L. Guerra, Cristina Veiga-Pires, M. L. González-Regalado, M. Abad, Antonio Toscano, J. Muñoz, F. Ruiz, Joaquín Rodríguez Vidal, L. M. Cáceres, Tatiana Izquierdo, M. I. Carretero, M. Pozo, Guadalupe Monge, J. Tosquella, Paula Gómez, Verónica Romero, Marta Arroyo, Gabrlel Gómez
{"title":"El contraste micropaleontológico de la Historia: el Lacus Ligustinus romano","authors":"L. Guerra, Cristina Veiga-Pires, M. L. González-Regalado, M. Abad, Antonio Toscano, J. Muñoz, F. Ruiz, Joaquín Rodríguez Vidal, L. M. Cáceres, Tatiana Izquierdo, M. I. Carretero, M. Pozo, Guadalupe Monge, J. Tosquella, Paula Gómez, Verónica Romero, Marta Arroyo, Gabrlel Gómez","doi":"10.3989/EGEOL.43851.585","DOIUrl":null,"url":null,"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 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.","PeriodicalId":50496,"journal":{"name":"Estudios Geologicos-Madrid","volume":"23 1","pages":"131"},"PeriodicalIF":0.8000,"publicationDate":"2020-09-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Estudios Geologicos-Madrid","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.3989/EGEOL.43851.585","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOLOGY","Score":null,"Total":0}
引用次数: 0
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 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.
期刊介绍:
Since 1945 Estudios Geologicos publishes original research works, as well as reviews, about any topic on Earth Sciences.
Estudios Geologicos is published as one yearly volume, divided into two half-yearly issues. It is edited by the Spanish National Research Council (Consejo Superior de Investigaciones Científicas, CSIC) at the Instituto de Geociencias (CSIC-UCM).
Estudios Geologicos provides free access to full-text articles through this electronic edition. Accepted articles appear online as "Forthcoming articles" as soon as the galley proofs have been approved by the authors and the Editor-in-Chief. No changes can be made after online publication.