碳循环在经历了末灭绝后的恢复过程中发生了大量的碳循环扰乱
Jonathan L Payne1, Daniel J Lehrmann, Jiayong Wei
1Department of Earth and Planetary Sciences, Harvard University, 20 Oxford Street, Cambridge, MA 02138, USA. jpayne@fas.harvard.edu
概括
珀米亚-特里亚斯纪边界碳同位素游览是许多早期特里亚斯纪波动中的第一个. 这种碳循环的不稳定性推迟了地球最严重的大规模灭绝后生命的恢复.
科学领域:
- 古气候学 古气候学
- 地质化学 地质化学
- 古生物学的古生物学
背景情况:
- 珀米亚-特里亚斯纪的边界标志着地球上最严重的大规模灭绝事件.
- 在这个边界上发现了显著的碳同位素外流.
- 在此事件发生后,生态系统的恢复显著延迟.
研究的目的:
- 为了研究经过二叠纪-三叠纪边界的碳循环扰动的持续时间和程度.
- 为了将碳循环的行为与生物恢复的速度相关联.
- 了解末珀米纪灭绝对环境的长期影响.
主要方法:
- 高分辨率的碳同位素测量.
- 在中国南部的多个部分的平流图分析.
- 化石记录分析以评估生物再多样化.
主要成果:
- 在米-三叠纪边界的碳同位素外流并不是孤立的,而是启动了一系列的波动.
- 这些碳循环波动持续了整个三叠纪早期,并在三叠纪中期早期结束.
- 珀米纪末期灭绝的基于化石的恢复延迟与这些碳循环异常相关.
结论:
- 在波斯末期灭绝之后,碳循环经历了长期的不稳定.
- 地球系统的功能,特别是碳循环,直接影响了生物复杂化.
- 了解这些过去的事件,可以了解大规模灭绝后的生态系统弹性.
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