在米-三叠纪超毒性事件期间的光热区域 euxinia
Kliti Grice1, Changqun Cao, Gordon D Love
1Curtin University of Technology, Perth, Australia. K.Grice@curtin.edu.au
概括
珀米亚-特里亚斯纪的灭绝是由海洋中广泛的eocinic (无毒和硫化) 条件驱动的.
科学领域:
- 古海洋学是古海洋学.
- 地质化学 地质化学
- 生物地质化学生物地质化学
背景情况:
- 珀米亚-特里亚斯纪的边界标志着一个主要的大规模灭绝事件.
- 了解这个时期的环境条件对于解释灭绝的严重程度和恢复至关重要.
- 之前的研究表明无氧条件,但 euxinia 的程度是有争议的.
研究的目的:
- 调查珀斯盆地的古海洋学条件在米-三叠纪超毒事件期间.
- 为了确定 euxinic 条件和硫化物毒性在灭绝和恢复中的作用.
- 为了比较珀斯盆地与其他当代盆地的条件.
主要方法:
- 对碳和硫同位素的分析.
- 生物标志物分析,特别针对Chlorobiaceae的无氧光合作用.
- 铁的物种化分析.
主要成果:
- 在珀斯盆地的古水柱中,在米-三叠纪超毒性事件期间,尤克辛状况普遍存在.
- 生物标志物表明,在克罗罗罗比亚科的边界和早期的三亚纪中,有显著的无氧光合作用.
- 类似的eocinic条件被发现在南中国附近的当代海域.
结论:
- 广泛的光热带 euxinic 条件表明硫化物毒性在推动波斯-三叠纪灭绝中发挥了关键作用.
- 硫化物毒性也导致了灭绝事件后的长期恢复.
- 这些发现突出了海洋无氧和 euxinia 对海洋生态系统的影响.
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