Palynological assemblages from the holocene sediments of the Changjiang (Yangtze) River Delta and its implications

Wang Kaifa; Zhang Yulan; Jiang Hui; Han Xinbin

doi:10.1007/BF02850435

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Palynological assemblages from the holocene sediments of the Changjiang (Yangtze) River Delta and its implications

OriginalPaper | Updated：2023-05-16

- Palynological assemblages from the holocene sediments of the Changjiang (Yangtze) River Delta and its implications
- Palynological assemblages from the holocene sediments of the Changjiang (Yangtze) River Delta and its implications
- 海洋湖沼学报（英文） 1986年4卷第2期页码：196-210
- Affiliations：
  
  Department of Marine Geology Tongji University
- Author bio：
- Funds：
- DOI：10.1007/BF02850435
  中图分类号：
- 纸质出版：1986
- Accepted：
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Palynological assemblages from the holocene sediments of the Changjiang (Yangtze) River Delta and its implications[J]. 海洋湖沼学报（英文）, 1986,4(2):196-210.

Kaifa, W., Yulan, Z., Hui, J. et al. Palynological assemblages from the holocene sediments of the Changjiang (Yangtze) River Delta and its implications., Chin. J. Ocean. Limnol. 4, 196–210 (1986). https://doi.org/10.1007/BF02850435
Palynological assemblages from the holocene sediments of the Changjiang (Yangtze) River Delta and its implications[J]. 海洋湖沼学报（英文）, 1986,4(2):196-210. DOI： 10.1007/BF02850435.

Kaifa, W., Yulan, Z., Hui, J. et al. Palynological assemblages from the holocene sediments of the Changjiang (Yangtze) River Delta and its implications., Chin. J. Ocean. Limnol. 4, 196–210 (1986). https://doi.org/10.1007/BF02850435 DOI：

摘要

Abstract

The palynological study on the Quaternary sediments of 42 cores in the region of the Yangtze River Delta and the sections of 4 relics had been done since 1960. Palynological assemblages from the region of the Yangtze River Delta

showing obviously common characteristics but with slight differences because of the vast areas covered can be divided into five spores and pollen zones and three subzones in ascendant order: The lower limit of the Holocene period in the region of the Yangtze River Delta is also discussed in this paper. We consider that it is suitable for the limit to be dated 12

000 yr. B.P.

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references

Wang Kaifa et al., 1978. Some inferences of the climatic changes in Shanghai during the last 6,000 years based on spores and pollen analysis.Scientia Atmospherica Sinica 2(2): 139–144. (in Chinese with English abstract)

Wang Kaifa et al., 1980. Palynological study of Songze Site in Qingpu County, Shanghai.Kaogu Xuebao 1: 59–66. (in Chinese with English abstract)

Wang Kaifa et al., 1981. Spores and pollen assemblages of Tinglin Site in Jinshan County, Shanghai and its paleogeography. Geomorphologic Papers, Science Press, Beijing. pp. 329–333. (in Chinese)

Wang Kaifa et al., 1979. The spore-pollen and algal assemblages and its stratigraphy in the marine sediments in the north of East China Sea.Tongji Daxue Xuebao 2: 129–152. (in Chinese with English abstract)

Guo Xumin et al., 1979. Stratigraphy and areal subdivision of Holocene deposites of Yangtze Estuary region.Tongji Daxue Xuebao 2: 15–26. (in Chinese with English abstract)

Zhou Kunshu, 1965. Investigation of the two burried peat bogs near Beijing and their spores and pollen analysis.Quaternaria Sinica 4(1): 118–142 (in Chinese)

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Wang Kaifa, 1974. Palynological analysis peat-bogs of Siyao Lake, Mount Hsishan, Nanchang, Jiangsi Province.Acta Botanica Sinica 16(1): 83–93. (in Chinese with English abstract)

Flint, F., and Brandther, F., 1961. Climatic changes since the last interglacial epoch.American Journal of Science 259: 321–327.

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