冷渗微生物群落在日本海沟陆坡较深的地方更为丰富。

Shizuka Arakawa, M. Mori, L. Li, Y. Nogi, Takako Sato, Yasuhiko Yoshida, R. Usami, C. Kato
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引用次数: 9

摘要

我们分析了日本海沟陆坡不同深度(5800 ~ 7500 m)冷渗沉积物样品中的微生物群落。结果表明,不同深度环境下典型的冷渗菌群细菌和古细菌基本相似,由三角洲变形菌群(含硫酸盐还原菌群)和产甲烷古细菌组成,它们在渗环境中硫循环中起重要作用。在更深的冷渗环境中也发现了更丰富的微生物。这些观测结果表明,在日本海沟最深处的冷渗活动可能比在较浅的陆地斜坡上更有活力。这是描述微生物数量与冷渗活性之间关系的第一个建议。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Cold-seep microbial communities are more abundant at deeper depths in the Japan Trench land slope.
We have analyzed the microbial communities in the cold-seep sediment samples obtained from different depths (5800∼7500 m) of the Japan Trench land slope. The results indicated that the typical cold-seep microbial communities of bacteria and archaea were basically similar in different depth environments and consisted of the delta-Proteobacteria (including sulfate reducing bacterial group) as well as methanogenic archaea, which played an important role in sulfur circulation in the seep environment. More abundant microbes were also identified in deeper cold-seep environments. These observations suggested that the cold-seep activity at the deepest depths of the Japan Trench might be more dynamic than in the shallower land slope. This is the first suggestion describing the relationship between microbial mass and cold-seep activity.
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