The objective of the present study was to analyze chondrogenesis and the ossification pattern of the limbs of Melanosuchus niger in order to contribute with possible discussions on homology and the fusion pattern of autopodial elements and phylogeny. In the Reserva Extrativista do Lago Cuniã, Rondônia, Brazil, six nests were marked and two eggs removed from each nest at 24-hour intervals until hatching. Embryos were cleared using KOH; bone tissue was stained with alizarin red S and cartilage with Alcian blue. Routine staining with HE was also performed. In the pectoral girdle, the scapula showed ossification centers before the coracoid process. In the pelvic girdle, the ilium and the ischium were condensed as a single cartilage, although ossification took place through two separate centers, forming distinct elements in the adult. The pubis developed from an independent cartilaginous center with free end, which reflects its function in breathing. In the initial stages, the stylopodium and the zeugopodium developed from the condensation of a Y-shaped cartilage in the limbs, and differentiation of the primary axis and digital arch were observed. The greatest changes were observed in the mesopodia. In their evolution, Crocodylia underwent a vast reduction in the number of autopodial elements as a consequence of fusions and ossification of some elements. This study shows that the chondrogenesis and ossification sequences are dissociated. Moreover, the differences between M. niger and other species show clear variation in the patterns for these events in Alligatoridae.

Palavras-chave: Formação Barreiras, sistemas deposicionais, caracterização faciológica. RESUMOAo longo da costa brasileira são encontrados depósitos sedimentares atribuídos à Formação Barreiras. No Rio Grande do Norte, estes depósitos ocorrem principalmente na linha de costa, tendo como melhor exemplo a Barreira do Inferno, um afloramento com mais de 1 km de extensão e até 20 m de espessura, situado no município de Parnamirim (RN). As associações de fácies descritas foram interpretadas como indicativas da deposição em um contexto fluvial, sendo as de granulação mais grossa relacionadas a depósitos de preenchimento de canais e as de textura mais fina, atribuídas a depósitos de planície de inundação. Estes depósitos mostram lateralmente uma clara diminuição da proporção entre arenitos e conglomerados versus lamitos. Na região que foi interpretada como a porção mais central de um suposto cinturão fluvial, a sucessão apresenta quase 80% de arenitos e conglomerados, ao passo que, lateralmente, a menos de 200 m, chega a ter 40% de rochas de granulação mais fina, o que sugere a proximidade da planície de inundação. Apesar de o sistema fluvial interpretado apresentar algumas características de um sistema entrelaçado, a abundância de fácies pelíticas, bem como a ocorrência freqüente de estratos com geometria de preenchimento de canais, permite estabelecer uma maior aproximação a um sistema fluvial meandrante. Considerando esses aspectos, o modelo "Meandrante de Granulometria Grossa" é o que melhor representa estes depósitos.Keywords: Barreiras Formation, fluvial systems, facies analysis. ABSTRACTThe Barreiras Formation is composed of sedimentary siliciclastic rocks that crop out at the continental scale along the Brazilian coastline from the State of Rio de Janeiro to the State of Amapá. In the State of Rio Grande do Norte, this formation is well exposed in cliffs along the coastline, best represented by the Barreira do Inferno cliff, which is 1 km long and 20 m high. Facies characterization and interpretation of depositional systems of the Barreiras Formation in this cliff were based on stratigraphic columnar sections and digital photomosaics. The Barreira do Inferno cliff comprises a large area affording continuous exposure of bed geometries, generally tabular in shape with secondary channels filled by mudstones, indicative of a fluvial context. Coarse facies characterize channel environments, whereas fine facies represent flood plains. This interpretation is supported by a lateral decrease in the ration of sandstone/conglomerates versus mudstones along the outcrop. In the central portion of the fluvial belt, sands and conglomerates comprise up to 80% of the deposits. Laterally, in the flood plain, up to 40% of the deposits are mudstones, fine sands, and very fine sands. This system is similar to braided fluvial systems, but the facies association (with pelites) and layer geometries (abandoned channels filled by mudstones) are characteristic of meandering rivers. The model that best explains these deposits is the "coar...

RESUMO.-O objetivo foi realizar a descrição anatômica do esqueleto de Melanosuchus niger, com o intuito de contribuir com informações evolutivas sobre a espécie. Utilizaram-se três espécimes adultos de M. niger, com comprimento médio de 2,40m, provenientes da coleção biológica do Lapas-UFU. Na cintura peitoral, a escápula é maior do que o coracóide. Já nos elementos da cintura pelvina, o púbis não participa da formação do acetábulo, o contato com o ilío, ocorre por ligamentos, e sua articulação com o ísquio, permite movimentos dorso-ventrais. The objective was an anatomical description of the skeleton of Melanosuchus niger, in order to contribute with evolutionary information about the species. Three adult specimens of M. niger with an average length of 2.40m were used, originating from the biologic collection of Lapas-UFU. In the forelimb, the scapula is bigger than the coracoid. Regarding the hindlimbs, the pubic does not participate in the formation of the acetabulum; the contact with the ilium is made by ligaments, and its articulation with the rump allows dorsal-ventral movements. Regarding the forelimbs, the humerus is a stylopodium element, and the ulna and radius a zeugopodium element. The carpus exibits the ulnar-radial+intermedium fusion, fusion of the distal carpals 3+4+5, and the pisiform. It has five metacarpals, numbered lateromedially as metacarpal 1, 2, 3, 4, and 5. The phalangeal formula is 2:3:4:3:2. Regarding the pelvic limbs, the stylopodium is formed by the femur, and the zeugopodium by tibia and fibula. In tarsus has four bones: fusion of the intermedium+centrale, fibulare, distal tarsal 3, and distal tarsal 4. It has four long metatarsals I, II, III and IV, with metatarsal II and III being relatively longer than the others. Metatarsal V is a very small bone; the feet have the phalangeal formula 2:3:4:4. At the skull, the nasal opening is only the palatine bones, vomer, pterygoid, premaxilla and maxilla forming the bone structure of the secondary palate; the parietal bone is the only element on the cranial roof. In the pos-axial skeleton ist distinct pairs of ribs which articulate with the cervical, dorsal, lumbar, sacral and caudal vertebrae. The gastralia consists of seven rows of fine bone located between the pubic bone and caudal part of the sternum.

Lobos pulmonares e formação dos brônquios do gato mourisco