Climate model and proxy data constraints on ocean warming across the Paleocene–Eocene Thermal Maximum-Reference-Cited by-同舟云学术

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Climate model and proxy data constraints on ocean warming across the Paleocene–Eocene Thermal Maximum

Published:2013-10 Issue: Volume:125 Page:123-145
ISSN:0012-8252
Container-title:Earth-Science Reviews
language:en
Short-container-title:Earth-Science Reviews

Author:

Dunkley Jones Tom,Lunt Daniel J.,Schmidt Daniela N.,Ridgwell Andy,Sluijs Appy,Valdes Paul J.,Maslin Mark

Funder

Natural Environment Research Council (NERC)

The Royal Society Dorothy Hodgkin (TDJ)

University Research (AR, DS) Fellowships

European Research Council

European Community's Seventh Framework Program

Publisher

Elsevier BV

Subject

General Earth and Planetary Sciences

Reference115 articles.

1. Calibration of Mg/Ca thermometry in planktonic foraminifera from a sediment trap time series;Anand;Paleoceanography,2003

2. Reevaluation of the oxygen isotopic composition of planktonic foraminifera: experimental results and revised paleotemperature equations;Bemis;Paleoceanography,1998

3. A model for calcium, magnesium and sulfate in seawater over Phanerozoic time;Berner;American Journal of Science,2004

4. Early Palaeogene temperature evolution of the southwest Pacific Ocean;Bijl;Nature,2009

5. Transient middle Eocene atmospheric CO2 and temperature variations;Bijl;Science,2010

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