The paper describes the sedimentary features and biostratigraphy of the transitional Jurassic to Cretaceous deposits in the continental basins of Priamurie formed after the collision between the Siberian and North China blocks.In Upper Priamurie,the collision occurred in the late Early Jurassic as dated by the emplacement of the post-collisional granites (191 Ma).While in Lower Priamurie and West Priokhotie it could take place in the late Middle Jurassic on the basis of fossil evidence from an accretionary turbidite complex.This event reflected the environmental change from coastal-marine to alluvial plains,often boggy,where coals accumulated.The environmental change is in harmony with that of biota.Systematic study of floral and spores/pollen assemblages,particularly in the sections of interbedded marine and non-marine deposits,makes clear the chronostratigraphic succession of floral associations and shows the possibility of their application for subdivision and correlation of the continental deposits of Priamurie.The coastal-marine environment of the residual post-collisional sublatitudinal basins in the western part of Priamurie (Upper Amur and Dep basins) was replaced by the continental in the late Middle Jurassic and in the eastern part in the Berriasian-Valanginian (Torom Basin).Similar environmental change commenced in the submeridional rift basins:the Bureya Basin in the Callovian and the Partizansk Basin in the Hauterivian.Changes in ecosystems occurred frequently during the Middle Jurassic--Neocomian,but the most substantial changes took place in the late Middle Jurassic and in the end of Late Jurassic. The paper describes the sedimentary features and biostratigraphy of the transitional Jurassic to Cretaceous deposits in the continental basins of Priamurie formed after the collision between the Siberian and North China blocks. In Upper Priamurie, the collision occurred in the late Early Jurassic as dated by the emplacement of the post-collisional granites (191 Ma). White in Lower Priamurie and West Priokhotie it could take place in the late Middle Jurassic on the basis of fossil evidence from an accretionary turbidite complex. This event reflected the environmental change from coastal-marine to alluvial plains, often boggy, where coals accumulated.The environmental change is in harmony with that of biota. Systematic study of floral and spores / pollen assemblages, particularly in the sections of interbedded marine and non-marine deposits, makes clear the chronostratigraphic succession of floral associations and shows the possibility of their application for subdivision and correlation of the con tinental deposits of Priamurie. The coastal-marine environment of the residual post-collisional sublatitudinal basins in the western part of Priamurie (Upper Amur and Dep basins) was replaced by the continental in the late Middle Jurassic and in the eastern part in the Berriasian- Valanginian (Torom Basin). Similar environmental change commenced in the submeridional rift basins: the Bureya Basin in the Callovian and the Partizansk Basin in the Hauterivian. Changes in ecosystems occurred frequently during the Middle Jurassic - Neocomian, but the most substantial took took place in the late Middle Jurassic and in the end of Late Jurassic.