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).     

Des Normapolles du Crétacé supérieur de Piedras Negras (Coahuila,Mexique)

Normapolles pollen grains found in the Upson andSan Miguel Formations of northeastern Mexico extend the atlantic Normapolles Province of North America to the northern part of Middle America. Besides, since one admits the Lower Maastrichtian age of the Olmos Formation, the biostratigraphic extinction of the group appears regionally earlier than in the Atlantic Coastal Plain.     

Innervation du muscle rétracteur antérieur du byssus (ABRM) de Mytilus edulis L.

Summary Detection of nerve structures containing 5-HT were described in the anterior byssus retractor muscle (ABRM) in Mytilus edulis L. after using the fluorescence microscope technique of Falck. We are able to confirm our previous results and assumptions given by histology and electron microscope studies: the neuromuscular en passage junctions, largely distributed within the ABRM, contain 5-HT.     

L’industrie du Paléolithique inférieur du site de Wujiagou,Hubei Province,République Populaire de Chine

The site of Wujiagou, Hubei Province in China, dated to just over 800,000 years, in sandy deposits and sandy-silt which covers a river terrace of the end of the Early Pleistocene, delivered a rich lithic industry, mainly composed of pebbles tools. This industry has an archaic aspect, consisted by the abundance of pebbles tools, the presence of hand-axes, and the small amount of small tools. The pebble tools include choppers and picks, in addition of band-axes. Small tools are relatively poor and have few simple retouched scrapers.     

Isorthid AE (Brachiopoda) du dévonien inférieur du massif armoricain

Three species of Isorthidae are described in the Lower Devonian of the Armorican Massif. Two of them were hitherto badly known, being never adequately described nor figured: Isorthis (Protocortezorthis) miloni from the Gahard Formation (Gedinnian) and Isorthis (Protocortezorthis) trigeri from the Saint-Céneré Formation (Gedinnian-Siegenian). Isorthis oehlertiSolle, 1976 is considered as a synonym of Isorthis (Protocortezorthis) trigeri. The geographic distribution of these species allows to corroborate that until the top of the Lower Devonian (top of Le Faou Formation), two provinces with different faunal associations exist in the Armorican Massif.     

Interprétation paléogéographique des données palynologiques du site du Paléolithique supérieur de Mezhyrich (Ukraine)

The results of palynological study of the Upper Paleolithic Mezhyrich site in central Ukraine are presented. Four local pollen zones were identified. The results of the palynological investigations allow us to hypothesize that the plant cover during Upper Paleolithic had a mosaic structure. The pollen record shows the presence of a few tree species with the predominance of herbaceous plants. We suggest that the river valleys and other local favorable sites were natural refugia where forest elements could survive even during the Last Glacial Maximum. These favorable landscapes to the existence of prehistoric hunters may have persisted during the Last Pleniglacial.     

Biostratigraphie des Miospores et des Chitinozoaires du Silurien supérieur et du Dévonien dans le bassin d'Illizi (S.E. du Sahara algérien)

Core samples from the Illizi basin yielded well preservedmiospores and Chitinozoa. The detailed study of the range of these microfossils allows accurate age assignment for upper Silurian and Devonian subsurface strata of the southeastern part of the algerian Sahara. On the other hand, these biostratigraphical data demonstrate the occurrence of important stratigraphical gaps related to recurrent emersions.     

Réinterprétation de Peltoceratoides athletoides (Lahusen), 1883 (Ammonitina,Aspidoceratidae). Conséquences sur la biozonation du Callovien supérieur et de l'Oxfordien inférieur

Peltoceratoides athletoides (Lahusen) is currently used in the Tethyan domain (Submediterranean province) as an index-species for two separate biochronological units: one a horizon near the top of the Callovian, the other a zone at the base of the Oxfordian. Paleontological revision of the species, from specimens collected in situ in South East France and in Normandy shows that species is strictly localized in the lowermost Oxfordian. Consequently, the Callovian horizon, originally defined in Anjou, should be renamed the Schroederi horizon. The usefulness of Peltoceratoides athletoides as an indicator of the first Oxfordian zone in the Tethyan domain, the counterpart of the Mariae zone, is confirmed. In addition, strict localization of the species makes it is possible to define a subzone and a horizon for the base of the Oxfordian, which are the boreal equivalents of the Scarburgense subzone and Scarburgense horizon. These new data contribute to build a standard West Tethyan scale entirely independant of the boreal zonation for the Upper Callovian and Lower Oxfordian.     

Ultrastructure du lobe postérieur de l'hypophyse du rat et ses modifications au cours de l'excrétion de vasopressine

Résumé Le lobe postérieur de l'hypophyse a été examiné sur coupes ultrafines chez 45 rats (24 normaux, 17 déshydratés respectivement 1, 2 et 4 jours, et 4 anesthésiés à l'éther), après fixation au glutaraldéhyde ou selon la méthode de Karnovsky, post-fixation osmiée et double contraste à l'acétate d'uranyle et au citrate de plomb. Des fibres neurosécrétoires sombres et claires sont reconnaissables, mais les données manquent encore pour interpréter cette différence. Des densifications juxta-membranaires sont observées dans les terminaisons neurosécrétoires là où se trouvent des amas de microvésicules. Des fibres neurosécrétoires traversent parfois des pituicytes; il est aussi souvent observé des fibres, chargées de granules, libres dans un espace péricapillaire. Les espaces péricapillaires, ramifiés en tous sens loin des vaisseaux, développent une large surface de contact avec les extrémités nerveuses et les prolongements de pituicytes.Dans des conditions techniques bien contrôlées, la déshydratation n'entraîne pas de modifications appréciables des granules de neurosécrétat après 24 h. Ensuite les granules sont diminués en nombre, de façon très considérable le 4e jour; mais les granules restants ont un contenu dense normal; jamais il n'a été observé d'aspects de granules vides . Après anesthésie prolongée à l'éther, il n'y a aucune modification visible ni du nombre, ni de la densité des granules. Ces observations sont discutées quant au mécanisme de l'excrétion de vasopressine; elles sont en faveur de l'existence de deux pools hormonaux, l'un libre et rapidement disponible, l'autre plus fortement lié et certainement contenu dans les granules jouant le rôle de réserve. Toutefois un mécanisme d'exocytose granulaire ne peut être formellement exclu.

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Ultrastructure of the rat's hypophysial neural lobe and it's changes during vasopressin release

Summary Hypophysial neural lobes of 45 rats (24 controls, 17 dehydrated resp. 1, 2 and 4 days, and 4 ether anesthetized) were fixed either with glutaraldehyde or according to Karnovsky and post-fixed in osmium tetroxyde; ultrathin sections were stained by uranyl acetate and lead citrate. Dark and clear neurosecretory fibres were observed, but sufficient data are still lacking for a valuable interpretation of these aspects. Juxta-membraneous densifications are visible in limited areas of neurosecretory terminals where clusters of microvesicles are present. Neurosecretory fibres happen to be completely encircled by pituioyte cytoplasm; fibres loaded with elementary granules are frequently encountered running free in a pericapillary space. Pericapillary spaces stretch out branching far away from vessels, resulting in a widespread contact with nerve terminals and pituicyte processes.In accurately controlled technical conditions, dehydratation does not result in any noticeable change of neurosecretory granules after 24 h. A decrease of the number of granules follows and is extremely conspicuous after 4 days; though, remaining granules keep a normal dense content, and aspects of empty granules have never been observed. After prolonged ether anesthesia, no visible change either in number or electron density of granules was observed. These findings are discussed in consideration of the mechanism of vasopressin release; they support the hypothesis of two hormonal pools, one of which would be free and rapidly available for release, the other being more tightly bound and certainly located in granules representing a storage site. Though granular exocytosis cannot be absolutely excluded.

Travail effectué avec l'aide, en matériel et en assistance technique, du Centre National de la Recherche Scientifique. — Nous remercions particulièrement Mme J. Bottini pour son aide précieuse dans la préparation du manuscrit et Mr. B. Dutillet pour sa participation aux contrôles en microscopie optique.     

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.     

Innervation du muscle rétracteur antérieur du byssus (ABRM) de Mytilus edulis L. et de Mytilus galloprovincialis Lmk.

Summary Specific and non specific cholinesterase activities were demonstrated in the ABRM of Mytilus edulis L. and Mytilus galloprovincialis L. by means of different techniques. The results were found identical for both species: neuromuscular junctions en grappe-type scarcely distributed within the ABRM, contain AChE.According to the histochemical inhibition tests, (a) the eserine inhibits AChE activity of the ABRM with a level of 5·10^–5 M or higher, (b) the ChE non specific activities are inhibited by iso-OMPA level between 5·10^–5 to 10^–4 M.The histo- and cytochemical observations were completed by showing the existence of neuromuscular junctions containing small clear vesicles: they probably are the morphological support for ACh presence.Moreover, specific and non specific ChE activities were localized in the glio-interstitial cells. AChE precipitates were developped along the ABRM sarcolemma, some muscle mitochondria and in the intercellular spaces remain enigmatic.

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L'auteur dédicace cette contribution à son père, Mr. Anthime Gilloteaux à l'occasion de son 75ème anniversaire     

Les sclérobiontes des huîtres du Cénomanien supérieur du Mans (Sarthe,France)

Oysters of the Marnes à Pycnodonte biauriculata Formation, Upper Cenomanian (Guerangeri biozone) were significantly sampled in building works within the town of Le Mans (Sarthe, France). They are colonized by episkeletobionts (encrusting organisms) and endoskeletobionts (boring and bioeroding organisms). First ones include bivalves, polychaetes, foraminiferans and bryozoans. Second ones are represented by about fifteen ichnotaxa, the producers of which, when they are known, belong to ten taxa. The oysters, some of which have a large fixation surface, are allochtonous or at least parautochtonous. The settlement of sclerobionts began when the oysters were alive (Entobia isp.) and continued post-mortem on isolated valves, transported in their final depositional environment (Gnathichnus pentax). The significance of the coexistence of both Entobia and Gnathichnus ichnocoenosis is discussed.     

Nouvelles espèces de Madréporaires dans le Kimméridgien supérieur du Jura (France)

The study of an Upper Kimmeridgian madreporarianfauna collected in the southern french Jura (between Valfin and Belley), allowed: 1) to describe five Scleractinian new species: Mitrodendron biennensis nov. sp., Hexapetalum nemorosum nov. sp., Thalamocoenia gironensis nov. sp., Cryptocoenia stelliserrata nov. sp., Columnocoenia miniflora nov. sp. and a new variety of Heliocoenia (Kobycoenia) claudiopolisensisBeauv., 1964, characterized by its small calices; 2) to modify the diagnosis and the systematic position of the species Baryhelia crassa (de From.) which was created as Heterocoenia crassade From.; 3) to increase of a new species the genus Hexapetalum only known, till now, by its Stramberg Tithon type-species; and 4) to give some palaeoenvironmental conclusions = the Upper Jurassic reef formations in the Southern Jura grew in shallow water characterized by an abundant carbonate sedimentation. Genera associations and distribution confirm the presence, between Oyonnax and Belley, of a low energy area, protected by a barrier reef and, northern of this barrier, of a higher hydrodynamic environment.     

L’assemblage lithique du site Acheuléen de Namib IV (Namib central,Namibie)

Despite a rich archaeological record, the old prehistory of Namibia, particularly from the Earlier Stone Age, is poorly documented, due to the surface context of the findings, exposed by erosional processes. In this context, human behaviors and responses to environment changes in this region during the Middle Pleistocene remain unclear. In the late 1970's, Myra Shackley surveyed the Central Namib dune desert and discovered lithic artefacts associated to fragmented fossilized bones of antelopes, elephants, zebras and buffalos at Namib IV. She interpreted this locality as an Acheulean butchery site on the shores of a paleolake. The radiometric dating suggested an age of ~347ka whereas biochronology broadly pointed the human occupation to the Mid-Pleistocene Transition (1–0.5 Ma). Thanks to these ages, Namib IV is currently the earliest dated evidence of human presence in the current Namib coastal desert. Contextualized by the existing chronological and paleoenvironmental data, we analyzed the unstudied lithic material recovered at Namib IV. To do so, we applied a qualitative morpho-structural approach to the stone tools and tried to reconstruct the productional schemes (chaînes opératoires). Our results argue for an important economy of the raw material, a spatial fragmentation of stone tool production and an important technical homogeneity of the lithic assemblage despite few possible intrusive elements. In the light of these analyses, we finally discussed the advanced site function of Namib IV as butchery site.     

Sélaciens nouveaux (Chondrichthyes,Neoselachii) du Paléocène supérieur de la région d’Ouarzazate,Maroc

Three new selachian species belonging to new genera from the Thanetian of Ouarzazate Basin are described: Tingaleus dakkai n. gen. et nov. sp., Microbatis sabatieri n. gen. et n. sp. and Garabatis atlasi n. gen. et n. sp. These new taxa as well as the associated selachian species confirm the original feature of this fauna in comparison with contemporaneous faunas occurring in the phosphate-bearing horizons of central Morocco.     

Nouvelles espèces de dasycladales du crétacé inférieur de provence (S.E. France)

In the Lower Cretaceous of Provence Cylindroporella faronensis n. sp. and Cylindroporella massiliana n. sp. represent small size species with a limited number of branches. The former ranges from the Middle (or Lower p.p. ?) Berriasian to the Lower Valanginian, the latter is found in the Lower Hauterivian, but could appear earlier in other regions. Clypeina isabellae n. sp. is also a small size form with a fibrous, yellowish microstructure, close to Clypeina sulcata, it is restricted to the Middle (or Lower p.p. ?) and Upper Berriasian. Besides their biostratigraphic and palaeobiogeographic potential value this material from Provence is also interesting from an evolutionary point of view. At generic levels it shows distinctive patterns relatively to the “Cope law”.     

La technique de débitage au Paléolithique supérieur de l’archipel du Japon

The representative debitage technique is the one of the culture of knife-to-back in the name of the superior Paleolithic of Japan. She/it can be he divided in two, the one of the first half and the one of the second half. The first corresponds at the time of apparition, either to the stage of launching of the technique of debitage laminaire whose debitage didn’t provide elaborate blades being little successive. As for the stage of fortifying of the debitage laminaire, the industries lithic to knife-to-back of the Sugikubo type developed themselves in the oriental Honshû. With regard to the region of Kantô to the second half of the first where the knife-to-back of Moro type mingled equally with those while shaping on the blade. To the recent stage of development, one can note the industry lithic to knife-to-back of Moro type is based on the technical very blady in the western Japan. Succeeding in the second half of the superior Paleolithic that the technique of debitage of Sétoüchi developed itself in this part whose debitage is characterized by the strut oblong in wing, are the transverse blades These gotten supports used especially for making the knife-to-back of Koü type while spilling country-wide. To the second recent half, the technical blade of Sunagawa type took place in all regions of Japan except the inshore regions of the Interior Sea of Séto and the region of Kinki (Kyoto-Osaka).     

Ostéologie et affinités de Trematochampsa taqueti (Crocodylia,Mesosuchia) du Sénonien inférieur d'In Beceten (République du Niger)

Among the abundant remains of Mesosuchia that have been yielded by the early Senonian locality of In Beceten (Niger), the most numerous belong to the species Trematochampsa taquetiBuffetaut, 1974. The osteology of this species is described here. This medium-sized crocodilian, with a moderately elongated skull, is characterized, among other features, by its antorbital fenestra, its surangular-quadratojugal articulation, its slightly displaced post-orbital pillar, its teeth with wrinkled enamel, and its amphicoelous vertebrae. In its general outlook, this animal is rather reminiscent of the Goniopholidae, from the Upper Jurassic and the Cretaceous of Laurasia, but it is more primitive than them, and resemblances are probably due to convergence phenomena. The family Trematochampsidae is probably essentially Gondwanian, and could persist until the Senonian thanks to a certain isolation from Laurasia, where more progressive Crocodylia became predominant much earlier than in Africa and South America.     

Les crocodiliens fossiles du Jurassique moyen et supérieur de Bourgogne

The middle and upper Jurassic limestones of Côte-d'Or (France) contain some crocodilian remains referred to the genera Teleidosaurus, Steneosaurus, and Metriorhynchus. Their preservation allows a determination at a specific level only for Teleidosaurus gaudryi (Lower Bathonian), Steneosaurus larteti (Upper Bathonian), S. heberti and S. cf. intermedius (Middle Oxfordian). Sedimentological evidence shows that Steneosaurus and Teleidosaurus are found either in very pure limestones sedimented on an epicontinental platform, in a very calm and sheltered environment, in the intertidal or supratidal zone, often associated with subrecifal facies; or in the infratidal zone, more distinctly subjected to open-sea influences (deposits, currents, reworkings). Specialised Metriorhynchidae such as Metriorhynchus are completely absent in the former type of sediment but are present in the later. One may infer, considering anatomical evidence (no dermal armour, caudal fin…) that Metriorhynchus was better adapted to swimming and rather lived in the open sea. The Teleosauridae preferred very shallow or temporarily emerged places, where they could move around thanks to their limbs which were still capable of walking on land; however, this did not prevent them from going out to sea, where the habitats of both families probably largely overlapped.