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Late Palaeozoic palynomorph assemblages from the Karoo Supergroup and their potential for biostratigraphic correlation, Kalahari Karoo Basin, Botswana

机译:博茨瓦纳卡拉哈里卡鲁盆地,来自卡鲁超群的晚古生古孢粉组合及其与生物地层学联系的潜力

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摘要

Late Carbonifeous to Permian core samples from two borehole sections, STRAT 1 and CKP 6, that penetrate the glacial to postglacial and coal-bearing Lower Karoo sequence, Kalahari Karoo Basin, Botswana, contain well preserved pollen and spore palynomorphs. The palynomorph assemblages comprise 165 species of spores and pollen, and few acritarchs and chlorophycean algae. This paper presents a local biozonation of three succeeding assemblage zones, recognisable in each borehole section. The assemblage zones are named: the Hamiapollenites bullaeformis Biozone, the Cyclogranisporites gondwanensis Biozone and the Platysaccus papilionis–Striatopodocarpites fusus Biozone, in ascending order of stratigraphy. Assemblages are compared and correlated with assemblages described from other Gondwana areas of Africa, Australia, Arabia, South America and Antarctica. A general analysis of taxa from the Kalahari Karoo Basin indicates a distinct similarity with assemblages from the Paraná Basin of South America. The Hamiapollenites bullaeformis Biozone is comparable with the Vittatina costabilis Interval Zone of the Paraná Basin. Assemblages from the Cyclogranisporites gondwanensis and the Platysaccus papilionis–Striatopodocarpites fusus zones are comparable with the Lueckisporites virkkiae Interval Zone. Age determination for the assemblages in the Kalahari Karoo Basin is inferred from comparison with similar assemblages from previous Gondwana studies, and ranges from the Late Carboniferous (Kasimovian–Gzhelian) to latest Early or possibly earliest Middle Permian (Late Cisularian to Early Guadalupian). • Key words: Kalahari Karoo Basin, Late Carboniferous–Permian, pollen, spores, assemblage zones.
机译:来自博茨瓦纳Kalahari Karoo盆地的两个钻孔段STRAT 1和CKP 6的晚石炭纪至二叠纪岩心样品,其渗透到冰川至后冰期和含煤的下Karoo层,其中保存完好的花粉和孢子孢粉。古代形态的组合包括165种孢子和花粉,很少有顶头纲动物和叶绿藻藻类。本文介绍了在每个井眼断面都可以识别的三个连续组合带的局部生物区划。组合地带的名称依次为:地层上的大孢粉生物区,冈旺氏环孢子虫生物区和乳头侧柏-梭状腕果类生物区。将组合与来自非洲,澳大利亚,阿拉伯,南美和南极洲的其他冈瓦纳地区描述的组合进行比较和关联。对来自卡拉哈里卡鲁盆地的分类单元的一般分析表明,其与来自南美巴拉那盆地的组合有着明显的相似性。 Hamiapollenites bullaeformis生物区与Paraná盆地的Vittatina costabilis间隔区相当。来自冈多克环孢子虫和乳头侧柏-纹状腕果融合区的组合物可与拟南芥virkkiae间隔区相媲美。卡拉哈里卡鲁盆地组合的年龄确定是通过与先前冈瓦纳研究的类似组合进行比较得出的,范围从石炭纪晚期(卡西维亚-格热利安)到最新的早期或可能最早的中二叠纪(晚西索拉期到瓜达尔普期)。 •关键词:卡拉哈里卡鲁盆地,石炭纪-二叠纪晚期,花粉,孢子,组合带。

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