4 resultados para Cu(II) complex
em Universidad Politécnica de Madrid
Resumo:
In this work, electrochemical maltose biosensors based on mutants of the maltose binding protein (MBP) are developed. A ruthenium II complex (Ru II ), which is covalently attached to MBP, serves as an electrochemical reporter of MBP conformational changes. Biosensors were made through direct attachment of Ru II complex modified MBP to gold electrode surfaces. The responses of some individual mutants were evaluated using square wave voltammetry. A maltose-dependent change in Faradic current and capacitance was observed. It is therefore demonstrated that biosensors using generically this family of bacterial periplasmic binding proteins (bPBP) can be made lending themselves to facile biorecognition element preparation and low cost electrochemical transduction.
Resumo:
A gene encoding a homolog to the cation diffusion facilitator protein DmeF from Cupriavidus metallidurans has been identified in the genome of Rhizobium leguminosarum UPM791. The R. leguminosarum dmeF gene is located downstream of an open reading frame (designated dmeR) encoding a protein homologous to the nickel- and cobalt-responsive transcriptional regulator RcnR from Escherichia coli. Analysis of gene expression showed that the R. leguminosarum dmeRF genes are organized as a transcriptional unit whose expression is strongly induced by nickel and cobalt ions, likely by alleviating the repressor activity of DmeR on dmeRF transcription. An R. leguminosarum dmeRF mutant strain displayed increased sensitivity to Co(II) and Ni(II), whereas no alterations of its resistance to Cd(II), Cu(II), or Zn(II) were observed. A decrease of symbiotic performance was observed when pea plants inoculated with an R. leguminosarum dmeRF deletion mutant strain were grown in the presence of high concentrations of nickel and cobalt. The same mutant induced significantly lower activity levels of NiFe hydrogenase in microaerobic cultures. These results indicate that the R. leguminosarum DmeRF system is a metal-responsive efflux mechanism acting as a key element for metal homeostasis in R. leguminosarum under free-living and symbiotic conditions. The presence of similar dmeRF gene clusters in other Rhizobiaceae suggests that the dmeRF system is a conserved mechanism for metal tolerance in legume endosymbiotic bacteria.
Resumo:
Los suelos ultramáficos, que poseen elevadas concentraciones de níquel, cobalto y cromo de manera natural, son fuente de bacterias resistentes a altas concentraciones de metales. Se realizó la caracterización físico-química de seis suelos ultramáficos del suroeste europeo, seleccionándose un suelo de la región de Gorro, Italia, como el más adecuado para aislar bacterias endosimbióticas resistentes a metales. A partir de plantas-trampa de guisante y lenteja inoculados con suspensiones de ese suelo, se obtuvieron 58 aislados de Rhizobium leguminosarum bv. viciae (Rlv) que fueron clasificados en 13 grupos según análisis de PCR-RAPDs. Se determinó la resistencia a cationes metálicos [Ni(II), Co(II), Cu(II), Zn(II)] de una cepa representante de cada grupo, así como la secuencia de los genomas de las cepas que mostraron altos niveles (UPM1137 y UPM1280) y bajos niveles (UPM1131 y UPM1136) de tolerancia a metales. Para identificar mecanismos de resistencia a metales se realizó una mutagénesis al azar en dicha cepa mediante la inserción de un minitransposón. El análisis de 4313 transconjugantes permitió identificar 14 mutantes que mostraron una mayor sensibilidad a Ni(II) que la cepa silvestre. Se determinó el punto de inserción del minitransposón en todos ellos y se analizaron en más detalle dos de los mutantes (D2250 y D4239). En uno de los mutantes (D2250), el gen afectado codifica para una proteína que presenta un 44% de identidad con dmeF (divalent efflux protein) de Cupriavidus metallidurans. Cadena arriba de dmeF se identificó un gen que codifica una proteína con un 39% de identidad con el regulador RcnR de Escherichia coli. Se decidió nombrar a este sistema dmeRF, y se generó un mutante en ambos genes en la cepa Rlv SPF25 (Rlv D15). A partir de experimentos de análisis fenotípico y de regulación se pudo demostrar que el sistema dmeRF tiene un papel relevante en la resistencia a Ni(II) y sobre todo a Co(II) en células en vida libre y en simbiosis con plantas de guisante. Ambos genes forman un operón cuya expresión se induce en respuesta a la presencia de Ni(II) y Co(II). Este sistema se encuentra conservado en distintas especies del género Rhizobium como un mecanismo general de resistencia a níquel y cobalto. Otro de los mutantes identificados (D4239), tiene interrumpido un gen que codifica para un regulador transcripcional de la familia AraC. Aunque inicialmente fue identificado por su sensibilidad a níquel, experimentos posteriores demostraron que su elevada sensibilidad a metales era debida a su sensibilidad al medio TY, y más concretamente a la triptona presente en el medio. En otros medios de cultivo el mutante no está afectado específicamente en su tolerancia a metales. Este mutante presenta un fenotipo simbiótico inusual, siendo inefectivo en guisantes y efectivo en lentejas. Análisis de complementación y de mutagénesis dirigida sugieren que el fenotipo de la mutación podría depender de otros factores distintos del gen portador de la inserción del minitransposón. ABSTRACT Ultramafic soils, having naturally high concentrations of nickel, cobalt and chrome, are potential sources of highly metal-resistant bacteria. A physico-chemical characterization of six ultramafic soils from the European southwest was made. A soil from Gorro, Italy, was chosen as the most appropriated for the isolation of heavy-metal-resistant endosymbiotic bacteria. From pea and lentil trap plants inoculated with soil suspensions, 58 isolates of Rhizobium leguminosarum bv. viciae (Rlv) were obtained and classified into 13 groups based on PCR-RAPDs analysis. The resistance to metallic cations [Ni(II), Co(II), Cu(II), Zn(II)] was analyzed in a representative strain of each group. From the results obtained in the resistance assays, the Rlv UPM1137 strain was selected to identify metal resistance mechanism. A random mutagenesis was made in UPM1137 by using minitransposon insertion. Analysis of 4313 transconjugants allowed to identify 14 mutants with higher sensitivity to Ni(II) than the wild type strain. The insertion point of the minitransposon was determined in all of them, and two mutants (D2250 and D4239) were studied in more detail. In one of the mutants (D2250), the affected gene encodes a protein with 44% identity in compared with DmeF (divalent efflux protein) from Cupriavidus metallidurans. Upstream R. leguminosarum dmeF, a gene encoding a protein with 39% identity with RcnR regulator from E. coli was identified. This protein was named DmeR. A mutant with both genes in the dmeRF deleted was generated and characterized in Rlv SPF25 (Rlv D15). From phenotypic and regulation analysis it was concluded that the dmeRF system is relevant for Ni(II) and specially Co(II) tolerance in both free living and symbiotic forms of the bacteria. This system is conserved in different Rhizobium species like a general mechanism for nickel and cobalt resistance. Other of the identified mutants (D4239) contains the transposon insert on a gene that encodes for an AraC-like transcriptional regulator. Although initially this mutant was identified for its nickel sensitivity, futher experiments demonstrated that its high metal sensitivity is due to its sensitivity to the TY medium, specifically for the tryptone. In other media the mutant is not affected specifically in their tolerance to metals. This mutant showed an unusual symbiotic phenotype, being ineffective in pea and effective in lentil. Complementation analysis and directed mutagenesis suggest that the mutation phenotype could depend of other factors different from the insertion minitransposon gene.
Resumo:
As a result of the variscan collision, several allochtonous complexes were emplaced on the Iberian margin in Devonian times, among them the Cabo Ortegal Complex comprising the Moeche ophiolitic sequence. Copper has been won from several mines (Piquitos I & II, Barqueira, Maruxa) from disseminated ores and thin massive sulphide layers in the Moeche Unit, a strongly deformed meta-volcanic sequence comprising mainly quartz-chlorite schists and mylonites, which defines the top of the ophiolite. The ores were metamorphosed and strongly deformed under brittle conditions (for pyrite), but their textures are often apparently post-deformational, due to very common solution-transfer processes; they are composed mostly of pyrite and chalcopyrite, with minor sphalerite, pyrrhotite, etc., and with traces of native gold and PGE. The geology, mineralogy, and geochemistry of the orebodies relate closely to VMS of the Cu-Zn (Cyprus) type. Fluid inclusion studies allowed an estimation of metamorphic conditions at pressures of 2/2’5 kb and T 325/350ºC. New determinations using the chlorite geothermometer yield temperatures around 320 ºC, corresponding to pressures near 2 kb according to the isochores deduced from the fluid inclusion study, although in the Barqueira mine higher temperatures, up to 350 ºC, are found, corresponding to presssures up to 2’5 kb. Pb isotopic compositions of pyrite point to a double source of Pb, i.e. a main mantle and a subordinate crustal source. The values for 87SR/86Sr in pyrite support this interpretation, but some results suggest later mobilization in an open system, corresponding to solution-transfer. Age determinations of pyrite deduced from the Pb isotope uranogenic graph, ≈ 480 Ma, do not fit with the metamorphic ages published for the Moeche Unit, and might point to the age of Pb extraction from the mantle.