Évolution et transformation des industries lithiques taillées et polies durant le Chalcolithique et l’Âge du Bronze en Corse

Lithic industries in Corsica have been subject to important modifications during the 3rd and 2nd millennium cal. BC. Polished tools changed almost totally during that period, the majority of all lithic tools disappeared. The development of metallurgy is probably the main reason for these changes; they show the new place of lithic productions in the activities of the different communities within the island.     

Catalytically active hybrids formed in vitro between large and small subunits of different procaryotic ribulose bisphosphate carboxylases

Ribulose bisphosphate carboxylase from the procaryotic green alga, Prochloron (the symbiont of Lissoclinum patellum), has eight large and eight small subunits, and a low affinity for CO2, similar to that of cyanobacterial carboxylases. The small subunits were progressively removed from this carboxylase and from that from the cyanobacterium, Synechococcus ACMM 323, by twice-repeated, mild-acid precipitation. This procedure produced large-subunit octamers, greatly depleted in small subunits, as well as isolated small subunits. Catalytic activity of the large-subunit preparations reflected their residual small-subunit content. The two large-subunit preparations were reconstituted with both homologous and heterologous small subunits. The reassembled enzymes were catalytically competent in all cases. When fully saturated with small subunits, the hybrid enzymes were only about 20% less active than the homologously reconstituted enzymes. Heterologous reconstitution underscores the essential function of the small subunits in catalysis.     

Bioconstructions bajociennes a madréporaires et faciès associés dans l'Île Crémieu (Jura du Sud; France)

First of all this study brings necessary details aboutregional stratigraphy. It goes on to reconstitute the paleobiocenoses and the environmental conditions of bajocian coral limestone deposits: weak currents, fairly high depth, varied substrates, low relief. In the low areas scleractinians disappear and are replaced by sponges, Pseudomelania or pholadomyes communities. In order to explain the particularities of bajocian constructions, some hypothesis have been put forward, mentioning the slope of the platforms, the speed of the growth of organisms and the stability of the sea-level.     

The Permian/Triassic mass extinction among brachiopods in the Northern Caucasus (northern Palaeo-Tethys): A tentative assessment

A palaeontological record of the Northern Caucasus provides new data to evaluate the influence of the Permian/Triassic mass extinction on brachiopod communities. The study region is currently located in the southwest of Russia; it laid on the northern margin of the Palaeo-Tethys Ocean during the late Paleozoic-early Mesozoic. A total of 168 genera and 36 superfamilies are known from the Changhsingian-Bajocian deposits of this region. The total diversity of brachiopods was very high in the Changhsingian (57 genera and 19 superfamilies), but these organisms disappeared entirely at the Permian/Triassic boundary. Three genera and three superfamilies existed in the Induan, but brachiopods perished again in the Olenekian. A recovery began in the Anisian, but the Changhsingian diversity was never reached again. No genera crossed the Permian/Triassic boundary, whereas 4 superfamilies became able to do this. Ambocoelioidea was a “dead clade walking” and went extinct in the Induan, whereas three other superfamilies (Dialasmatoidea, Rhynchonelloidea, and Wellerelloidea) were more successful. Survivors included no less than 20% of genera during the entire Induan-Bajocian time interval. The Changhsingian-Anisian interval is dominated by just one type of facies in the studied region, which may explain differences in the post-extinction diversity patterns between the Northern Caucasus, South China, and other parts of the World. Use of the alternative Triassic time scale does not change the absolute duration of the post-extinction stress (5.1 myr), whereas it highlights higher rates for the Anisian recovery (appearance of 0.9 superfamilies and 2.8 genera per myr).     

Discovery of a new open-air Hoabinhian site in Luang Prabang province (Lao PDR). Dating and technological study of the lithic assemblage

The Hoabinhian is a distinctive lithic techno-complex of mainland and Island Southeast Asia. Knowledge of its relationships with key patterns of technological change at a global scale has progressed over the last two decades. However, our understanding of the Hoabinhian as an indicator of evolution during Prehistory can be substantially enhanced by examining its regional and chronological variability. Here, we present the characteristics of original Hoabinhian artefacts found in a new open-air site at Houay Pano, near Lak Sip (Luang Prabang province, Laos). This technological study of such a classic assemblage, including sumatraliths dated to 5.5 ± 0.6 ka, is a major contribution to Laotian prehistory and our understanding of the tempo-spatial variability of the Hoabinhian techno-complex.     

Le Paléolithique moyen et supérieur de la Hongrie du nord : nouvelles investigations dans la région d’Eger

The region of Eger town at the foot of the Bükk Mountains in Northeastern Hungary has particular importance for the understanding the Middle and Upper Palaeolithic periods of the Carpathian Basin. One of the key-problems is the association of carinated tools and foliate points in the lithic assemblages of the sites. New investigations at the Egerszalók-K?vágó site give fundamental data for the animated discussion on the relation between Aurignacian and Szeletian.