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Bacterial oxidation of arsenite at H...
~
Salmassi, Tina Megerdichian.
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Bacterial oxidation of arsenite at Hot Creek: Characterization of biofilm communities and isolation of novel bacteria associated with aquatic macrophytes (California).
紀錄類型:
書目-電子資源 : Monograph/item
正題名/作者:
Bacterial oxidation of arsenite at Hot Creek: Characterization of biofilm communities and isolation of novel bacteria associated with aquatic macrophytes (California)./
作者:
Salmassi, Tina Megerdichian.
面頁冊數:
226 p.
附註:
Source: Dissertation Abstracts International, Volume: 62-04, Section: B, page: 1716.
Contained By:
Dissertation Abstracts International62-04B.
標題:
Biology, Microbiology. -
電子資源:
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3011604
ISBN:
0493209492
Bacterial oxidation of arsenite at Hot Creek: Characterization of biofilm communities and isolation of novel bacteria associated with aquatic macrophytes (California).
Salmassi, Tina Megerdichian.
Bacterial oxidation of arsenite at Hot Creek: Characterization of biofilm communities and isolation of novel bacteria associated with aquatic macrophytes (California).
- 226 p.
Source: Dissertation Abstracts International, Volume: 62-04, Section: B, page: 1716.
Thesis (Ph.D.)--California Institute of Technology, 2001.
Hot Creek, a tributary of the Owens River in the Long Valley Caldera in California, contains naturally elevated concentrations of arsenic as a result of geothermal activity. This site is of particular interest because of its substantial impact on the quality of the drinking water supply for the City of Los Angeles.
ISBN: 0493209492Subjects--Topical Terms:
1017734
Biology, Microbiology.
Bacterial oxidation of arsenite at Hot Creek: Characterization of biofilm communities and isolation of novel bacteria associated with aquatic macrophytes (California).
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226 p.
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Source: Dissertation Abstracts International, Volume: 62-04, Section: B, page: 1716.
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Adviser: Janet G. Hering.
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Thesis (Ph.D.)--California Institute of Technology, 2001.
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Hot Creek, a tributary of the Owens River in the Long Valley Caldera in California, contains naturally elevated concentrations of arsenic as a result of geothermal activity. This site is of particular interest because of its substantial impact on the quality of the drinking water supply for the City of Los Angeles.
520
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Previous studies revealed a rapid in situ oxidation of arsenite in Hot Creek. In this work, bacterial oxidation of arsenite is viewed from the perspective of cultivation-based studies (focusing on pure cultures of arsenite oxidizers) and molecular technique-based studies (surveying the community under ambient conditions).
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The cultivation-based techniques yielded four new arsenite oxidizers. One isolate, Agrobacterium albertimagni strain AOL15, is an alpha-proteobacterium that was isolated using an enrichment-based isolation technique with arsenite concentrations much higher than ambient levels. Values of the kinetic parameters Ks(3.4 +/- 2.2 muM) and V max (1.81 +/- 0.58 x 10-12 mumole·cell -1·min-1) were determined for AOL15. The Ks is near the ambient concentration of arsenite in Hot Creek. However, molecular-based techniques suggested that AOL15 is not a significant member of the biofilm associated with submerged macrophytes.
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The other three oxidizers, YED1--18, YED6--4, and YED6--21, all beta-proteobacteria of the genus Hydrogenophaga, were isolated from solid media. Molecular techniques suggested that beta-proteobacteria are important members of the macrophyte surface community. In the molecular survey, one sequence from Clone #44 (partial) was found to be 99.6% identical to YED6--21. This result, coupled with the isolation of the Hydrogenophaga oxidizers from a million-fold dilution of a suspension of cells from the macrophyte surface, suggests that the Hydrogenophaga are significant members of this community and may be the dominant arsenite oxidizers.
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The densities of total and oxidizer cells associated with the submerged macrophytes in Hot Creek were estimated using most probable number (MIPN) analysis. The normalized MEPN values were 1.4 x 109 total cells/g dry wt. plant and 3.3 x 108 oxidizer cells/g dry wt. plant. These estimates suggest that the oxidizers constitute a significant fraction (on average 24%) of the overall biofilm community.
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http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3011604
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