Fluvial response to abrupt global warming at the Palaeocene/Eocene boundary

Brady Z. Foreman (), Paul L. Heller and Mark T. Clementz
Additional contact information
Brady Z. Foreman: University of Wyoming, 1000 East University Avenue
Paul L. Heller: University of Wyoming, 1000 East University Avenue
Mark T. Clementz: University of Wyoming, 1000 East University Avenue

Nature, 2012, vol. 491, issue 7422, 92-95

Abstract: The fluvial response in western Colorado to the Palaeocene/Eocene thermal maximum involves a large increase in sediment flux that lasted much longer than the vegetation, monsoon and carbon dioxide changes of the thermal maximum.

Date: 2012
References: Add references at CitEc
Citations:

Downloads: (external link)
https://www.nature.com/articles/nature11513 Abstract (text/html)
Access to the full text of the articles in this series is restricted.

Related works:
This item may be available elsewhere in EconPapers: Search for items with the same title.

Export reference: BibTeX RIS (EndNote, ProCite, RefMan) HTML/Text

Persistent link: https://EconPapers.repec.org/RePEc:nat:nature:v:491:y:2012:i:7422:d:10.1038_nature11513

Ordering information: This journal article can be ordered from
https://www.nature.com/

DOI: 10.1038/nature11513

Access Statistics for this article

Nature is currently edited by Magdalena Skipper

More articles in Nature from Nature
Bibliographic data for series maintained by Sonal Shukla () and Springer Nature Abstracting and Indexing ().