Abstract: A great deal of Spumellaria and Nassellaria were found by the author (H. Huang) in 1982 in Late Sinian silicalites between Sandu and Songtao, Guizhou and later in 1087, small amounts of them were recognized again by the authors in carbonate manganese ores from the Early Sinian Datangpo Formation in western Hunan and eastern Guizhou, which is the oldest horizon for the occurrence of radiolaria so far. The manganese deposits in the Datangpo Formation which are placed in between the Early Sinian Nantuo Moraine Bed ("Large Moraine") and the Tiesi'ao Formation ("Small Moraine")are widely distributed over the area between Sichuan, Hunan and Guizhou Provinces. The manganese orebodies are stratiform, stratoid and lentieular, trending from NE to SW. The ores may be divided into two types: massive and banded, among which the latter is dominated. The ore beds not only have well-developed horizontal fine beddings but also contain abundant mietoplankton fossils including radiolaria which can be used for .indicating depositional environments. The manganese deposits were formed in a deeper restricted marine basin with a water depth of about 100 m or more. The contents of radiolarian skeletons preserved in manganese ores range generally between 2 and 5 percent. Nassellaria occupies first place and Spumellaria comes second ;conversely, Spumellaria occupies first place and Nassellaria comes second in Mn-bearing siliceous shale (rhodochrosite-poor) in which the contents of radiolarian skeletons may locally reach up to 25 to 30 percent. Nassellaria is mostly 0.09 to 0.13 mm in height and shows a wide range of shapes., lampshade——like, tower-like and umbrella-like, whereas Spumellaria, round to elliptic, generally 0.02 to 0.05mm in diameter. The individuals tend to be smaller as compared with those in the younger Cambrian, Permian, Triassic and Cretaceous siliceous rocks. Both Nassellaria and Spumellaria usually show oriented distribution along the bedding planes and occasionally are enriched to form bands or laminae interbedded with rhodoehrosite bands, thus resulting in the formation of well-defined banded or laminated ores. The ra-diolaria is characterized by well-preserved skeleton, well-defined outline and clear reticulated and acie-ular structures. Part of the skeletons were dissolved and replaced completely or in varying degrees by rhodochrosite and dolomite, but its outline remains retained. The preserved status of radiolarian mor-phology depends mainly upon epidiagenesis.