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综合分析黄河源区—青海玛多地区斗格涌盆地钻孔剖面的孢粉及易溶盐等气候代用指标，揭示了该区１３０ｋａＢＰ以来的古气候演变规律。即：１３０．０—１１０．０ｋａＢＰ寒冷干旱；１１０．０—８２．０ｋａＢＰ寒温较湿；８２．０—１０．４ｋａＢＰ寒冷干旱；１０．４ｋａＢＰ至现代（即全新世）温湿冷干交替。全新世古气候又可划分为３期：早全新世升温期（１０．４—７．５ｋａＢＰ）（Ａｎａｔｈｅｒｍａｌ）；中全新世大暖期（７．５—３．５ｋａＢＰ）（Ｍｅｇａｔｈｅｒｍａｌ）；晚全新世降温期（３．５ｋａＢＰ至今）（Ｋａｔａｔｈｅｒｍａｌ）。本区古气候总的规律是：冷期长且比全球其它地方提前，暖期短且开始时期滞后。全新世以来气候波动具有千年尺度的振荡规律，晚全新世至今，气温有逐渐降低，湿度逐渐变干的趋势。
A comprehensive analysis was made of the climatic proxies such as sporopollen and soluble salt in the borehole profile of the Dougeong basin in the Yellow River source region - Maduo, Qinghai Province, revealing the paleoclimate evolution since 130 kaBP. Namely: 130.0-110.0kaBP cold and dry; 110.0-82.0kaBP cold and wet; 82.0-10.4kaBP cold and dry; 10.4kaBP to modern (ie, Holocene) alternation of warm, wet and dry. The Holocene Paleoclimate can be divided into three phases: Anathermal in the early Holocene (Megathermal), Megathermal in the Middle Holocene Cooling period (3.5kaBP to date) (Katathermal). The general rule of paleoclimate in this area is that the cold period is long and earlier than the rest of the world, with a short warm period and a lagged initial period. Since the Holocene, the climate fluctuation has the oscillation law of the millennium scale. Since the late Holocene, the temperature gradually decreases and the humidity gradually becomes dry.