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于1986－1994年间，陆续对南黄海7个柱状样品进行了孢粉分析研究，结合14C测年数据，参考古地磁、热释光测年等分析资料，以其中3个主要岩芯剖面资料为代表，论述了南黄海陆架区15Ka以来的古气候环境演变．结果表明，在第四纪末次冰期冰消期中，气候曾剧烈波动，并逐渐由晚冰期向冰后期过渡．这一演变特点与全球气候背景下的中国东部地理环境相关．同时识别出3个短期降温和两个升温事件：其中A声带冷期出现在约15－14KaB．P，是冰消或早期的一次降温事件，可与最老仙女木期对比；A3亚带冷期出现在12－11Ka.B．P，可与新仙女木期对比．B2亚带冷期反映早全新世的一次降温事件．A2亚带相对暖期可能属布林升温波动，发生在14－13ka.B.P.。C带气候暖湿，为气候最适宜期，当属冰后期中的高温阶段，在中国东部沿海普遍存在，发生在中全新世8—3Ka．BP．．
From 1986 to 1994, 7 columnar samples from the South Yellow Sea were successively analyzed by means of spore-pollen analysis. According to 14C dating data, paleomagnetic data and thermoluminescence dating data, the data of 3 major core sections were , Elaborated on the paleoclimatic evolution of the South Yellow Sea shelf since 15Ka. The results show that during the last glacial ice extinction in Quaternary, the climate once violently fluctuated and gradually shifted from late glacial to late glacial ice. This evolutionary feature is associated with the geography of eastern China in a global climate context. Three short-term and two warming events were identified at the same time: A was about 15-14KaB. P, ice or early cooling event, with the oldest fairy wood phase contrast; A3 sub-band cold in 12-11Ka.B. P, with the new fairy wood period contrast. B2 sub-belt cold period reflects a cooling event in the early Holocene. The relative warming of the A2 sub-belt may be due to fluctuations in the Bollinger fever, occurring at 14-13ka.B.P .. C with warm and humid climate, the climate is the most suitable period, was the high temperature in the late ice stage, widespread in the eastern coast of China, occurred in the Middle Holocene 8-3Ka. BP. .