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

YAN Jia xin

Article Contents

Article Navigation > Acta Sedimentologica Sinica > 2004 > 22(4): 579-587

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

[1]	黄思静.上扬子地台区晚古生代海相碳酸盐岩的碳、锶同位素研究.地质学报,1997, 71(1): 45～53[Huang Sijing. A sudy on carbon and strontium isotopes of Late Paleozoic carbonate rocks in the Upper Yangtze Platform. Acta Geologica Sinica, 1997, 71(1): 45～53]
[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
[11]	Shi G R, Grunt T A. Permian Gondwana-Boreal antitropicality with special reference to brachiopod faunas. Palaeogeogr., Palaeoclimat., Palaeoecol., 2000, 155: 239～263
[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
[15]	Wang Y, Jin Y G. Permian palaeogeographic evolution of the Jiangnan Basin, South China. Palaeogeogr., Palaeoclimat., Palaeoecol., 2000, 160(1-2): 35～44
[16]	Summerhayes C P. Upwelling system: evolution since Early Miocene. Geological Society Special Publication, London, 1992, 64: 1～519
[17]	Summerhayes C P. Upwelling in the ocean: modern processes and ancient records. Report of the Dahlem workshop, Berlin, 1994. 1～422
[18]	Pedersen T F, Calvert S E. Anoxia vs. productivity: what controls the formation of organic-carbon-rich sediments and sedimentary rocks. AAPG Bulletin, 1990, 74(4): 454～466
[19]	Sageman B B. Stratigraphic hierarchy of organic carbon-rich siltstones in deep-water facies, Brushy Canyon Formation (Guadalupian), Delaware Basin, West Texas. Geology, 1998, 26(5): 451～454
[20]	沙庆安,吴望始,傅家谟. 黔桂地区二叠系综合研究-兼论含油气性. 北京: 科学出版社,1990. 1～215[Sha Qing'an, Wu Wanshi, Fu Jiamo. Comprehensive research on Permian in Guizhou-Guangxi area and its petroleum potential. Beijing: Science Press, 1990. 1～215]
[21]	毕华.栖霞组燧石结核成因新证据.地层学杂志,1994,18(4): 214～216[Bi Hua. New evidences for the origin of the Chihsian chert nodules. Journal of Stratigraphy, 1994, 18(4), 214～216]
[22]	朱嗣昭. 赣西湘东地区下二叠统沉积中水玉髓的研究. 见:王英华,鲍志东,朱筱敏编,沉积学及岩相古地理学新进展. 北京:石油工业出版社,1995.53～55[Zhu Sizhao. Lutecite in the Lower Permian of Eastern Hunan-Western Jiangxi area. In: Wang Yinhua, Bao Zhidong, Zhu Xiaoming, eds. Progress in Sedimentology and Lithofacies. Beijing: Petroleum Industry Publishing House, 1995. 53～55]
[23]	何海清.浙江省栖霞组沉积微相,韵律,沉积旋回及层序地层分析.石油实验地质,1997,19(2): 127～130[He Haiqing. Depositional microfactes, rhythms, cycles and sequence stratigraphy of Qixia Formation in Zhejiang Province, China. Experimental Petroleum Geology, 1997, 19(2): 127～130]
[24]	颜佳新.论华南栖霞组中的菊花石.岩相古地理,1992,12(1): 47～51[Yan Jiaxin. Reviews on the chrysanthemum stones from the Qixia Formation in South China. Sedimentary Facies and Palaeogeography, 1992, 12(1): 47～51]
[25]	Baker B K, Bloomer S H. The origin of celestite in deep-sea carbonate sediments. Geochim. Cosmochim. Acta, 1988, 52: 335～339
[26]	Melim L A, Westphal H, Swart P K, et al. Questioning carbonate diagenetic paradigms: evidence from the Neogene of the Bahamas. Marine Geology, 2002, 185: 27～53
[27]	Canfield D E. Sulfate reduction in deep-sea sediments. American Journal of Science, 1991, 291(2): 177～188
[28]	Capone D G, Kiene R P. Comparison of microbial dynamics in marine and freshwater sediments: contrasts in anaerobic carbon catabolism. Limnol. Oceanogr., 1988, 33: 725～749
[29]	施春华,颜佳新.早期成岩作用过程中硫酸盐还原作用研究进展.广西地质,2001, 14(1): 21～26[Shi Chunhua, Yan Jiaxin, Han Xin. Development of sulfate reduction during early diagenesis. Guangxi Geology, 2001, 14(1): 21～26]
[30]	李文光.海泡石矿的成矿地质条件.吉林地质,1999,18(3): 61～67[Li Wenguang. The ore-forming geological features of sepiolite deposit and its prespective for prespecting ore. Jilin Geology, 1999. 18(3), 61～67]
[31]	李文光,张瑛.我国海泡石矿床成矿条件及成因类型初探.陕西地质,1999,17(1): 43～47[Li Wenguang, Zhang Ying. A preliminary discussion on the ore-forming conditions and genetic types of sepiolite deposits in China. Geology of Shaanxi, 1999,17(1): 43～47]
[32]	暨雄卓.海泡石原矿加工与橡胶应用研究.中国矿业,1998,7(6): 79～81[Ji Xiongzhuo. Researches on processing sea form and applying it in rubber. China Mineral-Resources Industry, 1998,7(6): 79～81]
[33]	周时光.朝天海泡石矿的开发利用方向.中国非金属矿工业导刊,2000,No.17: 42～45[Zhou Siguang. Exploration and utility of the Chaotian sepiolite. Chinese Bulletin of non-metallic Mine Industry, 2000, No.17: 42～45]
[34]	Singer A, Galan E. Palygorskite-sepiolite: occurrences, genesis and uses. Amsterdam: Elsevier, 1984. 1-352
[35]	杨振强,陈善庆,林金明,等."江南古陆"两侧早二叠世海泡石的形成环境及成矿预测.岩相古地理文集, 北京:地质出版社,1991. 1～46[Yang Zhengqiang, Chen Shanqing, Lin Jinming, et al. Sedimentary environments and forecast prospect of the Early Permian sepiolite deposits around the "Jiangnan Old Land". Collections of Lithofacies and Palaeogeography,Beijing: Geological Publishing House, 1991. 1～46]
[36]	章人俊,邱翠微,彭长琪, 等.湖南醴陵地区镁质粘土的特征及成因讨论.中国地质科学院宜昌地矿所所刊,1985, (9): 1～13[Zhang Renjun, Qiu Cuiwei, Peng Changqi, et al. The characteristics of magnesium-rich clay in Liling area, Hunan Province and a discussion on its genesis. Bull. Yichang Inst. Geol. Mineral Resources, CAGS, 1986, .9: 1～13]
[37]	杨振强,许俊文.萍乐坳陷海泡石的形成及后期变化.中国地质科学院宜昌地矿所所刊,1986, 12: 31～51[Yang Zhengqiang, Xu Junwen. The formation and post-sedimentary alternation of sepiolite in the Pingle Depression. Bull. Yichang Inst. Geol. Mineral Resources, CAGS, 1986, No.12: 31-51]
[38]	Liu D Y. Sedimentary sepiolite of the Early Permian period in South China. Clay Minerals, 1985, 20(4): 529～535
[39]	任磊夫.粘土矿物与粘土岩.北京:地质出版社,1992.135～136[Ren Leifu. Clay minerals and rocks. Beijing: Geological Publishing House, 1992. 135～136]
[40]	颜佳新,夏琼霞,Carlson E H. 华南栖霞组菊花石假象内正延性玉髓的成因及其地质意义.沉积学报, 2001, 19(3): 444～448[Yan Jiaxin, Xia Qiongxia, Carlson E H. Length-slow chalcedony in chrysanthemum stone of Chihsia Formation, South China and its geological implication. Acta Sedimentologica Sinica, 2001, 19(3): 444～448]
[41]	Sandberg P A. An oscillating trend in Phanerozoic nonskeletal carbonate mineralogy. Nature, 1983, 305: 19～22
[42]	颜佳新,伍明,李方林,等.湖北省巴东栖霞组沉积成岩作用地球化学特征研究.沉积学报,1998,16(4):78～84[Yan Jiaxin, Wu Ming, Li Fanglin, et al. Geochemistry of sedimentation and diagenesis in Qixia Formation (Early Permian) of Badong, Hubei Province. Acta Sedimentologica Sinica, 1998, 16(4), 78～84]
[43]	颜佳新,施春华,李军虹,等.华南地区栖霞组菊花状天青石的交代及其地质意义.岩石矿物学杂志, 2001, 20(1): 75～83[Yan Jiaxin, Shi Chunhua, Li Junhong,et al. Replacement of chrysanthemum-shaped celestite in the Chihsia Formation of South China and its geological implication. Acta Petrologica et Mineralogica, 2001, 20(1), 75～83]
[44]	颜佳新,张宽忠,Carlson E H.华南地区栖霞组"菊花石"假象与海泡石矿成因关系探讨.矿物岩石, 2000, 20(4): 1～5[Yan Jiaxin, Zhang Kuanzhong, E H Carlson, Remarks on origin of sepiolite with evidences from replacement history of nodular celestite in the Chihsia Formation of South China. Journal of Mineralogy and Petrology, 2000, 20(4): 1～5]
[45]	Mu X N, Riding R. Silicification of Permian calcareous algae from Nanjing, China. Geological Magazine, 1988, 125(2): 123～139
[46]	Bentor Y K. Phosphorites - the unsolved problem. SEPM Special Publication 29, 1980. 3～18
[47]	Odin G S, Letolle R. Glauconitization and phosphatization environments: a tentative comparison. SEPM Special Publication 29, 1980. 227～237
[48]	Allison M A, Riggs S R. Clay-mineral suites in cyclic Miocene sediments: a model for continental margin deposition in a mixed siliciclastic-phosphatic-dolomitic-biogenic system. Journal of Sedimentary Research, 1994, 64(2): 386～395
[49]	Riggs S R. Paleoceanographic model of Neogene phosphate deposition, U S Atlantic continental margin. Science, 1984, 223: 123～131
[50]	Baker P A, Burns S J. Occurrence and formation of dolomite in organic-rich continental margin sediments. AAPG Bulletin, 1985, 69: 1917～1930
[51]	颜佳新.非热带浅海碳酸盐岩研究新进展.地质科技情报,1991,10(4): 15～18[Yan Jiaxin. Reviews on the non-tropical shelf carbonates. Geol. Sci. and Technol. Inform., 1991, 10(4), 15～18]
[52]	James N P. The cool-water carbonate depositional realm. SEPM Special Publication, 1997, 56: 1-20
[53]	Hallock P, Schlager W. Nutrient excess and the demise of coral reefs and carbonate platforms. Palaios, 1986, 1: 389～398
[54]	Murchey B L, Jones D L. A mid-Permian chert event: widespread deposition of biogenic siliceous sediments in coastal, island arc and oceanic basins. Palaeogeogr., Paleoclimat., Palaeoecol, 1992., 96: 161～174
[55]	Kidder D L, Erwin D H. Secular distribution of biogenetic silica through the Phanerozoic: comparisons of silica-replaced fossils and bedded cherts at the series level. The Journal of Geology, 2001, 110: 509～522
[56]	Beauchamp B, Baud A. Growth and demise of Permian biogenic chert along northwest Pangea: evidence for end-Permian collapse of thermohalone circulation. Palaeogeogr. Palaeoclimat. Palaeoecol., 2002, 184: 37～63
[57]	Grotzinger J P, Knoll A H. Anomalous carbonate precipitates: is the Precambrian the key to the Permian? Palaio, 1995, 10: 578～596
[58]	Lowenstein T K, Timofeeff M N, Brennan S T, et al. Oscillations in Phanerozoic seawater chemistry: Evidences from fluid inclusions: Science, 2001, 294: 1086～1088
[59]	Kovalevich V M, Peryt T M, and Petrichenko O I. Secular variations in seawater chemistry during the Phanerozoic as indicated by brine inclusion in halite: The Journal of Geology, 1998, 106: 695～712
[60]	Parrish J T. Climate of the supercontinent Pangea. The Journal of Geology, 1993, 101: 215～233
[61]	颜佳新.东特提斯地区二叠-三叠纪古气候特征及其古地理意义.地球科学, 1999, 24(1): 13～20[Yan Jiaxin. Permian-Triassic paleoclimate of eastern Tethys and its paleogeographic implication. Earth Science-Journal of China University of Geosciences, 1999, 24(1), 13～20]
[62]	Tabor N J, Montanez I P. Shifts in late Paleozoic atmospheric circulation over western equatorial Pangea: insights from pedogenic mineral δ18O compositions. Geology, 2002, 30(12): 1127～1130
[63]	Rees P M, Ziegler A M, Gibbs M T, et al. Permian phytogeographic patterns and climate data/model comparisons. The Journal of Geology, 2002, 110(1): 1～31
[64]	Gibbs M T. Simulations of Permian climate and comparisons with climate-sensitive sediments. The Journal of Geology, 2002, 110(1): 33～55
[65]	Boyd P W. A mesoscale phytoplankton bloom in the polar Southern Ocean stimulated by iron fertilization. Nature, 2000, 407: 695～702
[66]	Soreghan G S, Soreghan M J. Atmospheric dust and algal dominance in the Late Paleozoic: a hypothesis. Journal of Sedimentary Research, 2002, 72(4): 457～461
[67]	Shimizu H. Sources and depositional environments of some Permian and Triassic cherts: significance of Rb-Sr and Sm-Nd isotopic and REE abundance data. The Journal of Geology, 2001, 109: 105～125
[68]	Millot G. Geology of Clays. New York: Springer Verlag, 1970, 262～276
[69]	McClellan G H, Van Kauwenbergh S J. Clay mineralogy of the phosphorites of the southeastern Unites States. In: Burnett W C, Riggs S R, eds. Phosphate deposits of the world, Vol. 3, Neogene to Modern Phosphorites. Cambridge: Cambridge University Press, 1989. 337～351
[70]	Sheldon R P. Phosphorites deposits of the Phosphoria Formation, western Unites States. In: Notholt A J G, Sheldon R P, Davidson D F, eds. Phosphate deposits of the world, Vol. 2, Phosphate rock resources. Cambridge: Cambridge University Press, 1989. 53～70
[71]	Munnecke A, Westphal H, Elrick M, et al. The mineralogical composition of precursor sediments of calcareous rhythmites - a new approach. International Journal of Earth Sciences, 2001, 90: 795～812

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Get Citation

PDF

XML

Article Metrics

Article views(775) PDF downloads(725) Cited by()

Proportional views

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.

HTML

Reference (71)

[1]	黄思静.上扬子地台区晚古生代海相碳酸盐岩的碳、锶同位素研究.地质学报,1997, 71(1): 45～53[Huang Sijing. A sudy on carbon and strontium isotopes of Late Paleozoic carbonate rocks in the Upper Yangtze Platform. Acta Geologica Sinica, 1997, 71(1): 45～53]
[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
[11]	Shi G R, Grunt T A. Permian Gondwana-Boreal antitropicality with special reference to brachiopod faunas. Palaeogeogr., Palaeoclimat., Palaeoecol., 2000, 155: 239～263
[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
[15]	Wang Y, Jin Y G. Permian palaeogeographic evolution of the Jiangnan Basin, South China. Palaeogeogr., Palaeoclimat., Palaeoecol., 2000, 160(1-2): 35～44
[16]	Summerhayes C P. Upwelling system: evolution since Early Miocene. Geological Society Special Publication, London, 1992, 64: 1～519
[17]	Summerhayes C P. Upwelling in the ocean: modern processes and ancient records. Report of the Dahlem workshop, Berlin, 1994. 1～422
[18]	Pedersen T F, Calvert S E. Anoxia vs. productivity: what controls the formation of organic-carbon-rich sediments and sedimentary rocks. AAPG Bulletin, 1990, 74(4): 454～466
[19]	Sageman B B. Stratigraphic hierarchy of organic carbon-rich siltstones in deep-water facies, Brushy Canyon Formation (Guadalupian), Delaware Basin, West Texas. Geology, 1998, 26(5): 451～454
[20]	沙庆安,吴望始,傅家谟. 黔桂地区二叠系综合研究-兼论含油气性. 北京: 科学出版社,1990. 1～215[Sha Qing'an, Wu Wanshi, Fu Jiamo. Comprehensive research on Permian in Guizhou-Guangxi area and its petroleum potential. Beijing: Science Press, 1990. 1～215]
[21]	毕华.栖霞组燧石结核成因新证据.地层学杂志,1994,18(4): 214～216[Bi Hua. New evidences for the origin of the Chihsian chert nodules. Journal of Stratigraphy, 1994, 18(4), 214～216]
[22]	朱嗣昭. 赣西湘东地区下二叠统沉积中水玉髓的研究. 见:王英华,鲍志东,朱筱敏编,沉积学及岩相古地理学新进展. 北京:石油工业出版社,1995.53～55[Zhu Sizhao. Lutecite in the Lower Permian of Eastern Hunan-Western Jiangxi area. In: Wang Yinhua, Bao Zhidong, Zhu Xiaoming, eds. Progress in Sedimentology and Lithofacies. Beijing: Petroleum Industry Publishing House, 1995. 53～55]
[23]	何海清.浙江省栖霞组沉积微相,韵律,沉积旋回及层序地层分析.石油实验地质,1997,19(2): 127～130[He Haiqing. Depositional microfactes, rhythms, cycles and sequence stratigraphy of Qixia Formation in Zhejiang Province, China. Experimental Petroleum Geology, 1997, 19(2): 127～130]
[24]	颜佳新.论华南栖霞组中的菊花石.岩相古地理,1992,12(1): 47～51[Yan Jiaxin. Reviews on the chrysanthemum stones from the Qixia Formation in South China. Sedimentary Facies and Palaeogeography, 1992, 12(1): 47～51]
[25]	Baker B K, Bloomer S H. The origin of celestite in deep-sea carbonate sediments. Geochim. Cosmochim. Acta, 1988, 52: 335～339
[26]	Melim L A, Westphal H, Swart P K, et al. Questioning carbonate diagenetic paradigms: evidence from the Neogene of the Bahamas. Marine Geology, 2002, 185: 27～53
[27]	Canfield D E. Sulfate reduction in deep-sea sediments. American Journal of Science, 1991, 291(2): 177～188
[28]	Capone D G, Kiene R P. Comparison of microbial dynamics in marine and freshwater sediments: contrasts in anaerobic carbon catabolism. Limnol. Oceanogr., 1988, 33: 725～749
[29]	施春华,颜佳新.早期成岩作用过程中硫酸盐还原作用研究进展.广西地质,2001, 14(1): 21～26[Shi Chunhua, Yan Jiaxin, Han Xin. Development of sulfate reduction during early diagenesis. Guangxi Geology, 2001, 14(1): 21～26]
[30]	李文光.海泡石矿的成矿地质条件.吉林地质,1999,18(3): 61～67[Li Wenguang. The ore-forming geological features of sepiolite deposit and its prespective for prespecting ore. Jilin Geology, 1999. 18(3), 61～67]
[31]	李文光,张瑛.我国海泡石矿床成矿条件及成因类型初探.陕西地质,1999,17(1): 43～47[Li Wenguang, Zhang Ying. A preliminary discussion on the ore-forming conditions and genetic types of sepiolite deposits in China. Geology of Shaanxi, 1999,17(1): 43～47]
[32]	暨雄卓.海泡石原矿加工与橡胶应用研究.中国矿业,1998,7(6): 79～81[Ji Xiongzhuo. Researches on processing sea form and applying it in rubber. China Mineral-Resources Industry, 1998,7(6): 79～81]
[33]	周时光.朝天海泡石矿的开发利用方向.中国非金属矿工业导刊,2000,No.17: 42～45[Zhou Siguang. Exploration and utility of the Chaotian sepiolite. Chinese Bulletin of non-metallic Mine Industry, 2000, No.17: 42～45]
[34]	Singer A, Galan E. Palygorskite-sepiolite: occurrences, genesis and uses. Amsterdam: Elsevier, 1984. 1-352
[35]	杨振强,陈善庆,林金明,等."江南古陆"两侧早二叠世海泡石的形成环境及成矿预测.岩相古地理文集, 北京:地质出版社,1991. 1～46[Yang Zhengqiang, Chen Shanqing, Lin Jinming, et al. Sedimentary environments and forecast prospect of the Early Permian sepiolite deposits around the "Jiangnan Old Land". Collections of Lithofacies and Palaeogeography,Beijing: Geological Publishing House, 1991. 1～46]
[36]	章人俊,邱翠微,彭长琪, 等.湖南醴陵地区镁质粘土的特征及成因讨论.中国地质科学院宜昌地矿所所刊,1985, (9): 1～13[Zhang Renjun, Qiu Cuiwei, Peng Changqi, et al. The characteristics of magnesium-rich clay in Liling area, Hunan Province and a discussion on its genesis. Bull. Yichang Inst. Geol. Mineral Resources, CAGS, 1986, .9: 1～13]
[37]	杨振强,许俊文.萍乐坳陷海泡石的形成及后期变化.中国地质科学院宜昌地矿所所刊,1986, 12: 31～51[Yang Zhengqiang, Xu Junwen. The formation and post-sedimentary alternation of sepiolite in the Pingle Depression. Bull. Yichang Inst. Geol. Mineral Resources, CAGS, 1986, No.12: 31-51]
[38]	Liu D Y. Sedimentary sepiolite of the Early Permian period in South China. Clay Minerals, 1985, 20(4): 529～535
[39]	任磊夫.粘土矿物与粘土岩.北京:地质出版社,1992.135～136[Ren Leifu. Clay minerals and rocks. Beijing: Geological Publishing House, 1992. 135～136]
[40]	颜佳新,夏琼霞,Carlson E H. 华南栖霞组菊花石假象内正延性玉髓的成因及其地质意义.沉积学报, 2001, 19(3): 444～448[Yan Jiaxin, Xia Qiongxia, Carlson E H. Length-slow chalcedony in chrysanthemum stone of Chihsia Formation, South China and its geological implication. Acta Sedimentologica Sinica, 2001, 19(3): 444～448]
[41]	Sandberg P A. An oscillating trend in Phanerozoic nonskeletal carbonate mineralogy. Nature, 1983, 305: 19～22
[42]	颜佳新,伍明,李方林,等.湖北省巴东栖霞组沉积成岩作用地球化学特征研究.沉积学报,1998,16(4):78～84[Yan Jiaxin, Wu Ming, Li Fanglin, et al. Geochemistry of sedimentation and diagenesis in Qixia Formation (Early Permian) of Badong, Hubei Province. Acta Sedimentologica Sinica, 1998, 16(4), 78～84]
[43]	颜佳新,施春华,李军虹,等.华南地区栖霞组菊花状天青石的交代及其地质意义.岩石矿物学杂志, 2001, 20(1): 75～83[Yan Jiaxin, Shi Chunhua, Li Junhong,et al. Replacement of chrysanthemum-shaped celestite in the Chihsia Formation of South China and its geological implication. Acta Petrologica et Mineralogica, 2001, 20(1), 75～83]
[44]	颜佳新,张宽忠,Carlson E H.华南地区栖霞组"菊花石"假象与海泡石矿成因关系探讨.矿物岩石, 2000, 20(4): 1～5[Yan Jiaxin, Zhang Kuanzhong, E H Carlson, Remarks on origin of sepiolite with evidences from replacement history of nodular celestite in the Chihsia Formation of South China. Journal of Mineralogy and Petrology, 2000, 20(4): 1～5]
[45]	Mu X N, Riding R. Silicification of Permian calcareous algae from Nanjing, China. Geological Magazine, 1988, 125(2): 123～139
[46]	Bentor Y K. Phosphorites - the unsolved problem. SEPM Special Publication 29, 1980. 3～18
[47]	Odin G S, Letolle R. Glauconitization and phosphatization environments: a tentative comparison. SEPM Special Publication 29, 1980. 227～237
[48]	Allison M A, Riggs S R. Clay-mineral suites in cyclic Miocene sediments: a model for continental margin deposition in a mixed siliciclastic-phosphatic-dolomitic-biogenic system. Journal of Sedimentary Research, 1994, 64(2): 386～395
[49]	Riggs S R. Paleoceanographic model of Neogene phosphate deposition, U S Atlantic continental margin. Science, 1984, 223: 123～131
[50]	Baker P A, Burns S J. Occurrence and formation of dolomite in organic-rich continental margin sediments. AAPG Bulletin, 1985, 69: 1917～1930
[51]	颜佳新.非热带浅海碳酸盐岩研究新进展.地质科技情报,1991,10(4): 15～18[Yan Jiaxin. Reviews on the non-tropical shelf carbonates. Geol. Sci. and Technol. Inform., 1991, 10(4), 15～18]
[52]	James N P. The cool-water carbonate depositional realm. SEPM Special Publication, 1997, 56: 1-20
[53]	Hallock P, Schlager W. Nutrient excess and the demise of coral reefs and carbonate platforms. Palaios, 1986, 1: 389～398
[54]	Murchey B L, Jones D L. A mid-Permian chert event: widespread deposition of biogenic siliceous sediments in coastal, island arc and oceanic basins. Palaeogeogr., Paleoclimat., Palaeoecol, 1992., 96: 161～174
[55]	Kidder D L, Erwin D H. Secular distribution of biogenetic silica through the Phanerozoic: comparisons of silica-replaced fossils and bedded cherts at the series level. The Journal of Geology, 2001, 110: 509～522
[56]	Beauchamp B, Baud A. Growth and demise of Permian biogenic chert along northwest Pangea: evidence for end-Permian collapse of thermohalone circulation. Palaeogeogr. Palaeoclimat. Palaeoecol., 2002, 184: 37～63
[57]	Grotzinger J P, Knoll A H. Anomalous carbonate precipitates: is the Precambrian the key to the Permian? Palaio, 1995, 10: 578～596
[58]	Lowenstein T K, Timofeeff M N, Brennan S T, et al. Oscillations in Phanerozoic seawater chemistry: Evidences from fluid inclusions: Science, 2001, 294: 1086～1088
[59]	Kovalevich V M, Peryt T M, and Petrichenko O I. Secular variations in seawater chemistry during the Phanerozoic as indicated by brine inclusion in halite: The Journal of Geology, 1998, 106: 695～712
[60]	Parrish J T. Climate of the supercontinent Pangea. The Journal of Geology, 1993, 101: 215～233
[61]	颜佳新.东特提斯地区二叠-三叠纪古气候特征及其古地理意义.地球科学, 1999, 24(1): 13～20[Yan Jiaxin. Permian-Triassic paleoclimate of eastern Tethys and its paleogeographic implication. Earth Science-Journal of China University of Geosciences, 1999, 24(1), 13～20]
[62]	Tabor N J, Montanez I P. Shifts in late Paleozoic atmospheric circulation over western equatorial Pangea: insights from pedogenic mineral δ18O compositions. Geology, 2002, 30(12): 1127～1130
[63]	Rees P M, Ziegler A M, Gibbs M T, et al. Permian phytogeographic patterns and climate data/model comparisons. The Journal of Geology, 2002, 110(1): 1～31
[64]	Gibbs M T. Simulations of Permian climate and comparisons with climate-sensitive sediments. The Journal of Geology, 2002, 110(1): 33～55
[65]	Boyd P W. A mesoscale phytoplankton bloom in the polar Southern Ocean stimulated by iron fertilization. Nature, 2000, 407: 695～702
[66]	Soreghan G S, Soreghan M J. Atmospheric dust and algal dominance in the Late Paleozoic: a hypothesis. Journal of Sedimentary Research, 2002, 72(4): 457～461
[67]	Shimizu H. Sources and depositional environments of some Permian and Triassic cherts: significance of Rb-Sr and Sm-Nd isotopic and REE abundance data. The Journal of Geology, 2001, 109: 105～125
[68]	Millot G. Geology of Clays. New York: Springer Verlag, 1970, 262～276
[69]	McClellan G H, Van Kauwenbergh S J. Clay mineralogy of the phosphorites of the southeastern Unites States. In: Burnett W C, Riggs S R, eds. Phosphate deposits of the world, Vol. 3, Neogene to Modern Phosphorites. Cambridge: Cambridge University Press, 1989. 337～351
[70]	Sheldon R P. Phosphorites deposits of the Phosphoria Formation, western Unites States. In: Notholt A J G, Sheldon R P, Davidson D F, eds. Phosphate deposits of the world, Vol. 2, Phosphate rock resources. Cambridge: Cambridge University Press, 1989. 53～70
[71]	Munnecke A, Westphal H, Elrick M, et al. The mineralogical composition of precursor sediments of calcareous rhythmites - a new approach. International Journal of Earth Sciences, 2001, 90: 795～812

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

Abstract

References

Proportional views

通讯作者: 陈斌, bchen63@163.com

Article Metrics

Proportional views

Related