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Late holocene benthic Foraminifera of the Roman Lacus ligustinus (SW Spain): a paleoenvironmental approach

2020Journal article Restricted access
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dc.contributor.authorGuerra, Liliana
dc.contributor.authorVeiga-Pires, Cristina
dc.contributor.authorLuz Gonzalez Regalado, M. L.
dc.contributor.authorAbad, M.
dc.contributor.authorToscano, A.
dc.contributor.authorManuel Munoz, J. M.
dc.contributor.authorRuiz, F.
dc.contributor.authorVidal, J. R.
dc.contributor.authorCaceres, L. M.
dc.contributor.authorIzquierdo, T.
dc.contributor.authorCarretero, M. I.
dc.contributor.authorPozo, M.
dc.contributor.authorMonge, G.
dc.contributor.authorTosquella, J.
dc.contributor.authorPrudencio, M. I.
dc.contributor.authorDias, M.I.
dc.contributor.authorMarques, R.
dc.contributor.authorGomez, P.
dc.contributor.authorRomero, V.
dc.date.accessioned2021-07-28T11:37:54Z
dc.date.available2021-07-28T11:37:54Z
dc.date.issued2020
dc.date.updated2021-07-27T21:35:26Z
dc.description.abstractThis paper studies the Late Holocene benthic foraminifera from a continuous core extracted in the Doliana National Park (SW Spain). In this core, the foraminiferal assemblages confirm the Late Holocene lagoon (historically so-called Locus Ligustinus) during the Roman period, about 2000 years ago. The more open, deepest areas of this lagoon were dominated by Ammonia tepida and Elphidium spp., while Haynesina germanise was the most representative species of the shallow, more restricted zones. The vertical variations of these assemblages, together with associated sedimentological and macrofaunal changes, allow recognizing three high-energy events (HEE) between 500 BCE and 500 CE, which also left an extensive sedimentary record in nearby coastal areas: two tsunamis (HEE-1 and HEE-3) and a storminess period (HEE-2).pt_PT
dc.description.sponsorshipDEATLANTIR II - HAR2017-89154-P- (Plan Nacional de I+D+i); Groups HUM-132, RNM-238 and RNM-293pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.authenticusidP-00T-2Q5
dc.identifier.doi10.5710/amgh.08.05.2020.3336pt_PT
dc.identifier.eid2-s2.0-85096384369
dc.identifier.issn0002-7014
dc.identifier.slugcv-prod-2516541
dc.identifier.urihttp://hdl.handle.net/10400.1/16827
dc.identifier.wosWOS:000592805800002
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.subjectBenthic foraminiferapt_PT
dc.subjectLagoonpt_PT
dc.subjectHigh-energy eventspt_PT
dc.subjectLate Holocenept_PT
dc.subjectSW Spainpt_PT
dc.titleLate holocene benthic Foraminifera of the Roman Lacus ligustinus (SW Spain): a paleoenvironmental approachpt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.citation.endPage432pt_PT
oaire.citation.startPage419pt_PT
oaire.citation.titleAMEGHINIANApt_PT
oaire.citation.volume57pt_PT
person.familyNameGuerra
person.familyNameVeiga-Pires
person.givenNameLiliana
person.givenNameCristina
person.identifier113325
person.identifier.ciencia-idBB1D-6ED9-88E0
person.identifier.ciencia-id4A1F-CEDA-E66C
person.identifier.orcid0000-0003-1645-3939
person.identifier.orcid0000-0002-9323-0723
person.identifier.ridB-5144-2008
person.identifier.scopus-author-id7801372905
rcaap.cv.cienciaid4A1F-CEDA-E66C | Cristina Veiga Pires
rcaap.rightsrestrictedAccesspt_PT
rcaap.typearticlept_PT
relation.isAuthorOfPublicationb9b4de81-6807-43bb-9534-5206204b25db
relation.isAuthorOfPublicationd1541efa-0eaa-48dc-aea3-a1e64aa0065a
relation.isAuthorOfPublication.latestForDiscoveryd1541efa-0eaa-48dc-aea3-a1e64aa0065a

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