摘要
According to the identification of sporopollen fossils from the 42 wells in north central Raoyang Sag, Central Hebei Depression, the palaeoecological classification of palynoflora in Shahejie Formation was discussed; one palynological assemblage with high proportion of Quercoidites-Ulmipollenites was recognized, and five sub-assemblages were established. The results showed that the proportion of mesic sporopollen was stable ,with an average of 70% or higher, while there was a little change for the proportion of xerophilous and hygrophilous sporopollen; vegetation pattern during the late member 4 of Shahejie Formation was mainly evergreen and deciduous broad-leaved forest in semi-arid warm temperate climate; vegetation pattern during the member 3 of Shahejie Formation was mainly coniferous forest, and secondly broad-leaved forest in sub-humid sub-tropical climate; vegetation pattern during the member 2 of Shahejie Formation was mainly coniferous and broad-leaf forest in semi-arid sub-tropical climate; vegetation pattern during the member 1 of Shahejie Formation was mainly coniferous and broad-leaf forest with an increase of hygrophilous herbaceous vegetation in humid sub-tropical climate.