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Vertical Distribution of Potentially Pathogenic Free‐Living Amoebae in Freshwater Lakes 1
Author(s) -
Kyle Dennis E.,
Noblet Gayle Pittman
Publication year - 1985
Publication title -
the journal of protozoology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.067
H-Index - 77
eISSN - 1550-7408
pISSN - 0022-3921
DOI - 10.1111/j.1550-7408.1985.tb03022.x
Subject(s) - distribution (mathematics) , ecology , environmental science , free water , biology , environmental engineering , mathematics , mathematical analysis
The vertical distribution of thermotolerant (37°C and 45°C) free‐living amoebae (FLA) in warm monomictic lakes was determined in relation to the onset of thermal stratification and associated physical and chemical changes. The position of abiotic or biotic paniculate layers in the water column was located by using a submersible horizontal beam transmissometer that measures attenuance, or the absorption and scattering of light by participates in the water column. During mixis, the vertical distribution of amoebae was sporadic with significant numbers of FLA only occurring in clay layers caused by runoff after heavy rains. With the onset of thermal stratification in the lakes, phytoplankton layers began to form. Few amoebae were isolated from layers containing flagellated phytoplankton; however, significant ( P < 0.005) numbers of FLA were isolated from two paniculate layers dominated by the filamentous blue‐green algae Aphanizomenon and Lyngbya, respectively. By late June, a persistent detrital or decomposition layer formed in the lower metalimnion, as well as a hypolimnetic iron layer where the Fe 2+ state was predominant. In this midsummer period, 13 Naegieria fowleri were isolated, with three from the detrital layer and seven from the iron layer. The presence of attenuation zones was found to be the best indicator of the vertical distribution of FLA in the water column, and such layers represent an important, previously undescribed habitat for potentially pathogenic FLA.