Les ostracodes neogenes du bassin de Savigne-sur-Lathan(Faluns de Touraine) I. Biostratigraphie et paleoecologie

The Neogen formations from the basin of Savigné-su-Lathan (Indre-et-Loire) have yielded 53 species of ostracods.The connections with the best known fauna from the Aquitaine basin and the Rhône basin are discussed.     

Deux nouveaux sites à traces de pas dinosauroïdes dans la Formation Dolomitique de l’Hettangien de Lozère,Languedoc-Roussillon,France

Recent ichnological studies revealed two new localities showing dinosaur footprints in the Hettangian Dolomitic Formation from the Causses Basin, southern France. The traces are reported from the northern part of the basin, in Lozère, an area where Lower Jurassic dinosaur ichnites were poorly documented. The surfaces bearing footprints are characterized by a large number of traces. The ichnites are ascribed to Grallator (Hitchcock, 1858), Dilophosauripus (Welles, 1971) and Eubrontes (Hitchcock, 1845) whose trackmakers were theropods. Although numerous tracksites were previously described in the southern part of the Causses Basin, these three ichnotaxa are for the first time observed in association into the Dolomitic Formation.     

Presence de Gazella deperdita (Gervais) 1847 du gisement du Miocene superieur (Turolien) des Mistrals (Vaucluse,Sud-Est de la France)

Among the two bovid genera represented in the turolian locality Mistrals I, Gazella and Miotragocerus, the most abundant is a gazelle which, after comparison with Gazella deperdita from the Mont-Luberon, turns out to belong to this species. Resemblances between the two faunas, already noticed in the study of the Hipparions, are thus comfirmed.     

Sur la presence de vegetaux a structure conservee du Viseen dans le poudingue mosaique du Stephanien du bassin de Saint-Etienne (France)

Upper Visean plant-bearing cherts have been discovered in association with others yielding a Stephanian A flora, in conglomerates (poudingue mosaïque) from the base of the Stephanian B at Grand'Croix. It confirms the distant source, from the Roanne region, of the Dinantian elements during the initial basin sedimentation and constitutes an excellent example of complex reworking of fossil plant material.     

Les haches polies du site de Chastel-sur-Murat (commune de Chastel-sur-Murat,Cantal, France)

A study of 25 probably Middle Neolithic polished axes discovered at the beginning of the 20th Century in the site of Chastel-sur-Murat (Cantal, France), allowed to establish the origin of these objects. Some were shaped in rocks of the sector (basalts and fibrolites). The other ones result from regions several hundred kilometres apart: cinerite from Aveyron, flint from Berry, eclogite from the Italian Alps. This surprising variety confirms the existence of long-distance traffic currents of lithic raw materials during the Neolithic. To cite this article: A. de Goër de Herve et al., C. R. Palevol 1 (2002) 123–128.     

Deux nouvelles tortues de l'Éocène inférieur de Saint-Papoul (Aude, France)

Two new turtles from the Lower Eocene of Saint-Papoul (Aude, France). Among the fossil turtles from of the Lower Eocene of Saint-Papoul (Aude, France), two new taxa of freshwater Testudinoidea are described. The first is a new species of the genus Palaeoemys, known before in the Lutetian of Germany. The second taxon is a new genus, also described on material of Pépieux-Cesseras and Eygalayes. To cite this article: S. Hervet, C. R. Palevol 2 (2003).     

Selaciens nouveaux de l'Albien superieur de Wissant (Pas-de-Calais)

Screening in the Albian of Wissant area has allowed to collect an interesting selachian fauna including some new elements: Orectoloboides nov. gen., Scyliorhinus destombesi nov. sp. and Protosqualus sigei nov. gen., nov. sp.. The relationships of these forms are discussed.     

Organismes filamenteux de l’ambre du Santonien de Belcodène (Bouches-du-Rhône,France)

Millimetric amber grains associated with lignite debris were recently reported in the Santonian marine series from Belcodène (Bouches-du-Rhône, France). These are mainly yellow to reddish drop-shaped grains, more or less transparent. They reveal the presence of various microorganisms, belonging to prokaryotes (bacteria, actinomycetes) and eukaryotes (filamentous fungi) here described for the first time. These microorganisms form sometimes crusts around the amber grains and grew centripetally into the ancient resin before its solidification. The depositional environment of amber was open to marine influences, while the original environment of resin flow was a coastal forest with dominant angiosperms.