Carbon sequestration during the Palaeocene–Eocene Thermal Maximum by an efficient biological pump-Reference-Cited by-同舟云学术

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Carbon sequestration during the Palaeocene–Eocene Thermal Maximum by an efficient biological pump

Published:2014-04-13 Issue:5 Volume:7 Page:382-388
ISSN:1752-0894
Container-title:Nature Geoscience
language:en
Short-container-title:Nature Geosci

Author:

Ma Zhongwu,Gray Ellen,Thomas Ellen,Murphy Brandon,Zachos James,Paytan Adina

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://www.nature.com/articles/ngeo2139.pdf

Reference50 articles.

1. 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).

2. Zachos, J., Pagani, M., Sloan, L., Thomas, E. & Billups, K. Trends, rhythms, and aberrations in global climate 65 Ma to present. Science 292, 686–693 (2001).

3. McInerney, F. A. & Wing, S. L. The Paleocene–Eocene Thermal Maximum: A perturbation of carbon cycle, climate, and biosphere with implications for the future. Annu. Rev. Earth Planet. Sci. 39, 489–516 (2011).

4. Pagani, M. et al. Arctic hydrology during global warming at the Palaeocene/Eocene Thermal Maximum. Nature 442, 671–675 (2006).

5. Panchuk, K., Ridgwell, A. & Kump, L. R. Sedimentary response to Paleocene–Eocene Thermal Maximum carbon release: A model–data comparison. Geology 36, 315–318 (2008).

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