The Pleistocene fauna (other than Primates) from Asbole, lower Awash Valley, Ethiopia, and its environmental and biochronological implications

The Asbole area in the Lower Awash Valley yielded a diverse fauna of large and small mammals, associated with an Acheulean industry. The most notable forms are a potentially new species of herpestid, a large collection of Kolpochoerus majus, and the earliest known Bos in Africa. Biochronologically, this fauna belongs to the earliest Middle Pleistocene, and is roughly contemporaneous with the Bodo site further south. Paleoenvironmentally, the fauna suggests a mosaic of landscapes among which humid environments, grasslands and forests, are predominant.     

L'Ichthyofaune des marnes messiniennes des environs de senigallia (Marche,Italie): Signification paleoecologique et paleogeographique

The revision of the fish fauna from the Messinian marls of Senigallia (Marche, Italy) leads to the reduction of the faunal list of the fossil Fishes found in this locality to only four species. One new genus is created: Cryptolebias new. gen.. This fish fauna characterizes an environment with a variable salt content: it may have been more or less temporarily connected with the sea, although it was also exposed to noticeable continental influences, as demonstrated by the occurrence of Amphibians and Reptiles (Ophidians).     

Deux nouveaux gisements a otolithes de teleosteens,dont une espece nouvelle,dans l'Aquitanien continental du Midi de la France

The continental Aquitanian of Southern France has yielded an otolith fauna containing seven species pertaining to the Umbridae and Cyprinodontoidei. One new species is here introduced: genus Cyprinodontidarum feistae. Such an assemblage indicates lacustrine deposition with possibly lagoonal influence. Two zones have been established: a first one, corresponding to the Lower and Middle Aquitanian is characterized by Prolebias praecursor; the second one, representing the Upper Aquitanian, is more diversified and characterized by genus Cyprinodontidarum angulosus.     

Restes de vertebres et de mollusques continentauxdans le Villafranchien de la Sardaigne

Remains of vertebrates of Villafranchian age have been found in the Nuraghe Su Casteddu (Nuoro, Sardinia) formation. The fossiliferous layer contain a rich fauna of continental molluscs. The composition of the vertebrate fauna is as follows: Rana sp., ? Coluber sp., Aves indet., Episoriculus aff. gibberodon PETENYI, Talpa sp., Chiroptera indet. and Rodentia indet. It is the first discovery of Villafranchian vetebrates in Sardinia.     

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.     

Une faune de petits mammiferes d'age turolien moyen(Miocene superieur) a Cucuron (Vaucluse); donnees nouvelles sur le genre Stephanomys (Rodentia) et consequences stratigraphiques

A small mammal fauna, including rodents and a new species of Murid, Stephanomys stadii n. sp., has been found in a continental formation underlying the deposits with the famous big mammal fauna of Mont Luberon. This fauna of small mammals is a little younger than the fauna of Los Mansuetos (Spain), so, the Pikermian fauna of Mont Luberon, which is said to be of the same age as the fauna of Pikermi is younger than the fauna of big and small mammals of Los Mansuetos.     

Eocene siliceous sponges from the Ebro Basin (Catalonia, Spain)

The Eocene (Bartonian) marls of the La Guixa Member and Gurb Member, Vic Marls Formation (Ebro Basin, Catalonia, Spain), contain a very rich and diversified siliceous sponge fauna. The fauna is dominated by hexactinellids; lithistids and other demosponges are rare. It consists of 16 species representing 16 genera. Eleven new species and two new genera are proposed for these sponges: Reguantella cavernosa nov. gen. nov. sp., Regadrella concinna nov. sp. (both Hexactinellida, Lyssacinosa), Eurete clava nov. sp., Pleuroguettardia iberica nov. sp., Aphrocallistes almeriae nov. sp., Hexactinella informis nov. sp. (all Hexactinellida, Hexactinosa), Brachiolites munterensis nov. sp., Centrosia viquensis nov. sp., Callicylix eocenicus nov. sp., Rhizocheton robustus nov. sp. (all Hexactinellida, Lychniscosa), Propetrosia pristina nov. gen. nov. sp. (Demospongia, Haplosclerida). Some genera of sponges in this fauna are still extant, but, in general, the predominant ones are very close in morphology, and, without doubt, closely related to the Late Cretaceous sponges. This fauna also differs considerably, in terms of composition, from most other described faunas of Tertiary sponges from the Mediterranean region, which are dominated by lithistid sponges. Lithistid sponges are rare in this investigated assemblage, which seems most similar to an as yet undescribed Eocene fauna from Italy. There is ecological differentiation in the proportions of particular sponges in various outcrops and/or stratigraphical levels that is clearly associated with water-depth-related controlling factor(s): Munter, Tona and Sta. Cecilia represent the deepest facies, Gurb is intermediate, and St. Roc and Vespella are the most shallow. The exact bathymetric position of the sponge fauna is difficult to estimate, but it seems that 100 m (but probably 200 m and more in the case of the deepest parts) of water depth may be inferred for this facies.     

Arvicolidae (Rodentia) from the Pliocene of Tollo de Chiclana (Granada, SE Spain)

Several new fossiliferous Pliocene localities have been identified in the continental deposits of the area of Tollo de Chiclana (Guadix Basin, SE Spain), that have yielded a rich rodent and insectivore fauna. In this paper, we study the Arvicolidae from these localities. Remains adscribed to the genera Dolomys, Mimomys and Kislangia have been found, which are very interesting from a biostratigraphical point of view.     

Tremadoc (earliest Ordovician) brachiopods from Purmamarca and the Sierra de Mojotoro, Cordillera Oriental of northwestern Argentina

The Late Tremadoc storm-dominated shoreface to inner platform deposits exposed west of the Purmamarca village (Coquena Formation) contain a considerably more diverse brachiopod fauna than previously reported. Coquinite horizons from the lower heterolitic succession have yielded monospecific associations of Nanorthis purmamarcaensis nov. sp. (formerly assigned to N. christianiae KJERULF), which is also reported from the Late Tremadoc rocks of the Cerro San Bernardo area. The fine-grained Upper Member of the Coquena Formation contains a more diverse fauna composed by Nanorthis brachymyaria nov. sp., Astraborthis quebradensis nov. sp. and the new plectorthid genus Lipanorthis (type species L. andinus nov. sp.). A different species of Lipanorthis (L. santalaurae nov. sp.) from the Mid Tremadoc Floresta Formation of the Sierra de Mojotoro is also described.     

Euxinomys galaticus N. G. N. Sp. (Muridae,rodentia, mammalia) du pliocene de çalta (Ankara,Turquie)

Among the abundant fauna of Mammals from Çalta, a new Murid was found: Euxinomys galaticus, characterized by its internal cusps which are very back-placed, its t1 separated from the t2 but linked to the t5 on the M¹. The inferior molars present a strong median longitudinal crest. This new genus. Euxinomys also contains «Parapodemus similis from the Odessa's Catacombs.     

Lopingian (Late Permian) brachiopods around the Wuchiapingian-Changhsingian boundary at the Meishan Sections C and D, Changxing, South China

The strata below the defined Wuchiapingian-Changhsingian boundary GSSP are mostly covered and obscured by faulting at the Meishan Section D. Therefore, it is very difficult to collect fossils there. After an intensive excavation at Meishan Section C, a diverse fauna based on high-resolution biostratigraphy comprising brachiopods, ammonoids, conodonts, fusulinids and small foraminifers were found. Among these fossils, brachiopods are the most dominant. Eleven species of 10 genera based on more than 1300 specimens are identified. This brachiopod fauna is of late Wuchiapingian-Changhsingian of Lopingian (Late Permian) in age as well constrained by the associated ammonoid Pseudogastrioceras sp., Jinjiangoceras and Konglingites sp., the fusulinid Palaeofusulina and the conodont lineage from C. longicuspidata to C. wangi. In terms of the changes of brachiopod fauna composition around Wuchiapingian-Changhsingian boundary, it clearly indicates a continuous transgression from the upper part of the Lungtan Formation to the lower part of the Changhsing Formation. A new species, Neochonetes (Huangichonetes) meishanensis, is described and some other species are discussed based on the new collection from Meishan Sections C and D.     

Les nouveaux gisements villafranchiens du ravin de Cornillet (Moustiers Sainte-Marie,Alpes de Haute Provence,France) et leur contexte géologique

Several mammal remains were recently discovered in the Cornillet gully deposits: Nyctereutes megamastoides, Pachycrocuta perrieri, Dicerorhinus etruscus, Gazella borbonica. Eucladoceros senezensis, Croizetoceros ramosus. This fauna is attributed to the middle Villafranchian.The most recent beds of the Riez-Valensole basin include several superimposed units with three type of facies: fluvio-eolian (i. e. a conglomeratesand-silt sequence), lacustrine and breccian. The Upper Pliocene represented in the Puimoisson-Ségriès region by fossiliferous lacustrine deposits is covered with coarse detrital material. The Cornillet deposits can be found at the lower part of the calcareous formation continuing this Plio-Pleistocene stratigraphy.The breccias of Balène, located at the top ofthese formations, constitute a thick spread of the detrital material of cryoclastic origin. This spread appeared later than the tectonical thrust of the surrounding calcareous mountains upon the Tertiary basin.     

Ostracodes de la Formation de Bhanness,Kimméridgien (Jurassique supérieur) du Liban central : taxonomie,paléoécologie et paléobiogéographie

A microfauna composed of 11 species of ostracodes belonging to 11 genera have been recovered from the Bhanness Formation of Kimmeridgian age, in Central Lebanon. Four species are new and are described herein: Ektyphocythere dahressawanensis nov. sp., Dicrorygma (Orthorygma) libanensis nov. sp., Citrella? elongata nov. sp. and Procytherura inflata nov. sp. From a palaeobiogeographical standpoint, this fauna characterizes the North Gondwana province which differs from the South Gondwana province, particularly by the presence of the genus Schuleridea and the absence of the genus Majungaella.     

Planktic foraminiferal biostratigraphy of theMaastrichtian sedimentary beds at Ain Mdeker,northeastern Tunisia

Maastrichtian Foraminifera from the sedimentary beds at Ain Mdeker are recorded and identified. The fauna examined is found to be clearly Tethyan in composition. On the basis of this fauna, four planktic foraminiferal zones, the Globotruncana falsostuarti Zone, the Rugotruncana gansseri Zone, the Abathomphalus mayaroensis Zone and the Globotruncana falsocalcarata Zone are distinguished in the Maastrichtian of the sequence studied. These zones are futher compared with the zones established in equivalent strata in the sequence at El Kef, the most complete sequence in Tunisia. In addition to the index species only the biostratigraphically most important species from the fauna studied are illustrated.     

Silurian reef-dwelling pentamerid brachiopods, Wisconsin and Illinois, USA

Eight species of pentamerid brachiopods, assigned toApopentamerus, Capelliniella, Kirkidium, Lissocoelina, Rhipidium, Supertrilobus andStenopentamerus, occur in stromatoporoid-coral reefs of the Silurian (Wenlockian) Racine Formation, Wisconsin and Illinois, USA. One new taxon,Rhipidium kuglitschi n.sp., is described. In contrast to level-bottom communities, where single pentamerid species occur in great numbers over large areas, pentamerids were generally rare members of the Racine reef fauna, and most species have localized distributions. An increase in diversity from one pentamerid species in the north to six species in the south correlates with a southward increase in reef size. Four morphologic groups of pentamerid species differed in the shape of the mantle cavity, which suggests different dynamics of suspension-feeding. Where two or more species are present in single reefs, co-occurrence of these groups represents a partitioning of the pentamerid niche. The relatively high diversity, local distributions, and morphologic distinctions among the Racine pentamerid fauna represent an evolutionary radiation and functional specialization of pentamerids in Wenlock reefs.     

The Darriwilian Hiswah fauna of western Gondwana (Jordan): Biostratigraphy,palaeogeography and palaeoecology

The fauna and facies of the Hiswah Formation in southern Jordan were investigated. The formation indicates deposition under low energy, open-marine, siliciclastic shelf conditions and reflects the maximum of the first regional post-Cambrian marine transgression on the northern edge of the Arabian-Nubian Shield. This eustatic signal accompanied by a maximum flooding surface can be traced over the entire Arabian Plate and Turkey. The lower part of the Hiswah Fm. consists of pelagic mudstones with only occasional thin beds of rippled, hummocky cross-bedded siltstone and mudstone concretions, and contains a distinct fauna of low diversity. The upper part of the formation is characterized by sandstone-siltstone alternations with some hummocky cross-stratification in its lower portion and trough cross-bedding and ripple marks above indicating somewhat shallower conditions. A very detailed re-investigation of the fauna from the lower part of the Hiswah Fm. and extensive new fossil material indicates that the most remarkable faunal element is the planktonic graptolite Didymograptus murchisoni (Beck in Murchison, 1839in) which, in the past, has been determined erroneously as D. bifidus (Hall in Berry, 1962). Numerous specimens of small obolid brachiopod Palaeoglossa sp. cf. P. attenuata (Sowerby, 1839) represent the most common benthic element within the Hiswah fauna. The exceptional arthropod Hanadirella cf. bramkampi El-Khayal, 1985, is reported for the first time from Jordan, representing its fifth known region of occurrence in addition to Saudi Arabia, Algeria, Spain, and France. For the first time, cephalopod remains are described from the Ordovician of Jordan by the occurrence of ?Dideroceras sp. and a second, indeterminate species. The biostratigraphic age of the Hiswah fauna is revised to late Darriwilian (Dw 3, upper Middle Ordovician) according to our re-investigation of the graptolites. The Hiswah fauna represents the oldest body fossils of the Ordovician marine sedimentation in southern Jordan and is palaeogeographically strongly related to northern and northeastern Saudi-Arabia and to high/mid-latitude Gondwana margins in general.     

Observations sur les Esthéries de la Lettenkohle (Passage muschelkalk-keuper) dans les vosges moyennes

New outcrops in the Rambervillers and Mirecourt area (Vosges) have provided a fine Estherian fauna in Lettenkohle horizons. Euestheria minuta and E. laxitexta lived together, E. minuta being the most numerous species, thoughout the Middle Lettenkohle, when the environment was favorable.