草植物体的元素组成:环境控制和对溶解的影响
Oleg S Pokrovsky1, Alisson Akerman2, Fabrice Fraysse3
1Geoscience and Environment Toulouse, UMR 5563 CNRS, University of Toulouse, 14 Avenue Edouard Belin, 31400 Toulouse, France; BIO-GEO-CLIM Laboratory, Tomsk State University, Lenin Ave, 36, Tomsk 634050, Russia.
The Science of the total environment
|January 4, 2024
概括
植物植物体的植物石.
科学领域:
- 地质化学和环境科学,专注于植物生物矿化.
背景情况:
- 植物植物石,二氧化生物矿物化,保持关键的古老环境和农业数据.
- 它们的元素组成影响土壤的保存和元素循环,但控制机制尚不清楚.
研究的目的:
- 调查控制植物体元素组成的因素.
- 评估元素组成对植物体反应性和土壤保存的影响.
主要方法:
- 来自不同植物物种和地区的植物石中主要和微量元素的分析.
- 用不同的微量金属度测试植物石溶解速率的实验性确定.
主要成果:
- 植物石的元素组成在物种和地区之间有很大的差异,受到大气中的尘埃,气候和当地地质的影响.
- 与欧洲样本相比,西伯利亚草植物石显示出不同的元素配置.
- 尽管存在广泛的元素变异,但植物石溶解率在研究的植物类型中是相似的.
结论:
- 元素成分对土壤中的植物石保存有很小的影响.
- 大气中的尘埃和气候是植物石元素构成的关键驱动因素.
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