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托尔西亚海洋无氧事件期间的脉冲生物甲排放与偶发变暖相结合
Ruoyuan Qiu1,2, Zhichao Yu1, Benjamin J W Mills3
1Key Laboratory of Deep Petroleum Intelligent Exploration and Development, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China.
概括
古代的变暖事件释放了大量的甲, 这项研究量化了托尔克海洋无氧事件期间的生物甲释放,揭示了它在过去的变暖和大规模灭绝中的作用.
科学领域:
- 古气候学
- 生物地质化学
- 地球科学
背景情况:
- 了解古代气候动态对于预测未来气候变化至关重要.
- 托尔西亚海洋无氧事件 (T-OAE) 提供了有关快速变暖和碳循环扰乱的见解.
研究的目的:
- 在T-OAE过程中调查生物甲释放的规模.
- 评估甲对气候变化和大规模灭绝的贡献.
主要方法:
- 开发了一个全球生物地化学模型.
- 使用马尔科夫链蒙特卡洛 (MCMC) 模拟应用贝叶斯反向.
- 使用来自约克郡地区的高分辨率碳同位素探测数据.
主要成果:
- 要解释观察到的碳同位素转移,至少需要释放4700Gt的生物甲 (δ13C为-50至-70‰).
- 这种甲释放可能会增加大气中的甲度,导致全球气候变暖超过2°C.
- 在海洋环境中,甲氧化增加和甲氧化减少促进了甲的释放.
结论:
- 在T-OAE期间,生物甲释放起了显著的积极反作用.
- 甲循环加剧了环境变化,导致海洋生物大规模灭绝.
- 重建过去的甲流改善了未来碳循环和气候动态的预测.
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