An experimental evaluation of the use of Δ13C as a proxy for palaeoatmospheric CO2-Reference-Cited by-同舟云学术

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An experimental evaluation of the use of Δ13C as a proxy for palaeoatmospheric CO2

Published:2019-02 Issue: Volume:247 Page:162-174
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Lomax Barry H.^ORCID,Lake Janice A.,Leng Melanie J.,Jardine Phillip E.^ORCID

Funder

University of Sheffield Biology Division

Royal Society Dorothy Hodgkin Fellowship

Leverhulme Trust Early Career Fellowship

NERC New Investigators

NERC Isotope Geosciences Facilities Steering Committee

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference51 articles.

1. Carbon sequestration activated by a volcanic CO2 pulse during Ocean Anoxic Event 2;Barclay;Nat. Geosci.,2010

2. CO2 and temperature decoupling at the million-year scale during the Cretaceous Greenhouse;Barral;Sci. Rep.,2017

3. COPSE: a new model of biogeochemical cycling over Phanerozoic time;Bergman;Am. J. Sci.,2004

4. GEOCARB III: a revised model of atmospheric CO2 over Phanerozoic time;Berner;Am. J. Sci.,2001

5. GEOCARBSULF: a combined model for Phanerozoic atmospheric O2 and CO2;Berner;Geochim. Cosmochim. Acta,2006

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