Helium and methane sources and fluxes of shallow submarine hydrothermal plumes near the Tokara Islands, Southern Japan View Full Text


Ontology type: schema:ScholarlyArticle      Open Access: True


Article Info

DATE

2016-12

AUTHORS

Hsin-Yi Wen, Yuji Sano, Naoto Takahata, Yama Tomonaga, Akizumi Ishida, Kentaro Tanaka, Takanori Kagoshima, Kotaro Shirai, Jun-Ichiro Ishibashi, Hisayoshi Yokose, Urumu Tsunogai, Tsanyao F Yang

ABSTRACT

Shallow submarine volcanoes have been newly discovered near the Tokara Islands, which are situated at the volcanic front of the northern Ryukyu Arc in southern Japan. Here, we report for the first time the volatile geochemistry of shallow hydrothermal plumes, which were sampled using a CTD-RMS system after analyzing water column images collected by multi-beam echo sounder surveys. These surveys were performed during the research cruise KS-14-10 of the R/V Shinsei Maru in a region stretching from the Wakamiko Crater to the Tokara Islands. The 3He flux and methane flux in the investigated area are estimated to be (0.99-2.6) × 104 atoms/cm2/sec and 6-60 t/yr, respectively. The methane in the region of the Tokara Islands is a mix between abiotic methane similar to that found in the East Pacific Rise and thermogenic one. Methane at the Wakamiko Crater is of abiotic origin but affected by isotopic fractionation through rapid microbial oxidation. The helium isotopes suggest the presence of subduction-type mantle helium at the Wakamiko Crater, while a larger crustal component is found close to the Tokara Islands. This suggests that the Tokara Islands submarine volcanoes are a key feature of the transition zone between the volcanic front and the spreading back-arc basin. More... »

PAGES

34126

References to SciGraph publications

Identifiers

URI

http://scigraph.springernature.com/pub.10.1038/srep34126

DOI

http://dx.doi.org/10.1038/srep34126

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1002364408

PUBMED

https://www.ncbi.nlm.nih.gov/pubmed/27671524


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