Effect of salinity on mercury methylating benthic microbes and their activities in Great Salt Lake, Utah

dc.contributor.authorBoyd, Eric S.
dc.contributor.authorYu, Ri-Qing
dc.contributor.authorBarkay, Tamar
dc.contributor.authorHamilton, Trinity L.
dc.contributor.authorBaxter, Bonnie K.
dc.contributor.authorNaftz, David L.
dc.contributor.authorMarvin-DiPasquale, Mark
dc.date.accessioned2017-08-15T19:17:18Z
dc.date.available2017-08-15T19:17:18Z
dc.date.issued2017-03
dc.description.abstractSurface water and biota from Great Salt Lake (GSL) contain some of the highest documented concentrations of total mercury (THg) and methylmercury (MeHg) in the United States. In order to identify potential biological sources of MeHg and controls on its production in this ecosystem, THg and MeHg concentrations, rates of Hg(II)-methylation and MeHg degradation, and abundances and compositions of archaeal and bacterial 16 rRNA gene transcripts were determined in sediment along a salinity gradient in GSL. Rates of Hg(II)-methylation were inversely correlated with salinity and were at or below the limits of detection in sediment sampled from areas with hypersaline surface water. The highest rates of Hg(II)-methylation were measured in sediment with low porewater salinity, suggesting that benthic microbial communities inhabiting less saline environments are supplying the majority of MeHg in the GSL ecosystem. The abundance of 16S rRNA gene transcripts affiliated with the sulfate reducer Desulfobacterium sp. was positively correlated with MeHg concentrations and Hg(II)-methylation rates in sediment, indicating a potential role for this taxon in Hg(II)-methylation in low salinity areas of GSL. Reactive inorganic Hg(II) (a proxy used for Hg(II) available for methylation) and MeHg concentrations were inversely correlated with salinity. Thus, constraints imposed by salinity on Hg(II)-methylating populations and the availability of Hg(II) for methylation are inferred to result in higher MeHg production potentials in lower salinity environments. Benthic microbial MeHg degradation was also most active in lower salinity environments. Collectively, these results suggest an important role for sediment anoxia and microbial sulfate reducers in the production of MeHg in low salinity GSL sub-habitats and may indicate a role for salinity in constraining Hg(II)-methylation and MeHg degradation activities by influencing the availability of Hg(II) for methylation.en_US
dc.identifier.citationBoyd, Eric S., Ri-Qing Yu, Tamar Barkay, Trinity L. Hamilton, Bonnie K. Baxter, David L. Naftz, and Mark Marvin-DiPasquale. "Effect of salinity on mercury methylating benthic microbes and their activities in Great Salt Lake, Utah." Science of the Total Environment 581-582 (March 2017): 495-506. https://dx.doi.org/10.1016/j.scitotenv.2016.12.157 .en_US
dc.identifier.issn0048-9697
dc.identifier.urihttps://scholarworks.montana.edu/handle/1/13508
dc.titleEffect of salinity on mercury methylating benthic microbes and their activities in Great Salt Lake, Utahen_US
dc.typeArticleen_US
mus.citation.extentfirstpage495en_US
mus.citation.extentlastpage506en_US
mus.citation.journaltitleScience of the Total Environmenten_US
mus.citation.volume581-582en_US
mus.data.thumbpage3en_US
mus.identifier.categoryLife Sciences & Earth Sciencesen_US
mus.identifier.doi10.1016/j.scitotenv.2016.12.157en_US
mus.relation.collegeCollege of Agricultureen_US
mus.relation.collegeCollege of Letters & Scienceen_US
mus.relation.departmentMicrobiology & Immunology.en_US
mus.relation.universityMontana State University - Bozemanen_US

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