Rising atmospheric CO2 reduces sequestration of root-derived soil carbon

被引:112
|
作者
Heath, J [1 ]
Ayres, E
Possell, M
Bardgett, RD
Black, HIJ
Grant, H
Ineson, P
Kerstiens, G
机构
[1] Univ Lancaster, Inst Environm & Nat Sci, Dept Biol Sci, Lancaster LA1 4YQ, England
[2] Univ Lancaster, Inst Environm & Nat Sci, Dept Environm Sci, Lancaster LA1 4YQ, England
[3] Lancaster Environm Ctr, Ctr Ecol & Hydrol, Soil Ecol Grp, Lancaster LA1 4AP, England
[4] Lancaster Environm Ctr, Ctr Ecol & Hydrol, Nat Environm Res Council Life Sci Mass Spectromet, Lancaster LA1 4AP, England
[5] Univ York, Dept Biol, Stockholm Environm Inst, York YO10 5YW, N Yorkshire, England
关键词
D O I
10.1126/science.1110700
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Forests have a key role as carbon sinks, which could potentially mitigate the continuing increase in atmospheric carbon dioxide concentration and associated climate change. We show that carbon dioxide enrichment, although causing short-term growth stimulation in a range of European tree species, also leads to an increase in soil microbial respiration and a marked decline in sequestration of root-derived carbon in the soil. These findings indicate that, should similar processes operate in forest ecosystems, the size of the annual terrestrial carbon sink may be substantially reduced; resulting in a positive feedback on the rate of increase in atmospheric carbon dioxide concentration.
引用
收藏
页码:1711 / 1713
页数:3
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