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

  1. Bekkali, R. 1
  2. Nachite, D. 1
  3. Rodriguez-Lazaro, J. 2
  4. Martín, M. 2
  1. 1 Université Abdelamalek Essaadi, Marruecos
  2. 2 Universidad del País Vasco/Euskal Herriko Unibertsitatea
    info

    Universidad del País Vasco/Euskal Herriko Unibertsitatea

    Lejona, España

    ROR https://ror.org/000xsnr85

Revista:
Geogaceta

ISSN: 0213-683X

Año de publicación: 2003

Número: 34

Páginas: 91-94

Tipo: Artículo

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Otras publicaciones en: Geogaceta

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.

Fuente de los datos: Dialnet