文献类型： 外文期刊
作者： Fu, Haoran 1 ; Chen, Hong 5 ; Ma, Zhengbo 6 ; Liang, Guopeng 7 ; Chadwick, David R. 4 ; Jones, Davey L. 4 ; Wanek, Wolfgang 10 ; Wu, Lianghuan 1 ; Ma, Qingxu 1 ;
作者机构： 1.Zhejiang Univ, Coll Environm & Resource Sci, Minist Educ, Key Lab Environm Remediat & Ecosyst Hlth, Hangzhou, Peoples R China
2.Zhejiang Univ, State Key Lab Soil Pollut Control & Safety, Hangzhou, Peoples R China
3.Zhejiang Univ, Zhejiang Prov Key Lab Agr Resources & Environm, Hangzhou, Peoples R China
4.Bangor Univ, Sch Environm & Nat Sci, Bangor, Gwynedd, Wales
5.Zhejiang Univ, Sch Publ Affairs, Hangzhou, Peoples R China
6.Chinese Acad Agr Sci, Inst Agr Resources & Reg Planning, Key Lab Plant Nutr & Fertiliser, Minist Agr, Beijing, Peoples R China
7.Yale Univ, Dept Ecol & Evolutionary Biol, New Haven, CT USA
8.Univ Michigan, Inst Global Change Biol, Ann Arbor, MI USA
9.Univ Michigan, Sch Environm & Sustainabil, Ann Arbor, MI USA
10.Univ Vienna, Ctr Microbiol & Environm Syst Sci, Dept Microbiol & Ecosyst Sci, Div Terr Ecosyst Res, Vienna, Austria
关键词： bacterial necromass carbon; ecosystem; fungal necromass carbon; plant-derived carbon; soil organic carbon
期刊名称：GLOBAL CHANGE BIOLOGY （ 影响因子：12.0； 五年影响因子：14.0 ）
ISSN： 1354-1013
年卷期： 2025 年 31 卷 8 期
页码：
收录情况： SCI
摘要： Soil organic carbon (C) is derived primarily from plant and microbial necromass; however, the global distribution and contribution of different necromass inputs to soil C storage remain unclear. We conducted a global meta-analysis encompassing 2410 observations from 249 microbial necromass studies and 786 observations from 72 plant residue studies. The results showed that the content of microbial-derived C (10.63 +/- 0.39 g C kg-1 soil) exceeded that of plant-derived C (lignin phenol carbon (LPC), 5.63 +/- 0.45 g C kg-1 soil), across the 0-100 cm soil profile, with fungal necromass carbon (FNC; 7.24 +/- 0.21 g C kg-1) contributing the most to soil C-a pattern consistently observed across all depths. In addition, in the topsoil (0-20 cm), forests (9.39 +/- 1.22 g C kg-1) and grasslands (9.73 +/- 1.74 g C kg-1) showed significantly higher LPC contents than croplands and wetlands; therefore, cropland expansion significantly reduces microbial- and plant-derived carbon stocks in topsoil. Global FNC, BNC, and LPC stocks were estimated to be 211 Pg (95% CI: 156-270 Pg), 71 Pg (95% CI: 59-88 Pg) and 168 Pg (95% CI: 151-186 Pg) in topsoil, respectively. Lower soil pH and mean annual temperature were associated with higher FNC, BNC, and LPC contents, particularly in high-latitude regions like North America. These results demonstrate that microbial necromass, rather than plant residues, dominates soil C storage globally. These findings highlight the need for management strategies that address both land-use change and rising temperatures to protect microbial and plant C pools.
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