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Título: | Late Holocene evolution of the southwestern Doñana National Park (Guadalquivir Estuary, SW Spain): a multivariate approach |
Autor: | Ruiz Muñoz, F.; Clemente Salas, Luis CSIC; Yáñez, C.; Abad de los Santos, M. | Palabras clave: | Geomorphology Mineralogy Paleontology Estuarine evolution Late Holocene SW Spain |
Fecha de publicación: | feb-2004 | Editor: | Elsevier | Citación: | Palaeogeography, Palaeoclimatology, Palaeoecology 204(1-2): 47-64 (2004) | Resumen: | Four phases are distinguished in the Late Holocene evolution of the southwestern Doñana National Park (SW Spain), based on a multidisciplinary analysis of the sediments present in drill cores. In the oldest phase (>2400–2500 cal. yr BP), a coastal lagoon (the Roman Lacus Ligustinus) was recognized in the central part of this area, partly closed by the Doñana spit and limited by fluvial levees. The following phase (∼2400–2200 cal. yr BP) is characterized by high-energy events, which caused the breakthrough of the Doñana spit and the creation of new littoral strands in the inner areas. In the third phase (∼2200–2050 cal. yr BP), this new outlet was closed, coinciding with the progradation of the Doñana spit. The last phase (∼2050 cal. yr BP–Recent) comprises three periods: (a) an unstable period (∼2050–1950 cal. yr BP), with the deposit of cheniers over the previous levees; (b) an infilling period, with a diminution of the marine influence; and (c) the appearance of temporary ponds between the emerged levees and cheniers. | Descripción: | 18 pages, 7 figures, 1 table, 67 references.-- Ruiz Muñoz et al.-- | Versión del editor: | http://dx.doi.org/10.1016/S0031-0182(03)00721-1 | URI: | http://hdl.handle.net/10261/48425 | DOI: | 10.1016/S0031-0182(03)00721-1 | ISSN: | 0031-0182 |
Aparece en las colecciones: | (IRNAS) Artículos |
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Late Holocene evolution.pdf | 1,95 MB | Adobe PDF | Visualizar/Abrir |
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