变暖削弱了土壤稳定路径,推动了亚北极生态系统的比例碳损失
Sara Marañón-Jiménez1,2, Xi Luo3, Andreas Richter4
1CREAF, Bellaterra, Catalonia, Spain.
Global change biology
|June 24, 2025
概括
气候变暖减少了亚北极土壤中的保留,导致碳的损失. 这种变暖破坏了土壤营养循环和生态系统功能,对寒冷的环境产生了潜在的不可逆转的后果.
科学领域:
- 生态生态学 生态生态学
- 生物地质化学生物地质化学
- 气候变化研究 气候变化研究
背景情况:
- 亚北极生态系统对气候变暖敏感,影响 (N) 和碳 (C) 循环.
- 在这些寒冷的环境中,土壤的营养保留对于生态系统的长期运作至关重要.
研究的目的:
- 调查持续的土壤变暖对亚北极草原土壤中固和稳定的影响.
- 使用15N追踪实验在变暖条件下量化N损失和C动态.
主要方法:
- 在不同季节的亚北极草原进行了15N追踪实验.
- 在各种土壤池中测量N保留,包括微生物生物质,细根和不可提取的分数.
- 评估有机化合物,微生物生物质,细根生物质,地表植物生物质和N吸收的变化.
主要成果:
- 变暖显著降低了土壤池中的N留,特别是在不可提取的土壤部分.
- 损失归因于耗尽的有机化合物用于稳定和弱化的体内机制.
- 变暖减少了微生物和细根生物量,但增加了地面植物生物量和N吸收,尽管不足以弥补土壤N损失.
- 在所有土壤池中观察到结合和比例的C损失.
结论:
- 持续的土壤变暖破坏了亚北极生态系统中的N稳定通路.
- 这种干扰导致N循环的"开放"和显著的,潜在的不可逆转的C损失.
- 变暖改变了资源分配,将从土壤池转移到地面植物生物质中.
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