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).     

Une nouvelle espèce d'Apodemus (Rodentia,Mammalia)du Pliocène de la dépression de Guadix-Baza (Grenade,Espagne)

This paper describes a new species of Apodemus,A. agustii, a Middle Pliocene Muridae from the Guadix-Baza basin. Its morphology is far from that postulated as more frequent in Apodemus: its molars crowns are relatively high: there is no connection between t6 and t9 in M¹ and M². Taking in account this and its age, it is placed in an evolutionary branch, convergent with “Rhagapodemus” morphotype.     

Présence de Tyto balearica (Aves,Strigiformes) dans des gisements continentaux du Pliocène de France et d'Espagne

Tyto balearica was described as an endemic insularform of Barn Owl from the Balearics. New remains referable to this species have been found in continental localities from Spain and Southern France, older than or contemporaneous with the Balearic sites. The great size of this species, comparatively to the recent European Barn Owl, Tyto alba, can be related to a diet including mainly large size rodents, larger than the preys which constitute the food of the recent European form. However the existence of a connection between the size of the Owl species studied and the high abundance of prey remains observed in every site is not excluded.     

Bovidae (Mammalia) du Pliocène final d’Ahl al Oughlam, Casablanca, Maroc

Only seven bovid species are present at Ahl al Oughlam: aTragelaphus (rare), a Bovine close toPelorovis ? praeafricanus but mostly known by teeth, a new species of kob (perhaps of an endemic lineage), aParmularius slightly more primitive than at Olduvai,Beatragus (mentioned for the first time in North Africa),Gazella thomasi, and a new species of gazelle noticeable by its nasal region. The Ahl al Oughlam bovids are in good agreement with an age of 2.5 Ma. They point towards an open and probably rather unfavourable, perhaps cold, environment.     

Révision d’Oryctolagus lacosti (Lagomorpha,Mammalia) du Pliocène supérieur de Perrier (Auvergne,France)

Fossil leporids from the Upper Pliocene of the locality of Perrier-Étouaires (Auvergne, France) are here revisited. They were initially attributed to Lepus lacosti by Pomel (1853), and later to the genus Oryctolagus. This material had been neither accurately described nor figured until now. Thus, a lectotype and two paralectotypes have been chosen among the material of the original collection. The diagnostic character of Oryctolagus lacosti is its big size, similar to that of modern hares (Lepus), together with other morphological characters that fit in the variability range of European rabbits (Oryctolagus cuniculus). Fossils of leporids similar to those of Perrier have also been found in several Plio-Pleistocene localities from western Europe.     

Synthèse biostratigraphique du plio-pléistocène de Guadix-Baza (Province de Granada,Sud-Est de l'Espagne)

In the Guadix-Baza basin, a continental sequence 0214 ranging from the Upper Miocene (Upper Turolian) to the Middle Pleistocene (Cromerian) has been established. An essay of biozonation by means of the Rodent succession is proposed, based on the following biozones: Trilophomys castroi, Mimomys occitanus, Mimomys cappetai, Mimomys cf. reidi, Mimomys ostramosensis, Allophaiomys pliocaenicus, Mimomys savini and Arvicola cantiana.     

Suoidea du Miocène inférieur de Laugnac (Lot-et-Garonne, France)

The fossil vertebrate locality of Laugnac is the type locality of the Neogene mammalian zone MN2b. It has yielded many remains of Suoidea belonging to two different genera.Xenohyus venitor is characterized by its large size and especially its large central upper incisors, I1/ and I2/. It is quite difficult to know its phyletic relationships because the material is not abundant.Hyotherium cf.meisneri is more abundant with a quite good skull, pieces of skull, jaws and isolated teeth. It belongs to a peculiar lineage different from that ofH. major from Saint Gérand-le-Puy, France. It has some similarities withAureliachoerus aurelianensis from later geological levels (MN3-MN5).     

Première découverte de Viperidae (Reptilia,Serpentes) dans les îles Baléares (Espagne) : des vipères du Néogène de Minorque. Description d’une nouvelle espèce du Pliocène

Two viperid snakes, Vipera natiensis sp. n. (belonging to the Vipera aspis group) and Vipera sp., have been found in the Pliocene of Minorca. On the other hand, an indeterminate viperid extends back the fossil record of the family in the Balearic Islands, to the Middle Miocene. These fossils represent the first report of viperids from the Balearic Islands. Vertebra of Vipera natiensis sp. n. are characterised by a concave anterior border of zygosphene, dorsoventrally flattened, short (as wide as long) and blunt prezygapophyseal processes. Centrum convex in transverse section, subcentral margins poorly marked and presence of two well defined subcotylar tubercles. Hypapophysis located posteriorly on the centrum and not prolonged anteriorly, or only slightly prolonged as a keel. The dorsal border of the neural spine is slightly thickened; the posterior border of the neural spine is markedly inclined posteriorly; as a result, the spine forms a posterior point, which is more or less developed, depending on the position of the vertebra along the vertebral column. The presence of Viperidae in the Neogene of the Balearic Islands involves the existence of a terrestrial connection between this archipelago and the continent during the Early Miocene and/or Middle Miocene and perhaps the presence of a later connection during the Late Miocene.     

Une nouvelle espèce du genre Bohlinia (Mammalia,Giraffidae) du Miocène supérieur de Toros-Menalla,Tchad

New Giraffidae specimens discovered from the Late Miocene fossiliferous sector of Toros-Menalla (northern Chad) are described. These specimens are assigned to Bohlinia, a genus known so far only in some Late Miocene localities of Eurasia. This is the first occurrence of the genus in Africa. Analysis of the material allows us to describe a new species of giraffid, Bohlinia adoumi n. sp., probably close to the Eurasian forms.     

Clausiliidae (Gastropoda,Euthyneura)du Néogène du bassin rhodanien (France)

Clausilids of the Neogene of the Rhone province are known by twelve species among whose three are news. During the Miocene, and specially during its upper part, the only genus Triptychia is undoubtedly known. It is represented by Triptychia (Milne-Edwardsia) lageti nov. sp. and two others species.The absence of others genera of Clausilids during this period and in this province makeup an information of bads conditions of growth.During the Pliocene, the Clausilids fauna is very varied. Genus Triptychia includes twospecies: T. (M.-E.) terveri, in the northern part of the Rhone province and T. (M.-E.) sinistrorsa in its southern part. Serrulina, Clausilia, Iphigena, Laminifera and Nordsieckia nov. gen. (near Serrulina) are to be found in many outcrops. Two news species of Laminifera: L. (L.) meini and L. (Polloneria) ballesioi are characteristics of the pliocene southern fauna of the Rhone province.Many Clausilids of the Neogene have disappeared because of the Quaternary bad climatic circumstances. But during the Pliocene appear the genus Clausilia very abundant actually in the western Europe.     

Sur les bois fossiles du paléocène de sessao (Niger)

In this article three structures discovered in the Palaeocene marine beds of the Krebb de Sessao (southern part of Niger) are described. These beds havevalso yielded remains of vertebrates. The formation in which these fossils were found corresponds to a marine regression; it suggests that the sea was shallow and extended rather far to the east beyond the Krebb de Sessao. A tentative synthesis presented at the end of this work seems to indicate that the types of dicotyledon wood structure of the Upper Cretaceous and the Palaeocene, at least those described from Africa, differ from the types known from more recent levels.     

Nouveaux genres de Squaliformes (Chondrichthyes) du Paléogène des Landes (Sud-Ouest de la France)

Résumé  Parmi les nombreux squaliformes récoltés dans le Lutétien des Landes (SO de la France), deux genres et espèces nouveaux ont été reconnus:Squaliodalatias weltoni n. gen. n. sp. etAngoumeius paradoxus n. gen. n. sp. La morphologie dentaire du premier permet de le rapprocher des Dalatiidae. Les relations phylétiques du second taxon sont pour 1’instant moins claires, en raison de sa denture supérieure inhabituelle pour un Dalatiiforme aussi évolué au niveau de la denture inférieure. Ces taxa nouveaux viennent enrichir nos connaissances sur un groupe encore mal connu à l’état fossile en raison de son habitat bathyal ainsi que sur la mise en place et la radiation, encore trop peu documentée, des faunes profondes.      

Hemicyon mayorali nov. sp., Ursidae du Miocène moyen de Tarazona de Aragon (bassin de l'Ebre,Aragon, Espagne)

Study of a new species of an ursid, Hemicyon mayorali of Tarazona de Aragon in Spain. This species differs from the other species of the genus by the lengthening of the snout and the morphology of M2.