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近190ka B.P.以来西太平洋暖池北缘上层海水结构和古生产力演化特征及其控制因素——来自钙质超微化石、有孔虫和同位素的证据

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DOI：10.11693/hyhz20080453053

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EVOLUTION IN UPPER WATER STRUCTURE AND PALEOPRODUCTITY IN THE NORTHERN MARGIN OF THE WESTERN PACIFIC WARM POOL AND ITS FORCING MECHANISM DURING THE LAST 190 ka B.P. EVIDENCE FROM NANNOFOSSIL,FORAMINIFERA AND THEIR ISOTOPE COMPOSITION

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