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  1. 131 地震研究所
  2. 東京大学地震研究所彙報
  3. 76
  4. 3
  1. 0 資料タイプ別
  2. 30 紀要・部局刊行物
  3. 東京大学地震研究所彙報
  4. 76
  5. 3

An Introduction to the Serpentinite Biosphere in the Mariana Forearc : Capsule of the Deep Subsurface Biosphere from the Chamorro Seamount

https://doi.org/10.15083/0000032613
199517f5-9a7b-4a3b-ad8c-4e8543a96fdf
名前 / ファイル ライセンス アクション
ji0763012.pdf ji0763012.pdf (1.1 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2008-05-30
タイトル
タイトル An Introduction to the Serpentinite Biosphere in the Mariana Forearc : Capsule of the Deep Subsurface Biosphere from the Chamorro Seamount
言語 en
言語
言語 eng
キーワード
主題 Serpentinite
主題Scheme Other
キーワード
主題 serpentinite seamount
主題Scheme Other
キーワード
主題 subsurface biosphere
主題Scheme Other
キーワード
主題 serpentinite biosphere
主題Scheme Other
キーワード
主題 extremophile life
主題Scheme Other
キーワード
主題 mantle peridotite
主題Scheme Other
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
ID登録
ID登録 10.15083/0000032613
ID登録タイプ JaLC
その他のタイトル
その他のタイトル マリアナ前弧の蛇紋岩生物圏への招待 : チャモロ海山からの地下生物圏のカプセル
著者 Fujioka, Kantaro

× Fujioka, Kantaro

WEKO 126210

Fujioka, Kantaro

Search repository
Yamanaka, Toshiro

× Yamanaka, Toshiro

WEKO 126211

Yamanaka, Toshiro

Search repository
Gamo, Toshitaka

× Gamo, Toshitaka

WEKO 126212

Gamo, Toshitaka

Search repository
Inagaki, Fumio

× Inagaki, Fumio

WEKO 126213

Inagaki, Fumio

Search repository
Miwa, Tetsuya

× Miwa, Tetsuya

WEKO 126214

Miwa, Tetsuya

Search repository
Sato, Hiroshi

× Sato, Hiroshi

WEKO 126215

Sato, Hiroshi

Search repository
著者別名
識別子
識別子 126216
識別子Scheme WEKO
姓名
姓名 藤岡, 換太郎
著者別名
識別子
識別子 126217
識別子Scheme WEKO
姓名
姓名 山中, 寿郎
著者別名
識別子
識別子 126218
識別子Scheme WEKO
姓名
姓名 蒲生, 俊敬
著者別名
識別子
識別子 126219
識別子Scheme WEKO
姓名
姓名 稲垣, 史夫
著者別名
識別子
識別子 126220
識別子Scheme WEKO
姓名
姓名 三輪, 哲也
著者別名
識別子
識別子 126221
識別子Scheme WEKO
姓名
姓名 佐藤, 暢
著者所属
著者所属 海洋科学技術センター
著者所属
著者所属 筑波大学
著者所属
著者所属 北海道大学理学部
著者所属
著者所属 東京大学海洋研究所
抄録
内容記述タイプ Abstract
内容記述 n this paper we propose the possible existence of a new biosphere called the ""serpentinite biosphere."" We also suggest that serpentinites act as a receptacle of the deep biosphere. Analyses of geology, geophysics, biology, and chemistry of these ""serpentinite capsules"" are useful for determining the deepest limits of the subsurface biosphere. We obtained bathymetry, sediments, geochemical, and microbiological data from the Chamorro Seamount, a serpentinite seamount consisting of a pile of serpentinite flows in the Mariana forearc. These data reveal that serpentinite flows are products of upper mantle peridotite altered by the addition of water from the subducting slab. Alteration of peridotite to serpentinite provides hydrogen gas and methane, which are the most important energy sources for extremophile life. It also induces a buoyant rise of serpentinite diapirs, which are likely to capture and transport portions of the deep biosphere during their ascent to the surface. The conditions and the characteristics of serpentinite seamounts indicate that the serpentinite diapir is a transported capsule, or a ""postcard"" from the deep subsurface biosphere, as if meteorites are packages from space and snow is a letter from heaven. We should read them carefully to obtain a broader understanding of the subsurface biosphere.
抄録
内容記述タイプ Abstract
内容記述 我々は蛇紋岩生物圏と呼ばれる新しい生物圏の存在と蛇紋岩が地下生物圏の容器として働いている可能性を提唱する.地質学,地球物理学,生物学そして化学的な検討から蛇紋岩カプセルが地下生物圏の深さ方向の限界を知るのに有用であることを示した.マリアナ前弧の蛇紋岩フローの積み重なりからなる蛇紋岩海山の一つ,チャモロ海山から地形,堆積物,化学,微生物の試料やデータを得た.これらのデータは蛇紋岩フローは上部マントルのカンラン岩が沈み込むスラブからの水の供給によって変質したものであることを示している.カンラン岩が変質して蛇紋岩になるときに極限の生命にとって有用なエネルギーである水素ガスやメタンを供給する.また蛇紋岩ダイアピルの浮力を生じそれが地表まで上昇してくる途中に地下生物圏の物質を捕獲する可能性がある.蛇紋岩海山は蛇紋岩ダイアピルが運搬されてきた地下生物圏のカプセルまたは手紙であることを示す.あたかも隕石が宇宙からの雪が空からの手紙であるように.地下生物圏を広く理解するためにこれらを注意深く読まなければならない.
書誌情報 東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo

巻 76, 号 3, p. 417-424, 発行日 2002-02-12
ISSN
収録物識別子タイプ ISSN
収録物識別子 00408972
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AN00162258
フォーマット
内容記述タイプ Other
内容記述 application/pdf
日本十進分類法
主題 458
主題Scheme NDC
出版者
出版者 東京大学地震研究所
出版者別名
Earthquake Research Institute, University of Tokyo
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