Three microfloral assemblages are distinguished among palynomorphs occurring in Upper Permian (Vyatka Horizon) and Lower Triassic (Vokhma Horizon) terrestrial deposits of the Moscow syneclise. One of them, typical of the ...
Four palynological assemblages characteristic of the Nedubrovo, basal Astashikha, middle-upper Astashikha-Ryabi, and Sarafanikha members of the Vokhma Formation are distinguished in Lower Triassic continental deposits of ...