地球历史的比较和晚期波斯纪大规模灭绝
A H Knoll1, R K Bambach, D E Canfield
1Botanical Museum, Harvard University, Cambridge, MA 02138, USA.
概括
波斯纪晚期的大规模灭绝可能是由无氧深海翻转引起的,释放二氧化碳并影响生物. 这反映了新新生态时代的情况,将古代和最近的地质事件联系起来.
科学领域:
- 古海洋学是古海洋学.
- 地质事件 地质事件
- 大规模灭绝事件的事件.
背景情况:
- 晚期的新新生代 (Neoproterozoic Era) 见证了碳同位素游览,冰川和不寻常的碳酸盐降水的融合.
- 这些现象为了解末波斯地球上类似条件提供了一个模型.
研究的目的:
- 解释在末珀米亚时代中新新生态条件的复苏.
- 解释古海洋学变化与大规模灭绝事件之间的联系.
主要方法:
- 开发一个古海洋学模型.
- 对平流图和同位素数据的分析.
- 新新生代和晚期波斯纪地质记录的比较.
主要成果:
- 该模型表明,珀米亚纪晚期无氧深海翻转引入了高二氧化碳度.
- 这种二氧化碳的释放影响了表面环境和大气条件.
结论:
- 预测的生理和气候后果与观察到的Permian大灭绝的时间和选择性一致.
- 海洋翻转是Permian晚期灭绝事件的一个合理机制.
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