摘要
简述了十五万年来古气候变化旋回及其中的短期波动事件,如新仙女木事件;概要地介绍了黄土、古海洋沉积、冰岩芯、树木年轮、洞穴碳酸钙等的古气候研究方法的最新进展;并指出在古气候研究中,必须注意多种方法的互相对比印证,才能保证结论的准确性与可靠性。
This paper presents the changs of the Earth's climate during the last 150 000 and shortterm climate events such as Younger Dryas event,Heinrich event.It instroduces the latest progress in the study methods of paleoclimate in loess,ice cores,deep sea cores,annual ring of trees and speleothems.The accurate and reliable result can be obtained only under a comprehensive study of different subjects which can be confirmed each other.
出处
《地质科技情报》
EI
CAS
CSCD
北大核心
1998年第2期39-44,共6页
Geological Science and Technology Information
基金
国家自然科学基金