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Deepest and hottest hydrothermal activity in the Okinawa Trough: the Yokosuka site at Yaeyama Knoll

Since the initial discovery of hydrothermal vents in 1977, these ‘extreme’ chemosynthetic systems have been a focus of interdisciplinary research. The Okinawa Trough (OT), located in the semi-enclosed East China Sea between the Eurasian continent and the Ryukyu arc, hosts more than 20 known vent sit...

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Autores principales: Miyazaki, Junichi, Kawagucci, Shinsuke, Makabe, Akiko, Takahashi, Ayu, Kitada, Kazuya, Torimoto, Junji, Matsui, Yohei, Tasumi, Eiji, Shibuya, Takazo, Nakamura, Kentaro, Horai, Shunsuke, Sato, Shun, Ishibashi, Jun-ichiro, Kanzaki, Hayato, Nakagawa, Satoshi, Hirai, Miho, Takaki, Yoshihiro, Okino, Kyoko, Watanabe, Hiromi Kayama, Kumagai, Hidenori, Chen, Chong
Formato: Online Artículo Texto
Lenguaje:English
Publicado: The Royal Society Publishing 2017
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5750039/
https://www.ncbi.nlm.nih.gov/pubmed/29308272
http://dx.doi.org/10.1098/rsos.171570
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author Miyazaki, Junichi
Kawagucci, Shinsuke
Makabe, Akiko
Takahashi, Ayu
Kitada, Kazuya
Torimoto, Junji
Matsui, Yohei
Tasumi, Eiji
Shibuya, Takazo
Nakamura, Kentaro
Horai, Shunsuke
Sato, Shun
Ishibashi, Jun-ichiro
Kanzaki, Hayato
Nakagawa, Satoshi
Hirai, Miho
Takaki, Yoshihiro
Okino, Kyoko
Watanabe, Hiromi Kayama
Kumagai, Hidenori
Chen, Chong
author_facet Miyazaki, Junichi
Kawagucci, Shinsuke
Makabe, Akiko
Takahashi, Ayu
Kitada, Kazuya
Torimoto, Junji
Matsui, Yohei
Tasumi, Eiji
Shibuya, Takazo
Nakamura, Kentaro
Horai, Shunsuke
Sato, Shun
Ishibashi, Jun-ichiro
Kanzaki, Hayato
Nakagawa, Satoshi
Hirai, Miho
Takaki, Yoshihiro
Okino, Kyoko
Watanabe, Hiromi Kayama
Kumagai, Hidenori
Chen, Chong
author_sort Miyazaki, Junichi
collection PubMed
description Since the initial discovery of hydrothermal vents in 1977, these ‘extreme’ chemosynthetic systems have been a focus of interdisciplinary research. The Okinawa Trough (OT), located in the semi-enclosed East China Sea between the Eurasian continent and the Ryukyu arc, hosts more than 20 known vent sites but all within a relatively narrow depth range (600–1880 m). Depth is a significant factor in determining fluid temperature and chemistry, as well as biological composition. However, due to the narrow depth range of known sites, the actual influence of depth here has been poorly resolved. Here, the Yokosuka site (2190 m), the first OT vent exceeding 2000 m depth is reported. A highly active hydrothermal vent site centred around four active vent chimneys reaching 364°C in temperature, it is the hottest in the OT. Notable Cl depletion (130 mM) and both high H(2) and CH(4) concentrations (approx. 10 mM) probably result from subcritical phase separation and thermal decomposition of sedimentary organic matter. Microbiota and fauna were generally similar to other sites in the OT, although with some different characteristics. In terms of microbiota, the H(2)-rich vent fluids in Neuschwanstein chimney resulted in the dominance of hydrogenotrophic chemolithoautotrophs such as Thioreductor and Desulfobacterium. For fauna, the dominance of the deep-sea mussel Bathymodiolus aduloides is surprising given other nearby vent sites are usually dominated by B. platifrons and/or B. japonicus, and a sponge field in the periphery dominated by Poecilosclerida is unusual for OT vents. Our insights from the Yokosuka site implies that although the distribution of animal species may be linked to depth, the constraint is perhaps not water pressure and resulting chemical properties of the vent fluid but instead physical properties of the surrounding seawater. The potential significance of these preliminary results and prospect for future research on this unique site are discussed.
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spelling pubmed-57500392018-01-07 Deepest and hottest hydrothermal activity in the Okinawa Trough: the Yokosuka site at Yaeyama Knoll Miyazaki, Junichi Kawagucci, Shinsuke Makabe, Akiko Takahashi, Ayu Kitada, Kazuya Torimoto, Junji Matsui, Yohei Tasumi, Eiji Shibuya, Takazo Nakamura, Kentaro Horai, Shunsuke Sato, Shun Ishibashi, Jun-ichiro Kanzaki, Hayato Nakagawa, Satoshi Hirai, Miho Takaki, Yoshihiro Okino, Kyoko Watanabe, Hiromi Kayama Kumagai, Hidenori Chen, Chong R Soc Open Sci Earth Science Since the initial discovery of hydrothermal vents in 1977, these ‘extreme’ chemosynthetic systems have been a focus of interdisciplinary research. The Okinawa Trough (OT), located in the semi-enclosed East China Sea between the Eurasian continent and the Ryukyu arc, hosts more than 20 known vent sites but all within a relatively narrow depth range (600–1880 m). Depth is a significant factor in determining fluid temperature and chemistry, as well as biological composition. However, due to the narrow depth range of known sites, the actual influence of depth here has been poorly resolved. Here, the Yokosuka site (2190 m), the first OT vent exceeding 2000 m depth is reported. A highly active hydrothermal vent site centred around four active vent chimneys reaching 364°C in temperature, it is the hottest in the OT. Notable Cl depletion (130 mM) and both high H(2) and CH(4) concentrations (approx. 10 mM) probably result from subcritical phase separation and thermal decomposition of sedimentary organic matter. Microbiota and fauna were generally similar to other sites in the OT, although with some different characteristics. In terms of microbiota, the H(2)-rich vent fluids in Neuschwanstein chimney resulted in the dominance of hydrogenotrophic chemolithoautotrophs such as Thioreductor and Desulfobacterium. For fauna, the dominance of the deep-sea mussel Bathymodiolus aduloides is surprising given other nearby vent sites are usually dominated by B. platifrons and/or B. japonicus, and a sponge field in the periphery dominated by Poecilosclerida is unusual for OT vents. Our insights from the Yokosuka site implies that although the distribution of animal species may be linked to depth, the constraint is perhaps not water pressure and resulting chemical properties of the vent fluid but instead physical properties of the surrounding seawater. The potential significance of these preliminary results and prospect for future research on this unique site are discussed. The Royal Society Publishing 2017-12-20 /pmc/articles/PMC5750039/ /pubmed/29308272 http://dx.doi.org/10.1098/rsos.171570 Text en © 2017 The Authors. http://creativecommons.org/licenses/by/4.0/ Published by the Royal Society under the terms of the Creative Commons Attribution License http://creativecommons.org/licenses/by/4.0/, which permits unrestricted use, provided the original author and source are credited.
spellingShingle Earth Science
Miyazaki, Junichi
Kawagucci, Shinsuke
Makabe, Akiko
Takahashi, Ayu
Kitada, Kazuya
Torimoto, Junji
Matsui, Yohei
Tasumi, Eiji
Shibuya, Takazo
Nakamura, Kentaro
Horai, Shunsuke
Sato, Shun
Ishibashi, Jun-ichiro
Kanzaki, Hayato
Nakagawa, Satoshi
Hirai, Miho
Takaki, Yoshihiro
Okino, Kyoko
Watanabe, Hiromi Kayama
Kumagai, Hidenori
Chen, Chong
Deepest and hottest hydrothermal activity in the Okinawa Trough: the Yokosuka site at Yaeyama Knoll
title Deepest and hottest hydrothermal activity in the Okinawa Trough: the Yokosuka site at Yaeyama Knoll
title_full Deepest and hottest hydrothermal activity in the Okinawa Trough: the Yokosuka site at Yaeyama Knoll
title_fullStr Deepest and hottest hydrothermal activity in the Okinawa Trough: the Yokosuka site at Yaeyama Knoll
title_full_unstemmed Deepest and hottest hydrothermal activity in the Okinawa Trough: the Yokosuka site at Yaeyama Knoll
title_short Deepest and hottest hydrothermal activity in the Okinawa Trough: the Yokosuka site at Yaeyama Knoll
title_sort deepest and hottest hydrothermal activity in the okinawa trough: the yokosuka site at yaeyama knoll
topic Earth Science
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5750039/
https://www.ncbi.nlm.nih.gov/pubmed/29308272
http://dx.doi.org/10.1098/rsos.171570
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