Articles | Volume 16, issue 10
https://doi.org/10.5194/essd-16-4767-2024
© Author(s) 2024. 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-16-4767-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
A revised marine fossil record of the Mediterranean before and after the Messinian salinity crisis
Konstantina Agiadi
CORRESPONDING AUTHOR
Department of Geology, University of Vienna, Josef-Holaubek-Platz 2, 1090 Vienna, Austria
Niklas Hohmann
Faculty of Geosciences, Department of Earth Sciences, Utrecht University, Vening Meineszgebouw A, Princetonlaan 8a, 3584 CB Utrecht, the Netherlands
Institute of Evolutionary Biology, University of Warsaw, Krakowskie Przedmieście 26/28, 00-927, Warsaw, Poland
Elsa Gliozzi
Dipartimento di Scienze, Università Roma Tre, L.go S. Leonardo Murialdo, 1 – 00146 Rome, Italy
Danae Thivaiou
Natural History Museum of Basel, Augustinergasse 2, 4001 Basel, Switzerland
Department of Historical Geology and Palaeontology, Faculty of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimioupolis Zografou 15784, Athens, Greece
Francesca R. Bosellini
Dipartimento di Scienze Chimiche e Geologiche, Università degli Studi di Modena e Reggio Emilia, 09124 Cagliari, Italy
Marco Taviani
Institute of Marine Science – National Research Council, ISMAR-CNR, Via Gobetti 101, 40129 Bologna, Italy
Stazione Zoologica “Anton Dohrn”, Villa Comunale, Via Caracciolo, 80122 Naples, Italy
Giovanni Bianucci
Dipartimento di Scienze della Terra, Università di Pisa, Pisa, Italy
Alberto Collareta
Dipartimento di Scienze della Terra, Università di Pisa, Pisa, Italy
Laurent Londeix
Université de Bordeaux/UMR “EPOC” CNRS 5805, allée Geoffroy St-Hilaire, 33615 Pessac CEDEX, France
Costanza Faranda
Dipartimento di Scienze, Università Roma Tre, L.go S. Leonardo Murialdo, 1 – 00146 Rome, Italy
Francesca Bulian
Department of Geology, University of Salamanca, Plaza de Los Caidos s/n, 37008, Salamanca, Spain
Groningen Institute of Archaeology, University of Groningen, Postsraat 6, 9712 Groningen, the Netherlands
Efterpi Koskeridou
Department of Historical Geology and Palaeontology, Faculty of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimioupolis Zografou 15784, Athens, Greece
Francesca Lozar
Department of Earth Sciences, University of Torino, Via Valperga Caluso 35, 10125 Turin, Italy
Alan Maria Mancini
Department of Earth Sciences, University of Torino, Via Valperga Caluso 35, 10125 Turin, Italy
Department of Life and Environmental Science, Università Politecnica delle Marche, 60122 Ancona, Italy
Stefano Dominici
Museo di Storia Naturale, Università degli Studi di Firenze, 50121 Florence, Italy
Pierre Moissette
Department of Historical Geology and Palaeontology, Faculty of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimioupolis Zografou 15784, Athens, Greece
Ildefonso Bajo Campos
Sección de Paleontología, Museo de Alcalá de Guadaíra, Seville, Spain
Enrico Borghi
Società Reggiana di Scienza Naturali, Reggio Emilia, Italy
George Iliopoulos
Department of Geology, University of Patras, University Campus, 26504 Rio, Achaia, Greece
Assimina Antonarakou
Department of Historical Geology and Palaeontology, Faculty of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimioupolis Zografou 15784, Athens, Greece
George Kontakiotis
Department of Historical Geology and Palaeontology, Faculty of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimioupolis Zografou 15784, Athens, Greece
Evangelia Besiou
Department of Historical Geology and Palaeontology, Faculty of Geology and Geoenvironment, National and Kapodistrian University of Athens, Panepistimioupolis Zografou 15784, Athens, Greece
Stergios D. Zarkogiannis
Department of Earth Sciences, University of Oxford, Oxford, UK
Mathias Harzhauser
Natural History Museum, Burgring 7, 1010 Vienna, Austria
Francisco Javier Sierro
Department of Geology, University of Salamanca, Plaza de Los Caidos s/n, 37008, Salamanca, Spain
Angelo Camerlenghi
OGS Istituto Nazionale di Oceanografia e di Geofisica Sperimentale, Trieste, Italy
Daniel García-Castellanos
Geosciences Barcelona (GEO3BCN-CSIC), Solé i Sabarís s/n, Barcelona, Spain
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Konstantina Agiadi, Iuliana Vasiliev, Geanina Butiseacă, George Kontakiotis, Danae Thivaiou, Evangelia Besiou, Stergios Zarkogiannis, Efterpi Koskeridou, Assimina Antonarakou, and Andreas Mulch
Biogeosciences, 21, 3869–3881, https://doi.org/10.5194/bg-21-3869-2024, https://doi.org/10.5194/bg-21-3869-2024, 2024
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Seven million years ago, the marine gateway connecting the Mediterranean Sea with the Atlantic Ocean started to close, and, as a result, water circulation ceased. To find out how this phenomenon affected the fish living in the Mediterranean Sea, we examined the changes in the isotopic composition of otoliths of two common fish species. Although the species living at the surface fared pretty well, the bottom-water fish starved and eventually became extinct in the Mediterranean.
Konstantina Agiadi, Efterpi Koskeridou, and Danae Thivaiou
Foss. Rec., 24, 233–246, https://doi.org/10.5194/fr-24-233-2021, https://doi.org/10.5194/fr-24-233-2021, 2021
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Climate and connection between marine basins have formed the modern Mediterranean fish fauna. Here, we present new data for the early stages of the fish fauna, 20–23 million years ago, when the Mediterranean Sea was starting to take its actual shape, and we show its relationship to the fish faunas of the surrounding seas. Two new fish species are described: Ariosoma mesohellenica and Gnathophis elongatus.
Niklas Hohmann, David De Vleeschouwer, Sietske Batenburg, and Emilia Jarochowska
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Age-depth models assign ages to sampling locations (e.g., in drill cores), making them crucial to determined timing and pace of past changes. We present two methods to estimate age-depth models from sedimentological and stratigraphic information, resulting in richer and more empirically realistic age-depth models. As a use case, we determine (1) the timing of the Frasnian-Famennian extinction and (2) examine the duration of PETM, an potential deep time analogue for anthropogenic climate change.
Thibauld M. Béjard, Andrés S. Rigual-Hernández, Javier P. Tarruella, José-Abel Flores, Anna Sanchez-Vidal, Irene Llamas-Cano, and Francisco J. Sierro
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The Mediterranean Sea is regarded as a climate change hotspot. Documenting the population of planktonic foraminifera is crucial. In the Sicily Channel, fluxes are higher during winter and positively linked with chlorophyll a concentration and cool temperatures. A comparison with other Mediterranean sites shows the transitional aspect of the studied zone. Finally, modern populations significantly differ from those in the sediment, highlighting a possible effect of environmental change.
Konstantina Agiadi, Iuliana Vasiliev, Geanina Butiseacă, George Kontakiotis, Danae Thivaiou, Evangelia Besiou, Stergios Zarkogiannis, Efterpi Koskeridou, Assimina Antonarakou, and Andreas Mulch
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Seven million years ago, the marine gateway connecting the Mediterranean Sea with the Atlantic Ocean started to close, and, as a result, water circulation ceased. To find out how this phenomenon affected the fish living in the Mediterranean Sea, we examined the changes in the isotopic composition of otoliths of two common fish species. Although the species living at the surface fared pretty well, the bottom-water fish starved and eventually became extinct in the Mediterranean.
Judit Torner, Isabel Cacho, Heather Stoll, Ana Moreno, Joan O. Grimalt, Francisco J. Sierro, Hai Cheng, and R. Lawrence Edwards
Clim. Past Discuss., https://doi.org/10.5194/cp-2024-54, https://doi.org/10.5194/cp-2024-54, 2024
Revised manuscript accepted for CP
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This study presents a new speleothem record of the western Mediterranean region that offers new insights into the timeline of glacial terminations TIV, TIII, and TIII.a. The comparison among the studied deglaciations reveals differences in terms of intensity and duration and opens the opportunity to evaluate marine sediment chronologies based on orbital tuning from the North Atlantic and the Western Mediterranean.
Mathias Harzhauser, Oleg Mandic, and Werner E. Piller
Biogeosciences, 20, 4775–4794, https://doi.org/10.5194/bg-20-4775-2023, https://doi.org/10.5194/bg-20-4775-2023, 2023
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Bowl-shaped spirorbid microbialite bioherms formed during the late Middle Miocene (Sarmatian) in the central Paratethys Sea under a warm, arid climate. The microbialites and the surrounding sediment document a predominance of microbial activity in the shallow marine environments of the sea at that time. Modern microbialites are not analogues for these unique structures, which reflect a series of growth stages with an initial “start-up stage”, massive “keep-up stage” and termination of growth.
Thibauld M. Béjard, Andrés S. Rigual-Hernández, José A. Flores, Javier P. Tarruella, Xavier Durrieu de Madron, Isabel Cacho, Neghar Haghipour, Aidan Hunter, and Francisco J. Sierro
Biogeosciences, 20, 1505–1528, https://doi.org/10.5194/bg-20-1505-2023, https://doi.org/10.5194/bg-20-1505-2023, 2023
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The Mediterranean Sea is undergoing a rapid and unprecedented environmental change. Planktic foraminifera calcification is affected on different timescales. On seasonal and interannual scales, calcification trends differ according to the species and are linked mainly to sea surface temperatures and carbonate system parameters, while comparison with pre/post-industrial assemblages shows that all three species have reduced their calcification between 10 % to 35 % according to the species.
Jonathan Ford, Angelo Camerlenghi, Francesca Zolezzi, and Marilena Calarco
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The Cryosphere, 16, 2009–2024, https://doi.org/10.5194/tc-16-2009-2022, https://doi.org/10.5194/tc-16-2009-2022, 2022
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Konstantina Agiadi, Efterpi Koskeridou, and Danae Thivaiou
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Andrés S. Rigual Hernández, Thomas W. Trull, Scott D. Nodder, José A. Flores, Helen Bostock, Fátima Abrantes, Ruth S. Eriksen, Francisco J. Sierro, Diana M. Davies, Anne-Marie Ballegeer, Miguel A. Fuertes, and Lisa C. Northcote
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Julie A. Trotter, Charitha Pattiaratchi, Paolo Montagna, Marco Taviani, James Falter, Ron Thresher, Andrew Hosie, David Haig, Federica Foglini, Quan Hua, and Malcolm T. McCulloch
Biogeosciences Discuss., https://doi.org/10.5194/bg-2018-319, https://doi.org/10.5194/bg-2018-319, 2018
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The first ROV exploration of the Perth Canyon offshore southwest Australia discovered diverse
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Andrés S. Rigual Hernández, José A. Flores, Francisco J. Sierro, Miguel A. Fuertes, Lluïsa Cros, and Thomas W. Trull
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Benjamin Ramassamy, Olivier Lambert, Alberto Collareta, Mario Urbina, and Giovanni Bianucci
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Alberto Collareta, Olivier Lambert, Christian de Muizon, Mario Urbina, and Giovanni Bianucci
Foss. Rec., 20, 259–278, https://doi.org/10.5194/fr-20-259-2017, https://doi.org/10.5194/fr-20-259-2017, 2017
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Extant pygmy and dwarf sperm whales (Kogia spp.) are known as small-sized and enigmatic relatives of the great sperm whale Physeter. Here we describe Koristocetus pescei, a new fossil kogiid from the late Miocene (ca 7 million years ago) of Peru. The description of this new form evokes a long history of morphological and ecological diversity in fossil kogiids, thus suggesting that our comprehension of the evolutionary history of diminutive sperm whales is still far from being exhaustive.
Quentin Dubois-Dauphin, Paolo Montagna, Giuseppe Siani, Eric Douville, Claudia Wienberg, Dierk Hebbeln, Zhifei Liu, Nejib Kallel, Arnaud Dapoigny, Marie Revel, Edwige Pons-Branchu, Marco Taviani, and Christophe Colin
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Mathias Harzhauser, Ana Djuricic, Oleg Mandic, Thomas A. Neubauer, Martin Zuschin, and Norbert Pfeifer
Biogeosciences, 13, 1223–1235, https://doi.org/10.5194/bg-13-1223-2016, https://doi.org/10.5194/bg-13-1223-2016, 2016
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We present the first analysis of population structure and cohort distribution in a fossil oyster reef. Data are derived from Terrestrial Laser Scanning of a Miocene shell bed covering 459 m². A growth model was calculated, revealing this species as the giant oyster Crassostrea gryphoides was the fastest growing oyster known so far. The shell half-lives range around few years, indicating that oyster reefs were geologically short-lived structures, which were degraded on a decadal scale.
G. Auer, W. E. Piller, and M. Harzhauser
Clim. Past, 11, 283–303, https://doi.org/10.5194/cp-11-283-2015, https://doi.org/10.5194/cp-11-283-2015, 2015
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High-resolution analyses of paleoecological and geochemical proxies give insight into environmental processes and climate variations in the past on a timescale that is relevant for humans. This study, as the first of its kind, aims to resolve cyclic variations of nannofossil assemblages on a decadal to centennial scale in a highly sensitive Early Miocene (~17Ma) shallow marine setting. Our results indicate that solar variation played a major role in shaping short-term climate variability.
D. Hebbeln, C. Wienberg, P. Wintersteller, A. Freiwald, M. Becker, L. Beuck, C. Dullo, G. P. Eberli, S. Glogowski, L. Matos, N. Forster, H. Reyes-Bonilla, and M. Taviani
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M. Harzhauser, O. Mandic, A. K. Kern, W. E. Piller, T. A. Neubauer, C. Albrecht, and T. Wilke
Biogeosciences, 10, 8423–8431, https://doi.org/10.5194/bg-10-8423-2013, https://doi.org/10.5194/bg-10-8423-2013, 2013
M. Reuter, W. E. Piller, M. Harzhauser, and A. Kroh
Clim. Past, 9, 2101–2115, https://doi.org/10.5194/cp-9-2101-2013, https://doi.org/10.5194/cp-9-2101-2013, 2013
M. Taviani, L. Angeletti, A. Ceregato, F. Foglini, C. Froglia, and F. Trincardi
Biogeosciences, 10, 4653–4671, https://doi.org/10.5194/bg-10-4653-2013, https://doi.org/10.5194/bg-10-4653-2013, 2013
R. A. Eagle, J. M. Eiler, A. K. Tripati, J. B. Ries, P. S. Freitas, C. Hiebenthal, A. D. Wanamaker Jr., M. Taviani, M. Elliot, S. Marenssi, K. Nakamura, P. Ramirez, and K. Roy
Biogeosciences, 10, 4591–4606, https://doi.org/10.5194/bg-10-4591-2013, https://doi.org/10.5194/bg-10-4591-2013, 2013
Related subject area
Domain: ESSD – Ocean | Subject: Palaeooceanography, palaeoclimatology
Coral skeletal proxy records database for the Great Barrier Reef, Australia
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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
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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.
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
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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
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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.
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
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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
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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).
Cited articles
Agiadi, K., Hohmann, N., Gliozzi, E., Thivaiou, D., Francesca, B., Taviani, M., Bianucci, G., Collareta, A., Londeix, L., Faranda, C., Bulian, F., Koskeridou, E., Lozar, F., Mancini, A. M., Dominici, S., Moissette, P., Bajo Campos, I., Borghi, E., Iliopoulos, G., Antonarakou, A., Kontakiotis, G., Besiou, E., Zarkogiannis, S. D., Harzhauser, M., Sierro, F., Camerlenghi, A., and Garcia-Castellanos, D.: Revised marine fossil record of the Mediterranean before and after the Messinian Salinity Crisis, Zenodo [data set], https://doi.org/10.5281/zenodo.13358435, 2024.
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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.
We present a dataset of 23032 fossil occurrences of marine organisms from the Late Miocene to...
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