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Leaf stoichiometry is synergistically-driven by climate, site, soil characteristics and phylogeny in karst areas, Southwest China

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A Correction to this article was published on 27 July 2021

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Abstract

Leaf stoichiometry and its biogeography play vital roles in nutrient cycling of plant communities. To understand the potential drivers of leaf stoichiometry in karst ecosystems, we measured leaf morphological traits (dry mass content (DM), specific leaf area (SLA)), and biochemical traits (C, N, P, K and Ca stoichiometry) of 53 species of different functional groups, as well as soil properties, across seven karst sites in Southwest China, and explored the relationships between these leaf traits and environmental factors. The results showed that: (1) in karst areas of Southwest China, there were higher leaf C and Ca concentrations as well as higher N/P and K/P ratios compared to other ecosystems, plants were more limited by P rather than by N; (2) mean annual temperature positively influenced leaf N, P, and Ca, while mean annual precipitation exerted more influence on leaf K; (3) a strong phylogeny signal was detected in leaf N (p < 0.05), and significant influence of species composition on the variance of leaf N, K, and Ca was observed (p < 0.05); (4) the influence of soil properties on leaf P and Ca, and the influence of leaf features (SLA and DM) on leaf K were also observed based on a variance partitioning analysis. Abiotic factors such as soil, site, and climate were more important than biotic factors (leaf features and phylogeny) in determining leaf N, P, and Ca. In general, the driving factors exhibited a synergistic effect on leaf stoichiometry across different sites, offering a key mechanism that needs to be integrated into the modeling of biogeochemical nutrients cycling in karst ecosystems.

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All data generated or analyzed during this study are included in this published article and its supplementary information files.

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Acknowledgements

This study was financially supported by National Nature Science Foundation of China (41630752, 31670410), and the Young People Fund of Guangxi Science and Technology Department (2019GXNSFBA245036, 2019GXNSFBA245097). Special thanks to Peter Hahn for providing language help in the revision of this manuscript.

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YL and WH designed the experiment. YL, WH and TC performed the experiment and collected the leaf and soil samples. YL, LO and GN analyzed the data. YL, PZ and LZ wrote the manuscript, YL, JW, PZ and DH revised the manuscript, JW particularly modified the revised MS both in contents and English writing. All authors contributed critically to the drafts and gave final approval for publication.

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Correspondence to Ping Zhao.

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We declare that we have no financial and personal relationships with other people or organizations that can inappropriately influence our work, there is no professional or other personal interest of any nature or kind in any product, service or company that could be construed as influencing the position presented in, or the review of, the manuscript entitled.

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Responsible Editor: Melanie A. Mayes

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The original version of this article was revised: the figure legends of Figures 3–4 were corrected.

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Li, Y., He, W., Wu, J. et al. Leaf stoichiometry is synergistically-driven by climate, site, soil characteristics and phylogeny in karst areas, Southwest China. Biogeochemistry 155, 283–301 (2021). https://doi.org/10.1007/s10533-021-00826-3

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  • DOI: https://doi.org/10.1007/s10533-021-00826-3

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