4.7 Article

Carbon, Nitrogen and Phosphorus Stoichiometry in Natural and Plantation Forests in China

Journal

FORESTS
Volume 13, Issue 5, Pages -

Publisher

MDPI
DOI: 10.3390/f13050755

Keywords

C N P stoichiometry; natural forests; plantations; succession stage; climatic factors

Categories

Funding

  1. China National Science Foundation [42130506]
  2. Startup Foundation for Introducing Talent of NUIST [2019r065]
  3. Ministry of Science and Technology of China [G2021014071L]
  4. Spanish Government [PID2019-110521GB-I00]
  5. Catalan government project [SGR2017-1005]
  6. Fundacion Ramon Areces project [CIVP20A6621]

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This study indicates that natural forests are more efficient in utilizing phosphorus compared to plantation forests; the growth of plantation forests is limited by phosphorus; geographical and climatic factors do not fully explain the difference in phosphorus content between natural forests and plantation forests; native forests with native species are better at conserving phosphorus.
Ecological stoichiometry is essential for understanding the biogeochemical cycle in forest ecosystems. However, previous studies of ecological stoichiometry have rarely considered the impacts of forest origins, which could help explain why to date so much uncertainty has been reported on this subject. In this study, we tried to reduce this uncertainty by examining carbon (C), nitrogen (N) and phosphorus (P) in roots, litter and soil in both natural and plantation forests throughout China. The sampled forest sites were divided into three groups according to the identified succession stages: early (ES), middle (MS) and late (LS) stages. Our results show that soil C, N and P concentrations were significantly higher in natural (NF) than in plantation (PL) forests. As succession/growth proceeded, P concentrations significantly increased in litter, roots and soil in NF, while the opposite occurred in PL. These results indicate that NF are able to use P more efficiently than PL, especially in the LS. Furthermore, the higher root N:P ratio indicates that the growth of PL was limited by P in both MS and LS. Our results also suggest that geographical and climatic factors are not the dominant factors in the differences in P between NF and PL, and, even more clearly and importantly, that native forests with native species are more capable of conserving P than planted forests, which are frequently less diverse and dominated by fast-growing non-site native species. These results will help improve biogeochemical models and forest management throughout the world.

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