Fluid geochemistry, local hydrology, and metabolic activity define methanogen community size and composition in deep-sea hydrothermal vents.

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作者： Lucy C,Stewart ^[1] ; Christopher K,Algar ^[2] ; Caroline S,Fortunato ^[3] ; Benjamin I,Larson ^[4] ; Joseph J,Vallino ^[5] ; Julie A,Huber ^[6] ; David A,Butterfield ^[7] ; James F,Holden ^[5]

作者单位： Department of Microbiology, University of Massachusetts, Amherst, MA, 01003, USA. ^[1] GNS Science, Wellington, 5010, New Zealand. ^[2] Department of Oceanography, Dalhousie University, Halifax, B3H 4R2, Canada. ^[3] Department of Biology, Wilkes University, Wilkes-Barre, PA, 18766, USA. ^[4] Joint Institute for the Study of Atmosphere and Ocean, University of Washington, Seattle, WA, 98195, USA. ^[5] Ecosystems Center, Marine Biological Laboratory, Woods Hole, MA, 02543, USA. ^[6] Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA, 02543, USA. ^[7] Department of Microbiology, University of Massachusetts, Amherst, MA, 01003, USA. jholden@microbio.umass.edu. ^[8]

主题词古细菌(Archaea);化能自养生长(Chemoautotrophic Growth);氢(Hydrogen);甲烷(Methane);海洋(Oceans and Seas)

DOI 10.1038/s41396-019-0382-3

PMID 30842565

发布时间 2023-10-14

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