Middle Holocene warm period and sea level high in coastal areas, North China

Meng Guanglan; Han Yousong; Wang Shaoqing

doi:10.1007/BF02894247

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Middle Holocene warm period and sea level high in coastal areas, North China

Updated：2023-05-16

- Middle Holocene warm period and sea level high in coastal areas, North China
- Journal of Oceanology and Limnology Vol. 23, Issue 2, Pages: 252-258(2005)
- Affiliations：
  
  Institute of Oceanology Chinese Academy of Sciences
- Author bio：
- Funds：
- DOI：10.1007/BF02894247
  CLC：
- Published：2005
- Accepted：
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Guanglan, M., Yousong, H. & Shaoqing, W. Middle Holocene warm period and sea level high in coastal areas, North China., Chin. J. Ocean. Limnol. 23, 252–258 (2005). https://doi.org/10.1007/BF02894247
DOI：

Guanglan, M., Yousong, H. & Shaoqing, W. Middle Holocene warm period and sea level high in coastal areas, North China., Chin. J. Ocean. Limnol. 23, 252–258 (2005). https://doi.org/10.1007/BF02894247 DOI：

摘要

Abstract

Relevant geological

geographical

archaeological data were collected to study the characteristics of middle Holocene warm period and sea level high on North China coast. Middle Holocene climate and sea level change on North China coast were correlated to warm marine environment events in about 8-3 ka B.P. The sea level in about 8 ka B.P. was higher than present mean sea level

then fluctuated for 5 000 years and after that it became even in 3 ka B.P. The highest sea level occurred in about 6-5 ka B.P.; the maximum was about 2–3 m and minimum was about 1–2 m.

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references

Kong, Z. and N. Du, 1990. Preliminary study on Holocene vegetation during high-temperature times and climate in some areas of China.Marine Geology & Quaternary Geology 10(1): 99–102. (in Chinese)

Han, Y. and G. Meng, 1986. Changes of paleogeographical environment of the Qingdao Coast during the past 20 000 years.Oceanol. Limnol. Sin. 17(3): 196–205. (in Chinese)

Meng, G and S. Wang, 1987. Studies on the Quaternary sporo-pollen assemblage from the Bohai Sea drilling core Bc-1 and its paleoclimate.Oceanol. Limnol. Sin. 18(3): 253–263. (in Chinese)

Yang, Z, Y. Li, Q. Ding and B. Yi, 1979. Some fundamental problems of Quaternary geology of the Eastern Hebei plain.Acta Geologica Sin. 53(4): 263–278. (in Chinese)

Luo, B., Y. Wang, et al., 1982. Studies on the biogeography and paleoclimate of Eastern China during the past 70 000 years.Bulletin Tianjin Institute Geol. Min. Res. 5: 107–114. (in Chinese)

Li, W. and Y. Liang, 1985. Vegetation and environment of the hypsithermal interval of Holocene in the eastern Hebei plain.Acta Botanica Sin. 27(6): 640–651. (in Chinese)

Zhou, B., 1982.Alligater sinensis fossils in Neolithic Age relics at Wangyin of Yanzhou, Shandong Province.Acta Arcgeology Sin. 2: 251–259. (in Chinese)

Li, X., 1984. The characteristics of Holocene climatic changes from the temporal and spatial distributions ofElaphurus davidianus subfossils in China. Selected Papers Form the Ist National C Symposium Science Press, Beijing. p. 186–193. (in Chinese)

Han, Y., 1980. Ostracean reefs and the Xinhe paleocoastline. Studia Marine Sin, Science press, Beijing, Science press, China.16: 59–65. (in Chinese)

Han, Y. and G. Meng, 1984. Holocene transgression and sea-level changes in the area of Jiaozhou Bay.Science Bulletin 29(20): 1 255–1 258. (in Chinese)

Zheng, S., Z. Z. Zhong and X. Wang, 1978. Quaternary foraminifera of the Dayuzhang irrigation area, Shandong Province, and a preliminary attempt at interpretation of its depositional environment. Studia Marina Sin. Science Press, Beijing, China.13: 16–30. (in Chinese)

Wang, S., 1979. A Preliminary study of Laizhou Bay west coast marine strata and their depositional environment in Late Quaternary.Oceanol Limnol Sin. 10(1): 9–22. (in C Chinese)

Li, Y. and F. An, 1985. The Quaternary micropaleontological fossils in Tianjin plain and their paleogeographic significance.Acta Geographica Sin. 40(2): 155–167. (in Chinese)

Wang, H., 1983. Expansion and contraction of Baiyangdian Lake since 10 000 years.Geographical Researce 2(3): 8–18. (in Chinese)

Han, Y., G. Meng, S. Wang and H. Song, 1988. On “environment tolerance zone of organisms” and bioclimato frontier-discussion on the paleenvironment of Eastern China coast.Marine Sciences 5: 15–18. (in Chinese)

Zhuang, Z. and Z. Lin, 1983. Paleocoastline in Holocene of the northwestern part of the Shandong Peninsula.Journal of Shandong College of Oceanology 13(3): 25–28. (in Chinese)

Zhao, X. and J. Zhang, 1980. The shell ridge of the Bohai Bay west coast.Science Bulletin 25(6): 279–281. (in Chinese)

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