The deep subsurface biosphere in igneous ocean crust: frontier habitats for microbiological exploration

We discuss ridge flank environments in the ocean crust as habitats for subseafloor microbial life. Oceanic ridge flanks, areas far from the magmatic and tectonic influence of seafloor spreading, comprise one of the largest and least explored microbial habitats on the planet. We describe the nature o...

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Main Authors: Katrina eEdwards, Andrew eFisher, C. Geoffrey eWheat
Format: Article
Language:English
Published: Frontiers Media S.A. 2012-02-01
Series:Frontiers in Microbiology
Subjects:
Online Access:http://journal.frontiersin.org/Journal/10.3389/fmicb.2012.00008/full
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spelling doaj-5babb12b1193498c87ddb47e930837332020-11-24T23:46:31ZengFrontiers Media S.A.Frontiers in Microbiology1664-302X2012-02-01310.3389/fmicb.2012.0000817854The deep subsurface biosphere in igneous ocean crust: frontier habitats for microbiological explorationKatrina eEdwards0Andrew eFisher1C. Geoffrey eWheat2University of Southern CaliforniaUniversity of California, Santa CruzUniversity of Alaska, FairbanksWe discuss ridge flank environments in the ocean crust as habitats for subseafloor microbial life. Oceanic ridge flanks, areas far from the magmatic and tectonic influence of seafloor spreading, comprise one of the largest and least explored microbial habitats on the planet. We describe the nature of the ridge flank crustal environments, and present a framework for delineating a continuum of conditions and processes that are likely to be important for defining subseafloor microbial "provinces." The basis for this framework is three governing sets of conditions that help to determine the nature of subseafloor biomes: crustal age, extent of fluid flow, and thermal state. We present a brief overview of subseafloor conditions, within the context of these three characteristics, for five field sites where microbial studies have been done, are underway, or have been proposed. Technical challenges remain and likely will limit progress in studies of microbial ridge-flank ecosystems, which is why it is vital to select and design future studies so as to leverage as much general understanding as possible. A characterization framework such as presented in this paper, perhaps including alternative or additional physical or chemical characteristics, is essential for achieving the greatest benefit from multidisciplinary microbial investigations of the oceanic ridge flanks.http://journal.frontiersin.org/Journal/10.3389/fmicb.2012.00008/fullEcologyMicrobiologydeep subsurfacemarinebasaltocean crust
collection DOAJ
language English
format Article
sources DOAJ
author Katrina eEdwards
Andrew eFisher
C. Geoffrey eWheat
spellingShingle Katrina eEdwards
Andrew eFisher
C. Geoffrey eWheat
The deep subsurface biosphere in igneous ocean crust: frontier habitats for microbiological exploration
Frontiers in Microbiology
Ecology
Microbiology
deep subsurface
marine
basalt
ocean crust
author_facet Katrina eEdwards
Andrew eFisher
C. Geoffrey eWheat
author_sort Katrina eEdwards
title The deep subsurface biosphere in igneous ocean crust: frontier habitats for microbiological exploration
title_short The deep subsurface biosphere in igneous ocean crust: frontier habitats for microbiological exploration
title_full The deep subsurface biosphere in igneous ocean crust: frontier habitats for microbiological exploration
title_fullStr The deep subsurface biosphere in igneous ocean crust: frontier habitats for microbiological exploration
title_full_unstemmed The deep subsurface biosphere in igneous ocean crust: frontier habitats for microbiological exploration
title_sort deep subsurface biosphere in igneous ocean crust: frontier habitats for microbiological exploration
publisher Frontiers Media S.A.
series Frontiers in Microbiology
issn 1664-302X
publishDate 2012-02-01
description We discuss ridge flank environments in the ocean crust as habitats for subseafloor microbial life. Oceanic ridge flanks, areas far from the magmatic and tectonic influence of seafloor spreading, comprise one of the largest and least explored microbial habitats on the planet. We describe the nature of the ridge flank crustal environments, and present a framework for delineating a continuum of conditions and processes that are likely to be important for defining subseafloor microbial "provinces." The basis for this framework is three governing sets of conditions that help to determine the nature of subseafloor biomes: crustal age, extent of fluid flow, and thermal state. We present a brief overview of subseafloor conditions, within the context of these three characteristics, for five field sites where microbial studies have been done, are underway, or have been proposed. Technical challenges remain and likely will limit progress in studies of microbial ridge-flank ecosystems, which is why it is vital to select and design future studies so as to leverage as much general understanding as possible. A characterization framework such as presented in this paper, perhaps including alternative or additional physical or chemical characteristics, is essential for achieving the greatest benefit from multidisciplinary microbial investigations of the oceanic ridge flanks.
topic Ecology
Microbiology
deep subsurface
marine
basalt
ocean crust
url http://journal.frontiersin.org/Journal/10.3389/fmicb.2012.00008/full
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