@article{10272/23598,
year = {2020},
url = {https://hdl.handle.net/10272/23598},
abstract = {The Doñana National Park is a Biosphere Reserve located within
the estuary of the Guadalquivir River (SW Spain). It is mainly composed of extensive fluvio-tidal marshes partially protected by an
elongated sandy spit. Three phases have been distinguished in the
late Holocene evolution of this spit based on textural, geochemical,
palaeontological and, chronological data recorded in a long core (31
m). Phase 1 (890 BCE-218 BCE) is characterized by the alternation
of lagoonal silty sediments and slightly polluted marsh deposits, the
latter with contamination from thousand-year-old mining. Phase
2 (218 BCE-90 CE) is characterized by several historical tsunamis,
which caused the erosion of previous dune systems and the deposit
of these sandy sediments on the adjacent bottom of the lagoon. Phase
3 (90 CE-Present) includes a regressive sequence (lagoonal bottommarsh-dune system), with the pollution of lagoonal sediments due
to Roman mining activities},
abstract = {El Parque Nacional de Doñana es una Reserva de la Biosfera localizada dentro del estuario del río Guadalquivir (S.O. de España). Esta Reserva
está formada principalmente por marismas fluvio-mareales parcialmente
protegidas por una flecha arenosa alargada. Se han diferenciado tres fases
en la evolución holocena tardía de esta flecha, con base en el análisis
multidisciplinar (textura, geoquímica, paleontologíca, cronología) de un
testigo largo (31 m). La fase 1 (890 BCE-218 BCE) se caracteriza por la
alternancia de sedimentos lagunares limosos y depósitos de marisma levemente contaminados por metales pesados debido a una actividad minera
milenaria. La fase 2 (218 BCE-90 CE) se distingue por la acción de varios
tsunamis históricos, que causaron la erosión de sistemas dunares previos,
así como el depósito de estos sedimentos arenosos sobre el fondo arcilloso
de la laguna adyacente. La fase 3 (90 CE-actual) incluye una secuencia
regresiva (laguna-marisma-sistema dunar) con una nueva contaminación
de los sedimentos lagunares debido a las actividades mineras romanas},
organization = {This work has been carried out through the following projects:
a) DGYCIT project CTM2006-06722/MAR; b) DGYCIT project
CGL2006-01412; c) ´Roman cities of the Baetica. CORPVS VRBIVM
BAETICARVM (I) (CUB)´ (Andalusian Gouvernement); and d) ´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 Centro de Investigación en Patrimonio Histórico,
Cultural y Natural (CIPHCN) of the Universidad de Huelva},
publisher = {Universidad Nacional Autónoma de Mexico},
title = {Imprints of historical pollution and the 218-60 BCE tsunamigenic period in southwestern Spain},
doi = {10.22201/cgeo.20072902e.2020.1.1543},
author = {González-Regalado Montero, María Luz and Rodríguez Vidal, Joaquín and Cáceres Puro, Luis Miguel and Campos Carrasco, Juan Manuel and Bermejo Meléndez, Javier and Tosquella Angrill, Josep and Gómez Gutiérrez, Paula and Toscano Grande, Antonio and Romero Aguilar, Verónica and Ruiz Muñoz, Francisco},
}