A microbial driver of clay mineral weathering and bioavailable Fe source under low-temperature conditions
Biotic and abiotic Fe(III) reduction of clay minerals (illite IMt-1) under low-temperature (0 and 4°C, pH 6) was studied to evaluate the effects of bioalteration on soil properties including clay structure and elemental composition. The extent of Fe reduction in bioreduced samples (∼3.8 % at 4°C and...
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ftpubmed:oai:pubmedcentral.nih.gov:9441888 2023-05-15T15:05:56+02:00 A microbial driver of clay mineral weathering and bioavailable Fe source under low-temperature conditions Jung, Jaewoo Chung, Hyun Young Ko, Youngtak Moon, Inkyeong Suh, Yeon Jee Kim, Kitae 2022-08-22 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9441888/ http://www.ncbi.nlm.nih.gov/pubmed/36071972 https://doi.org/10.3389/fmicb.2022.980078 en eng Frontiers Media S.A. http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9441888/ http://www.ncbi.nlm.nih.gov/pubmed/36071972 http://dx.doi.org/10.3389/fmicb.2022.980078 Copyright © 2022 Jung, Chung, Ko, Moon, Suh and Kim. https://creativecommons.org/licenses/by/4.0/This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms. CC-BY Front Microbiol Microbiology Text 2022 ftpubmed https://doi.org/10.3389/fmicb.2022.980078 2022-09-11T00:41:31Z Biotic and abiotic Fe(III) reduction of clay minerals (illite IMt-1) under low-temperature (0 and 4°C, pH 6) was studied to evaluate the effects of bioalteration on soil properties including clay structure and elemental composition. The extent of Fe reduction in bioreduced samples (∼3.8 % at 4°C and ∼3.1 % at 0°C) was lower than abiotic reduction (∼7.6 %) using dithionite as a strong reductant. However, variations in the illite crystallinity value of bioreduced samples (°Δ2θ = 0.580–0.625) were greater than those of abiotic reduced samples (°Δ2θ = 0.580–0.601), indicating that modification of crystal structure is unlikely to have occurred in abiotic reduction. Moreover, precipitation of secondary-phase minerals such as vivianite [Fe(2+)(3)(PO(4))(2)(⋅)8H(2)O] and nano-sized biogenic silica were shown as evidence of reductive dissolution of Fe-bearing minerals that is observed only in a bioreduced setting. Our observation of a previously undescribed microbe–mineral interaction at low-temperature suggests a significant implication for the microbially mediated mineral alteration in Arctic permafrost, deep sea sediments, and glaciated systems resulting in the release of bioavailable Fe with an impact on low-temperature biogeochemical cycles. Text Arctic permafrost PubMed Central (PMC) Arctic Frontiers in Microbiology 13 |
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PubMed Central (PMC) |
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language |
English |
topic |
Microbiology |
spellingShingle |
Microbiology Jung, Jaewoo Chung, Hyun Young Ko, Youngtak Moon, Inkyeong Suh, Yeon Jee Kim, Kitae A microbial driver of clay mineral weathering and bioavailable Fe source under low-temperature conditions |
topic_facet |
Microbiology |
description |
Biotic and abiotic Fe(III) reduction of clay minerals (illite IMt-1) under low-temperature (0 and 4°C, pH 6) was studied to evaluate the effects of bioalteration on soil properties including clay structure and elemental composition. The extent of Fe reduction in bioreduced samples (∼3.8 % at 4°C and ∼3.1 % at 0°C) was lower than abiotic reduction (∼7.6 %) using dithionite as a strong reductant. However, variations in the illite crystallinity value of bioreduced samples (°Δ2θ = 0.580–0.625) were greater than those of abiotic reduced samples (°Δ2θ = 0.580–0.601), indicating that modification of crystal structure is unlikely to have occurred in abiotic reduction. Moreover, precipitation of secondary-phase minerals such as vivianite [Fe(2+)(3)(PO(4))(2)(⋅)8H(2)O] and nano-sized biogenic silica were shown as evidence of reductive dissolution of Fe-bearing minerals that is observed only in a bioreduced setting. Our observation of a previously undescribed microbe–mineral interaction at low-temperature suggests a significant implication for the microbially mediated mineral alteration in Arctic permafrost, deep sea sediments, and glaciated systems resulting in the release of bioavailable Fe with an impact on low-temperature biogeochemical cycles. |
format |
Text |
author |
Jung, Jaewoo Chung, Hyun Young Ko, Youngtak Moon, Inkyeong Suh, Yeon Jee Kim, Kitae |
author_facet |
Jung, Jaewoo Chung, Hyun Young Ko, Youngtak Moon, Inkyeong Suh, Yeon Jee Kim, Kitae |
author_sort |
Jung, Jaewoo |
title |
A microbial driver of clay mineral weathering and bioavailable Fe source under low-temperature conditions |
title_short |
A microbial driver of clay mineral weathering and bioavailable Fe source under low-temperature conditions |
title_full |
A microbial driver of clay mineral weathering and bioavailable Fe source under low-temperature conditions |
title_fullStr |
A microbial driver of clay mineral weathering and bioavailable Fe source under low-temperature conditions |
title_full_unstemmed |
A microbial driver of clay mineral weathering and bioavailable Fe source under low-temperature conditions |
title_sort |
microbial driver of clay mineral weathering and bioavailable fe source under low-temperature conditions |
publisher |
Frontiers Media S.A. |
publishDate |
2022 |
url |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9441888/ http://www.ncbi.nlm.nih.gov/pubmed/36071972 https://doi.org/10.3389/fmicb.2022.980078 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic permafrost |
genre_facet |
Arctic permafrost |
op_source |
Front Microbiol |
op_relation |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9441888/ http://www.ncbi.nlm.nih.gov/pubmed/36071972 http://dx.doi.org/10.3389/fmicb.2022.980078 |
op_rights |
Copyright © 2022 Jung, Chung, Ko, Moon, Suh and Kim. https://creativecommons.org/licenses/by/4.0/This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms. |
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CC-BY |
op_doi |
https://doi.org/10.3389/fmicb.2022.980078 |
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Frontiers in Microbiology |
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13 |
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1766337618919817216 |