Climate of the Past
Climate of the Past
CP
Articles | Volume 17, issue 1
Articles | Volume 17, issue 1
https://doi.org/10.5194/cp-17-229-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-17-229-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 17, issue 1
Research article
 | 
18 Jan 2021
Research article |  | 18 Jan 2021

Exploring a link between the Middle Eocene Climatic Optimum and Neotethys continental arc flare-up

Annique van der Boon, Klaudia F. Kuiper, Robin van der Ploeg, Marlow Julius Cramwinckel, Maryam Honarmand, Appy Sluijs, and Wout Krijgsman

Viewed

Total article views: 4,166 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,891 1,162 113 4,166 221 141 175
  • HTML: 2,891
  • PDF: 1,162
  • XML: 113
  • Total: 4,166
  • Supplement: 221
  • BibTeX: 141
  • EndNote: 175
Views and downloads (calculated since 14 Apr 2020)
Cumulative views and downloads (calculated since 14 Apr 2020)

Viewed (geographical distribution)

Total article views: 4,166 (including HTML, PDF, and XML) Thereof 3,816 with geography defined and 350 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 09 Jan 2026
Download
Short summary
40.5 million years ago, Earth's climate warmed, but it is unknown why. Enhanced volcanism has been suggested, but this has not yet been tied to a specific region. We explore an increase in volcanism in Iran. We dated igneous rocks and compiled ages from the literature. We estimated the volume of igneous rocks in Iran in order to calculate the amount of CO2 that could have been released due to enhanced volcanism. We conclude that an increase in volcanism in Iran is a plausible cause of warming.
Read more
Share