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Chronology of Coastal Alluvial Deposits in The Ria de Coruña (NW Spain) Linked to the Upper Pleistocene Sea Level Regression
dc.contributor.author | Arce-Chamorro, Carlos | |
dc.contributor.author | Sanjurjo-Sánchez, Jorge | |
dc.contributor.author | Vidal Romaní, Juan Ramón | |
dc.date.accessioned | 2023-01-12T16:04:52Z | |
dc.date.available | 2023-01-12T16:04:52Z | |
dc.date.issued | 2022-10-04 | |
dc.identifier.citation | Arce-Chamorro, C.; Sanjurjo-Sánchez, J.; Vidal-Romaní, J.R. Chronology of Coastal Alluvial Deposits in The Ria de Coruña (NW Spain) Linked to the Upper Pleistocene Sea Level Regression. Appl. Sci. 2022, 12, 9982. https://doi.org/10.3390/app12199982 | es_ES |
dc.identifier.issn | 2076-3417 | |
dc.identifier.uri | http://hdl.handle.net/2183/32337 | |
dc.description | This article belongs to the Special Issue Novel Approaches for Exploring Geological Processes on Both Earth and Planetary | es_ES |
dc.description.abstract | [Abstract] The Ria de Coruña (NW Spain) is a wide estuary recently formed by the flooding of the Mero fluvial valley lowlands during the last postglacial transgression. During the last glacial episode, with the sea level located more than 100 m below the current one, the final section of the Mero river and lateral tributaries contributed numerous deposits that the postglacial rise in sea level has partially flooded. Until now, the presence of these alluvial deposits disconnected from the main network by the Holocene marine transgression had been misinterpreted, especially for lack of an absolute chronology that would place them in an adequate paleoclimatic context. For the first time, a deposition age was assessed in this work by optically stimulated luminescence (OSL) dating back from 128 ka to 51 ka. | es_ES |
dc.description.sponsorship | This research was funded and supported by Consellería de Cultura, Educación y Ordenación Universitaria, Xunta de Galicia (programmes ED431B 2018/47 and ED431B 2021/17) through the Grupo Interdisciplinar de Patrimonio Cultural e Xeolóxico (CULXEO) | es_ES |
dc.description.sponsorship | Xunta de Galicia; ED431B 2018/47 | es_ES |
dc.description.sponsorship | Xunta de Galicia; ED431B 2021/17 | es_ES |
dc.language.iso | eng | es_ES |
dc.publisher | MDPI | es_ES |
dc.relation.uri | https://doi.org/10.3390/app12199982 | es_ES |
dc.rights | Atribución 4.0 Internacional | es_ES |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/ | * |
dc.subject | Coastal fluvial sediments | es_ES |
dc.subject | Glacioeustasy | es_ES |
dc.subject | Optically stimulated luminescence | es_ES |
dc.subject | UpperPleistocene | es_ES |
dc.subject | Ria de Coruña (NW Spain) | es_ES |
dc.title | Chronology of Coastal Alluvial Deposits in The Ria de Coruña (NW Spain) Linked to the Upper Pleistocene Sea Level Regression | es_ES |
dc.type | info:eu-repo/semantics/article | es_ES |
dc.rights.access | info:eu-repo/semantics/openAccess | es_ES |
UDC.journalTitle | Applied Sciences | es_ES |
UDC.volume | 12 | es_ES |
UDC.issue | 19 | es_ES |
UDC.startPage | 9982 | es_ES |
dc.identifier.doi | 10.3390/app12199982 |
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