Evidence for propagation of cold‐adapted yeast in an ice core from a Siberian Altai glacier

[1] Cold environments, including glacier ice and snow, are known habitats for cold‐adapted microorganisms. We investigated the potential for cold‐adapted yeast to have propagated in the snow of the high‐altitude Belukha glacier. We detected the presence of highly concentrated yeast (over 104 cells mL−1) in samples of both an ice core and firn snow. Increasing yeast cell concentrations in the same snow layer from July 2002 to July 2003 suggests that the yeast cells propagated in the glacier snow. A cold‐adapted Rhodotorula sp. was isolated from the snow layer and found to be related to psychrophilic yeast previously found in other glacial environments (based on the D1/D2 26S rRNA domains). 26S rRNA clonal analysis directly amplified from meltwater within the ice core also revealed the presence of genus Rhodotorula. Analyses of the ice core showed that all peaks in yeast concentration corresponded to the peaks in indices of surface melting. These results support the hypothesis that occasional surface melting in an accumulation area is one of the major factors influencing cold‐adapted yeast propagation