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      Variation and evolution of C:N ratio among different organs enable plants to adapt to N-limited environments.

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          Abstract

          Carbon (C) and nitrogen (N) are the primary elements involved in the growth and development of plants. The C:N ratio is an indicator of nitrogen use efficiency (NUE) and an input parameter for some ecological and ecosystem models. However, knowledge remains limited about the convergent or divergent variation in the C:N ratios among different plant organs (e.g., leaf, branch, trunk, and root) and how evolution and environment affect the coefficient shifts. Using systematic measurements of the leaf-branch-trunk-root of 2,139 species from tropical to cold-temperate forests, we comprehensively evaluated variation in C:N ratio in different organs in different taxa and forest types. The ratios showed convergence in the direction of change but divergence in the rate of change. Plants evolved toward lower C:N ratios in the leaf and branch, with N playing a more important role than C. The C:N ratio of plant organs (except for the leaf) was constrained by phylogeny, but not strongly. Both the change of C:N during evolution and its spatial variation (lower C:N ratio at midlatitudes) help develop the adaptive growth hypothesis. That is, plants with a higher C:N ratio promote NUE under strong N-limited conditions to ensure survival priority, whereas plants with a lower C:N ratio under less N-limited environments benefit growth priority. In nature, larger proportion of species with a high C:N ratio enabled communities to inhabit more N-limited conditions. Our results provide new insights on the evolution and drivers of C:N ratio among different plant organs, as well as provide a quantitative basis to optimize land surface process models.

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          Author and article information

          Journal
          Glob Chang Biol
          Global change biology
          Wiley
          1365-2486
          1354-1013
          Dec 24 2019
          Affiliations
          [1 ] Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China.
          [2 ] College of Resources and Environment, University of Chinese Academy of Sciences, Beijing, China.
          [3 ] Institute of Grassland Science, Northeast Normal University and Key Laboratory of Vegetation Ecology, Ministry of Education, Changchun, China.
          [4 ] The Key Laboratory for Forest Resources and Ecosystem Processes of Beijing, Beijing Forestry University, Beijing, China.
          [5 ] College of Life and Environmental Sciences, Minzu University of China, Beijing, China.
          [6 ] Faculty of Natural Resources Management, Lakehead University, Thunder Bay, ON, Canada.
          [7 ] Key Laboratory for Humid Subtropical Eco-Geographical Processes of the Ministry of Education, Fujian Normal University, Fuzhou, China.
          [8 ] Department of Forest Resources, University of Minnesota, St Paul, MN, USA.
          [9 ] Hawkesbury Institute for the Environment, Western Sydney University, Penrith, NSW, Australia.
          Article
          10.1111/gcb.14973
          31873968
          a91a9095-db5c-4235-84de-809ba40112bb
          © 2019 John Wiley & Sons Ltd.
          History

          adaptation,carbon,ecological stoichiometry,evolution,forest,latitude,nitrogen,variation

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