Applied and Environmental Microbiology, December 1998, p. 4629-4636, Vol. 64, No. 12
United States Geological Survey, Menlo Park,
California 94025
Received 29 May 1998/Accepted 4 September 1998
Bacterial oxidation of
14CH2Br2 and
14CH3Br was measured in freshwater, estuarine,
seawater, and hypersaline-alkaline samples. In general,
bacteria from the various sites oxidized similar amounts of
14CH2Br2 and comparatively
less 14CH3Br. Bacterial oxidation of
14CH3Br was rapid in freshwater samples
compared to bacterial oxidation of 14CH3Br in
more saline waters. Freshwater was also the only site in which methyl
fluoride-sensitive bacteria (e.g., methanotrophs or nitrifiers)
governed brominated methane oxidation. Half-life calculations indicated
that bacterial oxidation of CH2Br2 was potentially significant in all of the waters tested. In contrast, only
in freshwater was bacterial oxidation of CH3Br as fast as chemical removal. The values calculated for more saline sites suggested
that bacterial oxidation of CH3Br was relatively slow compared to chemical and physical loss mechanisms.
However, enrichment cultures demonstrated that bacteria in seawater can
rapidly oxidize brominated methanes. Two distinct cultures of
nonmethanotrophic methylotrophs were recovered; one of these cultures
was able to utilize CH2Br2 as a sole carbon
source, and the other was able to utilize CH3Br as a sole
carbon source.
0099-2240/98/$04.00+0
Copyright © 1998, American Society for Microbiology. All rights reserved.
Bacterial Oxidation of Dibromomethane and Methyl
Bromide in Natural Waters and Enrichment Cultures
*
Corresponding author. Mailing address: United States
Geological Survey, 345 Middlefield Road, MS 480, Menlo Park, CA 94025. Phone: (650) 329-4473. Fax: (650) 329-4463. E-mail:
kgoodwin{at}usgs.gov.
This article has been cited by other articles:
| J. Bacteriol. | Microbiol. Mol. Biol. Rev. | Eukaryot. Cell | All ASM Journals |
|---|