Terrestrial carbon isotope stratigraphy and mammal turnover during post-PETM hyperthermals in the Bighorn Basin, Wyoming, USA
<p>Paleogene hyperthermals, including the Paleocene–Eocene Thermal Maximum (PETM) and several other smaller events, represent global perturbations to Earth's climate system and are characterized by warmer temperatures, changes in floral and faunal communities, and hydrologic changes. Thes...
Main Authors: | S. J. Widlansky, R. Secord, K. E. Snell, A. E. Chew, W. C. Clyde |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2022-04-01
|
Series: | Climate of the Past |
Online Access: | https://cp.copernicus.org/articles/18/681/2022/cp-18-681-2022.pdf |
Similar Items
-
Flow depth estimates and avulsion behaviour in alluvial stratigraphy (Willwood Formation, Bighorn Basin, Wyoming, USA)
by: Brady Z. Foreman, et al.
Published: (2023-11-01) -
Environmental impact and magnitude of paleosol carbonate carbon isotope excursions marking five early Eocene hyperthermals in the Bighorn Basin, Wyoming
by: H. A. Abels, et al.
Published: (2016-05-01) -
Wyoming oil and gas fields symposium : Bighorn and Wind River Basins /
by: Cardinal, Donald F., et al.
Published: (1989) -
Wyoming oil and gas fields symposium : Bighorn and Wind River Basins /
by: Cardinal, Donald F., et al.
Published: (1989) -
Respiratory pathogens and their association with population performance in Montana and Wyoming bighorn sheep populations.
by: Carson J Butler, et al.
Published: (2018-01-01)