植物在生态系统倒退期间维持陆地循环
F de Tombeur1, B L Turner2, E Laliberté3,4
1TERRA Teaching and Research Centre, Gembloux Agro-Bio Tech, University of Liege, 5030 Gembloux, Belgium. felix.detombeur@uliege.be.
概括
陆地循环在200万年间从土壤为基础的过程转变为植物驱动的过程. 植物的保留对营养不良的生态系统至关重要,突出显示了.
科学领域:
- 生物地质化学循环是什么
- 陆地生态系统发展发展.
- 土壤科学 土壤科学
背景情况:
- 全球循环对于初级生产力和碳循环至关重要.
- 陆地来源和循环的长期变化尚未得到充分理解.
- 的可用性受到土壤气候变化和生物过程的影响.
研究的目的:
- 在长期生态系统发展过程中调查陆地循环的变化.
- 了解老化土壤中对可用性的控制.
- 探索植物在营养贫乏环境中维持循环中的作用.
主要方法:
- 在西澳大利亚对200万年土壤时间序列的分析.
- 基于土壤年龄的源 (地质与生物) 的比较.
- 测量叶片度与土壤年龄和气候变化的关系.
主要成果:
- 在200万年间,陆地循环从地质控制到生物控制的过渡.
- 的可用性从年轻土壤中的源转移到老土壤中的植物回收.
- 叶片度随着土壤的老化而增加,与主要营养素的减少形成鲜明对比.
结论:
- 植物对的保留维持了陆地循环,特别是在营养不良,受气候影响的土壤中.
- 生态系统的发展导致生物在循环中占主导地位.
- 在营养有限的环境中,对植物的适应和生存起着至关重要的作用.
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