Temperature seasonality in the North American continental interior during the Early Eocene Climatic Optimum
<p>Paleogene greenhouse climate equability has long been a paradox in paleoclimate research. However, recent developments in proxy and modeling methods have suggested that strong seasonality may be a feature of at least some greenhouse Earth periods. Here we present the first multi-proxy r...
Main Authors: | E. G. Hyland, K. W. Huntington, N. D. Sheldon, T. Reichgelt |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2018-10-01
|
Series: | Climate of the Past |
Online Access: | https://www.clim-past.net/14/1391/2018/cp-14-1391-2018.pdf |
Similar Items
-
Exploring a link between the Middle Eocene Climatic Optimum and Neotethys continental arc flare-up
by: A. van der Boon, et al.
Published: (2021-01-01) -
Global mean surface temperature and climate sensitivity of the early Eocene Climatic Optimum (EECO), Paleocene–Eocene Thermal Maximum (PETM), and latest Paleocene
by: G. N. Inglis, et al.
Published: (2020-10-01) -
Seasonal trends and phenology shifts in sea surface temperature on the North American northeastern continental shelf
by: Andrew C. Thomas, et al.
Published: (2017-08-01) -
Paleobotanical proxies for early Eocene climates and ecosystems in northern North America from middle to high latitudes
by: C. K. West, et al.
Published: (2020-08-01) -
Ecology of foraminifera during the middle Eocene climatic optimum in Kutch, India
by: Sonal Khanolkar, et al.
Published: (2017-06-01)