J Plant Ecol ›› 2025, Vol. 18 ›› Issue (5): rtaf076.DOI: 10.1093/jpe/rtaf076

• Research Articles •    

Soil carbon storage and its driving factors in different plant communities of coastal wetland in the non-growing season

Chen Liang1, Lin-Shui Dong1, Ai-Yun Song1,*, Lei Wang2,* and Jing-Tao Liu1   

  1. 1Shandong Key Laboratory of Eco-Environmental Science for the Yellow River Delta, Shandong University of Aeronautics, Binzhou 256600, China
    2Jiangsu Academy of Forestry, Nanjing 211153, China

    *Corresponding authors. E-mail: xueshu210@126.com (A.Y.S.); 8967976@qq.com (L.W.)
  • Received:2025-01-01 Accepted:2025-05-09 Online:2025-05-24 Published:2025-10-01
  • Supported by:
    This work was supported by the Central Fiscal Forestry Science and Technology Extension Demonstration Project (Su[2023]TG10), Natural Science Foundation of Shandong Province (ZR2020MD007), Special Foundation of Marine Science and Technology Innovation of Jiangsu Province (JSZRHYKJ202305) and the Youth Innovation Support Program of Shandong Universities (2021KJ081).

非生长季滨海湿地不同植物群落土壤碳储量及其驱动因素

Abstract: Plant community composition influences soil carbon (C) storage and stability in coastal wetlands, but such effects remain unclear in the non-growing season. In this study, the soil C content, density and stability were examined across five coastal plant communities—Spartina alterniflora, Suaeda salsa, Phragmites australis, mixed S. alterniflora–S. salsa communities and bare flat in the non-growing season in Yancheng, Jiangsu Province, China. The S. alterniflora community exhibited elevated soil organic and inorganic C contents, owing to its high biomass, strong C retention capacity. The P. australis community showed higher dissolved organic C and microbial biomass C contents, possibly driven by increased soil moisture and inorganic nitrogen (N) that promote microbial decomposition of plant residue. The S. salsa community had the lowest soil organic C density due to its low aboveground biomass, soil moisture and inorganic N and jointly microbial effects. The highest soil inorganic C density was observed in bare flat, which was associated with its high soil moisture. The lowest resistance index of C in P. australis community was associated with low electric conductivity, high C and N availability and bacterial effects. Soil C fractions, densities and resistance index of C decreased with soil depth, likely reflecting reduced water and N availability that constrain root and microbial activities. The results suggest that the S. alterniflora community enhances soil C accumulation, while P. australis community accumulate more labile C fractions, evoking low C stability due to interaction between soil physicochemical and microbial properties.

Key words: coastal wetland, carbon storage, plant community, bare flat, resistance index of carbon

摘要:
植物群落组成显著影响滨海湿地土壤碳储量和稳定性,但这些影响在植物的非生长季尚不清楚。因此,本文研究了非生长季盐城滨海湿地5个植物群落—互花米草(Spartina alterniflora)、盐地碱蓬(Suaeda salsa)、芦苇(Phragmites australis)、互花米草-碱蓬(S. alterniflora–S. salsa)混生群落和无植被光滩土壤的碳含量、密度和稳定性的变化规律。结果表明,互花米草群落土壤有机碳和无机碳含量较高,这可能与互花米草群落植物生物量高、固碳能力强以及细菌丰度降低有关。芦苇群落土壤溶解有机碳和微生物生物量碳含量较高,这可能因为土壤水分和无机氮含量的增加促进了微生物的生长及其对植物残体的分解。受较低的地上生物量、土壤水分和无机氮含量以及微生物共同作用的影响,碱蓬群落土壤有机碳密度最低。然而,光滩土壤无机碳密度最高,且土壤含水量高。芦苇群落碳抵抗性指数最低,这可能与其较低的土壤电导率,较高的碳氮有效性和细菌丰度有关。在所有群落中,土壤碳组分和密度以及碳抵抗性指数均随土壤深度的增加而降低,这可能反映了土壤水分和养分有效性的降低,限制了根系生长和微生物活动。上述研究结果表明,互花米草群落增加了土壤碳积累,芦苇群落积累了更多的不稳定碳组分。由于土壤理化性质与微生物的相互作用,最终导致芦苇群落碳稳定性总体上有所降低。

关键词: 滨海湿地, 碳储量, 植物群落, 光滩, 碳抵抗性指数