Los ostrácodos lacustres del Plioceno superior de la Cuenca de Saïss (Norte de Marruecos)Principales características paleoambientales.

  1. Nachite, D. 1
  2. Bekkali, R. 1
  3. Rodríguez-Lazaro, J. 2
  4. Martín-Rubio, 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

Aldizkaria:
Geogaceta

ISSN: 0213-683X

Argitalpen urtea: 2003

Zenbakia: 34

Orrialdeak: 95-98

Mota: Artikulua

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Beste argitalpen batzuk: Geogaceta

Laburpena

Three main environment types have been distinguished in the Upper Pliocene deposits of Saiss Basin (N of Morocco) on the basis of the ostracod faunal assemblages. Fluvio-Iacustrine in the northern edge, with oligohaline to mesohaline NaCl-dominant water. Lacustrine to palustrine at the top, in the central area of the basin and palustrine to the western, with oligohaline bicarbonate-rich water.

Datuen iturria: Dialnet