The first organism to be described from the Deep Spring Formation in 2014 was Elainabella in the Esmeralda Member, an enigmatic alga with similarities to green algae, suggesting that part of the formation was at one point a shallow marine environment or a microbial reef community.[4] More organisms would be described in 2016, most of which are ichnogenus' like Planolites, and even some tubular forms, like Wutubus, expanding not only the stratigraphic range of some of these forms, but also their biogeographic range.[3]
^Smith, Emily F.; Nelson, Lyle L.; O’Connell, Nizhoni; Eyster, Athena; Lonsdale, Mary C. (22 September 2022). "The Ediacaran−Cambrian transition in the southern Great Basin, United States". GSA Bulletin. doi:10.1130/B36401.1.
^ abcSmith, E.F.; Nelson, L.L.; Strange, M.A.; Eyster, A.E.; Rowland, S.M.; Schrag, D.P.; Macdonald, F.A. (1 November 2016). "The end of the Ediacaran: Two new exceptionally preserved body fossil assemblages from Mount Dunfee, Nevada, USA". Geology. 44 (11): 911–914. doi:10.1130/G38157.1.