Los ostrácodos lacustres del Mioceno terminal de Salar (Margen NO de la Cuenca de Granada, España).

Bekkali, R. ^[2] ; Nachite, D. ^[2] ; Rodriguez-Lazaro, J. ^[1] ; Martín, M. ^[1]
1. [1] Universidad del País Vasco/Euskal Herriko Unibertsitatea
  
  Universidad del País Vasco/Euskal Herriko Unibertsitatea
  
  Leioa, España
2. [2] Université Abdelamalek Essaadi, Marruecos
Localización: Geogaceta, ISSN 0213-683X, Nº. 34, 2003, págs. 91-94
Idioma: español
Títulos paralelos:
- Terminal Miocene lacustrine Ostracoda from Salar (NW edge of the Granada Basin, Spain)
Enlaces
- Texto completo (pdf)

Resumen
- Three main episodes have been distinguished in the late Turolian lacustrine deposits of Salar (Granada Basin, Spain) on the basis of the ostracod faunal assemblages. The first episode corresponds probably to a deep lacustrine (sublittoral) environment, with oligohaline and relatively cold waters. The second corresponds to a shallow (Iittoral) environment, with oligohaline to mesohaline waters, recording a chloride character. The late episode is that of a very shallow environment, partially of palustrine type, with mesohaline to polyhaline waters and strong variations of salinity.