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Updated: May 13, 2026

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微生物による炭素と硫黄の循環が,深層に埋もれたの側面の玄武岩に存在する証拠です

Mark A Lever1, Olivier Rouxel, Jeffrey C Alt

  • 1Department of Marine Sciences, University of North Carolina at Chapel Hill, Chapel Hill, NC 27599, USA. mark.lever@biology.au.dk

Science (New York, N.Y.)
|March 16, 2013
PubMed
まとめ

中洋の山脊の地下ベースルトの微生物コミュニティは,メタンと硫黄を循環させます. これらの発見は,これらの地球深層の生態系の代謝機能を明らかにします.

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