Lake Taimyr in Siberia is northernmost among the world's large lakes:
73 degrees 40' -75 degrees 20' N, 99-106 degrees E. The lake area is u
p to 4650 km(2) in summer, with a maximum depth of 26 m and a mean dep
th of only 2.8 m. The ice-free period lasts about three months. The wa
ter level sinks 5.5-6 m during winter, so that 85% of the bottom surfa
ce is frozen into ice for some time and subjected to negative temperat
ures, probably down to -20 degrees C. In artificially melted sediment
samples, 75-92% of animals survived. The average summer biomass of zoo
benthos is about 1 g m(-2) wet weight, a half of this being formed by
Oligochaeta. Altogether 76 samples with 3742 oligochaete specimens col
lected by V. N. Greze in 1943-1944 were studied. At least 14 taxa of T
ubificidae, Lumbriculidae, and Enchytraeidae were found in the lake, a
nd some more enchytraeids in an adjacent river. Many immature animals
could not be identified to species. Naididae were completely lacking p
robably due to the absence of macrovegetation. The shallow freezing zo
ne is inhabited mostly by Alexandrovia ringulata. The profundal fauna
is dominated by Lamprodrilus isoporus, Stylodrilus sp., and Isochaetid
es sp.