地理学报 ›› 2016, Vol. 71 ›› Issue (5): 864-872.doi: 10.11821/dlxb201605014
收稿日期:
2016-03-06
修回日期:
2016-03-26
出版日期:
2016-05-25
发布日期:
2016-05-25
作者简介:
作者简介:胡小猛(1965-), 男, 安徽宣城人, 博士, 教授, 主要从事地貌第四纪研究。E-mail:
基金资助:
Xiaomeng HU(), Shun CAI, Meijun CHEN
Received:
2016-03-06
Revised:
2016-03-26
Online:
2016-05-25
Published:
2016-05-25
Supported by:
摘要:
目前对含大荔人化石的地层年代认识仍存很大争议。采用黄土—古土壤序列定年法广泛调查渭河盆地东北部区域和大荔人化石点附近洛河上下游河段过去的河湖环境演变历史;在此基础上,结合产出大荔人化石的地貌沉积体特征,分析其形成时所处的区域演化阶段及其中含化石的沉积层位堆积年代。结果显示,区域曾在S14、L9、L6、S2、L2和L1SS发育或堆积时期发生过数次古湖湖退或河流下切;含大荔人化石的沉积层是在区域发生于L6晚期的一次湖退后,洛河于出露至气下的古湖湖底上堆积而成的,其堆积时代与S5古土壤发育时代相当,平均年龄约0.55 Ma BP。由该研究结果推论,学界对北京猿人年龄估计的老的年龄框架可能偏年轻。
胡小猛, 蔡顺, 陈美君. 基于区域河湖地貌演化历史的大荔人化石层位年代分析[J]. 地理学报, 2016, 71(5): 864-872.
Xiaomeng HU, Shun CAI, Meijun CHEN. The deduction of the age of the fossil Dali Man from the history of the regional geomorphic-sedimentary evolution[J]. Acta Geographica Sinica, 2016, 71(5): 864-872.
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