Fractionation between inorganic and organic carbon during the Lomagundi (2.22–2.1 Ga) carbon isotope excursion-Reference-Cited by-同舟云学术

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Fractionation between inorganic and organic carbon during the Lomagundi (2.22–2.1 Ga) carbon isotope excursion

Published:2008-07 Issue:1-4 Volume:271 Page:278-291
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Bekker A.,Holmden C.,Beukes N.J.,Kenig F.,Eglinton B.,Patterson W.P.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference91 articles.

1. Evidence from the Lewisian limestone for isotopically heavy carbon in two-thousand-million-year-old sea water;Baker;Nature,1989

2. Heavy carbon in two-billion-year-old marbles from Lofoten-Vesterålen, Norway: implications for the Precambrian carbon cycle;Baker;Geochim. Cosmochim. Acta,1989

3. Genesis of Upper Proterozoic–Cambrian phosphorite deposits of India: isotopic inferences from carbonate fluorapatite, carbonate and organic carbon;Banerjee;Precambrian Res.,1986

4. Marine carbon reservoir, Corg–Ccarb coupling, and the evolution of the Proterozoic carbon cycle;Bartley;Geology,2004

5. Stable isotope transport and contact metamorphic fluid flow;Baumgartner;Rev. Mineral. Geochem.,2001

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