How it went down last time View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2010-11-21

AUTHORS

David Archer

ABSTRACT

The Palaeocene–Eocene Thermal Maximum 55 million years ago was triggered by the sudden release of carbon to the ocean–atmosphere system. The carbon may have been removed almost as abruptly 100,000 years later, in the form of organic carbon.

PAGES

819-820

Identifiers

URI

http://scigraph.springernature.com/pub.10.1038/ngeo1031

DOI

http://dx.doi.org/10.1038/ngeo1031

DIMENSIONS

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