Methane enrichment in low-temperature hydrothermal fluids from the Suiyo Seamount in the Izu-Bonin Arc of the western Pacific Ocean

Tomohiro Toki, Urumu Tsunogai, Jun Ichiro Ishibashi, Motoo Utsumi, Toshitaka Gamo

Research output: Contribution to journalArticle

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Abstract

The gas geochemistries of high-temperature and low-temperature hydrothermal fluids (HTHFs and LTHFs, respectively) were studied for the Suiyo Seamount hydrothermal system (140°39′E, 28°33′N) in the southern Izu-Bonin (Ogasawara) Arc of the western Pacific Ocean. HTHFs (290 ± 20°C) were collected from four active vents using a gas-tight fluid sampler, which prevented the loss of volatile components through degassing during sample processing. The end-member CH4 concentrations were homogeneous across the vent fields. LTHFs were collected from four diffuse flow zones using a funnel, which was deployed on the seafloor with replacement of the seawater inside the funnel by the LTHF. Strong linear relationships were found among the concentrations of CH4, ∑CO2, and Si of the obtained samples, which ensured that the end-member chemical composition of the LTHFs could be accurately estimated. While the ∑CO2 Concentrations of the HTHFs and LTHFs were similar, all four LTHFs showed enrichment of CH:4 as compared to the HTHFs. The carbon isotopic composition of CH4 also revealed a significant difference: the LTHFS (δ13C(CH4) = -4.8 ± 0.3‰PDB) showed 13C enrichment, as compared to the HTHFs (δ13C(CH4) = -5.8 0.4‰PDB). The 13C enrichment can be explained by a combination of microbial CH4 production and oxidation after formation of the LTHFs. On the basis of the observed differences in CH4 concentrations and carbon isotopic compositions of the HTHFs and LTHFs, microbial methane oxidation and production are estimated to have comparable impacts. These results support the notion of a subseafloor microbial consortium of methanogens and methanotrophs.

Original languageEnglish
Article numberB08S13
JournalJournal of Geophysical Research: Solid Earth
Volume113
Issue number8
DOIs
Publication statusPublished - Aug 4 2008

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seamounts
Pacific Ocean
Methane
seamount
hydrothermal fluid
methane
arcs
Vents
funnels
Fluids
fluids
vents
ocean
isotopic composition
Carbon
Gases
Chemical analysis
Methanogens
oxidation
Oxidation

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Geochemistry and Petrology
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science

Cite this

Methane enrichment in low-temperature hydrothermal fluids from the Suiyo Seamount in the Izu-Bonin Arc of the western Pacific Ocean. / Toki, Tomohiro; Tsunogai, Urumu; Ishibashi, Jun Ichiro; Utsumi, Motoo; Gamo, Toshitaka.

In: Journal of Geophysical Research: Solid Earth, Vol. 113, No. 8, B08S13, 04.08.2008.

Research output: Contribution to journalArticle

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