微生物新陈代谢放大了三次法内罗纪高热事件中的变暖
Yuyang Wu1,2, Haijun Song3, Daoliang Chu1
1State Key Laboratory of Geomicrobiology and Environmental Changes, School of Earth Sciences, China University of Geosciences, Wuhan, China.
Nature communications
|December 12, 2025
概括
海洋的生物碳 (BCP) 在古代的变暖事件中减弱. 增加的微生物活动减少了碳转移到深海,可能会放大全球变暖.
科学领域:
- 古气候学 古气候学
- 海洋学 海洋学 海洋学
- 生物地质化学生物地质化学
背景情况:
- 海洋的生物碳 (BCP) 对于气候调节至关重要,因为它能隔离大气中的二氧化碳.
- 了解过去极端变暖事件 (超热) 中的BCP动态至关重要,但有限.
研究的目的:
- 为了研究BCP在Perm-Triassic,早期Toarcian和Paleocene-Eocene高热时期的变化.
- 在快速变暖下确定驱动BCP变化的机制.
主要方法:
- 利用表面和中水之间的垂直碳同位素 (δ13C) 梯度作为BCP活动的代理.
- 分析了来自三个不同的地质超热事件的数据.
主要成果:
- 在超热过程中观察到垂直 δ13C梯度增加了两到三倍.
- 增加的梯度归因于通过微生物呼吸增强有机物重矿化.
- 记录了微粒有机碳转移效率的两到六倍降低.
结论:
- 在古代高温时期,由变暖引起的微生物代谢显著影响了BCP.
- 减少对深海的碳出口可能有有限的封存.
- 增强的微生物代谢可能通过积极的反循环放大了全球变暖.
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