechleitner, F. A., Meyer, H., Diengdoh, G., Mattey,
D., and Marwan, N.: Cave ventilation and rainfall signals in dripwater in a
monsoonal setting – a monitoring study from NE India, Chem. Geol., 402,
111–124, https://doi.org/10.1016/j.chemgeo.2015.03.011, 2015.
Bronk Ramsey, C.: Radiocarbon Calibration and Analysis of Stratigraphy: The
OxCal Program, Radiocarbon, 37, 425–430, https://doi.org/10.1017/S0033822200030903,
1995.
Bronk Ramsey, C.: Development of the Radiocarbon Calibration Program,
Radiocarbon, 43, 355–363, https://doi.org/10.1017/S0033822200038212, 2001.
Bronk Ramsey, C.: Deposition models for chronological records, Quaternary
Sci. Rev., 27, 42–60, https://doi.org/10.1016/j.quascirev.2007.01.019, 2008.
Burns, S. J.: A 780-year annually resolved record of Indian Ocean monsoon
precipitation from a speleothem from south Oman, J. Geophys. Res., 107, 4434,
https://doi.org/10.1029/2001jd001281, 2002.
Burns, S. J., Godfrey, L. R., Faina, P., McGee, D., Hardt, B.,
Ranivoharimanana, L., and Randrianasy, J.: Rapid human-induced landscape
transformation in Madagascar at the end of the first millennium of the Common
Era, Quaternary Sci. Rev., 134, 92–99, https://doi.org/10.1016/j.quascirev.2016.01.007,
2016.
Cai, Y., Cheng, H., An, Z., Edwards, R. L., Wang, X., Tan, L., and Wang, J.:
Large variations of oxygen isotopes in precipitation over south-central Tibet
during Marine Isotope Stage 5, Geology, 38, 243–246, https://doi.org/10.1130/g30306.1,
2010a.
Cai, Y., Tan, L., Cheng, H., An, Z., Edwards, R. L., Kelly, M. J., Kong, X.,
and Wang, X.: The variation of summer monsoon precipitation in central China
since the last deglaciation, Earth Planet. Sci. Lett., 291, 21–31,
https://doi.org/10.1016/j.epsl.2009.12.039, 2010b.
Cai, Y., Zhang, H., Cheng, H., An, Z., Lawrence Edwards, R., Wang, X., Tan,
L., Liang, F., Wang, J., Kelly, M., Edwards, R. L., Wang, X., Tan, L., Liang,
F., Wang, J., and Kelly, M.: The Holocene Indian monsoon variability over the
southern Tibetan Plateau and its teleconnections, Earth Planet. Sci. Lett.,
335–336, 135–144, https://doi.org/10.1016/j.epsl.2012.04.035, 2012.
Cai, Y., Fung, I. Y., Edwards, R. L., An, Z., Cheng, H., Lee, J.-E., Tan, L.,
Shen, C.-C., Wang, X., Day, J. A., Zhou, W., Kelly, M. J., and Chiang, J. C.
H.: Variability of stalagmite-inferred Indian monsoon precipitation over the
past 252,000 y, P. Natl. Acad. Sci. USA, 112, 2954–2959,
https://doi.org/10.1073/pnas.1424035112, 2015.
Caley, T., Roche, D. M., Waelbroeck, C., and Michel, E.: Oxygen stable
isotopes during the Last Glacial Maximum climate: perspectives from
data–model (iLOVECLIM) comparison, Clim. Past, 10, 1939–1955,
https://doi.org/10.5194/cp-10-1939-2014, 2014.
Carolin, S. A., Cobb, K. M., Adkins, J. F., Clark, B., Conroy, J. L., Lejau,
S., Malang, J., and Tuen, A. A.: Varied Response of Western Pacific Hydrology
to Climate Forcings over the Last Glacial Period, Science, 340, 1564–1566,
https://doi.org/10.1126/science.1233797, 2013.
Carolin, S. A., Cobb, K. M., Lynch-Stieglitz, J., Moerman, J. W., Partin, J.
W., Lejau, S., Malang, J., Clark, B., Tuen, A. A., and Adkins, J. F.:
Northern Borneo stalagmite records reveal West Pacific hydroclimate across
MIS 5 and 6, Earth Planet. Sci. Lett., 439, 182–193,
https://doi.org/10.1016/j.epsl.2016.01.028, 2016.
Chen, S., Hoffmann, S. S., Lund, D. C., Cobb, K. M., Emile-Geay, J., and
Adkins, J. F.: A high-resolution speleothem record of western equatorial
Pacific rainfall: Implications for Holocene ENSO evolution, Earth Planet.
Sci. Lett., 442, 61–71, https://doi.org/10.1016/j.epsl.2016.02.050, 2016.
Cheng, H., Edwards, R., Hoff, J., Gallup, C., Richards, D., and Asmerom, Y.:
The half-lives of uranium-234 and thorium-230, Chem. Geol., 169, 17–33,
https://doi.org/10.1016/S0009-2541(99)00157-6, 2000.
Cheng, H., Zhang, P. Z., Spötl, C., Edwards, R. L., Cai, Y. J., Zhang, D.
Z., Sang, W. C., Tan, M., and An, Z. S.: The climatic cyclicity in
semiarid-arid central Asia over the past 500,000 years, Geophys. Res. Lett.,
39, L01705, https://doi.org/10.1029/2011GL050202, 2012.
Cheng, H., Lawrence Edwards, R., Shen, C.-C., Polyak, V. J., Asmerom, Y.,
Woodhead, J., Hellstrom, J., Wang, Y., Kong, X., Spötl, C., Wang, X., and
Calvin Alexander, E.: Improvements in 230Th dating, 230Th and
234U half-life values, and U–Th isotopic measurements by
multi-collector inductively coupled plasma mass spectrometry, Earth Planet.
Sci. Lett., 371–372, 82–91, https://doi.org/10.1016/j.epsl.2013.04.006, 2013.
Cheng, H., Sinha, A., Verheyden, S., Nader, F. H., Li, X. L., Zhang, P. Z.,
Yin, J. J., Yi, L., Peng, Y. B., Rao, Z. G., Ning, Y. F., and Edwards, R. L.:
The climate variability in northern Levant over the past 20,000 years,
Geophys. Res. Lett., 42, 8641–8650, https://doi.org/10.1002/2015GL065397, 2015.
Cheng, H., Spötl, C., Breitenbach, S. F. M., Sinha, A., Wassenburg, J.
A., Jochum, K. P., Scholz, D., Li, X., Yi, L., Peng, Y., Lv, Y., Zhang, P.,
Votintseva, A., Loginov, V., Ning, Y., Kathayat, G., and Edwards, R. L.:
Climate variations of Central Asia on orbital to millennial timescales, Sci.
Rep., 6, 36975, https://doi.org/10.1038/srep36975, 2016a.
Cheng, H., Edwards, R. L., Sinha, A., Spötl, C., Yi, L., Chen, S., Kelly,
M., Kathayat, G., Wang, X., Li, X., Kong, X., Wang, Y., Ning, Y., and Zhang,
H.: The Asian monsoon over the past 640,000 years and ice age terminations,
Nature, 534, 640–646, https://doi.org/10.1038/nature18591, 2016b.
Cobb, K. M., Adkins, J. F., Partin, J. W., and Clark, B.: Regional-scale
climate influences on temporal variations of rainwater and cave dripwater
oxygen isotopes in northern Borneo, Earth Planet. Sci. Lett., 263, 207–220,
https://doi.org/10.1016/j.epsl.2007.08.024, 2007.
Cohen, K. M., Finney, S., and Gibbard, P. L.: International
Chronostratigraphic Chart, Int. Comm. Stratigr., available at:
http://www.stratigraphy.org (last access: 30 May 2018), 2015.
Columbu, A., Drysdale, R., Capron, E., Woodhead, J., Waele, J. De, Sanna, L.,
Hellstrom, J., and Bajo, P.: Early last glacial intra-interstadial climate
variability recorded in a Sardinian speleothem, Quaternary Sci. Rev., 169,
391–397, https://doi.org/10.1016/j.quascirev.2017.05.007, 2017.
Couchoud, I., Genty, D., Hoffmann, D., Drysdale, R., and Blamart, D.:
Millennial-scale climate variability during the Last Interglacial recorded in
a speleothem from south-western France, Quaternary Sci. Rev., 28, 3263–3274,
https://doi.org/10.1016/j.quascirev.2009.08.014, 2009.
Cruz, F. W., Burns, S. J., Karmann, I., Sharp, W. D., Vuille, M., Cardoso, A.
O., Ferrari, J. A., Dias, P. L. S., and Viana, O.: Insolation-driven changes
in atmospheric circulation over the past 116,000 years in subtropical Brazil,
Nature, 434, 63–66, https://doi.org/10.1038/nature03365, 2005.
Cruz, F. W., Vuille, M., Burns, S. J., Wang, X., Cheng, H., Werner, M.,
Lawrence Edwards, R., Karmann, I., Auler, A. S., and Nguyen, H.: Orbitally
driven east–west antiphasing of South American precipitation, Nat. Geosci.,
2, 210–214, https://doi.org/10.1038/ngeo444, 2009.
Daley, T. J., Thomas, E. R., Holmes, J. A., Street-Perrott, F. A., Chapman,
M. R., Tindall, J. C., Valdes, P. J., Loader, N. J., Marshall, J. D., Wolff,
E. W., Hopley, P. J., Atkinson, T., Barber, K. E., Fisher, E. H., Robertson,
I., Hughes, P. D. M., and Roberts, C. N.: The 8200 yr BP cold event in
stable isotope records from the North Atlantic region, Global Planet. Change,
79, 288–302, https://doi.org/10.1016/j.gloplacha.2011.03.006, 2011.
Demény, A., Czuppon, G., Siklósy, Z., Leél-Őssy, S., Lin, K.,
Shen, C.-C., and Gulyás, K.: Mid-Holocene climate conditions and moisture
source variations based on stable H, C and O isotope compositions of
speleothems in Hungary, Quatern. Int., 293, 150–156,
https://doi.org/10.1016/j.quaint.2012.05.035, 2013.
Demény, A., Kern, Z., Czuppon, G., Németh, A., Schöll-Barna, G.,
Siklósy, Z., Leél-Őssy, S., Cook, G., Serlegi, G., Bajnóczi,
B., Sümegi, P., Király, Á., Kiss, V., Kulcsár, G., and
Bondár, M.: Middle Bronze Age humidity and temperature variations, and
societal changes in East-Central Europe, Quatern. Int.,
https://doi.org/10.1016/j.quaint.2017.11.023, online first, 2017a.
Demény, A., Kern, Z., Czuppon, G., Németh, A., Leél-Őssy, S.,
Siklósy, Z., Lin, K., Hu, H.-M., Shen, C.-C., Vennemann, T. W., and
Haszpra, L.: Stable isotope compositions of speleothems from the last
interglacial – Spatial patterns of climate fluctuations in Europe,
Quaternary Sci. Rev., 161, 68–80, https://doi.org/10.1016/j.quascirev.2017.02.012,
2017b.
Denniston, R. F., Wyrwoll, K.-H., Polyak, V. J., Brown, J. R., Asmerom, Y.,
Wanamaker, A. D., LaPointe, Z., Ellerbroek, R., Barthelmes, M., Cleary, D.,
Cugley, J., Woods, D., and Humphreys, W. F.: A Stalagmite record of Holocene
Indonesian–Australian summer monsoon variability from the Australian
tropics, Quaternary Sci. Rev., 78, 155–168,
https://doi.org/10.1016/j.quascirev.2013.08.004, 2013a.
Denniston, R. F., Wyrwoll, K.-H., Asmerom, Y., Polyak, V. J., Humphreys, W.
F., Cugley, J., Woods, D., LaPointe, Z., Peota, J., and Greaves, E.: North
Atlantic forcing of millennial-scale Indo-Australian monsoon dynamics during
the Last Glacial period, Quaternary Sci. Rev., 72, 159–168,
https://doi.org/10.1016/j.quascirev.2013.04.012, 2013b.
Denniston, R. F., Villarini, G., Gonzales, A. N., Wyrwoll, K.-H., Polyak, V.
J., Ummenhofer, C. C., Lachniet, M. S., Wanamaker, A. D., Humphreys, W. F.,
Woods, D., and Cugley, J.: Extreme rainfall activity in the Australian
tropics reflects changes in the El Niño/Southern Oscillation over the
last two millennia, P. Natl. Acad. Sci. USA, 112, 4576–4581,
https://doi.org/10.1073/pnas.1422270112, 2015.
Denniston, R. F., Ummenhofer, C. C., Wanamaker, A. D., Lachniet, M. S.,
Villarini, G., Asmerom, Y., Polyak, V. J., Passaro, K. J., Cugley, J., Woods,
D., and Humphreys, W. F.: Expansion and Contraction of the Indo-Pacific
Tropical Rain Belt over the Last Three Millennia, Sci. Rep., 6, 34485,
https://doi.org/10.1038/srep34485, 2016.
Dong, J., Wang, Y., Cheng, H., Hardt, B., Edwards, R. L., Kong, X., Wu, J.,
Chen, S., Liu, D., Jiang, X., and Zhao, K.: A high-resolution stalagmite
record of the Holocene East Asian monsoon from Mt Shennongjia, central China,
The Holocene, 20, 257–264, https://doi.org/10.1177/0959683609350393, 2010.
Dorale, J. A., Edwards, R. L., Ito, E., and González, L. A.: Climate and
vegetation history of the midcontinent from 75 to 25 ka: a speleothem record
from Crevice Cave, Missouri, USA, Science, 282, 1871–1874,
https://doi.org/10.1126/science.282.5395.1871, 1998.
Drǎguşin, V., Staubwasser, M., Hoffmann, D. L., Ersek, V., Onac, B.
P., and Veres, D.: Constraining Holocene hydrological changes in the
Carpathian–Balkan region using speleothem δ18O and pollen-based
temperature reconstructions, Clim. Past, 10, 1363–1380,
https://doi.org/10.5194/cp-10-1363-2014, 2014.
Drysdale, R., Zanchetta, G., Hellstrom, J., Maas, R., Fallick, A., Pickett,
M., Cartwright, I., and Piccini, L.: Late Holocene drought responsible for
the collapse of Old World civilizations is recorded in an Italian cave
flowstone, Geology, 34, 101–104, https://doi.org/10.1130/g22103.1, 2006.
Drysdale, R. N., Zanchetta, G., Hellstrom, J. C., Fallick, A. E., Zhao, J.,
Isola, I., and Bruschi, G.: Palaeoclimatic implications of the growth history
and stable isotope (δ18O and δ13C) geochemistry of a
Middle to Late Pleistocene stalagmite from central-western Italy, Earth
Planet. Sci. Lett., 227, 215–229, https://doi.org/10.1016/j.epsl.2004.09.010, 2004.
Drysdale, R. N., Zanchetta, G., Hellstrom, J. C., Fallick, A. E., and Zhao,
J.: Stalagmite evidence for the onset of the Last Interglacial in southern
Europe at 129±1 ka, Geophys. Res. Lett., 32, L24708,
https://doi.org/10.1029/2005GL024658, 2005.
Drysdale, R. N., Zanchetta, G., Hellstrom, J. C., Fallick, A. E., McDonald,
J., and Cartwright, I.: Stalagmite evidence for the precise timing of North
Atlantic cold events during the early last glacial, Geology, 35, 77–80,
https://doi.org/10.1130/G23161A.1, 2007.
Drysdale, R. N., Hellstrom, J. C., Zanchetta, G., Fallick, A. E., Sanchez
Goni, M. F., Couchoud, I., McDonald, J., Maas, R., Lohmann, G., and Isola,
I.: Evidence for Obliquity Forcing of Glacial Termination II, Science, 325,
1527–1531, https://doi.org/10.1126/science.1170371, 2009.
Duan, W., Cheng, H., Tan, M., and Edwards, R. L.: Onset and duration of
transitions into Greenland Interstadials 15.2 and 14 in northern China
constrained by an annually laminated stalagmite, Sci. Rep., 6, 20844,
https://doi.org/10.1038/srep20844, 2016.
Dutt, S., Gupta, A. K., Clemens, S. C., Cheng, H., Singh, R. K., Kathayat,
G., and Edwards, R. L.: Abrupt changes in Indian summer monsoon strength
during 33,800 to 5500 years B.P., Geophys. Res. Lett., 42, 5526–5532,
https://doi.org/10.1002/2015GL064015, 2015.
Edwards, R. L., Chen, J. H., and Wasserburg, G. J.:
238U–234U–230Th–232Th systematics and the precise
measurement of time over the past 500,000 years, Earth Planet. Sci. Lett.,
81, 175–192, https://doi.org/10.1016/0012-821X(87)90154-3, 1987.
Ersek, V., Clark, P. U., Mix, A. C., Cheng, H., and Edwards, R. L.: Holocene
winter climate variability in mid-latitude western North America, Nat.
Commun., 3, 1219, https://doi.org/10.1038/ncomms2222, 2012.
Fairchild, I. J. and Baker, A.: Speleothem Science, John Wiley & Sons,
Ltd, Chichester, UK, 2012.
Feng, W., Hardt, B. F., Banner, J. L., Meyer, K. J., James, E. W., Musgrove,
M., Edwards, R. L., Cheng, H., and Min, A.: Changing amounts and sources of
moisture in the U.S. southwest since the Last Glacial Maximum in response to
global climate change, Earth Planet. Sci. Lett., 401, 47–56,
https://doi.org/10.1016/j.epsl.2014.05.046, 2014.
Finné, M., Bar-Matthews, M., Holmgren, K., Sundqvist, H. S., Liakopoulos,
I., and Zhang, Q.: Speleothem evidence for late Holocene climate variability
and floods in Southern Greece, Quaternary Res., 81, 213–227,
https://doi.org/10.1016/j.yqres.2013.12.009, 2014.
Finné, M., Holmgren, K., Shen, C.-C., Hu, H.-M., Boyd, M., and Stocker,
S.: Late Bronze Age climate change and the destruction of the Mycenaean
Palace of Nestor at Pylos, PLoS One, 12, e0189447,
https://doi.org/10.1371/journal.pone.0189447, 2017.
Fleitmann, D., Burns, S. J., Neff, U., Mudelsee, M., Mangini, A., and Matter,
A.: Palaeoclimatic interpretation of high-resolution oxygen isotope profiles
derived from annually laminated speleothems from Southern Oman, Quaternary
Sci. Rev., 23, 935–945, https://doi.org/10.1016/j.quascirev.2003.06.019, 2004.
Fleitmann, D., Burns, S. J., Mangini, A., Mudelsee, M., Kramers, J., Villa,
I., Neff, U., Al-Subbary, A. A., Buettner, A., Hippler, D., and Matter, A.:
Holocene ITCZ and Indian monsoon dynamics recorded in stalagmites from Oman
and Yemen (Socotra), Quaternary Sci. Rev., 26, 170–188,
https://doi.org/10.1016/j.quascirev.2006.04.012, 2007.
Fleitmann, D., Cheng, H., Badertscher, S., Edwards, R. L., Mudelsee, M.,
Göktürk, O. M., Fankhauser, A., Pickering, R., Raible, C. C., Matter,
A., Kramers, J., and Tüysüz, O.: Timing and climatic impact of
Greenland interstadials recorded in stalagmites from northern Turkey,
Geophys. Res. Lett., 36, L19707, https://doi.org/10.1029/2009gl040050, 2009.
Fohlmeister, J., Schröder-Ritzrau, A., Scholz, D., Spötl, C.,
Riechelmann, D. F. C., Mudelsee, M., Wackerbarth, A., Gerdes, A.,
Riechelmann, S., Immenhauser, A., Richter, D. K., and Mangini, A.: Bunker
Cave stalagmites: an archive for central European Holocene climate
variability, Clim. Past, 8, 1751–1764,
https://doi.org/10.5194/cp-8-1751-2012, 2012.
Fohlmeister, J., Vollweiler, N., Spötl, C., and Mangini, A.: COMNISPA II:
Update of a mid-European isotope climate record, 11 ka to present, The
Holocene, 23, 749–754, https://doi.org/10.1177/0959683612465446, 2013.
Fohlmeister, J., Plessen, B., Dudashvili, A. S., Tjallingii, R., Wolff, C.,
Gafurov, A., and Cheng, H.: Winter precipitation changes during the Medieval
Climate Anomaly and the Little Ice Age in arid Central Asia, Quaternary Sci.
Rev., 178, 24–36, https://doi.org/10.1016/j.quascirev.2017.10.026, 2017.
Frisia, S., Borsato, A., Mangini, A., Spötl, C., Madonia, G., and Sauro,
U.: Holocene Climate Variability in Sicily from a Discontinuous Stalagmite
Record and the Mesolithic to Neolithic Transition, Quaternary Res., 66,
388–400, https://doi.org/10.1016/j.yqres.2006.05.003, 2006.
Frisia, S., Fairchild, I. J., Fohlmeister, J., Miorandi, R., Spotl, C., and
Borsato, A.: Carbon mass-balance modelling and carbon isotope exchange
processes in dynamic caves, Geochim. Cosmochim. Acta, 75, 380–400,
https://doi.org/10.1016/j.gca.2010.10.021, 2011.
Frumkin, A., Ford, D. C., and Schwarcz, H. P.: Continental Oxygen Isotopic
Record of the Last 170,000 Years in Jerusalem, Quaternary Res., 51, 317–327,
https://doi.org/10.1006/qres.1998.2031, 1999.
Frumkin, A., Ford, D. C., and Schwarcz, H. P.: Paleoclimate and vegetation of
the Last Glacial Cycles in Jerusalem from a Speleothem Record, Global
Biogeochem. Cy., 14, 863–870, https://doi.org/10.1029/1999gb001245, 2000.
Genty, D., Vokal, B., Obelic, B., and Massault, M.: Bomb 14C time
history recorded in two modern stalagmites – importance for soil organic
matter dynamics and bomb 14C distribution over continents, Earth Planet.
Sci. Lett., 160, 795–809, https://doi.org/10.1016/S0012-821X(98)00128-9, 1998.
Genty, D., Massault, M., Gilmour, M., Baker, A., Verheyden, S., and Kepens,
E.: Calculation of Past Dead Carbon Proportion and Variability by the
Comparison of AMS 14C and Tims U/TH Ages on Two Holocene Stalagmites,
Radiocarbon, 41, 251–270, https://doi.org/10.1017/S003382220005712X, 1999.
Genty, D., Blamart, D., Ouahdi, R., Gilmour, M., Baker, A., Jouzel, J., and
Van-Exter, S.: Precise dating of Dansgaard–Oeschger climate oscillations in
western Europe from stalagmite data, Nature, 421, 833–837,
https://doi.org/10.1038/nature01391, 2003.
Genty, D., Blamart, D., Ghaleb, B., Plagnes, V., Causse, C., Bakalowicz, M.,
Zouari, K., Chkir, N., Hellstrom, J., and Wainer, K.: Timing and dynamics of
the last deglaciation from European and North African δ13C
stalagmite profiles—comparison with Chinese and South Hemisphere
stalagmites, Quaternary Sci. Rev., 25, 2118–2142,
https://doi.org/10.1016/j.quascirev.2006.01.030, 2006.
Genty, D., Combourieu-Nebout, N., Peyron, O., Blamart, D., Wainer, K.,
Mansuri, F., Ghaleb, B., Isabello, L., Dormoy, I., and von Grafenstein, U.:
Isotopic characterization of rapid climatic events during OIS3 and OIS4 in
Villars Cave stalagmites (SW-France) and correlation with Atlantic and
Mediterranean pollen records, Quaternary Sci. Rev., 29, 2799–2820,
https://doi.org/10.1016/j.quascirev.2010.06.035, 2010.
Grant, K. M., Rohling, E. J., Bar-Matthews, M., Ayalon, A., Medina-Elizalde,
M., Ramsey, C. B., Satow, C., and Roberts, A. P.: Rapid coupling between ice
volume and polar temperature over the past 150,000 years, Nature, 491,
744–747, https://doi.org/10.1038/nature11593, 2012.
Griffiths, M. L., Drysdale, R. N., Gagan, M. K., Zhao, J.-X., Ayliffe, L. K.,
Hellstrom, J. C., Hantoro, W. S., Frisia, S., Feng, Y.-X., Cartwright, I.,
Pierre, E. St., Fischer, M. J., and Suwargadi, B. W.: Increasing
Australian–Indonesian monsoon rainfall linked to early Holocene sea-level
rise, Nat. Geosci., 2, 636–639, https://doi.org/10.1038/ngeo605, 2009.
Griffiths, M. L., Drysdale, R. N., Gagan, M. K., Hellstrom, J. C., Couchoud,
I., Ayliffe, L. K., Vonhof, H. B., and Hantoro, W. S.: Australasian monsoon
response to Dansgaard–Oeschger event 21 and teleconnections to higher
latitudes, Earth Planet. Sci. Lett., 369–370, 294–304,
https://doi.org/10.1016/j.epsl.2013.03.030, 2013.
Griffiths, M. L., Kimbrough, A. K., Gagan, M. K., Drysdale, R. N., Cole, J.
E., Johnson, K. R., Zhao, J.-X., Cook, B. I., Hellstrom, J. C., and Hantoro,
W. S.: Western Pacific hydroclimate linked to global climate variability over
the past two millennia, Nat. Commun., 7, 11719, https://doi.org/10.1038/ncomms11719,
2016.
Haese, B., Werner, M., and Lohmann, G.: Stable water isotopes in the coupled
atmosphere–land surface model ECHAM5-JSBACH, Geosci. Model Dev., 6,
1463–1480, https://doi.org/10.5194/gmd-6-1463-2013, 2013.
Han, L.-Y., Li, T.-Y., Cheng, H., Edwards, R. L., Shen, C.-C., Li, H.-C.,
Huang, C.-X., Li, J.-Y., Yuan, N., Wang, H.-B., Zhang, T.-T., and Zhao, X.:
Potential influence of temperature changes in the Southern Hemisphere on the
evolution of the Asian summer monsoon during the last glacial period,
Quatern. Int., 392, 239–250, https://doi.org/10.1016/j.quaint.2015.05.068, 2016.
Hardt, B., Rowe, H. D., Springer, G. S., Cheng, H., and Edwards, R. L.: The
seasonality of east central North American precipitation based on three
coeval Holocene speleothems from southern West Virginia, Earth Planet. Sci.
Lett., 295, 342–348, https://doi.org/10.1016/j.epsl.2010.04.002, 2010.
Harrison, S. P., Bartlein, P. J., Brewer, S., Prentice, I. C., Boyd, M.,
Hessler, I., Holmgren, K., Izumi, K., and Willis, K.: Climate model
benchmarking with glacial and mid-Holocene climates, Clim. Dynam., 43,
671–688, https://doi.org/10.1007/s00382-013-1922-6, 2014.
Häuselmann, A. D., Fleitmann, D., Cheng, H., Tabersky, D., Günther,
D., and Edwards, R. L.: Timing and nature of the penultimate deglaciation in
a high alpine stalagmite from Switzerland, Quaternary Sci. Rev., 126,
264–275, https://doi.org/10.1016/j.quascirev.2015.08.026, 2015.
Hellstrom, J., McCulloch, M., and Stone, J.: A Detailed 31,000-Year Record of
Climate and Vegetation Change, from the Isotope Geochemistry of Two New
Zealand Speleothems, Quaternary Res., 50, 167–178,
https://doi.org/10.1006/qres.1998.1991, 1998.
Hellstrom, J. C.: U–Th dating of speleothems with high initial 230Th
using stratigraphical constraint, Quat. Geochronol., 1, 289–295,
https://doi.org/10.1016/j.quageo.2007.01.004, 2006.
Hendy, C.: The isotopic geochemistry of speleothems – I. The calculation of
the effects of different modes of formaion on the isotopic composition of
speleothems and their applicability as paleoclimatic indicators, Geochim.
Cosmochim. Acta, 35, 801–824, https://doi.org/10.1016/0016-7037(71)90127-X, 1971.
Holmgren, K., Lauritzen, S.-E., and Possnert, G.: 230Th234U and
14C dating of a late Pleistocene stalagmite in Lobatse II Cave,
Botswana, Quaternary Sci. Rev., 13, 111–119,
https://doi.org/10.1016/0277-3791(94)90036-1, 1994.
Holmgren, K., Karlén, W., and Shaw, P. A.: Paleoclimatic Significance of
the Stable Isotopic Composition and Petrology of a Late Pleistocene
Stalagmite from Botswana, Quaternary Res., 43, 320–328,
https://doi.org/10.1006/qres.1995.1038, 1995.
Holmgren, K., Karlén, W., Lauritzen, S. E., Lee-Thorp, J. A., Partridge,
T. C., Piketh, S., Repinski, P., Stevenson, C., Svanered, O., and Tyson, P.
D.: A 3000-year high-resolution stalagmitebased record of palaeoclimate for
northeastern South Africa, The Holocene, 9, 295–309,
https://doi.org/10.1191/095968399672625464, 1999.
Holmgren, K., Lee-Thorp, J. A., Cooper, G. R. J., Lundblad, K., Partridge, T.
C., Scott, L., Sithaldeen, R., Talma, A. S., and Tyson, P. D.: Persistent
millennial-scale climatic variability over the past 25,000 years in Southern
Africa, Quaternary Sci. Rev., 22, 2311–2326,
https://doi.org/10.1016/s0277-3791(03)00204-x, 2003.
Holzkämper, S., Holmgren, K., Lee-Thorp, J., Talma, S., Mangini, A., and
Partridge, T.: Late Pleistocene stalagmite growth in Wolkberg Cave, South
Africa, Earth Planet. Sci. Lett., 282, 212–221,
https://doi.org/10.1016/j.epsl.2009.03.016, 2009.
Hopley, P. J., Weedon, G. P., Marshall, J. D., Herries, A. I. R., Latham, A.
G., and Kuykendall, K. L.: High- and low-latitude orbital forcing of early
hominin habitats in South Africa, Earth Planet. Sci. Lett., 256, 419–432,
https://doi.org/10.1016/j.epsl.2007.01.031, 2007a.
Hopley, P. J., Marshall, J. D., Weedon, G. P., Latham, A. G., Herries, A. I.
R., and Kuykendall, K. L.: Orbital forcing and the spread of C4 grasses in
the late Neogene: stable isotope evidence from South African speleothems, J.
Hum. Evol., 53, 620–634, https://doi.org/10.1016/j.jhevol.2007.03.007, 2007b.
Hu, C., Henderson, G. M., Huang, J., Xie, S., Sun, Y., and Johnson, K. R.:
Quantification of Holocene Asian monsoon rainfall from spatially separated
cave records, Earth Planet. Sci. Lett., 266, 221–232,
https://doi.org/10.1016/j.epsl.2007.10.015, 2008.
Huang, W., Wang, Y., Cheng, H., Edwards, R. L., Shen, C.-C., Liu, D., Shao,
Q., Deng, C., Zhang, Z., and Wang, Q.: Multi-scale Holocene Asian monsoon
variability deduced from a twin-stalagmite record in southwestern China,
Quaternary Res., 86, 34–44, https://doi.org/10.1016/j.yqres.2016.05.001, 2016.
Ivanovich, M. and Harmon, R.: Uranium-series disequilibrium: applications to
earth, marine, and environmental sciences. 2, available at:
https://inis.iaea.org/search/search.aspx?orig_q=RN:25065862 (last
access: 30 January 2018), 1992.
Jaqueto, P., Trindade, R. I. F., Hartmann, G. A., Novello, V. F., Cruz, F.
W., Karmann, I., Strauss, B. E., and Feinberg, J. M.: Linking speleothem and
soil magnetism in the Pau d'Alho cave (central South America), J. Geophys.
Res.-Sol. Ea., 121, 7024–7039, https://doi.org/10.1002/2016JB013541, 2016.
Johnston, V. E., Borsato, A., Spötl, C., Frisia, S., and Miorandi, R.:
Stable isotopes in caves over altitudinal gradients: fractionation behaviour
and inferences for speleothem sensitivity to climate change, Clim. Past, 9,
99–118, https://doi.org/10.5194/cp-9-99-2013, 2013.
Joshi, L. M., Kotlia, B. S., Ahmad, S. M., Wu, C.-C., Sanwal, J., Raza, W.,
Singh, A. K., Shen, C.-C., Long, T., and Sharma, A. K.: Reconstruction of
Indian monsoon precipitation variability between 4.0 and 1.6 ka BP using
speleothem δ18O records from the Central Lesser Himalaya, India,
Arab. J. Geosci., 10, 356, https://doi.org/10.1007/s12517-017-3141-7, 2017.
Kacanski, A., Carmi, I., Shemesh, A., Kronfeld, J., Yam, R., and Flexer, A.:
Late Holocene Climatic Change in the Balkans: Speleothem Isotopic Data from
Serbia, Radiocarbon, 43, 647–658, https://doi.org/10.1017/s0033822200041308, 2001.
Kathayat, G., Cheng, H., Sinha, A., Spötl, C., Edwards, R. L., Zhang, H.,
Li, X., Yi, L., Ning, Y., Cai, Y., Lui, W. L., and Breitenbach, S. F. M.:
Indian monsoon variability on millennial-orbital timescales, Sci. Rep., 6,
24374, https://doi.org/10.1038/srep24374, 2016.
Kennett, D. J., Breitenbach, S. F. M., Aquino, V. V, Asmerom, Y., Awe, J.,
Baldini, J. U. L., Bartlein, P., Culleton, B. J., Ebert, C., Jazwa, C.,
Macri, M. J., Marwan, N., Polyak, V., Prufer, K. M., Ridley, H. E., Sodemann,
H., Winterhalder, B., and Haug, G. H.: Development and Disintegration of Maya
Political Systems in Response to Climate Change, Science, 338, 788–791,
https://doi.org/10.1126/science.1226299, 2012.
Koltai, G., Spötl, C., Shen, C.-C., Wu, C.-C., Rao, Z., Palcsu, L., Kele,
S., Surányi, G., and Bárány-Kevei, I.: A penultimate glacial
climate record from southern Hungary, J. Quaternary Sci., 32, 946–956,
https://doi.org/10.1002/jqs.2968, 2017.
Kotlia, B. S., Singh, A. K., Sanwal, J., Raza, W., Ahmad, S. M., Joshi, L.
M., Sirohi, M., Sharma, A. K., and Sagar, N.: Stalagmite Inferred High
Resolution Climatic Changes through Pleistocene-Holocene Transition in
Northwest Indian Himalaya, J. Earth Sci. Clim. Change, 7,
https://doi.org/10.4172/2157-7617.1000338, 2016.
Labuhn, I., Genty, D., Vonhof, H., Bourdin, C., Blamart, D., Douville, E.,
Ruan, J., Cheng, H., Edwards, R. L., Pons-Branchu, E., and Pierre, M.: A
high-resolution fluid inclusion δ18O record from a stalagmite in SW
France: modern calibration and comparison with multiple proxies, Quaternary
Sci. Rev., 110, 152–165, https://doi.org/10.1016/j.quascirev.2014.12.021, 2015.
Lachniet, M. S.: A 1500-year El Niño/Southern Oscillation and rainfall
history for the Isthmus of Panama from speleothem calcite, J. Geophys. Res.,
109, D20117, https://doi.org/10.1029/2004jd004694, 2004.
Lachniet, M. S., Asmerom, Y., and Polyak, V.: Deglacial paleoclimate in the
southwestern United States: an abrupt 18.6 ka cold event and evidence for a
North Atlantic forcing of Termination I, Quaternary Sci. Rev., 30,
3803–3811, https://doi.org/10.1016/j.quascirev.2011.09.022, 2011.
Lachniet, M. S., Bernal, J. P., Asmerom, Y., Polyak, V., and Piperno, D.: A
2400 yr Mesoamerican rainfall reconstruction links climate and cultural
change, Geology, 40, 259–262, https://doi.org/10.1130/g32471.1, 2012.
Lachniet, M. S., Asmerom, Y., Bernal, J. P., Polyak, V. J., and
Vazquez-Selem, L.: Orbital pacing and ocean circulation-induced collapses of
the Mesoamerican monsoon over the past 22,000 y, P. Natl. Acad. Sci. USA,
110, 9255–9260, https://doi.org/10.1073/pnas.1222804110, 2013.
Lachniet, M. S., Denniston, R. F., Asmerom, Y., and Polyak, V. J.: Orbital
control of western North America atmospheric circulation and climate over two
glacial cycles, Nat. Commun., 5, 3805, https://doi.org/10.1038/ncomms4805, 2014.
Lachniet, M. S., Asmerom, Y., Polyak, V., and Bernal, J. P.: Two millennia of
Mesoamerican monsoon variability driven by Pacific and Atlantic synergistic
forcing, Quaternary Sci. Rev., 155, 100–113,
https://doi.org/10.1016/j.quascirev.2016.11.012, 2017.
Lechleitner, F. A., Breitenbach, S. F. M., Cheng, H., Plessen, B., Rehfeld,
K., Goswami, B., Marwan, N., Eroglu, D., Adkins, J., and Haug, G.: Climatic
and in-cave influences on δ18O and δ13C in a stalagmite
from northeastern India through the last deglaciation, Quaternary Res., 88,
458–471, https://doi.org/10.1017/qua.2017.72, 2017.
Lee-Thorp, J. A., Holmgren, K., Lauritzen, S.-E., Linge, H., Moberg, A.,
Partridge, T. C., Stevenson, C., and Tyson, P. D.: Rapid climate shifts in
the southern African interior throughout the Mid to Late Holocene, Geophys.
Res. Lett., 28, 4507–4510, https://doi.org/10.1029/2000gl012728, 2001.
Lewis, S. C., Gagan, M. K., Ayliffe, L. K., Zhao, J., Hantoro, W. S., Treble,
P. C., Hellstrom, J. C., LeGrande, A. N., Kelley, M., Schmidt, G. A., and
Suwargadi, B. W.: High-resolution stalagmite reconstructions of
Australian–Indonesian monsoon rainfall variability during Heinrich stadial 3
and Greenland interstadial 4, Earth Planet. Sci. Lett., 303, 133–142,
https://doi.org/10.1016/j.epsl.2010.12.048, 2011.
Li, H.-C., Lee, Z.-H., Wan, N.-J., Shen, C.-C., Li, T.-Y., Yuan, D.-X., and
Chen, Y.-H.: The δ18O and δ13C records in an aragonite
stalagmite from Furong Cave, Chongqing, China: A-2000-year record of
monsoonal climate, J. Asian Earth Sci., 40, 1121–1130,
https://doi.org/10.1016/j.jseaes.2010.06.011, 2011.
Li, J.-Y., Li, H.-C., Li, T.-Y., Mii, H.-S., Yu, T.-L., Shen, C.-C., and Xu,
X.: High-resolution δ18O and δ13C records of an AMS
14C and 230Th/U dated stalagmite from Xinya Cave in Chongqing:
Climate and vegetation change during the late Holocene, Quatern. Int., 447,
75–88, https://doi.org/10.1016/j.quaint.2017.06.075, 2017.
Li, T., Yuan, D., Li, H., Yang, Y., Wang, J., Wang, X., Li, J., Qin, J.,
Zhang, M., and Lin, Y.: High-resolution climate variability of southwest
China during 57–70 ka reflected in a stalagmite δ18O record from
Xinya Cave, Sci. China Earth Sci., 50, 1202–1208,
https://doi.org/10.1007/s11430-007-0059-z, 2007.
Li, T.-Y., Shen, C.-C., Li, H.-C., Li, J.-Y., Chiang, H.-W., Song, S.-R.,
Yuan, D.-X., Lin, C. D.-J., Gao, P., Zhou, L., Wang, J.-L., Ye, M.-Y., Tang,
L.-L., and Xie, S.-Y.: Oxygen and carbon isotopic systematics of aragonite
speleothems and water in Furong Cave, Chongqing, China, Geochim. Cosmochim.
Acta, 75, 4140–4156, https://doi.org/10.1016/j.gca.2011.04.003, 2011.
Li, T.-Y., Shen, C.-C., Huang, L.-J., Jiang, X.-Y., Yang, X.-L., Mii, H.-S.,
Lee, S.-Y., and Lo, L.: Stalagmite-inferred variability of the Asian summer
monsoon during the penultimate glacial–interglacial period, Clim. Past, 10,
1211–1219, https://doi.org/10.5194/cp-10-1211-2014, 2014.
Li, T.-Y., Han, L.-Y., Cheng, H., Edwards, R. L., Shen, C.-C., Li, H.-C., Li,
J.-Y., Huang, C.-X., Zhang, T.-T., and Zhao, X.: Evolution of the Asian
summer monsoon during Dansgaard/Oeschger events 13–17 recorded in a
stalagmite constrained by high-precision chronology from southwest China,
Quaternary Res., 88, 121–128, https://doi.org/10.1017/qua.2017.22, 2017.
Linge, H., Lauritzen, S.-E., Lundberg, J., and Berstad, I. M.: Stable isotope
stratigraphy of Holocene speleothems: examples from a cave system in Rana,
northern Norway, Palaeogeogr. Palaeocl., 167, 209–224,
https://doi.org/10.1016/s0031-0182(00)00225-x, 2001.
Linge, H., Lauritzen, S.-E., Andersson, C., Hansen, J. K., Skoglund, R.
Ø., and Sundqvist, H. S.: Stable isotope records for the last 10 000 years
from Okshola cave (Fauske, northern Norway) and regional comparisons, Clim.
Past, 5, 667–682, https://doi.org/10.5194/cp-5-667-2009, 2009a.
Linge, H., Baker, A., Andersson, C., and Lauritzen, S.-E.: Variability in
luminescent lamination and initial 230 Th/232 Th activity ratios in a late
Holocene stalagmite from northern Norway, Quat. Geochronol., 4, 181–192,
2009b.
Liu, Y.-H., Henderson, G. M., Hu, C.-Y., Mason, A. J., Charnley, N., Johnson,
K. R., and Xie, S.-C.: Links between the East Asian monsoon and North
Atlantic climate during the 8,200 year event, Nat. Geosci., 6, 117–120,
https://doi.org/10.1038/ngeo1708, 2013.
Lone, M. A., Ahmad, S. M., Dung, N. C., Shen, C.-C., Raza, W., and Kumar, A.:
Speleothem based 1000-year high resolution record of Indian monsoon
variability during the last deglaciation, Palaeogeogr. Palaeocl., 395, 1–8,
https://doi.org/10.1016/j.palaeo.2013.12.010, 2014.
Lorrey, A., Williams, P., Salinger, J., Martin, T., Palmer, J., Fowler, A.,
Zhao, J., and Neil, H.: Speleothem stable isotope records interpreted within
a multi-proxy framework and implications for New Zealand palaeoclimate
reconstruction, Quatern. Int., 187, 52–75, https://doi.org/10.1016/j.quaint.2007.09.039,
2008.
Luetscher, M., Hoffmann, D. L., Frisia, S., and Spötl, C.: Holocene
glacier history from alpine speleothems, Milchbach cave, Switzerland, Earth
Planet. Sci. Lett., 302, 95–106, https://doi.org/10.1016/j.epsl.2010.11.042, 2011.
Luetscher, M., Boch, R., Sodemann, H., Spötl, C., Cheng, H., Edwards, R.
L., Frisia, S., Hof, F., and Müller, W.: North Atlantic storm track
changes during the Last Glacial Maximum recorded by Alpine speleothems, Nat.
Commun., 6, 6344, https://doi.org/10.1038/ncomms7344, 2015.
Ma, Z.-B., Cheng, H., Tan, M., Edwards, R. L., Li, H.-C., You, C.-F., Duan,
W.-H., Wang, X., and Kelly, M. J.: Timing and structure of the Younger Dryas
event in northern China, Quaternary Sci. Rev., 41, 83–93,
https://doi.org/10.1016/j.quascirev.2012.03.006, 2012.
Madonia, G., Frisia, S., Borsato, A., Macaluso, T., Mangini, A., Paladini,
M., Piccini, L., Miorandi, R., Spötl, C., Sauro, U., Agnesi, V., Di
Pietro, R., Palmeri, A., and Vattano, M.: La Grotta di
Carburangeli–ricostruzione climatica dell'Olocene per la piana costiera
della Sicilia nord-occidentale, Stud. Trent Sci Nat Acta Geol, 80, 153–167
available at:
http://www2.muse.it/pubblicazioni/6/actaG80/Vol_ACTA_80_2003_153-167.pdf (last access: 30 May 2018), 2005.
Mattey, D., Lowry, D., Duffet, J., Fisher, R., Hodge, E., and Frisia, S.: A
53 year seasonally resolved oxygen and carbon isotope record from a modern
Gibraltar speleothem: Reconstructed drip water and relationship to local
precipitation, Earth Planet. Sci. Lett., 269, 80–95,
https://doi.org/10.1016/j.epsl.2008.01.051, 2008.
Mattey, D. P., Fairchild, I. J., Atkinson, T. C., Latin, J.-P., Ainsworth,
M., and Durell, R.: Seasonal microclimate control of calcite fabrics, stable
isotopes and trace elements in modern speleothem from St Michaels Cave,
Gibraltar, Geol. Soc. London, Spec. Publ., 336, 323–344,
https://doi.org/10.1144/sp336.17, 2010.
McDermott, F.: Centennial-Scale Holocene Climate Variability Revealed by a
High-Resolution Speleothem δ18O Record from SW Ireland, Science,
294, 1328–1331, https://doi.org/10.1126/science.1063678, 2001.
McDermott, F.: Palaeo-climate reconstruction from stable isotope variations
in speleothems: a review, Quaternary Sci. Rev., 23, 901–918,
https://doi.org/10.1016/j.quascirev.2003.06.021, 2004.
McDermott, F., Frisia, S., Huang, Y., Longinelli, A., Spiro, B., Heaton, T.
H. E., Hawkesworth, C. J., Borsato, A., Keppens, E., Fairchild, I. J., van
der Borg, K., Verheyden, S., and Selmo, E.: Holocene climate variability in
Europe: Evidence from δ18O, textural and extension-rate variations
in three speleothems, Quaternary Sci. Rev., 18, 1021–1038,
https://doi.org/10.1016/S0277-3791(98)00107-3, 1999.
Meckler, A. N., Clarkson, M. O., Cobb, K. M., Sodemann, H., and Adkins, J.
F.: Interglacial Hydroclimate in the Tropical West Pacific Through the Late
Pleistocene, Science, 336, 1301–1304, https://doi.org/10.1126/science.1218340, 2012.
Medina-Elizalde, M., Burns, S. J., Lea, D. W., Asmerom, Y., von Gunten, L.,
Polyak, V., Vuille, M., and Karmalkar, A.: High resolution stalagmite climate
record from the Yucatán Peninsula spanning the Maya terminal classic
period, Earth Planet. Sci. Lett., 298, 255–262,
https://doi.org/10.1016/j.epsl.2010.08.016, 2010.
Meyer, M. C., Spötl, C., and Mangini, A.: The demise of the Last
Interglacial recorded in isotopically dated speleothems from the Alps,
Quaternary Sci. Rev., 27, 476–496, https://doi.org/10.1016/j.quascirev.2007.11.005,
2008.
Mickler, P. J., Stern, L. A., and Banner, J. L.: Large kinetic isotope
effects in modern speleothems Large kinetic isotope effects in modern
speleothems, Geol. Soc. Am. Bull., 118, 65–81, https://doi.org/10.1130/B25698.1, 2006.
Moerman, J. W., Cobb, K. M., Adkins, J. F., Sodemann, H., Clark, B., and
Tuen, A. A.: Diurnal to interannual rainfall δ18O variations in
northern Borneo driven by regional hydrology, Earth Planet. Sci. Lett.,
369–370, 108–119, https://doi.org/10.1016/j.epsl.2013.03.014, 2013.
Moerman, J. W., Cobb, K. M., Partin, J. W., Meckler, A. N., Carolin, S. A.,
Adkins, J. F., Lejau, S., Malang, J., Clark, B., and Tuen, A. A.:
Transformation of ENSO-related rainwater to dripwater δ 18 O
variability by vadose water mixing, Geophys. Res. Lett., 41, 7907–7915,
https://doi.org/10.1002/2014GL061696, 2014.
Moreno, A., Stoll, H., Jiménez-Sánchez, M., Cacho, I.,
Valero-Garcés, B., Ito, E., and Edwards, R. L.: A speleothem record of
glacial (25–11.6kyr BP) rapid climatic changes from northern Iberian
Peninsula, Global Planet. Change, 71, 218–231,
https://doi.org/10.1016/j.gloplacha.2009.10.002, 2010.
Moreno, A., Pérez-Mejías, C., Bartolomé, M., Sancho, C., Cacho,
I., Stoll, H., Delgado-Huertas, A., Hellstrom, J., Edwards, R. L., and Cheng,
H.: New speleothem data from Molinos and Ejulve caves reveal Holocene
hydrological variability in northeast Iberia, Quaternary Res., 88, 223–233,
https://doi.org/10.1017/qua.2017.39, 2017.
Moseley, G. E., Spötl, C., Svensson, A., Cheng, H., Brandstätter, S.,
and Edwards, R. L.: Multi-speleothem record reveals tightly coupled climate
between central Europe and Greenland during Marine Isotope Stage 3, Geology,
42, 1043–1046, https://doi.org/10.1130/g36063.1, 2014.
Moseley, G. E., Spötl, C., Cheng, H., Boch, R., Min, A., and Edwards, R.
L.: Termination-II interstadial/stadial climate change recorded in two
stalagmites from the north European Alps, Quaternary Sci. Rev., 127,
229–239, https://doi.org/10.1016/j.quascirev.2015.07.012, 2015.
Moseley, G. E., Edwards, R. L., Wendt, K. A., Cheng, H., Dublyansky, Y., Lu,
Y., Boch, R., and Spotl, C.: Reconciliation of the Devils Hole climate record
with orbital forcing, Science, 351, 165–168, https://doi.org/10.1126/science.aad4132,
2016.
Muñoz, A., Bartolomé, M., Muñoz, A., Sancho, C., Moreno, A.,
Hellstrom, J. C., Osácar, M. C., and Cacho, I.: Solar influence and
hydrological variability during the Holocene from a speleothem annual record
(Molinos Cave, NE Spain), Terra Nov., 27, 300–311, https://doi.org/10.1111/ter.12160,
2015.
Neff, U., Burns, S. J., Mangini, A., Mudelsee, M., Fleitmann, D., and Matter,
A.: Strong coherence between solar variability and the monsoon in Oman
between 9 and 6 kyr ago, Nature, 411, 290–293, https://doi.org/10.1038/35077048, 2001.
Nehme, C., Verheyden, S., Noble, S. R., Farrant, A. R., Sahy, D., Hellstrom,
J., Delannoy, J. J., and Claeys, P.: Reconstruction of MIS 5 climate in the
central Levant using a stalagmite from Kanaan Cave, Lebanon, Clim. Past, 11,
1785–1799, https://doi.org/10.5194/cp-11-1785-2015, 2015.
Nehme, C., Verheyden, S., Breitenbach, S. F. M., Gillikin, D. P., Verheyden,
A., Cheng, H., Edwards, R. L., Hellstrom, J., Noble, S. R., Farrant, A. R.,
Sahy, D., Goovaerts, T., Salem, G., and Claeys, P.: Climate dynamics during
the penultimate glacial period recorded in a speleothem from Kanaan Cave,
Lebanon (central Levant), Quaternary Res., 90, 10–25,
https://doi.org/10.1017/qua.2018.18, 2018.
Novello, V. F., Cruz, F. W., Karmann, I., Burns, S. J., Stríkis, N. M.,
Vuille, M., Cheng, H., Lawrence Edwards, R., Santos, R. V, Frigo, E., and
Barreto, E. A. S.: Multidecadal climate variability in Brazil's Nordeste
during the last 3000 years based on speleothem isotope records, Geophys. Res.
Lett., 39, L23706, https://doi.org/10.1029/2012GL053936, 2012.
Novello, V. F., Vuille, M., Cruz, F. W., Stríkis, N. M., de Paula, M.
S., Edwards, R. L., Cheng, H., Karmann, I., Jaqueto, P. F., Trindade, R. I.
F., Hartmann, G. A., and Moquet, J. S.: Centennial-scale solar forcing of the
South American Monsoon System recorded in stalagmites, Sci. Rep., 6, 24762,
https://doi.org/10.1038/srep24762, 2016.
Novello, V. F., Cruz, F. W., Vuille, M., Stríkis, N. M., Edwards, R. L.,
Cheng, H., Emerick, S., de Paula, M. S., Li, X., Barreto, E. de S., Karmann,
I., and Santos, R. V: A high-resolution history of the South American Monsoon
from Last Glacial Maximum to the Holocene, Sci. Rep., 7, 44267,
https://doi.org/10.1038/srep44267, 2017.
Onac, B. P., Constantin, S., Lundberg, J., and Lauritzen, S.-E.: Isotopic
climate record in a Holocene stalagmite from Ursilor Cave (Romania), J.
Quaternary Sci., 17, 319–327, https://doi.org/10.1002/jqs.685, 2002.
Orland, I. J., Bar-Matthews, M., Kita, N. T., Ayalon, A., Matthews, A., and
Valley, J. W.: Climate deterioration in the Eastern Mediterranean as revealed
by ion microprobe analysis of a speleothem that grew from 2.2 to 0.9 ka in
Soreq Cave, Israel, Quaternary Res., 71, 27–35,
https://doi.org/10.1016/j.yqres.2008.08.005, 2009.
Orland, I. J., Bar-Matthews, M., Ayalon, A., Matthews, A., Kozdon, R.,
Ushikubo, T., and Valley, J. W.: Seasonal resolution of Eastern Mediterranean
climate change since 34 ka from a Soreq Cave speleothem, Geochim. Cosmochim.
Acta, 89, 240–255, https://doi.org/10.1016/j.gca.2012.04.035, 2012.
Oster, J. L., Montañez, I. P., Sharp, W. D., and Cooper, K. M.: Late
Pleistocene California droughts during deglaciation and Arctic warming, Earth
Planet. Sci. Lett., 288, 434–443, https://doi.org/10.1016/j.epsl.2009.10.003, 2009.
Oster, J. L., Montañez, I. P., Santare, L. R., Sharp, W. D., Wong, C.,
and Cooper, K. M.: Stalagmite records of hydroclimate in central California
during termination 1, Quaternary Sci. Rev., 127, 199–214,
https://doi.org/10.1016/j.quascirev.2015.07.027, 2015.
Partin, J. W., Cobb, K. M., Adkins, J. F., Clark, B., and Fernandez, D. P.:
Millennial-scale trends in west Pacific warm pool hydrology since the Last
Glacial Maximum, Nature, 449, 452–455, https://doi.org/10.1038/nature06164, 2007.
Partin, J. W., Quinn, T. M., Shen, C.-C., Emile-Geay, J., Taylor, F. W.,
Maupin, C. R., Lin, K., Jackson, C. S., Banner, J. L., Sinclair, D. J., and
Huh, C.-A.: Multidecadal rainfall variability in South Pacific Convergence
Zone as revealed by stalagmite geochemistry, Geology, 41, 1143–1146,
https://doi.org/10.1130/g34718.1, 2013a.
Partin, J. W., Cobb, K. M., Adkins, J. F., Tuen, A. A., and Clark, B.: Trace
metal and carbon isotopic variations in cave dripwater and stalagmite
geochemistry from northern Borneo, Geochemistry, Geophys. Geosystems, 14,
3567–3585, https://doi.org/10.1002/ggge.20215, 2013b.
Pérez-Mejías, C., Moreno, A., Sancho, C., Bartolomé, M., Stoll,
H., Cacho, I., Cheng, H., and Edwards, R. L.: Abrupt climate changes during
Termination III in Southern Europe, P. Natl. Acad. Sci. USA, 114,
10047–10052, https://doi.org/10.1073/pnas.1619615114, 2017.
Plagnes, V., Causse, C., Genty, D., Paterne, M., and Blamart, D.: A
discontinuous climatic record from 187 to 74 ka from a speleothem of the
Clamouse Cave (south of France), Earth Planet. Sci. Lett., 201, 87–103,
https://doi.org/10.1016/s0012-821x(02)00674-x, 2002.
Pollock, A. L., van Beynen, P. E., DeLong, K. L., Polyak, V., and Asmerom,
Y.: A speleothem-based mid-Holocene precipitation reconstruction for
West-Central Florida, The Holocene, 27, 987–996,
https://doi.org/10.1177/0959683616678463, 2016.
Polyak, V. J. and Asmerom, Y.: Late Holocene Climate and Cultural Changes in
the Southwestern United States, Science, 294, 148–151,
https://doi.org/10.1126/science.1062771, 2001.
Polyak, V. J., Asmerom, Y., Burns, S. J., and Lachniet, M. S.: Climatic
backdrop to the terminal Pleistocene extinction of North American mammals,
Geology, 40, 1023–1026, https://doi.org/10.1130/g33226.1, 2012.
Ponte, J. M., Font, E., Veiga-Pires, C., Hillaire-Marcel, C., and Ghaleb, B.:
The effect of speleothem surface slope on the remanent magnetic inclination,
J. Geophys. Res.-Sol. Ea., 122, 4143–4156, https://doi.org/10.1002/2016jb013789, 2017.
Psomiadis, D., Dotsika, E., Albanakis, K., Ghaleb, B., and Hillaire-Marcel,
C.: Speleothem record of climatic changes in the northern Aegean region
(Greece) from the Bronze Age to the collapse of the Roman Empire,
Palaeogeogr. Palaeocl., 489, 272–283, https://doi.org/10.1016/j.palaeo.2017.10.021,
2018.
Railsback, L. B., Liang, F., Vidal Romaní, J. R., Grandal-d'Anglade, A.,
Vaqueiro Rodríguez, M., Santos Fidalgo, L., Fernández Mosquera, D.,
Cheng, H., and Edwards, R. L.: Petrographic and isotopic evidence for
Holocene long-term climate change and shorter-term environmental shifts from
a stalagmite from the Serra do Courel of northwestern Spain, and implications
for climatic history across Europe and the Mediterranean, Palaeogeogr.
Palaeocl., 305, 172–184, https://doi.org/10.1016/j.palaeo.2011.02.030, 2011.
Raza, W., Ahmad, S. M., Lone, M. A., Shen, C.-C., Sarma, D. S., and Kumar,
A.: Indian summer monsoon variability in southern India during the last
deglaciation: Evidence from a high resolution stalagmite δ18O
record, Palaeogeogr. Palaeocl., 485, 476–485,
https://doi.org/10.1016/j.palaeo.2017.07.003, 2017.
Repinski, P., Holmgren, K., Lauritzen, S. E., and Lee-Thorp, J. A.: A late
Holocene climate record from a stalagmite, Cold Air Cave, Northern Province,
South Africa, Palaeogeogr. Palaeocl., 150, 269–277,
https://doi.org/10.1016/s0031-0182(98)00223-5, 1999.
Ridley, H. E., Asmerom, Y., Baldini, J. U. L., Breitenbach, S. F. M., Aquino,
V. V, Prufer, K. M., Culleton, B. J., Polyak, V., Lechleitner, F. A.,
Kennett, D. J., Zhang, M., Marwan, N., Macpherson, C. G., Baldini, L. M.,
Xiao, T., Peterkin, J. L., Awe, J., and Haug, G. H.: Aerosol forcing of the
position of the intertropical convergence zone since ad 1550, Nat. Geosci.,
8, 195–200, https://doi.org/10.1038/ngeo2353, 2015.
Ruan, J., Kherbouche, F., Genty, D., Blamart, D., Cheng, H., Dewilde, F.,
Hachi, S., Edwards, R. L., Régnier, E., and Michelot, J.-L.: Evidence of
a prolonged drought ca. 4200 yr BP correlated with prehistoric settlement
abandonment from the Gueldaman GLD1 Cave, Northern Algeria, Clim. Past, 12,
1–14, https://doi.org/10.5194/cp-12-1-2016, 2016.
Rudzka, D., McDermott, F., Baldini, L. M., Fleitmann, D., Moreno, A., and
Stoll, H.: The coupled δ13C-radiocarbon systematics of three Late
Glacial/early Holocene speleothems; insights into soil and cave processes at
climatic transitions, Geochim. Cosmochim. Acta, 75, 4321–4339,
https://doi.org/10.1016/j.gca.2011.05.022, 2011.
Rudzka, D., Mcdermott, F., and Surić, M.: A late Holocene climate record
in stalagmites from Modrič Cave (Croatia), J. Quaternary Sci., 27,
585–596, https://doi.org/10.1002/jqs.2550, 2012.
Salomons, W. and Mook, W. G.: Isotope geochemistry of carbonates in the
weathering zone, in Handbook of environmental isotope geochemistry, 239–269,
1986.
Schmidt, G. A., LeGrande, A. N., and Hoffmann, G.: Water isotope expressions
of intrinsic and forced variability in a coupled ocean-atmosphere model, J.
Geophys. Res., 112, D10103, https://doi.org/10.1029/2006JD007781, 2007.
Schmidt, G. A., Annan, J. D., Bartlein, P. J., Cook, B. I., Guilyardi, E.,
Hargreaves, J. C., Harrison, S. P., Kageyama, M., LeGrande, A. N., Konecky,
B., Lovejoy, S., Mann, M. E., Masson-Delmotte, V., Risi, C., Thompson, D.,
Timmermann, A., Tremblay, L.-B., and Yiou, P.: Using palaeo-climate
comparisons to constrain future projections in CMIP5, Clim. Past, 10,
221–250, https://doi.org/10.5194/cp-10-221-2014, 2014.
Scholz, D. and Hoffmann, D. L.: StalAge – An algorithm designed for
construction of speleothem age models, Quat. Geochronol., 6, 369–382,
https://doi.org/10.1016/J.QUAGEO.2011.02.002, 2011.
Scholz, D., Frisia, S., Borsato, A., Spötl, C., Fohlmeister, J.,
Mudelsee, M., Miorandi, R., and Mangini, A.: Holocene climate variability in
north-eastern Italy: potential influence of the NAO and solar activity
recorded by speleothem data, Clim. Past, 8, 1367–1383,
https://doi.org/10.5194/cp-8-1367-2012, 2012.
Scroxton, N., Burns, S. J., McGee, D., Hardt, B., Godfrey, L. R.,
Ranivoharimanana, L., and Faina, P.: Hemispherically in-phase precipitation
variability over the last 1700 years in a Madagascar speleothem record,
Quaternary Sci. Rev., 164, 25–36, https://doi.org/10.1016/j.quascirev.2017.03.017, 2017.
Shah, A. M., Morrill, C., Gille, E. P., Gross, W. S., Anderson, D. M., Bauer,
B. A., Buckner, R., and Hartman, M.: Global Speleothem Oxygen Isotope
Measurements Since the Last Glacial Maximum, Dataset Pap. Geosci., 2013,
1–9, https://doi.org/10.7167/2013/548048, 2013.
Shakun, J. D., Burns, S. J., Fleitmann, D., Kramers, J., Matter, A., and
Al-Subary, A.: A high-resolution, absolute-dated deglacial speleothem record
of Indian Ocean climate from Socotra Island, Yemen, Earth Planet. Sci. Lett.,
259, 442–456, https://doi.org/10.1016/j.epsl.2007.05.004, 2007.
Shakun, J. D., Burns, S. J., Clark, P. U., Cheng, H., and Edwards, R. L.:
Milankovitch-paced Termination II in a Nevada speleothem?, Geophys. Res.
Lett., 38, L18701, https://doi.org/10.1029/2011GL048560, 2011.
Siklósy, Z., Demény, A., Vennemann, T. W., Pilet, S., Kramers, J.,
Leél-Össy, S., Bondár, M., Shen, C.-C., and Hegner, E.: Bronze
Age volcanic event recorded in stalagmites by combined isotope and trace
element studies, Rapid Commun. Mass Spectrom., 23, 801–808,
https://doi.org/10.1002/rcm.3943, 2009.
Sinha, A., Cannariato, K. G., Stott, L. D., Li, H.-C., You, C.-F., Cheng, H.,
Edwards, R. L., and Singh, I. B.: Variability of Southwest Indian summer
monsoon precipitation during the Bølling-Ållerød, Geology, 33,
813–816, https://doi.org/10.1130/G21498.1, 2005.
Sinha, A., Cannariato, K. G., Stott, L. D., Cheng, H., Edwards, R. L.,
Yadava, M. G., Ramesh, R., and Singh, I. B.: A 900-year (600 to 1500 A.D.)
record of the Indian summer monsoon precipitation from the core monsoon zone
of India, Geophys. Res. Lett., 34, L16707, https://doi.org/10.1029/2007gl030431, 2007.
Sinha, A., Berkelhammer, M., Stott, L., Mudelsee, M., Cheng, H., and Biswas,
J.: The leading mode of Indian Summer Monsoon precipitation variability
during the last millennium, Geophys. Res. Lett., 38, L15703,
https://doi.org/10.1029/2011gl047713, 2011.
Sinha, A., Kathayat, G., Cheng, H., Breitenbach, S. F. M., Berkelhammer, M.,
Mudelsee, M., Biswas, J., and Edwards, R. L.: Trends and oscillations in the
Indian summer monsoon rainfall over the last two millennia, Nat. Commun., 6,
6309, https://doi.org/10.1038/ncomms7309, 2015.
Sletten, H. R., Railsback, L. B., Liang, F., Brook, G. A., Marais, E., Hardt,
B. F., Cheng, H., and Edwards, R. L.: A petrographic and geochemical record
of climate change over the last 4600years from a northern Namibia stalagmite,
with evidence of abruptly wetter climate at the beginning of southern
Africa's Iron Age, Palaeogeogr. Palaeocl., 376, 149–162,
https://doi.org/10.1016/j.palaeo.2013.02.030, 2013.
Smart, P. L. and Friederich, H.: Water movement and storage in the
unsaturated zone of a maturely karstified carbonate aquifer, Mendip Hills,
England, in Proceedings of the Environmental Problems in Karst Terranes and
their Solutions Conference, 57–87, available at:
https://ci.nii.ac.jp/naid/10012582404/ (last access: 29 January 2018),
1987.
Smith, A. C., Wynn, P. M., Barker, P. A., Leng, M. J., Noble, S. R., and
Tych, W.: North Atlantic forcing of moisture delivery to Europe throughout
the Holocene, Sci. Rep., 6, 24745, https://doi.org/10.1038/srep24745, 2016.
Sone, T., Kano, A., Okumura, T., Kashiwagi, K., Hori, M., Jiang, X., and
Shen, C.-C.: Holocene stalagmite oxygen isotopic record from the Japan Sea
side of the Japanese Islands, as a new proxy of the East Asian winter
monsoon, Quaternary Sci. Rev., 75, 150–160,
https://doi.org/10.1016/j.quascirev.2013.06.019, 2013.
Spötl, C. and Mangini, A.: Stalagmite from the Austrian Alps reveals
Dansgaard-Oeschger events during isotope stage 3: Implications for the
absolute chronology of Greenland ice cores, Earth Planet. Sci. Lett., 203,
507–518, https://doi.org/10.1016/S0012-821X(02)00837-3, 2002.
Spötl, C., Fairchild, I. J., and Tooth, A. F.: Cave air control on
dripwater geochemistry, Obir Caves (Austria): Implications for speleothem
deposition in dynamically ventilated caves, Geochim. Cosmochim. Acta, 69,
2451–2468, https://doi.org/10.1016/j.gca.2004.12.009, 2005.
Spötl, C., Mangini, A., and Richards, D. A.: Chronology and
paleoenvironment of Marine Isotope Stage 3 from two high-elevation
speleothems, Austrian Alps, Quaternary Sci. Rev., 25, 1127–1136,
https://doi.org/10.1016/j.quascirev.2005.10.006, 2006.
Spötl, C., Scholz, D., and Mangini, A.: A terrestrial U∕Th-dated
stable isotope record of the Penultimate Interglacial, Earth Planet. Sci.
Lett., 276, 283–292, https://doi.org/10.1016/j.epsl.2008.09.029, 2008.
Springer, G. S., Rowe, H. D., Hardt, B., Cheng, H., and Edwards, R. L.: East
central North America climates during marine isotope stages 3-5, Geophys.
Res. Lett., 41, 3233–3237, https://doi.org/10.1002/2014gl059884, 2014.
Steen-Larsen, H. C., Risi, C., Werner, M., Yoshimura, K., and
Masson-Delmotte, V.: Evaluating the skills of isotope-enabled general
circulation models against in situ atmospheric water vapor isotope
observations, J. Geophys. Res.-Atmos., 122, 246–263,
https://doi.org/10.1002/2016JD025443, 2017.
Stevenson, C., Lee-Thorp, J. A., and Holmgren, K.: A 3000-year isotopic
record from a stalagmite in Cold Air Cave, Makapansgat Valley, Northern
Province, S. Afr. J. Sci., 95, 46–48, available at:
https://journals.co.za/content/sajsci/95/1/AJA00382353_7827 (last access: 30 May 2018), 1999.
Strikis, N. M., Cruz, F. W., Cheng, H., Karmann, I., Edwards, R. L., Vuille,
M., Wang, X., de Paula, M. S., Novello, V. F., and Auler, A. S.: Abrupt
variations in South American monsoon rainfall during the Holocene based on a
speleothem record from central-eastern Brazil, Geology, 39, 1075–1078,
https://doi.org/10.1130/g32098.1, 2011.
Stríkis, N. M., Chiessi, C. M., Cruz, F. W., Vuille, M., Cheng, H., de
Souza Barreto, E. A., Mollenhauer, G., Kasten, S., Karmann, I., Edwards, R.
L., Bernal, J. P., and Sales, H. dos R.: Timing and structure of Mega-SACZ
events during Heinrich Stadial 1, Geophys. Res. Lett., 42, 5477–5484A,
https://doi.org/10.1002/2015GL064048, 2015.
Sturm, C., Zhang, Q., and Noone, D.: An introduction to stable water isotopes
in climate models: benefits of forward proxy modelling for paleoclimatology,
Clim. Past, 6, 115–129, https://doi.org/10.5194/cp-6-115-2010, 2010.
Sundqvist, H. S., Holmgren, K., and Lauritzen, S.-E.: Stable isotope
variations in stalagmites from northwestern Sweden document climate and
environmental changes during the early Holocene, The Holocene, 17, 259–267,
https://doi.org/10.1177/0959683607073292, 2007.
Sundqvist, H. S., Holmgren, K., Moberg, A., Spötl, C., and Mangini, A.:
Stable isotopes in a stalagmite from NW Sweden document environmental changes
over the past 4000 years, Boreas, 39, 77–86,
https://doi.org/10.1111/j.1502-3885.2009.00099.x, 2010.
Sundqvist, H. S., Holmgren, K., Fohlmeister, J., Zhang, Q., Matthews, M. B.,
Spötl, C., and Körnich, H.: Evidence of a large cooling between 1690
and 1740 AD in southern Africa, Sci. Rep., 3, 1767, https://doi.org/10.1038/srep01767,
2013.
Talma, A. S. and Vogel, J. C.: Late Quaternary Paleotemperatures Derived from
a Speleothem from Cango Caves, Cape Province, South Africa, Quaternary Res.,
37, 203–213, https://doi.org/10.1016/0033-5894(92)90082-t, 1992.
Tan, L., Cai, Y., Cheng, H., An, Z., and Edwards, R. L.: Summer monsoon
precipitation variations in central China over the past 750years derived from
a high-resolution absolute-dated stalagmite, Palaeogeogr. Palaeocl., 280,
432–439, https://doi.org/10.1016/j.palaeo.2009.06.030, 2009.
Tan, L., Cai, Y., An, Z., Edwards, R. L., Cheng, H., Shen, C.-C., and Zhang,
H.: Centennial- to decadal-scale monsoon precipitation variability in the
semi-humid region, northern China during the last 1860 years: Records from
stalagmites in Huangye Cave, The Holocene, 21, 287–296,
https://doi.org/10.1177/0959683610378880, 2010.
Treble, P. C., Baker, A., Ayliffe, L. K., Cohen, T. J., Hellstrom, J. C.,
Gagan, M. K., Frisia, S., Drysdale, R. N., Griffiths, A. D., and Borsato, A.:
Hydroclimate of the Last Glacial Maximum and deglaciation in southern
Australia's arid margin interpreted from speleothem records (23–15 ka),
Clim. Past, 13, 667–687, https://doi.org/10.5194/cp-13-667-2017, 2017.
Tremaine, D. M., Froelich, P. N., and Wang, Y.: Speleothem calcite farmed in
situ: Modern calibration of δ18O and δ13C paleoclimate
proxies in a continuously-monitored natural cave system, Geochim. Cosmochim.
Acta, 75, 4929–4950, https://doi.org/10.1016/J.GCA.2011.06.005, 2011.
Trouet, V., Esper, J., Graham, N. E., Baker, A., Scourse, J. D., and Frank,
D. C.: Persistent Positive North Atlantic Oscillation Mode Dominated the
Medieval Climate Anomaly, Science, 324, 78–80, https://doi.org/10.1126/science.1166349,
2009.
Ünal-İmer, E., Shulmeister, J., Zhao, J.-X., Tonguç Uysal, I.,
Feng, Y.-X., Duc Nguyen, A., and Yüce, G.: An 80 kyr-long continuous
speleothem record from Dim Cave, SW Turkey with paleoclimatic implications
for the Eastern Mediterranean, Sci. Rep., 5, 13560, https://doi.org/10.1038/srep13560,
2015.
Vaks, A., Bar-Matthews, M., Ayalon, A., Schilman, B., Gilmour, M.,
Hawkesworth, C. J., Frumkin, A., Kaufman, A., and Matthews, A.: Paleoclimate
reconstruction based on the timing of speleothem growth and oxygen and carbon
isotope composition in a cave located in the rain shadow in Israel,
Quaternary Res., 59, 182–193, https://doi.org/10.1016/s0033-5894(03)00013-9, 2003.
Vansteenberge, S., Verheyden, S., Cheng, H., Edwards, R. L., Keppens, E., and
Claeys, P.: Paleoclimate in continental northwestern Europe during the Eemian
and early Weichselian (125–97 ka): insights from a Belgian speleothem,
Clim. Past, 12, 1445–1458, https://doi.org/10.5194/cp-12-1445-2016, 2016.
Voarintsoa, N. R. G., Wang, L., Railsback, L. B., Brook, G. A., Liang, F.,
Cheng, H., and Edwards, R. L.: Multiple proxy analyses of a U∕Th-dated
stalagmite to reconstruct paleoenvironmental changes in northwestern
Madagascar between 370CE and 1300CE, Palaeogeogr. Palaeocl., 469, 138–155,
https://doi.org/10.1016/j.palaeo.2017.01.003, 2017a.
Voarintsoa, N. R. G., Brook, G. A., Liang, F., Marais, E., Hardt, B., Cheng,
H., Edwards, R. L., and Railsback, L. B.: Stalagmite multi-proxy evidence of
wet and dry intervals in northeastern Namibia: Linkage to latitudinal shifts
of the Inter-Tropical Convergence Zone and changing solar activity from AD
1400 to 1950, The Holocene, 27, 384–396, https://doi.org/10.1177/0959683616660170,
2017b.
Voarintsoa, N. R. G., Railsback, L. B., Brook, G. A., Wang, L., Kathayat, G.,
Cheng, H., Li, X., Edwards, R. L., Rakotondrazafy, A. F. M., and Madison
Razanatseheno, M. O.: Three distinct Holocene intervals of stalagmite
deposition and nondeposition revealed in NW Madagascar, and their
paleoclimate implications, Clim. Past, 13, 1771–1790,
https://doi.org/10.5194/cp-13-1771-2017, 2017c.
Vogel, J. C.: 14C Variations During the Upper Pleistocene, Radiocarbon,
25, 213–218, https://doi.org/10.1017/s0033822200005506, 1983.
Vogel, J. C. and Kronfeld, J.: Calibration of Radiocarbon Dates for the Late
Pleistocene Using U∕Th Dates on Stalagmites, Radiocarbon, 39, 27–32,
https://doi.org/10.1017/s003382220004087x, 1997.
Wagner, J. D. M., Cole, J. E., Beck, J. W., Patchett, P. J., Henderson, G.
M., and Barnett, H. R.: Moisture variability in the southwestern United
States linked to abrupt glacial climate change, Nat. Geosci., 3, 110–113,
https://doi.org/10.1038/ngeo707, 2010.
Wainer, K., Genty, D., Blamart, D., Hoffmann, D., and Couchoud, I.: A new
stage 3 millennial climatic variability record from a SW France speleothem,
Palaeogeogr. Palaeocl., 271, 130–139, https://doi.org/10.1016/j.palaeo.2008.10.009,
2009.
Wainer, K., Genty, D., Blamart, D., Daëron, M., Bar-Matthews, M., Vonhof,
H., Dublyansky, Y., Pons-Branchu, E., Thomas, L., van Calsteren, P., Quinif,
Y., and Caillon, N.: Speleothem record of the last 180 ka in Villars cave
(SW France): Investigation of a large δ18O shift between MIS6 and
MIS5, Quaternary Sci. Rev., 30, 130–146,
https://doi.org/10.1016/j.quascirev.2010.07.004, 2011.
Wang, X., Auler, A. S., Edwards, R. L., Cheng, H., Cristalli, P. S., Smart,
P. L., Richards, D. A., and Shen, C.-C.: Wet periods in northeastern Brazil
over the past 210 kyr linked to distant climate anomalies, Nature, 432,
740–743, https://doi.org/10.1038/nature03067, 2004.
Wang, X., Edwards, R. L., Auler, A. S., Cheng, H., Kong, X., Wang, Y., Cruz,
F. W., Dorale, J. A., and Chiang, H.-W.: Hydroclimate changes across the
Amazon lowlands over the past 45,000 years, Nature, 541, 204–207,
https://doi.org/10.1038/nature20787, 2017.
Wang, Y., Cheng, H., Edwards, R. L., Kong, X., Shao, X., Chen, S., Wu, J.,
Jiang, X., Wang, X., and An, Z.: Millennial- and orbital-scale changes in the
East Asian monsoon over the past 224,000 years, Nature, 451, 1090–1093,
https://doi.org/10.1038/nature06692, 2008.
Wang, Y. J.: A High-Resolution Absolute-Dated Late Pleistocene Monsoon Record
from Hulu Cave, China, Science, 294, 2345–2348, https://doi.org/10.1126/science.1064618,
2001.
Wassenburg, J. A., Dietrich, S., Fietzke, J., Fohlmeister, J., Jochum, K. P.,
Scholz, D., Richter, D. K., Sabaoui, A., Spötl, C., Lohmann, G., Andreae,
M., and Immenhauser, A.: Reorganization of the North Atlantic Oscillation
during early Holocene deglaciation, Nat. Geosci., 9, 602–605,
https://doi.org/10.1038/ngeo2767, 2016.
Webster, J. W., Brook, G. A., Railsback, L. B., Cheng, H., Edwards, R. L.,
Alexander, C., and Reeder, P. P.: Stalagmite evidence from Belize indicating
significant droughts at the time of Preclassic Abandonment, the Maya Hiatus,
and the Classic Maya collapse, Palaeogeogr. Palaeocl., 250, 1–17,
https://doi.org/10.1016/j.palaeo.2007.02.022, 2007.
Werner, M., Langebroek, P. M., Carlsen, T., Herold, M., and Lohmann, G.:
Stable water isotopes in the ECHAM5 general circulation model: Toward
high-resolution isotope modeling on a global scale, J. Geophys. Res.-Atmos.,
116, D15109, https://doi.org/10.1029/2011JD015681, 2011.
Whittaker, T. E.: High-resolution speleothem-based palaeoclimate records from
New Zealand reveal robust teleconnection to North Atlantic during MIS 1-4,
PhD Thesis, The University of Waikato, available at:
https://hdl.handle.net/10289/2575 (last access: 2 February 2018), 2008.
Whittaker, T. E., Hendy, C. H., and Hellstrom, J. C.: Abrupt millennial-scale
changes in intensity of Southern Hemisphere westerly winds during marine
isotope stages 2–4, Geology, 39, 455–458, https://doi.org/10.1130/G31827.1, 2011.
Williams, P. W., King, D. N. T., Zhao, J.-X., and Collerson, K. D.:
Speleothem master chronologies: combined Holocene 18O and 13C
records from the North Island of New Zealand and their palaeoenvironmental
interpretation, The Holocene, 14, 194–208, https://doi.org/10.1191/0959683604hl676rp,
2004.
Williams, P. W., King, D. N. T., Zhao, J.-X., and Collerson, K. D.: Late
Pleistocene to Holocene composite speleothem 18O and 13C
chronologies from South Island, New Zealand – did a global Younger Dryas
really exist?, Earth Planet. Sci. Lett., 230, 301–317,
https://doi.org/10.1016/j.epsl.2004.10.024, 2005.
Winter, A., Miller, T., Kushnir, Y., Sinha, A., Timmermann, A., Jury, M. R.,
Gallup, C., Cheng, H., and Edwards, R. L.: Evidence for 800 years of North
Atlantic multi-decadal variability from a Puerto Rican speleothem, Earth
Planet. Sci. Lett., 308, 23–28, https://doi.org/10.1016/j.epsl.2011.05.028, 2011.
Wong, C. I., Banner, J. L., and Musgrove, M.: Holocene climate variability in
Texas, USA: An integration of existing paleoclimate data and modeling with a
new, high-resolution speleothem record, Quaternary Sci. Rev., 127, 155–173,
https://doi.org/10.1016/j.quascirev.2015.06.023, 2015.
Wortham, B. E., Wong, C. I., Silva, L. C. R., McGee, D., Montañez, I. P.,
Troy Rasbury, E., Cooper, K. M., Sharp, W. D., Glessner, J. J. G., and
Santos, R. V: Assessing response of local moisture conditions in central
Brazil to variability in regional monsoon intensity using speleothem
87Sr/86Sr values, Earth Planet. Sci. Lett., 463, 310–322,
https://doi.org/10.1016/j.epsl.2017.01.034, 2017.
Yoshimura, K., Kanamitsu, M., Noone, D., and Oki, T.: Historical isotope
simulation using Reanalysis atmospheric data, J. Geophys. Res.-Atmos., 113,
D19108, https://doi.org/10.1029/2008JD010074, 2008.
Yuan, D.: Timing, Duration, and Transitions of the Last Interglacial Asian
Monsoon, Science, 304, 575–578, https://doi.org/10.1126/science.1091220, 2004.
Zanchetta, G., Regattieri, E., Isola, I., Drysdale, R. N., Bini, M.,
Baneschi, I., and Hellstrom, J. C.: The so-called “4.2 event” in the
central Mediterranean and its climatic teleconnections, Alp. Mediterr. Quat.,
29, 5–17, available at:
http://amq.aiqua.it/index.php/issues-2012-2017/alpine-and-mediterranean-quaternary-29-1-2016/12-the-so-called-4-2-event-in-the-central-mediterranean-and-
its-climatic-teleconnections (last access: 15 January 2018), 2016.
Zhang, T.-T., Li, T.-Y., Cheng, H., Edwards, R. L., Shen, C.-C., Spötl,
C., Li, H.-C., Han, L.-Y., Li, J.-Y., Huang, C.-X., and Zhao, X.:
Stalagmite-inferred centennial variability of the Asian summer monsoon in
southwest China between 58 and 79 ka BP, Quaternary Sci. Rev., 160, 1–12,
https://doi.org/10.1016/j.quascirev.2017.02.003, 2017.
Zhou, H., Zhao, J., Zhang, P., Shen, C.-C., Chi, B., Feng, Y., Lin, Y., Guan,
H., and You, C.-F.: Decoupling of stalagmite-derived Asian summer monsoon
records from North Atlantic temperature change during marine oxygen isotope
stage 5d, Quaternary Res., 70, 315–321, https://doi.org/10.1016/j.yqres.2008.04.007,
2008.
Download
The requested paper has a corresponding corrigendum published. Please read the corrigendum first before downloading the article.
- Article
(1670 KB) - Full-text XML
- Corrigendum
- Companion paper
-
Supplement
(320 KB) - BibTeX
- EndNote
Short summary
This paper is an overview of the contents of the SISAL database and its structure. The database contains oxygen and carbon isotope measurements from 371 individual speleothem records and 10 composite records from 174 cave systems from around the world. The SISAL database is created by a collective effort of the members of the Past Global Changes SISAL working group, which aims to provide a comprehensive compilation of speleothem isotope records for climate reconstruction and model evaluation.
This paper is an overview of the contents of the SISAL database and its structure. The database...
Altmetrics
Final-revised paper
Preprint