After gathering and analyzing over 300 samples of permafrost deposits, the team found that two of them contained viable specimens of soil nematodes (worms). One of these samples was taken from a ground squirrel burrow in the Duvanny Yar outcrop, which has previously been radiocarbon dated to about 32,000 years. The second sample was a drilled ice core from a glacial deposit near the Alazeya River, which corresponds to around 41,700 years of age.