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Revision of the conodont zonation of the uppermost Hwajeol Formation (Furongian), Taebaeksan Basin, Korea

机译:韩国太白山盆地最上层的花竹组(芙蓉系)的牙形石带划分

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摘要

The uppermost interval of the Hwajeol Formation, Taebaeksan Basin, has been assigned to the Fryxellodontus inornatus-Monocostodus sevierensis-Semiacontiodus lavadamensis Zone. The main species in the zone are Fryxellodontus inornatus Miller, Hirsutodontus hirsutus Miller, Monocostodus sevierensis (Miller), Semiacontiodus lavadamensis (Miller), S. nogamii Miller, Utahconus utahensis (Miller), and Cordylodus proavus Muller. These species were re-examined to evaluate the biostratigraphy of the Bangteogol and Maesangol sections. Data were added from eleven sections around the Taebaeksan Basin, which were studied previously by the first author. Conodont occurrences above the Cambrooistodus minutus Zone are characterized by a lack of vertical and lateral continuity in sections. Conodont recovery is relatively poor but is sufficient for biostratigraphic assignment. This trend of conodont occurrence seems to be related to sedimentary process, including debris slides and eustatic sea-level fluctuation. Nevertheless, detailed study of the characteristic species of the zone leads to the conclusion that retention of the zone is reasonable. However, it is renamed the M. sevierensis-S. lavadamensis Zone because Fryellodontus inornatus occurs stratigraphically lower than the other two nominate species. The M. sevierensis-S. lavadamensis Zone is correlated with equivalent zones of western USA, Canada, North China, and Australia.
机译:Taebaeksan盆地Hwajeol组的最上层层段已被划分为Fryxellodontus inornatus-Monocostodus sevierensis-Semiacontiodus lavadamensis带。该区域的主要物种是米色的Fryxellodontus inornatus,米勒的Hirsutodontus hirsutus Miller,米勒的Monocostodus lavadamensis,米勒的Semiacontiodus,米氏犹他菌,犹他州的犹他锥虫Miller,米氏的犹他线虫。重新检查这些物种,以评估Bangteogol和Maesangol剖面的生物地层。数据是从太白山盆地周围的11个断层中添加的,第一作者先前已对其进行了研究。在Cambrooistodus minutus区上方的牙形石出现的特点是断面缺乏垂直和横向连续性。牙形石的恢复相对较差,但足以进行生物地层划分。牙形石出现的趋势似乎与沉积过程有关,包括泥石流和海平面涨落。然而,对该区域特征种类的详细研究得出结论,该区域的保留是合理的。但是,它被重命名为S. sevierensis-S。 lavadamensis带,因为在地层上发生Fryellodontus inornatus低于其他两个提名物种。 M. sevierensis-S。 lavadamensis带与美国西部,加拿大,华北和澳大利亚的等效带相关。

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