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南黄海EY02-2孔碳酸盐含量特征与沉积物来源
引用本文:庄丽华,阎军,常凤鸣,李铁刚.南黄海EY02-2孔碳酸盐含量特征与沉积物来源[J].海洋科学,2004,28(1):8-10.
作者姓名:庄丽华  阎军  常凤鸣  李铁刚
作者单位:中国科学院,海洋研究所,山东,青岛,266071
摘    要:南黄海中部泥质区EY02—2孔柱样碳酸盐含量在0~34.55%之间变化,呈现为大西洋型CaCO3溶解旋回;冰后期以来碳酸盐高含量与高碳酸盐的现代黄河和废黄河物质有关;而末次间冰期碳酸盐极高含量与贝壳含量有关。

关 键 词:南黄海  碳酸盐含量  沉积物来源  贝壳含量
文章编号:1000-3096(2004)01-0008-03
收稿时间:2002/12/27 0:00:00
修稿时间:2003/3/28 0:00:00

Carbonate content character and sediment source from the core EY02-2 in the southern Yellow Sea
ZHUANG Li-hua,YAN Jun,CHANG Feng-ming,LI Tie-gang.Carbonate content character and sediment source from the core EY02-2 in the southern Yellow Sea[J].Marine Sciences,2004,28(1):8-10.
Authors:ZHUANG Li-hua  YAN Jun  CHANG Feng-ming  LI Tie-gang
Abstract:The carbonate content varied from 0 to 34.55% in the column of the drilling core EY02-2, the dissolved cycle appeared to be the carbonate dissolved cycle of the Atlantic Mode. The higher carbonate content related to materials of modern and old Yellow River in the postglacial period, while the peak carbonate content related to shell fragment in the sediment during the last interglacial period.
Keywords:the southern Yellow Sea  carbonate content  sediment source
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