State Key Laboratory of Biocontrol, Guangdong Provincial Key Laboratory of Plant Stress Biology, School of Agriculture and Biotechnology, Shenzhen Campus of Sun Yat-sen University, Sun Yat-sen University, Shenzhen, Guangdong 518107, China; Jiangsu Provincial Key Lab for Solid Organic Waste Utilization, Jiangsu Collaborative Innovation Center for Solid Organic Waste Resource Utilization, Nanjing Agricultural University, Nanjing 210095, China; Center for Grassland Microbiome, State Key Laboratory of Herbage Improvement and Grassland Agro-Ecosystems, College of Pastoral Agriculture Science and Technology, Lanzhou University, Lanzhou 730020, Gansu, China.
State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi, Xinjiang 830011, China.
Environ Int. 2024 Oct;192:109043. doi: 10.1016/j.envint.2024.109043. Epub 2024 Oct 2.
The frequency and intensity of extreme weather events, including rapid temperature fluctuations, are increasing because of climate change. Long-term fertilization practices have been observed to alter microbial physiology and community structure, thereby affecting soil carbon sequestration. However, the effects of warming on the carbon sequestration potential of soil microbes adapted to long-term fertilization remain poorly understood. In this study, we utilized O isotope labeling to assess microbial carbon use efficiency (CUE) and employed stable isotope probing (SIP) with O-HO to identify growing taxa in response to temperature changes (5-35 °C). Organic amendment with manure or straw residue significantly increased microbial CUE by 86-181 % compared to unfertilized soils. The microorganisms inhabiting organic amended soils displayed greater resistance of microbial CUE to high temperatures (25-35 °C) compared to those inhabiting soils fertilized only with minerals. Microbial growth patterns determined by the classification of taxa into incorporators or non-incorporators based on O incorporation into DNA exhibited limited phylogenetic conservation in response to temperature changes. Microbial clusters were identified by grouping taxa with similar growth patterns across different temperatures. Organic amendments enriched microbial clusters associated with increased CUE, whereas clusters in unfertilized or mineral-only fertilized soils were linked to decreased CUE. Specifically, shifts in the composition of growing bacteria were correlated with enhanced microbial CUE, whereas modifications in the composition of growing fungi were associated with diminished CUE. Notably, the responses of microbial CUE to temperature fluctuations were primarily driven by changes in the bacterial composition. Overall, our findings demonstrate that organic amendments enhance soil microbial CUE and promote the enrichment of specific microbial clusters that are better equipped to cope with temperature changes. This study establishes a theoretical foundation for manipulating soil microbes to enhance carbon sequestration under global climate scenarios.
由于气候变化,包括快速温度波动在内的极端天气事件的频率和强度正在增加。长期施肥实践已被观察到改变微生物生理和群落结构,从而影响土壤碳固存。然而,变暖对适应长期施肥的土壤微生物的碳固存潜力的影响仍知之甚少。在这项研究中,我们利用 O 同位素标记来评估微生物碳利用效率 (CUE),并使用 O-HO 的稳定同位素探测 (SIP) 来识别对温度变化 (5-35°C) 做出响应的生长类群。与未施肥土壤相比,有机肥(粪肥或秸秆残渣)添加可使微生物 CUE 提高 86-181%。与仅施矿物质的土壤相比,栖息在有机添加土壤中的微生物对高温(25-35°C)的微生物 CUE 具有更强的抵抗力。基于 O 掺入 DNA 将分类为掺入者或非掺入者的分类来确定微生物生长模式,对温度变化的表现出有限的系统发育保守性。通过将具有相似生长模式的分类群分组为聚类,可以识别微生物聚类。有机添加物富集了与 CUE 增加相关的微生物聚类,而在未施肥或仅施矿物质的土壤中,聚类与 CUE 降低相关。具体而言,生长细菌组成的变化与增强的微生物 CUE 相关,而生长真菌组成的变化与降低的 CUE 相关。值得注意的是,微生物 CUE 对温度波动的响应主要受细菌组成变化的驱动。总体而言,我们的研究结果表明,有机添加物可提高土壤微生物的 CUE,并促进特定微生物聚类的富集,这些聚类更有能力应对温度变化。这项研究为在全球气候情景下操纵土壤微生物以增强碳固存提供了理论基础。