Abstract
Lake Rotongaio, a warm monomictic lake, was sampled at monthly intervals for 1 year to investigate water temperature, transparency, chemistry, zooplankton, and benthic macroinver‐tebrates. Phytoplankton composition and standing crop represented by concentration of chlorophyll a, were measured for 6 months. Secchi disc values were always less than 2 m because of the large standing crops of algae dominated throughout the year by Anabaena oscillarioides. The major ion composition of the lake water indicated a source typical of a pumice aquifer. The average concentration of dissolved reactive phosphorus during the circulation period was 275 mg m‐3and the average reactive N:P ratio was 0.55. The decline in concentration of inorganic N during the breakdown of thermal stratification could not be accounted for by mixing, and 606 kg or 6.71 mg m‐3d‐lof inorganic N was lost from the lake. The zooplankton comprised rotifers (57%), crustaceans (34%), and ciliates (9%). There was 1 species of calanoid copepod, 2 species of cladocera, and 6 species of rotifer. Ninetyone percent of the benthic macroinverte‐brates were chironomids; the rest were other insects, oligochaete worms, and molluscs. © 1983 Taylor & Francis Group, LLC.
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Forsyth, D. J., Downes, M. T., Gibbs, M. M., Kemp, L., McCallum, I., Mackenzie, L., & Payne, G. (1983). Aspects of the limnology of lake rotongaio. New Zealand Journal of Marine and Freshwater Research, 17(4), 423–435. https://doi.org/10.1080/00288330.1983.9516017
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