Microbial drought resistance may destabilize soil carbon

被引:42
作者
Allison, Steven D. [1 ,2 ]
机构
[1] Univ Calif Irvine, Dept Ecol & Evolutionary Biol, Irvine, CA 92697 USA
[2] Univ Calif Irvine, Dept Earth Syst Sci, Irvine, CA 92697 USA
基金
美国国家科学基金会;
关键词
COMMUNITIES; RESPONSES; DECOMPOSITION; CONSEQUENCES; DESICCATION; INCREASES; CLIMATE; LEGACY; LIFE;
D O I
10.1016/j.tim.2023.03.002
中图分类号
Q5 [生物化学]; Q7 [分子生物学];
学科分类号
071010 ; 081704 ;
摘要
Droughts are becoming more frequent and intense with climate change. As plants and microbes respond to drought, there may be consequences for the vast stocks of organic carbon stored in soils. If microbes sustain their activity under drought, soils could lose carbon, especially if inputs from plants decline. Empirical and theoretical studies reveal multiple mechanisms of microbial drought resistance, including tolerance and avoidance. Physiological responses allow microbes to acclimate to drought within minutes to days. Along with dis-persal, shifts in community composition could allow microbiomes to maintain functioning despite drought. Microbes might also adapt to drier conditions through evolutionary processes. Together, these mechanisms could result in soil carbon losses larger than currently anticipated under climate change.
引用
收藏
页码:780 / 787
页数:8
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