New Late Cretaceous dinosaur findings from northwestern Transylvania (Romania)

In 1905, Nopcsa tentatively identified a fragmentary rib from the Jibou Formation at Someş Odorhei as belonging to an ornithopod dinosaur. Therefore, he concluded that the base of this formation is Late Cretaceous, but this hypothesis was subsequently ignored or rejected by other authors. New dinosaur bones discovered in this locality by new excavations are here interpreted as belonging to the euornithopod Zalmoxes shqiperorum Weishampel, Jianu, Csiki and Norman, 2003. The base of the Jibou Formation can therefore be regarded as Maastrichtian, correlative to the Sânpetru Formation and to the middle member of the Densuş Ciula Formation from the Haţeg Basin, as well as the base of the Şard Formation in the southwestern Basin of Transylvania, in the Alba Iulia area. The presence of Zalmoxes at Someş Odorhei also confirms the northeastern extension for the ‘Haţeg Island’ in Transylvania.     

A Late Campanian sphenodontid (Reptilia, Diapsida) from northern Patagonia

The fossil record of sphenodontids in the Southern Hemisphere is much longer than in Laurasia, where they became extinct after Early Cretaceous times. Recent works demonstrated the persistence of at least eilenodontine sphenodontids until the ‘mid’-Cretaceous of Patagonia. Focused examination of the Los Alamitos Formation collections provided remains of Late Campanian sphenodontids. Although the phylogenetic position of these remains is still uncertain, they belong to a new, unrecorded species of sphenodontid perhaps related to opisthodontians or primitive, toothed sapheosaurs. To cite this article: S. Apesteguía, C. R. Palevol 4 (2005).     

Étude de la matière colorante de la grotte d'Arenaza (Galdames, Pays Basque, Espagne)

The present work completed the research that we have developed during the last years in the cave. The analysis of the painting matter has been made to recognize the anthropic origin of certain figures, to compare the natural iron oxide deposits with one of the paintings with the purpose of establishing the supply area, and to compare the pictorial matter of the different figures to characterize the technical process of the cave. Nineteen samples were taken, from the painted figures and from natural depots. The analysis made in the C2RMF have confirmed the anthropic origin of two figures and have shown the preparation of different pigments for a same painting.     

Madonna dell'Arma (San Remo, Italie) : expression locale de la végétation ligure au cours du Paléolithique moyen

Pollen analysis of Madonna dell’Arma cave inside part (Liguria, Italy) allowed us to reconstitute, at local scale, the Ligurian coastal vegetation between the end of the last interglacial period and the beginning of the pleniglacial. This transition period shows an important representation of arboreal cover and a persistence of thermophilous elements that allowed us to considerate the western Liguria as a periglacial refuge. During the end of the last interglacial, xerophytic, halophytic herbs and shrubs taken over from a Mediterranean pre-forest unit in the first slopes constituted the coastal zone. The nearness of Argentina torrent and the Armea influenced, in the coast, the existence of marshy zones colonized by hygrophilous trees. In the Ligurian lowlands spread out sclerophyllous and mesophilous forests according to altitude. The beginning of the pleniglacial is indicated in the sequence by increases of Pinus, Cupressaceae and Artemisia in the context of a decline in the thermophilous components. This picture of vegetation has become integrated into the multidisciplinary studies of the site and contributed to the elaboration of palaeoclimatic hypothesis similar as those revealed by the fauna.     

Les industries acheuléennes de la France septentrionale

The excavations of several open air sites in Northern France and, especially in the Somme basin, have given numerous data concerning the age and the environment of the human occupations for the period from MIS 12 to MIS 8. The quality of the raw material and the function of the different sites have a great effect on the composition of the lithic assemblages as it has been seen for the different sites located near the confluence of the Somme and Avre (Cagny-la Garenne, Cagny-l’Épinette, Ferme de l’Épinette, Gentelles). The characteristics of the lithic industries of Gouzeaucourt show the complexity of the transition from Lower to Middle Palaeolithic.     

Palaeoneuroanatomy of Brachiosaurus

An overview of the palaeoneuroanatomy (brain and spinal cord) of the sauropod dinosaur Brachiosaurus is given. Although having a flexed brain configuration, Brachiosaurus presents on the whole a rather moderately derived neuroanatomical pattern. As other sauropods, Brachiosaurus shows an enlargement of the spinal cord in the sacral area. New Encephalization Quotients are calculated and found to be about 0.62 or 0.79 (depending on the body volume taken into consideration) when Hurlburt's formula is used. This suggests that Brachiosaurus, although it may not have been as a low encephalized taxon (by reptilian standards) as previously believed, did have an undersized relative brain volume.     

Une dent humaine perforée découverte en contexte Gravettien ancien à l’abri Pataud (Dordogne, France)

The existence of an Early Gravettian perforated human tooth at the abri Pataud came to light thanks to the reexamination of the osseous artefacts from the level 5. Even if the method of perforation of this tooth is analogous to the one used to pierce the animal teeth discovered in the same level, this pendant would have a particular meaning.     

Taxonomic notes on the genus Eupoa ?abka, 1985 (Arachnida,Araneae, Salticidae)

The south-east Asian genus Eupoa is redescribed and diagnosed. Seven new species are diagnosed, described and illustrated: E. daklak sp. n. (♀) from Viet-Nam; E. lehtineni sp. n. (♂♀) from India, Thailand and Viet-Nam; E. lobli sp. n. (♂) from Malaysia; E. pappi sp. n. (♂) from Thailand; E. pulchella sp. n.(♂) from Thailand; E. schwendingeri sp. n. (♂♀) from Thailand; and E. thailandica sp. n. (♂♀) from Thailand. Eupoa prima Żabka, 1985 and E. yunnanensis Peng & Kim, 1997 are redescribed and illustrated on the basis of type and/or newly collected materials. The female of E. yunnanensis Peng & Kim, 1997 is found and described for the first time.     

Yeast-based screening of natural product extracts results in the identification of prion inhibitors from a marine sponge

ABSTRACT

One of the major medical challenges of the twenty-first century is the treatment of incurable and fatal neurodegenerative disorders caused by misfolded prion proteins. Since the discovery of these diseases a number of studies have been conducted to identify small molecules for their treatment, however to date no curative treatment is available. These studies can be highly expensive and time consuming, but more recent experimental approaches indicate a significant application for yeast prions in these studies. We therefore used yeast prions to optimize previous high-throughput methods for the cheaper, easier and more rapid screening of natural extracts. Through this approach we aimed to identify natural yeast-prion inhibitors that could be useful in the development of novel treatment strategies for neurodegenerative disorders. We screened 500 marine invertebrate extracts from temperate waters in Australia allowing the identification of yeast-prion inhibiting extracts. Through the bioassay-driven chemical investigation of an active Suberites sponge extract, a group of bromotyrosine derivatives were identified as potent yeast-prion inhibitors. This study outlines the importance of natural products and yeast prions as a first-stage screen for the identification of new chemically diverse and bioactive compounds.     

Tragoportax cf. rugosifrons (Schlosser, 1904) from the late Miocene of Cessaniti (Southern Italy)

This paper describes remains attributable to Tragoportax cf. rugosifrons (Schlosser, 1904) found in the late Miocene site of Cessaniti (Vibo Valentia, Calabria) and the surrounding area. The studied specimens come from the Clypeaster sandstones, included in a marine/fluvial succession dated between 8 and 7.2 Ma. At Cessaniti, Tragoportax is associated with Stegotetrabelodon syrticus Petrocchi, 1941; Samotherium cf. boissieri Forsyth-Major, 1888; Bohlinia cf. attica Matthew, 1929; and an undetermined Rhinocerotid still under study. The genus Tragoportax was common in Eurasia and Africa during the late Miocene. The occurrence of Tragoportax cf. rugosifrons at Cessaniti confirms the peculiarity of the assemblage, with its association of species of North African and Pikermian (Greco-Iranian bioprovince) affinities.