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地球学报  2005 

西藏错鄂及邻区晚更新世高位湖相沉积的发现及其意义

DOI: 10.3975/cagsb.2005.04.01

Keywords: 西藏错鄂晚更新世高位湖相沉积古植被古气候

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Abstract:

西藏那曲县西的错鄂(31°24′~31°32′N,91°28′~91°33′E,湖面海拔4515m)东南岸(嘎杂西北坡),发育了拔湖18~271m的湖相沉积。错鄂及邻区湖相沉积的U系法测年和孢粉分析结果表明,至少在75.3~48.8kaBP间,当地植被经历了早期以松、蒿、桦为主的森林草原和晚期以松、蒿、水龙骨科为主的森林草原或森林等两个阶段,反映了气候由温和较干到温和偏干的状况,但晚期温度与湿度均较早期为高,而干燥度则略有降低。同时,包括错鄂盆地在内的“那曲盆地”则是古“羌塘东湖”的东半部。约在37kaBP左右,可能由于怒江的溯源侵蚀,切开了“羌塘东湖”与怒江的分水岭,使“羌塘东湖”的东半部古湖外泄,而成为外流区———怒江(上游那曲)流域的一部分。正因为有古湖外泄的一段历史,故可以理解钻穿了整个第四纪地层的错鄂孔B/M界线以上部分的地层较薄的原因了。

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