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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...
Autores principales: | , , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
PeerJ Inc.
2020
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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. |
format | Online Article Text |
id | pubmed-6982410 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2020 |
publisher | PeerJ Inc. |
record_format | MEDLINE/PubMed |
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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