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首页> 外文期刊>Geologica Carpathica >Conodonts across the Permian-Triassic boundary in the Bukk Mountains (NE Hungary)
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Conodonts across the Permian-Triassic boundary in the Bukk Mountains (NE Hungary)

机译:跨越Bukk山脉(匈牙利东北)的二叠纪-三叠纪边界的牙形石

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摘要

The results of micropaleontological studies, especially of conodonts, across the Permian-Triassic (P-T) bound-ary interval in the Balvany-North, Balvany-East and Gerennavar sections of the Bukk Mountains (NE Hungary) arepresented. Conodont zones for the boundary interval have been identified on the basis of biostratigraphic data forconodont taxa (Hindeodus parvus, H. praeparvus, Hindeodus sp., Isarcicella cf. prisca, Hindeodus/Isarcicella sp.) andthe FOD of H. parvus. The praeparvus Zone possibly the Late praeparvus Zone (uppermost part of Changhsingian, LatePermian) in the Nagyvisnyo Limestone, inclusive of the 'Boundary Shale Bed', and the parvus Zone (earliest Induan,Early Triassic) in the Gerennavar Limestone are discriminated.
机译:展示了Bukk山北部(北部匈牙利)Balvany-North,Balvany-East和Gerennavar断层的二叠纪-三叠纪(P-T)边界范围的微古生物学研究结果,尤其是牙形石。根据牙形生物群的生物地层学数据(Hindeodus parvus,H. praeparvus,Hindeodus sp。,Isarcicella cf. prisca,Hindeodus / Isarcicella sp。)和H. parvus的FOD,已确定了边界区间的牙形石区域。 Nagyvisnyo石灰岩中的praeparvus带可能是晚praeparvus带(晚二叠纪的昌兴盆地的最上部),包括“边界页岩床”,而Gerennavar石灰岩中的parvus带(最早的印度盾,早三叠世)已被区分。

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