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新疆巴里坤湖全新世环境记录及区域对比研究

, PP. 610-620

Keywords: 巴里坤湖,全新世气候环境,区域对比

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Abstract:

选择位于西风环流显著影响区的巴里坤湖作为研究对象,采用14C测年建立了巴里坤湖沉积剖面约9400cal.aB.P.以来的时间序列。对该湖泊剖面沉积物的矿物X射线衍射、自生碳酸盐稳定同位素、碳酸盐含量和粒度指标的综合分析表明,9400cal.aB.P.以来,巴里坤湖地区的气候环境变化大致经历了冷干(9400~7400cal.aB.P.)-暖湿(7400~5900cal.aB.P.)-暖干(5900~3100cal.aB.P.)-凉湿(3100~1100cal.aB.P.)-冷干(1100~500cal.aB.P.)-暖干(500cal.aB.P.以来)的气候变化过程,该过程基本上同周边区域的气候环境变化记录相一致。在3800cal.aB.P.左右,北疆地区的几个典型湖泊沉积记录序列都指示该时期气候环境发生了较为明显的转折,可能暗示了这一时期亚洲中部干旱区(至少在北疆地区)大气环流状况发生了重大调整。

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