温室气候温和和碳酸盐的快速形成后,马里诺亚雪球地球地球
Lennart Ramme1,2, Tatiana Ilyina3,4,5, Jochem Marotzke3,4
1Max Planck Institute for Meteorology, Hamburg, Germany. lennart.ramme@mpimet.mpg.de.
Nature communications
|April 26, 2024
概括
海洋的海洋海洋的海洋.
科学领域:
- 地球科学 地球科学 地球科学
- 气候科学 气候科学
- 地质化学 地质化学
背景情况:
- 马里诺斯雪球地球事件以由于高大气二氧化碳 (CO2) 的快速变暖而结束.
- 以前的假设表明,气候在地质时间尺度上通过大陆气候变化缓慢恢复.
- 海洋在调节大气二氧化碳中的作用 雪球后的地球在很大程度上没有得到量化.
研究的目的:
- 为了量化海洋对大气二氧化碳的影响在后海洋雪球地球时期.
- 探索海洋碳循环影响超级温室气候演变的机制.
- 为了调查马里诺山顶石头的起源.
主要方法:
- 利用定量模型来模拟海洋碳循环的动态.
- 将海洋性和碳酸盐沉积物形成纳入气候模型.
- 分析地质数据以测试模型预测.
主要成果:
- 海洋的碳循环显著影响了超级温室气候的演变.
- 确定了可能导致超级温室气候迅速下降或加剧的机制.
- 建议从海洋性中快速碳酸盐沉积物形成,以解释帽子石头.
结论:
- 温和而短暂的超级温室气候是海上雪球地球后的一个合理的场景.
- 海洋碳循环在气候恢复中发挥着至关重要的,以前未被定量化的作用.
- 这挑战了长期以来关于仅仅通过气候变化的缓慢气候衰退的假设.
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