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  Sulfate reduction and anaerobic oxidation of methane in hydrothermal sediments of Guaymas Basin

Kallmeyer, J., & Boetius, A. (2004). Sulfate reduction and anaerobic oxidation of methane in hydrothermal sediments of Guaymas Basin. Geochimica et Cosmochimica Acta, 68(11 Suppl. Suppl. S), A406-A406.

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 Creators:
Kallmeyer, J.1, Author           
Boetius, A.2, Author           
Affiliations:
1Department of Biogeochemistry, Max Planck Institute for Marine Microbiology, Max Planck Society, ou_2481693              
2HGF MPG Joint Research Group for Deep Sea Ecology & Technology, Max Planck Institute for Marine Microbiology, Max Planck Society, ou_2481702              

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 Abstract: Rates of sulfate reduction (SR) and anaerobic oxidation of methane (AOM) in hydrothermal deep-sea sediments from Guaymas Basin were measured at temperatures of 5 to 200°C and pressures of 1 × 105, 2.2 × 107, and 4.5 × 107 Pa. A maximum SR of several micromoles per cubic centimeter per day was found at between 60 and 95°C and 2.2 × 107 and 4.5 × 107 Pa. Maximal AOM was observed at 35 to 90°C but generally accounted for less than 5% of SR.

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Language(s): eng - English
 Dates: 2004-022004-06
 Publication Status: Issued
 Pages: 3
 Publishing info: -
 Table of Contents: -
 Rev. Type: -
 Identifiers: eDoc: 222368
ISI: 000221923400700
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Title: Geochimica et Cosmochimica Acta
  Abbreviation : Geochim. Cosmochim. Acta
Source Genre: Journal
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Publ. Info: Oxford : Pergamon
Pages: - Volume / Issue: 68 (11 Suppl. Suppl. S) Sequence Number: - Start / End Page: A406 - A406 Identifier: ISSN: 0016-7037
CoNE: https://pure.mpg.de/cone/journals/resource/954925401558