崔美玲, 罗运利, 孙湘君. 吉林哈尼湖钻孔5 000年以来的古植被气候变化指示[J]. 海洋地质与第四纪地质, 2006, 26(5): 117-122.
引用本文: 崔美玲, 罗运利, 孙湘君. 吉林哈尼湖钻孔5 000年以来的古植被气候变化指示[J]. 海洋地质与第四纪地质, 2006, 26(5): 117-122.
CUI Mei-ling, LUO Yun-li, SUN Xiang-jun. PALEOVEGETATIONAL AND PALEOCLIMATIC CHANGES IN HA'NI LAKE, JILIN SINCE 5 kaBP[J]. Marine Geology & Quaternary Geology, 2006, 26(5): 117-122.
Citation: CUI Mei-ling, LUO Yun-li, SUN Xiang-jun. PALEOVEGETATIONAL AND PALEOCLIMATIC CHANGES IN HA'NI LAKE, JILIN SINCE 5 kaBP[J]. Marine Geology & Quaternary Geology, 2006, 26(5): 117-122.

吉林哈尼湖钻孔5 000年以来的古植被气候变化指示

PALEOVEGETATIONAL AND PALEOCLIMATIC CHANGES IN HA'NI LAKE, JILIN SINCE 5 kaBP

  • 摘要: 选取哈尼湖钻孔360~0 cm (5 112 aBP以来)的沉积物进行孢粉分析,共采取样品85个,平均时间分辨率约为60 a。样品中花粉含量非常丰富,种类以乔木为主,其百分含量多在80%以上,最高可达96%,根据花粉组成在钻孔上的变化,结合花粉沉积率进行样品分析,自下而上可分为4个花粉组合带,进而将该区5 000 a以来气候演化大致分为4个阶段:阶段1(5 112~3 784 aBP),阔叶类乔木占优势,湿生及水生草本比较丰富,气候温暖湿润;阶段2(3 784~1 380 aBP),针叶类乔木占优势,湿生及水生草本消失,气候变凉干;阶段3(1 380~994 aBP),以松为主的针叶类仍占绝对优势,喜温湿的灌木草本含量持续下降,说明气候继续变冷变干;阶段4(994 aBP以来),植物种类比较丰富,湿生植物的沉积率明显增高,气候变得更加湿润。

     

    Abstract: According to the spore pollen analysis results of 85 core samples from Ha'ni Lake,the history of vegetation and environment can be divided into four stages as follows:① StageⅠ(5 112~3 784 aBP):Broadleaved trees dominated in this stage, and the climate was warm and wet;② Stage Ⅱ(3 784~1 380 aBP):The coniferous trees dominated during the whole stage, hydrophytic herbaceous plants disappeared, and the climate changed to be cold and dry;③ Stage Ⅲ(1 380~994 aBP):The percent of coniferous trees continued to increase but hydrophytic herbaceous plants began to appear, suggesting that the climate was colder but a little more humid; ④Stage Ⅳ(994~0 aBP):The diversity of plants was great, and the pollen sedimentation rate of hydrophytic herbaceous plants obviously increased, so the climate changed to be more humid.

     

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