在罗纪-罗纪边界的海洋酸化脉冲
Molly Trudgill1,2, James W B Rae3, Ross Whiteford3
1School of Earth and Environmental Sciences, University of St Andrews, St Andrews, UK. molly.trudgill@lsce.ipsl.fr.
Nature communications
|July 14, 2025
概括
海洋酸化发生在特里亚纪末期灭绝后,与二氧化碳释放有关. 这种长期的环境变化可能阻碍了生态系统的恢复,影响了地球的历史和未来.
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:
- 大量灭绝是地球历史上重要的事件,其原因往往不清楚.
- 海洋酸化被认为是过去环境变化的一个因素,但直接pH值数据对于罗纪-罗纪时期很少.
研究的目的:
- 为了重建三叠纪末期灭绝事件期间海洋pH值的变化.
- 研究海洋酸化,碳循环扰乱和生态系统恢复之间的联系.
主要方法:
- 从化石中分析同位素数据,以确定过去的海洋pH值.
- 使用地球系统建模 (cGENIE) 来模拟环境条件.
主要成果:
- 证据表明,在三叠纪末期灭绝后,海洋酸化至少达到0.29pH单位.
- 偶发的2 ‰负碳同位素外流 (CIE) 表示碳的大量释放.
- 建模表明,地幔衍生的碳是这种酸化事件的主要驱动因素.
结论:
- 由于二氧化碳的释放,海洋酸化是特里亚纪末期灭绝后的一个重要因素.
- 这种长时间的干扰可能推迟了生态系统的恢复.
- 海洋酸化现在与五大灭绝事件中的三大事件有关,这凸显了它对碳循环的生态影响.
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