Abstract: The Red Beds of Nandian consists mainly of red mud stone, marlite, quartzitic sand- stanc, Sabulous psephyte and fine psephyte. Predecessor divided them into three formations referring to Upper Triassic-Jurassic. The marlite in Upper Formation of the Red Beds are rich in fossil Sporo-pollen. The fossil spores and pollen contain 17 genera and 15 species, including 3 new species and 2 new combinations. The Sporo-pollen assemblage is characterized by the absolut predominance of the pollen of gymnospcrms (84.8%) compared with the spores of pteridophyta (15.2%), The pollen are specially characterized by the abundance of Classeopollis Pfiug (75.3%) with a certain amount of Psophosphaera (4.5%), Monosulites (2.4%) and a minority of Pinuspollenites (0.6%). The spores grains are characterized by the abundance of Cyathidites (4.1%), and also by presence of Calamospora (2.1%), Reticulatisporitcs (2.4%), Indeterminable form (1.2%), and rare Schizaeisporites (0.3%). Based on the sporo-pollen assemblage of Upper Jurrassic of the Eurasia continent is characterized by the absolute abundance of Classpollis Pflug (>50% of the total number), the Upper Formation oi the Red Beds of Nandian may be referred to Upper Jurassic age. The climate of the Nandian region in the Late Jurassic period is supposed to be as arid as that of Africa at the present time. Bundary of the eastern termination of southern part of the Eurasia continent in- ferred by Vakhrameev (1970) should be complemented.