The life sulfuric: microbial ecology of sulfur cycling in marine sediments

Summary Almost the entire seafloor is covered with sediments that can be more than 10 000 m thick and represent a vast microbial ecosystem that is a major component of Earth's element and energy cycles. Notably, a significant proportion of microbial life in marine sediments can exploit energy c...

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Vydáno v:Environmental microbiology reports Ročník 9; číslo 4; s. 323 - 344
Hlavní autoři: Wasmund, Kenneth, Mußmann, Marc, Loy, Alexander
Médium: Journal Article
Jazyk:angličtina
Vydáno: United States John Wiley & Sons, Inc 01.08.2017
John Wiley and Sons Inc
Témata:
Bacteria - classification
Bacteria - genetics
Bacteria - isolation & purification
Bacteria - metabolism
Biogeochemistry
Biosphere
carbon
Carbon cycle
Cycles
Cytochrome
Ecological niches
Ecology
Ecosystem
energy
Energy conservation
Enzymes
Genetic diversity
Genetic transformation
Geologic Sediments - chemistry
Geologic Sediments - microbiology
Guilds
Hydrogen sulfide
iron
Manganese
Marine ecology
Marine ecosystems
Marine microorganisms
Marine sediments
microbial ecology
Microorganisms
Minireview
Minireviews
Molybdenum
niches
nitrogen
Ocean floor
organic sulfur compounds
Organosulfur compounds
Oxidation
phenotype
Phylogeny
Physiology
Proteins
Redox properties
Respiration
Seawater - analysis
Seawater - microbiology
Sediments
Sulfate reduction
Sulfates
Sulfur
Sulfur - analysis
Sulfur - metabolism
Sulfur compounds
Sulfur cycle
ISSN:1758-2229, 1758-2229
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Abstract Summary Almost the entire seafloor is covered with sediments that can be more than 10 000 m thick and represent a vast microbial ecosystem that is a major component of Earth's element and energy cycles. Notably, a significant proportion of microbial life in marine sediments can exploit energy conserved during transformations of sulfur compounds among different redox states. Sulfur cycling, which is primarily driven by sulfate reduction, is tightly interwoven with other important element cycles (carbon, nitrogen, iron, manganese) and therefore has profound implications for both cellular‐ and ecosystem‐level processes. Sulfur‐transforming microorganisms have evolved diverse genetic, metabolic, and in some cases, peculiar phenotypic features to fill an array of ecological niches in marine sediments. Here, we review recent and selected findings on the microbial guilds that are involved in the transformation of different sulfur compounds in marine sediments and emphasise how these are interlinked and have a major influence on ecology and biogeochemistry in the seafloor. Extraordinary discoveries have increased our knowledge on microbial sulfur cycling, mainly in sulfate‐rich surface sediments, yet many questions remain regarding how sulfur redox processes may sustain the deep‐subsurface biosphere and the impact of organic sulfur compounds on the marine sulfur cycle.
AbstractList Summary Almost the entire seafloor is covered with sediments that can be more than 10 000 m thick and represent a vast microbial ecosystem that is a major component of Earth's element and energy cycles. Notably, a significant proportion of microbial life in marine sediments can exploit energy conserved during transformations of sulfur compounds among different redox states. Sulfur cycling, which is primarily driven by sulfate reduction, is tightly interwoven with other important element cycles (carbon, nitrogen, iron, manganese) and therefore has profound implications for both cellular‐ and ecosystem‐level processes. Sulfur‐transforming microorganisms have evolved diverse genetic, metabolic, and in some cases, peculiar phenotypic features to fill an array of ecological niches in marine sediments. Here, we review recent and selected findings on the microbial guilds that are involved in the transformation of different sulfur compounds in marine sediments and emphasise how these are interlinked and have a major influence on ecology and biogeochemistry in the seafloor. Extraordinary discoveries have increased our knowledge on microbial sulfur cycling, mainly in sulfate‐rich surface sediments, yet many questions remain regarding how sulfur redox processes may sustain the deep‐subsurface biosphere and the impact of organic sulfur compounds on the marine sulfur cycle.
Almost the entire seafloor is covered with sediments that can be more than 10 000 m thick and represent a vast microbial ecosystem that is a major component of Earth's element and energy cycles. Notably, a significant proportion of microbial life in marine sediments can exploit energy conserved during transformations of sulfur compounds among different redox states. Sulfur cycling, which is primarily driven by sulfate reduction, is tightly interwoven with other important element cycles (carbon, nitrogen, iron, manganese) and therefore has profound implications for both cellular‐ and ecosystem‐level processes. Sulfur‐transforming microorganisms have evolved diverse genetic, metabolic, and in some cases, peculiar phenotypic features to fill an array of ecological niches in marine sediments. Here, we review recent and selected findings on the microbial guilds that are involved in the transformation of different sulfur compounds in marine sediments and emphasise how these are interlinked and have a major influence on ecology and biogeochemistry in the seafloor. Extraordinary discoveries have increased our knowledge on microbial sulfur cycling, mainly in sulfate‐rich surface sediments, yet many questions remain regarding how sulfur redox processes may sustain the deep‐subsurface biosphere and the impact of organic sulfur compounds on the marine sulfur cycle.
Almost the entire seafloor is covered with sediments that can be more than 10 000 m thick and represent a vast microbial ecosystem that is a major component of Earth's element and energy cycles. Notably, a significant proportion of microbial life in marine sediments can exploit energy conserved during transformations of sulfur compounds among different redox states. Sulfur cycling, which is primarily driven by sulfate reduction, is tightly interwoven with other important element cycles (carbon, nitrogen, iron, manganese) and therefore has profound implications for both cellular- and ecosystem-level processes. Sulfur-transforming microorganisms have evolved diverse genetic, metabolic, and in some cases, peculiar phenotypic features to fill an array of ecological niches in marine sediments. Here, we review recent and selected findings on the microbial guilds that are involved in the transformation of different sulfur compounds in marine sediments and emphasise how these are interlinked and have a major influence on ecology and biogeochemistry in the seafloor. Extraordinary discoveries have increased our knowledge on microbial sulfur cycling, mainly in sulfate-rich surface sediments, yet many questions remain regarding how sulfur redox processes may sustain the deep-subsurface biosphere and the impact of organic sulfur compounds on the marine sulfur cycle.Almost the entire seafloor is covered with sediments that can be more than 10 000 m thick and represent a vast microbial ecosystem that is a major component of Earth's element and energy cycles. Notably, a significant proportion of microbial life in marine sediments can exploit energy conserved during transformations of sulfur compounds among different redox states. Sulfur cycling, which is primarily driven by sulfate reduction, is tightly interwoven with other important element cycles (carbon, nitrogen, iron, manganese) and therefore has profound implications for both cellular- and ecosystem-level processes. Sulfur-transforming microorganisms have evolved diverse genetic, metabolic, and in some cases, peculiar phenotypic features to fill an array of ecological niches in marine sediments. Here, we review recent and selected findings on the microbial guilds that are involved in the transformation of different sulfur compounds in marine sediments and emphasise how these are interlinked and have a major influence on ecology and biogeochemistry in the seafloor. Extraordinary discoveries have increased our knowledge on microbial sulfur cycling, mainly in sulfate-rich surface sediments, yet many questions remain regarding how sulfur redox processes may sustain the deep-subsurface biosphere and the impact of organic sulfur compounds on the marine sulfur cycle.
Almost the entire seafloor is covered with sediments that can be more than 10 000 m thick and represent a vast microbial ecosystem that is a major component of Earth's element and energy cycles. Notably, a significant proportion of microbial life in marine sediments can exploit energy conserved during transformations of sulfur compounds among different redox states. Sulfur cycling, which is primarily driven by sulfate reduction, is tightly interwoven with other important element cycles (carbon, nitrogen, iron, manganese) and therefore has profound implications for both cellular- and ecosystem-level processes. Sulfur-transforming microorganisms have evolved diverse genetic, metabolic, and in some cases, peculiar phenotypic features to fill an array of ecological niches in marine sediments. Here, we review recent and selected findings on the microbial guilds that are involved in the transformation of different sulfur compounds in marine sediments and emphasise how these are interlinked and have a major influence on ecology and biogeochemistry in the seafloor. Extraordinary discoveries have increased our knowledge on microbial sulfur cycling, mainly in sulfate-rich surface sediments, yet many questions remain regarding how sulfur redox processes may sustain the deep-subsurface biosphere and the impact of organic sulfur compounds on the marine sulfur cycle.
Author Loy, Alexander
Wasmund, Kenneth
Mußmann, Marc
AuthorAffiliation 1 Department of Microbiology and Ecosystem Science, Division of Microbial Ecology, Research Network “Chemistry meets Microbiology” University of Vienna Althanstrasse 14 Vienna A‐1090 Austria
2 Austrian Polar Research Institute Vienna Austria
AuthorAffiliation_xml – name: 1 Department of Microbiology and Ecosystem Science, Division of Microbial Ecology, Research Network “Chemistry meets Microbiology” University of Vienna Althanstrasse 14 Vienna A‐1090 Austria
– name: 2 Austrian Polar Research Institute Vienna Austria
Author_xml – sequence: 1
  givenname: Kenneth
  surname: Wasmund
  fullname: Wasmund, Kenneth
  organization: Austrian Polar Research Institute
– sequence: 2
  givenname: Marc
  surname: Mußmann
  fullname: Mußmann, Marc
  organization: University of Vienna
– sequence: 3
  givenname: Alexander
  orcidid: 0000-0001-8923-5882
  surname: Loy
  fullname: Loy, Alexander
  email: loy@microbial-ecology.net
  organization: Austrian Polar Research Institute
BackLink https://www.ncbi.nlm.nih.gov/pubmed/28419734$$D View this record in MEDLINE/PubMed
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2017 The Authors. Environmental Microbiology published by Society for Applied Microbiology and John Wiley & Sons Ltd.
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Snippet Summary Almost the entire seafloor is covered with sediments that can be more than 10 000 m thick and represent a vast microbial ecosystem that is a major...
Almost the entire seafloor is covered with sediments that can be more than 10 000 m thick and represent a vast microbial ecosystem that is a major component of...
Almost the entire seafloor is covered with sediments that can be more than 10 000 m thick and represent a vast microbial ecosystem that is a major component of...
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StartPage 323
SubjectTerms Bacteria - classification
Bacteria - genetics
Bacteria - isolation & purification
Bacteria - metabolism
Biogeochemistry
Biosphere
carbon
Carbon cycle
Cycles
Cytochrome
Ecological niches
Ecology
Ecosystem
energy
Energy conservation
Enzymes
Genetic diversity
Genetic transformation
Geologic Sediments - chemistry
Geologic Sediments - microbiology
Guilds
Hydrogen sulfide
iron
Manganese
Marine ecology
Marine ecosystems
Marine microorganisms
Marine sediments
microbial ecology
Microorganisms
Minireview
Minireviews
Molybdenum
niches
nitrogen
Ocean floor
organic sulfur compounds
Organosulfur compounds
Oxidation
phenotype
Phylogeny
Physiology
Proteins
Redox properties
Respiration
Seawater - analysis
Seawater - microbiology
Sediments
Sulfate reduction
Sulfates
Sulfur
Sulfur - analysis
Sulfur - metabolism
Sulfur compounds
Sulfur cycle
Title The life sulfuric: microbial ecology of sulfur cycling in marine sediments
URI https://onlinelibrary.wiley.com/doi/abs/10.1111%2F1758-2229.12538
https://www.ncbi.nlm.nih.gov/pubmed/28419734
https://www.proquest.com/docview/3092268671
https://www.proquest.com/docview/1889782533
https://www.proquest.com/docview/2020911969
https://pubmed.ncbi.nlm.nih.gov/PMC5573963
Volume 9
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