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

doi:10.1126/science.1151414

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

研究成果 › 査読

3 被引用数 (Scopus)

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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 δ³⁴S and Δ³³S values recorded for the microscopic sulfides at the North Pole.

本文言語	English
ページ（範囲）	1336c
ジャーナル	Science
巻	319
号	5868
DOI	https://doi.org/10.1126/science.1151414
出版ステータス	Published - 3月 7 2008
外部発表	はい

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10.1126/science.1151414

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AU - Farquhar, James

AU - Van Kranendonk, Martin J.

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N2 - 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 δ34S and Δ33S values recorded for the microscopic sulfides at the North Pole.

AB - 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 δ34S and Δ33S values recorded for the microscopic sulfides at the North Pole.

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Response to comment on "early archaean microorganisms preferred elemental sulfur, not sulfate"

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