Do microbes control the formation of giant copper deposits?
[EN] The formation of secondary copper deposits, the source of more than half of the world's production, is usually interpreted as abiogenic. In this study of the Las Cruces deposit (southwestern Spain), in situ hybridization and scanning electron microscopy analysis together with integrated ge...
| Autores: | , , , , , , , , , , |
|---|---|
| Formato: | artículo |
| Estado: | Versión aceptada para publicación |
| Fecha de publicación: | 2019 |
| País: | España |
| Recursos: | Consejo Superior de Investigaciones Científicas (CSIC) |
| Repositorio: | DIGITAL.CSIC. Repositorio Institucional del CSIC |
| OAI Identifier: | oai:digital.csic.es:10261/206071 |
| Acesso em linha: | http://hdl.handle.net/10261/206071 |
| Access Level: | acceso abierto |
| Palavra-chave: | Copper ores Cores Covellite electron microscopy data Europe giant deposits Iberian Peninsula Iberian pyrite belt massive deposits massive sulfide deposits metal ores microorganisms mineral deposits, genesis mineralization pyrite secondary minerals SEM data Southern Europe Spain sulfides southwestern Spain Las Cruces Deposit Bacteria |
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Do microbes control the formation of giant copper deposits?Tornos, F.Oggerin, M.Ríos, Asunción de losRodríguez, N.Amils, RicardoSanz, J.L.Rojas, PatriciaVelasco, F.Escobar, J.M.Gómez, C.Slack, J.F.Copper oresCoresCovelliteelectron microscopy dataEuropegiant depositsIberian PeninsulaIberian pyrite beltmassive depositsmassive sulfide depositsmetal oresmicroorganismsmineral deposits, genesismineralizationpyritesecondary mineralsSEM dataSouthern EuropeSpainsulfidessouthwestern SpainLas Cruces DepositBacteria[EN] The formation of secondary copper deposits, the source of more than half of the world's production, is usually interpreted as abiogenic. In this study of the Las Cruces deposit (southwestern Spain), in situ hybridization and scanning electron microscopy analysis together with integrated genomic and bioinformatic studies on cultures provide compelling evidence that a microbial community controls the current formation of the secondary copper mineralization. The cementation zone of this deposit contains abundant microbial life dominated by sulfate-reducing bacteria that coexist with methanogens and with other prokaryotes having unknown roles. Fractures in the primary massive sulfides are coated by extracellular polymeric substances in which the microbial cells are embedded. Covellite crystals have nucleated within these microbial aggregates, accreting and forming large crystals attached to the vein walls. These results strongly suggest that in situ microbial sulfate reduction can control the formation of secondary copper deposits. Equivalent processes could be widespread in similar deposits elsewhere, but they are probably overlooked due to the presumed low capability for fossilization of the microbes.Geological Society of AmericaConsejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]2020202020192020info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501Postprintinfo:eu-repo/semantics/acceptedVersionhttp://hdl.handle.net/10261/206071reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)Ingléshttp://dx.doi.org/10.1130/G45573.1Síinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/2060712026-05-22T06:33:51Z |
| dc.title.none.fl_str_mv |
Do microbes control the formation of giant copper deposits? |
| title |
Do microbes control the formation of giant copper deposits? |
| spellingShingle |
Do microbes control the formation of giant copper deposits? Tornos, F. Copper ores Cores Covellite electron microscopy data Europe giant deposits Iberian Peninsula Iberian pyrite belt massive deposits massive sulfide deposits metal ores microorganisms mineral deposits, genesis mineralization pyrite secondary minerals SEM data Southern Europe Spain sulfides southwestern Spain Las Cruces Deposit Bacteria |
| title_short |
Do microbes control the formation of giant copper deposits? |
| title_full |
Do microbes control the formation of giant copper deposits? |
| title_fullStr |
Do microbes control the formation of giant copper deposits? |
| title_full_unstemmed |
Do microbes control the formation of giant copper deposits? |
| title_sort |
Do microbes control the formation of giant copper deposits? |
| dc.creator.none.fl_str_mv |
Tornos, F. Oggerin, M. Ríos, Asunción de los Rodríguez, N. Amils, Ricardo Sanz, J.L. Rojas, Patricia Velasco, F. Escobar, J.M. Gómez, C. Slack, J.F. |
| author |
Tornos, F. |
| author_facet |
Tornos, F. Oggerin, M. Ríos, Asunción de los Rodríguez, N. Amils, Ricardo Sanz, J.L. Rojas, Patricia Velasco, F. Escobar, J.M. Gómez, C. Slack, J.F. |
| author_role |
author |
| author2 |
Oggerin, M. Ríos, Asunción de los Rodríguez, N. Amils, Ricardo Sanz, J.L. Rojas, Patricia Velasco, F. Escobar, J.M. Gómez, C. Slack, J.F. |
| author2_role |
author author author author author author author author author author |
| dc.contributor.none.fl_str_mv |
Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72] |
| dc.subject.none.fl_str_mv |
Copper ores Cores Covellite electron microscopy data Europe giant deposits Iberian Peninsula Iberian pyrite belt massive deposits massive sulfide deposits metal ores microorganisms mineral deposits, genesis mineralization pyrite secondary minerals SEM data Southern Europe Spain sulfides southwestern Spain Las Cruces Deposit Bacteria |
| topic |
Copper ores Cores Covellite electron microscopy data Europe giant deposits Iberian Peninsula Iberian pyrite belt massive deposits massive sulfide deposits metal ores microorganisms mineral deposits, genesis mineralization pyrite secondary minerals SEM data Southern Europe Spain sulfides southwestern Spain Las Cruces Deposit Bacteria |
| description |
[EN] The formation of secondary copper deposits, the source of more than half of the world's production, is usually interpreted as abiogenic. In this study of the Las Cruces deposit (southwestern Spain), in situ hybridization and scanning electron microscopy analysis together with integrated genomic and bioinformatic studies on cultures provide compelling evidence that a microbial community controls the current formation of the secondary copper mineralization. The cementation zone of this deposit contains abundant microbial life dominated by sulfate-reducing bacteria that coexist with methanogens and with other prokaryotes having unknown roles. Fractures in the primary massive sulfides are coated by extracellular polymeric substances in which the microbial cells are embedded. Covellite crystals have nucleated within these microbial aggregates, accreting and forming large crystals attached to the vein walls. These results strongly suggest that in situ microbial sulfate reduction can control the formation of secondary copper deposits. Equivalent processes could be widespread in similar deposits elsewhere, but they are probably overlooked due to the presumed low capability for fossilization of the microbes. |
| publishDate |
2019 |
| dc.date.none.fl_str_mv |
2019 2020 2020 2020 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article http://purl.org/coar/resource_type/c_6501 Postprint info:eu-repo/semantics/acceptedVersion |
| format |
article |
| status_str |
acceptedVersion |
| dc.identifier.none.fl_str_mv |
http://hdl.handle.net/10261/206071 |
| url |
http://hdl.handle.net/10261/206071 |
| dc.language.none.fl_str_mv |
Inglés |
| language_invalid_str_mv |
Inglés |
| dc.relation.none.fl_str_mv |
http://dx.doi.org/10.1130/G45573.1 Sí |
| dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess |
| eu_rights_str_mv |
openAccess |
| dc.publisher.none.fl_str_mv |
Geological Society of America |
| publisher.none.fl_str_mv |
Geological Society of America |
| dc.source.none.fl_str_mv |
reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC instname:Consejo Superior de Investigaciones Científicas (CSIC) |
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Consejo Superior de Investigaciones Científicas (CSIC) |
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DIGITAL.CSIC. Repositorio Institucional del CSIC |
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DIGITAL.CSIC. Repositorio Institucional del CSIC |
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1869411849809690624 |
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15,811543 |