Aoki Masataka, Ehara Masayuki, Saito Yumi, Yoshioka Hideyoshi, Miyazaki Masayuki, Saito Yayoi, Miyashita Ai, Kawakami Shuji, Yamaguchi Takashi, Ohashi Akiyoshi, Nunoura Takuro, Takai Ken, Imachi Hiroyuki
Department of Subsurface Geobiological Analysis and Research (D-SUGAR), Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka, Kanagawa, Japan; Department of Environmental Systems Engineering, Nagaoka University of Technology, Nagaoka, Niigata, Japan.
Department of Environmental Systems Engineering, Nagaoka University of Technology, Nagaoka, Niigata, Japan.
PLoS One. 2014 Aug 20;9(8):e105356. doi: 10.1371/journal.pone.0105356. eCollection 2014.
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°C. Following incubation, an active AOM activity was confirmed by a tracer experiment using 13C-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.
海洋沉积物中的甲烷厌氧氧化(AOM)是一个重要的全球甲烷汇,但与AOM相关的微生物的生理特性仍知之甚少。在此,我们报告了使用一种带有聚氨酯海绵的连续流生物反应器,即向下流动悬挂海绵(DHS)生物反应器,从深海甲烷渗漏沉积物中培养AOM微生物群落的方法。我们在生物反应器中于10°C对从日本南海海槽采集的深海甲烷渗漏沉积物进行了2013天的厌氧培养。培养后,通过使用13C标记甲烷的示踪实验证实了活跃的AOM活性。系统发育分析表明,系统发育多样的古菌和细菌在生物反应器中生长。培养2013天后,主要的古菌成分是厌氧甲烷氧化菌(ANME)-2a、深海古菌群和海洋底栖菌群-D,γ-变形菌是主要的细菌谱系。荧光原位杂交分析表明,ANME-1和-2a以及大多数ANME-2c细胞在没有与潜在细菌伙伴密切物理相互作用的情况下出现。我们的数据表明,DHS生物反应器系统是培养挑剔的与甲烷渗漏相关的沉积微生物的有用系统。