Warm and wet conditions in the Arctic region during Eocene Thermal Maximum 2-Reference-Cited by-同舟云学术

Warm and wet conditions in the Arctic region during Eocene Thermal Maximum 2

Published:2009-10-25 Issue:11 Volume:2 Page:777-780
ISSN:1752-0894
Container-title:Nature Geoscience
language:en
Short-container-title:Nature Geosci

Author:

Sluijs Appy,Schouten Stefan,Donders Timme H.,Schoon Petra L.,Röhl Ursula,Reichart Gert-Jan,Sangiorgi Francesca,Kim Jung-Hyun,Sinninghe Damsté Jaap S.,Brinkhuis Henk

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://www.nature.com/articles/ngeo668.pdf

Reference30 articles.

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3. Stap, L., Sluijs, A., Thomas, E. & Lourens, L. J. Patterns and magnitude of deep sea carbonate dissolution during Eocene Thermal Maximum 2 and H2, Walvis Ridge, southeastern Atlantic Ocean. Paleoceanography 24, 10.1029/2008PA001655 (2009).

4. Nicolo, M. J., Dickens, G. R., Hollis, C. J. & Zachos, J. C. Multiple early Eocene hyperthermals: Their sedimentary expression on the New Zealand continental margin and in the deep sea. Geology 35, 699–702 (2007).

5. Royer, D. L., Osborne, C. P. & Beerling, D. High CO2 increases the freezing sensitivity of plants: Implications for paleoclimatic reconstructions from fossil floras. Geology 30, 963–966 (2000).

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