Articles | Volume 17, issue 5
https://doi.org/10.5194/cp-17-1989-2021
© Author(s) 2021. 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-17-1989-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
01 Oct 2021
Research article |
| 01 Oct 2021
| 01 Oct 2021
Rapid and sustained environmental responses to global warming: the Paleocene–Eocene Thermal Maximum in the eastern North Sea
Ella W. Stokke
CORRESPONDING AUTHOR
CEED, University of Oslo, P.O. Box 1028, 0315 Oslo, Norway
Morgan T. Jones
CEED, University of Oslo, P.O. Box 1028, 0315 Oslo, Norway
Lars Riber
Department of Geosciences, University of Oslo, P.O. Box 1047,
Blindern, 0316 Oslo, Norway
Haflidi Haflidason
Department of Earth Science, University of Bergen, Allégt. 41,
5007 Bergen, Norway
Bjerknes Centre for Climate Research, Jahnebakken 5, 5007 Bergen,
Norway
Ivar Midtkandal
Department of Geosciences, University of Oslo, P.O. Box 1047,
Blindern, 0316 Oslo, Norway
Bo Pagh Schultz
Museum Salling, Fur Museum, Nederby 28, 7884 Fur, Denmark
Henrik H. Svensen
CEED, University of Oslo, P.O. Box 1028, 0315 Oslo, Norway
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Cited
15 citations as recorded by crossref.
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- 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
- Stratigraphic expression of the Paleocene-Eocene Thermal Maximum climate event during long-lived transient uplift—An example from a shallow to deep-marine clastic system in the Norwegian Sea T. Sømme et al. 10.3389/feart.2023.1082203
- Spatiotemporal distribution of global mercury enrichments through the Paleocene-Eocene Thermal Maximum and links to volcanism S. Jin et al. 10.1016/j.earscirev.2023.104647
- High-resolution sediment mass-budget of the Shetland Platform during the Paleocene–Early Eocene; constraints on external forcing by uplift and climate L. Valore et al. 10.1144/jgs2024-058
- Paleoredox conditions and paleoproductivity of the early-Eocene sediments in the Gaga Section, Western Desert, Egypt A. Mahmoud et al. 10.1016/j.jafrearsci.2025.105640
- Advances in Glendonite Understanding and Its Potential for Carbon Capture B. Schultz & J. Huggett 10.3390/min15040410
- The Eurasian epicontinental sea was an important carbon sink during the Palaeocene-Eocene thermal maximum M. Kaya et al. 10.1038/s43247-022-00451-4
- Tracing North Atlantic volcanism and seaway connectivity across the Paleocene–Eocene Thermal Maximum (PETM) M. Jones et al. 10.5194/cp-19-1623-2023
- Linking the PETM and North Atlantic volcanism using tellurium in sediments N. Baumann et al. 10.1016/j.palaeo.2024.112575
- The interplay between siliciclastic and carbonate depositional systems: Maastrichtian to Danian basin‐floor sediments of the mid‐Norwegian Møre Basin H. Kjøll et al. 10.1111/bre.12827
- Late Cretaceous evolution of chemical weathering at the northeastern South American margin inferred from mineralogy and Hf-Nd isotopes P. Corentin et al. 10.1016/j.margeo.2022.106968
- Links between Ikaite Morphology, Recrystallised Ikaite Petrography and Glendonite Pseudomorphs Determined from Polar and Deep-Sea Ikaite B. Schultz et al. 10.3390/min13070841
- Paleocene/Eocene carbon feedbacks triggered by volcanic activity S. Kender et al. 10.1038/s41467-021-25536-0
14 citations as recorded by crossref.
- The minerals ikaite and its pseudomorph glendonite: Historical perspective and legacies of Douglas Shearman and Alec K. Smith B. Schultz et al. 10.1016/j.pgeola.2022.02.003
- Middle Eocene Climatic Optimum (MECO) and its imprint in the continental Escanilla Formation, Spain N. Sharma et al. 10.5194/cp-20-935-2024
- 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
- Stratigraphic expression of the Paleocene-Eocene Thermal Maximum climate event during long-lived transient uplift—An example from a shallow to deep-marine clastic system in the Norwegian Sea T. Sømme et al. 10.3389/feart.2023.1082203
- Spatiotemporal distribution of global mercury enrichments through the Paleocene-Eocene Thermal Maximum and links to volcanism S. Jin et al. 10.1016/j.earscirev.2023.104647
- High-resolution sediment mass-budget of the Shetland Platform during the Paleocene–Early Eocene; constraints on external forcing by uplift and climate L. Valore et al. 10.1144/jgs2024-058
- Paleoredox conditions and paleoproductivity of the early-Eocene sediments in the Gaga Section, Western Desert, Egypt A. Mahmoud et al. 10.1016/j.jafrearsci.2025.105640
- Advances in Glendonite Understanding and Its Potential for Carbon Capture B. Schultz & J. Huggett 10.3390/min15040410
- The Eurasian epicontinental sea was an important carbon sink during the Palaeocene-Eocene thermal maximum M. Kaya et al. 10.1038/s43247-022-00451-4
- Tracing North Atlantic volcanism and seaway connectivity across the Paleocene–Eocene Thermal Maximum (PETM) M. Jones et al. 10.5194/cp-19-1623-2023
- Linking the PETM and North Atlantic volcanism using tellurium in sediments N. Baumann et al. 10.1016/j.palaeo.2024.112575
- The interplay between siliciclastic and carbonate depositional systems: Maastrichtian to Danian basin‐floor sediments of the mid‐Norwegian Møre Basin H. Kjøll et al. 10.1111/bre.12827
- Late Cretaceous evolution of chemical weathering at the northeastern South American margin inferred from mineralogy and Hf-Nd isotopes P. Corentin et al. 10.1016/j.margeo.2022.106968
- Links between Ikaite Morphology, Recrystallised Ikaite Petrography and Glendonite Pseudomorphs Determined from Polar and Deep-Sea Ikaite B. Schultz et al. 10.3390/min13070841
1 citations as recorded by crossref.
Discussed (final revised paper)
Latest update: 05 Jul 2025
Short summary
In this paper, we present new sedimentological, geochemical, and mineralogical data exploring the environmental response to climatic and volcanic impact during the Paleocene–Eocene Thermal Maximum (~55.9 Ma; PETM). Our data suggest a rise in continental weathering and a shift to anoxic–sulfidic conditions. This indicates a rapid environmental response to changes in the carbon cycle and temperatures and highlights the important role of shelf areas as carbon sinks driving the PETM recovery.
In this paper, we present new sedimentological, geochemical, and mineralogical data exploring...
