El contraste micropaleontológico de la Historiael Lacus Ligustinus romano

  1. Guerra, Liliana 1
  2. Veiga-Pires, Cristina 1
  3. González-Regalado, María Luz 2
  4. Abad, Manuel 3
  5. Toscano, Antonio 2
  6. Muñoz, Juan Manuel 4
  7. Ruiz, Francisco 2
  8. Rodríguez Vidal, Joaquín 2
  9. Izquierdo, Tatiana 5
  10. Carretero, María Isabel 4
  11. Pozo, Manuel 6
  12. Monge, Guadalupe 4
  13. Tosquella, Josep 2
  14. Gómez, Paula 2
  15. Romero, Verónica 2
  16. Arroyo, Marta 2
  17. Gómez, Gabrlel 2
  1. 1 Universidad do Algarve, Portugal
  2. 2 Universidad de Huelva, España
  3. 3 Universidad Rey Juan Carlos, España
  4. 4 Universidad de Sevilla, España
  5. 5 Universidad de Atacama, Chile
  6. 6 Universidad Autónoma de Madrid, España
Journal:
Estudios geológicos

ISSN: 0367-0449

Year of publication: 2020

Volume: 76

Issue: 2

Type: Article

DOI: 10.3989/EGEOL.43851.585 DIALNET GOOGLE SCHOLAR lock_openOpen access editor

More publications in: Estudios geológicos

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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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