东秦岭陕西聂家沟剖面二叠纪—三叠纪之交沉积特征及其古环境意义<sup>*</sup>

doi:10.7605/gdlxb.2022.04.054

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Abstract The marine carbonate strata of the Permian-Triassic transition were found in the Niejiagou section of Zhen'an,Shaanxi. It records the succession of biota and environmental changes of shallow-marine carbonate platform in the Permian-Triassic transition,and is a perfect area for studying the depositional response and palaeoenvironmental changes before and after the end-Permian mass extinction. Based on the detailed analysis of carbonate microfacies and biology combination in the Permian-Triassic transition of the Neijiagou section,11 microfacies types are identified,including patched agglomerates,stromatolites,oolitic-layered stromatolites,foraminiferal grainstone,algal-crinoid grainstone,wackestone containing coated and eroded bone debris particles,oolitic grainstone,aggregate grainstone,oolitic wackestone,mudstone and micrite. According to the characteristics of carbonate microfacies and sedimentary indicators,marginal shoal facies,open platform facies and restricted platform facies are divided in the Permian-Triassic transition. The microfacies characteristics reflect frequent sedimentary microfacies changes in the Permian-Triassic transition. The biological succession and stratigraphic sequence of the Permian-Triassic transition in the Niejiagou section have good uniformity correlation with other sections in South China. After the end-Permian mass extinction,low biodiversity and biological abundance,e.g.,small bivalves and crinoid,occur in the shallow-marine carbonate platform in the Early Triassic. The special microbial sedimentary structures dominated around the mass extinction event boundary. Afterwards,the microbialites disappeared and the bioclastic limestone reoccupied. This research can provide new understanding for the coevolution of organisms and the environment caused by the end-Permian mass extinction.

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	LI Feiyang
	ZHANG Lijun
	LI Tairan
	YANG Qiqi
	NIU Yongbin
	SONG Huibo

Key words： carbonate microfacies community succession sedimentary environment end-Permian mass extinction Qinling

Received: 29 December 2021

ZTFLH:

P531

Fund:National Natural Sicence Foundation of China(No.41602112),the Natural Science Foundation of Henan(No.212300410349),and the Fundamental Research Funds for the Universities of Henan Province(No. NSFRF200340),and the Program for Innovative Research Team(in Science and Technology)of Henan Polytechnic University(No.2022-05)

Corresponding Authors: ZHANG Lijun,born in 1982,an associate professor of Henan Polytechnic University,is engaged in ichnology and sedimentology. E-mail: Ljzhanghpu@gmail.com.

About author: LI Feiyang,born in 1993,is a master degree candidate. He is engaged in sedimentology. E-mail: 1169006628@qq.com.

Cite this article:

LI Feiyang,ZHANG Lijun,LI Tairan et al. Sedimentary characteristics and palaeoenvironmental significance of the Permian-Triassic transition at Niejiagou section of Shaanxi in eastern Qinling[J]. JOPC, 2022, 24(4): 649-662.

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http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2022.04.054 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2022/V24/I4/649

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