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Microfacies, Development, and Controlling Factors of Coral Reef During the Early Permian in Southern Guizhou
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EnPu GONG1, Xiao LI1, LiFu WANG1, 2, YongLi ZHANG1, ChangQing GUAN1
Acta Sedimentologica Sinica | 2026, 44(4) : 1495 - 1506
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Acta Sedimentologica Sinica | 2026, 44(4): 1495-1506
Microfacies, Development, and Controlling Factors of Coral Reef During the Early Permian in Southern Guizhou
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EnPu GONG1, Xiao LI1, LiFu WANG1, 2, YongLi ZHANG1, ChangQing GUAN1
Affiliations
  • 1.School of Resources & Civil Engineering, Northeastern University, Shenyang 110819, China
  • 2.School of Green Mining and Resource Engineering, Liaoning Petrochemical University, Fushun, Liaoning 113001, China
Published: 2026-08-10 doi: 10.14027/j.issn.1000-0550.2025.028
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Objective The Wuotuo village in Zongdi town， Ziyun county， southern Guizhou province， developed an Early Permian coral reef that is exposed with a thickness of approximately 45 m and lateral exposure of nearly 100 m. The reef displays a positive relief. It is of great importance to the study of the construction of shallow marine organisms and the paleoenvironment. Methods The coral reef in this area was systematically studied from the perspectives of paleontology and sedimentary petrology. Results The fusulinids collected from the reef indicated an Early Asselian age. The primary reef-building organism was identified as the fasciculate colonial coral Fomichevella， whereas biotic compositions of the coral reef included foraminifers， brachiopods， gastropods， and calcareous algae. The coral reef in Wotuo village and its underlying and overlying strata contained a broad variety of microfacies types， including bioclastic wackestone-packstone， coral bafflestone， bioclastic packstone， bioclastic grainstone， phylloid algae-cement framestone， fasciculate coral framestone， bioclastic wackestone， and foraminifer-fusulinid grainstone. Conclusions During the Early Permian， glacial-interglacial cycles were the primary factors influencing the variations in palaeoocean temperature and global sea levels. The vertical microfacies succession in this study provides a record of relative sea-level change. The decline of Late Paleozoic glaciation， which resulted in global warming and a relative rise in sea level， played a pivotal role in the development and flourishing of the coral reefs in southern Guizhou province.

coral reef  /  Asselian  /  reef community  /  microfacies  /  southern Guizhou
EnPu GONG, Xiao LI, LiFu WANG, YongLi ZHANG, ChangQing GUAN. Microfacies, Development, and Controlling Factors of Coral Reef During the Early Permian in Southern Guizhou[J]. Acta Sedimentologica Sinica, 2026 , 44 (4) : 1495 -1506 . DOI: 10.14027/j.issn.1000-0550.2025.028
Funding
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  • National Natural Science Foundation of China(42272008)
  • Talent Scientific Research Fund of Liaoning Petrochemical University(2024XJJL-025)
Appendix
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Year 2026 volume 44 Issue 4
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73
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Article Info
doi: 10.14027/j.issn.1000-0550.2025.028
  • Receive Date：2025-03-03
  • Online Date：2026-09-02
  • Published：2026-08-10
Article Data
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History
  • Received：2025-03-03
  • Revised：2025-07-19
  • Accepted：2025-08-21
Funding
National Natural Science Foundation of China(42272008)
Talent Scientific Research Fund of Liaoning Petrochemical University(2024XJJL-025)
Affiliations
    1.School of Resources & Civil Engineering, Northeastern University, Shenyang 110819, China
    2.School of Green Mining and Resource Engineering, Liaoning Petrochemical University, Fushun, Liaoning 113001, China

Corresponding:

WANG LiFu, E-mail:
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表12种不同金属材料的力学参数
科
Family		 属数
Number of
genus		 种数
Number of
species		 占总种数比例
Percentage of
total species (%)		 属
Genus		 种数
Number of
species		 占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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