土壤碳
碳纤维
温带气候
微生物种群生物学
土壤有机质
生态系统
碳循环
环境科学
环境化学
生态学
温带雨林
垃圾箱
有机质
温带森林
总有机碳
溶解有机碳
土壤水分
温带落叶林
化学
陆地生态系统
植物凋落物
气候变化
土壤生物学
全球变化
生物地球化学
生物地球化学循环
作文(语言)
土壤生态学
土壤科学
农学
固碳
作者
Meiling Man,Laura Castañeda‐Gómez,Marie‐Ange Moisan,Patrick Gagne,Christine Martineau,Rajshree Ghosh Biswas,Melissa A. Knorr,Serita D. Frey,Marc W. Cadotte,Knute J. Nadelhoffer,Kate Lajtha,André J. Simpson,Myrna J. Simpson
标识
DOI:10.1021/acs.est.5c08706
摘要
Natural climate solutions that focus on increasing carbon in forests rely on the potential for additional carbon that may be incorporated into soil organic matter (SOM). The fate of soil carbon in temperate forests remains uncertain due to the complex role of microbes and their regulation of carbon flows in soils, especially with the addition of extra litter. We identified comprehensive molecular-level evidence that revealed shifts in SOM composition and microbial communities after 30 years of added litter in a temperate deciduous forest. Chronic litter addition failed to add new soil carbon after 30 years and correlated with reorganization in microbial community composition and altered carbon use. Excluding detrital inputs decreased soil carbon content, resulting in enhanced SOM decomposition and shifts toward specific bacterial groups (such as oligotrophs) that can utilize less energetically favorable carbon substrates that are typically more recalcitrant. Collectively, we found that microbial communities shifted in composition and altered carbon use strategies and traits, which aligned with changes to the molecular composition of SOM. Finally, this work demonstrates that in mesic temperate forests, decadal increases in litterfall, resulting from increased ecosystem productivity or management, may not offset soil carbon losses from climate change nor enhance carbon sequestration.
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