概括
陆地植被显著影响大气中的二氧化碳和氧气水平. 陆地生态系统的变化,比如在海洋中发生的变化,改变了全球初级生产力,影响了大气气体度.
科学领域:
- 古生物学的古生物学
- 生态生态学 生态生态学
- 气候科学 气候科学
背景情况:
- 自中生代以来,陆地植被一直是大气中二氧化碳和氧气动态的主要驱动因素.
- 现代陆地生态系统,不包括特定类型,表现出比海洋生态系统更高的单位面积生产率.
- 在生产力方面,这种陆地主导地位很可能在罗纪晚期的大部分时间内持续存在.
研究的目的:
- 分析陆地生态系统变化对大气气体组成的影响.
- 在地质时间内评估陆地生态系统与海洋生态系统的比较生产力.
主要方法:
- 生态系统生产率比率 (生产率/面积) 的比较分析.
- 模拟海洋侵权和回归对全球初级生产力的影响.
主要成果:
- 陆地生态系统通常显示出比海洋生态系统更高的生产率/面积比率.
- 陆地生态系统的减少 (例如,在海洋侵蚀期间) 会导致全球初级生产率下降.
- 初级生产率下降导致大气中二氧化碳增加和氧气水平降低.
结论:
- 陆地生态系统范围的变化是大气二氧化碳和氧气的关键调节者.
- 由于它们对陆地植被的影响,海洋的过度和回归对大气组成有着显著的,相反的影响.
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