Zhisheng Yao , Rui Wang , Han Zhang , Lei Ma , Xunhua Zheng , Chunyan Liu , Wei Zhang , Yanqiang Wang , Bo Zhu , Klaus Butterbach-Bahl
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Here we report two-year field measurements of these trace-gas fluxes and associated environmental controls from different degradation treatments (unaffected or moderately affected meadow, heavily affected meadow with very severe signs of degradation) across three alpine meadow sites at different elevations on the Tibetan Plateau. Our results show that seasonal patterns of these gas fluxes were driven by the variations in soil temperature, moisture and C or N availability, and that non-growing season fluxes contributed 29 %-39 %, 29 %-93 % and 16 %-61 % to the annual CH<sub>4</sub>, N<sub>2</sub>O and NO budgets, respectively. Over the multiple site-years, annual CH<sub>4</sub> uptake ranged from 1.14–1.49 kg C ha<sup>-1</sup> yr<sup>-1</sup> for the healthy meadows to 1.42–2.85 kg C ha<sup>-1</sup> yr<sup>-1</sup> for the degraded meadows, indicating significant increases in CH<sub>4</sub> uptake following grassland degradation by rodents. However, the climate benefits of increased CH<sub>4</sub> uptake were overshadowed by a significant stimulation of annual N<sub>2</sub>O emissions following the degradation, resulting in the net non-CO<sub>2</sub> greenhouse gas (GHG) fluxes of 48.1–364 kg CO<sub>2</sub>-eq ha<sup>-1</sup> yr<sup>-1</sup>. Also, grassland degradation by rodents significantly increased annual NO emissions to 0.35–1.19 kg N ha<sup>-1</sup> yr<sup>-1</sup>. Based on estimates of rodent-induced degradation across the Tibetan alpine grasslands, we estimated that degradation increased soil non-CO<sub>2</sub> GHG emissions by 2012 Gg CO<sub>2</sub>-eq yr<sup>-1</sup> and stimulated NO losses by 9.54 Gg N yr<sup>-1</sup>. Our results highlight the important contribution of rodent-induced grassland degradation to regional or global climate change, and point to the urgent need for policy development for the sustainable use of grasslands.</div></div>","PeriodicalId":50839,"journal":{"name":"Agricultural and Forest Meteorology","volume":"368 ","pages":"Article 110534"},"PeriodicalIF":5.6000,"publicationDate":"2025-04-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Rodent-induced grassland degradation increases annual non-CO2 greenhouse gas fluxes and NO losses despite CH4 uptake enhancement\",\"authors\":\"Zhisheng Yao , Rui Wang , Han Zhang , Lei Ma , Xunhua Zheng , Chunyan Liu , Wei Zhang , Yanqiang Wang , Bo Zhu , Klaus Butterbach-Bahl\",\"doi\":\"10.1016/j.agrformet.2025.110534\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Widespread degradation of grasslands due to human activities and climate change provides favorable habitats for subterranean rodents, whose subsequent bioturbation such as burrowing and mound building further exacerbates the ongoing degradation, thereby directly and indirectly altering biogeochemical C and N cycles. However, it remains unclear how rodent-induced degradation of grasslands affects soil CH<sub>4</sub>, N<sub>2</sub>O and NO fluxes. Here we report two-year field measurements of these trace-gas fluxes and associated environmental controls from different degradation treatments (unaffected or moderately affected meadow, heavily affected meadow with very severe signs of degradation) across three alpine meadow sites at different elevations on the Tibetan Plateau. Our results show that seasonal patterns of these gas fluxes were driven by the variations in soil temperature, moisture and C or N availability, and that non-growing season fluxes contributed 29 %-39 %, 29 %-93 % and 16 %-61 % to the annual CH<sub>4</sub>, N<sub>2</sub>O and NO budgets, respectively. Over the multiple site-years, annual CH<sub>4</sub> uptake ranged from 1.14–1.49 kg C ha<sup>-1</sup> yr<sup>-1</sup> for the healthy meadows to 1.42–2.85 kg C ha<sup>-1</sup> yr<sup>-1</sup> for the degraded meadows, indicating significant increases in CH<sub>4</sub> uptake following grassland degradation by rodents. However, the climate benefits of increased CH<sub>4</sub> uptake were overshadowed by a significant stimulation of annual N<sub>2</sub>O emissions following the degradation, resulting in the net non-CO<sub>2</sub> greenhouse gas (GHG) fluxes of 48.1–364 kg CO<sub>2</sub>-eq ha<sup>-1</sup> yr<sup>-1</sup>. Also, grassland degradation by rodents significantly increased annual NO emissions to 0.35–1.19 kg N ha<sup>-1</sup> yr<sup>-1</sup>. 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引用次数: 0
摘要
人类活动和气候变化造成的草地大面积退化为地下啮齿动物提供了有利的栖息地,而啮齿动物随后的生物扰动(如穴居和筑土堆)进一步加剧了草地的持续退化,从而直接和间接地改变了生物地球化学的碳和氮循环。然而,啮齿动物引起的草地退化如何影响土壤中的甲烷、一氧化二氮和一氧化氮通量,目前仍不清楚。在此,我们报告了对青藏高原三个不同海拔高度的高寒草甸不同退化处理(未受影响或中度受影响草甸、受严重影响且退化迹象非常严重的草甸)的这些痕量气体通量及相关环境控制的两年实地测量结果。我们的研究结果表明,这些气体通量的季节性模式是由土壤温度、湿度和碳或氮的可用性变化驱动的,非生长季节的通量对全年甲烷、一氧化二氮和一氧化氮预算的贡献率分别为29%-39%、29%-93%和16%-61%。在多个地点年中,健康草地的年CH4吸收量为1.14-1.49 kg C ha-1 yr-1,退化草地的年CH4吸收量为1.42-2.85 kg C ha-1 yr-1,这表明啮齿动物造成草地退化后,CH4吸收量显著增加。然而,啮齿动物造成草地退化后,每年一氧化二氮(N2O)的排放量显著增加,从而导致非二氧化碳温室气体(GHG)净通量为每年每公顷 48.1-364 千克二氧化碳当量。此外,啮齿动物造成的草地退化也大大增加了氮氧化物的年排放量,达到 0.35-1.19 千克氮(每公顷每年)。根据对整个西藏高寒草原啮齿动物引起的退化的估计,我们估计退化使土壤非二氧化碳温室气体排放量增加了2012千兆克二氧化碳当量/年-1,并使氮氧化物的损失增加了9.54千兆克氮当量/年-1。我们的研究结果突显了啮齿动物引起的草地退化对区域或全球气候变化的重要影响,并指出迫切需要制定可持续利用草地的政策。
Rodent-induced grassland degradation increases annual non-CO2 greenhouse gas fluxes and NO losses despite CH4 uptake enhancement
Widespread degradation of grasslands due to human activities and climate change provides favorable habitats for subterranean rodents, whose subsequent bioturbation such as burrowing and mound building further exacerbates the ongoing degradation, thereby directly and indirectly altering biogeochemical C and N cycles. However, it remains unclear how rodent-induced degradation of grasslands affects soil CH4, N2O and NO fluxes. Here we report two-year field measurements of these trace-gas fluxes and associated environmental controls from different degradation treatments (unaffected or moderately affected meadow, heavily affected meadow with very severe signs of degradation) across three alpine meadow sites at different elevations on the Tibetan Plateau. Our results show that seasonal patterns of these gas fluxes were driven by the variations in soil temperature, moisture and C or N availability, and that non-growing season fluxes contributed 29 %-39 %, 29 %-93 % and 16 %-61 % to the annual CH4, N2O and NO budgets, respectively. Over the multiple site-years, annual CH4 uptake ranged from 1.14–1.49 kg C ha-1 yr-1 for the healthy meadows to 1.42–2.85 kg C ha-1 yr-1 for the degraded meadows, indicating significant increases in CH4 uptake following grassland degradation by rodents. However, the climate benefits of increased CH4 uptake were overshadowed by a significant stimulation of annual N2O emissions following the degradation, resulting in the net non-CO2 greenhouse gas (GHG) fluxes of 48.1–364 kg CO2-eq ha-1 yr-1. Also, grassland degradation by rodents significantly increased annual NO emissions to 0.35–1.19 kg N ha-1 yr-1. Based on estimates of rodent-induced degradation across the Tibetan alpine grasslands, we estimated that degradation increased soil non-CO2 GHG emissions by 2012 Gg CO2-eq yr-1 and stimulated NO losses by 9.54 Gg N yr-1. Our results highlight the important contribution of rodent-induced grassland degradation to regional or global climate change, and point to the urgent need for policy development for the sustainable use of grasslands.
期刊介绍:
Agricultural and Forest Meteorology is an international journal for the publication of original articles and reviews on the inter-relationship between meteorology, agriculture, forestry, and natural ecosystems. Emphasis is on basic and applied scientific research relevant to practical problems in the field of plant and soil sciences, ecology and biogeochemistry as affected by weather as well as climate variability and change. Theoretical models should be tested against experimental data. Articles must appeal to an international audience. Special issues devoted to single topics are also published.
Typical topics include canopy micrometeorology (e.g. canopy radiation transfer, turbulence near the ground, evapotranspiration, energy balance, fluxes of trace gases), micrometeorological instrumentation (e.g., sensors for trace gases, flux measurement instruments, radiation measurement techniques), aerobiology (e.g. the dispersion of pollen, spores, insects and pesticides), biometeorology (e.g. the effect of weather and climate on plant distribution, crop yield, water-use efficiency, and plant phenology), forest-fire/weather interactions, and feedbacks from vegetation to weather and the climate system.