Abstract:The sediments, overlain by the Middle Jurassic strata in the Wangjia-shan Basin, are a sequence of grey-green sandstones and mudstones and sum more than700 m. It was originally refered to Late Triassic in age. The palynomorph-bearingsamples were collected from the upper part of the sequence in a bore hole. Three sam-ples yielded a, bundant plant microfossils. The sporepollen assemblage consists of 63 species (types) and 51 genera, including 3 new species, namely, Cyclogranisporites callosus, Verrucosisporites wangjiashanensis and Longdongspora jingyuanensis. The component and constituent percentages of palynological assemblage are listedin Tab. 1, in which Pteridophytic spores hold predominant place (67.1%), Gymnospermous pollen reach 32.9%. Among the Pteridophytic spares Punctatisporites (8 forms)plays an important role in assemblage up to 32.3%, followed by Verrucosisporites, Calamospora, Duplexisporites and Apiculatisporis. Besides, Lundbladispora, Kraeuselis-porites and Aratrisporites are represented only by individual specimens. In Gymnospe-rmous pollen Disaccites hold 11.3%, Disaccite striatiti 13.1%, by amplification of Tae-niaesporites reaching 7.2%,others are Piceites, Protoconiferus and Parataeniaesporites.Angustisulcites and Chordasporites are a few in the assemblage. The present assemblage is quite different from the early and upper Triassic paly-nological assemblages of Shan-Gan-Ning Basin, (Qu Li-fan, 1980, 1982) but rather similar to that of the middle Triassic Tongchuan Formation. (Qu Li-fan, 1980; Liu Zhao-sheng et al, 1981) There are 33 genera and 18 species in common between the present assemblage and that of the Tongchuan Formation. Therefore, the present assemblage maybe assigned to the younger age of Middle Triassic. The bearingbed of the spore-pollen assemblage is called the Nanyinger Group. Thisgroup was compared originally with the Yanchang Group of Shan-Gan-Ning Basin, referring to Late Triassic. Based on present data, the Nanyinger Group may include se-diments of younger age of Middle Triassic.