Iron corrosion by methanogenic archaea characterized by stable isotope effects and crust mineralogy
Summary Carbon and hydrogen stable isotope effects associated with methane formation by the corrosive archaeon Methanobacterium strain IM1 were determined during growth with hydrogen and iron. Isotope analyses were complemented by structural, elemental and molecular composition analyses of corrosion...
Gespeichert in:
| Veröffentlicht in: | Environmental microbiology 2022-02, Vol.24 (2), p.583-595 |
|---|---|
| Hauptverfasser: | , , , , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 595 |
|---|---|
| container_issue | 2 |
| container_start_page | 583 |
| container_title | Environmental microbiology |
| container_volume | 24 |
| creator | Tamisier, Marc Schmidt, Matthias Vogt, Carsten Kümmel, Steffen Stryhanyuk, Hryhoriy Musat, Niculina Richnow, Hans‐Hermann Musat, Florin |
| description | Summary
Carbon and hydrogen stable isotope effects associated with methane formation by the corrosive archaeon Methanobacterium strain IM1 were determined during growth with hydrogen and iron. Isotope analyses were complemented by structural, elemental and molecular composition analyses of corrosion crusts. During growth with H2, strain IM1 formed methane with average δ13C of −43.5‰ and δ2H of −370‰. Corrosive growth led to methane more depleted in 13C, with average δ13C ranging from −56‰ to −64‰ during the early and the late growth phase respectively. The corresponding δ2H were less impacted by the growth phase, with average values ranging from −316 to −329‰. The stable isotope fractionation factors, α13CCO2/CH4, were 1.026 and 1.042 for hydrogenotrophic and corrosive growth respectively. Corrosion crusts formed by strain IM1 have a domed structure, appeared electrically conductive and were composed of siderite, calcite and iron sulfide, the latter formed by precipitation of sulfide (from culture medium) with ferrous iron generated during corrosion. Strain IM1 cells were found attached to crust surfaces and encrusted deep inside crust domes. Our results may assist to diagnose methanogens‐induced corrosion in the field and suggest that intrusion of sulfide in anoxic settings may stimulate corrosion by methanogenic archaea via formation of semiconductive crusts. |
| doi_str_mv | 10.1111/1462-2920.15658 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_2546975735</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2632742276</sourcerecordid><originalsourceid>FETCH-LOGICAL-c4128-560ab154726e10a11486513c7cf7c9323c4c8e11c51ee5b95aeb7f29ffed98253</originalsourceid><addsrcrecordid>eNqFkMFPwyAUh4nRuDk9ezMkXrzMFSjQHs0ydcmMFz0TSl-3Lm2Z0MbMv15q5w5e5PB4j3z8IB9C1yS6J2HNSCzolKY0jFzw5ASNjyenx57QEbrwfhtFRDIZnaMRi0kasUSMkVk622BjnbO-DF22xzW0G93YNTSlwdqZjQaNQ3XatODKL8h7yrc6qwCX3rZ2BxiKAkzrsW5ybFznW1yXDThd2fX-Ep0VuvJwddgn6P1x8TZ_nq5en5bzh9XUxIQmUy4inREeSyqARJqQOBGcMCNNIU3KKDOxSYAQwwkAz1KuIZMFTcPLeZpQzibobsjdOfvRgW9VXXoDVaUbsJ1XlMcilVyyHr39g25t55rwO0UFozKmVIpAzQbKBDveQaF2rqy12ysSqd6_6g2r3rb68R9u3Bxyu6yG_Mj_Cg8AH4DPsoL9f3lq8bIcgr8BpMCPTw</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2632742276</pqid></control><display><type>article</type><title>Iron corrosion by methanogenic archaea characterized by stable isotope effects and crust mineralogy</title><source>MEDLINE</source><source>Wiley Online Library Journals Frontfile Complete</source><creator>Tamisier, Marc ; Schmidt, Matthias ; Vogt, Carsten ; Kümmel, Steffen ; Stryhanyuk, Hryhoriy ; Musat, Niculina ; Richnow, Hans‐Hermann ; Musat, Florin</creator><creatorcontrib>Tamisier, Marc ; Schmidt, Matthias ; Vogt, Carsten ; Kümmel, Steffen ; Stryhanyuk, Hryhoriy ; Musat, Niculina ; Richnow, Hans‐Hermann ; Musat, Florin</creatorcontrib><description>Summary
Carbon and hydrogen stable isotope effects associated with methane formation by the corrosive archaeon Methanobacterium strain IM1 were determined during growth with hydrogen and iron. Isotope analyses were complemented by structural, elemental and molecular composition analyses of corrosion crusts. During growth with H2, strain IM1 formed methane with average δ13C of −43.5‰ and δ2H of −370‰. Corrosive growth led to methane more depleted in 13C, with average δ13C ranging from −56‰ to −64‰ during the early and the late growth phase respectively. The corresponding δ2H were less impacted by the growth phase, with average values ranging from −316 to −329‰. The stable isotope fractionation factors, α13CCO2/CH4, were 1.026 and 1.042 for hydrogenotrophic and corrosive growth respectively. Corrosion crusts formed by strain IM1 have a domed structure, appeared electrically conductive and were composed of siderite, calcite and iron sulfide, the latter formed by precipitation of sulfide (from culture medium) with ferrous iron generated during corrosion. Strain IM1 cells were found attached to crust surfaces and encrusted deep inside crust domes. Our results may assist to diagnose methanogens‐induced corrosion in the field and suggest that intrusion of sulfide in anoxic settings may stimulate corrosion by methanogenic archaea via formation of semiconductive crusts.</description><identifier>ISSN: 1462-2912</identifier><identifier>EISSN: 1462-2920</identifier><identifier>DOI: 10.1111/1462-2920.15658</identifier><identifier>PMID: 34190386</identifier><language>eng</language><publisher>Hoboken, USA: John Wiley & Sons, Inc</publisher><subject>Anoxia ; Archaea ; Calcite ; Carbon Isotopes - analysis ; Cell culture ; Chemical composition ; Concretions ; Corrosion ; Corrosion cell ; Corrosion effects ; Crusts ; Culture media ; Euryarchaeota ; Fractionation ; Growth ; Iron ; Iron sulfides ; Isotope fractionation ; Isotopes ; Methane ; Methanogenic archaea ; Methanogenic bacteria ; Mineralogy ; Siderite ; Stable isotopes ; Sulphides</subject><ispartof>Environmental microbiology, 2022-02, Vol.24 (2), p.583-595</ispartof><rights>2021 The Authors. published by Society for Applied Microbiology and John Wiley & Sons Ltd.</rights><rights>2021 The Authors. Environmental Microbiology published by Society for Applied Microbiology and John Wiley & Sons Ltd.</rights><rights>2021. This article is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4128-560ab154726e10a11486513c7cf7c9323c4c8e11c51ee5b95aeb7f29ffed98253</citedby><cites>FETCH-LOGICAL-c4128-560ab154726e10a11486513c7cf7c9323c4c8e11c51ee5b95aeb7f29ffed98253</cites><orcidid>0000-0002-4240-3495 ; 0000-0002-4455-158X ; 0000-0001-9539-189X</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1111%2F1462-2920.15658$$EPDF$$P50$$Gwiley$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1111%2F1462-2920.15658$$EHTML$$P50$$Gwiley$$Hfree_for_read</linktohtml><link.rule.ids>314,776,780,1411,27901,27902,45550,45551</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/34190386$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Tamisier, Marc</creatorcontrib><creatorcontrib>Schmidt, Matthias</creatorcontrib><creatorcontrib>Vogt, Carsten</creatorcontrib><creatorcontrib>Kümmel, Steffen</creatorcontrib><creatorcontrib>Stryhanyuk, Hryhoriy</creatorcontrib><creatorcontrib>Musat, Niculina</creatorcontrib><creatorcontrib>Richnow, Hans‐Hermann</creatorcontrib><creatorcontrib>Musat, Florin</creatorcontrib><title>Iron corrosion by methanogenic archaea characterized by stable isotope effects and crust mineralogy</title><title>Environmental microbiology</title><addtitle>Environ Microbiol</addtitle><description>Summary
Carbon and hydrogen stable isotope effects associated with methane formation by the corrosive archaeon Methanobacterium strain IM1 were determined during growth with hydrogen and iron. Isotope analyses were complemented by structural, elemental and molecular composition analyses of corrosion crusts. During growth with H2, strain IM1 formed methane with average δ13C of −43.5‰ and δ2H of −370‰. Corrosive growth led to methane more depleted in 13C, with average δ13C ranging from −56‰ to −64‰ during the early and the late growth phase respectively. The corresponding δ2H were less impacted by the growth phase, with average values ranging from −316 to −329‰. The stable isotope fractionation factors, α13CCO2/CH4, were 1.026 and 1.042 for hydrogenotrophic and corrosive growth respectively. Corrosion crusts formed by strain IM1 have a domed structure, appeared electrically conductive and were composed of siderite, calcite and iron sulfide, the latter formed by precipitation of sulfide (from culture medium) with ferrous iron generated during corrosion. Strain IM1 cells were found attached to crust surfaces and encrusted deep inside crust domes. Our results may assist to diagnose methanogens‐induced corrosion in the field and suggest that intrusion of sulfide in anoxic settings may stimulate corrosion by methanogenic archaea via formation of semiconductive crusts.</description><subject>Anoxia</subject><subject>Archaea</subject><subject>Calcite</subject><subject>Carbon Isotopes - analysis</subject><subject>Cell culture</subject><subject>Chemical composition</subject><subject>Concretions</subject><subject>Corrosion</subject><subject>Corrosion cell</subject><subject>Corrosion effects</subject><subject>Crusts</subject><subject>Culture media</subject><subject>Euryarchaeota</subject><subject>Fractionation</subject><subject>Growth</subject><subject>Iron</subject><subject>Iron sulfides</subject><subject>Isotope fractionation</subject><subject>Isotopes</subject><subject>Methane</subject><subject>Methanogenic archaea</subject><subject>Methanogenic bacteria</subject><subject>Mineralogy</subject><subject>Siderite</subject><subject>Stable isotopes</subject><subject>Sulphides</subject><issn>1462-2912</issn><issn>1462-2920</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><sourceid>24P</sourceid><sourceid>EIF</sourceid><recordid>eNqFkMFPwyAUh4nRuDk9ezMkXrzMFSjQHs0ydcmMFz0TSl-3Lm2Z0MbMv15q5w5e5PB4j3z8IB9C1yS6J2HNSCzolKY0jFzw5ASNjyenx57QEbrwfhtFRDIZnaMRi0kasUSMkVk622BjnbO-DF22xzW0G93YNTSlwdqZjQaNQ3XatODKL8h7yrc6qwCX3rZ2BxiKAkzrsW5ybFznW1yXDThd2fX-Ep0VuvJwddgn6P1x8TZ_nq5en5bzh9XUxIQmUy4inREeSyqARJqQOBGcMCNNIU3KKDOxSYAQwwkAz1KuIZMFTcPLeZpQzibobsjdOfvRgW9VXXoDVaUbsJ1XlMcilVyyHr39g25t55rwO0UFozKmVIpAzQbKBDveQaF2rqy12ysSqd6_6g2r3rb68R9u3Bxyu6yG_Mj_Cg8AH4DPsoL9f3lq8bIcgr8BpMCPTw</recordid><startdate>202202</startdate><enddate>202202</enddate><creator>Tamisier, Marc</creator><creator>Schmidt, Matthias</creator><creator>Vogt, Carsten</creator><creator>Kümmel, Steffen</creator><creator>Stryhanyuk, Hryhoriy</creator><creator>Musat, Niculina</creator><creator>Richnow, Hans‐Hermann</creator><creator>Musat, Florin</creator><general>John Wiley & Sons, Inc</general><general>Wiley Subscription Services, Inc</general><scope>24P</scope><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7QL</scope><scope>7ST</scope><scope>7T7</scope><scope>7TN</scope><scope>7U9</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H94</scope><scope>H95</scope><scope>H97</scope><scope>L.G</scope><scope>M7N</scope><scope>P64</scope><scope>SOI</scope><scope>7X8</scope><orcidid>https://orcid.org/0000-0002-4240-3495</orcidid><orcidid>https://orcid.org/0000-0002-4455-158X</orcidid><orcidid>https://orcid.org/0000-0001-9539-189X</orcidid></search><sort><creationdate>202202</creationdate><title>Iron corrosion by methanogenic archaea characterized by stable isotope effects and crust mineralogy</title><author>Tamisier, Marc ; Schmidt, Matthias ; Vogt, Carsten ; Kümmel, Steffen ; Stryhanyuk, Hryhoriy ; Musat, Niculina ; Richnow, Hans‐Hermann ; Musat, Florin</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4128-560ab154726e10a11486513c7cf7c9323c4c8e11c51ee5b95aeb7f29ffed98253</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>Anoxia</topic><topic>Archaea</topic><topic>Calcite</topic><topic>Carbon Isotopes - analysis</topic><topic>Cell culture</topic><topic>Chemical composition</topic><topic>Concretions</topic><topic>Corrosion</topic><topic>Corrosion cell</topic><topic>Corrosion effects</topic><topic>Crusts</topic><topic>Culture media</topic><topic>Euryarchaeota</topic><topic>Fractionation</topic><topic>Growth</topic><topic>Iron</topic><topic>Iron sulfides</topic><topic>Isotope fractionation</topic><topic>Isotopes</topic><topic>Methane</topic><topic>Methanogenic archaea</topic><topic>Methanogenic bacteria</topic><topic>Mineralogy</topic><topic>Siderite</topic><topic>Stable isotopes</topic><topic>Sulphides</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Tamisier, Marc</creatorcontrib><creatorcontrib>Schmidt, Matthias</creatorcontrib><creatorcontrib>Vogt, Carsten</creatorcontrib><creatorcontrib>Kümmel, Steffen</creatorcontrib><creatorcontrib>Stryhanyuk, Hryhoriy</creatorcontrib><creatorcontrib>Musat, Niculina</creatorcontrib><creatorcontrib>Richnow, Hans‐Hermann</creatorcontrib><creatorcontrib>Musat, Florin</creatorcontrib><collection>Wiley Online Library Open Access</collection><collection>Medline</collection><collection>MEDLINE</collection><collection>MEDLINE (Ovid)</collection><collection>MEDLINE</collection><collection>MEDLINE</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>Aqualine</collection><collection>Bacteriology Abstracts (Microbiology B)</collection><collection>Environment Abstracts</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Oceanic Abstracts</collection><collection>Virology and AIDS Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>AIDS and Cancer Research Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 3: Aquatic Pollution & Environmental Quality</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>Environment Abstracts</collection><collection>MEDLINE - Academic</collection><jtitle>Environmental microbiology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Tamisier, Marc</au><au>Schmidt, Matthias</au><au>Vogt, Carsten</au><au>Kümmel, Steffen</au><au>Stryhanyuk, Hryhoriy</au><au>Musat, Niculina</au><au>Richnow, Hans‐Hermann</au><au>Musat, Florin</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Iron corrosion by methanogenic archaea characterized by stable isotope effects and crust mineralogy</atitle><jtitle>Environmental microbiology</jtitle><addtitle>Environ Microbiol</addtitle><date>2022-02</date><risdate>2022</risdate><volume>24</volume><issue>2</issue><spage>583</spage><epage>595</epage><pages>583-595</pages><issn>1462-2912</issn><eissn>1462-2920</eissn><abstract>Summary
Carbon and hydrogen stable isotope effects associated with methane formation by the corrosive archaeon Methanobacterium strain IM1 were determined during growth with hydrogen and iron. Isotope analyses were complemented by structural, elemental and molecular composition analyses of corrosion crusts. During growth with H2, strain IM1 formed methane with average δ13C of −43.5‰ and δ2H of −370‰. Corrosive growth led to methane more depleted in 13C, with average δ13C ranging from −56‰ to −64‰ during the early and the late growth phase respectively. The corresponding δ2H were less impacted by the growth phase, with average values ranging from −316 to −329‰. The stable isotope fractionation factors, α13CCO2/CH4, were 1.026 and 1.042 for hydrogenotrophic and corrosive growth respectively. Corrosion crusts formed by strain IM1 have a domed structure, appeared electrically conductive and were composed of siderite, calcite and iron sulfide, the latter formed by precipitation of sulfide (from culture medium) with ferrous iron generated during corrosion. Strain IM1 cells were found attached to crust surfaces and encrusted deep inside crust domes. Our results may assist to diagnose methanogens‐induced corrosion in the field and suggest that intrusion of sulfide in anoxic settings may stimulate corrosion by methanogenic archaea via formation of semiconductive crusts.</abstract><cop>Hoboken, USA</cop><pub>John Wiley & Sons, Inc</pub><pmid>34190386</pmid><doi>10.1111/1462-2920.15658</doi><tpages>13</tpages><orcidid>https://orcid.org/0000-0002-4240-3495</orcidid><orcidid>https://orcid.org/0000-0002-4455-158X</orcidid><orcidid>https://orcid.org/0000-0001-9539-189X</orcidid><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 1462-2912 |
| ispartof | Environmental microbiology, 2022-02, Vol.24 (2), p.583-595 |
| issn | 1462-2912 1462-2920 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_2546975735 |
| source | MEDLINE; Wiley Online Library Journals Frontfile Complete |
| subjects | Anoxia Archaea Calcite Carbon Isotopes - analysis Cell culture Chemical composition Concretions Corrosion Corrosion cell Corrosion effects Crusts Culture media Euryarchaeota Fractionation Growth Iron Iron sulfides Isotope fractionation Isotopes Methane Methanogenic archaea Methanogenic bacteria Mineralogy Siderite Stable isotopes Sulphides |
| title | Iron corrosion by methanogenic archaea characterized by stable isotope effects and crust mineralogy |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-09T22%3A08%3A18IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Iron%20corrosion%20by%20methanogenic%20archaea%20characterized%20by%20stable%20isotope%20effects%20and%20crust%20mineralogy&rft.jtitle=Environmental%20microbiology&rft.au=Tamisier,%20Marc&rft.date=2022-02&rft.volume=24&rft.issue=2&rft.spage=583&rft.epage=595&rft.pages=583-595&rft.issn=1462-2912&rft.eissn=1462-2920&rft_id=info:doi/10.1111/1462-2920.15658&rft_dat=%3Cproquest_cross%3E2632742276%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2632742276&rft_id=info:pmid/34190386&rfr_iscdi=true |