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The geological record of a mid-Holocene marine storm in southwestern Spain
Authors:Francisco Ruiz  José Borrego  Manuel Abad  Berta Carro  Joaquín Rodríguez-Vidal  Maria Isabel Prudêncio
Institution:a Departamento de Geodinámica y Paleontología, Facultad de Ciencias Experimentales, Universidad de Huelva, Avda. Fuerzas Armadas s/n, 21071 Huelva, Spain
b Departamento de Geología, Facultad de Ciencias Experimentales, Universidad de Huelva, Avda. Fuerzas Armadas s/n, 21071 Huelva, Spain
c Instituto Tecnológico e Nuclear, EN 10, 2686-953 Sacavém, Portugal
Abstract:Integrated analysis of a 50-m long sedimentary core collected in the central part of the Odiel estuary (SW Atlantic coast of Spain) allows delineation of the main paleoenvironmental changes that occurred in this area during the Holocene. Eight sedimentary facies were deposited in the last ca. 9000 years BP, confirming a transgressive-regressive cycle that involves the transition from fluvial to salt marsh deposits with intermediate marine tidal deposits. A storm event is detected at ca. 5705 14C years BP (mean calibrated age) with distinct lithostratigraphical, textural, geochemical, and palaeontological features.
Keywords:Estuarine facies  Storm  Holocene  SW Spain
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