Detailed biostratigraphy of the Middle Callovian – lowest Oxfordian in the Mikhaylov reference section (Ryazan region, European part of Russia) by ammonites

Q2 Earth and Planetary Sciences
D. Kiselev, M. Rogov
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引用次数: 11

Abstract

Study of the sections near the Mikhaylov (Ryazan region) has made it possible to improve the infrazonal subdivision of the Middle Callovian – Lower Oxfordian of the European Russia by ammonites. The Athleta Zone is the most complete in the studied sections. A sequence of kosmoceratid biohorizons (phaeinum, proniae, rowlstonense and kuklikum) is established here, as well as infrazonal units based on a phylogenetic sequence of species of the genus Funiferites. A study of the paleobiodiversity and frequency of occurrence of ammonites at different intervals of the section showed that the ammonite assemblages of the Athleta Zone are Sub-Boreal or Sub-Tethyan, while in the Lamberti Zone they are Boreal, and in the Lower Oxfordian they are Arctic. It is also shown that the change in ammonite composition in the sections coincides with the cycles of transgressions and regressions of Boreal basins. New species and subspecies of the ammonites Funiferites allae compressum, Cadoceras (Eichwaldiceras) intermedium, Brightia (B.) lominadzei, B. (B.) progzhellensis, B. (B.) eccentrtica, B. (Glyptia) canaliculata stankevitchae, Zieteniceras rarecostatum are described.
米哈伊洛夫参考剖面(俄罗斯梁赞地区,欧洲部分)中卡洛世-最低牛津世的详细生物地层学
通过对米哈伊洛夫(梁赞地区)附近剖面的研究,可以通过菊石改善欧洲俄罗斯的中卡洛世-下牛津世的次地界细分。运动区是研究区域中最完整的。这里建立了一个宇宙虫纲生物层序(phaeinum, proniae, rowlstonense和kuklikum),以及基于Funiferites属物种系统发育序列的次区单位。对该剖面不同时间间隔的古生物多样性和菊石出现频率的研究表明,阿特莱塔带菊石组合属于亚北方或亚特提斯,而兰伯蒂带菊石组合属于北方,下牛津带菊石组合属于北极。剖面中菊石组成的变化与北方盆地的海侵和海退旋回相吻合。描述了菊石类的新种和亚种:压缩菊石(Funiferites allae compressum)、中间菊石(Cadoceras (Eichwaldiceras) intermedium、Brightia (B.) lominadzei、B. (B.) progzhellensis、B. (B.) eccentrtica、B. (Glyptia) canaliculata stankevitchae、Zieteniceras rarecostatum。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Volumina Jurassica
Volumina Jurassica Earth and Planetary Sciences-Stratigraphy
CiteScore
3.40
自引率
0.00%
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