格陵兰岛的大陆冰在伊纪和奥利古纪期间
James S Eldrett1, Ian C Harding, Paul A Wilson
1School of Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton, European Way, Southampton SO14 3ZH, UK.
Nature
|February 9, 2007
概括
格陵兰早期的冰川比以前认为的早了2000万年,发生在欧 - 奥利古过渡时期. 来自冰河的碎片的证据表明是冰川冰,而不是海冰,运输的沉积物.
科学领域:
- 古气候学 古气候学
- 古海洋学是古海洋学.
- 地质地质地质地质地质地
背景情况:
- 欧 - 奥利古过渡 (55-2300万年前) 标志着全球气候从一个没有冰的世界转变为一个拥有南极冰盖的世界.
- 北半球早期的冰川历史仍然存在争议.
- 以前的理解表明北半球冰川发生的时间比新的发现表明的要晚.
研究的目的:
- 调查北半球早期冰川的时间和起源.
- 为了提供证据,以冰川活动在晚期伊奥森到早期的奥利古森.
主要方法:
- 分析了层级学上广泛的冰上飞碎片,包括宏观的落石.
- 来自挪威-格陵兰海的样本的沉积物学分析.
- 沉积物约定时间为大约38-30万年前的时期.
主要成果:
- 发现了冰碎片的发现,表明冰川运输在伊欧纪晚期到早期的奥利古纪沉积物 (38-30万年前).
- 确定东格陵兰岛是冰上漂浮物质的可能来源.
- 有证据表明,格陵兰岛上孤立的冰川存在的时间比以前记录的时间早约2000万年.
结论:
- 这些发现挑战了北半球冰川形成的现有时间表.
- 在格陵兰岛,在气温和大气二氧化碳度大幅上升的时期,存在着孤立的冰川.
- 这项研究有助于了解早期的纪气候动态和冰盖的形成.
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