Production of Dibromomethane and Changes in the Bacterial Community in Bromoform-Enriched Seawater

The responses of bacterial communities to halocarbon were examined using a 28-d incubation of bromoform- and methanol-enriched subarctic surface seawater. Significant increases were observed in dibromomethane concentrations and bacterial 16S rRNA gene copy numbers in the treated substrates incubated...

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Bibliographic Details
Published in:Microbes and Environments
Main Authors: Kataoka, Takafumi, Ooki, Atsushi, Nomura, Daiki
Format: Text
Language:English
Published: the Japanese Society of Microbial Ecology (JSME)/the Japanese Society of Soil Microbiology (JSSM)/the Taiwan Society of Microbial Ecology (TSME)/the Japanese Society of Plant Microbe Interactions (JSPMI) 2019
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Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6594743/
http://www.ncbi.nlm.nih.gov/pubmed/30773515
https://doi.org/10.1264/jsme2.ME18027
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Summary:The responses of bacterial communities to halocarbon were examined using a 28-d incubation of bromoform- and methanol-enriched subarctic surface seawater. Significant increases were observed in dibromomethane concentrations and bacterial 16S rRNA gene copy numbers in the treated substrates incubated for 13 d. The accumulated bacterial community was investigated by denaturing gradient gel electrophoresis and amplicon analyses. The dominant genotypes corresponded to the genera Roseobacter, Lentibacter, and Amylibacter; the family Flavobacteriaceae; and the phylum Planctomycetes, including methylotrophs of the genus Methylophaga and the family Methylophilaceae. Therefore, various phylotypes responded along with the dehalogenation processes in subarctic seawater.