机译:东海围州岛泥土泥土地区全新环境变化:来自底栖多峰集装的证据和稳定同位素记录
Chinese Acad Sci South China Sea Inst Oceanol Key Lab Ocean &
Marginal Sea Geol Innovat Acad South China Sea Ecol &
Environm Engn Guangzhou 510301 Peoples R China;
Chinese Acad Sci South China Sea Inst Oceanol Key Lab Ocean &
Marginal Sea Geol Innovat Acad South China Sea Ecol &
Environm Engn Guangzhou 510301 Peoples R China;
Chinese Acad Sci South China Sea Inst Oceanol Key Lab Ocean &
Marginal Sea Geol Innovat Acad South China Sea Ecol &
Environm Engn Guangzhou 510301 Peoples R China;
North Carolina State Univ Dept Marine Earth &
Atmospher Sci Raleigh NC USA;
Chinese Acad Sci South China Sea Inst Oceanol Key Lab Ocean &
Marginal Sea Geol Innovat Acad South China Sea Ecol &
Environm Engn Guangzhou 510301 Peoples R China;
Minist Nat Resources Key Lab Marine Sedimentol &
Environm Geol Inst Oceanog 1 Qingdao 266061 Peoples R China;
Ocean Univ China Coll Marine Geosci Qingdao 266100 Peoples R China;
Mud deposit; Yellow Sea warm current; East China Sea; Benthic foraminifera; Holocene; Oxygen and carbon isotope;
机译:东海围州岛泥土泥土地区全新环境变化:来自底栖多峰集装的证据和稳定同位素记录
机译:利用有孔虫组合和稳定的碳同位素对南海珠江口的全新世古环境进行早期和晚期重建
机译:早期和晚期全新居古环境重建珠江河口,南海采用多孔组装和稳定的碳同位素
机译:验证东海内层全新世东亚冬季季风粒度的新替代物
机译:英属哥伦比亚西温哥华岛峡湾埃芬汉姆湾的底栖有孔虫组合:对东北太平洋晚全新世古生产力的影响。
机译:采样地点季节和底物对科孚岛(希腊爱奥尼亚海)泻湖沉积物繁殖繁殖后的有孔虫组合的影响
机译:浮游和底栖有孔虫稳定同位素,ssT和温跃层温度,coccoliths和底栖有孔虫组合,以及沉积物岩心mD06-3067的生产力重建