Deep-biosphere methane production stimulated by geofluids in the Nankai accretionary complex

Deep-biosphere methane production stimulated by geofluids in the Nankai accretionary complex

Microbial life inhabiting subseafloor sediments plays an important role in Earth’s carbon cycle. However, the impact of geodynamic processes on the distributions and carbon-cycling activities of subseafloor life remains poorly constrained. We explore a submarine mud volcano of the Nankai accretionar...

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Bibliographic Details
Main Authors: Ijiri, Akira, Inagaki, Fumio, Kubo, Yusuke, Adhikari, Rishi R., Hattori, Shohei, Hoshino, Tatsuhiko, Imachi, Hiroyuki, Kawagucci, Shinsuke, Morono, Yuki, Ohtomo, Yoko, Ono, Shuhei, Sakai, Sanae, Takai, Ken, Toki, Tomohiro, Wang, David T., Yoshinaga, Marcos Y., Arnold, Gail L., Ashi, Juichiro, Case, David H., Feseker, Tomas, Hinrichs, Kai-Uwe, Ikegawa, Yojiro, Ikehara, Minoru, Kallmeyer, Jens, Kumagai, Hidenori, Lever, Mark A., Morita, Sumito, Nakamura, Ko-ichi, Nakamura, Yuki, Nishizawa, Manabu, Orphan, Victoria J., Røy, Hans, Schmidt, Frauke, Tani, Atsushi, Tanikawa, Wataru, Terada, Takeshi, Tomaru, Hitoshi, Tsuji, Takeshi, Tsunogai, Urumu, Yamaguchi, Yasuhiko T., Yoshida, Naohiro
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Format: Article
Published: American Association for the Advancement of Science (AAAS) 2018
Online Access:http://hdl.handle.net/1721.1/118590

Internet

http://hdl.handle.net/1721.1/118590

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