Los ostrácodos lacustres del Mioceno terminal de Salar (Margen NO de la Cuenca de Granada, España)
Three main episodes have been distinguished in the late Turolian lacustrine deposits of Salar (Granada Basin, Spain) on the basis of the ostracod faunaI assemblages. The first episode corresponds probably to a deep lacustrine (sublittoral) environment, with oligohaline and relatively cold waters. Th...
| Autores: | , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 2003 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/9060 |
| Acceso en línea: | http://hdl.handle.net/10272/9060 |
| Access Level: | acceso abierto |
| Palabra clave: | Ostracods Palaeoecology Late Turolian Salar Granada Basin Spain |
| Sumario: | Three main episodes have been distinguished in the late Turolian lacustrine deposits of Salar (Granada Basin, Spain) on the basis of the ostracod faunaI assemblages. The first episode corresponds probably to a deep lacustrine (sublittoral) environment, with oligohaline and relatively cold waters. The second corresponds to a shallow (littoral) environment, with oligohaline to mesohaline waters, recording a chloride character. The late episode is that of a very shallow environment, partially of palustrlne type, with mesohaline to polyhaline waters and strong variations of salinity |
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