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

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发表于 2025-3-21 16:48:02 | 显示全部楼层 |阅读模式
书目名称Subseafloor Biosphere Linked to Hydrothermal Systems
副标题TAIGA Concept
编辑Jun-ichiro Ishibashi,Kyoko Okino,Michinari Sunamur
视频video
概述Is the first synthesis of hydrothermal sites both in arc–back-arc and mid ocean ridge settings.Presents an overview as well as original work to enhance understanding.Delivers all results of the compre
图书封面Titlebook: Subseafloor Biosphere Linked to Hydrothermal Systems; TAIGA Concept Jun-ichiro Ishibashi,Kyoko Okino,Michinari Sunamur Book‘‘‘‘‘‘‘‘ 2015 Th
描述.This book is the comprehensive volume of the TAIGA (“a great river ” in Japanese) project. Supported by the Japanese government, the project examined the hypothesis that the subseafloor fluid advection system (subseafloor TAIGA)   can be categorized into four types, TAIGAs of sulfur, hydrogen, carbon (methane), and iron, according to the most dominant reducing substance, and the chemolithoautotrophic bacteria/archaea that are inextricably associated with respective types of TAIGAs which are strongly affected by their geological background such as surrounding host rocks and tectonic settings. Sub-seafloor ecosystems are sustained by hydrothermal circulation or TAIGA that carry chemical energy to the chemosynthetic microbes living in an extreme environment.  The results of the project have been summarized comprehensively in 50 chapters, and this book provides an overall introduction and relevant topics on the mid-ocean ridge system of the Indian Ocean and on the arc-backarc systems ofthe Southern Mariana Trough and Okinawa Trough..
出版日期Book‘‘‘‘‘‘‘‘ 2015
关键词Chemosynthesis; Global Biogeochemic Cycle; Hydrothermal Activity and Water-rock; Linkage between biosph
版次1
doihttps://doi.org/10.1007/978-4-431-54865-2
isbn_softcover978-4-431-56191-0
isbn_ebook978-4-431-54865-2
copyrightThe Editor(s) (if applicable) and the Author(s) 2015
The information of publication is updating

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发表于 2025-3-21 20:37:53 | 显示全部楼层
Experimental Hydrogen Production in Hydrothermal and Fault Systems: Significance for Habitability ofthat abundant H. can also be generated in a simulated fault system. This result suggests that microbial ecosystems might exist in subseafloor fault systems. Here we review the experimental constraints on hydrogen production in hydrothermal and fault systems.
发表于 2025-3-22 00:33:17 | 显示全部楼层
Introduction of TAIGA Conceptin the Earth’s element cycle. We designate these fluid advections as sub-seafloor TAIGAs (which stand for .rans-crustal .dvection and .n-situ biogeochemical processes of .lobal sub-seafloor Aquifers. In Japanese, “taiga” refers to “a great river”). This concept emphasizes dynamic signature of subsea
发表于 2025-3-22 06:37:07 | 显示全部楼层
Geochemical Constraints on Potential Biomass Sustained by Subseafloor Water–Rock Interactionsthe seafloor have attracted the interest of many researchers. This type of microorganism is known to obtain energy from inorganic substances (e.g., reduced sulfur compounds, molecular hydrogen, and methane) derived from subsurface physical and chemical processes, such as water–rock interactions. As
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Systematics of Distributions of Various Elements Between Ferromanganese Oxides and Seawater from Natissolved iron and manganese from various sources including hydrothermal activities. These precipitates can adsorb or incorporate various elements, which can affect the behavior of the elements in marine environment. In addition, these precipitates can be resources of rare metals due to their high ab
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Evaluating Hydrothermal System Evolution Using Geochronological Dating and Biological Diversity Analof obtaining reliable age information. As geochemical dating techniques, two methods applicable for hydrothermal ore minerals were developed and improved: electron spin resonance method and uranium–thorium disequilibrium method. Cross checks between the two methods generally showed good agreement fo
发表于 2025-3-23 00:13:26 | 显示全部楼层
Quantification of Microbial Communities in Hydrothermal Vent Habitats of the Southern Mariana Troughnt fields were quantitatively evaluated using catalyzed reporter deposition-fluorescence in situ hybridization (CARD-FISH). The hydrothermal vent of the Southern Mariana Trough (SMT) was dominated by colonization of gastropods in the low-temperature diffuse hydrothermal fluid, whereas macrofauna in
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