This paper studies the Late Holocene benthic foraminifera from a continuous core extracted in the Doñana National Park (SW Spain). In this core, the foraminiferal assemblages confirm the Late Holocene lagoon (historically so-called Lacus 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 germanica 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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31 October 2020
Late Holocene Benthic Foraminifera of the Roman Lacus ligustinus (SW Spain): A Paleoenvironmental Approach
Liliana Guerra,
Cristina Veiga-Pires,
María Luz González-Regalado,
Manuel Abad,
Antonio Toscano,
Juan Manuel Muñoz,
Francisco Ruiz,
Joaquín Rodríguez Vidal,
Luis Miguel Cáceres,
Tatiana Izquierdo,
María Isabel Carretero,
Manuel Pozo,
Guadalupe Monge,
Josep Tosquella,
María Isabel Prudencio,
María Isabel Dias,
Rosa Marques,
Paula Gómez,
Verónica Romero
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Ameghiniana
Vol. 57 • No. 5
October 2020
Vol. 57 • No. 5
October 2020
Benthic foraminifera
High-energy events
Lagoon
late Holocene
SW Spain