Articles | Volume 10, issue 4
Earth Syst. Sci. Data, 10, 2123–2139, 2018
https://doi.org/10.5194/essd-10-2123-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Earth Syst. Sci. Data, 10, 2123–2139, 2018
https://doi.org/10.5194/essd-10-2123-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Brief communication
30 Nov 2018
Brief communication
| 30 Nov 2018
OCTOPUS: an open cosmogenic isotope and luminescence database
Alexandru T. Codilean et al.
Related authors
Klaus M. Wilcken, Alexandru T. Codilean, Réka-H. Fülöp, Steven Kotevski, Anna H. Rood, Dylan H. Rood, Alexander J. Seal, and Krista Simon
Geochronology, 4, 339–352, https://doi.org/10.5194/gchron-4-339-2022, https://doi.org/10.5194/gchron-4-339-2022, 2022
Short summary
Short summary
Cosmogenic nuclides are now widely applied in the Earth sciences; however, more recent applications often push the analytical limits of the technique. Our study presents a comprehensive method for analysis of cosmogenic 10Be and 26Al samples down to isotope concentrations of a few thousand atoms per gram of sample, which opens the door to new and more varied applications of cosmogenic nuclide analysis.
Alexandru T. Codilean, Henry Munack, Wanchese M. Saktura, Tim J. Cohen, Zenobia Jacobs, Sean Ulm, Paul P. Hesse, Jakob Heyman, Katharina J. Peters, Alan N. Williams, Rosaria B. K. Saktura, Xue Rui, Kai Chishiro-Dennelly, and Adhish Panta
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2022-50, https://doi.org/10.5194/essd-2022-50, 2022
Preprint under review for ESSD
Short summary
Short summary
OCTOPUS v.2 is a web-enabled database that allows users to visualise, query, and download cosmogenic radionuclide, luminescence, and radiocarbon ages and denudation rates associated with erosional landscapes, Quaternary depositional landforms and archaeological records, along with ancillary geospatial data layers. OCTOPUS v.2 hosts five major data collections. Supporting data are comprehensive and include bibliographic, contextual, and sample preparation and measurement related information.
Martin Struck, John D. Jansen, Toshiyuki Fujioka, Alexandru T. Codilean, David Fink, Réka-Hajnalka Fülöp, Klaus M. Wilcken, David M. Price, Steven Kotevski, L. Keith Fifield, and John Chappell
Earth Surf. Dynam., 6, 329–349, https://doi.org/10.5194/esurf-6-329-2018, https://doi.org/10.5194/esurf-6-329-2018, 2018
Short summary
Short summary
Measurements of cosmogenic nuclides 10Be and 26Al in sediment along central Australian streams show that lithologically controlled magnitudes of source-area erosion rates (0.2–11 m Myr-1) are preserved downstream despite sediment mixing. Conversely, downstream-increasing sediment burial signals (> 400 kyr) indicate sediment incorporation from adjacent, long-exposed storages, which, combined with low sediment supply and discontinuous flux, likely favours source-area 10Be–26Al signal masking.
J. K. Willenbring, A. T. Codilean, K. L. Ferrier, B. McElroy, and J. W. Kirchner
Earth Surf. Dynam. Discuss., https://doi.org/10.5194/esurfd-2-1-2014, https://doi.org/10.5194/esurfd-2-1-2014, 2014
Revised manuscript has not been submitted
Klaus M. Wilcken, Alexandru T. Codilean, Réka-H. Fülöp, Steven Kotevski, Anna H. Rood, Dylan H. Rood, Alexander J. Seal, and Krista Simon
Geochronology, 4, 339–352, https://doi.org/10.5194/gchron-4-339-2022, https://doi.org/10.5194/gchron-4-339-2022, 2022
Short summary
Short summary
Cosmogenic nuclides are now widely applied in the Earth sciences; however, more recent applications often push the analytical limits of the technique. Our study presents a comprehensive method for analysis of cosmogenic 10Be and 26Al samples down to isotope concentrations of a few thousand atoms per gram of sample, which opens the door to new and more varied applications of cosmogenic nuclide analysis.
Fiona J. Clubb, Eliot F. Weir, and Simon M. Mudd
Earth Surf. Dynam., 10, 437–456, https://doi.org/10.5194/esurf-10-437-2022, https://doi.org/10.5194/esurf-10-437-2022, 2022
Short summary
Short summary
River valleys are important components of mountain systems: they are the most fertile part of landscapes and store sediment which is transported from mountains to surrounding basins. Our knowledge of the location and shape of valleys is hindered by our ability to measure them over large areas. We present a new method for measuring the width of mountain valleys continuously along river channels from digital topography and show that our method can be used to test common models of river widening.
Alexandru T. Codilean, Henry Munack, Wanchese M. Saktura, Tim J. Cohen, Zenobia Jacobs, Sean Ulm, Paul P. Hesse, Jakob Heyman, Katharina J. Peters, Alan N. Williams, Rosaria B. K. Saktura, Xue Rui, Kai Chishiro-Dennelly, and Adhish Panta
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2022-50, https://doi.org/10.5194/essd-2022-50, 2022
Preprint under review for ESSD
Short summary
Short summary
OCTOPUS v.2 is a web-enabled database that allows users to visualise, query, and download cosmogenic radionuclide, luminescence, and radiocarbon ages and denudation rates associated with erosional landscapes, Quaternary depositional landforms and archaeological records, along with ancillary geospatial data layers. OCTOPUS v.2 hosts five major data collections. Supporting data are comprehensive and include bibliographic, contextual, and sample preparation and measurement related information.
Daniel L. Evans, John N. Quinton, Andrew M. Tye, Ángel Rodés, Jessica A. C. Davies, Simon M. Mudd, and Timothy A. Quine
SOIL, 5, 253–263, https://doi.org/10.5194/soil-5-253-2019, https://doi.org/10.5194/soil-5-253-2019, 2019
Short summary
Short summary
Policy to conserve thinning arable soils relies on a balance between the rates of soil erosion and soil formation. Our knowledge of the latter is meagre. Here, we present soil formation rates for an arable hillslope, the first of their kind globally, and a woodland hillslope, the first of their kind in Europe. Rates range between 26 and 96 mm kyr−1. On the arable site, erosion rates are 2 orders of magnitude greater, and in a worst-case scenario, bedrock exposure could occur in 212 years.
Boris Gailleton, Simon M. Mudd, Fiona J. Clubb, Daniel Peifer, and Martin D. Hurst
Earth Surf. Dynam., 7, 211–230, https://doi.org/10.5194/esurf-7-211-2019, https://doi.org/10.5194/esurf-7-211-2019, 2019
Short summary
Short summary
The shape of landscapes is influenced by climate changes, faulting or the nature of the rocks under the surface. One of the most sensitive parts of the landscape to these changes is the river system that eventually adapts to such changes by adapting its slope, the most extreme example being a waterfall. We here present an algorithm that extracts changes in river slope over large areas from satellite data with the aim of investigating climatic, tectonic or geologic changes in the landscape.
Simon M. Mudd, Fiona J. Clubb, Boris Gailleton, and Martin D. Hurst
Earth Surf. Dynam., 6, 505–523, https://doi.org/10.5194/esurf-6-505-2018, https://doi.org/10.5194/esurf-6-505-2018, 2018
Short summary
Short summary
Rivers can reveal information about erosion rates, tectonics, and climate. In order to make meaningful inferences about these influences, one must be able to compare headwaters to downstream parts of the river network. We describe new methods for normalizing river steepness for drainage area to better understand how rivers record erosion rates in eroding landscapes.
Martin Struck, John D. Jansen, Toshiyuki Fujioka, Alexandru T. Codilean, David Fink, Réka-Hajnalka Fülöp, Klaus M. Wilcken, David M. Price, Steven Kotevski, L. Keith Fifield, and John Chappell
Earth Surf. Dynam., 6, 329–349, https://doi.org/10.5194/esurf-6-329-2018, https://doi.org/10.5194/esurf-6-329-2018, 2018
Short summary
Short summary
Measurements of cosmogenic nuclides 10Be and 26Al in sediment along central Australian streams show that lithologically controlled magnitudes of source-area erosion rates (0.2–11 m Myr-1) are preserved downstream despite sediment mixing. Conversely, downstream-increasing sediment burial signals (> 400 kyr) indicate sediment incorporation from adjacent, long-exposed storages, which, combined with low sediment supply and discontinuous flux, likely favours source-area 10Be–26Al signal masking.
Guillaume C. H. Goodwin, Simon M. Mudd, and Fiona J. Clubb
Earth Surf. Dynam., 6, 239–255, https://doi.org/10.5194/esurf-6-239-2018, https://doi.org/10.5194/esurf-6-239-2018, 2018
Short summary
Short summary
Salt marshes are valuable environments that provide multiple services to coastal communities. However, their fast-paced evolution poses a challenge to monitoring campaigns due to time-consuming processing. The Topographic Identification of Platforms (TIP) method uses high-resolution topographic data to automatically detect the limits of salt marsh platforms within a landscape. The TIP method provides sufficient accuracy to monitor salt marsh change over time, facilitating coastal management.
Fiona J. Clubb, Simon M. Mudd, David T. Milodowski, Declan A. Valters, Louise J. Slater, Martin D. Hurst, and Ajay B. Limaye
Earth Surf. Dynam., 5, 369–385, https://doi.org/10.5194/esurf-5-369-2017, https://doi.org/10.5194/esurf-5-369-2017, 2017
Short summary
Short summary
Floodplains and fluvial terraces can provide information about current and past river systems, helping to reveal how channels respond to changes in both climate and tectonics. We present a new method of identifying these features objectively from digital elevation models by analysing their slope and elevation compared to the modern river. We test our method in eight field sites, and find that it provides rapid and reliable extraction of floodplains and terraces across a range of landscapes.
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.
Simon Marius Mudd, Marie-Alice Harel, Martin D. Hurst, Stuart W. D. Grieve, and Shasta M. Marrero
Earth Surf. Dynam., 4, 655–674, https://doi.org/10.5194/esurf-4-655-2016, https://doi.org/10.5194/esurf-4-655-2016, 2016
Short summary
Short summary
Cosmogenic nuclide concentrations are widely used to calculate catchment-averaged denudation rates. Despite their widespread use, there is currently no open source method for calculating such rates, and the methods used to calculate catchment-averaged denudation rates vary widely between studies. Here we present an automated, open-source method for calculating basin averaged denudation rates, which may be used as a stand-alone calculator or as a front end to popular online calculators.
Stuart W. D. Grieve, Simon M. Mudd, David T. Milodowski, Fiona J. Clubb, and David J. Furbish
Earth Surf. Dynam., 4, 627–653, https://doi.org/10.5194/esurf-4-627-2016, https://doi.org/10.5194/esurf-4-627-2016, 2016
Short summary
Short summary
High-resolution topographic data are becoming more prevalent, yet many areas of geomorphic interest do not have such data available. We produce topographic data at a range of resolutions to explore the influence of decreasing resolution of data on geomorphic analysis. We test the accuracy of the calculation of curvature, a hillslope sediment transport coefficient, and the identification of channel networks, providing guidelines for future use of these methods on low-resolution topographic data.
Stuart W. D. Grieve, Simon M. Mudd, Martin D. Hurst, and David T. Milodowski
Earth Surf. Dynam., 4, 309–325, https://doi.org/10.5194/esurf-4-309-2016, https://doi.org/10.5194/esurf-4-309-2016, 2016
Short summary
Short summary
Relationships between the erosion rate and topographic relief of hillslopes have been demonstrated in a number of diverse settings and such patterns can be used to identify the impact of tectonic plate motion on the Earth's surface. Here we present an open-source software tool which can be used to explore these relationships in any landscape where high-resolution topographic data have been collected.
D. T. Milodowski, S. M. Mudd, and E. T. A. Mitchard
Earth Surf. Dynam., 3, 483–499, https://doi.org/10.5194/esurf-3-483-2015, https://doi.org/10.5194/esurf-3-483-2015, 2015
Short summary
Short summary
Rock is exposed at the Earth surface when erosion rates locally exceed rates of soil production. This transition is marked by a diagnostic increase in topographic roughness, which we demonstrate can be a powerful indicator of the location of rock outcrop in a landscape. Using this to explore how hillslopes in two landscapes respond to increasing erosion rates, we find that the transition from soil-mantled to bedrock hillslopes is patchy and spatially heterogeneous.
M. Baggs Sargood, T. J. Cohen, C. J. Thompson, and J. Croke
Earth Surf. Dynam., 3, 265–279, https://doi.org/10.5194/esurf-3-265-2015, https://doi.org/10.5194/esurf-3-265-2015, 2015
Short summary
Short summary
We document the responses of bedrock-confined rivers to an extreme flood which occurred in southeast Queensland, Australia, in 2011. Through a combination of field- and desktop-based analyses we show that widespread removal of coarse-grained mantle occurred, with boulders up to 4m in diameter being locally mobilised. We show that normalised erosion in this extreme event is scaled to basin area and that this large flood has exposed bedrock steps and straths exposing them to ongoing erosion.
M. Attal, S. M. Mudd, M. D. Hurst, B. Weinman, K. Yoo, and M. Naylor
Earth Surf. Dynam., 3, 201–222, https://doi.org/10.5194/esurf-3-201-2015, https://doi.org/10.5194/esurf-3-201-2015, 2015
Short summary
Short summary
Steeper landscapes tend to erode faster. In this study, we also find that sediment produced on steeper landscapes is coarser. Soils are coarser because fragments spend less time in the soil so are less exposed to processes that can break them down. Change in sediment sources impact the sediment transported by rivers: rivers transport sediment up to cobble size in low-slope, soil-mantled areas; they transport much coarser sediment (including boulders supplied from landslides) in the steep areas.
J. K. Willenbring, A. T. Codilean, K. L. Ferrier, B. McElroy, and J. W. Kirchner
Earth Surf. Dynam. Discuss., https://doi.org/10.5194/esurfd-2-1-2014, https://doi.org/10.5194/esurfd-2-1-2014, 2014
Revised manuscript has not been submitted
Related subject area
Geology and geochemistry
A new local meteoric water line for Inuvik (NT, Canada)
A national landslide inventory of Denmark
Description of a global marine particulate organic carbon-13 isotope data set
The Database of the Active Faults of Eurasia (AFEAD): Ontology and Design behind the Continental-Scale Dataset
Introducing GloRiSe – a global database on river sediment composition
CASCADE – The Circum-Arctic Sediment CArbon DatabasE
Synoptic analysis of a decade of daily measurements of SO2 emission in the troposphere from volcanoes of the global ground-based Network for Observation of Volcanic and Atmospheric Change
A European map of groundwater pH and calcium
Bioavailable soil and rock strontium isotope data from Israel
Isoscape of amount-weighted annual mean precipitation tritium (3H) activity from 1976 to 2017 for the Adriatic–Pannonian region – AP3H_v1 database
The dead line for oil and gas and implication for fossil resource prediction
TephraKam: geochemical database of glass compositions in tephra and welded tuffs from the Kamchatka volcanic arc (northwestern Pacific)
Global whole-rock geochemical database compilation
Gridded maps of geological methane emissions and their isotopic signature
Data on geochemical and hydraulic properties of a characteristic confined/unconfined aquifer system of the younger Pleistocene in northeast Germany
The IRHUM (Isotopic Reconstruction of Human Migration) database – bioavailable strontium isotope ratios for geochemical fingerprinting in France
Michael Fritz, Sebastian Wetterich, Joel McAlister, and Hanno Meyer
Earth Syst. Sci. Data, 14, 57–63, https://doi.org/10.5194/essd-14-57-2022, https://doi.org/10.5194/essd-14-57-2022, 2022
Short summary
Short summary
From 2015 to 2018 we collected rain and snow samples in Inuvik, Canada. We measured the stable water isotope composition of oxygen (δ18O) and hydrogen (δ2H) with a mass spectrometer. This data will be of interest for other scientists who work in the Arctic. They will be able to compare our modern data with their own isotope data in old ice, for example in glaciers, and in permafrost. This will help to correctly interpret the climate signals of the environmental history of the Earth.
Gregor Luetzenburg, Kristian Svennevig, Anders Anker Bjørk, Marie Keiding, and Aart Kroon
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2021-414, https://doi.org/10.5194/essd-2021-414, 2021
Revised manuscript accepted for ESSD
Short summary
Short summary
We produced the first landslide inventory for Denmark. Over 3200 landslides were mapped using a high-resolution elevation model and orthophotos. We implemented an independent validation into our mapping and found an overall level of completeness of 87 %. The national inventory represents a range of landslide sizes covering all regions that were covered by glacial ice during the last glacial period. This inventory will be used for investigating landslide causes and for natural hazard mitigation.
Maria-Theresia Verwega, Christopher J. Somes, Markus Schartau, Robyn Elizabeth Tuerena, Anne Lorrain, Andreas Oschlies, and Thomas Slawig
Earth Syst. Sci. Data, 13, 4861–4880, https://doi.org/10.5194/essd-13-4861-2021, https://doi.org/10.5194/essd-13-4861-2021, 2021
Short summary
Short summary
This work describes a ready-to-use collection of particulate organic carbon stable isotope ratio data sets. It covers the 1960s–2010s and all main oceans, providing meta-information and gridded data. The best coverage exists in Atlantic, Indian and Southern Ocean surface waters during the 1990s. It indicates no major difference between methods and shows decreasing values towards high latitudes, with the lowest in the Southern Ocean, and a long-term decline in all regions but the Southern Ocean.
Egor Zelenin, Dmitry Bachmanov, Sofya Garipova, Vladimir Trifonov, and Andrey Kozhurin
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2021-312, https://doi.org/10.5194/essd-2021-312, 2021
Revised manuscript accepted for ESSD
Short summary
Short summary
Active faults are faults in the Earth's crust with a possible future slip. A slip at the fault will cause an earthquake, and it draws particular attention to active faults in tectonic studies and seismic hazard assessment. We present the Active Faults of Eurasia Database (AFEAD), a high-detail continental-scale geodatabase comprising 46,775 faults. Location, name, slip characteristics, and a reference to source publications are provided for database entries.
Gerrit Müller, Jack J. Middelburg, and Appy Sluijs
Earth Syst. Sci. Data, 13, 3565–3575, https://doi.org/10.5194/essd-13-3565-2021, https://doi.org/10.5194/essd-13-3565-2021, 2021
Short summary
Short summary
Rivers are major freshwater resources, connectors and transporters on Earth. As the composition of river waters and particles results from processes in their catchment, such as erosion, weathering, environmental pollution, nutrient and carbon cycling, Earth-spanning databases of river composition are needed for studies of these processes on a global scale. While extensive resources on water and nutrient composition exist, we provide a database of river particle composition.
Jannik Martens, Evgeny Romankevich, Igor Semiletov, Birgit Wild, Bart van Dongen, Jorien Vonk, Tommaso Tesi, Natalia Shakhova, Oleg V. Dudarev, Denis Kosmach, Alexander Vetrov, Leopold Lobkovsky, Nikolay Belyaev, Robie W. Macdonald, Anna J. Pieńkowski, Timothy I. Eglinton, Negar Haghipour, Salve Dahle, Michael L. Carroll, Emmelie K. L. Åström, Jacqueline M. Grebmeier, Lee W. Cooper, Göran Possnert, and Örjan Gustafsson
Earth Syst. Sci. Data, 13, 2561–2572, https://doi.org/10.5194/essd-13-2561-2021, https://doi.org/10.5194/essd-13-2561-2021, 2021
Short summary
Short summary
The paper describes the establishment, structure and current status of the first Circum-Arctic Sediment CArbon DatabasE (CASCADE), which is a scientific effort to harmonize and curate all published and unpublished data of carbon, nitrogen, carbon isotopes, and terrigenous biomarkers in sediments of the Arctic Ocean in one database. CASCADE will enable a variety of studies of the Arctic carbon cycle and thus contribute to a better understanding of how climate change affects the Arctic.
Santiago Arellano, Bo Galle, Fredy Apaza, Geoffroy Avard, Charlotte Barrington, Nicole Bobrowski, Claudia Bucarey, Viviana Burbano, Mike Burton, Zoraida Chacón, Gustavo Chigna, Christian Joseph Clarito, Vladimir Conde, Fidel Costa, Maarten De Moor, Hugo Delgado-Granados, Andrea Di Muro, Deborah Fernandez, Gustavo Garzón, Hendra Gunawan, Nia Haerani, Thor H. Hansteen, Silvana Hidalgo, Salvatore Inguaggiato, Mattias Johansson, Christoph Kern, Manne Kihlman, Philippe Kowalski, Pablo Masias, Francisco Montalvo, Joakim Möller, Ulrich Platt, Claudia Rivera, Armando Saballos, Giuseppe Salerno, Benoit Taisne, Freddy Vásconez, Gabriela Velásquez, Fabio Vita, and Mathieu Yalire
Earth Syst. Sci. Data, 13, 1167–1188, https://doi.org/10.5194/essd-13-1167-2021, https://doi.org/10.5194/essd-13-1167-2021, 2021
Short summary
Short summary
This study presents a dataset of volcanic sulfur dioxide (SO2) emissions from 2005–2017. Measurements were obtained by Network for Observation of Volcanic and Atmospheric Change (NOVAC) scanning differential optical absorption spectrometer (ScanDOAS) instruments at 32 volcanoes and processed using a standardized procedure. We show statistics of volcanic gas emissions under a variety of conditions and compare them with averages derived from measurements from space and historical inventories.
Michal Hájek, Borja Jiménez-Alfaro, Ondřej Hájek, Lisa Brancaleoni, Marco Cantonati, Michele Carbognani, Anita Dedić, Daniel Dítě, Renato Gerdol, Petra Hájková, Veronika Horsáková, Florian Jansen, Jasmina Kamberović, Jutta Kapfer, Tiina Hilkka Maria Kolari, Mariusz Lamentowicz, Predrag Lazarević, Ermin Mašić, Jesper Erenskjold Moeslund, Aaron Pérez-Haase, Tomáš Peterka, Alessandro Petraglia, Eulàlia Pladevall-Izard, Zuzana Plesková, Stefano Segadelli, Yuliya Semeniuk, Patrícia Singh, Anna Šímová, Eva Šmerdová, Teemu Tahvanainen, Marcello Tomaselli, Yuliya Vystavna, Claudia Biţă-Nicolae, and Michal Horsák
Earth Syst. Sci. Data, 13, 1089–1105, https://doi.org/10.5194/essd-13-1089-2021, https://doi.org/10.5194/essd-13-1089-2021, 2021
Short summary
Short summary
We developed an up-to-date European map of groundwater pH and Ca (the major determinants of diversity of wetlands) based on 7577 measurements. In comparison to the existing maps, we included much a larger data set from the regions rich in endangered wetland habitats, filled the apparent gaps in eastern and southeastern Europe, and applied geospatial modelling. The latitudinal and altitudinal gradients were rediscovered with much refined regional patterns, as is associated with bedrock variation.
Ian Moffat, Rachel Rudd, Malte Willmes, Graham Mortimer, Les Kinsley, Linda McMorrow, Richard Armstrong, Maxime Aubert, and Rainer Grün
Earth Syst. Sci. Data, 12, 3641–3652, https://doi.org/10.5194/essd-12-3641-2020, https://doi.org/10.5194/essd-12-3641-2020, 2020
Short summary
Short summary
This research has measured the bioavailable strontium isotope composition of soil and rock samples from the major geological units in Israel. Plants, animals and people take up this value into their bones and teeth via food and water and so mapping these values has important implications for understanding where archaeological, ecological, food science and forensic samples are from.
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.
Xiongqi Pang, Chengzao Jia, Kun Zhang, Maowen Li, Youwei Wang, Junwen Peng, Boyuan Li, and Junqing Chen
Earth Syst. Sci. Data, 12, 577–590, https://doi.org/10.5194/essd-12-577-2020, https://doi.org/10.5194/essd-12-577-2020, 2020
Short summary
Short summary
Based on geochemical data of 13 634 source rock samples from 1286 wells and 116 489 drilling results for oil and gas from 4978 wells in six major basins of China, we proposed the concept of the active source rock depth limit. It can be used to clarify and predict the maximum depth of fossil fuel distribution in sedimentary basins. The study provides fundamental information for deep hydrocarbon exploration and also advances understanding of the vertical distribution of fossil fuels on our planet.
Maxim V. Portnyagin, Vera V. Ponomareva, Egor A. Zelenin, Lilia I. Bazanova, Maria M. Pevzner, Anastasia A. Plechova, Aleksei N. Rogozin, and Dieter Garbe-Schönberg
Earth Syst. Sci. Data, 12, 469–486, https://doi.org/10.5194/essd-12-469-2020, https://doi.org/10.5194/essd-12-469-2020, 2020
Short summary
Short summary
Tephra is fragmented material produced by explosive volcanic eruptions. Geochemically characterized tephra layers are excellent time marker horizons and samples of magma composition. TephraKam is database of the ages and chemical composition of volcanic glass in tephra from the Kamchatka volcanic arc (northwestern Pacific). TephraKam enables the identification of tephra sources, correlation and dating of natural archives, and reconstruction of spatiotemporal evolution of volcanism in Kamchatka.
Matthew Gard, Derrick Hasterok, and Jacqueline A. Halpin
Earth Syst. Sci. Data, 11, 1553–1566, https://doi.org/10.5194/essd-11-1553-2019, https://doi.org/10.5194/essd-11-1553-2019, 2019
Short summary
Short summary
We compiled a database of more than 1 million chemical analyses of igneous, sedimentary and metamorphic rocks, derived from existing databases, governmental data and academic studies. Our database enhances temporal distributions, simplifies the structure, and adds geochemical indices, naming schema, and estimates of physical properties such as density. This database provides a source for the rapid production of crustal models and chemical evolution throughout 4 billion years of geologic history.
Giuseppe Etiope, Giancarlo Ciotoli, Stefan Schwietzke, and Martin Schoell
Earth Syst. Sci. Data, 11, 1–22, https://doi.org/10.5194/essd-11-1-2019, https://doi.org/10.5194/essd-11-1-2019, 2019
Short summary
Short summary
We developed the first global maps of natural geological CH4 flux and isotopic values which can be used for new atmospheric CH4 modelling. The maps, based on updated, measured and theoretically estimated data, show that the highest geo-CH4 emissions are located in the Northern Hemisphere (N. America, Caspian region, Europe, Siberian Arctic Shelf), and that geo-CH4 is less 13C-enriched than what has been assumed so far in other studies. Other CH4 sources can now be estimated with higher accuracy.
C. Merz and J. Steidl
Earth Syst. Sci. Data, 7, 109–116, https://doi.org/10.5194/essd-7-109-2015, https://doi.org/10.5194/essd-7-109-2015, 2015
Short summary
Short summary
The paper presents a database of hydrochemical and hydraulic groundwater measurements of a younger Pleistocene aquifer system in NE Germany. The Leibniz Centre for Agricultural Landscape Research (ZALF) operates seven groundwater monitoring wells in the Quillow catchment located in the Uckermark region (Federal State of Brandenburg, Germany). This database can be used for the investigation of subsurface water geochemistry under changing hydraulic boundary conditions regarding a 14-year period.
M. Willmes, L. McMorrow, L. Kinsley, R. Armstrong, M. Aubert, S. Eggins, C. Falguères, B. Maureille, I. Moffat, and R. Grün
Earth Syst. Sci. Data, 6, 117–122, https://doi.org/10.5194/essd-6-117-2014, https://doi.org/10.5194/essd-6-117-2014, 2014
Cited articles
Aitken, M. J.: Thermoluminescence dating, Academic Press, London, 1985. a
Aitken, M. J.: An Introduction to Optical Dating, Oxford University Press,
Oxford, 1998. a
Argento, D. C., Stone, J. O., Reedy, R. C., and O'Brien, K.: Physics-based
modeling of cosmogenic nuclides part I: Radiation transport methods and new
insights, Quat. Geochronol., 26, 29–43,
https://doi.org/10.1016/j.quageo.2014.09.004, 2015a. a
Argento, D. C., Stone, J. O., Reedy, R. C., and O'Brien, K.: Physics-based
modeling of cosmogenic nuclides part II: Key aspects of in-situ cosmogenic
nuclide production, Quat. Geochronol., 26, 44–55,
https://doi.org/10.1016/j.quageo.2014.09.005, 2015b. a
Arnold, L. J., Demuro, M., Parés, J. M., Pérez-González, A., Arsuaga,
J. L., de Castro, J. M. B., and Carbonell, E.: Evaluating the suitability of
extended-range luminescence dating techniques over early and Middle
Pleistocene timescales: Published datasets and case studies from Atapuerca,
Spain, Quaternary Int., 389, 167–190,
https://doi.org/10.1016/j.quaint.2014.08.010, 2015. a
Balco, G.: Contributions and unrealized potential contributions of
cosmogenic-nuclide exposure dating to glacier chronology, 1990–2010,
Quaternary Sci. Rev., 30, 3–27, https://doi.org/10.1016/j.quascirev.2010.11.003,
2011. a
Balco, G., Stone, J. O., Lifton, N. A., and Dunai, T. J.: A complete and
easily accessible means of calculating surface exposure ages or erosion rates
from 10Be and 26Al measurements, Quat. Geochronol., 3,
174–195, https://doi.org/10.1016/j.quageo.2007.12.001, 2008. a, b, c
Bierman, P. R. and Nichols, K. K.: Rock to sediment – slope to sea with
10Be – rates of landscape change, Annu. Rev. Earth
Pl. Sc., 32, 215–255,
https://doi.org/10.1146/annurev.earth.32.101802.120539, 2004. a
Bierman, P. R. and Steig, E.: Estimating rates of denudation using
cosmogenic
isotope abundances in sediment, Earth Surf. Proc. Land., 21,
125–139,
https://doi.org/10.1002/(SICI)1096-9837(199602)21:2<125::AID-ESP511>3.0.CO;2-8, 1996. a
Borchers, B., Marrero, S., Balco, G., Caffee, M. W., Goehring, B. M., Lifton,
N. A., Nishiizumi, K., Phillips, F., Schaefer, J. M., and Stone, J. O.:
Geological calibration of spallation production rates in the CRONUS-Earth
project, Quat. Geochronol., 31, 188–198,
https://doi.org/10.1016/j.quageo.2015.01.009, 2015. a
Bourman, R. P., Prescott, J. R., Banerjee, D., Alley, N. F., and Buckman, S.:
Age and origin of alluvial sediments within and flanking the Mt Lofty
Ranges, southern South Australia: a Late Quaternary archive of climate and
environmental change, Aust. J. Earth Sci., 57, 175–192,
https://doi.org/10.1080/08120090903416260, 2010. a
Braucher, R., Merchel, S., Borgomano, J., and Bourles, D. L.: Production of
cosmogenic radionuclides at great depth: A multi element approach, Earth
Planet. Sc. Lett., 309, 1–9, https://doi.org/10.1016/j.epsl.2011.06.036, 2011. a
Bristow, C., Augustinus, P., Wallis, I., Jol, H., and Rhodes, E.:
Investigation of the age and migration of reversing dunes in Antarctica
using GPR and OSL, with implications for GPR on Mars, Earth Planet.
Sc. Lett., 289, 30–42, https://doi.org/10.1016/j.epsl.2009.10.026, 2010. a
Brown, E., Stallard, R., Larsen, M. C., Raisbeck, G., and Yiou, F.:
Denudation
Rates Determined From the Accumulation of In Situ-Produced 10Be in the
Luquillo Experimental Forest, Puerto-Rico, Earth Planet. Sc.
Lett., 129, 193–202, https://doi.org/10.1016/0012-821X(94)00249-X, 1995. a
Callen, R. and Nanson, G.: Formation and age of dunes in the Lake Eyre
Depocentres, Geol. Rundsch., 81, 589–593, https://doi.org/10.1007/BF01828619,
1992. a
Chappell, J., Zheng, H., and Fifield, K.: Yangtse River sediments and erosion
rates from source to sink traced with cosmogenic 10Be: Sediments from
major rivers, Palaeogeogr. Palaeocl., 241, 79–94, https://doi.org/10.1016/j.palaeo.2006.06.010, 2006. a, b
Chmeleff, J., von Blanckenburg, F., Kossert, K., and Jakob, D.:
Determination
of the 10Be half-life by multicollector ICP-MS and liquid scintillation
counting, Nucl. Instrum. Meth. B, 268,
192–199, https://doi.org/10.1016/j.nimb.2009.09.012, 2010. a, b
Codilean, A. T.: Calculation of the cosmogenic nuclide production
topographic
shielding scaling factor for large areas using DEMs, Earth Surf. Proc.
Land., 31, 785–794, https://doi.org/10.1002/esp.1336, 2006. a, b, c
Codilean, A. T., Cohen, T. J., and Munack, H.: OCTOPUS –CRN International,
https://doi.org/10.4225/48/5a8367feac9b2, 2017a. a
Codilean, A. T., Cohen, T. J., and Munack, H.: OCTOPUS – CRN Australia,
https://doi.org/10.4225/48/5a836cdfac9b5, 2017b. a
Codilean, A. T., Cohen, T. J., Munack, H., and Saktura, W. M.: OCTOPUS –
OSL/TL Australia, https://doi.org/10.4225/48/5a836db1ac9b6, 2017c. a
Compo, G. P., Whitaker, J. S., Sardeshmukh, P. D., Matsui, N., Allan, R. J.,
Yin, X., Gleason, B. E., Vose, R. S., Rutledge, G., Bessemoulin, P.,
Brönnimann, S., Brunet, M., Crouthamel, R. I., Grant, A. N., Groisman,
P. Y., Jones, P. D., Kruk, M. C., Kruger, A. C., Marshall, G. J., Maugeri,
M., Mok, H. Y., Nordli, O., Ross, T. F., Trigo, R. M., Wang, X. L., Woodruff,
S. D., and Worley, S. J.: The Twentieth Century Reanalysis Project, Q.
J. Roy. Meteor. Soc., 137, 1–28,
https://doi.org/10.1002/qj.776, 2011. a, b
Croke, J., Bartley, R., Chappell, J., Austin, J. M., Fifield, K., Tims,
S. G.,
Thompson, C. J., and Furuichi, T.: 10Be-derived denudation rates from
the Burdekin catchment: The largest contributor of sediment to the Great
Barrier Reef, Geomorphology, 241, 122–134,
https://doi.org/10.1016/j.geomorph.2015.04.003, 2015. a
Croke, J., Thompson, C., Denham, R., Haines, H., Sharma, A., and Pietsch, T.:
Reconstructing a millennial-scale record of flooding in a single valley
setting: the 2011 flood-affected Lockyer Valley, south-east Queensland,
Australia, J. Quaternary Sci., 31, 936–952,
https://doi.org/10.1002/jqs.2919, 2016. a, b
DiBiase, R. A.: Short communication: Increasing vertical attenuation length
of cosmogenic nuclide production on steep slopes negates topographic
shielding corrections for catchment erosion rates, Earth Surf. Dynam., 6,
923–931, https://doi.org/10.5194/esurf-6-923-2018, 2018. a, b
Dunai, T. J. and Stuart, F. M.: Reporting of cosmogenic nuclide data for
exposure age and erosion rate determinations, Quat. Geochronol., 4,
437–440, https://doi.org/10.1016/j.quageo.2009.04.003, 2009. a
Dunne, J., Elmore, D., and Muzikar, P.: Scaling factors for the rates of
production of cosmogenic nuclides for geometric shielding and attenuation at
depth on sloped surfaces, Geomorphology, 27, 3–11,
https://doi.org/10.1016/S0169-555X(98)00086-5, 1999. a
Farr, T. G., Rosen, P. A., Caro, E., Crippen, R., Duren, R., Hensley, S.,
Kobrick, M., Paller, M., Rodriguez, E., Roth, L., Seal, D., Shaffer, S.,
Shimada, J., Umland, J., Werner, M., Oskin, M., Burbank, D., and Alsdorf, D.:
The Shuttle Radar Topography Mission, Rev. Geophys., 45, RG2004,
https://doi.org/10.1029/2005RG000183, 2007. a
Fitzsimmons, K. E., Rhodes, E. J., Magee, J. W., and Barrows, T. T.: The
timing of linear dune activity in the Strzelecki and Tirari Deserts,
Australia, Quaternary Sci. Rev., 26, 2598–2616,
https://doi.org/10.1016/j.quascirev.2007.06.010, 2007. a
Frankel, K. L., Finkel, R. C., and Owen, L.: Terrestrial Cosmogenic Nuclide
Geochronology Data Reporting Standards Needed, Eos T. Am.
Geophys. Un., 91, 31–32, https://doi.org/10.1029/2010EO040003, 2010. a
Fuchs, M. and Owen, L. A.: Luminescence dating of glacial and associated
sediments: review, recommendations and future directions, Boreas, 37,
636–659, https://doi.org/10.1111/j.1502-3885.2008.00052.x, 2008. a
Fujioka, T., Chappell, J., Fifield, L. K., and Rhodes, E. J.: Australian
desert dune fields initiated with Pliocene–Pleistocene global climatic
shift, Geology, 37, 51–54, https://doi.org/10.1130/G25042A.1, 2009. a
Galbraith, R. F., Roberts, R. G., Laslett, G. M., Yoshida, H., and Olley,
J. M.: Optical dating of single and multiple grains of quartz from Jinmium
rock shelter, northern Australia: Part I, experimental design and statistical
models, Archaeometry, 41, 339–364,
https://doi.org/10.1111/j.1475-4754.1999.tb00987.x, 1999. a
Geoscience Australia: GEODATA 9 second DEM and D8: Digital Elevation Model
Version 3 and Flow Direction Grid 2008. Bioregional Assessment Source
Dataset, available at:
http://data.bioregionalassessments.gov.au/dataset/ebcf6ca2-513a-4ec7-9323-73508c5d7b93
(last access: 28 November 2018), 2008. a
Geoscience Australia: Geoscience Australia, 1 second SRTM Digital Elevation
Model (DEM), Bioregional Assessment Source Dataset, available at:
http://data.bioregionalassessments.gov.au/dataset/9a9284b6-eb45-4a13-97d0-91bf25f1187b
(last access: 28 November 2018), 2011. a
Granger, D. E. and Schaller, M.: Cosmogenic Nuclides and Erosion at the
Watershed Scale, Elements, 10, 369–373, https://doi.org/10.2113/gselements.10.5.369, 2014. a, b, c
Granger, D. E., Kirchner, J. W., and Finkel, R. C.: Spatially averaged
long-term erosion rates measured from in situ-produced cosmogenic nuclides in
alluvial sediment, J. Geol., 104, 249–257, 1996. a
Granger, D. E., Lifton, N. A., and Willenbring, J. K.: A cosmic trip: 25
years
of cosmogenic nuclides in geology, Geol. Soc. Am. Bull.,
125, 1379, https://doi.org/10.1130/B30774.1, 2013. a, b, c
Harel, M. A., Mudd, S. M., and Attal, M.: Global analysis of the stream power
law parameters based on worldwide 10Be denudation rates,
Geomorphology, 268, 184–196, https://doi.org/10.1016/j.geomorph.2016.05.035, 2016. a
Henck, A. C., Huntington, K. W., Stone, J. O., Montgomery, D. R., and Hallet,
B.: Spatial controls on erosion in the Three Rivers Region, southeastern
Tibet and southwestern China, Earth Planet. Sc. Lett., 303,
71–83, https://doi.org/10.1016/j.epsl.2010.12.038, 2011. a
Herman, F., Seward, D., Valla, P. G., Carter, A., Kohn, B., Willett, S. D.,
and
Ehlers, T. A.: Worldwide acceleration of mountain erosion under a cooling
climate, Nature, 504, 423–426, https://doi.org/10.1038/nature12877, 2013. a
Huntley, D. J., Godfrey-Smith, D. I., and Thewalt, M. L. W.: Optical dating
of
sediments, Nature, 313, 105–107, https://doi.org/10.1038/313105a0, 1985. a
Iacovella, S. and Youngblood, B.: GeoServer Beginner's Guide, Packt
Publishing, Birmingham, 2013. a
Ivy-Ochs, S. and Briner, J. P.: Dating Disappearing Ice with Cosmogenic
Nuclides, Elements, 10, 351–356, https://doi.org/10.2113/gselements.10.5.351, 2014. a
Jansen, J., Nanson, G., Cohen, T., Fujioka, T., Fabel, D., Larsen, J.,
Codilean, A., Price, D., Bowman, H., May, J.-H., and Gliganic, L.: Lowland
river responses to intraplate tectonism and climate forcing quantified with
luminescence and cosmogenic 10Be, Earth Planet Sc.
Lett., 366, 49–58, https://doi.org/10.1016/j.epsl.2013.02.007, 2013. a
Korschinek, G., Bergmaier, A., Faestermann, T., Gerstmann, U. C., Knie, K.,
Rugel, G., Wallner, A., Dillmann, I., Dollinger, G., von Gostomski, C. L.,
Kossert, K., Maiti, M., Poutivtsev, M., and Remmert, A.: A new value for the
half-life of 10Be by Heavy-Ion Elastic Recoil Detection and liquid
scintillation counting, Nucl. Instrum. Meth. B, 268, 187–191, https://doi.org/10.1016/j.nimb.2009.09.020, 2010. a, b
Lal, D.: Cosmic ray labeling of erosion surfaces: in situ nuclide production
rates and erosion models, Earth Planet. Sc. Lett., 104,
424–439, https://doi.org/10.1016/0012-821X(91)90220-C, 1991. a
Lewis, C. J., McDonald, E. V., Sancho, C., Peña, J. L., and Rhodes,
E. J.:
Climatic implications of correlated Upper Pleistocene glacial and fluvial
deposits on the Cinca and Gállego Rivers (NE Spain) based on OSL dating and
soil stratigraphy, Global Planet. Change, 67, 141–152,
https://doi.org/10.1016/j.gloplacha.2009.01.001, 2009. a
Lifton, N. A., Sato, T., and Dunai, T. J.: Scaling in situ cosmogenic
nuclide production rates using analytical approximations to atmospheric
cosmic-ray fluxes, Earth Planet. Sc. Lett., 386, 149–160,
https://doi.org/10.1016/j.epsl.2013.10.052, 2014. a
Lupker, M., Blard, P.-H., Lavé, J., France-Lanord, C., Leanni, L., Puchol,
N., Charreau, J., and Bourlès, D.: 10Be-derived Himalayan
denudation rates and sediment budgets in the Ganga basin, Earth
Planet. Sc. Lett, 333–334, 146–156,
https://doi.org/10.1016/j.epsl.2012.04.020, 2012. a, b
Lupker, M., Lavé, J., France-Lanord, C., Christl, M., Bourlès, D.,
Carcaillet, J., Maden, C., Wieler, R., Rahman, M., Bezbaruah, D., and
Xiaohan, L.: 10Be systematics in the Tsangpo-Brahmaputra catchment:
the cosmogenic nuclide legacy of the eastern Himalayan syntaxis, Earth Surf.
Dynam., 5, 429–449, https://doi.org/10.5194/esurf-5-429-2017, 2017. a, b
Molnar, P. and England, P.: Late Cenozoic Uplift of Mountain-Ranges and
Global Climate Change – Chicken or Egg, Nature, 346, 29–34,
https://doi.org/10.1038/346029a0, 1990. a
Mudd, S. M., Harel, M.-A., Hurst, M. D., Grieve, S. W. D., and Marrero, S.
M.: The CAIRN method: automated, reproducible calculation of
catchment-averaged denudation rates from cosmogenic nuclide concentrations,
Earth Surf. Dynam., 4, 655–674, https://doi.org/10.5194/esurf-4-655-2016,
2016. a, b, c
Nishiizumi, K., Imamura, M., Caffee, M. W., Southon, J. R., Finkel, R. C.,
and
Mcaninch, J.: Absolute calibration of 10Be AMS standards, Nucl.
Instrum. Meth. B, 258, 403–413, https://doi.org/10.1016/j.nimb.2007.01.297, 2007. a
Olley, J., Deckker, P. D., Roberts, R., Fifield, L., Yoshida, H., and
Hancock,
G.: Optical dating of deep-sea sediments using single grains of quartz: a
comparison with radiocarbon, Sediment. Geol., 169, 175–189,
https://doi.org/10.1016/j.sedgeo.2004.05.005, 2004. a
Pietsch, T., Brooks, A., Spencer, J., Olley, J., and Borombovits, D.: Age,
distribution, and significance within a sediment budget, of in-channel
depositional surfaces in the Normanby River, Queensland, Australia,
Geomorphology, 239, 17–40, https://doi.org/10.1016/j.geomorph.2015.01.038, 2015. a
Portenga, E. W. and Bierman, P. R.: Understanding Earth's eroding surface
with
10Be, GSA Today, 21, 4–10, https://doi.org/10.1130/G111A.1, 2011. a
Raymo, M. E. and Ruddiman, W. F.: Tectonic Forcing of Late Cenozoic Climate,
Nature, 359, 117–122, https://doi.org/10.1038/359117a0, 1992. a
Reber, R., Delunel, R., Schlunegger, F., Litty, C., Madella, A., Akçar,
N.,
and Christl, M.: Environmental controls on 10Be-based
catchment-averaged denudation rates along the western margin of the Peruvian
Andes, Terra Nova, 29, 282–293, https://doi.org/10.1111/ter.12274, 2017. a
Rhodes, E. and Bailey, R.: The effect of thermal transfer on the zeroing of
the luminescence of quartz from recent glaciofluvial sediments, Quaternary
Sci. Rev., 16, 291–298, https://doi.org/10.1016/S0277-3791(96)00100-X, 1997. a
Rhodes, E. J.: Optically Stimulated Luminescence Dating of Sediments over the
Past 200,000 Years, Annu. Rev. Earth Planet. Sc., 39,
461–488, https://doi.org/10.1146/annurev-earth-040610-133425, 2011. a, b
Richards, B. W., Benn, D. I., Owen, L. A., Rhodes, E. J., and Spencer, J. Q.:
Timing of late Quaternary glaciations south of Mount Everest in the Khumbu
Himal, Nepal, Geol. Soc. Am. Bull., 112, 1621–1632, https://doi.org/10.1130/0016-7606(2000)112<1621:TOLQGS>2.0.CO;2, 2000. a
Rustomji, P. and Pietsch, T.: Alluvial sedimentation rates from southeastern
Australia indicate post-European settlement landscape recovery,
Geomorphology, 90, 73–90, https://doi.org/10.1016/j.geomorph.2007.01.009, 2007. a
Safran, E. B., Bierman, P. R., Aalto, R., Dunne, T., Whipple, K. X., and
Caffee, M.: Erosion rates driven by channel network incision in the Bolivian
Andes, Earth Surf. Proc. Land., 30, 1007–1024,
https://doi.org/10.1002/esp.1259, 2005. a
Schaefer, J. M., Denton, G. H., Kaplan, M. R., Putnam, A., Finkel, R. C.,
Barrell, D. J. A., Andersen, B. G., Schwartz, R., Mackintosh, A., Chinn, T.,
and Schluechter, C.: High-Frequency Holocene Glacier Fluctuations in New
Zealand Differ from the Northern Signature, Science, 324, 622–625, 2009. a
Schaller, M., von Blanckenburg, F., Hovius, N., Veldkamp, A., van den Berg,
M.,
and Kubik, P. W.: Paleoerosion Rates from Cosmogenic 10Be in a 1.3 Ma
Terrace Sequence: Response of the River Meuse to Changes in Climate and Rock
Uplift, J. Geol., 112, 127–144, https://doi.org/10.1086/381654, 2004. a
Singarayer, J., Bailey, R., Ward, S., and Stokes, S.: Assessing the
completeness of optical resetting of quartz OSL in the natural environment,
Radiat. Meas., 40, 13–25, https://doi.org/10.1016/j.radmeas.2005.02.005,
2005. a
Spencer, J. Q. and Owen, L. A.: Optically stimulated luminescence dating of
Late Quaternary glaciogenic sediments in the upper Hunza valley: validating
the timing of glaciation and assessing dating methods, Quaternary Sci.
Rev., 23, 175–191, https://doi.org/10.1016/S0277-3791(03)00220-8, 2004. a
Stone, J. O.: Air pressure and cosmogenic isotope production, J.
Geophys. Res.-Sol. Ea., 105, 23753–23759,
https://doi.org/10.1029/2000JB900181, 2000. a, b
Vermeesch, P.: CosmoCalc: An Excel add-in for cosmogenic nuclide
calculations, Geochem. Geophy. Geosy., 8, Q08003,
https://doi.org/10.1029/2006GC001530, 2007. a
Veth, P., Smith, M., Bowler, J., Fitzsimmons, K., Williams, A., and Hiscock,
P.: Excavations At Parnkupirti, Lake Gregory, Great Sandy Desert: OSL Ages
for Occupation before the Last Glacial Maximum, Australian Archaeology, 69,
1–10, https://doi.org/10.1080/03122417.2009.11681896, 2009. a
von Blanckenburg, F.: The control mechanisms of erosion and weathering at
basin scale from cosmogenic nuclides in river sediment, Earth Planet.
Sc. Lett., 237, 462–479, https://doi.org/10.1016/j.epsl.2005.06.030, 2005. a, b, c
von Blanckenburg, F. and Willenbring, J. K.: Cosmogenic Nuclides: Dates and
Rates of Earth-Surface Change, Elements, 10, 341–346,
https://doi.org/10.2113/gselements.10.5.341, 2014. a
Wallinga, J., Hobo, N., Cunningham, A. C., Versendaal, A. J., Makaske, B.,
and
Middelkoop, H.: Sedimentation rates on embanked floodplains determined
through quartz optical dating, Quat. Geochronol., 5, 170–175,
https://doi.org/10.1016/j.quageo.2009.01.002, 2010. a
Willenbring, J. K. and von Blanckenburg, F.: Long-term stability of global
erosion rates and weathering during late-Cenozoic cooling, Nature, 465,
211–214, https://doi.org/10.1038/nature09044, 2010.
a
Willenbring, J. K., Codilean, A. T., and McElroy, B.: Earth is (mostly)
flat:
Apportionment of the flux of continental sediment over millennial time
scales, Geology, 41, 343–346, https://doi.org/10.1130/G33918.1, 2013. a
Wintle, A. G.: Luminescence dating: where it has been and where it is
going,
Boreas, 37, 471–482, https://doi.org/10.1111/j.1502-3885.2008.00059.x, 2008. a
Wittmann, H., von Blanckenburg, F., Guyot, J., Maurice, L., and Kubik, P.:
From source to sink: Preserving the cosmogenic 10Be-derived
denudation rate signal of the Bolivian Andes in sediment of the Beni and
Mamoré foreland basins, Earth Planet. Sc. Lett., 288, 463–474,
https://doi.org/10.1016/j.epsl.2009.10.008, 2009. a, b
Wittmann, H., von Blanckenburg, F., Maurice, L., Guyot, J.-L., Filizola, N.,
and Kubik, P. W.: Sediment production and delivery in the Amazon River basin
quantified by in situ-produced cosmogenic nuclides and recent river loads,
Geol. Soc. Am. Bull., 123, 934–950, https://doi.org/10.1130/B30317.1,
2011. a, b
Wolfe, S. A., Huntley, D. J., and Ollerhead, J.: Recent and late Holocene
sand
dune activity in southwestern Saskatchewan, Current Research, Geological
Survey of Canada, 1995-B, 131–140, 1995. a
Short summary
OCTOPUS is a database of cosmogenic radionuclide and luminescence measurements in fluvial sediment made available to the research community via an Open Geospatial Consortium compliant web service. OCTOPUS and its associated data curation framework provide the opportunity for researchers to reuse previously published but otherwise unusable CRN and luminescence data. This delivers the potential to harness old but valuable data that would otherwise be lost to the research community.
OCTOPUS is a database of cosmogenic radionuclide and luminescence measurements in fluvial...
