Orlando N. Grillo

Acidocalcisomes of Trypanosomatids have Species-Specific Elemental Composition

The elemental composition and stoichiometric profile of elements present in acidocalcisomes of different genera of the Trypanosomatidae family (insect, plant, and mammalian parasites) submitted to parallel cultivation conditions were studied. X-ray microanalysis using transmission electron microscopy in conjunction with a morphometric approach was used to investigate the elemental content, number, distribution, and volumetric density of acidocalcisomes of different species. Microanalytical data showed that the different parasites possess the same elemental composition (oxygen, sodium, magnesium, phosphorus, calcium, iron, and zinc) in their acidocalcisomes. However, the relative concentrations of the elements varied among species, but not within acidocalcisomes of individual species. Iron was detected in acidocalcisomes of all species analyzed, characterizing this element as a constituent of these organelles. Taken together, the results strongly indicate a species-specific composition of acidocalcisomes in trypanosomatid parasites.

The oldest plesiosaur (Reptilia, Sauropterygia) from Antarctica

Antarctic plesiosaurs are known from the Upper Cretaceous López de Bertodano and Snow Hill Island formations (Campanian to upper Maastrichtian), which crop out within the James Ross Basin region of the Antarctic Peninsula. Here we describe the first plesiosaur fossils from the Lachman Crags Member of the Santa Marta Formation, north-western James Ross Island. This material constitutes the stratigraphically oldest plesiosaur occurrence presently known from Antarctica, extending the occurrence of plesiosaurians in this continent back to Santonian times (86.3–83.5 Mya). Furthermore, MN 7163-V represents the first plesiosaur from this region not referable to the Elasmosauridae nor Aristonectes, indicating a greater diversity of this group of aquatic reptiles in Antarctica than previously suspected.

Pelvic and hind limb musculature of Staurikosaurus pricei (Dinosauria: Saurischia)

The study of pelvic and hind limb bones and muscles in basal dinosaurs is important for understanding the early evolution of bipedal locomotion in the group. The use of data from both extant and extinct taxa placed into a phylogenetic context allowed to make well-supported inferences concerning most of the hind limb musculature of the basal saurischian Staurikosaurus pricei Colbert, 1970 (Santa Maria Formation, Late Triassic of Rio Grande do Sul, Brazil). Two large concavities in the lateral surface of the ilium represent the origin of the muscles iliotrochantericus caudalis plus iliofemoralis externus (in the anterior concavity) and iliofibularis (in the posterior concavity). Muscle ambiens has only one head and originates from the pubic tubercle. The origin of puboischiofemoralis internus 1 possibly corresponds to a fossa in the ventral margin of the pré-acetabular iliac process. This could represent an intermediate stage prior to the origin of a true pré-acetabular fossa. Muscles caudofemorales longus et brevis were likely well developed, and Staurikosaurus is unique in bearing a posteriorly projected surface for the origin of caudofemoralis brevis.

Recovering missing data: estimating position and size of caudal vertebrae in Staurikosaurus pricei Colbert, 1970

Missing data is a common problem in paleontology. It makes it difficult to reconstruct extinct taxa accurately and restrains the inclusion of some taxa on comparative and biomechanical studies. Particularly, estimating the position of vertebrae on incomplete series is often non-empirical and does not allow precise estimation of missing parts. In this work we present a method for calculating the position of preserved middle sequences of caudal vertebrae in the saurischian dinosaur Staurikosaurus pricei, based on the length and height of preserved anterior and posterior caudal vertebral centra. Regression equations were used to estimate these dimensions for middle vertebrae and, consequently, to assess the position of the preserved middle sequences. It also allowed estimating these dimensions for non-preserved vertebrae. Results indicate that the preserved caudal vertebrae of Staurikosaurus may correspond to positions 1-3, 5, 7, 14-19/15-20, 24-25/25-26, and 29-47, and that at least 25 vertebrae had transverse processes. Total length of the tail was estimated in 134 cm and total body length was 220-225 cm.

Biomechanical comments about Triassic dinosaurs from Brazil

Triassic dinosaurs of Brazil are found in Santa Maria and Caturrita formations, Rio Grande do Sul state, Brazil. There are three species known from the Santa Maria Formation (Staurikosaurus pricei, Saturnalia tupiniquim and Pampadromaeus barberenai), and two from Caturrita Formation (Guaibasaurus candelariensis and Unaysaurus tolentinoi). These dinosaur materials are, for the most part, well preserved and allow for descriptions of musculature and biomechanical studies. The lateral rotation of the Saturnalia femur is corroborated through calculations of muscle moment arms. The enhanced supracetabular crest of Saturnalia, Guaibasaurus, Staurikosaurus, Herrerasaurus ischigualastensis, Efraasia minor and Chormogisaurus novasi suggests that basal dinosaurs may have maintained an inclination of the trunk at least 20o on the horizontal axis. The pectoral girdle articulation of basal sauropodomorphs (Saturnalia and Unaysaurus) was established using a new method, the Clavicular Ring, and the scapular blade remains near 60o on the horizontal axis. This is a plesiomorphic condition among sauropodomorphs and is also seen in the articulated plateosauridae Seitaad ruessi. The Brazilian basal dinosaurs were lightweight with a body mass estimated around 18.5 kg for Staurikosaurus, 6.5 kg for Saturnalia, and 17 kg for Guaibasaurus. Pampadromaeus probably weighed 2.5 kg, but measures of its femur are necessary to confirm this hypothesis. The Triassic dinosaurs from Brazil were diversified but shared some functional aspects that were important in an evolutionary context.

Following the Footsteps of the South American Equus : Are Autopodia Taxonomically Informative?

The genus Equus originated in the Pliocene Epoch of North America, and its arrival in South America is likely related to the Great American Biotic Interchange that took place in the transition of Pliocene to Pleistocene. Currently, there are five recognized species for the South American continent: Equus neogeus, E. santaeelenae, E. insulatus, E. andium, and E. lasallei. The taxonomy of the genus is traditionally based in part upon the proportions of the autopodia. The aim of this study is to evaluate the diagnostic importance of the autopodia of South American Equus through comparative and multiple statistical analyses. Therefore, we analyzed metacarpals, metatarsals, and phalanges from all available South American Equus, with the exception of E. lasallei, which is only known by a skull. We also examined the North American species E. occidentalis, as it has been interpreted to be closely related to South American Equus. Results showed no significant differences between the various South American species according to the dimensions and proportions of the autopodia. A continuum of gradual linear variation among the species was revealed, with superimposition between autopodial characters. The succession and overlap of species indicated that the South American Equus might represent a type of cline.

Comentários sobre o artigo modelagem 3D e suas aplicações na pesquisa paleontológica

Reconstrucoes virtuais tridimensionais sao uma ponderosa ferramenta para pesquisa paleontologica e para entretenimento em educacao. Os metodos e tecnologias disponiveis foram revisados por Dardon et al. (2010), fornecendo uma introducao as tecnicas de obtencao de imagens 3D. Entretanto, algumas informacoes apresentadas no referido trabalho apresentam inconsistencias que sao discutidas aqui. Palavras-chave: paleontologia, modelos 3D, Shape-from-silhouette, scanner 3D, divulgacao cientifica.