早期陆地植物迫使岩岩的演变
William J McMahon1, Neil S Davies2
1Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK.
概括
陆地植物大大增加了地球上的泥量. 这项研究表明,在植被进化后,泥岩的比例激增,影响了地球的历史和气候.
科学领域:
- 地质科学
- 古生物学
- 沉积物学
背景情况:
- 泥石是地球历史的重要档案, 影响海洋化学和气候.
- 了解泥岩的形成是重建过去环境的关键.
研究的目的:
- 研究陆地植物进化与陆地保留的泥比例之间的联系.
- 在地球历史上测量泥石沉积的变化.
主要方法:
- 分析了704个岩形成的层级数据,涵盖了古石器到石灰岩时期.
- 在陆地植物进化之前和之后的沉积沉积物中的泥岩比例的比较.
主要成果:
- 在陆地植物进化后,陆地保留的泥比例显著增加.
- 这种泥石浪潮始于奥尔多维纪-西卢纪时期.
- 植物生长后的浮岩平均比植物生长前的浮岩多1.4个数量级.
结论:
- 植被进化从根本上改变了来自大陆的泥生产和沉积物流.
- 这种泥岩沉积的变化对海洋化学和气候调节产生了深远的影响.
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