Temporal dynamics of climate sensitivity of litter decomposition in a semi-arid grassland

Climate warming, precipitation changes, and reactive nitrogen (N) input are important environmental changes that can critically affect litter decomposition and soil carbon (C) dynamics. However, it remains unclear whether and how their effects and/or relative contribution vary across different decom...

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Main Authors: Zhen Li, Fuwei Wang, Yue Wen, Chenglong Ye, Peng Wang, Tongshuo Bai, Xudong Gu, Liang Guo, Yunpeng Qiu, Yi Zhang, Yi Wang, Shuijin Hu
Format: Article
Language:English
Published: Elsevier 2025-01-01
Series:Geoderma
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Online Access:http://www.sciencedirect.com/science/article/pii/S0016706124003860
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author Zhen Li
Fuwei Wang
Yue Wen
Chenglong Ye
Peng Wang
Tongshuo Bai
Xudong Gu
Liang Guo
Yunpeng Qiu
Yi Zhang
Yi Wang
Shuijin Hu
author_facet Zhen Li
Fuwei Wang
Yue Wen
Chenglong Ye
Peng Wang
Tongshuo Bai
Xudong Gu
Liang Guo
Yunpeng Qiu
Yi Zhang
Yi Wang
Shuijin Hu
author_sort Zhen Li
collection DOAJ
description Climate warming, precipitation changes, and reactive nitrogen (N) input are important environmental changes that can critically affect litter decomposition and soil carbon (C) dynamics. However, it remains unclear whether and how their effects and/or relative contribution vary across different decomposition stages. We assessed the effects of warming, precipitation changes and N addition, alone and in combination, on litter loss at various stages of the decomposition process in a semi-arid grassland. We found that warming inhibited litter decomposition in the early stage (1–2 years) and promoted it in the later stage (3–4 years). The temperature sensitivity of decomposition was affected by both soil moisture and N addition. Increased precipitation significantly accelerated litter decomposition initially, but not in the later stages. In the litter-soil incubation experiment, we observed that high-quality litter, characterized by low carbohydrate C:methoxyl C (CC:MC) ratio and/or CN ratios, displayed greater sensitivity to changes in moisture. In comparison, low-quality litter exhibits high temperature sensitivity of microbial respiration. Overall, our findings show that the climate sensitivity of litter decomposition exhibited distinct temporal dynamics, with increasing warming sensitivity of decomposition and decreasing moisture sensitivity of decomposition over time. Given that many current decomposition models use a constant sensitivity parameter (e.g., Q10 value = 2.0) throughout the decay process, our results suggest that incorporation of such temporal dynamics into decomposition models may enhance their predictive power.
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spelling doaj-art-da861a6eeb33469cb763f88f7e694d4e2025-01-10T04:36:48ZengElsevierGeoderma1872-62592025-01-01453117157Temporal dynamics of climate sensitivity of litter decomposition in a semi-arid grasslandZhen Li0Fuwei Wang1Yue Wen2Chenglong Ye3Peng Wang4Tongshuo Bai5Xudong Gu6Liang Guo7Yunpeng Qiu8Yi Zhang9Yi Wang10Shuijin Hu11Ecosystem Ecology Lab, College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing 210095, ChinaEcosystem Ecology Lab, College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing 210095, ChinaEcosystem Ecology Lab, College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing 210095, ChinaEcosystem Ecology Lab, College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing 210095, ChinaEcosystem Ecology Lab, College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing 210095, ChinaEcosystem Ecology Lab, College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing 210095, ChinaNingxia Yunwu Mountains Grassland Natural Reserve Administration, Guyuan 756000, ChinaState Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Northwest A&F University, Yangling, Shaanxi 712100, China; Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, Shaanxi 712100, China; University of Chinese Academy of Sciences, Beijing 100049, ChinaEcosystem Ecology Lab, College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing 210095, ChinaEcosystem Ecology Lab, College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing 210095, ChinaState Key Laboratory of Loess and Quaternary, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710061, ChinaEcosystem Ecology Lab, College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing 210095, China; Department of Entomology & Plant Pathology, North Carolina State University, Raleigh, NC 27695, USA; Corresponding author at: Department of Entomology & Plant Pathology, North Carolina State University, Raleigh, NC 27695-7616, USA.Climate warming, precipitation changes, and reactive nitrogen (N) input are important environmental changes that can critically affect litter decomposition and soil carbon (C) dynamics. However, it remains unclear whether and how their effects and/or relative contribution vary across different decomposition stages. We assessed the effects of warming, precipitation changes and N addition, alone and in combination, on litter loss at various stages of the decomposition process in a semi-arid grassland. We found that warming inhibited litter decomposition in the early stage (1–2 years) and promoted it in the later stage (3–4 years). The temperature sensitivity of decomposition was affected by both soil moisture and N addition. Increased precipitation significantly accelerated litter decomposition initially, but not in the later stages. In the litter-soil incubation experiment, we observed that high-quality litter, characterized by low carbohydrate C:methoxyl C (CC:MC) ratio and/or CN ratios, displayed greater sensitivity to changes in moisture. In comparison, low-quality litter exhibits high temperature sensitivity of microbial respiration. Overall, our findings show that the climate sensitivity of litter decomposition exhibited distinct temporal dynamics, with increasing warming sensitivity of decomposition and decreasing moisture sensitivity of decomposition over time. Given that many current decomposition models use a constant sensitivity parameter (e.g., Q10 value = 2.0) throughout the decay process, our results suggest that incorporation of such temporal dynamics into decomposition models may enhance their predictive power.http://www.sciencedirect.com/science/article/pii/S0016706124003860Climate changesThe sensitivity of decompositionSemi-arid grasslandsTemporal dynamics13C NMRLitter quality
spellingShingle Zhen Li
Fuwei Wang
Yue Wen
Chenglong Ye
Peng Wang
Tongshuo Bai
Xudong Gu
Liang Guo
Yunpeng Qiu
Yi Zhang
Yi Wang
Shuijin Hu
Temporal dynamics of climate sensitivity of litter decomposition in a semi-arid grassland
Geoderma
Climate changes
The sensitivity of decomposition
Semi-arid grasslands
Temporal dynamics
13C NMR
Litter quality
title Temporal dynamics of climate sensitivity of litter decomposition in a semi-arid grassland
title_full Temporal dynamics of climate sensitivity of litter decomposition in a semi-arid grassland
title_fullStr Temporal dynamics of climate sensitivity of litter decomposition in a semi-arid grassland
title_full_unstemmed Temporal dynamics of climate sensitivity of litter decomposition in a semi-arid grassland
title_short Temporal dynamics of climate sensitivity of litter decomposition in a semi-arid grassland
title_sort temporal dynamics of climate sensitivity of litter decomposition in a semi arid grassland
topic Climate changes
The sensitivity of decomposition
Semi-arid grasslands
Temporal dynamics
13C NMR
Litter quality
url http://www.sciencedirect.com/science/article/pii/S0016706124003860
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