极端气候温暖的证据来自晚白时期的北极脊椎动物
1J. A. Tarduno, R. D. Cottrell, H. Scher, Department of Earth and Environmental Sciences, University of Rochester, Rochester, NY, 14627, USA. D. B. Brinkman, Royal Tyrrell Museum of Palaeontology, Drumheller, Alberta, TOJ OYO, Canada. P. R. Re.
概括
在白纪晚期的极地气候令人惊地温暖,超过14°C,不接近结点. 这一发现得到了脊椎动物化石和火山活动证据的支持.
科学领域:
- 古气候学 古气候学
- 脊椎动物古生物学 脊椎动物古生物学
- 地质化学 地质化学
背景情况:
- 晚白纪极地地区的气候受到争议,一些证据表明条件凉爽.
- 了解过去的极地气候对于预测未来的气候变化至关重要.
- 大火山区 (LIP) 与大量的火山排放有关.
研究的目的:
- 利用古生物学证据重建了晚白纪北极的气候.
- 调查火山活动在这个时期推动极地温暖的潜在作用.
主要方法:
- 来自加拿大阿克塞尔海伯格岛的脊椎动物化石组合的分析.
- 同时的大型火山性省份的地化学分析.
主要成果:
- 发现了一组脊椎动物,包括大型香龙 (已灭绝的鱼类爬行动物),表明温暖的极地气候 (平均年温度>14°C).
- 在同一时期 (92-86百万年前) 活跃的六个主要的大火性省份的识别.
结论:
- 晚白时期的极地气候明显比以前假设的要温暖,挑战现有模型.
- 与此同时发生的火山二氧化碳排放可能导致全球变暖和极地温度升高.
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