Petrology and chemistry of ODP Site 134-828 magmatic rocks

Petrography, major and trace elements, mineral chemistry, and Sr, Nd, and Pb isotopic ratios are reported for igneous rocks drilled on the northern flank of the North d'Entrecasteaux Ridge (NDR) during Ocean Drilling Program (ODP) Leg 134 Site 828. These rocks comprise a breccia unit beneath a middle Eocene foraminiferal ooze. Both geophysical characteristics and the variety of volcanic rocks found at the bottom of Holes 828A and 828B indicate that a very immature breccia or scree deposit was sampled. Basalts are moderately to highly altered, but primary textures are well preserved. Two groups with different magmatic affinities, unrelated to the stratigraphic height, have been distinguished. One group consists of aphyric to sparsely plagioclase + clinopyroxene-phyric basalts, characterized by high TiO2 (~2 wt%) and low Al2O3 (less than 15 wt%) contents, with flat MORB-normalized incompatible element patterns and LREE-depleted chondrite-normalized REE patterns. This group resembles N-MORB. The other group comprises moderately to highly olivine + plagioclase-phyric basalts with low TiO2 (<1 wt%) and high Al2O3 (usually >15 wt%) contents, and marked HFSE depletion and LFSE enrichment. Some lavas in this group are picritic, with relatively high modal olivine abundances, and MgO contents up to 15 wt%. Both the basalts and picritic basalts of this group reflect an influence by subduction-related processes, and have compositions transitional between MORB and IAT. Lavas with similar geochemical features have been reported from small back-arc basins such as the Mariana Trough, Lau Basin, Sulu Sea, and the North Fiji Basin and are referred to as back-arc basin basalts. However, regional tectonic considerations suggest that the spreading that produced these backarc basin basalts may have occurred in the forearc region of the southwest-facing island arc that existed in this region in the Eocene.

Características clínico-evolutivas de 134 pacientes com histoplasmose disseminada associada a SIDA no Estado do Ceará

INTRODUÇÃO: Desde o início da epidemia de HIV no Ceará, histoplasmose disseminada tem sido detectada com frequência em pacientes com aids. MÉTODOS: De modo a conhecer características clínico-laboratoriais, evolução e sobrevida da co-infecção HD/AIDS, analisou-se retrospectivamente 134 prontuários casos de HD internados de 1999 a 2005 no hospital referência para HIV no Ceará. RESULTADOS: Pacientes com HD apresentaram maior frequência de febre diária, tosse, perda de peso, hepatoesplenomegalia e insuficiência renal aguda. Diagnóstico foi dado por pesquisa e/ou cultura. À admissão, foram fatores de risco relacionados ao óbito de pacientes com HD: vômitos, dispnéia, insuficiência respiratória e IRA, hemoglobina<8g/L, uréia>40mg/dL e creatinina >1,5mg/dL. CONCLUSÕES: pacientes com HD apresentaram caracteristicamente febre mais elevada, internamentos anteriores por infecção respiratória, mais complicações clínicas e como fatores independentes para óbito, anemia importante e elevação de uréia.