A Long-Term Cultivation of an Anaerobic Methane-Oxidizing Microbial Community from Deep-Sea Methane-Seep Sediment Using a Continuous-Flow Bioreactor

被引:20
|
作者
Aoki, Masataka [1 ,2 ]
Ehara, Masayuki [2 ]
Saito, Yumi [1 ]
Yoshioka, Hideyoshi [3 ]
Miyazaki, Masayuki [1 ]
Saito, Yayoi [1 ,2 ]
Miyashita, Ai [2 ]
Kawakami, Shuji [2 ,4 ]
Yamaguchi, Takashi [2 ]
Ohashi, Akiyoshi [5 ]
Nunoura, Takuro [6 ]
Takai, Ken [1 ]
Imachi, Hiroyuki [1 ]
机构
[1] Japan Agcy Marine Earth Sci & Technol JAMSTEC, Dept Subsurface Geobiol Anal & Res D SUGAR, Yokosuka, Kanagawa, Japan
[2] Nagaoka Univ Technol, Dept Environm Syst Engn, Nagaoka, Niigata 94021, Japan
[3] Natl Inst Adv Ind Sci & Technol, Inst Georesources & Environm, Tsukuba, Ibaraki, Japan
[4] Anan Natl Coll Technol, Dept Construct Syst Engn, Anan, Tokushima, Japan
[5] Hiroshima Univ, Dept Social & Environm Engn, Hiroshima, Japan
[6] JAMSTEC, Res & Dev Ctr Marine Biosci, Yokosuka, Kanagawa, Japan
来源
PLOS ONE | 2014年 / 9卷 / 08期
基金
日本学术振兴会;
关键词
16S RIBOSOMAL-RNA; IN-SITU HYBRIDIZATION; SULFATE-REDUCING BACTERIA; MARINE SUBSURFACE SEDIMENTS; HANGING SPONGE-CUBES; METHANOTROPHIC ARCHAEA; MESSENGER-RNA; UASB REACTOR; MUD VOLCANO; SP NOV;
D O I
10.1371/journal.pone.0105356
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Anaerobic oxidation of methane (AOM) in marine sediments is an important global methane sink, but the physiological characteristics of AOM-associated microorganisms remain poorly understood. Here we report the cultivation of an AOM microbial community from deep-sea methane-seep sediment using a continuous-flow bioreactor with polyurethane sponges, called the down-flow hanging sponge (DHS) bioreactor. We anaerobically incubated deep-sea methane-seep sediment collected from the Nankai Trough, Japan, for 2,013 days in the bioreactor at 10 degrees C. Following incubation, an active AOM activity was confirmed by a tracer experiment using C-13-labeled methane. Phylogenetic analyses demonstrated that phylogenetically diverse Archaea and Bacteria grew in the bioreactor. After 2,013 days of incubation, the predominant archaeal components were anaerobic methanotroph (ANME)-2a, Deep-Sea Archaeal Group, and Marine Benthic Group-D, and Gammaproteobacteria was the dominant bacterial lineage. Fluorescence in situ hybridization analysis showed that ANME-1 and -2a, and most ANME-2c cells occurred without close physical interaction with potential bacterial partners. Our data demonstrate that the DHS bioreactor system is a useful system for cultivating fastidious methane-seep-associated sedimentary microorganisms.
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页数:14
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