首页> 外文期刊>Micropaleontology >Santonian-Maastrichtian planktonic foraminifers (Globigerinelloididae, Hedbergellidae, Globotruncanidae and Rugoglobigerinidae) in the Romanian Black Sea offshore
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Santonian-Maastrichtian planktonic foraminifers (Globigerinelloididae, Hedbergellidae, Globotruncanidae and Rugoglobigerinidae) in the Romanian Black Sea offshore

机译:罗马尼亚黑海近海的Santonian-Maastrichtian浮游有孔虫(Globigerinelloididae,Hedbergellidae,Globotruncanidae和Rugoglobigerinidae)

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摘要

Forty four planktonic foraminiferal species are now reported from the Santonian, Campanian and Maastrichtian deposits of the Romanian Black Sea offshore. The Late Cretaceous deposits consist of white yellowish limestones of the Unirea Formation [(? Late) Santonian to Early Maastrichtian] and white chalk with flints of the White Chalk Formation ("Middle" to Late Maastrichtian in age). The taxa of the family Globotruncanidae are dominant but within it the plano-convex tests are rare. The most frequent species have biconvex tests. The planispirally enrolled taxa, hedbergellid forms as well as the rugoglobigerinids, are rare. The maximal faunal diversity is encountered during Early - "Middle" Maastrichtian. A local biostratigraphical scale consisting of six biozones is established.
机译:据报道,罗马尼亚黑海近海的桑顿,坎帕尼亚和马斯特里赫特沉积物中有44种浮游有孔虫物种。白垩纪晚期的沉积物由Unirea组的白色微黄色石灰岩[(?)Santonian到Maastrichtian早期]和白垩与白色粉笔组的chalk石(年龄为“ Middle”至Maastrichtian晚期)组成。 Globotruncanidae科的分类单元占优势,但其中平凸测试很少。最常见的物种进行双凸检验。平面上登记的分类单元,赫德贝格形式以及rugoglobigerinids很少见。在早期-“中”马斯特里赫特时期遇到了最大的动物多样性。建立了由六个生物区组成的当地生物地层规模。

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