与三纪-罗纪边界大规模灭绝相关的突然生产力崩
P D Ward1, J W Haggart, E S Carter
1Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195, USA.
概括
特里亚斯纪末期的大规模灭绝导致海洋浮游生物的生产力大幅下降. 这一由碳同位素证明的事件反映了地球历史上其他重大灭绝事件.
科学领域:
- 古生物学的古生物学
- 地质化学 地质化学
- 地球科学 地球科学 地球科学
背景情况:
- 特里亚斯纪末期的大规模灭绝是地球历史上五大灭绝事件之一.
- 了解这一事件的原因和影响对于理解Phanerozoic生物多样性动态至关重要.
研究的目的:
- 为了调查三叠纪末期大规模灭绝的原因.
- 为了分析碳同位素证据,分析三叠纪-罗纪边界的生产力变化.
主要方法:
- 位于加拿大不列颠哥伦比亚省夏洛特女王群岛的部分的平流图分析.
- 沉积物记录的碳同位素分析.
主要成果:
- 证据表明,在特里亚斯纪末期的边界,海洋生产力明显崩.
- 观察到类似于其他重大灭绝事件 (百米纪-三叠纪,白纪-三叠纪) 的碳同位素游览.
结论:
- 特里亚斯纪末期的大规模灭绝与海洋生态系统生产力的重大崩有关.
- 碳同位素数据表明,在这个灭绝事件期间,环境压力的全球模式.
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