Intensified plant N and C pool with more available nitrogen under experimental warming in an alpine meadow ecosystem
Nitrogen (N) availability is projected to increase in a warming climate. But whether the more available N is immobilized by microbes (thus stimulates soil carbon (C) decomposition), or is absorbed by plants (thus intensifies C uptake) remains unknown in the alpine meadow ecosystem. Infrared heaters...
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ftpubmed:oai:pubmedcentral.nih.gov:5167058 2023-05-15T17:57:49+02:00 Intensified plant N and C pool with more available nitrogen under experimental warming in an alpine meadow ecosystem Peng, Fei Xue, Xian You, Quangang Xu, Manhou Chen, Xiang Guo, Jian Wang, Tao 2016-11-06 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5167058/ https://doi.org/10.1002/ece3.2583 en eng John Wiley and Sons Inc. http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5167058/ http://dx.doi.org/10.1002/ece3.2583 © 2016 The Authors. Ecology and Evolution published by John Wiley & Sons Ltd. This is an open access article under the terms of the Creative Commons Attribution (http://creativecommons.org/licenses/by/4.0/) License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. CC-BY Original Research Text 2016 ftpubmed https://doi.org/10.1002/ece3.2583 2017-01-01T01:03:59Z Nitrogen (N) availability is projected to increase in a warming climate. But whether the more available N is immobilized by microbes (thus stimulates soil carbon (C) decomposition), or is absorbed by plants (thus intensifies C uptake) remains unknown in the alpine meadow ecosystem. Infrared heaters were used to simulate climate warming with a paired experimental design. Soil ammonification, nitrification, and net mineralization were obtained by in situ incubation in a permafrost region of the Qinghai‐Tibet Plateau (QTP). Available N significantly increased due to the stimulation of net nitrification and mineralization in 0–30 cm soil layer. Microbes immobilized N in the end of growing season in both warming and control plots. The magnitude of immobilized N was lower in the warming plots. The root N concentration significantly reduced, but root N pool intensified due to the significant increase in root biomass in the warming treatment. Our results suggest that a warming‐induced increase in biomass is the major N sink and will continue to stimulate plant growth until plant N saturation, which could sustain the positive warming effect on ecosystem productivity. Text permafrost PubMed Central (PMC) Ecology and Evolution 6 23 8546 8555 |
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Original Research Peng, Fei Xue, Xian You, Quangang Xu, Manhou Chen, Xiang Guo, Jian Wang, Tao Intensified plant N and C pool with more available nitrogen under experimental warming in an alpine meadow ecosystem |
topic_facet |
Original Research |
description |
Nitrogen (N) availability is projected to increase in a warming climate. But whether the more available N is immobilized by microbes (thus stimulates soil carbon (C) decomposition), or is absorbed by plants (thus intensifies C uptake) remains unknown in the alpine meadow ecosystem. Infrared heaters were used to simulate climate warming with a paired experimental design. Soil ammonification, nitrification, and net mineralization were obtained by in situ incubation in a permafrost region of the Qinghai‐Tibet Plateau (QTP). Available N significantly increased due to the stimulation of net nitrification and mineralization in 0–30 cm soil layer. Microbes immobilized N in the end of growing season in both warming and control plots. The magnitude of immobilized N was lower in the warming plots. The root N concentration significantly reduced, but root N pool intensified due to the significant increase in root biomass in the warming treatment. Our results suggest that a warming‐induced increase in biomass is the major N sink and will continue to stimulate plant growth until plant N saturation, which could sustain the positive warming effect on ecosystem productivity. |
format |
Text |
author |
Peng, Fei Xue, Xian You, Quangang Xu, Manhou Chen, Xiang Guo, Jian Wang, Tao |
author_facet |
Peng, Fei Xue, Xian You, Quangang Xu, Manhou Chen, Xiang Guo, Jian Wang, Tao |
author_sort |
Peng, Fei |
title |
Intensified plant N and C pool with more available nitrogen under experimental warming in an alpine meadow ecosystem |
title_short |
Intensified plant N and C pool with more available nitrogen under experimental warming in an alpine meadow ecosystem |
title_full |
Intensified plant N and C pool with more available nitrogen under experimental warming in an alpine meadow ecosystem |
title_fullStr |
Intensified plant N and C pool with more available nitrogen under experimental warming in an alpine meadow ecosystem |
title_full_unstemmed |
Intensified plant N and C pool with more available nitrogen under experimental warming in an alpine meadow ecosystem |
title_sort |
intensified plant n and c pool with more available nitrogen under experimental warming in an alpine meadow ecosystem |
publisher |
John Wiley and Sons Inc. |
publishDate |
2016 |
url |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5167058/ https://doi.org/10.1002/ece3.2583 |
genre |
permafrost |
genre_facet |
permafrost |
op_relation |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5167058/ http://dx.doi.org/10.1002/ece3.2583 |
op_rights |
© 2016 The Authors. Ecology and Evolution published by John Wiley & Sons Ltd. This is an open access article under the terms of the Creative Commons Attribution (http://creativecommons.org/licenses/by/4.0/) License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. |
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CC-BY |
op_doi |
https://doi.org/10.1002/ece3.2583 |
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Ecology and Evolution |
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6 |
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23 |
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8546 |
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8555 |
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1766166317691305984 |