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本文引用的文献

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Bacterial Sulfate Reduction Above 100{degrees}C in Deep-Sea Hydrothermal Vent Sediments.深海热液喷口沉积物中100℃以上的细菌硫酸盐还原作用
Science. 1992 Dec 11;258(5089):1756-7. doi: 10.1126/science.258.5089.1756.
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Extremely thermophilic fermentative archaebacteria of the genus desulfurococcus from deep-sea hydrothermal vents.深海热液喷口极端嗜热发酵古菌属脱硫球菌。
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Biogeochemical evidence that thermophilic archaea mediate the anaerobic oxidation of methane.嗜热古菌介导甲烷厌氧氧化的生物地球化学证据。
Appl Environ Microbiol. 2003 Mar;69(3):1680-6. doi: 10.1128/AEM.69.3.1680-1686.2003.
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Microbial reefs in the Black Sea fueled by anaerobic oxidation of methane.黑海的微生物礁由甲烷厌氧氧化提供能量。
Science. 2002 Aug 9;297(5583):1013-5. doi: 10.1126/science.1072502.
6
In vitro demonstration of anaerobic oxidation of methane coupled to sulphate reduction in sediment from a marine gas hydrate area.海洋天然气水合物区域沉积物中甲烷厌氧氧化耦合硫酸盐还原的体外实验证明
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7
Microbial diversity of hydrothermal sediments in the Guaymas Basin: evidence for anaerobic methanotrophic communities.瓜伊马斯盆地热液沉积物的微生物多样性：厌氧甲烷营养群落的证据
Appl Environ Microbiol. 2002 Apr;68(4):1994-2007. doi: 10.1128/AEM.68.4.1994-2007.2002.
8
A marine microbial consortium apparently mediating anaerobic oxidation of methane.一个明显介导甲烷厌氧氧化的海洋微生物群落。
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温度和压力对瓜伊马斯盆地热液沉积物中硫酸盐还原及甲烷厌氧氧化的影响

Effects of temperature and pressure on sulfate reduction and anaerobic oxidation of methane in hydrothermal sediments of Guaymas Basin.

作者信息

Kallmeyer Jens, Boetius Antje

机构信息

Max Planck Institute for Marine Microbiology, 28359 Bremen, Germany.

出版信息

Appl Environ Microbiol. 2004 Feb;70(2):1231-3. doi: 10.1128/AEM.70.2.1231-1233.2004.

DOI:10.1128/AEM.70.2.1231-1233.2004
PMID:14766611
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC348843/
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 degrees C and pressures of 1 x 10(5), 2.2 x 10(7), and 4.5 x 10(7) Pa. A maximum SR of several micromoles per cubic centimeter per day was found at between 60 and 95 degrees C and 2.2 x 10(7) and 4.5 x 10(7) Pa. Maximal AOM was observed at 35 to 90 degrees C but generally accounted for less than 5% of SR.

摘要

在瓜伊马斯海盆热液深海沉积物中，于5至200摄氏度的温度以及1×10⁵、2.2×10⁷和4.5×10⁷帕的压力下，测量了硫酸盐还原（SR）速率和甲烷厌氧氧化（AOM）速率。在60至95摄氏度以及2.2×10⁷和4.5×10⁷帕的条件下，发现最大硫酸盐还原速率为每天每立方厘米几微摩尔。在35至90摄氏度观察到最大甲烷厌氧氧化速率，但通常占硫酸盐还原速率不到5%。