B iological soil crusts, or biocrusts, are major contributors to the biodiversity and ecosystem functions of deserts, semideserts, woodlands, and grasslands worldwide (Belnap 2003; Weber et al. 2016). Biocrust communities contain a diverse assemblage of cyanobacteria, algae, lichens, and bryophytes, as well as bacteria, archaea, fungi, and other associated soil organisms. Collectively, biocrust organisms influence erosion rates, water infiltration, nutrient cycling, carbon (C) storage, and vascular plant composition, among other ecological attributes (Weber et al. 2016). Increasing recognition of the pivotal role that biocrusts play in dryland ecosystems has spurred calls for greater appreciation, protection, and restoration of these com