Carbon cycle dynamics and ecology revealed by the carbon isotopic composition of single organic microfossils during the Late Devonian Biotic Crisis

Author:

Cohen Phoebe A.1ORCID,Junium Christopher K.2ORCID,King Phillips Ezekiel1,Uveges Benjamin T.2ORCID

Affiliation:

1. Geosciences Department Williams College Williamstown Massachusetts USA

2. Department of Earth and Environmental Sciences Syracuse University Syracuse New York USA

Funder

American Chemical Society

National Science Foundation

Publisher

Wiley

Subject

General Earth and Planetary Sciences,General Environmental Science,Ecology, Evolution, Behavior and Systematics

Reference117 articles.

1. Carbon isotope fractionation in formation of amino acids by photosynthetic organisms;Abelson P. H.;Proceedings of the National Academy of Sciences of the United States of America,1961

2. Hydrographic conditions of the Devono‐Carboniferous North American Seaway inferred from sedimentary Mo–TOC relationships;Algeo T. J.;Palaeogeography, Palaeoclimatology, Palaeoecology,2007

3. A possible chlorophycean affinity of some Neoproterozoic acritarchs;Arouri K.;Organic Geochemistry,1999

4. Phanerozoic biodiversity mass extinctions;Bambach R. K.;Annual Review of Earth and Planetary Sciences,2006

5. Marine carbon reservoir, Corg‐Ccarb coupling, and the evolution of the Proterozoic carbon cycle;Bartley J. K.;Geology,2004

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