Global change reshapes glomalin‐mediated soil carbon sequestration by influencing plant inputs

土壤碳 环境科学 农学 固碳 气候变化 全球变暖 全球变化 营养物 生态系统 碳循环 土壤有机质 地球大气中的二氧化碳 磷 二氧化碳 土壤水分 丛枝菌根真菌 大气碳循环 植物生理学 生物 碳纤维 总有机碳 农林复合经营 生态学 氮气 农业生态系统 土壤科学 氮气循环 格洛马林 全球变暖的影响 含水量 水分 陆地生态系统 土壤肥力
作者
Xianzhen Luo,Lingling Zhang,Hans Lambers,Akhter B. Hossain,S Liu,Hanxia Yu,yuanwen kuang,Dazhi Wen,Enqing Hou
出处
期刊:Functional Ecology [Wiley]
卷期号:40 (3): 655-667
标识
DOI:10.1111/1365-2435.70256
摘要

Abstract Glomalin‐related soil protein (GRSP), a by‐product of arbuscular mycorrhizal fungi (AMF), plays a crucial role in stabilizing soil organic carbon (SOC). Global change factors (GCFs) such as elevated atmospheric carbon dioxide (CO 2 ), climate warming and anthropogenic nitrogen (N) input strongly affect soil AMF activity, consequently influencing GRSP formation. However, the impacts of these GCFs on GRSP dynamics remain poorly understood despite their critical role in SOC accumulation and stability. Through a systematic search of publications, we synthesized 529 observations from 122 primary studies worldwide. We conducted a meta‐analysis to reveal general patterns and drivers of the effects of N, phosphorus (P), their co‐addition, warming, elevated [CO 2 ], drought and forest restoration on easily extractable (EE‐GRSP) and total GRSP (T‐GRSP), and quantitatively assessed the role of GRSP in SOC sequestration. Results showed that N, P, their co‐addition and forest restoration increased EE‐GRSP by 12%, 3.1%, 13.4% and 49%, and T‐GRSP by 13%, 10%, 11% and 65%, respectively, because reduced nutrient limitation stimulated plant inputs and AMF growth, promoting the formation of GRSP. In contrast, elevated [CO 2 ], warming, and drought had negligible effects on GRSP. Machine learning identified plant inputs (partly proxied by plant biomass) as the primary mediator of GRSP changes along with AMF activity. The increases in GRSP were positively correlated with the soil aggregate stability (e.g. mean weight diameter [MWD] of soil aggregates) and SOC, which itself was positively related to the MWD of soil aggregates. Structural equation modelling further validated that GRSP changes, mainly influenced by altered plant inputs and AMF activity, directly enhance SOC accumulation and indirectly contribute to soil aggregate formation and SOC stability. These findings provide insights into the positive role of mycorrhizal fungal metabolites in SOC sequestration and highlight the potential to improve GRSP production to promote carbon sequestration under global environmental change. Read the free Plain Language Summary for this article on the Journal blog.
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