首页> 外文期刊>Journal of the Palaeontological Society of India >RECORD OF EDIACARAN COMPLEX ACANTHOMORPHIC ACRITARCHS FROM THE LOWER VINDHYAN SUCCESSION OF THE CHAMBAL VALLEY (EAST RAJASTHAN), INDIA AND THEIR BIOSTRATIGRAPHIC SIGNIFICANCE
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RECORD OF EDIACARAN COMPLEX ACANTHOMORPHIC ACRITARCHS FROM THE LOWER VINDHYAN SUCCESSION OF THE CHAMBAL VALLEY (EAST RAJASTHAN), INDIA AND THEIR BIOSTRATIGRAPHIC SIGNIFICANCE

机译:冰巴谷(东拉贾斯坦邦),印度和生物数据学意义较低的vindhyan复合素晶素核心的记录

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摘要

Abundant and well-preserved Ediacaran complex acanthomorphic acritarchs are recorded from the Lower Vindhyan succession in the recently drilled wells of CH-A, PL-A and SK-A in the Chambal Valley part of Vindhyan Basin. Important complex acanthomorphs recorded include various species of Apodastoides, Appendisphaera, Cavaspina, Ceratosphaeridium, Densisphaera, Gyalosphaeridium, Knollisphaeridium, Sinosphaera and Tanarium. Other significant forms are the species of Lophosphaeridium, Obruchevella, Schizofusa and Vandalosphaeridium. In addition, three new acanthomorph taxa, viz. Archaeoacanthodiacrodium, Chambalasphaeridium and Triloboacanthosphaeridium are identified. The above-mentioned complex acanthomorphs first appear in the basal part of the Lower Vindhyan Group, become abundant in the middle and finally disappear in the upper part of the Lower Vindhyan Group within the lower Suket Shale, suggesting an early Ediacaran age for the above succession. The middle and upper parts of the Suket Shale are dominated by Lophosphaeridium rarum, Obruchevella spp. and Leiosphaeridia spp. along with abundant filamentous microfossils, suggesting late Ediacaran age. The uppermost part of the Suket Shale and the overlying Upper Vindhyan succession are marked by the occurrence of Asteridium tornatum, Comasphaeridium sp., Cristallinium cambriense, Dictyotidium birvetense and Lophosphaeridium tentativum of Early Cambrian age.
机译:丰富且保存完好的埃迪基甘兰复杂刺激素素在vindhyan盆地的Ch-a,Pl-a和sk-a的最近钻井井中的较低vindhyan连续中记录。记录的重要复合素素包括各种各样的Apodastoides,Appendisphaera,Cavappina,Cerat alpaeridium,Densisphaera,Gyalidium,Knollisphaeridium,SiNosphaera和Tanium。其他重要形式是氯氰酸盐,Obruchevella,Schizofusa和vandalosphaeridium的种类。此外,三个新的acanthomorph atcha,viz。鉴定了夏吖啶啶,Chambalasphaeridium和Triloboacanthαeridium。上述复杂的丙烷素首先出现在下vindhyan组的基底部分中,在中间变得丰富,最终在下留下古酮群中的上部消失,暗示了上述继承的早期ediCaran年龄。 Suket Shale的中间部分和上部由洛杉矶洛杉矶洛姆,Obruchevella SPP占主导地位。和雷磷酸盐菌。随着丰富的丝状微基,暗示晚埃德加伦时代。 Suket Shale的最上部和覆盖的上vindhyan连续是由Asteridium Tornatum,Comasphaeridium sp的发生而标志着。,Cristallinium Cambriense,Dictyotidium Birvetense和早期寒武纪时代的紫红素紫红色。

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