Patterns and environmental drivers of C, N, and P stoichiometry in the leaf‐litter‐soil system associated with Mongolian pine forests

Abstract

AbstractEcological stoichiometry is an important approach to understand plant nutrient cycling and balance in the forest ecosystem. However, understanding of stoichiometric patterns through the leaf‐litter‐soil system of Mongolian pine among different stand origins is still scarce. Therefore, to reveal the variations in Mongolian pine carbon (C), nitrogen (N), and phosphorus (P) stoichiometry and stoichiometric homeostasis among different stand origins, we measured C, N, and P concentrations of leaves, litter, and soil, and analyzed the nutrient resorption efficiencies of leaves in differently aged plantations and natural forests from semi‐arid and dry sub‐humid regions. The results showed that (1) the stand origin had a significant effect on the C–N–P stoichiometry, and also significantly affected leaf N and P reabsorption efficiencies. Leaf N/P ratios indicated that Mongolian pine was co‐limited by N and P in the NF, HB and HQ, and was mainly limited by P in MU. (2) With increasing stand age, C concentrations in the leaf‐litter‐soil system initially increased and then decreased, the N and P concentrations and reabsorption efficiencies in the leaf‐litter‐soil system were gradually increased. Overall, stand age had a significant effect on N concentrations, C/N and C/P ratios in the leaf‐litter‐soil system. (3) The C and N elements between the leaf‐litter‐soil system had a strong coupling relationship, and the P element between litter‐soil had a strong coupling relationship. In addition, plantations exhibited greater N/P homeostasis than natural forests, and N/P exhibited greater homeostasis than N and P alone, which may be a nutrient utilization strategy for forests to alleviate N or P limitation. (4) Environmental factors have a significant influence on C–N–P stoichiometry in the leaf‐litter‐soil system, the most important soil properties and meteorological factors being soil water content and precipitation, respectively. These results will be essential to provide guidance for plantation restoration and management in desert regions.