Browsing by Author "Chakraborty, R."

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High-quality draft genome sequence of Desulfovibrio carbinoliphilus FW-101-2B, an organic acid-oxidizing sulfate-reducing bacterium isolated from uranium(VI)-contaminated groundwater
(2015-03) Ramsay, Bradley D.; Hwang, Chiachi; Woo, Hannah L.; Carroll, Sue L.; Lucas, Susan; Han, Jie; Lapidus, Alla; Cheng, J. F.; Goodwin, L. A.; Pitluck, S.; Peters, L.; Chertkov, Olga; Held, B; Detter, John C.; Han, C.; Tapia, R.; Land, M. L.; Hauser, Loren; Kyrpides, Nikos; Ivanova, N. N.; Mikhailova, Natalia; Pagani, I.; Woyke, Tanja; Arkin, Adam P.; Dehal, P.; Chivian, D.; Criddle, Craig S.; Wu, Wei-Min; Chakraborty, R.; Hazen, Terry C.; Fields, Matthew W.
Desulfovibrio carbinoliphilus subsp. oakridgensis FW-101-2B is an anaerobic, organic acid/alcohol-oxidizing, sulfate-reducing d-proteobacterium. FW-101-2B was isolated from contaminated groundwater at The Field Research Center at Oak Ridge National Lab after in situ stimulation for heavy metal-reducing conditions. The genome will help elucidate the metabolic potential of sulfate-reducing bacteria during uranium reduction.
Impact of hydrologic boundaries on microbial planktonic and biofilm communities in shallow terrestrial subsurface environments
(2018-09) Smith, Heidi J.; Zelaya, Anna J.; De León, Kara B.; Chakraborty, R.; Elias, Dwayne A.; Hazen, Terry C.; Arkin, Adam P.; Cunningham, Alfred B.; Fields, Matthew W.
Subsurface environments contain a large proportion of planetary microbial biomass and harbor diverse communities responsible for mediating biogeochemical cycles important to groundwater used by human society for consumption, irrigation, agriculture and industry. Within the saturated zone, capillary fringe and vadose zones, microorganisms can reside in two distinct phases (planktonic or biofilm), and significant differences in community composition, structure and activity between free-living and attached communities are commonly accepted. However, largely due to sampling constraints and the challenges of working with solid substrata, the contribution of each phase to subsurface processes is largely unresolved. Here, we synthesize current information on the diversity and activity of shallow freshwater subsurface habitats, discuss the challenges associated with sampling planktonic and biofilm communities across spatial, temporal and geological gradients, and discuss how biofilms may be constrained within shallow terrestrial subsurface aquifers. We suggest that merging traditional activity measurements and sequencing/-omics technologies with hydrological parameters important to sediment biofilm assembly and stability will help delineate key system parameters. Ultimately, integration will enhance our understanding of shallow subsurface ecophysiology in terms of bulk-flow through porous media and distinguish the respective activities of sessile microbial communities from more transient planktonic communities to ecosystem service and maintenance.
A slow-release substrate stimulates groundwater microbial communities for long-term in-situ Cr(VI) reduction
(2015-11) Zhang, Ping; Van Nostrand, Joy D.; He, Zhili; Chakraborty, R.; Deng, Ye; Curtis, Daniel; Fields, Matthew W.; Hazen, Terry C.; Arkin, Adam P.; Zhou, Jizhong
Cr(VI) is a widespread environmental contaminant that is highly toxic and soluble. Previous work indicated that a one-time amendment of polylactate hydrogen-release compound (HRC) reduced groundwater Cr(VI) concentrations for >3.5 years at a contaminated aquifer; however, microbial communities responsible for Cr(VI) reduction are poorly understood. In this study, we hypothesized that HRC amendment would significantly change the composition and structure of groundwater microbial communities, and that the abundance of key functional genes involved in HRC degradation and electron acceptor reduction would increase long-term in response to this slowly degrading, complex substrate. To test these hypotheses, groundwater microbial communities were monitored after HRC amendment for >1 year using a comprehensive functional gene microarray. The results showed that the overall functional composition and structure of groundwater microbial communities underwent sequential shifts after HRC amendment. Particularly, the abundance of functional genes involved in acetate oxidation, denitrification, dissimilatory nitrate reduction, metal reduction, and sulfate reduction significantly increased. The overall community dynamics was significantly correlated with changes in groundwater concentrations of microbial biomass, acetate, NO3–, Cr(VI), Fe(II) and SO42–. Our results suggest that HRC amendment primarily stimulated key functional processes associated with HRC degradation and reduction of multiple electron acceptors in the aquifer toward long-term Cr(VI) reduction.