The micropaleontological contrast of the History: the Roman Lacus Ligustinus

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dc.contributor.authorGuerra, L
dc.contributor.authorVeiga-Pires, C
dc.contributor.authorGonzalez-Regalado, ML
dc.contributor.authorAbad de los Santos, Manuel
dc.contributor.authorToscano, A
dc.contributor.authorMunoz, JM
dc.contributor.authorRuiz, F
dc.contributor.authorVidal, JR
dc.contributor.authorCaceres, LM
dc.contributor.authorIzquierdo, Tatiana
dc.contributor.authorCarretero, MI
dc.contributor.authorPozo, M
dc.contributor.authorMonge, G
dc.contributor.authorTosquella, J
dc.contributor.authorGomez, P
dc.contributor.authorRomero, V
dc.contributor.authorArroyo, M
dc.contributor.authorGomez, G
dc.date.accessioned2025-10-20T07:37:31Z
dc.date.available2025-10-20T07:37:31Z
dc.date.issued2020-01-01
dc.date.updated2025-10-17T19:52:13Z
dc.description.abstractDuring the Roman period (3rd century BC-5th century AD), the areas located near the present-day mouth of the Guadalquivir River were occupied by a lagoon with marine connection, according to the paleoenvironmental interpretation of benthic foraminiferal assemblages obtained in a core extracted in the Donana National Park. The inner zones of this lagoon were occupied by clayey tidal flats, which suffered the effects of a storm towards the end of the 1st century A.D. The comparison with the ostracod assemblages of the same core confirms this reconstruction and the paleogeographic data provided by various chroniclers, although these microcrustaceans better record the paleoenvironmental changes in these coastal sectors.
dc.formatapplication/pdf
dc.identifier.citationGuerra, Liliana; Veiga-Pires, Cristina; Luz Gonzalez-Regalado, Maria; Abad, Manuel; Toscano, Antonio; Manuel Munoz, Juan; Ruiz, Francisco; Rodriguez V (2020). The micropaleontological contrast of the History: the Roman Lacus Ligustinus. Estudios Geologicos-Madrid, 76(2), e131-. DOI: 10.3989/egeol.43851.585
dc.identifier.doihttps://doi.org/10.3989/egeol.43851.585
dc.identifier.issn0367-0449
dc.identifier.urihttps://hdl.handle.net/10115/107717
dc.language.isoen
dc.relation.isformatofhttps://doi.org/10.3989/egeol.43851.585
dc.relation.ispartofEstudios Geologicos-Madrid, 2020, 76, 2, e131
dc.rightsOpenAccess
dc.rightsAttribution-NonCommercial 4.0 Internationalen
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess
dc.rights.urihttp://creativecommons.org/licenses/by-nc/4.0/
dc.sourceGuerra, Liliana; Veiga-Pires, Cristina; Luz Gonzalez-Regalado, Maria; Abad, Manuel; Toscano, Antonio; Manuel Munoz, Juan; Ruiz, Francisco; Rodriguez V (2020). The micropaleontological contrast of the History: the Roman Lacus Ligustinus. Estudios Geologicos-Madrid, 76(2), e131-. DOI: 10.3989/egeol.43851.585
dc.subjectBiodiversidade
dc.subjectCiências ambientais
dc.subjectGeociências
dc.subjectGeology
dc.subjectAndalucia
dc.subjectAtlantic coast
dc.subjectBenthic foraminifera
dc.subjectBenthic foraminiferal assemblages
dc.subjectBiostratigraphy
dc.subjectCrassostrea-angulata
dc.subjectDonana national park
dc.subjectEstuary
dc.subjectEvolution
dc.subjectForaminifera
dc.subjectGuadalquivir estuary
dc.subjectGuadalquivir river
dc.subjectHistorical perspective
dc.subjectLagoon
dc.subjectLate holocene
dc.subjectMicropaleontology
dc.subjectOstracod
dc.subjectOstracoda
dc.subjectPalaeoenvironmental reconstruction
dc.subjectPaleobiogeography
dc.subjectPark sw spain
dc.subjectRecord
dc.subjectRestricted environmental-conditions
dc.subjectRoman era
dc.subjectS.w. spain
dc.subjectSea
dc.subjectSpain
dc.subjectSw spain
dc.subjectTidal flat
dc.titleThe micropaleontological contrast of the History: the Roman Lacus Ligustinus
dc.typeinfo:eu-repo/semantics/article

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