ON THE POSITION OF THE BOUNDARY BETWEEN THE MOSCOVIAN AND KASIMOVIAN GLOBAL STAGES OF THE CARBONIFEROUS IN THE DONETS BASIN

T. Nemyrovska
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Abstract

Detailed new data on paleontology and stratigraphy were obtained in the process of fulfilling the tasks of the International Carboniferous Subcommission on definition of the scopes of the Moscovian and Kasimovian global stages and the precise position of the boundary between them. The analysis of these data has shown that the position of this boundary in the type  area and in the other regions needs the revision. Recently the investigation of the conodonts from the Moscovian–Kasimovian boundary deposits in the Donets Basin revealed that the boundary between the Moscovian and Kasimovian stages in the official Ukrainian Carboniferous Stratigraphic Scheme does not correspond to this boundary in the type area of these stages in the  Moscow Basin. To correct this situation the lower boundary of the Kasimovian in the Ukrainian Scheme must be downgraded by two conodont zones — Swadelina subexcelsa and Sw. makhlinae. To update this boundary in the type area to fulfill the task of the Carboniferous Subcommission four conodont species were proposed as potential index-species for the definition of the boundary between the Moscovian and Kasimovian global stages. These conodont species are as follows Sw. subexcelsa,  Idiognathodus sagittalis, I. turbatus and I. heckeli. One of these species, which is selected, will be used as a marker of the  studied boundary. None of these species is officially selected as a marker. If Sw. subexcelsa will be selected, the position of  the Moscovian–Kasimovian boundary will remain at the present position. In this case this boundary in the Donets Basin has to be downgraded by two conodont zones. If one of three Idiognathodus will be selected, this boundary in the type area will be   upgraded by one and a half regional substage. In the Donets Basin it will be upgraded by less than a cycle. Keywords: Carboniferous, stratigraphy, conodonts, extinction event, index-­species. 
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顿涅茨盆地石炭系莫斯科-卡西莫瓦全球期界线位置的探讨
在完成国际石炭纪小组委员会关于确定莫斯科和卡西莫维安全球阶段范围及其边界精确位置的任务过程中,获得了详细的古生物学和地层学新资料。对这些数据的分析表明,该边界在类型区域和其他区域的位置需要修正。最近对顿涅茨盆地莫斯科—卡西莫维安界线沉积物牙形刺的研究表明,乌克兰石炭系地层方案中莫斯科—卡西莫维安界线与莫斯科盆地这两个阶段类型区的界线并不一致。为了纠正这种情况,乌克兰方案中的Kasimovian的下边界必须被两个牙形石带- Swadelina subxcelsa和Sw降级。makhlinae。为了更新这一模式区边界,完成石石纪小组委员会的任务,提出了4种牙形石作为确定莫斯科和卡西莫瓦全球阶段边界的潜在指标种。这些牙形石种类如下:矢状齿、突状齿、突状齿和突状齿。其中一个被选择的物种将被用作研究边界的标记。这些物种都没有被正式选为标记。如果西南。将选择subxcelsa,莫斯科-卡西莫维奇边界的位置将保持在目前的位置。在这种情况下,顿涅茨盆地的边界必须被两个牙形石带降低。如果选择三种Idiognathodus中的一种,则该类型区域的边界将被升级为一个半区域子阶段。在Donets盆地,它将在不到一个循环的时间内升级。关键词:石炭纪,地层学,牙形刺,灭绝事件,物种指数。
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MAIN STAGES OF DEVELOPMENT OF THE LATE CARBONIFEROUS FLORA AND VEGETATION IN THE DONETS BASIN AS THE BASIS OF JUSTIFICATION OF REGIONAL STRATIGRAPHIC UNITS AT THE PALAEOECOSYSTEM LEVEL ON THE POSITION OF THE BOUNDARY BETWEEN THE MOSCOVIAN AND KASIMOVIAN GLOBAL STAGES OF THE CARBONIFEROUS IN THE DONETS BASIN ANTARCTIC RESEARCH – THE STATE PROGRAM OF UKRAINE PETRO FEODOSIIOVYCH GOZHYK: OCEANIC, MARINE AND ANTARCTIC RESEARCH IN MEMORIAM OF PROFESSOR PETRO F. GOZHIK, ACADEMICIAN OF THE NATIONAL ACADEMY OF SCIENCES OF UKRAINE
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