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Upper Cretaceous (Santonian-Campanian) radiolarians from Voronesh Anticline, southwestern Russia

机译:俄罗斯西南部沃罗涅什背斜的上白垩统(桑托尼-坎帕尼亚)放射虫

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摘要

Core-samples from wells and an outcrop located on the Voronesh Anticline in the southeastern part of the Russian Platform contain Late Cretaceous radiolaria. 83 species are described and illustrated (SEM and transmitted light images) from Santonian-early Campanian deposits, and two assemblages are distinguished. The older assemblage with Alievium gallowayi, Archaeospongoprunum bipartitum, Archaeospongoprunum. cf. A. salumi as well as other less age-diagnostic taxa, is interpreted as Santonian correlative with the Euchitonia santonica-Aiievium gallowayi Assemblage Zone of the Moscow Basin (Vishnevskaya 1993). The younger assemblage, of Santonian - early Campanian age, contains Patulibracchium cf. P. davisi, Crucella irwini, Cryptamphorella sphaerica, Praeconocaryomma californiensis, Dictyomitra lamellicostata among other species and is correlative with the Orbiculiforma quadrata-Lithostrobus rostovtsevi Assemblage Zone of the Moscow Basin. In terms of inter-regional faunal comparisons, both of the Voronesh Anticline radiolarian assemblages demonstrate relatively close affinities to coeval rocks from the Volga River region, but less similarity to the assemblages from the Moscow Basin. Only a few of the common endemic species of Siberian assemblages occur in our samples. On an inter-regional level, the radiolarian assemblages described herein have similarities with assemblages reported from Japan and California. Index-species characteristic for the Santonian-Campanian radiolarian biozonations of the Atlantic and Pacific Oceans are not found in our collection. However, the presence of many cosmopolitan species known from the European Platform, Japan and California suggests a marine connection between the Voronesh Anticline region, the western Atlantic and eastern Tethys during Santonian-Early Campanian time.
机译:来自油井的岩心样品和位于俄罗斯平台东南部Voronesh背斜的露头包含晚白垩世放射虫。描述和说明了来自Santonian早期的Campanian矿床的83个物种(SEM和透射光图像),并区分了两种组合。与Alievium gallowayi,Archeeospongoprunum bipartitum,Archeeospongoprunum的较旧组合。 cf.沙鲁氏菌和其他不具年龄诊断意义的分类单元被解释为与莫斯科盆地的桑树金黄色葡萄球菌-盖洛维虫聚集区相关的桑顿系(Vishnevskaya 1993)。 Santonian的年轻组合-Campanian早期,包含Patulibracchiumcf。 P. davisi,Crucela irwini,Cryptamphorella sphaerica,Praeconocaryomma californiensis,Dictyomitra lamellicostata等物种与莫斯科盆地的Orbiculiforma quadrata-Lithostrobus rostovtsevi组合区相关。就区域间动物区系比较而言,两个Voronesh背斜放射虫组合都显示出与来自伏尔加河地区的近代岩石的亲缘关系相对较近,但与来自莫斯科盆地的组合相似度较低。在我们的样本中,只有少数几种常见的西伯利亚组合特有物种。在区域间的水平上,本文所述的放射虫组合与日本和加利福尼亚报道的组合相似。在我们的收藏中没有发现大西洋和太平洋的桑托尼亚-坎帕尼亚放射虫生物区带的索引物种。但是,从欧洲平台,日本和加利福尼亚州已知的许多世界性物种的存在表明,在Santonian-Early Campanian时期,Voronesh背斜地区,西部大西洋和特提斯东部之间存在海洋联系。

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