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Alluvial Pollen on the North China Plain

Published online by Cambridge University Press:  20 January 2017

Xu Qinghai ,
Yang Xiaolan ,
Wu Chen ,
Meng Lingyao  and
Wang Zihui
Xu Qinghai
Affiliation:
Institute of Geography, Hebei Academy of Sciences, Shijiazhuang, 050011, China
Yang Xiaolan
Affiliation:
Institute of Geography, Hebei Academy of Sciences, Shijiazhuang, 050011, China
Wu Chen
Affiliation:
Institute of Geography, Hebei Academy of Sciences, Shijiazhuang, 050011, China
Meng Lingyao
Affiliation:
Institute of Geography, Hebei Academy of Sciences, Shijiazhuang, 050011, China
Wang Zihui
Affiliation:
Institute of Geography, Hebei Academy of Sciences, Shijiazhuang, 050011, China
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Abstract

Mordern alluvial pollen varies with geomorphic setting and depositional facies in sediments of the Yellow, Hutuo, and Luan rivers and in Baiyangdian and Hengshuihu lakes. Most of the arboreal pollen is derived from the mountains, whereas most of the nonarboreal pollen is derived from the plain itself. Alluvium dominated by Pinus pollen and Selaginella spores was deposited during a flood. Hydrodynamic sorting of alluvial pollen exists in the sediments of floodplain, central bar, natural levees, and point bar. In reconstructing the ancient vegetation and past climate based on pollen in alluvium, it is important to consider sedimentary facies and geomorphologic setting.

Type
Research Article
Information
Quaternary Research , Volume 46 , Issue 3 , November 1996 , pp. 270 - 280
Copyright
University of Washington

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References

Brush, G.S., and Brush, L.M. Jr., (1972). Transport of pollen in a sediment-laden channel: A laboratory study. American Journal of Science 272, 359–381.Google Scholar
Cheng, Guodong, (1991). “Modern Sedimentation and Its Model of the Yellow River Delta,” pp. 1–110. Geology Press, Beijung.Google Scholar
Fall, P. L., (1987). Pollen taphonomy in a canyon stream. Quaternary Research 28, 393–406.CrossRefGoogle Scholar
Hall, S. A., (1985). Quaternary pollen analysis and vegetational history of the southwest. In “Pollen Records of Late-Quaternary orth American Sediments” (Bryant, V. M. Jr., and Holoway, R. G., Eds.), pp. 95–123. American Association of Stratigraphic Palynologists, Dallas.Google Scholar
Hall, S. A., (1989). Letter to the editor. Pollen analysis and palaeoecology of alluvium. Quaternary Research 31, 435–438.CrossRefGoogle Scholar
Kong, Zhaochen, Du, Naiqiu, and Zhang, Zibin, (1982). Vegetational and climate changes in the Beijing area during the past 10000 years. Acta Botanica Sinica 24(2), 172–180.Google Scholar
Liu, Jinling, (1965). Pollen assemblages at the south piedmont area of the Yanshan Mountain. Quaternary Sciences of Sinica 4(1), 105–117.Google Scholar
Li, Wenyi, and Liang, Yulian, (1985). Vegetation and environment of the hypsi-thermal interval of Holocene in Estern Hebei Plain. Acta Botanica Sinica 27(6), 640–651.Google Scholar
Martin, P. S., (1963). “The Last 10000 Years: A Fossil Pollen Record of the America Southwest.” Univ. of Arisona Press, Tucson.Google Scholar
Solomon, A.M., Blasing, T.J., and Solomon, J. A., (1982). Interpretation of floodplain pollen in alluvial sediments from an arid region. Quaternary Research 18, 52–71.CrossRefGoogle Scholar
Tong, Guobang, Ke, Manhong, and Yu, Shufeng, (1983). Quaternary pollen assemblages and their geological significance on the Hebei Plain Marine Geology and Quaternary Geology 3(4), 99–103.Google Scholar
Wu, Chen, Zhu, Xuanqing, He, Naihua, Xu, Qinghai, Yuan, Wenying, Wang, Zihui, Shi, Derong, and Zhao, Mingxuan, (1991). Ancient channels on the North China Plain. Science In China (Series B) 2, 188–197.Google Scholar
Xu, Qinghai, , and Wu, Chen, (1985). Division of the Holocene strata and vegetation changes in Heilonggang region with pollen analysis. Journal of Hebei Academy of Sciences 1(1), 18–25.Google Scholar
Xu, Qinghai, Chen, Shuyin, Kong, Zhaochen, and Du, Naiqiu, (1988). Preliminary discussion of vegetation succession and climate change since the Holocene in the Baiyangdian Lake district. Acta Phytoecologica et Geobotanica Sinica 12(2), 143–151.Google Scholar
Xu, Qinghai, Wu, Chen, Wang, Zihui, Tong, Guobang, Wu, Shaojie, Zhang, Junpai, Du, Naiqiu, and Kong, Zhaochen, (1993). Approach to palaeoenvi-ronment in the west coast of Bohai Bay since 25000 a B.P. Acta Phytoeco-logica et Geobotanica Sinica 17(1), 20–32.Google Scholar
Xu, Qinghai, Wu, Chen, Meng, Lingyao, Wang, Zihui, Yang, Xiaolan, and Yao, Zuju, (1994a). “Study on pollen assemblages of different deposi-tional Facies on the North China Plain.” Xian Cartography Press, pp. 1–132.Google Scholar
Xu, Qinghai, Wu, Chen, Meng, Lingyao, Wang, Zihui, and Yang, Xiaolan, (1994b) Alluvial pollen assemblages at different geomorphological zones on the North China Plain. Chinese Science Bulletin 39(19), 1792–1795.Google Scholar
Yu, Fenglan, Qian, Jinping, and Li, Enqing, (1994). “Water resource and its utilization of the Luan River,” pp. 1–214 Science Press.Google Scholar
Zhou, Kunshu, (1965). Investigation and pollen analysis on two burried peats near Beijing. Quaternary Sciences of Sinica 4(1), 188–142.Google Scholar