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Cheng Zhenbo,Fu Mingzuo,Ju Xiaohua. 1997. The geological significance of fossils in the coastal loess in the Bohai Straits and Liaodong Peninsula. Acta Oceanologica Sinica, (1):71-83
The geological significance of fossils in the coastal loess in the Bohai Straits and Liaodong Peninsula
The geological significance of fossils in the coastal loess in the Bohai Straits and Liaodong Peninsula
Received:March 15, 1996  Revised:May 25, 1996
DOI:
Key words:Coastal loess  material source  fossil organisms  paleoclimate
中文关键词:  Coastal loess  material source  fossil organisms  paleoclimate
基金项目:
Author NameAffiliation
Cheng Zhenbo First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China 
Fu Mingzuo First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China 
Ju Xiaohua First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China 
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Abstract:
      Based on the analysis of the characteristics of the fossils (mollusks,Radiolaria,planktonic and benthicForaminifera and Ostracoda) found in the four loess profiles located respectively at Heishigou and Beizhuang Villages on Daheishan Island in the Miaodao Islands in the Bohai Straits,and Daweijia and Yujiawaizi Villages in Jinzhou County,Liaodong Peninsula,the distribution and abundance variation of the fossils in vertical profiles are studied,the source of coastal loess is probed and the relationship between loess deposition and paleoclimatic environment as well as sea-level changes is discussed.
中文摘要:
      Based on the analysis of the characteristics of the fossils (mollusks,Radiolaria,planktonic and benthicForaminifera and Ostracoda) found in the four loess profiles located respectively at Heishigou and Beizhuang Villages on Daheishan Island in the Miaodao Islands in the Bohai Straits,and Daweijia and Yujiawaizi Villages in Jinzhou County,Liaodong Peninsula,the distribution and abundance variation of the fossils in vertical profiles are studied,the source of coastal loess is probed and the relationship between loess deposition and paleoclimatic environment as well as sea-level changes is discussed.
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