Imprints of historical pollution and the 218-60 BCE tsunamigenic period in southwestern Spain
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 b...
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Universidad Nacional Autónoma de México
2020-03-01
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| Series: | Revista Mexicana de Ciencias Geológicas |
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| Online Access: | https://rmcg.unam.mx/index.php/rmcg/article/view/1543 |
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| author | María Luz González-Regalado Guadalupe Monge María Isabel Carretero Manuel Pozo Joaquín Rodríguez-Vidal Luis Miguel Cáceres Manuel Abad Juan Manuel Campos Javier Bermejo Josep Tosquella Tatiana Izquierdo Maria Isabel Prudêncio Maria Isabel Dias Rosa Marques Paula Gómez Antonio Toscano Verónica Romero Francisco Ruiz |
| author_facet | María Luz González-Regalado Guadalupe Monge María Isabel Carretero Manuel Pozo Joaquín Rodríguez-Vidal Luis Miguel Cáceres Manuel Abad Juan Manuel Campos Javier Bermejo Josep Tosquella Tatiana Izquierdo Maria Isabel Prudêncio Maria Isabel Dias Rosa Marques Paula Gómez Antonio Toscano Verónica Romero Francisco Ruiz |
| author_sort | María Luz González-Regalado |
| collection | DOAJ |
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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 bottom-marsh-dune system), with the pollution of lagoonal sediments due to Roman mining activities.
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| format | Article |
| id | doaj-art-00f22c9486404103ab1031afeeefffbd |
| institution | OA Journals |
| issn | 1026-8774 2007-2902 |
| language | English |
| publishDate | 2020-03-01 |
| publisher | Universidad Nacional Autónoma de México |
| record_format | Article |
| series | Revista Mexicana de Ciencias Geológicas |
| spelling | doaj-art-00f22c9486404103ab1031afeeefffbd2025-08-20T02:32:42ZengUniversidad Nacional Autónoma de MéxicoRevista Mexicana de Ciencias Geológicas1026-87742007-29022020-03-0137110.22201/cgeo.20072902e.2020.1.1543Imprints of historical pollution and the 218-60 BCE tsunamigenic period in southwestern SpainMaría Luz González-Regalado0Guadalupe Monge1María Isabel Carretero2Manuel Pozo3Joaquín Rodríguez-Vidal4Luis Miguel Cáceres5Manuel Abad6Juan Manuel Campos7Javier Bermejo8Josep Tosquella9Tatiana Izquierdo10Maria Isabel Prudêncio11Maria Isabel Dias12Rosa Marques13Paula Gómez14Antonio Toscano15Verónica Romero16Francisco Ruiz17Departamento de Ciencias de la Tierra, Universidad de Huelva, Avda. Tres de Marzo, s/n, 21071-Huelva, Spain. Centro de Investigación en Patrimonio Histórico, Cultural y Natural (CIPHCN), Universidad de Huelva, Facultad de Humanidades, Avda. Tres de Marzo s/n, 21071 Huelva, Spain.– Centro de Investigación en Patrimonio Histórico, Cultural y Natural (CIPHCN), Universidad de Huelva, Facultad de Humanidades, Av. Tres de Marzo s/n, 21071 Huelva, Spain.Departamento de Cristalografía, Mineralogía y Química Agrícola, Universidad de Sevilla, C/ Profesor García González 1, 41012-Sevilla, Spain.Departamento de Cristalografía, Mineralogía y Química Agrícola, Universidad de Sevilla, C/ Profesor García González 1, 41012-Sevilla, Spain.Departamento de Geología y Geoquímica, Universidad Autónoma de Madrid, Avda. Francisco Tomás y Valiente 7, 28049-Madrid, Spain.Departamento de Ciencias de la Tierra, Universidad de Huelva, Av. Tres de Marzo, s/n, 21071-Huelva, Spain. – Centro de Investigación en Patrimonio Histórico, Cultural y Natural (CIPHCN), Universidad de Huelva, Facultad de Humanidades, Av. Tres de Marzo s/n, 21071 Huelva, Spain.Departamento de Ciencias de la Tierra, Universidad de Huelva, Av. Tres de Marzo, s/n, 21071-Huelva, Spain. – Centro de Investigación en Patrimonio Histórico, Cultural y Natural (CIPHCN), Universidad de Huelva, Facultad de Humanidades, Av. Tres de Marzo s/n, 21071 Huelva, Spain.Departamento de Biología y Geología, Física y Química Inorgánica, ESCET, Universidad Rey Juan Carlos, Calle Tulipán s/n, 28933 – Móstoles, Spain.Departamento de Historia, Geografía y Antropología, Universidad de Huelva, Av. Tres de Marzo s/n, 21071-Huelva, Spain. – Centro de Investigación en Patrimonio Histórico, Cultural y Natural (CIPHCN), Universidad de Huelva, Facultad de Humanidades, Av. Tres de Marzo s/n, 21071 Huelva, Spain.Departamento de Historia, Geografía y Antropología, Universidad de Huelva, Av. Tres de Marzo s/n, 21071-Huelva, Spain. – Centro de Investigación en Patrimonio Histórico, Cultural y Natural (CIPHCN), Universidad de Huelva, Facultad de Humanidades, Avda. Tres de Marzo s/n, 21071 Huelva, Spain.Departamento de Ciencias de la Tierra, Universidad de Huelva, Av. Tres de Marzo, s/n, 21071-Huelva, Spain. – Centro de Investigación en Patrimonio Histórico, Cultural y Natural (CIPHCN), Universidad de Huelva, Facultad de Humanidades, Av. Tres de Marzo s/n, 21071 Huelva, Spain.Instituto de Investigaciones Científicas y Tecnológicas de la Universidad de Atacama, IDICTEC-UDA. Av. Copayapu, 485. Copiapó, Chile.Centro de Ciências e Tecnologias Nucleares (C2TN), Instituto Superior Técnico, Universidade de Lisboa, Estrada Nacional 10 (k 139.7), 2695-066-Bobadela LRS, Portugal.Centro de Ciências e Tecnologias Nucleares (C2TN), Instituto Superior Técnico, Universidade de Lisboa, Estrada Nacional 10 (k 139.7), 2695-066-Bobadela LRS, Portugal.Centro de Ciências e Tecnologias Nucleares (C2TN), Instituto Superior Técnico, Universidade de Lisboa, Estrada Nacional 10 (k 139.7), 2695-066-Bobadela LRS, Portugal.Departamento de Ciencias de la Tierra, Universidad de Huelva, Av. Tres de Marzo, s/n, 21071-Huelva, Spain. – Centro de Investigación en Patrimonio Histórico, Cultural y Natural (CIPHCN), Universidad de Huelva, Facultad de Humanidades, Av. Tres de Marzo s/n, 21071 Huelva, Spain.Departamento de Ciencias de la Tierra, Universidad de Huelva, Av. Tres de Marzo, s/n, 21071-Huelva, Spain. – Centro de Investigación en Patrimonio Histórico, Cultural y Natural (CIPHCN), Universidad de Huelva, Facultad de Humanidades, Av. Tres de Marzo s/n, 21071 Huelva, Spain.Departamento de Ciencias de la Tierra, Universidad de Huelva, Av. Tres de Marzo, s/n, 21071-Huelva, Spain. – Centro de Investigación en Patrimonio Histórico, Cultural y Natural (CIPHCN), Universidad de Huelva, Facultad de Humanidades, Av. Tres de Marzo s/n, 21071 Huelva, Spain.Departamento de Ciencias de la Tierra, Universidad de Huelva, Av. Tres de Marzo, s/n, 21071-Huelva, Spain. – Centro de Investigación en Patrimonio Histórico, Cultural y Natural (CIPHCN), Universidad de Huelva, Facultad de Humanidades, Av. Tres de Marzo s/n, 21071 Huelva, Spain. – Centro de Ciências e Tecnologias Nucleares (C2TN), Instituto Superior Técnico, Universidade de Lisboa, Estrada Nacional 10 (k 139.7), 2695-066-Bobadela LRS, Portugal. 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 bottom-marsh-dune system), with the pollution of lagoonal sediments due to Roman mining activities. https://rmcg.unam.mx/index.php/rmcg/article/view/1543textureheavy metalsPalaeontologyhistorical tsunamisminingDoñana |
| spellingShingle | María Luz González-Regalado Guadalupe Monge María Isabel Carretero Manuel Pozo Joaquín Rodríguez-Vidal Luis Miguel Cáceres Manuel Abad Juan Manuel Campos Javier Bermejo Josep Tosquella Tatiana Izquierdo Maria Isabel Prudêncio Maria Isabel Dias Rosa Marques Paula Gómez Antonio Toscano Verónica Romero Francisco Ruiz Imprints of historical pollution and the 218-60 BCE tsunamigenic period in southwestern Spain Revista Mexicana de Ciencias Geológicas texture heavy metals Palaeontology historical tsunamis mining Doñana |
| title | Imprints of historical pollution and the 218-60 BCE tsunamigenic period in southwestern Spain |
| title_full | Imprints of historical pollution and the 218-60 BCE tsunamigenic period in southwestern Spain |
| title_fullStr | Imprints of historical pollution and the 218-60 BCE tsunamigenic period in southwestern Spain |
| title_full_unstemmed | Imprints of historical pollution and the 218-60 BCE tsunamigenic period in southwestern Spain |
| title_short | Imprints of historical pollution and the 218-60 BCE tsunamigenic period in southwestern Spain |
| title_sort | imprints of historical pollution and the 218 60 bce tsunamigenic period in southwestern spain |
| topic | texture heavy metals Palaeontology historical tsunamis mining Doñana |
| url | https://rmcg.unam.mx/index.php/rmcg/article/view/1543 |
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