Titlebook: Subseafloor Biosphere Linked to Hydrothermal Systems; TAIGA Concept Jun-ichiro Ishibashi,Kyoko Okino,Michinari Sunamur Book‘‘‘‘‘‘‘‘ 2015 Th

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Introduction of TAIGA Conceptemosynthesis. Our trans-disciplinary research between 2008 and 2012 indicates that the hypothesis is valid and the microbial activity within the flow of TAIGAs has strong linkage to chemical characteristics of each TAIGA; that is, the subseafloor TAIGA supplies four different kinds of electron donor

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Quantification of Microbial Communities in Hydrothermal Vent Habitats of the Southern Mariana Troughsed of approximately 88 % seawater. In contrast, sulfur oxidizers in . were most abundant near vent fauna habitats in the MOT. Our results suggest that the SMT hydrothermal environment is distinct from that of the MOT and affects the community structure of macrofauna and microbial flora.

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A Compilation of the Stable Isotopic Compositions of Carbon, Nitrogen, and Sulfur in Soft Body Partsnt and cold seep fields show some variations in energy sources, of both hydrothermal and microbial origins. Sediment-covered areas tend to be enriched in biomass and diversity relative to sediment-starved areas. The results suggest that fluid discharged through sediments to the seafloor are strongly

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Tectonic Background of Four Hydrothermal Fields Along the Central Indian Ridgeen newly discovered in the central CIR. The Solitaire field at 19°33′S is located about 2.6 km away from the neo-volcanic zone and is likely influenced by intra-plate volcanism. The Dodo field at 18°20′S is located at the center of the axial valley floor, where a basaltic sheet-lava flow buries the

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