温度依赖性低氧解释了波斯末期海洋大灭绝的生物地理和严重性
Justin L Penn1, Curtis Deutsch1,2, Jonathan L Payne3
1School of Oceanography, University of Washington, Seattle, WA 98195, USA. jpenn@uw.edu cdeutsch@uw.edu.
概括
快速的气候变化导致了二叠纪大灭绝. 海洋变暖和氧气损失造成了生理压力,
科学领域:
- 古气候学
- 古生物学
- 海洋生物学
背景情况:
- 波斯纪-三叠纪的边界 (约2亿5200万年前) 标志着地球最严重的灭绝事件,即"大灭绝".
- 快速的气候变化是大规模灭绝的主要假设.
- 了解具体的环境压力因素及其对海洋生物的影响至关重要.
研究的目的:
- 模拟二叠纪/三叠纪气候过渡及其对海洋环境的影响.
- 使用新陈代谢指数 (Φ) 评估海洋变暖和氧气损失对海洋动物生存的影响.
- 测试生理压力解释观察到的灭绝模式的假设.
主要方法:
- 利用气候模型模拟重建波斯/三叠纪海洋条件.
- 计算了各种现代物种的新陈代谢指数 (Φ),以评估有氧范围.
- 对海洋化石记录进行了空间显式分析,以与模型预测进行比较.
主要成果:
- 模型模拟成功复制了海洋变暖和氧气 (O2) 损失,符合地质证据.
- 代谢指数 (Φ) 表示有氧息地显著减少,特别是在热带地区.
- 化石记录分析证实热带地区的灭绝强度较低,符合模型预测.
结论:
- 在米-三叠纪过渡期间,海洋变暖和氧气损失是重要的环境压力因素.
- 这些综合生理压力可以解释"大死亡"的一半以上.
- 这项研究强调气候变化和氧气供应在海洋生物多样性危机中的关键作用.
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