9 research outputs found
A Nomenclature for Vertebral Fossae in Sauropods and Other Saurischian Dinosaurs
The axial skeleton of extinct saurischian dinosaurs (i.e., theropods, sauropodomorphs), like living birds, was pneumatized by epithelial outpocketings of the respiratory system. Pneumatic signatures in the vertebral column of fossil saurischians include complex branching chambers within the bone (internal pneumaticity) and large chambers visible externally that are bounded by neural arch laminae (external pneumaticity). Although general aspects of internal pneumaticity are synapomorphic for saurischian subgroups, the individual internal pneumatic spaces cannot be homologized across species or even along the vertebral column, due to their variability and absence of topographical landmarks. External pneumatic structures, in contrast, are defined by ready topological landmarks (vertebral laminae), but no consistent nomenclatural system exists. This deficiency has fostered confusion and limited their use as character data in phylogenetic analysis.We present a simple system for naming external neural arch fossae that parallels the one developed for the vertebral laminae that bound them. The nomenclatural system identifies fossae by pointing to reference landmarks (e.g., neural spine, centrum, costal articulations, zygapophyses). We standardize the naming process by creating tripartite names from “primary landmarks,” which form the zygodiapophyseal table, “secondary landmarks,” which orient with respect to that table, and “tertiary landmarks,” which further delineate a given fossa.The proposed nomenclatural system for lamina-bounded fossae adds clarity to descriptions of complex vertebrae and allows these structures to be sourced as character data for phylogenetic analyses. These anatomical terms denote potentially homologous pneumatic structures within Saurischia, but they could be applied to any vertebrate with vertebral laminae that enclose spaces, regardless of their developmental origin or phylogenetic distribution
Hospitais: espaços de cura e lugares de memória da saúde
O presente artigo pretende analisar o Hospital Gaffrée e Guinle, construído na década de 1920, na cidade do Rio de Janeiro, em um processo de tomada de controle, pela administração pública, da gestão da assistência hospitalar na capital federal. Esse hospital representa o encontro da filantropia com um projeto de saúde pública posto em prática no Distrito Federal à mesma época. A instituição sintetiza também o desenvolvimento da medicina e sua tradução na arquitetura hospitalar, bem como a efervescência intelectual do período, mais especificamente das idéias nacionalistas, interpretadas tanto na escolha do estilo arquitetônico - o neocolonial - quanto na questão da salvação da raça através do combate e controle da sífilis.This paper analyzes the Gaffrée & Guinle Hospital, built in Rio de Janeiro during the 1920s as the result of a process whereby the government took over the management of hospital care in the federal capital. The hospital is the point of convergence between philanthropy and a public healthcare project implemented in the Federal District at that time. It also synthesizes the development of medicine and how the latter translates into hospital architecture, as well as the intellectual effervescence at the time, more specifically the nationalist ideas which can be identified both in the choice of architectural style - namely the neocolonial - and in the theme of salvation of a race through the combat and control of syphilis
In situ DIC method to determine stress state in reinforced concrete structures
International audienc
Vertical profile of stratospheric ozone by lidar sounding from the ground
International audienceLIDAR measurements of stratospheric ozone by differential absorption (DIAL) technique were taken during July 1977 at the Haute-Provence Observatory (44N). A frequency doubled rhodamine 6G dye laser provided an output energy of 20–40 mJ in the wavelength range 300–310 nm. We report here preliminary measurements of stratospheric ozone in the altitude range 18–25 km. This experiment was carried out with the lidar facility previously used for the study of upper atmospheric metallic constituents at the mesopause level