Articles | Volume 19, issue 8
https://doi.org/10.5194/cp-19-1623-2023
© 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/cp-19-1623-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
08 Aug 2023
Research article |
| 08 Aug 2023
| 08 Aug 2023
Tracing North Atlantic volcanism and seaway connectivity across the Paleocene–Eocene Thermal Maximum (PETM)
Centre for Planetary Habitability, Department of Geosciences,
University of Oslo, P.O. Box 1028 Blindern, 0315 Oslo, Norway
Ella W. Stokke
Centre for Planetary Habitability, Department of Geosciences,
University of Oslo, P.O. Box 1028 Blindern, 0315 Oslo, Norway
Alan D. Rooney
Department of Earth and Planetary Sciences, Yale University, P.O. Box
208109, New Haven, CT 06520-8109, USA
Joost Frieling
Department of Earth Sciences, University of Oxford, South Parks Road,
Oxford, OX1 3AN, UK
Philip A. E. Pogge von Strandmann
Mainz Isotope and Geochemistry Centre (MIGHTY), Institute of
Geosciences, Johannes Gutenberg University, 55122 Mainz, Germany
London Geochemistry and Isotope Centre (LOGIC), Institute of Earth
and Planetary Sciences, University College London and Birkbeck, University
of London, Gower Street, London, WC1E 6BT, UK
David J. Wilson
London Geochemistry and Isotope Centre (LOGIC), Institute of Earth
and Planetary Sciences, University College London and Birkbeck, University
of London, Gower Street, London, WC1E 6BT, UK
Henrik H. Svensen
Department of Geosciences, University of Oslo, P.O. Box 1047 Blindern, 0316 Oslo, Norway
Sverre Planke
Department of Geosciences, University of Oslo, P.O. Box 1047 Blindern, 0316 Oslo, Norway
Volcanic Basin Petroleum Research (VBPR AS), Høienhald,
Blindernveien 5, 0361 Oslo, Norway
Thierry Adatte
Institute of Earth Sciences, University of Lausanne, 1015 Lausanne,
Switzerland
Nicolas Thibault
Department of Geosciences and Natural Resource Management, University of Copenhagen, 1350 Copenhagen K, Denmark
Madeleine L. Vickers
Centre for Planetary Habitability, Department of Geosciences,
University of Oslo, P.O. Box 1028 Blindern, 0315 Oslo, Norway
Tamsin A. Mather
Department of Earth Sciences, University of Oxford, South Parks Road,
Oxford, OX1 3AN, UK
Christian Tegner
Department of Geoscience, Aarhus University, Høegh-Guldbergs Gade 2, 8000 Aarhus C, Denmark
Valentin Zuchuat
Palaeontology and Geological Institute, Aachen University,
Bergbaugebäude 1140, Wüllnerstraße 2, Aachen, Germany
Bo P. Schultz
Museum Salling – Fur Museum, 7884 Fur, Denmark
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Cited
8 citations as recorded by crossref.
- Biogeochemical responses to global warming during the Paleocene–Eocene Thermal Maximum in the eastern Tethys Q. Wu et al. 10.1016/j.palaeo.2023.111969
- Stolleagrion foghnielseni (Odonata, Cephalozygoptera, Dysagrionidae) gen. et sp. nov.: a new odonatan from the PETM recovery phase of the earliest Ypresian Fur Formation, Denmark T. SIMONSEN et al. 10.11646/zootaxa.5415.3.9
- Rapid emplacement of a Palaeogene silicic volcanic centre, Arran, western Scotland R. Gooday et al. 10.1016/j.lithos.2024.107789
- Paleocene–Eocene age glendonites from the Mid-Norwegian Margin – indicators of cold snaps in the hothouse? M. Vickers et al. 10.5194/cp-20-1-2024
- High-precision U–Pb geochronology of the Lundy igneous complex: implications for North Atlantic volcanism and the far-field Paleocene–Eocene ash record K. Lisica et al. 10.1144/jgs2023-140
- The Baroch Nala section (NE Pakistan): A new PETM standard for the eastern Tethys M. Ali et al. 10.1016/j.marpetgeo.2024.107183
- The Paleocene–Eocene Thermal Maximum (PETM) interval in the southwestern Mediterranean Tethys at Morocco: New data from a high-resolution study of dinoflagellate cysts and palynofacies in the Rif Chain S. Aboutofail & H. Slimani 10.1016/j.palaeo.2024.112522
- Endocranial anatomy and phylogenetic position of the crocodylian Eosuchus lerichei from the late Paleocene of northwestern Europe and potential adaptations for transoceanic dispersal in gavialoids P. Burke et al. 10.1002/ar.25569
8 citations as recorded by crossref.
- Biogeochemical responses to global warming during the Paleocene–Eocene Thermal Maximum in the eastern Tethys Q. Wu et al. 10.1016/j.palaeo.2023.111969
- Stolleagrion foghnielseni (Odonata, Cephalozygoptera, Dysagrionidae) gen. et sp. nov.: a new odonatan from the PETM recovery phase of the earliest Ypresian Fur Formation, Denmark T. SIMONSEN et al. 10.11646/zootaxa.5415.3.9
- Rapid emplacement of a Palaeogene silicic volcanic centre, Arran, western Scotland R. Gooday et al. 10.1016/j.lithos.2024.107789
- Paleocene–Eocene age glendonites from the Mid-Norwegian Margin – indicators of cold snaps in the hothouse? M. Vickers et al. 10.5194/cp-20-1-2024
- High-precision U–Pb geochronology of the Lundy igneous complex: implications for North Atlantic volcanism and the far-field Paleocene–Eocene ash record K. Lisica et al. 10.1144/jgs2023-140
- The Baroch Nala section (NE Pakistan): A new PETM standard for the eastern Tethys M. Ali et al. 10.1016/j.marpetgeo.2024.107183
- The Paleocene–Eocene Thermal Maximum (PETM) interval in the southwestern Mediterranean Tethys at Morocco: New data from a high-resolution study of dinoflagellate cysts and palynofacies in the Rif Chain S. Aboutofail & H. Slimani 10.1016/j.palaeo.2024.112522
- Endocranial anatomy and phylogenetic position of the crocodylian Eosuchus lerichei from the late Paleocene of northwestern Europe and potential adaptations for transoceanic dispersal in gavialoids P. Burke et al. 10.1002/ar.25569
Discussed (final revised paper)
Latest update: 17 Nov 2024
Short summary
There are periods in Earth’s history when huge volumes of magma are erupted at the Earth’s surface. The gases released from volcanic eruptions and from sediments heated by the magma are believed to have caused severe climate changes in the geological past. We use a variety of volcanic and climatic tracers to assess how the North Atlantic Igneous Province (56–54 Ma) affected the oceans and atmosphere during a period of extreme global warming.
There are periods in Earth’s history when huge volumes of magma are erupted at the Earth’s...
