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寒冷的冬季可能是大规模灭绝的原因,发生在伊纪/奥利古纪的边界
L C Ivany1, W P Patterson, K C Lohmann
1Department of Geological Sciences, University of Michigan, Ann Arbor 48109, USA. lcivany@syr.edu
Nature
|November 1, 2000
概括
世/奥利古纪的边界出现了主要的海洋灭绝. 冬季温度变化增加,而不是平均温度变化,可能导致了这种显著的动物周转.
科学领域:
- 古气候学 古气候学
- 古生物学的古生物学
- 海洋生物学 海洋生物学
背景情况:
- 纪/纪边界 (33.7亿年前) 与主要的纪海洋无脊椎动物灭绝有关.
- 之前的假设表明,从温暖的欧到较冷的奥利古气候的转变,但气候重建缺乏支持的证据.
- 在此期间,美国海湾沿海平原发生了高的软体动物物种周转率 (超过90%).
研究的目的:
- 为了调查世/世灭绝事件的气候驱动因素.
- 为了测试假设,平均年温度的变化导致了动物的周转.
- 为了重建详细的古气温跨越世/世边界.
主要方法:
- 在化石鱼耳石 (耳石) 中对阿拉贡石的稳定氧同位素分析.
- 增量微采样耳石以解决季节性温度变化.
- 使用氧同位素值重建古气温.
主要成果:
- 平均奥托利斯氧同位素值表明,跨越边界的平均年温度变化最小.
- 季节性温度数据显示,冬季温度显著降低约4°C.
- 这表明温度变化增加了,而不是平均温度的变化.
结论:
- 增加的温度变化,特别是更寒冷的冬季,被认为是欧/奥利古动物周转的主要驱动因素.
- 这些发现挑战了以前的假设,这些假设仅集中在平均年温度变化上.
- 这项研究强调了考虑季节性气候变化的重要性,以了解过去的灭绝事件.
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