Apports de la palynologie a la connaissance du Pliocène du Roussillon (sud de la France)

The present study illustrates clearly how pollen analysis may be applied to stratigraphy from a botanical point of view. Within a chronologically reliable frame (Middle Pliocene for the marine deposits on the basis of Foraminifera record; two subzones for continental deposits on the basis of Mammals record: Hautimagne for Terrats fauna, Sète for Serrat-d'en-Vacquer fauna), palynology provides a good stratigraphical boundary: the extinction of the Taxodiaceae. In a remblayage area, it is established that a continental level is not necessarily younger than a marine one unless they are superposed. Many profiles are replaced according to the «progradation of the pliocene gulf of Roussillon. The boundary between marine and continental deposits cuts through the chronological line of the Taxodiaceae extinction. The flora investigated (93 taxa) is the first known for the Pliocene of this area. The extinction of the Taxodiaceae in southern France has a climatic cause: the setting in of a mediterranean rhythm (dry summers). This extinction is much older than the one which took place in Italy (Tiberian boundary) and in the Netherlands (Reuverian-Pretiglian boundary).     

Analyse pollinique des dépôts lacustresdu Pléistocène inférieur de Banyoles (Bañolas,site de la Bòbila Ordis - Espagne): un élément nouveau dans la reconstitution de l'histoire paléoclimatique des régions méditerranéennes d'Europe occidentale

Clays from Bòbila Ordis near Banyoles have yielded a rich pollen flora. Three pollen zones are recognizable: the lower and the middle parts are dominated by components of a deciduous forest (with numerous exotic taxa); in the upper part, Pinus pollen and NAP (especially Compositae) are in a majority with an increase of mediterranean taxa towards the top. This floristic evolution may be connected with a climatic change characterized by a decrease in humidity which is itself linked to a world cooling. We suggest a possible relation with the pollen flora published by H. Elhai. The pollen diagram of Bòbila Ordis is the second so far established from Lower Pleistocene deposits in the Mediterranean countries of Western Europe; chronologically it follows the Bernasso (Languedoc) pollen diagram and confirms the latter results.     

Un gisement a plantes des formations pliocènes des environs de Rasteau près Vaison-la-Romaine (Vaucluse): Stratigraphie,faune, étude des macrorestes végétaux,palynologie

A new Pliocene deposit with vegetal impressionswas discovered at Rasteau (near Vaison-la-Romaine, Vaucluse. The study of these impression and the sporopollinic analysis from many levels allows us to specify its stratigraphical position in the Pliocene of the Rhone valley. So, the above mentioned levels settled just before the Hautimagne deposit (Neogene zone MN 14 for the mammals). The macroflora and the microflora appear to be related with a temperate warm and wet climate.