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dc.contributor.authorS. O, Keya
dc.contributor.authorM, Alexander
dc.date.accessioned2013-02-26T14:48:04Z
dc.date.issued1975
dc.identifier.citationArch. Microbiol. 103, 37-43 (1975)en
dc.identifier.urihttp://erepository.uonbi.ac.ke:8080/xmlui/handle/123456789/11865
dc.description.abstractThe extent ofdecline in the population density of Rhizobium sp. exposed to Bdellovibno was markedly reduced in the presence of montmorillonite, kaolinite or vermiculite but not by a soil clay fraction. Increasing levels of montmorillonite reduced the numbers of vibrios that appeared in a two-membered culture and allowed for greater survival of the rhizobia. Bdellovibrio and not Rhizobium spwas retained when mixed with the three clay minerals, but no appreciable retention was evident with the soil clay fraction. Suspensions of colloidal soil organic matter protected the hosts from parasitism, although aqueous extracts of soil did not affect the relationship. Cells from old Rhizobium sp. cultures were attacked only after a lag phase, but rhizobia that had been stored were more rapidly lysed than cells tested immediately after removal from the growth medium. The possible significance of these findings to the survival of rhizobia in soils containing Bdellovibrio is discussed. Key words: Bdellovibrio - Clay Minerals - Parasitism- Rhizobium - Soil Ecologyen
dc.language.isoenen
dc.subjectBdellovibrioen
dc.subjectClay Mineralsen
dc.subjectParasitismen
dc.subjectRhizobiumen
dc.subjectSoil Ecologyen
dc.titleFactors Affecting Growth of Bdellovibrio on Rhizobiumen
dc.typeArticleen
local.publisherLaboratory of Soil Microbiology, Department of Agronomy, Cornell University Ithaca, New Yorken


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