Characteristics of Clay Mineral in South China Sea since Oligocene and Its Significance

TANG Song; SHAO Lei; ZHAO Quan-hong

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Article Navigation > Acta Sedimentologica Sinica > 2004 > 22(2): 337-342

TANG Song, SHAO Lei, ZHAO Quan-hong. Characteristics of Clay Mineral in South China Sea since Oligocene and Its Significance[J]. Acta Sedimentologica Sinica, 2004, 22(2): 337-342.

Citation:

TANG Song, SHAO Lei, ZHAO Quan-hong. Characteristics of Clay Mineral in South China Sea since Oligocene and Its Significance[J]. Acta Sedimentologica Sinica, 2004, 22(2): 337-342.

Characteristics of Clay Mineral in South China Sea since Oligocene and Its Significance

Key Laboratory of Marine Geology, Ministy of Education,Tongji University, Shanghai 200092

Received Date: 2003-05-28
Rev Recd Date: 2003-11-24
Publish Date: 2004-06-10

Abstract

The distribution of clay mineral in the sediments of ODP Leg 184 Site 1148, located on the north slope of the South China Sea and recovered 32.8Ma sediments,shows different character between 32.8-15.5 Ma and since 15.5-0Ma periods. In 32.8-15.5 Ma the sediments are dominated by smectite,whose relative abundance is as high as 70 percent,while the abundance of illite and chlorite increase gradually with the decrease of smectite into the last 15.5 Ma. Thus, the evolution of clay mineral in the sediments can be divided into two stages. 32.8-15.5 Ma is tectonic-controlled stage,in which the clay mineral record the speading history of South China Sea.Whereas the climate controlled the distribution of clay mineral since last 15.5 Ma.In this climate-controlled stage the distribution of clay mineral indicated that the temperature decreased gradually and droped rapidly at 3Ma.This result is well consistent with that of δ¹⁸O of benthic foraminifera.
- South China Sea,
- clay mineral,
- tectonic activity,
- climate change,
- ODP 1148

References

[1]	Chamley H. Clay Sedimentology.Berlin:Springer,1989.1～561
[2]	Singer A. The paleoclimatic interpretation of clay minerals in sediments. Earth Science Review, 1984, 21:251～293
[3]	Barker P F, Kennett J P, et al. Glacial history of Antarctica.Nature,1987,389:115-116
[4]	Clift P, Lee J I, Clark M K, et al. Erosional response of South China to arc rifting and monsoonal strengthening; a record from the South China Sea. Marine Geology, 2002,184:207～226
[5]	Wang P, Prell W L, Blum P,et al. Proceedings of the Ocean Drilling Program, Initial Reports.V184(CD-ROM).Nature Science Found & Joint Oceanography Inst,Inc,2000
[6]	赵杏媛,张有瑜.粘土矿物与粘土矿物分析.北京:海洋出版社,1990.73～166[Zhao Xingyuan,Zhang Youyu. Clay mineral and its analysis. Beijing: Ocean Press,1990.73～166]
[7]	张乃娴,李幼琴,赵惠敏, 等. 粘土矿物研究方法. 北京:科学出版社,1990.1～97[ Zhang Naixian,Li Youqin,Zhao Huimin,et al. Analytical technique of clay mineral. Beijing : Science Press, 1990.1～97]
[8]	林西生,应凤祥,郑乃萱, 等.X射线衍射分析技术及其地质应用.北京:石油工业出版社,1990.1～148[ Lin Xisheng,Ying Fengxiang,Zheng Naixuan,et al. Analytical technique of X-ray diffraction and its geological application.Beijing:Petroleum Industry Press,1990. 1～148]
[9]	Taylor B, Hayes D E. The tectonic evolution of the South China Basin. In: Hayes D E ed.The teceonic and geologic evolution of southeast Asian seas and islands. Geophysics Monography AGU, Washington,1980,27:89～104
[10]	Taylor B, Hayes D E. Origin and histoty of the South China Sea basin. In: Hayes D E ed. The teceonic and geologic evolution of southeast Asian seas and islands. Geophysics Monography, AGU,Washington,1983,27:23～56
[11]	Lee T Y, Lawver L A. Cenozoic plate reconstruction of the South China Sea region. Tectonophyics, 1994,235:149～180
[12]	Briais A, Patriat P, Tapponnier. Updated interpretation of magnetic anomalies and seafloor spreading stages in the South China Sea:Implications for the tertiary tectonics of sou- theast Asia. Journal of Geophysics Research,1993,98:6299～6328
[13]	Cande S C, Kent D V.A new geomagnetic polarity time scale for the late Cretaceous and Cenozoic. Journal of Geophysics Research,1992,97:13917～13951
[14]	Berggren W A, Kent D V, Swisher Ⅲ C C, et al. A revised Cenozoic geochronology and chronostratigraphy.In:Berggren W A,et al.eds.Geochronology,Time Scales and Global Stratigraphic Correlation.Spec PubI SEPM 54,1995.129～212
[15]	李乃胜,赵松龄,鲍.瓦西里耶夫.西北太平洋边缘海地质. 哈尔滨:黑龙江教育出版社,2000.522～524[ Li Naisheng, Zhao Songling, Wasiliev. Geology of Marinal Seas in the Northwest Pacific. Haerbin: Heilongjiang Education Press, 2000.522～524]
[16]	刘以宣.南海新构造与地壳稳定性.北京:科学出版社,1994.35-36[ Liu Yixuan.Neotectonics and Crustal Stability of South China Sea. Beijing: Science Press,1994.35-36]
[17]	许东禹,刘锡清,张训华.中国近海地质.北京:地质出版社,1997.88～90,255～260 [Xu DongYu, Liu Xiqing, Zhang Xunhua. China Offshore Geology. Beijing: Geological Publishing House, 1997.88～90,255～260]
[18]	刘昭蜀,赵焕庭,范时清, 等.南海地质.北京:科学出版社,2002.494-501 [Liu Zhaoshu,Zhao Huanting,Fan Shiqing, et al. Geology of the South China Sea. Beijing: Science Press, 2002.494-501]
[19]	金性春,周祖翼,汪品先.大洋钻探与中国地球科学. 上海: 同济大学出版社,1995.79～98, 216～222[Jin Xingchun, Zhou Zuyi, Wang Pinxian. Ocean Drilling Program and Earth Sciences in China.Shanghai: Tongji University Press,1995.79～98,216～222]
[20]	Miller K G, Faribanks R G, Mountain G S. Tertiary oxygen isotope synthesis, sea level history, and continental margin erosion. Paleoceanography,1987,2(1):1～19
[21]	Haq B J, Hardenbol J, Vail P R. Chronology of fluctuating sea-levels since the Triassic. Science, 1987, 235:1156～1166
[22]	赵泉鸿,翦知湣,王吉良,等.南海北部晚新生代氧同位素地层学.中国科学,2001,31:800～807 [Zhao Quanhong, Jian Zhimin, Wang Jiliang, et al. Neogene oxygen isotopic stratigraphy,ODP site 1148,northern South China Sea. Science in China, 2001,31:800～807]
[23]	汤艳杰,贾建业,谢先德.粘土矿物的环境意义.地学前缘,2002,9(2):337～344 [Tang Yanjie, Jia Jianye, Xie Xiande. Environment significance of clay minerals.Earth Science Frontiers, 2002,9(2):337-344]
[24]	Griffin J J, Windom H, Goldberg E D. The distribution of clay minerals in the world oceans. Deep -Sea Research,1968,15:433～459
[25]	吴国瑄,覃军干,茅绍智.南海深海相渐新统孢粉记录.科学通报,2003,48(17):1868～1871[Wu Guoxuan, Qin Jungan, Mao Shaozhi. The Oligocene record of spore and pollen in South China Sea. Chinese Science Bulletin, 2003,48(17):1868～1871]
[26]	Li Q, Jian Z, Li B. Oligocene-Miocene planktonic foraminifera biostratigraphy of Site 1148,northern South China Sea. In: Prell W, et al. Proc ODP Science Result,184 (in press)
[27]	陈晓良,赵泉鸿,翦知湣.南海北部ODP1148站中新世以来的碳酸盐含量变化及其古环境意义. 海洋地质与第四纪地质,2002,22(2):69～74[Chen Xiaoliang, Zhao Quanhong, Jian Zhimin. Carbonate content changes since the Miocene and paleoenvironmental implications, ODP Site 1148, northern South China Sea. Marine Geology & Quaternary,2002,22(2):69～74]
[28]	Zhao Quanhong. Late Cainozoic ostracod faunas and paleoenvironmental changes at ODP 1148, South China Sea. Marine Micropaleontology,(in press)
[29]	刘志飞,Trentesaux A,Clemens S C,等.南海北坡ODP1146站第四纪粘土矿物记录:洋流搬运与东亚季风演化.中国科学(D辑),2003,33(3):271～280[Liu Zhifei,Trentesaux A, Clemens S C, et al. Quaternary clay mineralogy in the northern South China Sea (ODP1146):implications for oceanic current transport and East monsoon evolution. Science in China(D), 2003, 33(3): 271 ～280]

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通讯作者: 陈斌, bchen63@163.com

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Characteristics of Clay Mineral in South China Sea since Oligocene and Its Significance

Key Laboratory of Marine Geology, Ministy of Education,Tongji University, Shanghai 200092

Received Date: 2003-05-28

Rev Recd Date: 2003-11-24

Publish Date: 2004-06-10

Key words:

Abstract: The distribution of clay mineral in the sediments of ODP Leg 184 Site 1148, located on the north slope of the South China Sea and recovered 32.8Ma sediments,shows different character between 32.8-15.5 Ma and since 15.5-0Ma periods. In 32.8-15.5 Ma the sediments are dominated by smectite,whose relative abundance is as high as 70 percent,while the abundance of illite and chlorite increase gradually with the decrease of smectite into the last 15.5 Ma. Thus, the evolution of clay mineral in the sediments can be divided into two stages. 32.8-15.5 Ma is tectonic-controlled stage,in which the clay mineral record the speading history of South China Sea.Whereas the climate controlled the distribution of clay mineral since last 15.5 Ma.In this climate-controlled stage the distribution of clay mineral indicated that the temperature decreased gradually and droped rapidly at 3Ma.This result is well consistent with that of δ¹⁸O of benthic foraminifera.

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Reference (29)

[1]	Chamley H. Clay Sedimentology.Berlin:Springer,1989.1～561
[2]	Singer A. The paleoclimatic interpretation of clay minerals in sediments. Earth Science Review, 1984, 21:251～293
[3]	Barker P F, Kennett J P, et al. Glacial history of Antarctica.Nature,1987,389:115-116
[4]	Clift P, Lee J I, Clark M K, et al. Erosional response of South China to arc rifting and monsoonal strengthening; a record from the South China Sea. Marine Geology, 2002,184:207～226
[5]	Wang P, Prell W L, Blum P,et al. Proceedings of the Ocean Drilling Program, Initial Reports.V184(CD-ROM).Nature Science Found & Joint Oceanography Inst,Inc,2000
[6]	赵杏媛,张有瑜.粘土矿物与粘土矿物分析.北京:海洋出版社,1990.73～166[Zhao Xingyuan,Zhang Youyu. Clay mineral and its analysis. Beijing: Ocean Press,1990.73～166]
[7]	张乃娴,李幼琴,赵惠敏, 等. 粘土矿物研究方法. 北京:科学出版社,1990.1～97[ Zhang Naixian,Li Youqin,Zhao Huimin,et al. Analytical technique of clay mineral. Beijing : Science Press, 1990.1～97]
[8]	林西生,应凤祥,郑乃萱, 等.X射线衍射分析技术及其地质应用.北京:石油工业出版社,1990.1～148[ Lin Xisheng,Ying Fengxiang,Zheng Naixuan,et al. Analytical technique of X-ray diffraction and its geological application.Beijing:Petroleum Industry Press,1990. 1～148]
[9]	Taylor B, Hayes D E. The tectonic evolution of the South China Basin. In: Hayes D E ed.The teceonic and geologic evolution of southeast Asian seas and islands. Geophysics Monography AGU, Washington,1980,27:89～104
[10]	Taylor B, Hayes D E. Origin and histoty of the South China Sea basin. In: Hayes D E ed. The teceonic and geologic evolution of southeast Asian seas and islands. Geophysics Monography, AGU,Washington,1983,27:23～56
[11]	Lee T Y, Lawver L A. Cenozoic plate reconstruction of the South China Sea region. Tectonophyics, 1994,235:149～180
[12]	Briais A, Patriat P, Tapponnier. Updated interpretation of magnetic anomalies and seafloor spreading stages in the South China Sea:Implications for the tertiary tectonics of sou- theast Asia. Journal of Geophysics Research,1993,98:6299～6328
[13]	Cande S C, Kent D V.A new geomagnetic polarity time scale for the late Cretaceous and Cenozoic. Journal of Geophysics Research,1992,97:13917～13951
[14]	Berggren W A, Kent D V, Swisher Ⅲ C C, et al. A revised Cenozoic geochronology and chronostratigraphy.In:Berggren W A,et al.eds.Geochronology,Time Scales and Global Stratigraphic Correlation.Spec PubI SEPM 54,1995.129～212
[15]	李乃胜,赵松龄,鲍.瓦西里耶夫.西北太平洋边缘海地质. 哈尔滨:黑龙江教育出版社,2000.522～524[ Li Naisheng, Zhao Songling, Wasiliev. Geology of Marinal Seas in the Northwest Pacific. Haerbin: Heilongjiang Education Press, 2000.522～524]
[16]	刘以宣.南海新构造与地壳稳定性.北京:科学出版社,1994.35-36[ Liu Yixuan.Neotectonics and Crustal Stability of South China Sea. Beijing: Science Press,1994.35-36]
[17]	许东禹,刘锡清,张训华.中国近海地质.北京:地质出版社,1997.88～90,255～260 [Xu DongYu, Liu Xiqing, Zhang Xunhua. China Offshore Geology. Beijing: Geological Publishing House, 1997.88～90,255～260]
[18]	刘昭蜀,赵焕庭,范时清, 等.南海地质.北京:科学出版社,2002.494-501 [Liu Zhaoshu,Zhao Huanting,Fan Shiqing, et al. Geology of the South China Sea. Beijing: Science Press, 2002.494-501]
[19]	金性春,周祖翼,汪品先.大洋钻探与中国地球科学. 上海: 同济大学出版社,1995.79～98, 216～222[Jin Xingchun, Zhou Zuyi, Wang Pinxian. Ocean Drilling Program and Earth Sciences in China.Shanghai: Tongji University Press,1995.79～98,216～222]
[20]	Miller K G, Faribanks R G, Mountain G S. Tertiary oxygen isotope synthesis, sea level history, and continental margin erosion. Paleoceanography,1987,2(1):1～19
[21]	Haq B J, Hardenbol J, Vail P R. Chronology of fluctuating sea-levels since the Triassic. Science, 1987, 235:1156～1166
[22]	赵泉鸿,翦知湣,王吉良,等.南海北部晚新生代氧同位素地层学.中国科学,2001,31:800～807 [Zhao Quanhong, Jian Zhimin, Wang Jiliang, et al. Neogene oxygen isotopic stratigraphy,ODP site 1148,northern South China Sea. Science in China, 2001,31:800～807]
[23]	汤艳杰,贾建业,谢先德.粘土矿物的环境意义.地学前缘,2002,9(2):337～344 [Tang Yanjie, Jia Jianye, Xie Xiande. Environment significance of clay minerals.Earth Science Frontiers, 2002,9(2):337-344]
[24]	Griffin J J, Windom H, Goldberg E D. The distribution of clay minerals in the world oceans. Deep -Sea Research,1968,15:433～459
[25]	吴国瑄,覃军干,茅绍智.南海深海相渐新统孢粉记录.科学通报,2003,48(17):1868～1871[Wu Guoxuan, Qin Jungan, Mao Shaozhi. The Oligocene record of spore and pollen in South China Sea. Chinese Science Bulletin, 2003,48(17):1868～1871]
[26]	Li Q, Jian Z, Li B. Oligocene-Miocene planktonic foraminifera biostratigraphy of Site 1148,northern South China Sea. In: Prell W, et al. Proc ODP Science Result,184 (in press)
[27]	陈晓良,赵泉鸿,翦知湣.南海北部ODP1148站中新世以来的碳酸盐含量变化及其古环境意义. 海洋地质与第四纪地质,2002,22(2):69～74[Chen Xiaoliang, Zhao Quanhong, Jian Zhimin. Carbonate content changes since the Miocene and paleoenvironmental implications, ODP Site 1148, northern South China Sea. Marine Geology & Quaternary,2002,22(2):69～74]
[28]	Zhao Quanhong. Late Cainozoic ostracod faunas and paleoenvironmental changes at ODP 1148, South China Sea. Marine Micropaleontology,(in press)
[29]	刘志飞,Trentesaux A,Clemens S C,等.南海北坡ODP1146站第四纪粘土矿物记录:洋流搬运与东亚季风演化.中国科学(D辑),2003,33(3):271～280[Liu Zhifei,Trentesaux A, Clemens S C, et al. Quaternary clay mineralogy in the northern South China Sea (ODP1146):implications for oceanic current transport and East monsoon evolution. Science in China(D), 2003, 33(3): 271 ～280]

Characteristics of Clay Mineral in South China Sea since Oligocene and Its Significance

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