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Science 7 March 2008:
Vol. 319. no. 5868, p. 1335
DOI: 10.1126/science.319.5868.1335a

Letters

Editorial Expression of Concern
Donald Kennedy and Bruce Alberts
Rewarding Reviewers
Matthew A. Metz
Rating Reviewers
Gary Marchionini
Preventing Inequity in International Research
Igor Rudan; Response Charles A. Nelson III, Charles H. Zeanah, Nathan A. Fox, Peter J. Marshall, Anna T. Smyke, Donald Guthrie
AIDS Vaccine Research: Consider Co-Infections
Rob Gruters and Ab Osterhaus
Corrections and Clarifications
Technical Comment Abstracts



How to Submit a Letter to the Editor



Technical Comment Abstracts

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COMMENT ON "Early Archaean Microorganisms Preferred Elemental Sulfur, Not Sulfate"
Huiming Bao, Tao Sun, Issaku Kohl, Yongbo Peng
Abstract: Philippot et al. (Reports, 14 September 2007, p. 1534) interpreted multiple-sulfur isotopic compositions of ~3.5-billion-year-old marine sulfide deposits as evidence that early Archaean microorganisms were not sulfate reducers but instead metabolized elemental sulfur. However, their data can be better explained by a scenario involving poor mixing of photochemical and surface sulfide sources.

Full text at www.sciencemag.org/cgi/content/full/319/5868/1336b

 

RESPONSE TO COMMENT ON "Early Archaean Microorganisms Preferred Elemental Sulfur, Not Sulfate"
Pascal Philippot, Mark Van Zuilen, Kevin Lepot, Christophe Thomazo, James Farquhar, Martin J. Van Kranendonk
Abstract: Our knowledge of the sulfur cycle on early Earth is still in its infancy. Nevertheless, there exist enough geochemical constraints from the rock record to show that the theoretical mixing models proposed by Bao et al. are highly unlikely to account for the range of delta34S and Delta33S values recorded for the microscopic sulfides at the North Pole.

Full text at www.sciencemag.org/cgi/content/full/319/5868/1336c

 





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Science. ISSN 0036-8075 (print), 1095-9203 (online)