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The palaeozoic palynostratigraphy of the Karoo supergroup and palynofacies insight into palaeoenvironmental interpretations, Kalahari Karoo Basin, Botswana

机译:博茨瓦纳卡拉哈里卡鲁盆地古生界古生界古地层学和古生界对古环境解释的认识

摘要

Late Carboniferous to Permian strata of the Lower Karoo sequence in the Kalahari Karoo Basin, Botswana, contains suitably preserved palynomorphs for biostratigraphic classifications. All taxa described from eight out of the nine coreholes sampled for the study comprise sixty-eight genera made of one hundred and sixty-five miospore species, eleven arcritarchs species, seven prasinophytes species, and 1 chlorophyte species. Two wellsampled coreholes, namely STRAT 1 and CKP6, have lacial facies, to warm and drier conditions during deposition of the lower Ecca sequences. Palaeoclimatic conditions ultimately turned wet during middle Ecca times generating coal-forming settings. Palaeoenvironmental interpretations based on palynofacies data indicate a predominantly proximal palaeo-depositional setting for the entire Lower Karoo sequence at STRAT 1 borehole. The broader depositional environment transformed from glacial sub-environments, during deposition of the Dwyka Group, into a relatively wider basin punctuated by some rare marine incursions, in the early Ecca Group, and ultimately developing into a deltaic system.
机译:博茨瓦纳卡拉哈里卡鲁盆地下部卡鲁序列的石炭纪至二叠纪晚期地层含有适当保存的脉石形态,用于生物地层学分类。在研究的9个岩心孔中,有8个描述了所有的分类单元,包括68个属,这些属由165个微孢子种,11个弓形目种,7个类藻类和1个绿藻类组成。有两个采样良好的岩心孔,即STRAT 1和CKP6,具有蕾丝相,可以在较低的Ecca序列沉积过程中变暖和干燥。在古埃加中期,古气候条件最终变湿,形成了成煤环境。基于古岩相数据的古环境解释表明,在STRAT 1井眼中,整个下卡鲁序列的古近沉积环境都以近端为主。在德凯(Dwyka)组沉积期间,更广泛的沉积环境从冰川亚环境转变为埃卡(Ecca)组早期由一些罕见的海洋入侵打断的相对较宽的盆地,并最终发展成三角洲系统。

著录项

  • 作者

    Modie Benson;

  • 作者单位
  • 年度 2007
  • 总页数
  • 原文格式 PDF
  • 正文语种 fr
  • 中图分类
  • 入库时间 2022-08-20 20:23:35

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