早期三叠纪的超温室气候是由植被驱动的,植被崩
Zhen Xu1,2, Jianxin Yu3, Hongfu Yin4
1State Key Laboratory of Geomicrobiology and Environmental Changes, School of Earth Sciences, China University of Geosciences, Wuhan, 430074, P.R. China. Z.xu@leeds.ac.uk.
Nature communications
|July 2, 2025
概括
珀米亚-纪大灭绝 (PTME) 被广泛的植物丧失所延长,这减少了碳捕获,并使地球温度保持高数百万年. 这凸显了植被在调节气候中的关键作用.
科学领域:
- 古气候学 古气候学
- 地球系统科学 地球系统科学
- 古生物学的古生物学
背景情况:
- 珀米亚-纪大灭绝 (PTME) 是法内罗纪最严重的灭绝事件.
- 由西伯利亚陷火山活动引起的全球变暖是首要的疑似原因.
- 火山活动后超级温室条件的长期持续仍然无法解释.
研究的目的:
- 为了调查在三叠纪早期持续存在的超级温室条件的原因.
- 重建整个PTME的陆地植物生产率的时空变化.
- 为了模拟植被崩对三叠纪早期气候碳系统的影响.
主要方法:
- 利用化石现象和岩石气候指标来绘制植物生产力的地图.
- 采用气候-生物地质化学建模来模拟早期的三叠纪条件.
- 分析了植被丧失,碳捕获和大气二氧化碳水平之间的关系.
主要成果:
- 在PTME期间,陆地植被发生了显著的损失,特别是在热带地区.
- 植物生产率下降导致有机碳封存减少.
- 受到限制的化学气候变化进一步导致了长时间的高大气二氧化碳水平.
结论:
- 陆地植被的崩通过减少碳捕获和化学气候变化而放大了变暖.
- 这种反循环有助于解释超级温室条件持续数百万年.
- 这项研究支持气候碳系统值的存在,其中植被丧失可以引发放大变暖.
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