Pyrite formation from FeS and H2S is mediated through microbial redox activity
Lade...
Dateien
Datum
2019
Autor:innen
Herausgeber:innen
ISSN der Zeitschrift
Electronic ISSN
ISBN
Bibliografische Daten
Verlag
Schriftenreihe
Auflagebezeichnung
URI (zitierfähiger Link)
DOI (zitierfähiger Link)
Internationale Patentnummer
Link zur Lizenz
Angaben zur Forschungsförderung
Projekt
Open Access-Veröffentlichung
Open Access Hybrid
Sammlungen
Core Facility der Universität Konstanz
Titel in einer weiteren Sprache
Publikationstyp
Zeitschriftenartikel
Publikationsstatus
Published
Erschienen in
Proceedings of the National Academy of Sciences of the United States of America (PNAS). 2019, 116(14), pp. 6897-6902. ISSN 0027-8424. eISSN 1091-6490. Available under: doi: 10.1073/pnas.1814412116
Zusammenfassung
Pyrite is the most abundant iron−sulfur mineral in sediments. Over geological times, its burial controlled oxygen levels in the atmosphere and sulfate concentrations in seawater. However, the mechanism of pyrite formation in sediments is still being debated. We show that lithotrophic microorganisms can mediate the transformation of FeS and H2S to FeS2 at ambient temperature if metabolically coupled to methane-producing archaea. Our results provide insights into a metabolic relationship that could sustain part of the deep biosphere and lend support to the iron−sulfur-world theory that postulated FeS transformation to FeS2 as a key energy-delivering reaction for life to emerge.
Zusammenfassung in einer weiteren Sprache
Fachgebiet (DDC)
570 Biowissenschaften, Biologie
Schlagwörter
Konferenz
Rezension
undefined / . - undefined, undefined
Zitieren
ISO 690
THIEL, Joana, James M. BYRNE, Andreas KAPPLER, Bernhard SCHINK, Michael PESTER, 2019. Pyrite formation from FeS and H2S is mediated through microbial redox activity. In: Proceedings of the National Academy of Sciences of the United States of America (PNAS). 2019, 116(14), pp. 6897-6902. ISSN 0027-8424. eISSN 1091-6490. Available under: doi: 10.1073/pnas.1814412116BibTex
@article{Thiel2019-04-02Pyrit-46517,
year={2019},
doi={10.1073/pnas.1814412116},
title={Pyrite formation from FeS and H<sub>2</sub>S is mediated through microbial redox activity},
number={14},
volume={116},
issn={0027-8424},
journal={Proceedings of the National Academy of Sciences of the United States of America (PNAS)},
pages={6897--6902},
author={Thiel, Joana and Byrne, James M. and Kappler, Andreas and Schink, Bernhard and Pester, Michael}
}RDF
<rdf:RDF
xmlns:dcterms="http://purl.org/dc/terms/"
xmlns:dc="http://purl.org/dc/elements/1.1/"
xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#"
xmlns:bibo="http://purl.org/ontology/bibo/"
xmlns:dspace="http://digital-repositories.org/ontologies/dspace/0.1.0#"
xmlns:foaf="http://xmlns.com/foaf/0.1/"
xmlns:void="http://rdfs.org/ns/void#"
xmlns:xsd="http://www.w3.org/2001/XMLSchema#" >
<rdf:Description rdf:about="https://kops.uni-konstanz.de/server/rdf/resource/123456789/46517">
<dspace:isPartOfCollection rdf:resource="https://kops.uni-konstanz.de/server/rdf/resource/123456789/28"/>
<dc:contributor>Thiel, Joana</dc:contributor>
<dc:contributor>Byrne, James M.</dc:contributor>
<dcterms:rights rdf:resource="http://creativecommons.org/licenses/by/4.0/"/>
<dspace:hasBitstream rdf:resource="https://kops.uni-konstanz.de/bitstream/123456789/46517/1/Thiel_2-v38o54qbcycq3.pdf"/>
<dc:creator>Pester, Michael</dc:creator>
<dc:rights>Attribution 4.0 International</dc:rights>
<dcterms:hasPart rdf:resource="https://kops.uni-konstanz.de/bitstream/123456789/46517/1/Thiel_2-v38o54qbcycq3.pdf"/>
<dcterms:issued>2019-04-02</dcterms:issued>
<dc:contributor>Kappler, Andreas</dc:contributor>
<dcterms:isPartOf rdf:resource="https://kops.uni-konstanz.de/server/rdf/resource/123456789/28"/>
<dcterms:title>Pyrite formation from FeS and H<sub>2</sub>S is mediated through microbial redox activity</dcterms:title>
<dc:contributor>Schink, Bernhard</dc:contributor>
<foaf:homepage rdf:resource="http://localhost:8080/"/>
<dc:contributor>Pester, Michael</dc:contributor>
<bibo:uri rdf:resource="https://kops.uni-konstanz.de/handle/123456789/46517"/>
<dc:creator>Kappler, Andreas</dc:creator>
<dc:language>eng</dc:language>
<void:sparqlEndpoint rdf:resource="http://localhost/fuseki/dspace/sparql"/>
<dc:creator>Thiel, Joana</dc:creator>
<dc:creator>Byrne, James M.</dc:creator>
<dc:date rdf:datatype="http://www.w3.org/2001/XMLSchema#dateTime">2019-07-24T12:41:45Z</dc:date>
<dcterms:available rdf:datatype="http://www.w3.org/2001/XMLSchema#dateTime">2019-07-24T12:41:45Z</dcterms:available>
<dcterms:abstract xml:lang="eng">Pyrite is the most abundant iron−sulfur mineral in sediments. Over geological times, its burial controlled oxygen levels in the atmosphere and sulfate concentrations in seawater. However, the mechanism of pyrite formation in sediments is still being debated. We show that lithotrophic microorganisms can mediate the transformation of FeS and H<sub>2</sub>S to FeS<sub>2</sub> at ambient temperature if metabolically coupled to methane-producing archaea. Our results provide insights into a metabolic relationship that could sustain part of the deep biosphere and lend support to the iron−sulfur-world theory that postulated FeS transformation to FeS<sub>2</sub> as a key energy-delivering reaction for life to emerge.</dcterms:abstract>
<dc:creator>Schink, Bernhard</dc:creator>
</rdf:Description>
</rdf:RDF>Interner Vermerk
xmlui.Submission.submit.DescribeStep.inputForms.label.kops_note_fromSubmitter
Prüfungsdatum der Dissertation
Finanzierungsart
Kommentar zur Publikation
Allianzlizenz
Corresponding Authors der Uni Konstanz vorhanden
Internationale Co-Autor:innen
Universitätsbibliographie
Ja
Begutachtet
Ja
