Age of the Upper Ordovician Koumenzi Formation in the Lenglongling area of the North Qilian Mountain: The evidence from conodonts
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摘要:
本文首次报道了北祁连冷龙岭地区上奥陶统扣门子组牙形石,共识别鉴定出牙形石5属,9种,其中3个未定种,根据牙形石的分布规律,建立了1个牙形石组合:Aphelognathus grandis - Panderodus gracilis组合。笔者通过对研究区牙形石组合与国内外其他地区相同层位的牙形石带对比,并结合扣门子组其它古生物化石资料,将北祁连冷龙岭地区扣门子组的时代重新厘定为晚奥陶世桑比期—赫南特期中期,相当于中国地层年表的艾家山期晚期—钱塘江期中期。
Abstract:Conodonts from the Upper Ordovician Koumenzi Formation in the Lenglongling area of the North Qilian Mountains are reported for the first time. Five genera and nine species of conodonts have been identified, including two undetermined species. On the basis of the characteristics of conodont fossil succession, a conodont assemblage has been established: the Aphelognathus grandis - Panderodus gracilis assemblage. We compared the conodont assemblages of the Koumenzi Formation with those at the same stratum at home and abroad. Combined with other fossil data for the Koumenzi Formation, the author concluded that the age of the Koumenzi Formation is the Kaidi-Middle Hernandian period, which is equivalent to the Late Aijiashan-Middle Qiantangjiang stage in the Chinese stratigraphic chronology.
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Key words:
- North Qilian /
- Late Ordovician /
- Koumenzi Formation /
- conodont assemblage
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图 1 祁连造山带大地构造位置图(a)和区域地质简图(b、c)(据李猛等,2021修改)
Figure 1.
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