Soil organic matter properties drive microbial enzyme activities and greenhouse gas fluxes along an elevational gradient

IF 5.6 1区 农林科学 Q1 SOIL SCIENCE
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Abstract

Mountain ecosystems, contributing substantially to the global carbon (C) and nitrogen (N) biogeochemical cycles, are heavily impacted by global changes. Although soil respiration and microbial activities have been extensively studied at different elevation, little is known on the relationships between environmental drivers, microbial functions, and greenhouse gas fluxes (GHGs; carbon dioxide [CO2], methane [CH4] and nitrous oxide [N2O]) in soils of different elevation. Here, we measured how in situ GHG fluxes were linked to soil properties, soil organic matter (SOM) quantity and composition (the proportion of humic-like vs. protein-like OM), microbial biomass, enzyme activities and functional gene abundances in natural soils spanning an elevational gradient of ∼2400 m in Switzerland. Soil CO2 fluxes did not significantly vary from low (lowland zone) to higher (montane and subalpine zones) elevation forests, but decreased significantly (P<0.001) from the treeline to the mountain summit. Multivariate analyses revealed that CO2 fluxes were controlled by C-acquiring enzymatic activities which were mainly controlled by air mean annual temperature (MAT) and SOM quantity and composition. CH4 fluxes were characterized by uptake of atmospheric CH4, but no trend was observed along the elevation. N2O fluxes were also dominated by uptake of atmospheric N2O. The flux rates remained stable with increasing elevation below the treeline, but decreased significantly (P<0.001) from the treeline to the summit. N2O fluxes were driven by specific nitrifying and denitrifying microbial genes (ammonia-oxidizing amoA and N2O-producing norB), which were again controlled by SOM quantity and composition. Our study indicates the treeline as a demarcation point changing the patterns of CO2 and N2O fluxes along the elevation, highlighting the importance of SOM quantity and composition in controlling microbial enzyme activities and GHG fluxes.

土壤有机质特性驱动微生物酶活动和温室气体通量沿海拔梯度变化
山区生态系统对全球碳(C)和氮(N)生物地球化学循环有重大贡献,受到全球变化的严重影响。虽然对不同海拔高度的土壤呼吸和微生物活动进行了广泛研究,但对不同海拔高度土壤中环境驱动因素、微生物功能和温室气体通量(GHGs;二氧化碳 [CO]、甲烷 [CH] 和氧化亚氮 [NO])之间的关系却知之甚少。在这里,我们测量了瑞士海拔高度在 2400 米以上的天然土壤中温室气体通量与土壤特性、土壤有机质(SOM)数量和组成(腐殖质类有机质与蛋白质类有机质的比例)、微生物生物量、酶活性和功能基因丰度之间的关系。从低海拔森林(低地带)到高海拔森林(山地带和亚高山带),土壤一氧化碳通量没有明显变化,但从林木线到山顶,土壤一氧化碳通量明显下降(P<0.001)。多变量分析表明,CO通量受C获取酶活性的控制,而C获取酶活性主要受空气年平均温度(MAT)和SOM数量及组成的控制。CH通量的特点是吸收大气中的CH,但没有观察到沿海拔上升的趋势。氮通量也以吸收大气中的氮为主。随着海拔高度的增加,树线以下的通量速率保持稳定,但从树线到山顶,通量速率显著下降(P<0.001)。氮氧化物通量由特定的硝化和反硝化微生物基因(氨氧化 A 和产生氮氧化物的 B)驱动,而这些基因又受 SOM 数量和组成的控制。我们的研究表明,树线是一个分界点,它改变了沿海拔高度的 CO 和 NO 通量模式,突出了 SOM 的数量和组成在控制微生物酶活性和温室气体通量方面的重要性。
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来源期刊
Geoderma
Geoderma 农林科学-土壤科学
CiteScore
11.80
自引率
6.60%
发文量
597
审稿时长
58 days
期刊介绍: Geoderma - the global journal of soil science - welcomes authors, readers and soil research from all parts of the world, encourages worldwide soil studies, and embraces all aspects of soil science and its associated pedagogy. The journal particularly welcomes interdisciplinary work focusing on dynamic soil processes and functions across space and time.
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