Chin J Plant Ecol ›› 2024, Vol. 48 ›› Issue (11): 1434-1444.DOI: 10.17521/cjpe.2023.0256  cstr: 32100.14.cjpe.2023.0256

Special Issue: 碳循环

• Research Articles • Previous Articles     Next Articles

Priming effect of soil organic carbon decomposition induced by Cunninghamia lanceolate leaf litter and fine root and its response to nitrogen addition in subtropical forests

WANG Liang1, ZHAO Xue-Chao1, YANG Shao-Bo1, WANG Qing-Kui1,2,*()   

  1. 1Anhui Provincial Key Laboratory of Forest Resource and Silviculture, School of Forestry & Landscape Architecture, Anhui Agricultural University, Hefei 230036, China
    2Huitong Experimental Station of Forest Ecology, CAS Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China
  • Received:2023-09-06 Accepted:2024-04-08 Online:2024-11-20 Published:2024-04-09
  • Contact: *WANG Qing-Kui (qwang@iae.ac.cn)
  • Supported by:
    National Natural Science Foundation of China(32171752);National Natural Science Foundation of China(31830015);Natural Science Foundation of Hunan Province of China(2022JJ30468)

Abstract:

Aims Priming effect (PE), as the change in the decomposition rate of soil organic carbon (SOC) caused by exogenous carbon (C) input, plays important roles in regulating the storage and dynamics of global SOC. Leaf litter and fine root are the main sources of SOC in forest ecosystems, which can significantly affect PE. In addition, increased soil nitrogen (N) availability caused by atmospheric N deposition also impacts PE. However, the differences between the PE induced by leaf litter and fine root differ and their response to increased soil N availability remain unclear.

Methods In this study, we conducted a 35-days incubation experiment by adding 13C-labelled leaf litter and fine root into Cunninghamia lanceolate soil. Leaf litter was covered on soil surface and fine root was mixed in the soils to simulate their natural field conditions. The amount and carbon isotope composition (δ13C) value of soil CO2 were measured during the experiment, and soil nutrient contents and microbial community composition were also measured after incubation.

Important findings 1) Leaf litter addition promoted the SOC decomposition, that is, leaf litter induced a positive PE, with the magnitude of 1.69 mg C·kg-1·d-1, while fine root addition induced a negative PE with the magnitude of -1.26 mg C·kg-1·d-1. 2) N addition reduced the magnitude of positive PE induced by leaf litter addition by 38.7%, while it increased the magnitude of negative PE induced by fine root addition by 16.6%. 3) Leaf litter addition reduced fungi bacteria ratio by 22.9%, while adding fine root increased the fungal biomass by 30.8%. Furthermore, N addition increased the fungal bacterial ratio and the fungal biomass. Our results demonstrated the differences in the PE induced by leaf litter and fine root addition, and provided theoretical support for the prediction and management of SOC in forests under the scenario of increasing atmospheric N deposition.

Key words: soil organic carbon decomposition, priming effect, nitrogen deposition, forest litter, soil microbial community composition