芬兰正在进行的泥炭地横向扩张
Teemu Juselius-Rajamäki1, Minna Väliranta1, Atte Korhola1
1Environmental Change Research Unit (ECRU), Ecosystems, Environment Research Programme, Faculty of Biological and Environmental Sciences, and Helsinki Institute of Sustainability Science (HELSUS), University of Helsinki, Helsinki, Finland.
Global change biology
|October 19, 2023
概括
北方的泥炭地仍在扩张,在过去1500年中,这一速度一直在增加. 这种泥炭地扩张受到地下条件和森林火灾的影响,影响了碳平衡.
科学领域:
- 生态生态学 生态生态学
- 地质科学 地质科学
- 环境科学 环境科学
背景情况:
- 泥炭地储存了大量的陆地碳 (400-1000 Gt C).
- 之前关于泥炭地开发的研究忽视了当前的利率,这表明扩张停止了.
- 关于最近的泥炭地边缘动态和横向扩张的知识差距存在.
研究的目的:
- 调查芬兰五个泥炭地最近的泥炭地边缘发展情况.
- 分析地下特征和过去的森林火灾对泥炭地扩张的影响.
- 挑战目前普遍认为泥炭地横向扩张放缓或停止的观点.
主要方法:
- 从芬兰的泥炭地采样了15个横断部分和47个泥炭核心.
- 在基底泥炭层上使用了14C放射性碳测年法.
- 评估了地底特征和过去森林火灾的证据 (木炭).
主要成果:
- 北方的泥炭地正在积极扩张,在边缘发现了1950年后的基底年龄.
- 在过去的1500年中,泥炭地横向扩张率有所增加 (每年0.1-6.4厘米).
- 扩张速度受到地下坡度的限制;森林火灾在南部地区充当扩张触发器.
结论:
- 北部泥炭地最近的横向扩张正在发生并加速.
- 地下地形和森林火灾是影响泥炭地扩张动态的关键因素.
- 目前正在进行的泥炭地扩张对全球碳平衡有重大影响.
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