書誌事項
- タイトル別名
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- Origin of methane in subseafloor geofluid systems
- カイテイ カ チカク ナイ リュウタイケイ ノ メタン ノ キゲン
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Geofluids venting from the seafloor have been regarded as window to view the invisible subseafloor environment where vast fuels, unique biosphere, and active faults causing terrible disasters are present. Because methane originates from hot, chemical reactions and cool, microbial metabolisms in reductive subseafloor environment, an understanding of the contributors to methanogenesis in geofluid systems can provide valuable insights into microbial activity and geochemical processes in the subseafloor environment. Interpretation of the origin of methane has relied heavily on the use of geochemical tracers, such as carbon and hydrogen isotope ratios. However, the currently used geochemical tracers to distinguish each methane source are problematic in some cases and should be revised to avoid the misunderstanding of the geofluid systems. Here, the principle defining the magnitude of the change of values of the geochemical tracers is reviewed. Improved knowledge to evaluate the origin of methane in the venting geofluids will promote to illustrate what goes on in the invisible subseafloor environment.
収録刊行物
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- 地球化学
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地球化学 44 (4), 137-154, 2010
一般社団法人日本地球化学会
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詳細情報
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- CRID
- 1390282680718551296
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- NII論文ID
- 110009327692
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- NII書誌ID
- AN00141280
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- ISSN
- 21885923
- 03864073
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- NDL書誌ID
- 10976344
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- 本文言語コード
- ja
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- データソース種別
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- JaLC
- NDL
- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可