Abstract
The habitat of glaciokarst plains in the Dolomites corresponds to ancient cirques carved by glaciers during the Pleistocene era and now determined by karstic processes. It has a rich bryological flora (eighty-seven species). Some of them proved to be statistically significant for indicating vegetation types. The latter are clearly correlated with different types of karstic landforms, each of which corresponding to a well-defined microenvironment.