25We report the first census of natural microbial communities of the Bonneville Salt Flats 26 (BSF), a perennial salt pan at the Utah-Nevada border. Environmental DNA sequencing of 27 archaeal and bacterial 16S rRNA genes was conducted on samples from multiple evaporite 28 sediment layers of the surface salt crust. Our results show that at the time of sampling 29 (September 2016), BSF hosted a robust microbial community dominated by diverse 30 Halobacteriaceae and Salinibacter species. Desulfuromonadales from GR-WP33-58 are also 31 abundant in all samples. We identified taxonomic groups enriched in each layer of the salt crust 32 sediment and revealed that the upper gypsum sediment layer found immediately under the 33 uppermost surface halite contains a robust microbial community. We found an increased 34 presence of Thermoplasmatales, Nanohaloarchaeota, Woesearchaeota, Acetothermia, 35 Halanaerobium, Parcubacteria, Planctomycetes, Clostridia, Gemmatimonadetes, Marinilabiaceae 36 and other Bacteroidetes in this upper gypsum layer. This study provides insight into the diversity, 37 spatial heterogeneity, and geologic context of a surprisingly complex microbial ecosystem within 38 this macroscopically-sterile landscape. 39 40 IMPORTANCE 41Over the last ~13,000 years the Pleistocene Lake Bonneville, which covered a large 42 portion of Utah, drained and desiccated leaving behind the Bonneville Salt Flats (BSF). Today 43 BSF is famous for its use as a speedway, which has hosted many land-speed records and a 44 community that greatly values this salty landscape. Additionally, the salts that saturate BSF basin 45 are extracted and sold as an additive for agricultural fertilizers. The salt crust is a well-known 46 recreational and economic commodity, but the roles of microbes in the formation and 47 3 maintenance of the salt crust are generally unknown. This study is the first geospatial analysis of 48 microbial diversity at this site using cultivation-independent environmental DNA sequencing 49 methods. Identification of the microbes present within this unique, dynamic, and valued 50 sedimentary evaporite environment is an important step toward understanding the potential 51 consequences of perturbations to the microbial ecology on the surrounding landscape and 52 ecosystem.53 54 65Human land use has altered many aspects of the hydrology and morphology of the environment 66 that facilitated deposition of the ~2m thick evaporite salt crust that caps BSF, and the amount 67 and extent of salt present at the site have been observed to change through time (Bowen, B.B., 68 Bernau, J., Kipnis, E.L., Lerback, J., Wetterlin, L. and Kleba, 2018; Bowen et al., 2018).69 4Examination of modern and ancient salt pan deposits demonstrates that these 70 environments undergo repeated cycles of desiccation (dry saline pan), flooding (brackish lake), 71 and evaporative concentration (drying to dry saline pan) (Bowen and Benison, 2009; 72 Lowenstein, T.K. and Hardie, 1985). While the desiccation stage is most common, it is 73 repeat...