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地质学报  2002 

渤海沿岸黄土中有孔虫化石对古风场的指示意义

, PP. 409-412

Keywords: 黄土有孔虫季风丰度出现频次古风场渤海

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Abstract:

通过对渤海沿岸末次冰期黄土中有孔虫化石的研究。发现含有主要生活在南黄海和东海水体较深的浮游有孔虫化石:Globigerinaflaconensis、Globorotaliapumilio和Neogloboquadrinadutertrei,后者的含量高达6.4%,进一步对比沉积在不同地貌单元上黄土中有孔虫的丰度和浮游有孔虫化石出现的频率,发现沉积在北坡(阴坡)和南坡(阳坡)的有孔虫化石有显著的差异,北坡的有孔虫丰度和出现频次明显高于南坡,分析认为渤海沿岸的黄土不但具有西北风和东北风从渤海和北黄海搬运来的成分,还有东南风从南黄海和东海搬运带来的成分。

References

[1]  曹家欣,李培英,石宁.1987.山东庙岛群岛的黄土.中国科学(B辑),(10):1116~1123.
[2]  郭正堂,魏兰英,吕厚远,等.1999.晚第四纪风尘物质成分的变化及其环境意义.第四纪研究,(1):41~47.
[3]  李培英,程振波,吕厚远,等.1992.辽东海岸带黄土.地质学报,66(1):82~94.
[4]  刘绣铭,许同春,刘东生.1989.中国黄土磁化率各向异性与成因及其对第四纪研究的意义.中国科学(B辑),(4):441~448.
[5]  赵泉鸿.1996.渤海庙岛黄土中微体化石再研究.中国科学(D辑),26(5):445~451.
[6]  Cao Jiaxin, Li Peiying, Shi Ning. 1988. Study on the loess of Miaodao Island islands in Shandong Province. Scientia Sinica (Series B),31(1): 120~127.
[7]  Guo Zhengtang, Wei Lanying, Lü Houyuan, et al. 1999. Changes in the composition of late Pleistocene aeolian dust and the environmental significance. Quaternary Sciences, (1) :41~47 (in Chincse with English abstract).
[8]  Han J T. 1987. Study on the Loess in Penglai District, Shandong Province. In: Liu Tungsheng ed. Aspects of Loess Research China Ocean Press, Beijing, 76~84.
[9]  Liu Tungsheng, et al. 1985. Loess and environment. Beijing: Science Press.
[10]  Rao K K, Wasson R J, Kutty M K. 1989. Foraminifera from late Quaternary dune sands of the Thar Desert, India Palaios, 4 (2):168~180.
[11]  Wang Pinxian, Zhang Jijun, Zhao Quanhong. 1988. Foraminifera and Ostracoda in bottom sediments of the east China sea. Beijing: Ocean Press. 1~438 (in Chincse with English abstract).
[12]  程振波,李培英,吕厚远.1995.渤海东侧海岸带黄土中的放射虫.海洋科学,(6):59~64.
[13]  季峻峰,陈骏,鹿化煜.1998.陕西洛川黄土中伊利石成因的透射电镜证据.科学通报,43(19):2095~2098.
[14]  刘东生等.1985.黄土与环境.北京:科学出版社.
[15]  孙继敏,丁仲礼,刘东生,等.1995.黄土与古土壤磁组构测定在重建冬季风向上的初步应用.科学通报,40(21):1976~1978.
[16]  汪品先,章纪军,赵泉鸿,等.1988.东海底质中的有孔虫和介形虫.北京:海洋出版社,1~438.
[17]  An Z S, Kukla G, Porter S C, Xiao J L. 1991. Magnetic susceptibility evidence of monsoon variation on the loess plateau of central China during the last 130, 000 years. Quaternary Research, 36:29~36.
[18]  Bagnold R A. 1941. Physics of Blown Sand and Desert Dunes. London: Methuen & Co. , 1~265.
[19]  Cheng Zhenbo, Li Peiying, Lü Houyuan. 1995. The radiolaria in the coastal loess in east Bohai Sea. Marian Sciences, (6): 59~64 (in Chincse with English abstract).
[20]  Ji Junfeng, Chen Jun, Lu Huayu. 1998. The evidence of genesis of il lite under TEM in the loess at Luochuan, Shanxi province. Chinese Science Bulletin, 43(19): 2054~2098 (in Chincse).
[21]  Li Peiying, Cheng Zhenbo, Lü Houyuan, et al. 1992. The coastal zone loess of the Liaodong peninsula, Liaoning Province. Acta Geological Sinica, 66 (1): 82 ~ 94 (in Chincse with English abstract).
[22]  Liu T S, An Z S, Yuan B Y, et al. 1985. The loess paleosol sequence in China and climatic history. Episodes, (8): 21~28.
[23]  Liu Xiuming, Xu Tongchun, Liu Tungsheng. 1990. Anisotropy of magnetic susceptibility and origin of the Chinese loess and its significance to the Quaternary research. Scientia Sinica (Series B),33(2): 253~260.
[24]  Sun Jiming, Ding Zhongli, Liu Tungsheng, et al. 1995. Measurement of magnetic fabric of loess and paleosoil and its implications in reconstructing the palaeowind pattern in the Loess Plateau. Chinese Science Bulletin, 40(21) : 1976~1978 (in Chincse).
[25]  Zhao Quanhong. 1996. Study on the microfossils of the loess in Miaodao. Science in China (Series D), 26 (5): 445 ~ 451 (in Chincse).

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