δ13C and δ18O-based interpretation of Miocene carbonates of the Miranda-Trebiño basin, NE Iberia: preliminary insights
The stable isotopes (C and O), bulk mineralogy and sedimentary facies types of the Miocene lacustrine-palustrine carbonates of the Cucho Section (Miranda-Trebiño basin, N Iberia) are studied. The results indicate deposition in a freshwater carbonate lake recording significant biogenic CO2 input, cha...
| Autores: | , , , |
|---|---|
| Tipo de recurso: | artículo |
| Fecha de publicación: | 2024 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | inglés |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/25006 |
| Acceso en línea: | https://hdl.handle.net/10272/25006 |
| Access Level: | acceso abierto |
| Palabra clave: | Lacustrine-palustrine Carbonates δ13C δ18O Climate Hydrology Lacustre-palustre Carbonatos Clima Hidrología 2506 Geología |
| id |
ES_51bdf44dea1be143dfe6635cf1504bbd |
|---|---|
| oai_identifier_str |
oai:ariasmontano.uhu.es:10272/25006 |
| network_acronym_str |
ES |
| network_name_str |
España |
| repository_id_str |
|
| spelling |
δ13C and δ18O-based interpretation of Miocene carbonates of the Miranda-Trebiño basin, NE Iberia: preliminary insightsInterpretación basada en δ13C y δ18O de los carbonatos del Mioceno de la cuenca de Miranda-Trebiño, NE Iberia: primeros resultadosLarena, ZuriñeArenas Abad, ConcepciónMurelaga, XabierBaceta, Juan IgnacioLacustrine-palustrineCarbonatesδ13Cδ18OClimateHydrologyLacustre-palustreCarbonatosClimaHidrología2506 GeologíaThe stable isotopes (C and O), bulk mineralogy and sedimentary facies types of the Miocene lacustrine-palustrine carbonates of the Cucho Section (Miranda-Trebiño basin, N Iberia) are studied. The results indicate deposition in a freshwater carbonate lake recording significant biogenic CO2 input, changing Precipitation/Evaporation rates and variations in vegetation cover and pedogenesis on palustrine areas. Short-lived stages of higher salinity and evaporative conditions are recorded by the relative abundance of fine-grained dolomite. The highest δ13C values suggest 12C sequestration in anoxic bottom waters due to water column stratification. These new data support the general deepening trend of the lake system established from previous sedimentological analysesSociedad Geológica de España20242024-01-0120242024-01-01journal articlehttp://purl.org/coar/resource_type/c_6501VoRhttp://purl.org/coar/version/c_970fb48d4fbd8a85info:eu-repo/semantics/articleapplication/pdfhttps://hdl.handle.net/10272/25006reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelvainstname:Universidad de Huelva (UHU)Inglésengopen accesshttp://purl.org/coar/access_right/c_abf2Atribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/info:eu-repo/semantics/openAccessoai:ariasmontano.uhu.es:10272/250062026-06-02T14:58:11Z |
| dc.title.none.fl_str_mv |
δ13C and δ18O-based interpretation of Miocene carbonates of the Miranda-Trebiño basin, NE Iberia: preliminary insights Interpretación basada en δ13C y δ18O de los carbonatos del Mioceno de la cuenca de Miranda-Trebiño, NE Iberia: primeros resultados |
| title |
δ13C and δ18O-based interpretation of Miocene carbonates of the Miranda-Trebiño basin, NE Iberia: preliminary insights |
| spellingShingle |
δ13C and δ18O-based interpretation of Miocene carbonates of the Miranda-Trebiño basin, NE Iberia: preliminary insights Larena, Zuriñe Lacustrine-palustrine Carbonates δ13C δ18O Climate Hydrology Lacustre-palustre Carbonatos Clima Hidrología 2506 Geología |
| title_short |
δ13C and δ18O-based interpretation of Miocene carbonates of the Miranda-Trebiño basin, NE Iberia: preliminary insights |
| title_full |
δ13C and δ18O-based interpretation of Miocene carbonates of the Miranda-Trebiño basin, NE Iberia: preliminary insights |
| title_fullStr |
δ13C and δ18O-based interpretation of Miocene carbonates of the Miranda-Trebiño basin, NE Iberia: preliminary insights |
| title_full_unstemmed |
δ13C and δ18O-based interpretation of Miocene carbonates of the Miranda-Trebiño basin, NE Iberia: preliminary insights |
| title_sort |
δ13C and δ18O-based interpretation of Miocene carbonates of the Miranda-Trebiño basin, NE Iberia: preliminary insights |
| dc.creator.none.fl_str_mv |
Larena, Zuriñe Arenas Abad, Concepción Murelaga, Xabier Baceta, Juan Ignacio |
| author |
Larena, Zuriñe |
| author_facet |
Larena, Zuriñe Arenas Abad, Concepción Murelaga, Xabier Baceta, Juan Ignacio |
| author_role |
author |
| author2 |
Arenas Abad, Concepción Murelaga, Xabier Baceta, Juan Ignacio |
| author2_role |
author author author |
| dc.contributor.none.fl_str_mv |
|
| dc.subject.none.fl_str_mv |
Lacustrine-palustrine Carbonates δ13C δ18O Climate Hydrology Lacustre-palustre Carbonatos Clima Hidrología 2506 Geología |
| topic |
Lacustrine-palustrine Carbonates δ13C δ18O Climate Hydrology Lacustre-palustre Carbonatos Clima Hidrología 2506 Geología |
| description |
The stable isotopes (C and O), bulk mineralogy and sedimentary facies types of the Miocene lacustrine-palustrine carbonates of the Cucho Section (Miranda-Trebiño basin, N Iberia) are studied. The results indicate deposition in a freshwater carbonate lake recording significant biogenic CO2 input, changing Precipitation/Evaporation rates and variations in vegetation cover and pedogenesis on palustrine areas. Short-lived stages of higher salinity and evaporative conditions are recorded by the relative abundance of fine-grained dolomite. The highest δ13C values suggest 12C sequestration in anoxic bottom waters due to water column stratification. These new data support the general deepening trend of the lake system established from previous sedimentological analyses |
| publishDate |
2024 |
| dc.date.none.fl_str_mv |
2024 2024-01-01 2024 2024-01-01 |
| dc.type.none.fl_str_mv |
journal article http://purl.org/coar/resource_type/c_6501 VoR http://purl.org/coar/version/c_970fb48d4fbd8a85 |
| dc.type.openaire.fl_str_mv |
info:eu-repo/semantics/article |
| format |
article |
| dc.identifier.none.fl_str_mv |
https://hdl.handle.net/10272/25006 |
| url |
https://hdl.handle.net/10272/25006 |
| dc.language.none.fl_str_mv |
Inglés eng |
| language_invalid_str_mv |
Inglés |
| language |
eng |
| dc.rights.none.fl_str_mv |
open access http://purl.org/coar/access_right/c_abf2 Atribución-NoComercial-SinDerivadas 3.0 España http://creativecommons.org/licenses/by-nc-nd/3.0/es/ |
| dc.rights.openaire.fl_str_mv |
info:eu-repo/semantics/openAccess |
| rights_invalid_str_mv |
open access http://purl.org/coar/access_right/c_abf2 Atribución-NoComercial-SinDerivadas 3.0 España http://creativecommons.org/licenses/by-nc-nd/3.0/es/ |
| eu_rights_str_mv |
openAccess |
| dc.format.none.fl_str_mv |
application/pdf |
| dc.publisher.none.fl_str_mv |
Sociedad Geológica de España |
| publisher.none.fl_str_mv |
Sociedad Geológica de España |
| dc.source.none.fl_str_mv |
reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelva instname:Universidad de Huelva (UHU) |
| instname_str |
Universidad de Huelva (UHU) |
| reponame_str |
Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| collection |
Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| repository.name.fl_str_mv |
|
| repository.mail.fl_str_mv |
|
| _version_ |
1869407985680252929 |
| score |
15.811543 |