This paper makes an analysis and study on altogether 8 palyniferous samples from the volcano-sedimentary rock series in the Half Three Point area of the Fildes Peninsula, King George Island, Antarctica, the rock series being grey tuffaceous siltstone in lithological characters, about 5m in thickness. Only after making a number of analyses, could we find the relatively abundant sporopollen fossils from 4 samples (Nos. GWP 4—7). But the fossils are poorly preserved, and most of them can hardly be identified; this might be related to the pyrometamorphism resulting from the later volcanic heating at the place. Although only a small part of the fossils in the assemblage are available for identification, they include some genera and species which are of significance to the determination of stratigraphical ages.