Iron mineral dissolution releases iron and associated organic carbon during permafrost thaw

Iron minerals trap carbon in permafrost, preventing microbial degradation and release to the atmosphere as CO2, but the stability of this carbon as permafrost thaws is unclear. Here the authors use nanoscale analyses to show that thaw conditions stimulate Fe-reducing bacteria that trigger carbon rel...

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Autores principales: Monique S. Patzner, Carsten W. Mueller, Miroslava Malusova, Moritz Baur, Verena Nikeleit, Thomas Scholten, Carmen Hoeschen, James M. Byrne, Thomas Borch, Andreas Kappler, Casey Bryce
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Lenguaje:EN
Publicado: Nature Portfolio 2020
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Acceso en línea:https://doaj.org/article/01af01e22865425a8b45eb32c9bb5667
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spelling oai:doaj.org-article:01af01e22865425a8b45eb32c9bb56672021-12-02T13:57:55ZIron mineral dissolution releases iron and associated organic carbon during permafrost thaw10.1038/s41467-020-20102-62041-1723https://doaj.org/article/01af01e22865425a8b45eb32c9bb56672020-12-01T00:00:00Zhttps://doi.org/10.1038/s41467-020-20102-6https://doaj.org/toc/2041-1723Iron minerals trap carbon in permafrost, preventing microbial degradation and release to the atmosphere as CO2, but the stability of this carbon as permafrost thaws is unclear. Here the authors use nanoscale analyses to show that thaw conditions stimulate Fe-reducing bacteria that trigger carbon release.Monique S. PatznerCarsten W. MuellerMiroslava MalusovaMoritz BaurVerena NikeleitThomas ScholtenCarmen HoeschenJames M. ByrneThomas BorchAndreas KapplerCasey BryceNature PortfolioarticleScienceQENNature Communications, Vol 11, Iss 1, Pp 1-11 (2020)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
Monique S. Patzner
Carsten W. Mueller
Miroslava Malusova
Moritz Baur
Verena Nikeleit
Thomas Scholten
Carmen Hoeschen
James M. Byrne
Thomas Borch
Andreas Kappler
Casey Bryce
Iron mineral dissolution releases iron and associated organic carbon during permafrost thaw
description Iron minerals trap carbon in permafrost, preventing microbial degradation and release to the atmosphere as CO2, but the stability of this carbon as permafrost thaws is unclear. Here the authors use nanoscale analyses to show that thaw conditions stimulate Fe-reducing bacteria that trigger carbon release.
format article
author Monique S. Patzner
Carsten W. Mueller
Miroslava Malusova
Moritz Baur
Verena Nikeleit
Thomas Scholten
Carmen Hoeschen
James M. Byrne
Thomas Borch
Andreas Kappler
Casey Bryce
author_facet Monique S. Patzner
Carsten W. Mueller
Miroslava Malusova
Moritz Baur
Verena Nikeleit
Thomas Scholten
Carmen Hoeschen
James M. Byrne
Thomas Borch
Andreas Kappler
Casey Bryce
author_sort Monique S. Patzner
title Iron mineral dissolution releases iron and associated organic carbon during permafrost thaw
title_short Iron mineral dissolution releases iron and associated organic carbon during permafrost thaw
title_full Iron mineral dissolution releases iron and associated organic carbon during permafrost thaw
title_fullStr Iron mineral dissolution releases iron and associated organic carbon during permafrost thaw
title_full_unstemmed Iron mineral dissolution releases iron and associated organic carbon during permafrost thaw
title_sort iron mineral dissolution releases iron and associated organic carbon during permafrost thaw
publisher Nature Portfolio
publishDate 2020
url https://doaj.org/article/01af01e22865425a8b45eb32c9bb5667
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