Origin of Permian Chihsian Carbonates from South China and Its Geological Implications

YAN Jia xin

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YAN Jia xin. Origin of Permian Chihsian Carbonates from South China and Its Geological Implications[J]. Acta Sedimentologica Sinica, 2004, 22(4): 579-587.

Citation:

YAN Jia xin. Origin of Permian Chihsian Carbonates from South China and Its Geological Implications[J]. Acta Sedimentologica Sinica, 2004, 22(4): 579-587.

Origin of Permian Chihsian Carbonates from South China and Its Geological Implications

YAN Jia xin

China University of Geosciences, Wuhan 430074

Received Date: 2003-10-30
Rev Recd Date: 2004-03-26
Publish Date: 2004-12-10

Abstract

The Permian Chihsia Formation of South China is a unique carbonate succession, which is rich in organic matter and chert nodule, and is characterized by the great lateral persistence with little variation in lithofacies and strata thickness. Two special diagenetic minerals, nodular celestite and sepiolite, are developed in the carbonate succession. Comprehensions on the origin of the above mentioned features implied that oxygen deficient environmental condition was a critical controlling factor among these features. Based on sedimentary features of the carbonate succession, it was proposed that the Chihsian deficient environments were derived from relatively high bioproductivity. This explanation is compatible with recent advancements in the Permian paleocliamatology and paleoceanography, but further work on the origin of the high bioproductivity is still desired.
- South China,
- Permian,
- Chihsia Formation,
- bioproductivity

References

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Origin of Permian Chihsian Carbonates from South China and Its Geological Implications

China University of Geosciences, Wuhan 430074

Received Date: 2003-10-30

Rev Recd Date: 2004-03-26

Publish Date: 2004-12-10

Key words:

Abstract: The Permian Chihsia Formation of South China is a unique carbonate succession, which is rich in organic matter and chert nodule, and is characterized by the great lateral persistence with little variation in lithofacies and strata thickness. Two special diagenetic minerals, nodular celestite and sepiolite, are developed in the carbonate succession. Comprehensions on the origin of the above mentioned features implied that oxygen deficient environmental condition was a critical controlling factor among these features. Based on sedimentary features of the carbonate succession, it was proposed that the Chihsian deficient environments were derived from relatively high bioproductivity. This explanation is compatible with recent advancements in the Permian paleocliamatology and paleoceanography, but further work on the origin of the high bioproductivity is still desired.

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Reference (71)

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[2]	Veizer J, Ala D, Azmy K, et al. 87Sr/86Sr, δ13C and δ18O evolution of Phanerozoic seawater. Chemical Geology, 1999, 161: 59～88
[3]	吕炳全,翟建军.下扬子地区早二叠世海进和上升流形成的缺氧环境的沉积. 科学通报,1989,22:1721～1724[Lu Binquan, Zhai Jianjun. Early Permian oxygen-deficient deposits of transgression and upwelling in origin in the Lower Yangtze Region. Kexue Tongbao, 1989, 22, 1721～1724
[4]	颜佳新,陈北岳,李思田,等.鄂湘桂地区栖霞组古氧相分析与层序地层和海平面变化.地质论评,1997, 43(2): 193～199[Yan Jiaxin, Chen Beiyue, Li Sitian, et al. Oxygen-related facies and sequence stratigraphy as well as sea-level changes in the Chihsia Formation of Hubei, Hunan and Guangxi area. Geological Review, 1997, 43(2), 193～199]
[5]	吴胜和,冯增昭,何幼斌.中下扬子地区二叠纪缺氧环境研究. 沉积学报,1994,12(2): 29～36[Wu Shenhe, Feng Zengzhao, He Youbin. Study on anoxic environments of Permian in the Middle and Lower Yangtze Region. Acta Sedimentologica Sinica, 1994, 12(2): 29～36]
[6]	颜佳新,徐四平,李方林.湖北巴东栖霞组缺氧沉积环境的地球化学特征. 岩相古地理, 1998,18(6): 27～32[Yan Jiaxin, Xu Siping, Li Fanglin. Geochemistry of aerobic depositional environment of Qixia Formation in Badong, Hubei Province. Lithofacies and Palaeogeography, 1998, 18(6), 27～32]
[7]	施春华,黄秋,颜佳新.广西来宾栖霞组缺氧沉积环境的地球化学特征.沉积与特提斯地质,2001,21(2): 72～77[Shi Chunhua, Huang Qiu, Yan Jiaxin. Geochemistry of the dysaerobic sedimentary environments of the Qixia Formation in Laibin, Guangxi. Sedimentary Geology and Tethyan Geology, 2001, 21: 72～77]
[8]	颜佳新,方念乔.湖北省栖霞组沉积环境,沉积旋回及层序地层划分.地球科学,1994,19(5): 620～626[Yan Jiaxin, Fang Nianqiao. Depositional environments, cycles and sequences of Chihsia Formation in Hubei Province. Earth Science, 1994, 19(5), 620～626]
[9]	颜佳新,杜远生.冰川发育对赤道地区碳酸盐沉积环境和沉积作用的影响.地质科技情报,1994,13(3): 48～56[Yan Jiaxin, Du Yuansheng. The influence of glaciation on low latitude shelf carbonate sedimentary environment and sedimentation: three cases from South China. Geol. Sci. and Technol. Information, 1994, 13(3), 48～56]
[10]	Ziegler A M, Gibbs M T, Hulver M L. A mini-atlas of oceanic water masses in the Permian Period. In: Shi G R, Archibold N W, Grover M, eds.The Permian of Eastern Tethys: Stratigraphy, Palaeogeography and Resources. Melbourne: The Royal Society of Victoria, 1998. 323～343
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[12]	Shi G R. Possible influence of Gondwana glaciation on low-latitude carbonate sedimentation and trans-equatorial faunal migration: the Lower Permian of South China. Geosciences Journal (Seoul), 2001, 5(1): 57～63
[13]	Yan J X, Carlson E H. Nodular celestite in the Chihsia Formation (Middle Permian) of South China. Sedimentology, 2003, 50: 265～278
[14]	Westphal H, Munnecke A. Limestone-marl alternations: a warm-water phenomenon? Geology, 2003, 31(3): 263～266
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Origin of Permian Chihsian Carbonates from South China and Its Geological Implications

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