氧化光合作用的早期起源延迟了大氧化过程
Julia Elizabeth Horne1, Colin Goldblatt1, Lee Kump2
1School of Earth and Ocean Sciences, University of Victoria, Victoria, British Columbia, Canada.
概括
大氧化事件的发生.
科学领域:
- 生物地质化学生物地质化学
- 地球系统科学 地球系统科学
- 进化生物学 进化生物学
背景情况:
- 大氧化事件 (GOE) 标志着地球在24亿年前发生的关键化学转变.
- 氧化光合作用是这一事件的关键代谢,可能早在35亿年前就已经演变.
- 早期氧化光合作用和GOE之间的长时间延迟仍然不太清楚.
研究的目的:
- 调查控制大氧化事件发生时间的因素.
- 评估早期代谢途径演变和的可用性对氧化的影响.
- 使用地球氧化和自然系统学 (EONS) 生物地质化学模型探索场景.
主要方法:
- 利用EONS生物地化学模型模拟地球系统动态.
- 测试了氧光合作用和固化的演变的各种场景.
- 评估了无机循环边界条件对氧化时间的影响.
主要成果:
- 与直觉相反的是,氧光合作用的早期起源导致了更长的延迟在GOE之前.
- 氧光合作用最早模拟的起源导致了最长的绝对延迟.
- 的可用性被确定为最终的控制,早期的新陈代谢导致生产力瓶.
结论:
- 的限制,加剧了海洋氧化还原分层和封存,显著延迟了氧气的积累.
- 早期代谢演变和营养物质的可用性之间的相互作用决定了 GOE 的时间.
- 了解这些古老的地球系统动态,可以了解生物圈的演变.
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