The taxonomic composition, structure, and spatial distribution of zoobenthos have been studied in 25 water bodies of the Arctic tundra. Eight types of thermokarst water bodies, representing the stages of the succession cycle, have been identified for the central Yamal Peninsula. Water bodies of the initial stages of the cycle are located on the hills, the middle stages are at the edge of the valleys, and the latest stages are in the valleys. In total, 161 species of zoobenthos have been found; their abundance and diversity vary within a wide range according to reservoir type. The number of species per sample ranges 1–33, abundance 0.02–23.40 thousand ind./m2, and biomass 0.05–73.09 g/m2. The trophic status of studied water bodies changes gradually from hypereutrophic at the beginning of the cycle (bog stage) to ultraoligotrophic (lake stage), becoming hypereutrophic at the end of the cycle (khasyrei stage). During succession, the abundance of zoobenthos decreases due to the replacement of small forms by larger ones: a complex dominating by biomass changes from chironomid at the beginning of the cycle, through bivalves and oligochaetes at lake stages, to gastropods and gammarids at the end of the cycle. Feeding preferences of zoobenthos change from phytophagous, through a wide spectrum (including filter-feeding), to phytophagous and detritus-feeding.
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