Ecological stoichiometry of Cinnamomum migao leaf litter and soil nutrients under nitrogen deposition in a karst region

Abstract Nitrogen (N) deposition, a major phenomenon of climate change, is increasing with industrialization and more human activity and can affect litter decomposition. Yet it remains unclear whether N deposition will accelerate or inhibit the decomposition of litter in karst regions, which are cha...

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Main Authors: Xuefeng Xiao, Jingzhong Chen, Xiaofeng Liao, Jiming Liu, Deng Wang, Jia Li, Qiuxiao Yan
Format: Article
Language:English
Published: Wiley 2021-09-01
Series:Ecosphere
Subjects:
Online Access:https://doi.org/10.1002/ecs2.3738
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spelling doaj-c2c3fc6a2c604b6f9ac99bfc932d759b2021-09-28T23:34:39ZengWileyEcosphere2150-89252021-09-01129n/an/a10.1002/ecs2.3738Ecological stoichiometry of Cinnamomum migao leaf litter and soil nutrients under nitrogen deposition in a karst regionXuefeng Xiao0Jingzhong Chen1Xiaofeng Liao2Jiming Liu3Deng Wang4Jia Li5Qiuxiao Yan6Forestry College Research Center of Forest Ecology Guizhou University Guiyang 550025 ChinaForestry College Research Center of Forest Ecology Guizhou University Guiyang 550025 ChinaInstitute of Mountain Resources Guizhou Academy of Science Guiyang 550001 ChinaForestry College Research Center of Forest Ecology Guizhou University Guiyang 550025 ChinaForestry College Research Center of Forest Ecology Guizhou University Guiyang 550025 ChinaForestry College Research Center of Forest Ecology Guizhou University Guiyang 550025 ChinaForestry College Research Center of Forest Ecology Guizhou University Guiyang 550025 ChinaAbstract Nitrogen (N) deposition, a major phenomenon of climate change, is increasing with industrialization and more human activity and can affect litter decomposition. Yet it remains unclear whether N deposition will accelerate or inhibit the decomposition of litter in karst regions, which are characterized by P‐limitation or N and P co‐limited stress conditions in soil. Here, to document the influence of simulated N deposition on litter decomposition in karst, the leaf litter of Cinnamomum migao was studied, this being a dominant perennial woody plant endemic to karst landforms. We conducted a 300‐d field decomposition experiment with four treatments: control (CK); addition of (+) N at 50 kg⋅ha−1⋅a−1 (N1); +N at 150 kg⋅ha−1⋅a−1 (N2), and +N at 300 kg⋅ha−1⋅a−1 (N3), in southwest Guizhou, the largest karst region in China (n = 4 treatments). From each treatment, the litter samples’ remaining mass were measured during the decomposition period, in addition to their nitrogen (N), phosphorus (P), carbon (C), and potassium (K) concentrations, as well as that of soils; the soil’s pH was also measured. The results showed that litter remaining mass increased significantly under nitrogen deposition, which, as expected, acidified the soil. Meanwhile, litter N, P, and K contents responded to nitrogen deposition, whereas C did not. Otherwise, no direct effects of nitrogen deposition upon soil nutrients were detected. The soil nutrient contents were related to the release of the elements in litter. In conclusion, nitrogen deposition suppressed the decomposition of C. migao litter in karst, but the nutrients of karst soil are mainly replenished by litter inputs.https://doi.org/10.1002/ecs2.3738Cinnamomum migaoecological stoichiometrykarst regionlitter decompositionnitrogen depositionsoil nutrient
collection DOAJ
language English
format Article
sources DOAJ
author Xuefeng Xiao
Jingzhong Chen
Xiaofeng Liao
Jiming Liu
Deng Wang
Jia Li
Qiuxiao Yan
spellingShingle Xuefeng Xiao
Jingzhong Chen
Xiaofeng Liao
Jiming Liu
Deng Wang
Jia Li
Qiuxiao Yan
Ecological stoichiometry of Cinnamomum migao leaf litter and soil nutrients under nitrogen deposition in a karst region
Ecosphere
Cinnamomum migao
ecological stoichiometry
karst region
litter decomposition
nitrogen deposition
soil nutrient
author_facet Xuefeng Xiao
Jingzhong Chen
Xiaofeng Liao
Jiming Liu
Deng Wang
Jia Li
Qiuxiao Yan
author_sort Xuefeng Xiao
title Ecological stoichiometry of Cinnamomum migao leaf litter and soil nutrients under nitrogen deposition in a karst region
title_short Ecological stoichiometry of Cinnamomum migao leaf litter and soil nutrients under nitrogen deposition in a karst region
title_full Ecological stoichiometry of Cinnamomum migao leaf litter and soil nutrients under nitrogen deposition in a karst region
title_fullStr Ecological stoichiometry of Cinnamomum migao leaf litter and soil nutrients under nitrogen deposition in a karst region
title_full_unstemmed Ecological stoichiometry of Cinnamomum migao leaf litter and soil nutrients under nitrogen deposition in a karst region
title_sort ecological stoichiometry of cinnamomum migao leaf litter and soil nutrients under nitrogen deposition in a karst region
publisher Wiley
series Ecosphere
issn 2150-8925
publishDate 2021-09-01
description Abstract Nitrogen (N) deposition, a major phenomenon of climate change, is increasing with industrialization and more human activity and can affect litter decomposition. Yet it remains unclear whether N deposition will accelerate or inhibit the decomposition of litter in karst regions, which are characterized by P‐limitation or N and P co‐limited stress conditions in soil. Here, to document the influence of simulated N deposition on litter decomposition in karst, the leaf litter of Cinnamomum migao was studied, this being a dominant perennial woody plant endemic to karst landforms. We conducted a 300‐d field decomposition experiment with four treatments: control (CK); addition of (+) N at 50 kg⋅ha−1⋅a−1 (N1); +N at 150 kg⋅ha−1⋅a−1 (N2), and +N at 300 kg⋅ha−1⋅a−1 (N3), in southwest Guizhou, the largest karst region in China (n = 4 treatments). From each treatment, the litter samples’ remaining mass were measured during the decomposition period, in addition to their nitrogen (N), phosphorus (P), carbon (C), and potassium (K) concentrations, as well as that of soils; the soil’s pH was also measured. The results showed that litter remaining mass increased significantly under nitrogen deposition, which, as expected, acidified the soil. Meanwhile, litter N, P, and K contents responded to nitrogen deposition, whereas C did not. Otherwise, no direct effects of nitrogen deposition upon soil nutrients were detected. The soil nutrient contents were related to the release of the elements in litter. In conclusion, nitrogen deposition suppressed the decomposition of C. migao litter in karst, but the nutrients of karst soil are mainly replenished by litter inputs.
topic Cinnamomum migao
ecological stoichiometry
karst region
litter decomposition
nitrogen deposition
soil nutrient
url https://doi.org/10.1002/ecs2.3738
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