Articles | Volume 20, issue 12
https://doi.org/10.5194/bg-20-2317-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-20-2317-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
21 Jun 2023
Research article |
| 21 Jun 2023
| 21 Jun 2023
The fossil bivalve Angulus benedeni benedeni: a potential seasonally resolved stable-isotope-based climate archive to investigate Pliocene temperatures in the southern North Sea basin
Nina M. A. Wichern
CORRESPONDING AUTHOR
Institute of Geology and Paleontology, Westfälische
Wilhelms-Universität, 48149 Münster, Germany
Invited contribution by Nina M. A. Wichern, recipient of the EGU Stratigraphy, Sedimentology and Palaeontology Outstanding Student and PhD candidate Presentation Award 2022.
Niels J. de Winter
Department of Earth Sciences, Faculty of Science, Vrije Universiteit
Amsterdam, Amsterdam, 1081 HV, the Netherlands
Department of Earth Sciences, Utrecht University, Utrecht, 3584 CB,
the Netherlands
Analytical, Environmental, and Geochemistry, Vrije Universiteit
Brussel, Brussels, 1050, Belgium
Andrew L. A. Johnson
School of Built and Natural Environment, University of Derby, Derby,
DE22 1GB, UK
Stijn Goolaerts
OD Earth & History of Life and Scientific Service of Heritage,
Royal Belgian Institute of Natural Sciences, Brussels, 1000, Belgium
Frank Wesselingh
Department of Earth Sciences, Utrecht University, Utrecht, 3584 CB,
the Netherlands
Naturalis Biodiversity Center, Leiden, 2333 CR, the Netherlands
Maartje F. Hamers
Department of Earth Sciences, Utrecht University, Utrecht, 3584 CB,
the Netherlands
Pim Kaskes
Analytical, Environmental, and Geochemistry, Vrije Universiteit
Brussel, Brussels, 1050, Belgium
Philippe Claeys
Analytical, Environmental, and Geochemistry, Vrije Universiteit
Brussel, Brussels, 1050, Belgium
Martin Ziegler
Department of Earth Sciences, Utrecht University, Utrecht, 3584 CB,
the Netherlands
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Chronology is fundamental in paleoclimatology for understanding timing of events and their origin. In this paper we try to obtain a more detailed chronology for the interval comprised between ca. 140 and 70 ka for the DEEP core in Lake Ohrid using regional independently-dated archives (i.e. speleothems and/or lacustrine succession with well-dated volcanic layers). This allows to insert the DEEP chronology within a common chronological frame between different continental and marine proxy records.
Janna Just, Norbert R. Nowaczyk, Leonardo Sagnotti, Alexander Francke, Hendrik Vogel, Jack H. Lacey, and Bernd Wagner
Biogeosciences, 13, 2093–2109, https://doi.org/10.5194/bg-13-2093-2016, https://doi.org/10.5194/bg-13-2093-2016, 2016
Short summary
Short summary
The magnetic record from Lake Ohrid reflects a strong change in geochemical conditions in the lake. Before 320 ka glacial sediments contain iron sulfides, while later glacials are dominated by siderite. Superimposed on this large-scale pattern are climatic induced changes in the magnetic mineralogy. Glacial and stadial sediments are characterized by relative increases of high- vs. low-coercivity minerals which relate to enhanced erosion in the catchment, possibly due to a sparse vegetation.
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Biogeosciences, 11, 3245–3258, https://doi.org/10.5194/bg-11-3245-2014, https://doi.org/10.5194/bg-11-3245-2014, 2014
T. Denk, G. W. Grimm, F. Grímsson, and R. Zetter
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M. Claussen, K. Selent, V. Brovkin, T. Raddatz, and V. Gayler
Biogeosciences, 10, 3593–3604, https://doi.org/10.5194/bg-10-3593-2013, https://doi.org/10.5194/bg-10-3593-2013, 2013
M.-N. Woillez, M. Kageyama, N. Combourieu-Nebout, and G. Krinner
Biogeosciences, 10, 1561–1582, https://doi.org/10.5194/bg-10-1561-2013, https://doi.org/10.5194/bg-10-1561-2013, 2013
G. Yu, X. Ke, H. D. Shen, and Y. F. Li
Biogeosciences, 10, 1441–1449, https://doi.org/10.5194/bg-10-1441-2013, https://doi.org/10.5194/bg-10-1441-2013, 2013
R. Touchan, V. V. Shishov, D. M. Meko, I. Nouiri, and A. Grachev
Biogeosciences, 9, 965–972, https://doi.org/10.5194/bg-9-965-2012, https://doi.org/10.5194/bg-9-965-2012, 2012
A. Sluijs and H. Brinkhuis
Biogeosciences, 6, 1755–1781, https://doi.org/10.5194/bg-6-1755-2009, https://doi.org/10.5194/bg-6-1755-2009, 2009
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Short summary
Fossil bivalves are an excellent climate archive due to their rapidly forming growth increments and long lifespan. Here, we show that the extinct bivalve species Angulus benedeni benedeni can be used to reconstruct past temperatures using oxygen and clumped isotopes. This species has the potential to provide seasonally resolved temperature data for the Pliocene to Oligocene sediments of the North Sea basin. In turn, these past climates can improve our understanding of future climate change.
Fossil bivalves are an excellent climate archive due to their rapidly forming growth increments...
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