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化石植物和全球变暖在纪-罗纪边界
1Department of Animal and Plant Sciences, University of Sheffield, Sheffield, S10 2TN, UK.
概括
在罗纪-罗纪边界发生的一次大规模灭绝事件与大气二氧化碳增加四倍和温室气体升温3-4°C有关,导致致命的叶子温度和大规模的植物灭绝.
科学领域:
- 古生物学的古生物学
- 气候科学 气候科学
- 古植物学是古植物学.
背景情况:
- 特里亚斯纪-罗纪的边界标志着一个主要的动物大规模灭绝.
- 跨越这个边界的环境变化记录很少.
- 古植物学数据为过去的气候条件提供了洞察力.
研究的目的:
- 为了研究与三-罗纪大灭绝有关的环境变化.
- 为了将古植物学证据与灭绝事件相关联.
- 评估大气中二氧化碳增加和气候变暖对大植物的影响.
主要方法:
- 对古植物学证据的分析.
- 计算大气中的二氧化碳度.
- 温室气体变暖效应的建模.
- 估计叶子温度. 叶子温度的估计.
主要成果:
- 发现大气二氧化碳度增加了四倍.
- 显著的温室气体变暖3~4°C发生在边界.
- 计算的叶子温度超过了植物的临界致命极限.
结论:
- 极端的环境条件可能导致了Triassic-Jurassic大型植物物种的超过95%的物种转移.
- 二氧化碳和温度的上升在三纪-罗纪大灭绝事件中起到了至关重要的作用.
- 这项研究强调了植物对快速气候变化的敏感性.
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