Uncovering the Neoproterozoic carbon cycle

D. T. Johnston (), F. A. Macdonald, B. C. Gill, P. F. Hoffman and D. P. Schrag
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D. T. Johnston: Harvard University, 20 Oxford Street, Cambridge, Massachusetts 02138, USA
F. A. Macdonald: Harvard University, 20 Oxford Street, Cambridge, Massachusetts 02138, USA
B. C. Gill: Harvard University, 20 Oxford Street, Cambridge, Massachusetts 02138, USA
P. F. Hoffman: Harvard University, 20 Oxford Street, Cambridge, Massachusetts 02138, USA
D. P. Schrag: Harvard University, 20 Oxford Street, Cambridge, Massachusetts 02138, USA

Nature, 2012, vol. 483, issue 7389, 320-323

Abstract: A quantitative mixing model coupled with new isotopic carbon data from Mongolia, northwest Canada and Namibia reveals that Neoproterozoic era carbonate isotopic anomalies can be accounted for by a primary perturbation to the surface carbon cycle, making other explanations unlikely.

Date: 2012
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DOI: 10.1038/nature10854

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