在北方高度地区,经过以欧纪到奥利古纪的过渡,季节性增加
James S Eldrett1, David R Greenwood, Ian C Harding
1Shell Exploration and Production UK Ltd, 1 Altens Farm Road, Nigg, Aberdeen, AB12 3FY, UK. james.eldrett@shell.com
Nature
|June 19, 2009
概括
全球气候在3350万年前从温室转变为冰室条件. 新的数据显示,在南极冰盖增长之前,北极地区出现了显著的降温和季节性增加.
科学领域:
- 古气候学 古气候学
- 气候变化科学 气候变化科学
- 古植物学是古植物学.
背景情况:
- 世 - 世过渡期 (大约. 3350万年前) 标志着全球气候从温室气候转变为冰室气候.
- 这一时期,南极冰盖扩大和北半球冰化,由轨道变化和大气二氧化碳减少所驱动.
- 之前的古气候研究提出了相互矛盾的数据,对高度气候动态的理解不佳.
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