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      Stoichiometric controls on carbon, nitrogen, and phosphorus dynamics in decomposing litter

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      Ecological Monographs
      Wiley-Blackwell

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          Global patterns of plant leaf N and P in relation to temperature and latitude.

          A global data set including 5,087 observations of leaf nitrogen (N) and phosphorus (P) for 1,280 plant species at 452 sites and of associated mean climate indices demonstrates broad biogeographic patterns. In general, leaf N and P decline and the N/P ratio increases toward the equator as average temperature and growing season length increase. These patterns are similar for five dominant plant groups, coniferous trees and four angiosperm groups (grasses, herbs, shrubs, and trees). These results support the hypotheses that (i) leaf N and P increase from the tropics to the cooler and drier midlatitudes because of temperature-related plant physiological stoichiometry and biogeographical gradients in soil substrate age and then plateau or decrease at high latitudes because of cold temperature effects on biogeochemistry and (ii) the N/P ratio increases with mean temperature and toward the equator, because P is a major limiting nutrient in older tropical soils and N is the major limiting nutrient in younger temperate and high-latitude soils.
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            C:N:P stoichiometry in soil: is there a “Redfield ratio” for the microbial biomass?

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              Litterfall, Nutrient Cycling, and Nutrient Limitation in Tropical Forests

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                Author and article information

                Journal
                Ecological Monographs
                Ecological Monographs
                Wiley-Blackwell
                0012-9615
                February 2010
                February 2010
                : 80
                : 1
                : 89-106
                Article
                10.1890/09-0179.1
                efd75cba-4b87-4d45-ba1e-a82af5156016
                © 2010

                http://doi.wiley.com/10.1002/tdm_license_1.1

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