Microbial uranium immobilization independent of nitrate reduction.

At many uranium processing and handling facilities, including sites in the US Department of Energy (DOE) complex, high levels of nitrate are present as co-contamination with uranium in groundwater. The daunting prospect of complete nitrate removal prior to the reduction of uranium provides a strong incentive to explore bioremediation strategies that allow for uranium bioreduction and stabilization in the presence of nitrate. Typical in situ strategies involving the stimulation of metal-reducing bacteria are hindered by low-pH environments and require that the persistent nitrate must first and continuously be removed or transformed prior to uranium being a preferred electron acceptor. This work investigated the possibility of stimulating nitrate-indifferent, pH-tolerant microorganisms to achieve bioreduction of U(VI) despite nitrate persistence. Enrichments from U-contaminated sediments demonstrated nearly complete reduction of uranium with very little loss of nitrate from pH 5.7-6.2 using methanol or glycerol as a carbon source. Bacterial 16S rRNA genes were amplified from uranium-reducing enrichments (pH 5.7-6.2) and sequenced. Phylogenetic analyses classified the clone sequences into four distinct clusters. Data from sequencing and terminal-restriction fragment length polymorphism (T-RFLP) profiles indicated that the majority of the microorganisms stimulated by these enrichment conditions consisted of low G+C Gram-positive bacteria most closely related to Clostridium and Clostridium-like organisms. This research demonstrates that the stimulation of a natural microbial community to immobilize U through bioreduction is possible without the removal of nitrate.

Insulin promotes shedding of syndecan ectodomains from 3T3-L1 adipocytes: a proposed mechanism for stabilization of extracellular lipoprotein lipase.

Syndecans are a family of four transmembrane heparan sulfate proteoglycans that act as coreceptors for a variety of cell-surface ligands and receptors. Receptor activation in several cell types leads to shedding of syndecan-1 and syndecan-4 ectodomains into the extracellular space by metalloproteinase-mediated cleavage of the syndecan core protein. We have found that 3T3-L1 adipocytes express syndecan-1 and syndecan-4 and that their ectodomains are shed in response to insulin in a dose-, time-, and metalloproteinase-dependent manner. Insulin responsive shedding is not seen in 3T3-L1 fibroblasts. This shedding involves both Ras-MAP kinase and phosphatidylinositol 3-kinase pathways. In response to insulin, adipocytes are known to secrete active lipoprotein lipase, an enzyme that binds to heparan sulfate on the luminal surface of capillary endothelia. Lipoprotein lipase is transported as a stable enzyme from its site of synthesis to its site of action, but the transport mechanism is unknown. Our studies indicate that shed adipocyte syndecans associate with lipoprotein lipase. The shed syndecan ectodomain can stabilize active lipoprotein lipase. These data suggest that syndecan ectodomains, shed by adipocytes in response to insulin, are physiological extracellular chaperones for lipoprotein lipase as it translocates from its site of synthesis to its site of action.

Quantification of ammonia-oxidizing bacteria and factors controlling nitrification in salt marsh sediments.

To elucidate the geomicrobiological factors controlling nitrification in salt marsh sediments, a comprehensive approach involving sediment geochemistry, process rate measurements, and quantification of the genetic potential for nitrification was applied to three contrasting salt marsh habitats: areas colonized by the tall (TS) or short (SS) form of Spartina alterniflora and unvegetated creek banks (CBs). Nitrification and denitrification potential rates were strongly correlated with one another and with macrofaunal burrow abundance, indicating that coupled nitrification-denitrification was enhanced by macrofaunal burrowing activity. Ammonia monooxygenase (amoA) gene copy numbers were used to estimate the ammonia-oxidizing bacterial population size (5.6 x 10(4) to 1.3 x 10(6) g of wet sediment(-1)), which correlated with nitrification potentials and was 1 order of magnitude higher for TS and CB than for SS. TS and CB sediments also had higher Fe(III) content, higher Fe(III)-to-total reduced sulfur ratios, higher Fe(III) reduction rates, and lower dissolved sulfides than SS sediments. Iron(III) content and reduction rates were positively correlated with nitrification and denitrification potential and amoA gene copy number. Laboratory slurry incubations supported field data, confirming that increased amounts of Fe(III) relieved sulfide inhibition of nitrification. We propose that macrofaunal burrowing and high concentrations of Fe(III) stimulate nitrifying bacterial populations, and thus may increase nitrogen removal through coupled nitrification-denitrification in salt marsh sediments.