The cryosphere hosts a widespread microbial community, yet microbial influences on silicate weathering have been historically neglected in cold-arid deserts. Here we investigate bioweathering by a cold-tolerant cyanobacteria (Leptolyngbya glacialis) via laboratory experiments using glaciofluvial drift sediments at 12ºC, analogous to predicted future permafrost surface temperatures. Our results show 3-fold enhanced Si weathering rates in pre-weathered, mixed-lithology Antarctic biotic reactors compared to abiotic controls, indicating significant influence of microbial life on weathering. While biotic and abiotic weathering rates are similar in Icelandic sediments, neo-formed clay and Fe-(oxy)hydroxide minerals observed in association with biofilms in biotic reactors are common on Icelandic mafic minerals, similar to features observed in unprocessed Antarctic drifts. This suggests that microbes enhance weathering in systems where they must scavenge for nutrients that aren’t easily liberated via abiotic pathways; potential biosignatures may form in nutrient-rich systems as well. In both sediment types we also observed up to 4-fold higher bicarbonate concentrations in biotic reactors relative to abiotic reactors, indicating that, as warming occurs, psychrotolerant biota will enhance bicarbonate flux to the oceans, thus stimulating carbonate deposition and providing a negative feedback to rising atmospheric CO2.