Articles | Volume 14, issue 10
https://doi.org/10.5194/cp-14-1391-2018
https://doi.org/10.5194/cp-14-1391-2018
Research article
 | 
04 Oct 2018
Research article |  | 04 Oct 2018

Temperature seasonality in the North American continental interior during the Early Eocene Climatic Optimum

Ethan G. Hyland, Katharine W. Huntington, Nathan D. Sheldon, and Tammo Reichgelt

Viewed

Total article views: 4,051 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,558 1,349 144 4,051 293 115 122
  • HTML: 2,558
  • PDF: 1,349
  • XML: 144
  • Total: 4,051
  • Supplement: 293
  • BibTeX: 115
  • EndNote: 122
Views and downloads (calculated since 28 Mar 2018)
Cumulative views and downloads (calculated since 28 Mar 2018)

Viewed (geographical distribution)

Total article views: 4,051 (including HTML, PDF, and XML) Thereof 3,852 with geography defined and 199 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Latest update: 20 Jan 2025
Download
Short summary
Climate equability is a paradox in paleoclimate research, but modeling suggests that strong seasonality should be a feature of greenhouse Earth periods too. Records of temperature from floral assemblages, paleosol geochemistry, clumped isotope thermometry, and downscaled models during the early Eocene show that the mean annual range of temperature was high, and may have increased during warming events. This has implications for predicting future seasonal climate impacts in continental regions.