鱼类碎片氧同位素显示的冲击后最早的古世变暖 (埃尔凯夫,突尼斯)
K G MacLeod1, P C Quinton2, J Sepúlveda3
1Department of Geological Sciences, University of Missouri, Columbia, MO, USA. macleodk@missouri.edu.
概括
奇克苏鲁布撞击可能导致温室气体变暖, 但数据很少. 鱼类碎片的新分析显示温度增加了5°C, 支持撞击驱动的变暖假说.
科学领域:
- 古气候学
- 地质化学
- 撞击坑
背景情况:
- 温室气体变暖是奇克苏鲁布撞击的预测结果, 但支持数据很少.
- 缺乏合适的古热量测量段阻碍了对撞击效应的理解.
- 之前的研究缺乏用于传统古热度测量和短期变化的分辨率的材料.
研究的目的:
- 调查在奇克苏鲁布事件之后可能发生的温室气体变暖.
- 解决温室气体变暖的支持数据的短缺问题.
- 在白纪/古纪的边界分析古气温变化.
主要方法:
- 鱼类残渣 (酸微化石) 的氧气同位素组成分析.
- 使用了抗基因改变的材料.
- 检查的样本来自突尼斯的El Kef的白纪/古纪边界全球平流体部分和点.
主要成果:
- 观察到氧同位素值下降约为每毫升1.
- 这种同位素变化相当于约5°C的变暖.
- 这种变暖趋势始于白纪/古纪的边界,持续了大约300厘米 (约10万年).
结论:
- 观察到的5°C升温模式与对撞击引发的温室变暖的预期一致.
- 鱼类残留物提供了一个可行的古热量测量方法,用于受化影响的部分.
- 这项研究提供了关键数据, 支持了奇克苏鲁布影响与随后的温室气体变暖之间的联系.
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