An evolving view on biogeochemical cycling of iron

Biogeochemical cycling of iron is crucial to many environmental processes, such as ocean productivity, carbon storage, greenhouse gas emissions and the fate of nutrients, toxic metals and metalloids. Knowledge of the underlying processes involved in iron cycling has accelerated in recent years along...

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Veröffentlicht in:Nature reviews. Microbiology Jg. 19; H. 6; S. 360 - 374
Hauptverfasser: Kappler, Andreas, Bryce, Casey, Mansor, Muammar, Lueder, Ulf, Byrne, James M, Swanner, Elizabeth D
Format: Journal Article
Sprache:Englisch
Veröffentlicht: England Nature Publishing Group 01.06.2021
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ISSN:1740-1526, 1740-1534, 1740-1534
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Abstract Biogeochemical cycling of iron is crucial to many environmental processes, such as ocean productivity, carbon storage, greenhouse gas emissions and the fate of nutrients, toxic metals and metalloids. Knowledge of the underlying processes involved in iron cycling has accelerated in recent years along with appreciation of the complex network of biotic and abiotic reactions dictating the speciation, mobility and reactivity of iron in the environment. Recent studies have provided insights into novel processes in the biogeochemical iron cycle such as microbial ammonium oxidation and methane oxidation coupled to Fe(III) reduction. They have also revealed that processes in the biogeochemical iron cycle spatially overlap and may compete with each other, and that oxidation and reduction of iron occur cyclically or simultaneously in many environments. This Review discusses these advances with particular focus on their environmental consequences, including the formation of greenhouse gases and the fate of nutrients and contaminants.
AbstractList Biogeochemical cycling of iron is crucial to many environmental processes, such as ocean productivity, carbon storage, greenhouse gas emissions and the fate of nutrients, toxic metals and metalloids. Knowledge of the underlying processes involved in iron cycling has accelerated in recent years along with appreciation of the complex network of biotic and abiotic reactions dictating the speciation, mobility and reactivity of iron in the environment. Recent studies have provided insights into novel processes in the biogeochemical iron cycle such as microbial ammonium oxidation and methane oxidation coupled to Fe(III) reduction. They have also revealed that processes in the biogeochemical iron cycle spatially overlap and may compete with each other, and that oxidation and reduction of iron occur cyclically or simultaneously in many environments. This Review discusses these advances with particular focus on their environmental consequences, including the formation of greenhouse gases and the fate of nutrients and contaminants.Biogeochemical cycling of iron is crucial to many environmental processes, such as ocean productivity, carbon storage, greenhouse gas emissions and the fate of nutrients, toxic metals and metalloids. Knowledge of the underlying processes involved in iron cycling has accelerated in recent years along with appreciation of the complex network of biotic and abiotic reactions dictating the speciation, mobility and reactivity of iron in the environment. Recent studies have provided insights into novel processes in the biogeochemical iron cycle such as microbial ammonium oxidation and methane oxidation coupled to Fe(III) reduction. They have also revealed that processes in the biogeochemical iron cycle spatially overlap and may compete with each other, and that oxidation and reduction of iron occur cyclically or simultaneously in many environments. This Review discusses these advances with particular focus on their environmental consequences, including the formation of greenhouse gases and the fate of nutrients and contaminants.
Biogeochemical cycling of iron is crucial to many environmental processes, such as ocean productivity, carbon storage, greenhouse gas emissions and the fate of nutrients, toxic metals and metalloids. Knowledge of the underlying processes involved in iron cycling has accelerated in recent years along with appreciation of the complex network of biotic and abiotic reactions dictating the speciation, mobility and reactivity of iron in the environment. Recent studies have provided insights into novel processes in the biogeochemical iron cycle such as microbial ammonium oxidation and methane oxidation coupled to Fe(III) reduction. They have also revealed that processes in the biogeochemical iron cycle spatially overlap and may compete with each other, and that oxidation and reduction of iron occur cyclically or simultaneously in many environments. This Review discusses these advances with particular focus on their environmental consequences, including the formation of greenhouse gases and the fate of nutrients and contaminants.
Biogeochemical cycling of iron is crucial to many environmental processes, such as ocean productivity, carbon storage, greenhouse gas emissions and the fate of nutrients, toxic metals and metalloids. Knowledge of the underlying processes involved in iron cycling has accelerated in recent years along with appreciation of the complex network of biotic and abiotic reactions dictating the speciation, mobility and reactivity of iron in the environment. Recent studies have provided insights into novel processes in the biogeochemical iron cycle such as microbial ammonium oxidation and methane oxidation coupled to Fe(iii) reduction. They have also revealed that processes in the biogeochemical iron cycle spatially overlap and may compete with each other, and that oxidation and reduction of iron occur cyclically or simultaneously in many environments. This Review discusses these advances with particular focus on their environmental consequences, including the formation of greenhouse gases and the fate of nutrients and contaminants.In this Review, Kappler and colleagues highlight recent advances in our understanding of the biogeochemical iron cycle, exploring the great complexity of the processes involved and novel mechanistic insights that have been gained.
Author Kappler, Andreas
Bryce, Casey
Lueder, Ulf
Byrne, James M
Mansor, Muammar
Swanner, Elizabeth D
Author_xml – sequence: 1
  givenname: Andreas
  orcidid: 0000-0002-3558-9500
  surname: Kappler
  fullname: Kappler, Andreas
  email: andreas.kappler@uni-tuebingen.de
  organization: Geomicrobiology, Center for Applied Geosciences, University of Tübingen, Tübingen, Germany. andreas.kappler@uni-tuebingen.de
– sequence: 2
  givenname: Casey
  surname: Bryce
  fullname: Bryce, Casey
  organization: School of Earth Sciences, University of Bristol, Bristol, UK
– sequence: 3
  givenname: Muammar
  orcidid: 0000-0001-7830-650X
  surname: Mansor
  fullname: Mansor, Muammar
  organization: Geomicrobiology, Center for Applied Geosciences, University of Tübingen, Tübingen, Germany
– sequence: 4
  givenname: Ulf
  surname: Lueder
  fullname: Lueder, Ulf
  organization: Geomicrobiology, Center for Applied Geosciences, University of Tübingen, Tübingen, Germany
– sequence: 5
  givenname: James M
  surname: Byrne
  fullname: Byrne, James M
  organization: School of Earth Sciences, University of Bristol, Bristol, UK
– sequence: 6
  givenname: Elizabeth D
  orcidid: 0000-0001-9507-0893
  surname: Swanner
  fullname: Swanner, Elizabeth D
  organization: Department of Geological and Atmospheric Sciences, Iowa State University, Ames, IA, USA
BackLink https://www.ncbi.nlm.nih.gov/pubmed/33526911$$D View this record in MEDLINE/PubMed
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Snippet Biogeochemical cycling of iron is crucial to many environmental processes, such as ocean productivity, carbon storage, greenhouse gas emissions and the fate of...
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SubjectTerms Ammonium
Biogeochemical cycles
Biogeochemistry
Carbon sequestration
Complexity
Contaminants
Cycles
Emissions
Greenhouse gases
Heavy metals
Iron
Metalloids
Microorganisms
Nutrients
Oxidation
Speciation
Title An evolving view on biogeochemical cycling of iron
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