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Middle Triassic Radiolaria from turbidites in Ziyun, Guizhou, South China

机译:中国南部贵州紫云的浊积岩中三叠世放射虫

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摘要

In the lower part of the widespread Middle Triassic turbidite succession in southern Guizhou and northern Guangxi (South China), a bed of radiolarian-bearing muddy chert intercalated with the dominant mudstone and thin-layered sandstone suite has yielded a Triassocampe deweveri-Pseudostylosphaera compacta radiolarian assemblage at Ziyun, Guizhou. Twelve genera and twenty-five species of Nassellaria and seven genera and ten species of Spumellaria are recognized in this radiolarian assemblage, two species of which are new. This radiolarian assemblage can be compared with the Triassocampe deweveri assemblage, the Pseudostylosphaera compacta and Emiluvia (?) cochleata assemblage, and the Eptingium manfredi(?) assemblage of Japan. This discovery confirms the assignment of the turbidite succession to the Anisian-Ladinian, and also indicates that an open, deep-sea environment was present during the Middle Triassic in South China.
机译:在贵州南部和广西北部(华南)广泛分布的中三叠纪浊积岩演替的下部,含放射线虫的泥质石床层插有优势泥岩和薄层砂岩组合,产生了三叠纪杜瓦里-Pseudostylosphaera compacta放射虫在贵州紫云集会。在这种放射虫组合中,可以识别出鹦鹉螺的十二属和二十五种,七子虫的七属和十种,其中两个是新的。这种放射虫的组合可以与日本的Triassocampe deweveri组合,Pseudostylosphaera compacta和Emiluvia(?)耳蜗组合以及日本的Eptingium manfredi(?)组合进行比较。这一发现证实了浊积岩演替作用属于阿尼西-拉迪尼安,并且表明在华南中三叠世期间存在着一个开放的深海环境。

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