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

被引：114

作者：

Kallmeyer, J

Boetius, A

机构：

[1] Max Planck Inst Marine Microbiol, D-28359 Bremen, Germany

[2] Geoforschungszentrum Potsdam, D-14473 Potsdam, Germany

[3] Alfred Wegener Inst Polar & Marine Res, D-27515 Bremerhaven, Germany

[4] Int Jacobs Univ Bremen, D-28759 Bremen, Germany

来源：

APPLIED AND ENVIRONMENTAL MICROBIOLOGY | 2004年 / 70卷 / 02期

关键词：

D O I：

10.1128/AEM.70.2.1231-1233.2004

中图分类号：

Q81 [生物工程学（生物技术）]; Q93 [微生物学];

学科分类号：

071005 ; 0836 ; 090102 ; 100705 ;

摘要：

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 200degreesC and pressures of I 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 95degreesC and 2.2 X 10(7) and 4.5 X 10(7) Pa. Maximal AOM was observed at 35 to 90degreesC but generally accounted for less than 5% of SR.

引用

收藏

页码：1231 / 1233

页数：3

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