TY - JOUR
T1 - Green Manure Coupled With Straw Returning Increases Soil Organic Carbon via Decreased Priming Effect and Enhanced Microbial Carbon Pump
AU - Zhou, Guopeng
AU - Li, Guilong
AU - Liang, Hai
AU - Liu, Rui
AU - Ma, Zhengbo
AU - Gao, Songjuan
AU - Chang, Danna
AU - Liu, Jia
AU - Chadwick, David R
AU - Jones, Davey L
AU - Cao, Weidong
N1 - © 2025 John Wiley & Sons Ltd.
PY - 2025/5/7
Y1 - 2025/5/7
N2 - ABSTRACTGreen manuring and crop straw returning are widely used to increase soil organic carbon (SOC) sequestration, while the pathways and drivers in native SOC mineralization and new SOC formation after implementing these practices remain unclear. Here, through a 10‐locations' network field experiment in southern China, the effects of green manuring (Mv), rice straw returning (Rs), and their combination (MR) on soil C sequestration efficiency (CSE) were evaluated. A microcosmic experiment was performed to trace the components and participants of SOC mineralization and formation under the three practices. The network experiment showed that Mv, Rs, and MR annually improved SOC stock by 119.7, 477.0, and 830.2 kg C ha−1, respectively, with MR having the highest CSE of 23.1%, followed by Rs (17.7%) and Mv (13.3%). The microcosmic experiment further revealed that the highest CSE in MR most likely resulted from the low mineralization of native SOC (positive priming effects, PE) and great formation of new SOC through microbial C pump (MCP). Therein, MR mainly downregulated the K‐strategists of the microbial community (e.g., Gaiellales) to yield negative PE on recalcitrant native SOC, such as protein/amino sugar‐ and lignin‐like molecules; meanwhile, MR had the highest bacterial and fungal MCPs, which were, respectively, led by r‐strategists (e.g., Sporobacter) and molds (e.g., Cladosporium). The study highlights the advantages of mixing low‐ (Rs) and high‐quality (Mv) residues for efficiently increasing SOC sequestration and firstly discovers the core microbes that dominate the mineralization and formation of SOC in paddy fields.
AB - ABSTRACTGreen manuring and crop straw returning are widely used to increase soil organic carbon (SOC) sequestration, while the pathways and drivers in native SOC mineralization and new SOC formation after implementing these practices remain unclear. Here, through a 10‐locations' network field experiment in southern China, the effects of green manuring (Mv), rice straw returning (Rs), and their combination (MR) on soil C sequestration efficiency (CSE) were evaluated. A microcosmic experiment was performed to trace the components and participants of SOC mineralization and formation under the three practices. The network experiment showed that Mv, Rs, and MR annually improved SOC stock by 119.7, 477.0, and 830.2 kg C ha−1, respectively, with MR having the highest CSE of 23.1%, followed by Rs (17.7%) and Mv (13.3%). The microcosmic experiment further revealed that the highest CSE in MR most likely resulted from the low mineralization of native SOC (positive priming effects, PE) and great formation of new SOC through microbial C pump (MCP). Therein, MR mainly downregulated the K‐strategists of the microbial community (e.g., Gaiellales) to yield negative PE on recalcitrant native SOC, such as protein/amino sugar‐ and lignin‐like molecules; meanwhile, MR had the highest bacterial and fungal MCPs, which were, respectively, led by r‐strategists (e.g., Sporobacter) and molds (e.g., Cladosporium). The study highlights the advantages of mixing low‐ (Rs) and high‐quality (Mv) residues for efficiently increasing SOC sequestration and firstly discovers the core microbes that dominate the mineralization and formation of SOC in paddy fields.
KW - Microbiota
KW - Carbon Sequestration
KW - Soil Microbiology
KW - China
KW - stable isotope probing
KW - Oryza
KW - biomarkers
KW - Carbon - analysis - metabolism
KW - priming effect
KW - Soil - chemistry
KW - Manure - analysis
KW - Agriculture - methods
KW - microbial carbon pump
KW - soil carbon components
U2 - 10.1111/gcb.70232
DO - 10.1111/gcb.70232
M3 - Article
C2 - 40329747
SN - 1365-2486
VL - 31
SP - e70232
JO - Global Change Biology
JF - Global Change Biology
IS - 5
ER -