Abstract

Matsumi-ike Bog is a swampy bog that has attained the climax stage of limnological succession. The dynamics of bacterioplankton were studied in relation to the influence of environment factors. The water temperature was shown primarily affect bacterial dynamics as a limiting factor throughout the year. The second most profound factor on the dynamics was the concentration of dissolved organic carbon (DOC) when dead phytoplankton were the major DOC source in the bog, whereas phosphate concentration was most important in the periods when the dead emergent plants were responsible for the DOC supply.

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