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This work is dedicated to Mrs. Isabel Munoz Calvo and Mr. Juan Antonio Garcia Rivera, in memoriam. It has been carried out through the projects Roman cities of the Baetica. CORPVS VRBIVM BAETICARVM (I) (CUB) '(Andalusian Government)' and From the Atlantic to the Tyrrhenian. The hispanic ports and their commercial relations with Ostia Antica. DEATLANTIR II -HAR2017-89154-P(Plan Nacional de I+ D+i). Other funds have come from Andalusian Government (groups HUM-132, RNM-238 and RNM-293). It is a contribution to the Research Center in Historical, Cultural and Natural Heritage (CIPHCN) of the University of Huelva. The authors want to thank two anonymous reviewers whose suggestions improved the final version of the manuscript and the editor, Dra. Alejandra Pagani, her kind help and comments during the revision process.

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LATE HOLOCENE BENTHIC FORAMINIFERA OF THE ROMAN LACUS LIGUSTINUS (SW SPAIN): A PALEOENVIRONMENTAL APPROACH

Publicado en:Ameghiniana. 57 (5): 419-432 - 2020-10-01 57(5), DOI: 10.5710/AMGH.08.05.2020.3336

Autores: Guerra, Liliana; Veiga-Pires, Cristina; Luz Gonzalez-Regalado, Maria; Abad, Manuel; Toscano, Antonio; Manuel Munoz, Juan; Ruiz, Francisco; Rodriguez Vidal, Joaquin; Miguel Caceres, Luis; Izquierdo, Tatiana; Isabel Carretero, Maria; Pozo, Manuel; Monge, Guadalupe; Tosquella, Josep; Isabel Prudencio, Maria; Isabel Dias, Maria; Marques, Rosa; Gomez, Paula; Romero, Veronica

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Resumen

This 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).

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