First report of the blaOXA-58 gene in a clinical isolate of Acinetobacter baumannii in Rio de Janeiro, Brazil

Carbapenemase production is an important mechanism of carbapenem resistance among nonfermentative Gram-negative isolates. This study aimed to report the detection of blaOXA-58 gene in multiresistant clinical isolates of Acinetobacter baumannii recovered from inpatients in a public hospital. Polymerase chain reaction tests were performed to detect the blaOXA-23-like, blaOXA-24-like, blaOXA-58-like and blaOXA-51-like genes. The blaOXA-58 and blaOXA-23 genes were detected in one and three isolates, respectively. Sequencing of the blaOXA-58-like amplicon revealed 100% identity with the A. baumannii blaOXA-58 gene listed in the GenBank database. This is the first report of an OXA-58-producing A. baumannii isolate in Rio de Janeiro, Brazil

A spatial approach for the epidemiology of antibiotic use and resistance in community-based studies: the emergence of urban clusters of Escherichia coli quinolone resistance in Sao Paulo, Brasil

Copyright © Kiffer et al; licensee BioMed Central Ltd. 2011 This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/2.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.Background Population antimicrobial use may influence resistance emergence. Resistance is an ecological phenomenon due to potential transmissibility. We investigated spatial and temporal patterns of ciprofloxacin (CIP) population consumption related to E. coli resistance emergence and dissemination in a major Brazilian city. A total of 4,372 urinary tract infection E. coli cases, with 723 CIP resistant, were identified in 2002 from two outpatient centres. Cases were address geocoded in a digital map. Raw CIP consumption data was transformed into usage density in DDDs by CIP selling points influence zones determination. A stochastic model coupled with a Geographical Information System was applied for relating resistance and usage density and for detecting city areas of high/low resistance risk. Results E. coli CIP resistant cluster emergence was detected and significantly related to usage density at a level of 5 to 9 CIP DDDs. There were clustered hot-spots and a significant global spatial variation in the residual resistance risk after allowing for usage density. Conclusions There were clustered hot-spots and a significant global spatial variation in the residual resistance risk after allowing for usage density. The usage density of 5-9 CIP DDDs per 1,000 inhabitants within the same influence zone was the resistance triggering level. This level led to E. coli resistance clustering, proving that individual resistance emergence and dissemination was affected by antimicrobial population consumption

Modern and fossil non-pollen palynomorphs from the Basque mountains (western Pyrenees, France): the use of coprophilous fungi to reconstruct pastoral activity

International audienceThis paper presents results from a modern dataset of non-pollen palynomorphs and its application to aca. 2,000 year peat record from the same area in the western Pyrenees (Basque Country, France). The modern dataset is composed of 35 surface samples (moss polsters) from a mountainous pasture-woodland landscape. Airborne fungal spores (ascospores and conidia), found dominant in the dataset, are linked to the degree of landscape openness and grazing pressure. The complete spectrum of 13 selected spore-types of dung-related Ascomycetes is positively linked with grazing pressure. However, different dung affinities between the spore-types have been identified. These are types clearly related to high grazing pressure and types with no or unclear dung indicative value. The modern dataset is used to aid interpretation of the local fossil pollen record as an independent 'proxy' to assess past pastoral dynamics. This study confirms the utility of modern nonpollen palynomorphs from terrestrial ecosystems in the reconstruction of historical local pastoral activities but also shows their limitation. It may be necessary to extend such study to wetland ecosystems and to investigate the spatial dimension of some fungal spores

Functional Significance of Calcium Binding to Tissue-Nonspecific Alkaline Phosphatase

<div><p>The conserved active site of alkaline phosphatases (AP) contains catalytically important Zn²⁺ (M1 and M2) and Mg²⁺-sites (M3) and a fourth peripheral Ca²⁺ site (M4) of unknown significance. We have studied Ca²⁺ binding to M1-4 of tissue-nonspecific AP (TNAP), an enzyme crucial for skeletal mineralization, using recombinant TNAP and a series of M4 mutants. Ca²⁺ could substitute for Mg²⁺ at M3, with maximal activity for Ca²⁺/Zn²⁺-TNAP around 40% that of Mg²⁺/Zn²⁺-TNAP at pH 9.8 and 7.4. At pH 7.4, allosteric TNAP-activation at M3 by Ca²⁺ occurred faster than by Mg²⁺. Several TNAP M4 mutations eradicated TNAP activity, while others mildly influenced the affinity of Ca²⁺ and Mg²⁺ for M3 similarly, excluding a catalytic role for Ca²⁺ in the TNAP M4 site. At pH 9.8, Ca²⁺ competed with soluble Zn²⁺ for binding to M1 and M2 up to 1 mM and at higher concentrations, it even displaced M1- and M2-bound Zn²⁺, forming Ca²⁺/Ca²⁺-TNAP with a catalytic activity only 4–6% that of Mg²⁺/Zn²⁺-TNAP. At pH 7.4, competition with Zn²⁺ and its displacement from M1 and M2 required >10-fold higher Ca²⁺ concentrations, to generate weakly active Ca²⁺/Ca²⁺-TNAP. Thus, in a Ca²⁺-rich environment, such as during skeletal mineralization at pH 7.4, Ca²⁺ adequately activates Zn²⁺-TNAP at M3, but very high Ca²⁺ concentrations compete with available Zn²⁺ for binding to M1 and M2 and ultimately displace Zn²⁺ from the active site, virtually inactivating TNAP. Those <i>ALPL</i> mutations that substitute critical TNAP amino acids involved in coordinating Ca²⁺ to M4 cause hypophosphatasia because of their 3D-structural impact, but M4-bound Ca²⁺ is catalytically inactive. In conclusion, during skeletal mineralization, the building Ca²⁺ gradient first activates TNAP, but gradually inactivates it at high Ca²⁺ concentrations, toward completion of mineralization.</p></div