热带地理 ›› 2016, Vol. 36 ›› Issue (3): 448-456.doi: 10.13284/j.cnki.rddl.002835
周厚云,刘淑华,彭小桃,邓肖敏,陈 琼,米小建
出版日期:
2016-05-05
发布日期:
2016-05-05
作者简介:
周厚云(1967―),湖南安乡人,教授,博士生导师,主要从事全球变化研究,(E-mail)hyzhou@gig.ac.cn。
基金资助:
ZHOU Houyun,LIU Shuhua,PENG Xiaotao,DENG Xiaomin,CHEN Qiong,MI Xiaojian
Online:
2016-05-05
Published:
2016-05-05
摘要: 对近些年来国内外广泛争议的话题——中国季风区岩溶洞穴沉积氧同位素组成(δ18O)的气候指示意义进行了梳理,简要介绍了有关争议各方的主要观点。同时针对中国季风区洞穴沉积δ18O的研究提出了几个重要问题:同位素平衡分馏的检验问题、洞穴沉积δ18O记录的相似性(重复性)与差异性,以及洞穴通风可能对洞穴沉积δ18O记录的影响等。这些问题涉及到洞穴沉积δ18O记录与气候指标之间的联系机制,对其探讨可能有助于解决有关争议。因此,建议在今后的研究中应该重点关注这些问题,因为洞穴沉积δ18O与气候环境指标之间的联系机制是中国季风区内应用洞穴沉积δ18O进行古气候古环境研究的基础。
周厚云,刘淑华,彭小桃,邓肖敏,陈琼,米小建.. 中国季风区石笋氧同位素气候指示意义: 主要争议与几个重要问题 [J]. 热带地理, 2016, 36(3): 448-456.
ZHOU Houyun,LIU Shuhua,PENG Xiaotao,DENG Xiaomin,CHEN Qiong,MI Xiaojian.. Paleoclimatic Interpretations of Speleothem δ18O Record in Monsoonal China: Controversies and Some Key Issues [J]. TROPICAL GEOGRAPHY, 2016, 36(3): 448-456.
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