二氧化碳导致的气候和植被不稳定在晚期古老时代的脱冰过程中
Isabel P Montañez1, Neil J Tabor, Deb Niemeier
1Department of Geology, University of California, Davis, CA 95616, USA. montanez@geology.ucdavis.edu
概括
晚期的古老时代脱冰过程使地球从冰河变成了温室. 这项研究揭示了二氧化碳 (CO2) 的转移导致了温度变化和主要的植物生命重组.
科学领域:
- 古气候学 古气候学
- 古植物学是古植物学.
- 地质化学 地质化学
背景情况:
- 晚期古老时代的脱冰标志着地球上独特的冰房到温室过渡.
- 了解这个时期的气候动态对于理解过去的气候变化至关重要.
研究的目的:
- 为了重建大气中的二氧化碳 (pCO2) 水平和热带海洋表面温度在晚期古老纪气候过渡期间.
- 为了研究pCO2,温度,冰体积和生物变化之间的关系.
主要方法:
- 对土壤矿物质,化石植物和足动物进行稳定同位素分析.
- 与南贡德瓦纳的冰川记录进行比较.
主要成果:
- 推断的pCO2和温度的变化与冰体积共同变化,支持温室气体的强迫.
- 西欧美洲古热带植物的重大重组与气候和pCO2的变化相吻合.
结论:
- 温室气体强迫在古老时代晚期从冰川到温室的过渡中发挥了关键作用.
- 由二氧化碳驱动的气候变化对古热带生态系统产生了深远的影响,导致永久的无冰世界.
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