估计来自Ir异常的Neoproterozoic雪球冰川的持续时间和强度
Bernd Bodiselitsch1, Christian Koeberl, Sharad Master
1Department of Geological Sciences, University of Vienna, Althanstrasse 14, A-1090 Vienna, Austria.
概括
在碳酸盐底部发现的外星物质,特别是异常的证据,支持全球新新生代冰川及其快速融化理论. 这表明了长期的马里诺冰川时期.
科学领域:
- 地质地质地质地质地质地
- 古气候学 古气候学
- 天文地质学 天文地质学
背景情况:
- 新新生态时代以超级温室环境结束,引发了快速的冰融和帽子碳酸盐的形成.
- 全球冰川会把外星物质集中在冰上,而冰在融化过程中会沉.
研究的目的:
- 为了调查在新新生代冰川和碳酸顶的边界存在的外星物质.
- 为了确认全球Neoproterozoic冰川的范围,并完善马里诺冰川事件的持续时间.
主要方法:
- 分析了来自东刚果克拉顿的三个钻井芯.
- 在顶层碳酸盐层中识别 (Ir) 异常.
主要成果:
- 在所有分析的钻井芯中,在盖子碳酸盐的底部检测到显著的异常.
- 这些发现证实了全球广泛的新新生代冰川的发生.
- 数据表明,马里诺冰川事件至少持续了300万年,可能长达1200万年.
结论:
- 异常的存在提供了强有力的证据,证明在新新生代冰川时期外星物质沉积.
- 这项研究证实了新新生代冰层的全球性质和显著持续时间,特别是马里诺冰川.
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