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GAO SHANMING,LI YUANFANG. 1985. SEA LEVEL FLUCTUATION ALONG THE NORTHERN COAST OF BOHAI GULF ABOUT 2000 YEARS BP. Acta Oceanologica Sinica, (2):244-253
SEA LEVEL FLUCTUATION ALONG THE NORTHERN COAST OF BOHAI GULF ABOUT 2000 YEARS BP
SEA LEVEL FLUCTUATION ALONG THE NORTHERN COAST OF BOHAI GULF ABOUT 2000 YEARS BP
Received:June 29, 1983  Revised:July 10, 1984
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Author NameAffiliation
GAO SHANMING Institute of Geography, Academia Sinica, Beijing 
LI YUANFANG Institute of Geography, Academia Sinica, Beijing 
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Abstract:
      Sea ingressions have happened twice in the Bohai Gulf since the Holocene.In the Mid-Holo-cene (about 6000 yrs BP) the sea reached the farthest inland and flooded the area about 4 meters ASL.Later, the seawater retrograded gradually and formed a coastal plain.It was once again submerged about 2000 BP, resulting in the submergence of large-scale cultural remains at about 2.5-3 m ASL from the Warring States to the Western Han Dynasty by marine accumulations, or the overlap of peat and clay layers of continental facies by the coastal dunes about 3000 BP.
中文摘要:
      Sea ingressions have happened twice in the Bohai Gulf since the Holocene.In the Mid-Holo-cene (about 6000 yrs BP) the sea reached the farthest inland and flooded the area about 4 meters ASL.Later, the seawater retrograded gradually and formed a coastal plain.It was once again submerged about 2000 BP, resulting in the submergence of large-scale cultural remains at about 2.5-3 m ASL from the Warring States to the Western Han Dynasty by marine accumulations, or the overlap of peat and clay layers of continental facies by the coastal dunes about 3000 BP.
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