Long-term, continuous OsmoSampler results for interstitial waters from an active gas venting site at a shallow gas hydrate field, Umitaka Spur, eastern margin of the Japan Sea

2019 ◽  
Vol 104 ◽  
pp. 25-32
Author(s):  
Satoko Owari ◽  
Hitoshi Tomaru ◽  
Ryo Matsumoto
2018 ◽  
Vol 76 (2) ◽  
pp. 61-75
Author(s):  
Shinsuke Aoki ◽  
Shu Kyono ◽  
Takeshi Oi ◽  
Satoko Owari ◽  
Fumio Akiba ◽  
...  

2012 ◽  
Vol 77 (4) ◽  
pp. 262-267 ◽  
Author(s):  
Hitoshi Tomaru ◽  
Akihiro Hachikubo ◽  
Katsunori Yanagawa ◽  
Yasuyuki Muramatsu ◽  
Hiroya Anzai ◽  
...  

2009 ◽  
Vol 118 (5) ◽  
pp. 986-1007 ◽  
Author(s):  
Hideaki MACHIYAMA ◽  
Masataka KINOSHITA ◽  
Rika TAKEUCHI ◽  
Ryo MATSUMOTO ◽  
Makoto YAMANO ◽  
...  

2012 ◽  
Vol 2012 ◽  
pp. 1-14 ◽  
Author(s):  
Antonio Fernando Menezes Freire ◽  
Ryo Matsumoto ◽  
Fumio Akiba

The Holocene sediments of the eastern margin of the Japan Sea are characterized by high total organic carbon (TOC) and total nitrogen (TN) contents, low TOC/TN and TS/TOC values with enriched δ13Corg signatures, as a result of high marine productivity during present oxic highstand. On the other hand, the LGM sediments are characterized by low TOC and TN contents, high TOC/TN and TS/TOC values with depleted δ13Corg signatures, characteristic of C3-derived terrestrial organic matter input during that anoxic lowstand. However, at the top of mounds at the seafloor, where gas hydrate and authigenic carbonate nodules occur, the host sediments have a mixture of both Holocene and LGM geochemical signatures. Both gas hydrate and authigenic carbonate, formed by the anaerobic oxidation of methane, increased the sedimentary volume and caused an uplift of older sediments, inducing mound formation. The thickness of the Holocene sediments over mounds is very small or absent exposing the last glacial maximum (LGM) sediments to the seafloor. The uplift of the LGM sediments within mounds is estimated to be >2 m. We conducted geochemical analysis to detect such sediment movement, using samples collected by shallow cores in the Joetsu Basin, eastern margin of the Japan Sea.


Island Arc ◽  
1995 ◽  
Vol 4 (3) ◽  
pp. 166-181 ◽  
Author(s):  
Yukinobu Okamura ◽  
Mahito Watanabe ◽  
Rie Morijiri ◽  
Mikio Satoh

2012 ◽  
Vol 27 (12) ◽  
pp. 2389-2402 ◽  
Author(s):  
Yasunori Mahara ◽  
Tomoko Ohta ◽  
Tomochika Tokunaga ◽  
Hiroyuki Matsuzaki ◽  
Eiji Nakata ◽  
...  

1999 ◽  
Vol 302 (1-2) ◽  
pp. 1-7 ◽  
Author(s):  
Toshinori Sato ◽  
Gou Fujie ◽  
Sadayuki Koresawa ◽  
Junzo Kasahara ◽  
Keisuke Tanaka ◽  
...  

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