“…The drying of the Aral Sea has induced succession processes of vegetative cover in the region through the stimulation of autogenous successions of the plant cover and the formation of climax vegetation on the dried bottom of the Aral Sea (Dimeyeva, 1995(Dimeyeva, , 2007(Dimeyeva, , 2015Wucherer and Breckle, 2001;Kuzmiona et al, 2006). In this process, the successions have three progressions: psammoseries, haloseries, and potamoseries, which exhibit differences through ecological conditions, regularity of dynamics, species variability indices, and formation stages, and are defined on the basis of the dominant vegetative communities under changes of soil ground conditions (Dimeyeva, 2015).…”