Articles | Volume 20, issue 1
https://doi.org/10.5194/cp-20-1-2024
© 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/cp-20-1-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Paleocene–Eocene age glendonites from the Mid-Norwegian Margin – indicators of cold snaps in the hothouse?
Madeleine L. Vickers
CORRESPONDING AUTHOR
Centre for Planetary Habitability (PHAB), University of Oslo, P.O. Box 1028 Blindern, 0315 Oslo, Norway
Morgan T. Jones
Centre for Planetary Habitability (PHAB), University of Oslo, P.O. Box 1028 Blindern, 0315 Oslo, Norway
Department of Ecology and Environmental Science (EMG), Umeå University, 901 87 Umeå, Sweden
Jack Longman
Department of Geography and Environmental Sciences, Northumbria University, Newcastle-upon-Tyne NE1 8ST, UK
David Evans
Institute of Geosciences, Goethe University Frankfurt, Altenhöferallee 1, 60438 Frankfurt am Main, Germany
FIERCE, Frankfurt Isotope & Element Research Center, Goethe University Frankfurt, Altenhöferallee 1, 60438 Frankfurt am Main, Germany
School of Ocean and Earth Science, University of Southampton, Southampton SO14 3ZH, UK
Clemens V. Ullmann
Camborne School of Mines, University of Exeter, Penryn Campus, Penryn TR10 9FE, UK
Ella Wulfsberg Stokke
Centre for Planetary Habitability (PHAB), University of Oslo, P.O. Box 1028 Blindern, 0315 Oslo, Norway
Martin Vickers
Department of Chemistry, UCL, 20 Gordon Street, London WC1H 0AJ, UK
Joost Frieling
Department of Earth Sciences, University of Oxford, Oxford OX1 3AN, UK
Dustin T. Harper
Department of Geology & Geophysics, University of Utah, Salt Lake City, UT 84112, USA
Vincent J. Clementi
Department of Marine and Coastal Sciences, Rutgers University, New Brunswick, NJ 08901, USA
A full list of authors appears at the end of the paper.
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Morgan T. Jones, Ella W. Stokke, Alan D. Rooney, Joost Frieling, Philip A. E. Pogge von Strandmann, David J. Wilson, Henrik H. Svensen, Sverre Planke, Thierry Adatte, Nicolas Thibault, Madeleine L. Vickers, Tamsin A. Mather, Christian Tegner, Valentin Zuchuat, and Bo P. Schultz
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Peter K. Bijl, Joost Frieling, Marlow Julius Cramwinckel, Christine Boschman, Appy Sluijs, and Francien Peterse
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Ella W. Stokke, Morgan T. Jones, Lars Riber, Haflidi Haflidason, Ivar Midtkandal, Bo Pagh Schultz, and Henrik H. Svensen
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Nicolai Schleinkofer, David Evans, Max Wisshak, Janina Vanessa Büscher, Jens Fiebig, André Freiwald, Sven Härter, Horst R. Marschall, Silke Voigt, and Jacek Raddatz
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Thomas Munier, Jean-François Deconinck, Pierre Pellenard, Stephen P. Hesselbo, James B. Riding, Clemens V. Ullmann, Cédric Bougeault, Mathilde Mercuzot, Anne-Lise Santoni, Émilia Huret, and Philippe Landrein
Clim. Past, 17, 1547–1566, https://doi.org/10.5194/cp-17-1547-2021, https://doi.org/10.5194/cp-17-1547-2021, 2021
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Appy Sluijs, Joost Frieling, Gordon N. Inglis, Klaas G. J. Nierop, Francien Peterse, Francesca Sangiorgi, and Stefan Schouten
Clim. Past, 16, 2381–2400, https://doi.org/10.5194/cp-16-2381-2020, https://doi.org/10.5194/cp-16-2381-2020, 2020
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We revisit 15-year-old reconstructions of sea surface temperatures in the Arctic Ocean for the late Paleocene and early Eocene epochs (∼ 57–53 million years ago) based on the distribution of fossil membrane lipids of archaea preserved in Arctic Ocean sediments. We find that improvements in the methods over the past 15 years do not lead to different results. However, data quality is now higher and potential biases better characterized. Results confirm remarkable Arctic warmth during this time.
Gordon N. Inglis, Fran Bragg, Natalie J. Burls, Marlow Julius Cramwinckel, David Evans, Gavin L. Foster, Matthew Huber, Daniel J. Lunt, Nicholas Siler, Sebastian Steinig, Jessica E. Tierney, Richard Wilkinson, Eleni Anagnostou, Agatha M. de Boer, Tom Dunkley Jones, Kirsty M. Edgar, Christopher J. Hollis, David K. Hutchinson, and Richard D. Pancost
Clim. Past, 16, 1953–1968, https://doi.org/10.5194/cp-16-1953-2020, https://doi.org/10.5194/cp-16-1953-2020, 2020
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This paper presents estimates of global mean surface temperatures and climate sensitivity during the early Paleogene (∼57–48 Ma). We employ a multi-method experimental approach and show that i) global mean surface temperatures range between 27 and 32°C and that ii) estimates of
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Short summary
The discovery of cold-water glendonite pseudomorphs in sediments deposited during the hottest part of the Cenozoic poses an apparent climate paradox. This study examines their occurrence, association with volcanic sediments, and speculates on the timing and extent of cooling, fitting this with current understanding of global climate during this period. We propose that volcanic activity was key to both physical and chemical conditions that enabled the formation of glendonites in these sediments.
The discovery of cold-water glendonite pseudomorphs in sediments deposited during the hottest...