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Shifts in soil nutrient concentrations and C:N:P stoichiometry during long-term natural vegetation restoration

BACKGROUND: Ecological stoichiometry (C:N:P ratios) in soil is an important indicator of the elemental balance in ecological interactions and processes. Long-term natural vegetation plays an important role in the accumulation and distribution of soil stoichiometry. However, information about the eff...

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Autores principales: Ma, Rentian, Hu, Feinan, Liu, Jingfang, Wang, Chunli, Wang, Zilong, Liu, Gang, Zhao, Shiwei
Formato: Online Artículo Texto
Lenguaje:English
Publicado: PeerJ Inc. 2020
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6982410/
https://www.ncbi.nlm.nih.gov/pubmed/32002329
http://dx.doi.org/10.7717/peerj.8382
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author Ma, Rentian
Hu, Feinan
Liu, Jingfang
Wang, Chunli
Wang, Zilong
Liu, Gang
Zhao, Shiwei
author_facet Ma, Rentian
Hu, Feinan
Liu, Jingfang
Wang, Chunli
Wang, Zilong
Liu, Gang
Zhao, Shiwei
author_sort Ma, Rentian
collection PubMed
description BACKGROUND: Ecological stoichiometry (C:N:P ratios) in soil is an important indicator of the elemental balance in ecological interactions and processes. Long-term natural vegetation plays an important role in the accumulation and distribution of soil stoichiometry. However, information about the effects of long-term secondary forest succession on soil stoichiometry along a deep soil profile is still limited. METHODS: We selected Ziwuling secondary succession forest developed from farmland as the study area, investigated the concentrations and stoichiometry of soil organic carbon (SOC), total nitrogen (TN), and total phosphorus (TP) at a depth of 0–100 cm along a 90-year succession chronosequence, including farmland (control), grassland, shrub, early forest, and climax forest. RESULTS: SOC and TN concentrations significantly increased with increasing restoration age, whereas soil P concentration remained relatively stable across various successional stages. SOC and TN concentrations decreased with an increase in soil depth, exhibiting distinct soil nutrient “surface-aggregation” (high nutrients concentration in the top soil layer). The soil C:P and N:P ratios increased with an increase in restoration age, whereas the variation of the C:N ratio was small and relatively stable across vegetation succession. The nutrient limitation changed along with vegetation succession, transitioning from limited N in the earlier successional stages to limited P in the later successional stages. CONCLUSION: Our results suggest that more nitrogen input should be applied to earlier succession stages, and more phosphorus input should be utilized in later succession stages in order to address limited availability of these elements. In general, natural vegetation restoration was an ecologically beneficial practice for the recovery of degraded soils in this area. The findings of this study strengthen our understanding of the changes of soil nutrient concentration and nutrient limitation after vegetation restoration, and provide a simple guideline for future vegetation restoration and reconstruction efforts on the Loess Plateau.
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spelling pubmed-69824102020-01-30 Shifts in soil nutrient concentrations and C:N:P stoichiometry during long-term natural vegetation restoration Ma, Rentian Hu, Feinan Liu, Jingfang Wang, Chunli Wang, Zilong Liu, Gang Zhao, Shiwei PeerJ Agricultural Science BACKGROUND: Ecological stoichiometry (C:N:P ratios) in soil is an important indicator of the elemental balance in ecological interactions and processes. Long-term natural vegetation plays an important role in the accumulation and distribution of soil stoichiometry. However, information about the effects of long-term secondary forest succession on soil stoichiometry along a deep soil profile is still limited. METHODS: We selected Ziwuling secondary succession forest developed from farmland as the study area, investigated the concentrations and stoichiometry of soil organic carbon (SOC), total nitrogen (TN), and total phosphorus (TP) at a depth of 0–100 cm along a 90-year succession chronosequence, including farmland (control), grassland, shrub, early forest, and climax forest. RESULTS: SOC and TN concentrations significantly increased with increasing restoration age, whereas soil P concentration remained relatively stable across various successional stages. SOC and TN concentrations decreased with an increase in soil depth, exhibiting distinct soil nutrient “surface-aggregation” (high nutrients concentration in the top soil layer). The soil C:P and N:P ratios increased with an increase in restoration age, whereas the variation of the C:N ratio was small and relatively stable across vegetation succession. The nutrient limitation changed along with vegetation succession, transitioning from limited N in the earlier successional stages to limited P in the later successional stages. CONCLUSION: Our results suggest that more nitrogen input should be applied to earlier succession stages, and more phosphorus input should be utilized in later succession stages in order to address limited availability of these elements. In general, natural vegetation restoration was an ecologically beneficial practice for the recovery of degraded soils in this area. The findings of this study strengthen our understanding of the changes of soil nutrient concentration and nutrient limitation after vegetation restoration, and provide a simple guideline for future vegetation restoration and reconstruction efforts on the Loess Plateau. PeerJ Inc. 2020-01-22 /pmc/articles/PMC6982410/ /pubmed/32002329 http://dx.doi.org/10.7717/peerj.8382 Text en ©2020 Ma et al. https://creativecommons.org/licenses/by/4.0/ This is an open access article distributed under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0/) , which permits unrestricted use, distribution, reproduction and adaptation in any medium and for any purpose provided that it is properly attributed. For attribution, the original author(s), title, publication source (PeerJ) and either DOI or URL of the article must be cited.
spellingShingle Agricultural Science
Ma, Rentian
Hu, Feinan
Liu, Jingfang
Wang, Chunli
Wang, Zilong
Liu, Gang
Zhao, Shiwei
Shifts in soil nutrient concentrations and C:N:P stoichiometry during long-term natural vegetation restoration
title Shifts in soil nutrient concentrations and C:N:P stoichiometry during long-term natural vegetation restoration
title_full Shifts in soil nutrient concentrations and C:N:P stoichiometry during long-term natural vegetation restoration
title_fullStr Shifts in soil nutrient concentrations and C:N:P stoichiometry during long-term natural vegetation restoration
title_full_unstemmed Shifts in soil nutrient concentrations and C:N:P stoichiometry during long-term natural vegetation restoration
title_short Shifts in soil nutrient concentrations and C:N:P stoichiometry during long-term natural vegetation restoration
title_sort shifts in soil nutrient concentrations and c:n:p stoichiometry during long-term natural vegetation restoration
topic Agricultural Science
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6982410/
https://www.ncbi.nlm.nih.gov/pubmed/32002329
http://dx.doi.org/10.7717/peerj.8382
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