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Composition of Benthic Invertebrate Communities in Relation to Phytoplankton Populations in Five Subarctic Lakes

โœ Scribed by Dr. James W. Moore


Publisher
John Wiley and Sons
Year
1980
Tongue
English
Weight
811 KB
Volume
65
Category
Article
ISSN
1434-2944

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โœฆ Synopsis


Abstract

The effects of algal food supply, temperature, water depth and lake size on the composition of benthic invertebrate communities were determined during 1978 und 1979 in 5 lakes in the Canadian subarctic. The lakes varied widely in physical conditions and trophic level, with peak algal densities ranging from 40 to 2100 mg/m^3^ during the summer and 10 to 750 mg/m^3^ in the winter. The correlation coefficients between the size of the populations of herbivorous chironomids (Chironomus riparius, Ch. plumosus, Ch. decorus, Tanytarsus xanthus) and the density of algae during the winter were highly significant and positive. There were also positive, albeit weak, correlations with the summer growth of algae, temperature, depth and lake size. In addition, the seasonal appearances of fourth instar larvae in the sediments were positively correlated with peaks in the abundance of phytoplankton. In contrast, algal food supplies probably had little impact on the density of oligotrophic indicator species (Heterotrissocladius oliveri, H. changi, Protanypus ramosus, Pontoporeia affinis) and were replaced in importance by temperature and water depth. Variations in the densities of the main oligochaete species (Uncinais uncinata, Arcteonais lomondi, Limnodrilus claparedeianus) and mollusc species (Valvata sincera helicoidea) could not be related to any of the factors that were measured. The diversity of the communities was probably limited by low temperatures, whereas food supply, lake depth and lake size had little impact on the fauna.


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โœ Dr. James W. Moore ๐Ÿ“‚ Article ๐Ÿ“… 1978 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 933 KB

The factors influencing the density, diversity and species composicion of benthic invertebrate communities in 20 lakes in the Canadian arctic and subarctic were determined during 1975, 1976 a n d 1977. Despite small differences in nutrient and phytoplankton levels among the lakes, there was a strong