Articles | Volume 15, issue 1
https://doi.org/10.5194/cp-15-217-2019
© Author(s) 2019. 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-15-217-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Mercury anomalies across the Palaeocene–Eocene Thermal Maximum
Centre for Earth Evolution and Dynamics (CEED), University of Oslo,
P.O. Box 1028 Blindern, 0315 Oslo, Norway
Lawrence M. E. Percival
Department of Earth Sciences, University of Oxford, South Parks Road,
Oxford, OX1 3AN, UK
current address: Vrije Universitet Brussel, Pleinlaan 2, 1050 Brussels, Belgium
Ella W. Stokke
Centre for Earth Evolution and Dynamics (CEED), University of Oslo,
P.O. Box 1028 Blindern, 0315 Oslo, Norway
Joost Frieling
Department of Earth Sciences, Utrecht University, Princetonlaan 8a,
3584 CB, Utrecht, the Netherlands
Tamsin A. Mather
Department of Earth Sciences, University of Oxford, South Parks Road,
Oxford, OX1 3AN, UK
Lars Riber
Department of Geosciences, University of Oslo, P.O. Box 1047 Blindern,
0316 Oslo, Norway
Brian A. Schubert
School of Geosciences, University of Louisiana at Lafayette, 611
McKinley St., Hamilton Hall #323, Lafayette, LA 70504, USA
Bo Schultz
Museum Salling – Fur Museum, 7884 Fur, Denmark
Christian Tegner
Department of Geoscience, Aarhus University, Høegh-Guldbergs Gade
2, building 1672, 321, 8000 Aarhus, Denmark
Sverre Planke
Centre for Earth Evolution and Dynamics (CEED), University of Oslo,
P.O. Box 1028 Blindern, 0315 Oslo, Norway
Volcanic Basin Petroleum Research (VBPR AS), Forskningsparken,
Gaustadalléen 21, 0349 Oslo, Norway
Henrik H. Svensen
Centre for Earth Evolution and Dynamics (CEED), University of Oslo,
P.O. Box 1028 Blindern, 0315 Oslo, Norway
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- Lithium isotope evidence for enhanced weathering and erosion during the Paleocene-Eocene Thermal Maximum P. Pogge von Strandmann et al. 10.1126/sciadv.abh4224
- Mercury contents and isotope ratios in marine and terrestrial archives across the Cretaceous/Paleocene boundary S. Li et al. 10.1016/j.earscirev.2023.104635
- Large Igneous Provinces and the Release of Thermogenic Volatiles from Sedimentary Basins H. Svensen et al. 10.2138/gselements.19.5.282
- Cretaceous to Palaeogene boundary events and palaeoenvironmental responses across pelagic sequences of the Žilina core section, Slovakia: Rock magnetic, biotic, and geochemical characterization T. Elbra et al. 10.1016/j.palaeo.2023.111682
- 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
Discussed (final revised paper)
Discussed (final revised paper)
Latest update: 14 Nov 2024
Short summary
Mercury anomalies in sedimentary rocks are used to assess whether there were periods of elevated volcanism in the geological record. We focus on five sites that cover the Palaeocene–Eocene Thermal Maximum, an extreme global warming event that occurred 55.8 million years ago. We find that sites close to the eruptions from the North Atlantic Igneous Province display significant mercury anomalies across this time interval, suggesting that magmatism played a role in the global warming event.
Mercury anomalies in sedimentary rocks are used to assess whether there were periods of elevated...