根和相关的真菌驱动北极森林的长期碳封存
K E Clemmensen1, A Bahr, O Ovaskainen
1Department of Forest Mycology and Plant Pathology, Uppsala BioCenter, Swedish University of Agricultural Sciences, Uppsala, Sweden. karina.clemmensen@slu.se
概括
玻里亚森林土壤储存大量的碳,主要来自根和相关微生物,而不仅仅是植物垃圾. 这一发现挑战了关于森林碳循环和有机物积累的传统观点.
科学领域:
- 生态生态学 生态生态学
- 土壤科学 土壤科学
- 生物地质化学生物地质化学
背景情况:
- 玻里亚森林土壤是关键的碳汇.
- 传统上,地面植物垃圾被认为是土壤有机物的主要来源.
- 了解碳积累机制对于全球碳循环研究至关重要.
研究的目的:
- 调查北极森林土壤有机物的主要来源.
- 探索根和相关微生物在碳储存中的作用.
- 检查真菌群落如何影响森林继承期间的碳动态.
主要方法:
- 使用放射性碳 (14C) 炸弹-碳建模来追踪碳来源.
- 分析了真菌生物标志物,以评估残留物的降解和保存.
- 采用了454次热测序和稳定同位素分析来确定微生物的作用.
主要成果:
- 50-70%的储存的土壤碳来源于根和与根相关的微生物.
- 菌生物标志物表明,在后来的连续森林中降低了降解和保存残留物.
- 根相关的真菌被确定为生态系统碳动态的关键调节者.
结论:
- 根源来源的有机物在北极森林土壤碳积累中发挥着主导作用.
- 森林继承影响真菌活动,影响碳的保存.
- 提出了一个在北极森林中有机物积累的替代机制,由根贡献驱动.
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