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首页> 外文期刊>Journal of Geology & Geophysics >Palynomorphs Distribution, Biostratigraphy and Paleoecology Study of the Superficial Sediments in Parts of Gombe Formation, Upper Benue Trough, Nigeria
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Palynomorphs Distribution, Biostratigraphy and Paleoecology Study of the Superficial Sediments in Parts of Gombe Formation, Upper Benue Trough, Nigeria

机译:尼日利亚上贝努尔海槽Gombe组部分表层沉积物的沉积形态,生物地层学和古生态研究

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Paleoecological conditions of part of Gombe formation of Upper Benue Trough were studied using outcrop samples from 22 sites of 1.5 m deep each. The samples were crushed, standard maceration method employed for analysis and slides prepared. The slides were examined for identification and counting using transmitted light microscope with times one hundred oil immersion objective lenses. The result showed a fairly rich assemblage of palynomorph which includes age diagnostic palynomorphs: Cingulatisporites ornatus, Proteacidites sigalli, Constructipollenites inflectus, Echitriporites trianguliformis, Longapertites microfoveilatus, Monocolpites sp. and Tricolpites sp. which effectively assigned the upper Maastritchtian age to the sequence. Also the abundance of woody and vegetal materials which are land derived in the shales, siltstones and kaolinite rich claystone at the upper part of the sequence studied suggest the prevalence of fresh water conditions. The presence of Ephedripites in some sections of the sequence studied reflects occasional dry conditions. The high abundance of Acrostichum aureum in sample BA-8 signifies flooding of the region in Maastrichtian times by the sea characterized by shallow water depth and restricted ecological circulation which also occurs in mangrove forest and other wetlands.
机译:使用22个1.5 m深的露头样本研究了上Benue Trough槽的Gombe地层的古生态条件。将样品压碎,采用标准浸渍法进行分析并制备载玻片。使用透射光显微镜用一百次油浸物镜检查载玻片的鉴定和计数。结果表明,古朴的形态非常丰富,其中包括年龄诊断古朴的形态:Cingulatisporites ornatus,Proteacidites sigalli,Constructipollenites inflectus,Echitriporites trianguliformis,Longapertites microfoveilatus,Monocolpites sp。和Tricolpites sp。有效地将上马斯特里奇时代分配给了该序列。同样,在研究序列的上部,大量的页岩,粉砂岩和富含高岭土的粘土中衍生出的木质和植物材料也表明淡水条件普遍存在。在所研究序列的某些部分中存在麻闪石,这反映了偶尔的干燥条件。样品BA-8中的金黄色芦荟含量很高,这表明马斯特里赫特时代的该地区被海水淹没,其特征是浅水深度和限制的生态循环,这也发生在红树林和其他湿地中。

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