Troglobitic scorpions: a new genus and species from Brazil

A new genus and species of troglobitic buthid scorpion are described on the basis of a single specimen collected in Brazil. This is the first cavernicolous scorpion ever found in Brazil, and only the second to be found in South America. Some considerations on troglobitic scorpions are proposed.     

A new species of Megalonychidae (Mammalia, Xenarthra) from the Quaternary of Poço Azul (Bahia, Brazil)

The new genus and species Ahytherium aureum (Mammalia, Xenarthra, Megalonychidae) from the Quaternary of Poço Azul (Bahia, Brazil) is described. It is the first Brazilian megalonychid known from reasonably complete and well-preserved remains. Purported Brazilian megalonychids described in the past, such as Ocnopus gracilis and Xenocnus cearesis, are noted as belonging to other sloth clades, and the acceptance by past paleontologists of the existence of ‘strange’ megalonychids in Brazil is shown to be erroneous. Ahytherium aureum, in fact, exhibits typical megalonychid morphology. It differs from other known members of Megalonychidae in several characters, including a markedly shortened, but high rostral region, with dorsally inflated frontals, wide zygomatic processes of the frontal, narrow, blade-like and anterolaterally oriented lacrimals, curved, slender and oval caniniforms, gracile humerus with less developed deltopectoral shelf, and relatively distal position of the greater trochanter of the femur. A second specimen from São Paolo state is tentatively assigned to the new genus and species.     

A new pleuropholid, Gondwanapleuropholis longimaxillaris n. g., n. sp. (Actinopterygii: Teleostei) from the Jurassic of north east Brazil

A basal teleost fish is described for the first time from the Upper Jurassic Pastos Bons Formation, Parnaíba Basin, northeastern Brazil. This new material is identified as a new genus and a new species, Gondwanapleuropholis longimaxillaris. This taxon shares a number of synapomorphies with the pleuropholids. The family Pleuropholidae is confirmed as member of the Teleostei.     

Utilisation du bois de feu par les chasseurs-cueilleurs de la « Cidade de Pedra » à partir de l’Holocène moyen (Brésil Central,Mato Grosso,Rondonópolis)

Located in the south-western Mato Grosso state (Central Brazil), the vast territory of the Cidade de Pedra was continuously occupied since the mid-Holocene by several groups of hunter-gatherers. Rock paintings, lithic industries, ceramics, ornaments, combustion remains (etc.) testify their passages in the many rock art sites discovered since 1983. In this paper are presented the results of the first anthracological analyzes conducted in four of these rock shelters. The studies were realized from macro-remains carbonized from hearths, embers and concentrations. From the taxonomic identification of charcoal, the objectives are to highlight the practices of hunter-gatherers related to the collection of wood and the environment in which they evolved for nearly 5000 years. The results indicate that they practiced an opportunistic collection mainly focused on dry wood available in the vegetation around the sites. They evolved in an environment similar to that currently characterizes the region, a typical flora of the Cerrado Biome and seasonal climate.     

Les Cervidae (Mammalia, Artiodactyla) du Pléistocène supérieur-Holocène ancien de la région du Parc National Serra da Capivara (Piauí, Brésil)

The Upper Pleistocene/Lower Holocene fossil-bearing sites of the Serra da Capivara National Park Region have yielded three cervid species: Mazama gouazoubira, M. americana and Blastocerus dichotomus, all currently living in South America, the two first in the region. A grand total of more than one hundred remains demonstrates the presence of Mazama gouazoubira in seven sites, mainly the Toca das Moendas, the Toca do Serrote do Artur, the Toca da Cima dos Pilão. This small species shows, since the Upper Pleistocene, a conspicuous tendency to reduce the average dimensions of its teeth and long bones. From the taller M. americana, only a dozen of remains were found in four sites, mainly the Sitio do Meio. In all of these it is sympatric with M. gouazoubira. It differs from this last one by its cheek teeth and its limb bones size and proportions. The oldest site where the species is known is Tarija (Bolivia, Middle Pleistocene) and it does not show any significant changes in size and proportions between recent and fossil samples. Sixteen remains of the large B. dichotomus were found in five sites, mainly the Toca das Moendas and the Toca da Barra do Antonião. The species is a rare fossil, but is frequently figured in the rock art painting of the region, where it is presently unknown.     

Gene regulation in the marine diatom Thalassiosira pseudonana upon exposure to polycyclic aromatic hydrocarbons (PAHs)

Diatoms are eukaryotic algae, which can be found worldwide in oceans and freshwaters. These organisms are ecologically relevant due to their key role in the global carbon cycle, contributing to about 25% to the global primary production [Falciatore, A., Bowler, C., 2002. Revealing the molecular secrets of marine diatoms. Annu. Rev. Plant Biol. 53, 109-130]. We investigated the effects of three polycyclic aromatic hydrocarbons (PAHs, pyrene, fluoranthene, and benzo[a]pyrene), either as single compound or as mixture, at molecular level. Dose-response curves for growth inhibition were determined and four concentrations eliciting from "no effect" up to a severe growth inhibition were chosen for further investigation to detect alterations at gene expression level by Real-Time PCR. Among the eight selected genes, two were strongly influenced by the PAH treatment. lacsA, which is involved in the fatty acid metabolism, was found to be strongly up-regulated by all single PAHs, as well as by the mixture. sil3, involved in the formation of the silica shell, was repressed by a factor up to three even at low PAH concentrations not eliciting any growth inhibition. For other genes, involved e.g. in photosynthesis, a slight down-regulation was detected. Based on the effects at gene expression level it can be assumed that PAHs impair the fatty acid metabolism and silica shell formation.     

Les kystes de dinoflagellés du Crétacé moyen de la marge atlantique brésilienne, le bassin de Santos

Organic dinoflagellate cysts are studied from the sedimentary sequence of hole 1-SPS-14A, drilled during oil exploration in the Santos Basin, Brazilian continental margin. The Ariri and Florianópolis Formations (Transitional sequence) do not contain any dinocysts. The oldest found dinocysts occur at the base of the Drift sequence in sediments, within platform carbonates of the Guarujá Formation. Continuous sea-level rise throughout the late Albian and Cenomanian submerged the carbonate platform with the terrigenous input of the Itanhaém Formation. The transgressive phase reached its peak during the Cenomanian/Turonian transition. Pelites were deposited during oceanic anoxic event (OAE-2), consisting the lower part of the Itajaí-Açu Formation. Normal oceanic conditions re-established in the late Turonian. The Brazilian dinocyst assemblage has tethyan affinities. Some species (i.e., Dinopterygium cladoides, Litosphaeridium arundum, Odontochitina rhakodes and Systematophora cretacea) suggest a middle Albian age for the carbonate platform of the Guarujá Formation. The lower part of the Guarujá Formation was not dated by other microfossils. An uppermost Albian or lower Cenomanian age is suggested for the base of the Itanhaém Formation on the basis of species Palaeohystrichophora infusorioides and Ovoidinium verrucosum. The Cenomanian-Turonian boundary cannot be characterized by dinocysts. Species Atopodinium iuvene, which is known from Turonian sediments in Europe, was found at the top of the Itajaí-Açu Formation. The observed dinocyst bioevents (i.e., last occurrence) are correlated with known foraminiferal, nannofossil and other palynological bioevents. The diversity of the assemblages remains constant throughout the various palaeoenvironments as these are reflected by the Guarujá and Itajaí-Açu Formations, but relative abundances of taxa are variable. Genera Coronifera, Florentinia, Ovoidinium, Spiniferites and Trichodinium are abundant in the carbonate platform assemblages (Guarujá Formation). Genera Cribroperidinium and Cyclonephelium are abundant in detrital sediments (Itajaí-Açu Formation). Only one species (Subtilisphaera guarujaensis n. sp.) is restricted to the carbonate platform environment.     

Nouvelles découvertes d'art rupestre au Mato Grosso (Cidade de Pedra, Rondonópolis, Brésil)

Since 1983, Professor Agueda Vilhena-Vialou is conducting in Mato Grosso (Brazil) the French-brasilian archeological mission Fossil men and their paleo-environments in the Paraná basin. Its goal is the study of the first prehistoric settlements of Latin America's heart, in their economic, social, cultural and symbolic dimensions. Thanks to the complementary and comparative analysis of the habitats, the regional settlements and the rock art, our research targets a more precise definition of territories and cultures proper of the prehistoric human groups from the South of the actual Mato Grosso state. The study of rock art, the most revealing aspect of symbolic behaviours, is one of the strongest programs inside our multidisciplinary team. Today, thanks to systematic prospections led along the Rio Vermelho (between Pantanal swamp at West and Rondonópolis city at East), a hundred rock art sites (walls, shelters and caves), decorated with signs, animals and humans, have been discovered, and, for the most of them, studied. These figures are painted, engraved and more rarely sculpted. Along those pages, the author is presenting the preliminary analysis of ten new rock art sites, recently identified in a cliff on the right bank of the Vermelho River. He starts a comparative study with the sites of the Cidade de Pedra and of close micro basin, from the left bank of the River. This research is showing the symbolic identities, both common and specific, proper to different territories of this major rock art region of Brazil, which is divided in several areas and micro territories, shared but autonomous.     

Gleditisioxylon riojana nov. sp. en el Neógeno de Argentina: sus relaciones paleoambientales y biogeográficas

A new fossil species of Leguminosae is described from Neogene of northwest of Argentina. The good preservation of tissues and the diagnostic characters present in this fossil wood let assigning it to a new species of Gleditisioxylon Müller-Stoll and Madel. Gleditisioxylon riojana nov. sp. (Caesalpinoideae) has diagnostic features such as: growth rings distinct, semi-annular porosity, vestured pits, helical thickenings, simple plates, paratracheal parenchyma and rays 1-6 seriate. The possible climatic conditions of Toro Negro Formation were inferred by the use of xylological characters presents in this fossil wood. The presence of Gleditsioxylon added to other data, suggest a new hypothesis to explain the disjunction of Gleditsia L. genus and the occurrence of a single extant species in tropical and subtropical South America.