摘要
本文根据孢粉分析、有孔虫氧同位素分析、历史记载及现代气温观测资料,综合探讨广西沿海全新世以来的气候变化。经过研究,初步划分了本区全新世以来的7个气候期,在晚全新世内,进一步划分了7个气候亚期。早全新世、中全新世的气候变化具有1500-2000a周期,晚全新世早期的气候变化具有500-1000a周期,晚全新世中-晚期的气候变化具有200a周期,200a来的气候变化呈冷、热交替出现,具有10-20a或30-50a周期,现代气温呈现波动上升的趋势。
This paper studies synthetically dimatic changes since Holocene on the basis of thesporopollen, foraminifera, oxygen isotope analysis,historic records and data of modernair temperature. Climatic changes since Holocene have been grouped into 7 climaticstages. In Late Holocene, there were 7 climatic substages.Climatic changes of EarlyHolocene and Middle Holocene had a cycle of 1500-2000 years,the early time of LateHolocene had a cycle of 500-1000 years,and middle and late time of Late Holocene hada cycle of 200 years. Hot stages have alternated with cold ones with a cycle of 10-20years or 30-50 years since 200 years ago,And the modern temperature shows a tenden-cy to rise undulately.
出处
《海洋地质与第四纪地质》
CAS
CSCD
北大核心
1996年第3期49-60,共12页
Marine Geology & Quaternary Geology
基金
国家自然科学基金
关键词
全新世
孢粉
氧同位素
气温记录
气候变化
Holocene sporopollen oxygen isotope air temperatureclimatic change