Asociaciones de Ostrácodos Bentónicos actuales y del Holoceno del Estuario de Bahía Blanca (Buenos Aires, Argentina): Interpretaciones Paleoambientales
The study of ostracod fauna in sediment samples from present environments at the Bahía Blanca estuary led to the identification of different ostracod associations, through which it was possible to identify Holocene depositional environments. Based on the systematic analysis of the ostracods present...
| Autores: | , , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2016 |
| País: | Argentina |
| Institución: | Consejo Nacional de Investigaciones Científicas y Técnicas |
| Repositorio: | CONICET Digital (CONICET) |
| Idioma: | español |
| OAI Identifier: | oai:ri.conicet.gov.ar:11336/44285 |
| Acceso en línea: | http://hdl.handle.net/11336/44285 |
| Access Level: | acceso abierto |
| Palabra clave: | ARGENTINA BAHÍA BLANCA ESTUARY PALEOENVIRONMENTS OSTRACODS https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
| Sumario: | The study of ostracod fauna in sediment samples from present environments at the Bahía Blanca estuary led to the identification of different ostracod associations, through which it was possible to identify Holocene depositional environments. Based on the systematic analysis of the ostracods present in different core levels, a total of 11 genera represented by 13 species of benthic ostracods were identified, out of which Neocytherideis ruidis, Loxocythere variasculpta and Callistocythere litoralensis were dominant along the core. The quantitative and qualitative analysis of ostracods from the Holocene allowed us to determine the following palaeoenvironments: at the base of the core the sediments were deposited in an intertidal environment with developed mudflats; the middle sector evidenced an increase in environmental energy; and the upper portion of the core contained deposits of marshes environment with greater freshwater input. The detailed study of the benthic Ostracoda allowed to identify palaeoenvironments and to provide new evidence of negative fluctuations of the mean sea level for the Holocene. |
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