Subseafloor Biosphere Linked to Hydrothermal Systems TAIGA Concept /
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, carbo...
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| Format: | Electronic eBook |
| Language: | English |
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Tokyo :
Springer Japan : Imprint: Springer,
2015.
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| Online Access: | http://dx.doi.org/10.1007/978-4-431-54865-2 |
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Table of Contents:
- 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℃
- 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.