Late Triassic radiolarians from the Grivska formation, internal Dinarides, SW Serbia

N. Bragin, L. Bragina, N. Djerić, Nataša Gerzina Spajić
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引用次数: 1

Abstract

Upper Triassic (upper carnian - rhaetian) grey cherty limestone are known in the internal Dinarides under the name of ?Grivska Formation?. Sediments of the Grivska Formation are characterized by microfossils only - conodonts and radiolarians, and did not yield any macrofossils. Micropa - laeontological research of Upper Triassic siliceous rocks was performed at the locality Lim river, in the vicinity of Bistrica Village in SW Serbia. Radiolarian assemblages are characterized by such species as Capnodoce anapetes De Wever, C. sarisa De Wever, Sarla hadrecaena (De Wever), Praehexasaturnalis tenuispinosus (Donofrio & Mostler), Xiphothecaellla longa (Kozur & Mock). According to the radiolarian data, the investigated cherts are of latest carnian to early norian age.
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塞尔维亚西南部Dinarides内部Grivska组的晚三叠世放射虫
上三叠统(上卡尼世-雷蒂亚世)灰色燧石灰岩在迪纳里纪内部被称为“格里夫斯卡组”。格里夫斯卡组沉积物仅以牙形刺和放射虫等微化石为特征,未发现宏观化石。在塞尔维亚西南部Bistrica村附近的Lim河地区对上三叠统硅质岩进行了显微古生物学研究。放射虫组合以Capnodoce anapetes De Wever、C. sarisa De Wever、Sarla hadrecaena (De Wever)、praehexasaturalis tenuispinosus (Donofrio & Mostler)、Xiphothecaellla longa (Kozur & Mock)等物种为特征。根据放射虫学资料,所调查的燧石年龄为卡尼世晚期至诺曼世早期。
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