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El contraste micropaleontológico de la Historia: el Lacus Ligustinus romano
Guerra, L.; Veiga-Pires, C.; González-Regalado, M.L.; Abad, M.; Toscano, T.; Muñoz, J.M.; Ruiz, R.; Rodríguez-Vidal, J.; Cáceres, L.M.; Izquierdo, T.; Carretero, M.I.; Pozo, M.; Monge, G.; Tosquella, J.; Gómez, P.; Romero, V.; Arroyo, M.; Gomez, G. (2020). El contraste micropaleontológico de la Historia: el Lacus Ligustinus romano. Estudios Geologicos-Madrid 76(2): e131. https://dx.doi.org/10.3989/egeol.43851.585
In: Estudios Geologicos-Madrid: Madrid. ISSN 0367-0449; e-ISSN 1988-3250
Peer reviewed article  
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Author keywords
    Benthic foraminifera; palaeoenvironmental reconstruction; Late Holocene; Guadalquivir estuary; S.W. Spain
Auteurs  Top 
  • Guerra, L.
  • Veiga-Pires, C.
  • González-Regalado, M.L.
  • Abad, M.
  • Toscano, T.
  • Muñoz, J.M.
  • Ruiz, R.
  • Rodríguez-Vidal, J.
  • Cáceres, L.M.
  • Izquierdo, T.
  • Carretero, M.I.
  • Pozo, M.
  • Monge, G.
  • Tosquella, J.
  • Gómez, P.
  • Romero, V.
  • Arroyo, M.
  • Gomez, G.
Abstract
    During 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 Doñana 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.
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