摘要
The study of Permian radiolarias in South and Southwest China has been advancedin recent years.A well—preserved radiolarian fauna of Triassic is recently found inSouthwest China.Eight radiolarian assemblage zones are recognized as follows in as-cending order:Pseudoalbaillella rhombothoracata assemblage zone(Qixian),Pseudoalbaillella fusiformis assemblage zone(early—middle Maokouan),Follicucullusassemblage zone(late Maokouan—Wujiapingian),Cangyuanella assemblage zone(early—middle Changxingian),Clavata assemblage zone(latest Permian),Triassocampe yini assemblage zone(early Early Triassic),Pseudoeucyrtis liui assem-blage zone(late Early Triassic)and Triassocampe deweveri assemblage zone(MiddleTriassic).The Permo—Triassic boundary in chert mono—facial sequence of the MuyinheFormation is discussed.
The study of Permian radiolarias in South and Southwest China has been advanced in recent years . A well-preserved radiolarian fauna of Triassic is recently found in Southwest China . Eight radiolarian assemblage zones are recognized as follows in ascending order: Pseudoalbaillella rhombothoracata assemblage zone (Qixian ), Pseudoalbaillella fusiformis assemblage zone (early-middle Maokouan ), Follicucullus assemblage zone (late Maokouan-Wujiapingian ), Cangyuanella assemblage zone (early-middle Changxingian ), Clavata assemblage zone (latest Permian), Triassocampe yini assemblage zone (early Early Triassic ), Pseudoeucyrtis liui assemblage zone (late Early Triassic )and Triassocampe dew even assemblage zone (Middle Triassic ). The Permo -Triassic boundary in chert mono -facial sequence of the Muyinhe Formation is discussed .
