Termination of global warmth at the Palaeocene/Eocene boundary through productivity feedback
Author:
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/35025035.pdf
Reference32 articles.
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4. Bains, S., Corfield, R. M. & Norris, R. D. Mechanisms of climate warming at the end of the Paleocene. Science 285, 724–727 (1999).
5. Dickens, G. R., O'Neil, J. R., Rea, D. K. & Owen, R. M. Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene. Paleoceanography 10, 965–971 (1995).
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