Selenium isotope evidence for pulsed flow of oxidative slab fluids
Isotope systematics of the redox sensitive and chalcophile element selenium (Se) were investigated on exhumed parts of subducted oceanic lithosphere to provide new constraints on slab dehydration conditions during subduction. The samples show increasing δ82/76SeNIST3149 with higher abundances of flu...
| Autores: | , , , , , , |
|---|---|
| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2021 |
| País: | España |
| Institución: | Consejo Superior de Investigaciones Científicas (CSIC) |
| Repositorio: | DIGITAL.CSIC. Repositorio Institucional del CSIC |
| OAI Identifier: | oai:digital.csic.es:10261/413854 |
| Acceso en línea: | http://hdl.handle.net/10261/413854 https://doi.org/10.7185/geochemlet.2110 |
| Access Level: | acceso abierto |
| Palabra clave: | Selenium isotopes Sulfur Sulfides Recycling Subduction Redox Slab fluids |
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Selenium isotope evidence for pulsed flow of oxidative slab fluidsKönig, StephanRosca, CarolinaKurzawa. T.Varas-Reus, M.I.Dragovic, B.Schoenberg, R.John, T.Selenium isotopesSulfurSulfidesRecyclingSubductionRedoxSlab fluidsIsotope systematics of the redox sensitive and chalcophile element selenium (Se) were investigated on exhumed parts of subducted oceanic lithosphere to provide new constraints on slab dehydration conditions during subduction. The samples show increasing δ82/76SeNIST3149 with higher abundances of fluid mobile elements, comprising a larger range (−1.89 to þ0.48 %) than that of mantle (−0.13 ± 0.12 %) and altered ocean crust (−0.35 to −0.07 %). Our data point to pronounced, local scale redox variations within the subducting crust, wherein oxidative fluids dissolve sulfides and mobilise oxidised Se species. Subsequently recrystallising sulfides preferentially incorporate isotopically lighter, reduced Se, which shifts evolving fluids and late stage sulfides to higher δ82/76SeNIST3149. Redistribution of Se by repeated cycles of sulfide reworking within the subducted crust can be reconciled with episodes of oxidised fluid pulses from underlying slab mantle in modern subduction zones.SK acknowledges ERC Starting Grant O2RIGIN (636808).Peer reviewedEuropean Association of GeochemistryEuropean Research CouncilEuropean CommissionConsejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]202620262021info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501Publisher's versioninfo:eu-repo/semantics/publishedVersionhttp://hdl.handle.net/10261/413854https://doi.org/10.7185/geochemlet.2110reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)Inglés#PLACEHOLDER_PARENT_METADATA_VALUE#info:eu-repo/grantAgreement/EC/H2020/636808https://doi.org/10.7185/geochemlet.2110Síinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/4138542026-05-22T06:33:51Z |
| dc.title.none.fl_str_mv |
Selenium isotope evidence for pulsed flow of oxidative slab fluids |
| title |
Selenium isotope evidence for pulsed flow of oxidative slab fluids |
| spellingShingle |
Selenium isotope evidence for pulsed flow of oxidative slab fluids König, Stephan Selenium isotopes Sulfur Sulfides Recycling Subduction Redox Slab fluids |
| title_short |
Selenium isotope evidence for pulsed flow of oxidative slab fluids |
| title_full |
Selenium isotope evidence for pulsed flow of oxidative slab fluids |
| title_fullStr |
Selenium isotope evidence for pulsed flow of oxidative slab fluids |
| title_full_unstemmed |
Selenium isotope evidence for pulsed flow of oxidative slab fluids |
| title_sort |
Selenium isotope evidence for pulsed flow of oxidative slab fluids |
| dc.creator.none.fl_str_mv |
König, Stephan Rosca, Carolina Kurzawa. T. Varas-Reus, M.I. Dragovic, B. Schoenberg, R. John, T. |
| author |
König, Stephan |
| author_facet |
König, Stephan Rosca, Carolina Kurzawa. T. Varas-Reus, M.I. Dragovic, B. Schoenberg, R. John, T. |
| author_role |
author |
| author2 |
Rosca, Carolina Kurzawa. T. Varas-Reus, M.I. Dragovic, B. Schoenberg, R. John, T. |
| author2_role |
author author author author author author |
| dc.contributor.none.fl_str_mv |
European Research Council European Commission Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72] |
| dc.subject.none.fl_str_mv |
Selenium isotopes Sulfur Sulfides Recycling Subduction Redox Slab fluids |
| topic |
Selenium isotopes Sulfur Sulfides Recycling Subduction Redox Slab fluids |
| description |
Isotope systematics of the redox sensitive and chalcophile element selenium (Se) were investigated on exhumed parts of subducted oceanic lithosphere to provide new constraints on slab dehydration conditions during subduction. The samples show increasing δ82/76SeNIST3149 with higher abundances of fluid mobile elements, comprising a larger range (−1.89 to þ0.48 %) than that of mantle (−0.13 ± 0.12 %) and altered ocean crust (−0.35 to −0.07 %). Our data point to pronounced, local scale redox variations within the subducting crust, wherein oxidative fluids dissolve sulfides and mobilise oxidised Se species. Subsequently recrystallising sulfides preferentially incorporate isotopically lighter, reduced Se, which shifts evolving fluids and late stage sulfides to higher δ82/76SeNIST3149. Redistribution of Se by repeated cycles of sulfide reworking within the subducted crust can be reconciled with episodes of oxidised fluid pulses from underlying slab mantle in modern subduction zones. |
| publishDate |
2021 |
| dc.date.none.fl_str_mv |
2021 2026 2026 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article http://purl.org/coar/resource_type/c_6501 Publisher's version info:eu-repo/semantics/publishedVersion |
| format |
article |
| status_str |
publishedVersion |
| dc.identifier.none.fl_str_mv |
http://hdl.handle.net/10261/413854 https://doi.org/10.7185/geochemlet.2110 |
| url |
http://hdl.handle.net/10261/413854 https://doi.org/10.7185/geochemlet.2110 |
| dc.language.none.fl_str_mv |
Inglés |
| language_invalid_str_mv |
Inglés |
| dc.relation.none.fl_str_mv |
#PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/EC/H2020/636808 https://doi.org/10.7185/geochemlet.2110 Sí |
| dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess |
| eu_rights_str_mv |
openAccess |
| dc.publisher.none.fl_str_mv |
European Association of Geochemistry |
| publisher.none.fl_str_mv |
European Association of Geochemistry |
| 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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1869410112021463040 |
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15,81155 |