Lava tube caves are host to a fascinating microbiota that grows in mats or crusts sometimes visible to the naked eye. The biogeochemistry of these microbes, including their adaptational response to these oligotrophic environments, potential roles in speleothem formation and biogeochemical cycling of basalt components. Furthermore, Icelandic lava tubes make for attractive planetary analogues for astrobilogical studies, as they share many features with comparable cave systems in other rocky planets where life may have subsisted in the past.