scholarly journals Post-drilling changes in fluid discharge pattern, mineral deposition, and fluid chemistry in the Iheya North hydrothermal field, Okinawa Trough

2013 ◽  
Vol 14 (11) ◽  
pp. 4774-4790 ◽  
Author(s):  
Shinsuke Kawagucci ◽  
Junichi Miyazaki ◽  
Ryota Nakajima ◽  
Tatsuo Nozaki ◽  
Yutaro Takaya ◽  
...  
2021 ◽  
Vol 167 ◽  
pp. 112277
Author(s):  
Xin Huang ◽  
Chao Huang ◽  
Yali Qi ◽  
Xiaoyuan Wang ◽  
Hansheng Cao

2018 ◽  
Vol 36 (4) ◽  
pp. 393-404 ◽  
Author(s):  
Yuxiang Zhang ◽  
Zhigang Zeng ◽  
Haiyan Qi ◽  
Xuebo Yin ◽  
He Li ◽  
...  

2014 ◽  
Vol 80 (19) ◽  
pp. 6126-6135 ◽  
Author(s):  
Katsunori Yanagawa ◽  
Anja Breuker ◽  
Axel Schippers ◽  
Manabu Nishizawa ◽  
Akira Ijiri ◽  
...  

ABSTRACTThe impacts of lithologic structure and geothermal gradient on subseafloor microbial communities were investigated at a marginal site of the Iheya North hydrothermal field in the Mid-Okinawa Trough. Subsurface marine sediments composed of hemipelagic muds and volcaniclastic deposits were recovered through a depth of 151 m below the seafloor at site C0017 during Integrated Ocean Drilling Program Expedition 331. Microbial communities inferred from 16S rRNA gene clone sequencing in low-temperature hemipelagic sediments were mainly composed of members of theChloroflexiand deep-sea archaeal group. In contrast, 16S rRNA gene sequences of marine group IThaumarchaeotadominated the microbial phylotype communities in the coarse-grained pumiceous gravels interbedded between the hemipelagic sediments. Based on the physical properties of sediments such as temperature and permeability, the porewater chemistry, and the microbial phylotype compositions, the shift in the physical properties of the sediments is suggested to induce a potential subseafloor recharging flow of oxygenated seawater in the permeable zone, leading to the generation of variable chemical environments and microbial communities in the subseafloor habitats. In addition, the deepest section of sediments under high-temperature conditions (∼90°C) harbored the sequences of an uncultivated archaeal lineage of hot water crenarchaeotic group IV that may be associated with the high-temperature hydrothermal fluid flow. These results indicate that the subseafloor microbial community compositions and functions at the marginal site of the hydrothermal field are highly affected by the complex fluid flow structure, such as recharging seawater and underlying hydrothermal fluids, coupled with the lithologic transition of sediments.


2014 ◽  
Vol 64 (Pt_11) ◽  
pp. 3668-3675 ◽  
Author(s):  
Yuichi Nogi ◽  
Mariko Abe ◽  
Shinsuke Kawagucci ◽  
Hisako Hirayama

A novel psychrophilic, marine, bacterial strain designated BJ-1T was isolated from the Iheya North hydrothermal field in the Okinawa Trough off Japan. Cells were Gram-negative, rod-shaped, non-spore-forming, aerobic chemo-organotrophs and motile by means of a single polar flagellum. Growth occurred at temperatures below 16 °C, with the optimum between 9 and 12 °C. Phylogenetic analysis based on the 16S rRNA gene sequence indicated that the closest relatives of strain BJ-1T were Shewanella denitrificans OS-217T (93.5 % similarity), Shewanella profunda DSM 15900T (92.9 %), Shewanella gaetbuli TF-27T (92.9 %), Paraferrimonas sedimenticola Mok-106T (92.1 %) and Ferrimonas kyonanensis Asr22-7T (91.7 %). The major respiratory quinone was Q-8. The predominant fatty acids were C16 : 1ω7c and C16 : 0. The G+C content of the novel strain was 40.5 mol%. Based on phylogenetic, phenotypic and chemotaxonomic evidence, it is proposed that strain BJ-1T represents a novel species in a new genus, for which the name Psychrobium conchae gen. nov., sp. nov. is proposed. The type strain of Psychrobium conchae is BJ-1T ( = JCM 30103T = DSM 28701T).


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