The incidence of necrotizing changes in adults with pneumococcal pneumonia

Background. Necrotizing pneumonia is generally considered a rare complication of pneumococcal pneumonia in adults. We systematically studied the incidence of necrotizing changes in adult patients with pneumococcal pneumonia, and examined the severity of infection, the role of causative serotype and the association with bacteremia. ^ Methods. We used a data base of all pneumococcal infections identified at our medical center between 2000 and 2010. Original readings of chest X-rays (CXR) and computerized tomography (CT) were noted. All images were then reread independently by 2 radiologists. The severity of disease was assessed using the SMART-COP scoring system. ^ Results. There were 351 cases of pneumococcal pneumonia. Necrosis was reported in no original CXR readings and 6 of 136 (4.4%) CTs. With re-reading, 8 of 351 (2.3%) CXR and 15 of 136 (11.0%) CT had necrotizing changes. Overall, these changes were found in 23 of 351 (6.6%, 95% CI 4.0 - 9.1) patients. The incidence of bacteremia and the admitting SMART-COP scores were similar in patients with and without necrosis (P=1.00 and P=0.32, respectively). Type 3 pneumococcus was more commonly isolated from patients with than from patients without necrotizing pneumonia (P=0.05), but a total of 10 serotypes were identified among 16 cases in which the organism was available for typing. ^ Conclusions. Necrotizing changes in the lungs were seen in 6.6% (95% CI 4.0 - 9.1) of a large series of adults with pneumococcal pneumonia. Patients with necrosis were not more likely to have bacteremia or more severe disease. Type 3 pneumococcus was commonly implicated, but 9 other serotypes were also identified.^

The yeast STM1 protein binds G*G multiplex nucleic acids in vitro and associates with ribosomes in vivo

The formation of triple helical, or triplex DNA has been suggested to occur in several cellular processes such as transcription, replication, and recombination. Our laboratory previously found proteins in HeLa nuclear extracts and in S. cerevisiae whole cell extracts that avidly bound a Purine-motif (Pu) triplex probe in gel shift assays, or EMSA. In order to identify a triplex DNA-binding protein, we used conventional and affinity chromatography to purify the major Pu triplex-binding protein in yeast. Peptide microsequencing and data base searches identified this protein as the product of the STM1 gene. Confirmation that Stm1p is a Pu triplex-binding protein was obtained by EMSA using both recombinant Stm1p and whole cell extracts from stm1Δ yeast. Stm1p had previously been identified as G4p2, a G-quartet DNA- and RNA-binding protein. To study the cellular role and identify the nucleic acid ligand of Stm1p in vivo, we introduced an HA epitope at either the N- or C-terminus of Stm1p and performed immunoprecipitations with the HA.11 mAb. Using peptide microsequencing and Northern analysis, we positively identified a subset of both large and small subunit ribosomal proteins and all four rRNAs as associating with Stm1p. DNase I treatment did not affect the association of Stm1p with ribosomal components, but RNase A treatment abolished the association with all ribosomal proteins and RNA, suggesting this association is RNA-dependent. Sucrose gradient fractionation followed by Western and EMSA analysis confirmed that Stm1p associates with intact 80S monosomes, but not polysomes. The presence of additional, unidentified RNA in the Stm1p-immunoprecipitate, and the absence of tRNAs and elongation factors suggests that Stm1p binds RNA and could be involved in the regulation of translation. Immunofluorescence microscopy data showed Stm1p to be located throughout the cytoplasm, with a specific movement to the bud during the G2 phase of the cell cycle. A dramatically flocculent, large cell phenotype is observed when Stm1p has a C-terminal HA tag in a protease-deficient strain background. When STM1 is deleted in this background, the same phenotype is not observed and the deletion yeast grow very slowly compared to the wild-type. These data suggest that STM1 is not essential, but plays a role in cell growth by interacting with an RNP complex that may contain G*G multiplex RNA. ^

Age analysis, aragonite and high magnesium calcite content from different IODP Holes from Exp 310

The widespread occurrence of microbialites in the last deglacial reef frameworks (16-6 Ka BP) implies that the accurate study of their development patterns is of prime importance to unravel the evolution of reef architecture through time and to reconstruct the reef response to sea-level variations and environmental changes. The present study is based on the sedimentological and chronological analysis (14C AMS dating) of drill cores obtained during the IODP Expedition #310 "Tahiti Sea Level" on the successive terraces which typify the modern reef slopes from Tahiti. It provides a comprehensive data base to investigate the microbialite growth patterns (i.e. growth rates and habitats), to analyze their roles in reef frameworks and to reconstruct the evolution of the reef framework architecture during sea-level rise. The last deglacial reefs from Tahiti are composed of two distinctive biological communities: (1) the coralgal communities including seven assemblages characterized by various growth forms (branching, robust branching, massive, tabular and encrusting) that form the initial frameworks and (2) the microbial communities developed in the primary cavities of those frameworks, a few meters (1.5 to 6 m) below the living coral reef surface, where they heavily encrusted the coralgal assemblages to form microbialite crusts. The dating results demonstrate the occurrence of two distinctive generations of microbialites: the "reefal microbialites" which developed a few hundred years after coralgal communities in shallow-water environments, whereas the "slope microbialites" grew a few thousands of years later in significantly deeper water conditions after the demise of coralgal communities. The development of microbialites was controlled by the volume and the shape of the primary cavities of the initial reef frameworks determined by the morphology and the packing of coral colonies. The most widespread microbialite development occurred in frameworks dominated by branching, thin encrusting, tabular and robust branching coral colonies which built loose and open frameworks typified by a high porosity (> 50%). In contrast, their growth was minimal in compact coral frameworks formed by massive and thick encrusting corals where primary cavities yielded a low porosity (~ 30%) and could not host a significant microbialite expansion.