Bibliographie complète
Stoichiometric and nutrient resorption characteristics of dominant tree species in subtropical Chinese forests
Type de ressource
Auteurs/contributeurs
- Zeng, Yelin (Auteur)
- Fang, Xi (Auteur)
- Xiang, Wenhua (Auteur)
- Deng, Xiangwen (Auteur)
- Peng, Changhui (Auteur)
Titre
Stoichiometric and nutrient resorption characteristics of dominant tree species in subtropical Chinese forests
Résumé
Abstract
This study investigated seasonal patterns in stoichiometric ratios, nutrient resorption characteristics, and nutrient use strategies of dominant tree species at three successional stages in subtropical China, which have not been fully understood. Fresh leaf and leaf litterfall samples were collected in growing and nongrowing seasons for determining the concentrations of carbon (C), nitrogen (N), and phosphorus (P). Then, stoichiometric ratios (i.e., C:N, C:P, N:P, and C:N:P) and resorption parameters were calculated. Our results found that there was no consistent variation in leaf C:N and C:P ratios among different species. However, leaf N:P ratios in late‐successional species became significantly higher, indicating that P limitation increases during successional development. Due to the P limitation in this study area, P resorption efficiency and proficiency were higher than corresponding N resorption parameters. Dominant tree species at early‐successional stage adopted “conservative consumption” nutrient use strategy, whereas the species at late‐successional stage inclined to adopt “resource spending” strategy.
Publication
Ecology and Evolution
Volume
7
Numéro
24
Pages
11033-11043
Date
12/2017
Abrév. de revue
Ecology and Evolution
Langue
en
ISSN
2045-7758, 2045-7758
Consulté le
18/11/2024 14:48
Catalogue de bibl.
DOI.org (Crossref)
Autorisations
Référence
Zeng, Y., Fang, X., Xiang, W., Deng, X., & Peng, C. (2017). Stoichiometric and nutrient resorption characteristics of dominant tree species in subtropical Chinese forests. Ecology and Evolution, 7(24), 11033–11043. https://doi.org/10.1002/ece3.3527
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