TY - JOUR
T1 - Millimeter-scale leaf litter placement modulates carbon dioxide and methane emissions in wetlands
AU - Liu, Hao
AU - Zhang, Yining
AU - Cai, Yu-Jia
AU - Liu, Zi-Yan
AU - Li, Liang
AU - Wang, Ya-Qin
AU - Shu, Xiao
AU - Goodacre, Royston
AU - Chen, Zheng
PY - 2025/6
Y1 - 2025/6
N2 - Flooded soils play a crucial role in global carbon cycling, acting as significant reservoirs of soil organic carbon and sources of carbon emissions. Leaf litter, especially from local vegetation, is a key contributor to soil organic carbon formation in these ecosystems, with its decomposition driving the production of carbon dioxide (CO2) and methane (CH4). Although numerous studies have examined the factors influencing leaf litter decomposition and associated greenhouse gas emissions, the impact of millimeter-scale variations in leaf litter placement within the soil-water interfaces (SWI) has received little attention. This study hypothesizes that even small changes in burial depth could significantly affect the emission patterns of CO2 and CH4. To test this hypothesis, a microcosm experiment was conducted to monitor gas fluxes and physicochemical profiles in treatments with leaf litter placed uncovered at the SWI (LU) or covered by a thin (10 mm) soil layer (LC). The results demonstrated substantial shifts in emissions: cumulative CH4 emissions were more than doubled in the LC group (115.3 μgC) compared to the LU group (42.5 μgC), while cumulative CO2 emissions were reduced by 25 % in the LC group (77 mgC) versus the LU group (103 mgC). Consequently, the overall global warming potential over a 20-year horizon (GWP20) was 13.2 % lower for the LC treatment (280.7 mgCO2e) compared to the LU treatment (323.3 mgCO2e). These findings advance our understanding of wetland carbon dynamics by revealing that a millimeter-scale change in leaf litter placement significantly alters the spatiotemporal patterns and partitioning of CO2 and CH4 emissions, highlighting the critical role of micro-scale heterogeneity in regulating greenhouse gas fluxes. Moreover, our results demonstrate a decoupling of CO2 and CH4 responses to this small-scale environmental variation, ultimately leading to a reduction in overall global warming potential despite increased methane release.
AB - Flooded soils play a crucial role in global carbon cycling, acting as significant reservoirs of soil organic carbon and sources of carbon emissions. Leaf litter, especially from local vegetation, is a key contributor to soil organic carbon formation in these ecosystems, with its decomposition driving the production of carbon dioxide (CO2) and methane (CH4). Although numerous studies have examined the factors influencing leaf litter decomposition and associated greenhouse gas emissions, the impact of millimeter-scale variations in leaf litter placement within the soil-water interfaces (SWI) has received little attention. This study hypothesizes that even small changes in burial depth could significantly affect the emission patterns of CO2 and CH4. To test this hypothesis, a microcosm experiment was conducted to monitor gas fluxes and physicochemical profiles in treatments with leaf litter placed uncovered at the SWI (LU) or covered by a thin (10 mm) soil layer (LC). The results demonstrated substantial shifts in emissions: cumulative CH4 emissions were more than doubled in the LC group (115.3 μgC) compared to the LU group (42.5 μgC), while cumulative CO2 emissions were reduced by 25 % in the LC group (77 mgC) versus the LU group (103 mgC). Consequently, the overall global warming potential over a 20-year horizon (GWP20) was 13.2 % lower for the LC treatment (280.7 mgCO2e) compared to the LU treatment (323.3 mgCO2e). These findings advance our understanding of wetland carbon dynamics by revealing that a millimeter-scale change in leaf litter placement significantly alters the spatiotemporal patterns and partitioning of CO2 and CH4 emissions, highlighting the critical role of micro-scale heterogeneity in regulating greenhouse gas fluxes. Moreover, our results demonstrate a decoupling of CO2 and CH4 responses to this small-scale environmental variation, ultimately leading to a reduction in overall global warming potential despite increased methane release.
KW - Soil-water interfaces
KW - Methane
KW - Carbon dioxide
KW - Leaf litter
KW - Physical disturbances
U2 - 10.1016/j.apgeochem.2025.106475
DO - 10.1016/j.apgeochem.2025.106475
M3 - Article
SN - 0883-2927
VL - 190
SP - 106475
JO - Applied Geochemistry
JF - Applied Geochemistry
ER -