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LEADER 00000cam  2200745Ii 4500 
001    ocn900729199 
003    OCoLC 
005    20200419055507.4 
006    m     o  d         
007    cr cnu|||unuuu 
008    150126s2015    ja a    ob    000 0 eng d 
015    GBB9C0900|2bnb 
016 7  019448277|2Uk 
019    903954749|a904724942 
020    9784431548652|q(electronic book) 
020    4431548653|q(electronic book) 
020    4431548645 
020    9784431548645 
020    |z9784431548645 
024 7  10.1007/978-4-431-54865-2|2doi 
035    (OCoLC)900729199|z(OCoLC)903954749|z(OCoLC)904724942 
037    com.springer.onix.9784431548652|bSpringer Nature 
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049    STJJ 
050  4 QH541.5.D35 
072  7 RGM|2bicssc 
072  7 SCI031000|2bisacsh 
072  7 SCI086000|2bisacsh 
082 04 577.7/99|223 
245 00 Subseafloor biosphere linked to hydrothermal systems :
       |bTAIGA concept /|cJun-ichiro Ishibashi, Kyoko Okino, 
       Michinari Sunamura, editors. 
264  1 Tokyo :|bSpringerOpen,|c2015. 
300    1 online resource (xviii, 666 pages) :|billustrations 
       (some color) 
336    text|btxt|2rdacontent 
337    computer|bc|2rdamedia 
338    online resource|bcr|2rdacarrier 
347    text file|bPDF|2rda 
504    Includes bibliographical references at the end of each 
       chapters. 
505 0  Introduction: concept of TAIGA -- Geochemical constraints 
       on potential biomass sustained by subseafloor water-rock 
       interactions -- Microbial cell densities, community 
       structures, and growth in the hydrothermal plumes of 
       subduction hydrothermal systems -- Systematics of 
       distributions of various elements between ferromanganese 
       oxides and seawater from natural observation, 
       thermodynamics, and structures -- Evaluating hydrothermal 
       system evolution using geochronological dating and 
       biological diversity analyses -- Quantification of 
       microbial communities in hydrothermal vent habitats of the
       Southern Mariana Trough and the Mid-Okinawa Trough -- 
       Development of hydrothermal and frictional experimental 
       systems to simulate sub-seafloor water?rock?microbe 
       interactions -- Experimental hydrogen production in 
       hydrothermal and fault systems: Significance for 
       habitability of subseafloor H2 chemoautotroph microbial 
       ecosystems -- Experimental assessment of microbial effects
       on chemical interaction between seafloor massive sulfides 
       and seawater at 4°C -- A compilation of the stable 
       isotopic compositions of carbon, nitrogen, and sulfur in 
       soft body parts of animals collected from deep-sea 
       hydrothermal vent and methane seep fields: variations in 
       energy source and importance of subsurface microbial 
       processes in the sediment-hosted systems -- Tectonic 
       background of four hydrothermal fields along the Central 
       Indian Ridge -- Indian Ocean hydrothermal systems: 
       seafloor hydrothermal activities, physical and chemical 
       characteristics of hydrothermal fluids, and vent-
       associated biological communities -- Petrology and 
       geochemistry of mid-ocean ridge basalts from the southern 
       Central Indian Ridge -- Petrology of peridotites and 
       related gabbroic rocks around the Kairei-hydrothermal 
       field in the Central Indian Ridge -- Distribution and 
       Biogeochemical Properties of Hydrothermal Plumes in the 
       Rodriguez Triple Junction -- Vent fauna in the Central 
       Indian Ridge -- The mantle dynamics, the crustal formation,
       and the hydrothermal activity of the Southern Mariana 
       Trough back-arc Basin -- Seismic structure and seismicity 
       in the Southern Mariana Trough and their relation to 
       hydrothermal activity -- Electrical resistivity structure 
       of the Snail site at the Southern Mariana Trough spreading
       center -- Asymmetric seafloor spreading of the southern 
       Mariana Trough back-arc basin -- Geochemical 
       characteristics of active backarc basin volcanisms at the 
       southern end of Mariana Trough -- Mineralogical and 
       geochemical characteristics of hydrothermal minerals 
       collected from hydrothermal vent fields in the Southern 
       Mariana spreading center -- Dating of hydrothermal 
       mineralization in active hydrothermal fields in the 
       Southern Mariana Trough -- Intra-field variation of 
       prokaryotic communities on and below the seafloor in the 
       back-arc hydrothermal system of the Southern Mariana 
       Trough -- Vent fauna in the Mariana Trough -- Population 
       history of a hydrothermal vent-endemic snail Alviniconcha 
       hessleri in the Mariana Trough -- Hydrothermal activity in
       the Okinawa Trough backarc basin -geological background 
       and hydrothermal mineralization- -- Active rifting 
       structures in Iheya Graben and adjacent area of the mid-
       Okinawa Trough observed through seismic reflection surveys
       -- ESR dating of barite in sea-floor hydrothermal sulfide 
       deposits in the Okinawa Trough -- Fluid geochemistry of 
       high-temperature hydrothermal fields in the Okinawa Trough
       -- Sediment?pore water system associated with native 
       sulfur formation at Jade hydrothermal field in Okinawa 
       Trough -- Comparative investigation of microbial 
       communities associated with hydrothermal activities in the
       Okinawa Trough -- In situ determination of bacterial 
       growth in mixing zone of hydrothermal vent field on the 
       Hatoma Knoll, Southern Okinawa Trough -- Vent Fauna in the
       Okinawa Trough -- Brief report of side-scan sonar 
       observations around the Yokoniwa NTO massif -- Examination
       of volcanic activity: AUV and submersible observations of 
       fine-scale lava flow distributions along the Southern 
       Mariana Trough spreading axis -- Brief report of side-scan
       sonar imagery observations of the Archaean, Pika, and 
       Urashima hydrothermal sites -- The Yoron Hole: the 
       shallowest hydrothermal site in the Okinawa Trough -- The 
       Irabu Knoll: Hydrothermal site at the eastern edge of the 
       Yaeyama Graben -- Tarama Knoll: Geochemical and biological
       profiles of hydrothermal activity -- Petrography and 
       geochemistry of basement rocks drilled from Snail, 
       Yamanaka, Archean, and Pika hydrothermal fields at the 
       Southern Mariana Trough by Benthic Multi-coring System 
       (BMS) -- Pore fluid chemistry beneath active hydrothermal 
       fields in the mid-Okinawa Trough: Results of shallow 
       drilling by BMS during TAIGA11 cruise -- The 
       characteristics of the seafloor massive sulfide deposits 
       at the Hakurei Site in the Izena Hole, the Middle Okinawa 
       Trough -- Occurrence of hydrothermal alteration minerals 
       at the Jade hydrothermal field, in the Izena Hole, mid-
       Okinawa Trough -- Geochemistry of hydrothermal fluids 
       collected from active hydrothermal systems in the southern
       Mariana Trough backarc spreading center -- Gamma ray doses
       in water around sea floor hydrothermal area in South 
       Mariana -- 226Ra-210Pb and 228Ra-228Th dating of barite in
       submarine hydrothermal sulfide deposits collected at 
       Okinawa Trough and South Mariana Trough -- OSL dating of 
       sea floor sediments at the Okinawa Trough -- Immediate 
       change of radiation doses from hydrothermal deposits -- 
       Periodic behavior of deep sea current in the Hatoma Knoll 
       hydrothermal system -- The gelatinous macroplankton 
       community at the Hatoma Knoll hydrothermal vent. 
520    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 of the Southern Mariana Trough and Okinawa Trough.
588 0  Online resource; title from PDF title page (SpringerLink, 
       viewed January 26, 2015). 
590    SpringerLink|bSpringer Nature Open Access eBooks 
650  0 Hydrothermal vent ecology. 
650  0 Biogeochemistry. 
650  0 Marine geophysics. 
650  7 Biogeochemistry.|2fast|0(OCoLC)fst00832090 
650  7 Hydrothermal vent ecology.|2fast|0(OCoLC)fst00965298 
650  7 Marine geophysics.|2fast|0(OCoLC)fst01009623 
653 00 biogeowetenschappen 
653 00 biogeosciences 
653 00 geochemie 
653 00 geochemistry 
653 00 aardwetenschappen 
653 00 earth sciences 
653 00 oceanografie 
653 00 oceanography 
653 10 Geology (General) 
653 10 Geologie (algemeen) 
700 1  Ishibashi, J.|q(Junichiro),|eeditor. 
700 1  Okino, Kyoko,|eeditor. 
700 1  Sunamura, Michinari,|eeditor. 
776 08 |iPrint version:|tSubseafloor biosphere linked to 
       hydrothermal systems : Taiga concept.|dTokyo, Japan : 
       Springer Open, ©2015|hxviii, 666 pages|z9784431548645 
914    ocn900729199 
994    92|bSTJ 
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