NEW DATA ON CONODONTS, BRACHIOPODS, AND OSTRACODES FROM THE STRATOTYPES OF THE ILMEN AND BUREGI BEDS (FRASNIAN, MAIN DEVONIAN FIELD)

I. Evdokimova, E. Sokiran, Andrey V. Zhuravlev
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引用次数: 8

Abstract

. The authors restudied biostratigraphically the stratotypes of the Ilmen Beds and Buregi Beds distinguished by R. Hecker in the Frasnian of the central part of the Main Devonian Field (Lake Ilmen region, Russian Platform). Abundant brachiopod, ostracode, and conodont associations were obtained and one new ostracode species Milanovskya bicristata was described. Both the Ilmen (mainly terrigenous) and Buregi (carbonate) beds correspond to relatively shallow-water facies. Conodont associations permit us to correlate these beds with the Middle-Upper asymmetricus Zone and to recognize two local zones (the Polygnathus pollocki Zone and the P. efimovae Zone). Ostracode, brachiopod, and conodont faunas observed in the Ilmen and Buregi beds resemble the Semilukian ones of the Central Devonian Field. Facial, taphonomical, and some palaeoecological observations allow for the reconstruction of the palaeolandscape succession which was caused by regional sea-level changes.
伊尔曼和布里吉地层层型中牙形虫、腕足类和介形虫的新资料(frasen,主泥盆系)
. 从生物地层学角度重新研究了俄罗斯地台伊尔门湖地区主泥盆纪中部frasian地区R. Hecker划分的伊尔门层和布里吉层的层型。获得了丰富的腕足类、介形虫和牙形虫组合,并发现了一种介形虫新种Milanovskya bicristata。Ilmen(主要为陆源)层和Buregi(碳酸盐岩)层均属于相对浅水相。牙形刺的关联使我们能够将这些床与中上不对称带联系起来,并识别出两个局部带(Polygnathus pollocki带和P. efimovae带)。在Ilmen和Buregi地层中观察到的介形虫、腕足动物和牙形石动物群与泥盆纪中部的Semilukian相似。地貌、地貌学和一些古生态观测资料可以重建由区域海平面变化引起的古景观演替。
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