中国第四纪综合地层和时间框架
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摘要
中国第四纪地层以陆相为主,沉积类型多样,北方以风成沉积、河湖相沉积为主,南方以受风化作用影响较强的网纹红土以及河湖相沉积和洞穴/裂隙沉积为特征,青藏高原地区主要为河湖相沉积及山麓沉积.海相第四系主要沉积类型有碎屑沉积和生物礁沉积.综合生物地层学、磁性地层学、气候地层学研究和轨道调谐定年,已建立海相第四系和黄土高原第四纪黄土-古土壤序列的高精度气候地层年代学标尺.通过230Th定年,已建立64万年来石笋记录的高精度绝对年代标尺及轨道-亚轨道尺度气候变化的高分辨率氧同位素时间序列.对于其他第四纪陆相地层,目前已建立地磁极性倒转控制下的第四纪年代地层学框架.中国陆相更新统自下而上包括下更新统泥河湾阶、中更新统周口店阶和上更新统萨拉乌苏阶,全新统待建阶.本文在总结中国代表性第四纪地层单元年代学进展的基础上,建立中国第四纪综合年代地层框架和中国各大区第四系对比格架.综合多学科的年代地层学研究,将来有望建立冰期-间冰期旋回尺度上的中国陆相第四系气候地层学年表以及综合考虑海陆相地层的、统一的中国第四纪年代地层系统.
引文
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