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      Carbon:Nitrogen:Phosphorus Stoichiometry in Fungi: A Meta-Analysis

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          Abstract

          Surveys of carbon:nitrogen:phosphorus ratios are available now for major groups of biota and for various aquatic and terrestrial biomes. However, while fungi play an important role in nutrient cycling in ecosystems, relatively little is known about their C:N:P stoichiometry and how it varies across taxonomic groups, functional guilds, and environmental conditions. Here we present the first systematic compilation of C:N:P data for fungi including four phyla (Ascomycota, Basidiomycota, Glomeromycota, and Zygomycota). The C, N, and P contents (percent of dry mass) of fungal biomass varied from 38 to 57%, 0.23 to 15%, and 0.040 to 5.5%, respectively. Median C:N:P stoichiometry for fungi was 250:16:1 (molar), remarkably similar to the canonical Redfield values. However, we found extremely broad variation in fungal C:N:P ratios around the central tendencies in C:N:P ratios. Lower C:P and N:P ratios were found in Ascomycota fungi than in Basidiomycota fungi while significantly lower C:N ratios ( p < 0.05) and higher N:P ratios ( p < 0.01) were found in ectomycorrhizal fungi than in saprotrophs. Furthermore, several fungal stoichiometric ratios were strongly correlated with geographic and abiotic environmental factors, especially latitude, precipitation, and temperature. The results have implications for understanding the roles that fungi play in function in symbioses and in soil nutrient cycling. Further work is needed on the effects of actual in situ growth conditions of fungal growth on stoichiometry in the mycelium.

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          Most cited references44

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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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              SCALING OF C:N:P STOICHIOMETRY IN FORESTS WORLDWIDE: IMPLICATIONS OF TERRESTRIAL REDFIELD-TYPE RATIOS

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                Author and article information

                Contributors
                Journal
                Front Microbiol
                Front Microbiol
                Front. Microbiol.
                Frontiers in Microbiology
                Frontiers Media S.A.
                1664-302X
                14 July 2017
                2017
                : 8
                : 1281
                Affiliations
                [1] 1Institute of Medicinal Plants, Yunnan Academy of Agricultural Sciences Kunming, China
                [2] 2School of Life Sciences, Arizona State University, Tempe AZ, United States
                [3] 3Flathead Lake Biological Station, University of Montana, Polson MT, United States
                Author notes

                Edited by: Télesphore Sime-Ngando, Centre National de la Recherche Scientifique (CNRS), France

                Reviewed by: Michael Danger, Université de Lorraine, France; Marcela Claudia Pagano, Universidade Federal de Minas Gerais, Brazil

                *Correspondence: James J. Elser, jim.elser@ 123456flbs.umt.edu

                This article was submitted to Aquatic Microbiology, a section of the journal Frontiers in Microbiology

                Article
                10.3389/fmicb.2017.01281
                5508194
                28751879
                3423b482-f3f7-4450-af7c-cbfe14da1325
                Copyright © 2017 Zhang and Elser.

                This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

                History
                : 28 February 2017
                : 26 June 2017
                Page count
                Figures: 3, Tables: 3, Equations: 0, References: 51, Pages: 9, Words: 0
                Funding
                Funded by: National Natural Science Foundation of China 10.13039/501100001809
                Award ID: 31460538
                Categories
                Microbiology
                Original Research

                Microbiology & Virology
                elemental composition,fungus,guild,homeostasis,redfield ratios,stoichiometry
                Microbiology & Virology
                elemental composition, fungus, guild, homeostasis, redfield ratios, stoichiometry

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