Etude palynologique des marnes de Celleneuve (Pléistocène inférieur). Hérault
- 1 January 1973
- journal article
- Published by PERSEE Program in Bulletin de l'Association française pour l'étude du quaternaire
- Vol. 10 (1) , 13-24
- https://doi.org/10.3406/quate.1973.1214
Abstract
Palynological study in marls of Celleneuve reveals the deposit origin : a lagoon alternatively depending on washes and sea-water ingressions. The presence of a local forest is proved ; the climate was warmer than it is now and a dry season settled. A lower Pleistocene age is assigned to this microflora.Keywords
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