长期变暖重组了北极原,但没有改变净土壤碳储存
Seeta A Sistla1, John C Moore, Rodney T Simpson
1Department of Ecology, Evolution and Marine Biology, University of California Santa Barbara, Santa Barbara, California 93108, USA. sistla@lifesci.ucsb.edu
Nature
|May 17, 2013
概括
北极原变暖加快了植物生长和深层土壤分解,增加了碳储存. 这项研究揭示了
科学领域:
- 生态生态学 生态生态学
- 土壤科学 土壤科学
- 气候变化研究 气候变化研究
背景情况:
- 高度的土壤储存了大量的全球碳.
- 低温限制了北极土壤生物群的活动,分解和营养物质的释放.
- 预计气温上升将改变北极陆地碳平衡.
研究的目的:
- 为了研究实验性变暖对阿拉斯加原生态系统的长期影响.
- 了解在变暖下影响土壤碳动态的结合的非生物-生物反循环.
主要方法:
- 在阿拉斯加的原进行了为期二十年的夏季变暖实验.
- 测量包括植物生物质,土壤温度,微生物活动和土壤碳/储量.
主要成果:
- 变暖增加了植物生物质和木质植物的主导地位.
- 冬季土壤温度因表面变化而间接增加.
- 表面土壤分解活性被抑制,但深层矿物地平线分解活性和碳储量增加 ("生物觉醒").
- 土壤总碳和储量保持不变,导致生态系统碳储量的增加.
结论:
- 北极原的变暖可能会导致生态系统碳储量的增加.
- 由于气候变暖导致的土壤生物群活动的变化,特别是在更深的地平线上,对碳平衡至关重要.
- 观察到的反应表明,在气候变化下,北极陆地生态系统可能发生重大变化.
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