Articles | Volume 15, issue 1
https://doi.org/10.5194/cp-15-217-2019
https://doi.org/10.5194/cp-15-217-2019
Research article
 | 
06 Feb 2019
Research article |  | 06 Feb 2019

Mercury anomalies across the Palaeocene–Eocene Thermal Maximum

Morgan T. Jones, Lawrence M. E. Percival, Ella W. Stokke, Joost Frieling, Tamsin A. Mather, Lars Riber, Brian A. Schubert, Bo Schultz, Christian Tegner, Sverre Planke, and Henrik H. Svensen

Viewed

Total article views: 8,135 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
6,160 1,767 208 8,135 637 119 131
  • HTML: 6,160
  • PDF: 1,767
  • XML: 208
  • Total: 8,135
  • Supplement: 637
  • BibTeX: 119
  • EndNote: 131
Views and downloads (calculated since 09 Oct 2018)
Cumulative views and downloads (calculated since 09 Oct 2018)

Viewed (geographical distribution)

Total article views: 8,135 (including HTML, PDF, and XML) Thereof 7,500 with geography defined and 635 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Discussed (final revised paper)

Latest update: 14 Nov 2024
Download
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.