西伯利亚的泥炭地是自全新世纪早期以来的净碳汇和全球甲来源
L C Smith1, G M MacDonald, A A Velichko
1Department of Geography, University of California, Los Angeles, CA 90095-1524, USA. lsmith@geog.ucla.edu
概括
西西伯利亚的早期Holocene泥炭地成为北半球主要的甲来源,储存大量的碳,并作为二氧化碳沉降器. 这一发现影响了我们对过去气候动态的理解.
科学领域:
- 古气候学 古气候学
- 地质化学 地质化学
- 生态生态学 生态生态学
背景情况:
- 冰芯数据显示,在全新世纪早期,甲的含量显著增加.
- 西西伯利亚低地在甲上升中的作用尚不清楚.
研究的目的:
- 研究西西伯利亚泥炭地开发的时间和规模.
- 量化早期Holocene期间该地区的碳库存和气体交换.
主要方法:
- 对西西伯利亚低地地区大量数据的分析.
- 与大气中甲数据和极际甲梯度 (IPG) 进行了泥炭地建立时间的比较.
主要成果:
- 大规模的泥炭地建立发生在11.5和9千年前之间.
- 碳储量估计为70.2皮塔克,代表了冰期后碳积累的很大一部分.
- 最小的灾难性氧化证据表明,二氧化碳的长期碳汇作用.
结论:
- 西西伯利亚低地成为早期全新世纪的主要甲来源.
- 该地区自全新世纪早期以来一直作为长期的二氧化碳沉地运作.
- 这些发现完善了我们对全球碳循环和甲动态的理解.
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