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The late holocene evolution of the adra delta subaqueous system (Northern Alboran Sea): seismic-stratigraphic and geomorphic evidence of millennial scale climatic and anthropic effects

dc.contributor.authorBárcenas, P.
dc.contributor.authorLobo, F.J.
dc.contributor.authorFernández-Salas, L.M.
dc.contributor.authorMendes, Isabel Maria de Paiva Pinto
dc.contributor.authorLópez-González, N.
dc.contributor.authorMacías, J.
dc.date.accessioned2024-11-29T12:11:59Z
dc.date.available2024-11-29T12:11:59Z
dc.date.issued2024-11
dc.description.abstractThe formation and development of a small Mediterranean deltaic system are investigated through a primary seismic stratigraphic interpretation of a high-resolution seismic profile network, combined with multiple bathymetric data (including multibeam bathymetric imagery) and collated with shallow sediment cores collected with a vibro-corer device. The submarine delta of the Adra River is divided into a basal patchy seismic unit and five wedge-shaped younger seismic units that are related to the Holocene highstand stabilization. Limited age control indicates that the two uppermost seismic units are very recent, most likely related to a dearth of fluvial fluxes led by channel deviations and by sediment retention. The formation of the three older seismic units is correlated to three humid periods during the Middle Holocene, Late Holocene and Little Ice Age, under a general context of progressive aridification of southeastern Iberia. The stacking patterns and spatial distribution of individual seismic units document a history of episodic progradation of successive prodeltaic lobes, with a long-term evolution mediated by climatically-induced changes in the river basin and more recent anthropogenic interventions. Overall, the subaqueous deltaic system registers the complete modification of a deltaic system that evolves from a fluvial-dominated delta to recent wave-dominated wedges. In between, the deltaic system exhibits a progressive asymmetric character, due to the instauration of Atlantic waters on the shelf and their subsequent eastward redistribution. The Adra deltaic system is proposed as an outstanding example of a small deltaic system that reacts almost immediately to the complex interaction between natural changes in the system and anthropogenic interventions in the drainage basin.eng
dc.description.sponsorshipDL57/2016/ CP1361/CT0009; CEECINST/00052/2021/CP2792/CT0012; UID/0350/2020
dc.identifier.doi10.1016/j.margeo.2024.107386
dc.identifier.issn0025-3227
dc.identifier.urihttp://hdl.handle.net/10400.1/26366
dc.language.isoeng
dc.peerreviewedyes
dc.publisherElsevier
dc.relationAquatic Research Infrastructure Network
dc.relation.ispartofMarine Geology
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/
dc.subjectMediterranean Sea
dc.subjectDeltaic system
dc.subjectStratigraphic architecture
dc.subjectClimatic cycles
dc.subjectAnthropogenic interventions
dc.titleThe late holocene evolution of the adra delta subaqueous system (Northern Alboran Sea): seismic-stratigraphic and geomorphic evidence of millennial scale climatic and anthropic effectseng
dc.typejournal article
dspace.entity.typePublication
oaire.awardTitleAquatic Research Infrastructure Network
oaire.awardURIinfo:eu-repo/grantAgreement/FCT/6817 - DCRRNI ID/LA%2FP%2F0069%2F2020/PT
oaire.citation.startPage107386
oaire.citation.titleMarine Geology
oaire.citation.volume477
oaire.fundingStream6817 - DCRRNI ID
oaire.versionhttp://purl.org/coar/version/c_970fb48d4fbd8a85
person.familyNameMendes
person.givenNameIsabel Maria de Paiva Pinto
person.identifier.ciencia-id5C15-242C-FDC0
person.identifier.orcid0000-0001-7004-7910
project.funder.identifierhttp://doi.org/10.13039/501100001871
project.funder.nameFundação para a Ciência e a Tecnologia
relation.isAuthorOfPublicationc34b90c6-5a34-472c-a658-1d2329a59936
relation.isAuthorOfPublication.latestForDiscoveryc34b90c6-5a34-472c-a658-1d2329a59936
relation.isProjectOfPublication5af011f9-3888-449a-a18c-d08b59e87091
relation.isProjectOfPublication.latestForDiscovery5af011f9-3888-449a-a18c-d08b59e87091

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