Decouverte de restes de Cyprinidae (Poissons teleosteens)dans l'Oligocene moyen de Marseille (Bouches-du-Rhone)

Cyprinid Fish-remain (an articulated skeleton of Varhostichthys sp. and isolated pharyngeal teeth) have been found in the Upper part of the “argiles de Saint-Henri”, a Middle oligocene formation of Marseilles basin. The finding of these Fish-remains confirms that these deposits have been sedimented under fresh-water conditions.     

Ultrastructure de la Grégarine Callynthrochlamys phronimae Frenzel; Étude Comparée de son Noyau avec Celui de Thalicola salpae (Frenzel) (Eugregarina)

SYNOPSIS. The structure of the gregarine Callynthrochlamys phronimae has been studied with the electron microscope. The cuticular complex is not different from those previously described in other species of gregarines. It is composed of 2 layers of different thickness delimited by 3 unit membranes and constitutes series of oblique folds at the surface of the deutomerite. Longitudinal rods of dense material surrounded by a slight pellicle are seen under the cuticle. Pinocytic vacuoles are present under the surface of the gregarine. Cytoplasmic organelles include mitochondria, Golgi complexes, endoplasmic reticulum, vacuoles and dense bodies from different sizes. There is a connection between the different features of the cytoplasm in the protomerite and deutomerite and the corresponding cuticular organization.
A characteristic feature of the species is the peculiar differentiation of the nuclear membrane. The nucleus is surrounded by a typical double membrane of which the inner one has a dense fibrillar layer apposed to it. In mature trophozoites, tubular expansions without inner layer arise from the double membrane; the same type of nuclear membrane occurs in another species, Thalicola salpae.     

Présence de l’éocrinoïde Ascocystites Barrande (Echinodermata,Blastozoa) dans l’Ordovicien supérieur (Caradoc) de l’Anti-Atlas (Maroc) : premières données

Family Ascocystitidae, defined and established by Georges Ubaghs in 1967, includes a single genus, Ascocystites. This genus was described and figured for the first time by Barrande in 1887, from Bohemian specimens. Thereafter, specimens brought close to Ascocystites or assigned to this genus were described starting from samples collected in Bohemia in the Armorican Massif or in Portugal. The new specimens were collected in Morocco in the Eastern Anti-Atlas, within the formation of Izzeguirene of Caradoc age. The studied material includes several sandy slabes often containing many well-preserved and almost complete individuals. These levels gather individuals of various sizes, corresponding to various stages of development. The morphological study in progress should allow a specific attribution by comparison with the Bohemian and Armorican forms actually known. The Moroccan material has, in addition, the advantage of corresponding to associations of several Echinodermata groups, rich in individuals, allowing a taphonomic and possibly paleoenvironmental study. Biostratigraphically, Ascocystitidae are actually known between Middle (Armorican Massif and Portugal) and Upper Ordovician (Bohemia and now Morocco). The discovery of Ascocystitidae in the Moroccan Anti-Atlas extends their distribution, within gondwanian domain, during Middle and Upper Ordovician.     

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.     

Nouveau matériel de Leptobos (Smertiobos) crassus (Artiodactyla, Mammalia) du Pléistocène inférieur à Renzidong (Chine de l’Est)

New remains of Leptobos (Smertiobos) crassus have been identified among the fossils excavated from a new early Pleistocene site at the Renzidong in Anhui Province, Eastern China. It is a Leptobos bearing frontal appendices with a simple curvature and its distal part turns higher than the other species of the subgenus. The present study shows that the first appearance of Leptobos in China is in the zone equivalent to the European MNQ 16b, later than its first appearance in Western Europe (MNQ 16a); and the genus Leptobos can serve as index fossil of the lower Pleistocene in China (2.5-0.78 Ma, Chinese definition).     

Nouvelles observations sur les Miogypsinidés du Miocène inférieur et moyen de Provence et de Corse (France) et de Sardaigne septentrionale (Italie)

The detailed study of the Miocene strata of Bonifacio has revealed an atypical Miogypsinid assemblage. In addition to the three already cited genera, Miogypsinoides, Miogypsina and Miolepidocyclina from this region, Miogypsinodella is for the first time represented by two new species (Mdella corsicana nov. sp. et Mdella pillaria nov.sp.). The stratigraphical ranges of each genus in the Miogypsinidae are not verified here. However, Mdes bantamensis is still present in the Upper Burdigalian and the genus Miogypsinoides is also present in the Lower Langhian. Six species of Miogypsina coexist in the Upper Burdigalian (M. tani, M. globulina, M. intermedia, M. cf. sabahensis, M. cushmani, M. mediterranea) and two species are present in the Lower Langhian (M. antillea, M. digitata). This distribution is apparently an example of palaeoendemism resulting from the geographic isolation and the rotation of the Corso-Sardinian block and also from the palaeogeographical and palaeoecological favourable environment during that time.     

Estudio paleoecológico de Foraminíferos de testigos del Holoceno de Golfo Nuevo (Patagonia, Argentina)

A micropaleontological study (Order Foraminiferida) was conducted on two Holocene cores from Golfo Nuevo (Patagonia, Argentina). The most abundant species are Buccellaperuviana f. campsi (Boltovskoy) and Bulimina patagonica (d’Orbigny), suggesting an inner-shelf environment. Qualitative and quantitative analyses indicate the paleoecological and paleoenvironmental variations along cores. A transition from normal marine conditions of the inner shelf during the Middle Holocene (ca. 8160-7700 years B.P.) to marginal marine conditions in the Late Holocene (ca. 1890 years B.P.) is inferred. This transition was accompanied by lower oxygen levels than the current values in Golfo Nuevo. These variations may have been due to an increase in precipitation near the study zone and a rise in sea level caused by an improvement in the climatic conditions related to the Climate Optimum (ca. 7000 years B.P.). These new conditions of higher temperature and lower salinity of the surface waters may have hindered deep-water renewal, producing a change in the circulation dynamics of the gulf and causing a reducing environment.