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Responses of soil microbial community structure under litter to changes in precipitation and nitrogen addition in a desert steppe 荒漠草原凋落物下土壤微生物群落结构对降水和氮添加变化的响应
IF 3.7 2区 农林科学 Q1 ECOLOGY Pub Date : 2024-11-30 DOI: 10.1016/j.ejsobi.2024.103696
Jinpeng Ma , Lin Chen , Danbo Pang , Yinglong Chen , Mengyao Wu , Yaqi Zhang , Wenqiang He , Xuebin Li
Soil microorganisms are essential in maintaining terrestrial ecosystem function and are central drivers of soil-plant nutrient cycling. However, relatively few studies have explored the impact of precipitation and nitrogen (N) addition on soil microbial community structure beneath litter. In this study, we conducted a field simulation control experiment on litter decomposition under varying precipitation regimes (normal, increased by 30 %, and decreased by 30 %) and N addition levels (0 and 10 g m−2 y−1) in the desert steppe of Yanchi County, China. Our findings revealed that changes in precipitation and N addition promoted litter decomposition and caused the accumulation of soil nutrients. Specifically, N addition significantly increased nitrate nitrogen (51.95 %), ammonium nitrogen (42.92 %), soil organic carbon (6.81 %), and total phosphorus (7.82 %)(P<0.05), decreased precipitation significantly elevated contents of nitrate nitrogen (26.80 %), total nitrogen (24.47 %), soil organic carbon (37.62 %), total phosphorus (22.78 %), and microbial biomass C (33.20 %) (P<0.05). N addition decreased microbial biomarkers content by 1.13 %, but increased microbial diversity indices (Shannon-Wiener index (1.53 %), Brillouin diversity index (0.54 %), Pielou evenness index (1.12 %), Simpson dominance index (0.91 %), Mcintosh diversity index (1.11 %)) (P<0.05). Meanwhile, decreased precipitation significantly enhanced microbial biomarkers content by 5.83 % and diversity indices (Shannon-Wiener index (3.67 %), Brillouin diversity index (2.16 %), Pielou evenness index (1.55 %), Simpson dominance index (1.82 %), Mcintosh diversity index (2.63 %)) (P<0.05). We indicated the decreased precipitation enhanced the effect of N addition on microbial community and diversity, while increased precipitation showed the opposite trend. Redundancy analysis highlighted MBC as a critical factor influencing microbial community structure, accounting for 35.3 % of the variation (P<0.01). This study provides valuable insights into managing and conserving desert steppe ecosystems.
土壤微生物对维持陆地生态系统功能至关重要,是土壤-植物养分循环的核心驱动力。然而,关于降水和氮添加对凋落物下土壤微生物群落结构影响的研究相对较少。在盐池县荒漠草原进行了不同降水(正常、增加30%和减少30%)和N添加水平(0和10 g m−2 y−1)下凋落物分解的野外模拟对照试验。结果表明,降水和施氮量的变化促进了凋落物的分解,引起了土壤养分的积累。其中,氮添加显著提高了硝态氮(51.95%)、铵态氮(42.92%)、土壤有机碳(6.81%)和全磷(7.82%)含量(P<0.05);降水减少显著提高了硝态氮(26.80%)、全氮(24.47%)、土壤有机碳(37.62%)、全磷(22.78%)和微生物生物量C(33.20%)含量(P<0.05)。添加氮使微生物生物标志物含量降低了1.13%,而微生物多样性指数(Shannon-Wiener指数(1.53%)、Brillouin多样性指数(0.54%)、Pielou均匀度指数(1.12%)、Simpson优势度指数(0.91%)、Mcintosh多样性指数(1.11%))升高(P<0.05)。同时,降水减少使微生物生物标志物含量和多样性指数(Shannon-Wiener指数(3.67%)、Brillouin多样性指数(2.16%)、Pielou均匀度指数(1.55%)、Simpson优势度指数(1.82%)、Mcintosh多样性指数(2.63%))显著提高了5.83% (P<0.05)。结果表明,降水减少增强了氮添加对微生物群落和多样性的影响,而降水增加则相反。冗余分析显示MBC是影响微生物群落结构的关键因素,占变异量的35.3% (P<0.01)。该研究为管理和保护荒漠草原生态系统提供了有价值的见解。
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引用次数: 0
Coupling methane oxidation and N2 fixation under methanogenic conditions in contrasting environments 对比环境中甲烷生成条件下甲烷氧化和 N2 固定的耦合作用
IF 3.7 2区 农林科学 Q1 ECOLOGY Pub Date : 2024-11-23 DOI: 10.1016/j.ejsobi.2024.103693
Yongliang Mo , Jiwei Li , Xiaotong Peng , Adrian Ho , Zhongjun Jia
Microbial methane oxidation under widespread suboxic environment is crucial for understanding methane emission. However, the role of aerobic methanotrophs in mediating methane oxidation and nitrogen fixation is less understood in oxygen-limiting environments. In this study, we identified diazotrophic methanotrophs under oxygen-limited conditions (initial O2 of 6–8 μM) in two contrasting habitats (paddy soil and marine sediment) using DNA-based stable isotope probing combined with amplicon sequencing. Consistently, we documented significant 13CH4 oxidation and 15N2 fixation after 740 days of suboxic isotope labeling. Sequencing analysis revealed the predominance of Methylobacter–affiliated aerobic methanotrophs in the 13C-labeled DNA fractions. These Methylobacter-like OTUs accounted for 97.86 % in paddy soil and 99.49 % in marine sediment of the total pmoA gene sequences; while relative abundances for the nifH gene sequences were 91.59 % in paddy soil and 99.49 % in marine sediment. Taken together, our analyses revealed that Methylobacter is responsible for methane oxidation and nitrogen fixation under oxygen limitation in both habitats, demonstrating convergent emergence of this aerobic methanotroph under oxygen deficiency.
广泛亚氧环境下的微生物甲烷氧化作用对于了解甲烷排放至关重要。然而,人们对限氧环境中好氧甲烷营养体在介导甲烷氧化和固氮作用方面的作用了解较少。在本研究中,我们利用基于 DNA 的稳定同位素探针结合扩增子测序,在两种截然不同的生境(水稻土壤和海洋沉积物)中鉴定了限氧条件(初始氧气为 6-8 μM)下的重氮甲烷营养体。一致的是,经过 740 天的亚缺氧同位素标记,我们记录了 13CH4 的显著氧化和 15N2 的固定。测序分析表明,在 13C 标记的 DNA 片段中,主要是与 Methylobacter 相关的需氧甲烷营养体。在水稻田土壤和海洋沉积物的 pmoA 基因总序列中,这些类似甲基杆菌的 OTU 分别占 97.86% 和 99.49%;而在水稻田土壤和海洋沉积物中,nifH 基因序列的相对丰度分别为 91.59% 和 99.49%。总之,我们的分析表明,在缺氧条件下,甲基细菌在两种生境中都负责甲烷氧化和固氮作用,这表明在缺氧条件下这种好氧甲烷营养体的出现是趋同的。
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引用次数: 0
Nutrient supply enhances positive priming of soil organic C under straw amendment and accelerates the incorporation of straw-derived C into organic C pool in paddy soils 养分供应增强了秸秆改良下土壤有机碳的正引力,并加快了秸秆衍生碳融入水稻田土壤有机碳库的速度
IF 3.7 2区 农林科学 Q1 ECOLOGY Pub Date : 2024-11-16 DOI: 10.1016/j.ejsobi.2024.103695
Yuxuan Zhang , Mengya Lu , Zhiquan Wang , Kun Zhang , Bin Zhang , Reziwanguli Naimaiti , Shangyuan Wei , Xueli Ding
Straw return accelerates the decomposition of soil organic C (SOC), a phenomenon referred to as the priming effect. However, the interactive influence of nutrient supply levels on priming effect intensity and SOC sequestration in paddy soils still needs to be better understood. In this study, we investigated the dynamics of the priming effect and associated changes in phospholipid fatty acids, enzyme activity, and microbial necromass following the addition of 13C-labelled rice straw (98 % atom) to soils under three nutrient supply levels during a 300-d incubation period. Our results showed that the addition of straw (5 g C kg−1 soil) with no-nutrient (S + Nu0), low nutrient (S + Nulow, 42 mg N kg−1, 10 mg P kg−1), and high nutrient (S + Nuhigh, 126 mg N kg−1, 30 mg P kg−1) supply increased total CO2 production by 42.9 %, 59.0 %, and 97.3 %, respectively, compared to the control soil. After 300 d, the cumulative priming effect was nearly doubled in the S + Nulow and tripled in the S + Nuhigh compared to the S + Nu0. Moreover, the intensity of priming varied with the incubation stage under nutrient treatments. Similar patterns of priming effect were observed across all straw amendments during the early incubation stages; however, the priming effect increased with the nutrient supply levels in the later stages. These patterns are linked to microbial metabolic limitation and resource acquisition strategies, as evidenced by a lower C-to-N stoichiometry of extracellular enzymes and necromass in the S + Nulow S + Nuhigh. A greater proportion of straw-derived C incorporation into SOC (indicated by higher levels 13C-SOC) in nutrient-enriched was found, which largely offset the native SOC losses, resulting in high SOC content by the end of incubation. Our findings highlight the critical role of nutrient supply in regulating the priming effect and the balance of SOC after straw return in paddy soils.
秸秆还田可加速土壤有机碳(SOC)的分解,这种现象被称为引诱效应。然而,养分供应水平对稻田土壤引诱效应强度和 SOC 固碳的交互影响仍有待进一步了解。在本研究中,我们研究了在三种养分供应水平下的土壤中添加 13C 标记的稻草(原子含量为 98%)后,在 300 天的培养期内引诱效应的动态变化以及磷脂脂肪酸、酶活性和微生物坏死物质的相关变化。结果表明,与对照土壤相比,在无养分(S + Nu0)、低养分(S + Nulow,42 mg N kg-1,10 mg P kg-1)和高养分(S + Nuhigh,126 mg N kg-1,30 mg P kg-1)条件下添加稻草(5 g C kg-1 土壤)可使二氧化碳总产量分别增加 42.9%、59.0% 和 97.3%。300 d 后,与 S + Nu0 相比,S + Nulow 的累积引诱效果几乎翻了一番,S + Nuhigh 的累积引诱效果则翻了三番。此外,在营养处理下,引诱作用的强度随培养阶段的不同而变化。在早期培养阶段,所有秸秆改良剂都观察到了类似的引诱效应模式;然而,在后期阶段,引诱效应随着营养供应水平的提高而增加。这些模式与微生物的代谢限制和资源获取策略有关,S + Nulow S + Nuhigh 中细胞外酶和坏死物质的 C-N 比化学计量较低就是证明。在营养丰富的情况下,秸秆衍生的碳有更大比例掺入 SOC(13C-SOC 含量更高),这在很大程度上抵消了原生 SOC 的损失,导致培养结束时 SOC 含量较高。我们的研究结果突显了养分供应在调节稻田土壤秸秆还田后的引诱效应和 SOC 平衡中的关键作用。
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引用次数: 0
In-depth insights into carbohydrate-active enzyme genes regarding the disparities in soil organic carbon after 12-year rotational cropping system field study 深入了解碳水化合物活性酶基因对 12 年轮作系统田间研究后土壤有机碳差异的影响
IF 3.7 2区 农林科学 Q1 ECOLOGY Pub Date : 2024-11-16 DOI: 10.1016/j.ejsobi.2024.103694
Hao Wang , JinPing Chen , Mingxue Du , Yihao Ruan , Jiameng Guo , Ruixin Shao , Yongchao Wang , Qinghua Yang
Carbohydrate-active enzymes (CAZymes) play a crucial role in plant-derived carbon utilization and decomposition and are influenced by the crop rotation system; however, our knowledge of how different agricultural systems impact CAZyme functionality is still limited. We conducted a metagenomic analysis to evaluate the functional genes of CAZymes in a 12-year in situ farmland with three commonly used crop rotation systems: wheat-maize rotation (WM), wheat-cotton rotation (WC), and wheat-soybean rotation (WS). We aimed to study the impact of long-term use of crop rotation, especially crop rotation involving soybean, on soil organic carbon (SOC) content and to gain an in-depth understanding of the CAZyme genes in context of the disparities in SOC. After 12 years, the SOC content was significantly higher in WS than in WC (5.44 %) and WM (17.6 %). Furthermore, the crop rotation system had a significant effect on the soil microbial communities and CAZyme function genes. Detailly, WS increased the phyla abundance of Proteobacteria, Actinobacteria, and Firmicutes and enriched the glycoside hydrolase (GH) and carbohydrate-binding modules (CBM) genes; WC increased the abundance of Acidobacteria and Bacteroidota and enriched the polysaccharide lyase gene; WM increased the abundance of Nitrospirae, Candidatus_Rokubacteria, Chloroflexi and Gemmatimonadetes and enriched the gene abundance of glycosyltransferases and auxiliary activity genes. Additionally, Acidobacteria, Proteobacteria, and Actinobacteria are key phyla involved in soil carbon cycling and collectively contribute >70 % of the total CAZyme functional genes, which highlights their importance. In addition, our results indicated that total nitrogen content played a major role in influencing genes related to CAZymes, especially those belonging to the GH family. Our study demonstrates that WS conferred the advantage of increasing SOC across the three crop rotation systems. CAZyme analysis revealed that WS's could potentially support the increased abundance of Proteobacteria, Actinobacteria and Firmicutes in the soil community, at the same time potentially leading to increased number of GH and CBM genes in the soil, which may bolster the decomposition and transformation of plant-derived carbon, thus promoting an increase in SOC content. The findings of this study offer new insights into the microbial factors contributing to SOC enhancement in rotation systems.
碳水化合物活性酶(CAZymes)在植物源碳利用和分解过程中发挥着至关重要的作用,并受到轮作制度的影响;然而,我们对不同农业制度如何影响 CAZyme 功能的了解仍然有限。我们进行了一项元基因组分析,以评估三种常用轮作制度(小麦-玉米轮作制度(WM)、小麦-棉花轮作制度(WC)和小麦-大豆轮作制度(WS))的 12 年原位农田中 CAZyme 的功能基因。我们的目的是研究长期轮作(尤其是大豆轮作)对土壤有机碳(SOC)含量的影响,并结合 SOC 的差异深入了解 CAZyme 基因。12 年后,WS 的 SOC 含量明显高于 WC(5.44%)和 WM(17.6%)。此外,轮作制度对土壤微生物群落和 CAZyme 功能基因也有显著影响。具体而言,WS 增加了变形菌、放线菌和固着菌的门类丰度,并富集了糖苷水解酶(GH)和碳水化合物结合模块(CBM)基因;WC 增加了酸性杆菌和类杆菌的丰度,并富集了多糖裂解酶基因;WM 增加了硝化细菌属(Nitrospirae)、念珠菌属(Candidatus_Rokubacteria)、绿僵菌属(Chloroflexi)和宝石花菌属(Gemmatimonadetes)的丰度,并丰富了糖基转移酶基因和辅助活性基因的丰度。此外,酸性细菌、蛋白质细菌和放线菌是参与土壤碳循环的关键门类,它们的功能基因总数占 CAZyme 功能基因总数的 70%,这凸显了它们的重要性。此外,我们的研究结果表明,全氮含量在影响 CAZyme 相关基因(尤其是 GH 家族的基因)方面发挥了重要作用。我们的研究表明,在三种轮作系统中,WS 具有增加 SOC 的优势。CAZyme 分析表明,WS 有可能支持土壤群落中变形菌、放线菌和固氮菌数量的增加,同时有可能导致土壤中 GH 和 CBM 基因数量的增加,这可能会促进植物源碳的分解和转化,从而促进 SOC 含量的增加。这项研究的结果为轮作系统中提高 SOC 的微生物因素提供了新的视角。
{"title":"In-depth insights into carbohydrate-active enzyme genes regarding the disparities in soil organic carbon after 12-year rotational cropping system field study","authors":"Hao Wang ,&nbsp;JinPing Chen ,&nbsp;Mingxue Du ,&nbsp;Yihao Ruan ,&nbsp;Jiameng Guo ,&nbsp;Ruixin Shao ,&nbsp;Yongchao Wang ,&nbsp;Qinghua Yang","doi":"10.1016/j.ejsobi.2024.103694","DOIUrl":"10.1016/j.ejsobi.2024.103694","url":null,"abstract":"<div><div>Carbohydrate-active enzymes (CAZymes) play a crucial role in plant-derived carbon utilization and decomposition and are influenced by the crop rotation system; however, our knowledge of how different agricultural systems impact CAZyme functionality is still limited. We conducted a metagenomic analysis to evaluate the functional genes of CAZymes in a 12-year in situ farmland with three commonly used crop rotation systems: wheat-maize rotation (WM), wheat-cotton rotation (WC), and wheat-soybean rotation (WS). We aimed to study the impact of long-term use of crop rotation, especially crop rotation involving soybean, on soil organic carbon (SOC) content and to gain an in-depth understanding of the CAZyme genes in context of the disparities in SOC. After 12 years, the SOC content was significantly higher in WS than in WC (5.44 %) and WM (17.6 %). Furthermore, the crop rotation system had a significant effect on the soil microbial communities and CAZyme function genes. Detailly, WS increased the phyla abundance of <em>Proteobacteria</em>, <em>Actinobacteria</em>, and <em>Firmicutes</em> and enriched the glycoside hydrolase (GH) and carbohydrate-binding modules (CBM) genes; WC increased the abundance of <em>Acidobacteria</em> and <em>Bacteroidota</em> and enriched the polysaccharide lyase gene; WM increased the abundance of <em>Nitrospirae</em>, <em>Candidatus_Rokubacteria</em>, <em>Chloroflexi</em> and <em>Gemmatimonadetes</em> and enriched the gene abundance of glycosyltransferases and auxiliary activity genes. Additionally, <em>Acidobacteria</em>, <em>Proteobacteria</em>, and <em>Actinobacteria</em> are key phyla involved in soil carbon cycling and collectively contribute &gt;70 % of the total CAZyme functional genes, which highlights their importance. In addition, our results indicated that total nitrogen content played a major role in influencing genes related to CAZymes, especially those belonging to the GH family. Our study demonstrates that WS conferred the advantage of increasing SOC across the three crop rotation systems. CAZyme analysis revealed that WS's could potentially support the increased abundance of <em>Proteobacteria</em>, <em>Actinobacteria</em> and <em>Firmicutes</em> in the soil community, at the same time potentially leading to increased number of GH and CBM genes in the soil, which may bolster the decomposition and transformation of plant-derived carbon, thus promoting an increase in SOC content. The findings of this study offer new insights into the microbial factors contributing to SOC enhancement in rotation systems.</div></div>","PeriodicalId":12057,"journal":{"name":"European Journal of Soil Biology","volume":"123 ","pages":"Article 103694"},"PeriodicalIF":3.7,"publicationDate":"2024-11-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142652448","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Dynamics of nitrogen mineralization and nitrogen cycling functional genes in response to soil pore size distribution 氮矿化和氮循环功能基因对土壤孔径分布的动态响应
IF 3.7 2区 农林科学 Q1 ECOLOGY Pub Date : 2024-11-06 DOI: 10.1016/j.ejsobi.2024.103692
Danni Li , Yi Li , Shuihong Yao , Hu Zhou , Shan Huang , Xianlong Peng , Yili Meng
Soil pore distribution influences the permeability of gas, water, and solutes, affecting microbial activities such as nitrogen (N) mineralization. Understanding its impact on N mineralization and the subsequent N transformations is essential for managing compacted paddy soils. This study conducted incubation experiments on two paddy soils from typical Chinese rice regions, Northeastern meadow chernozemic Mollisols, and Southern umbric Ferralsols, under three bulk densities (1.0 g cm−3, 1.2 g cm−3, and 1.4 g cm−3) to investigate the effects of soil porosity on N mineralization and N cycling functional genes. Although the cumulative mineralized N showed no significant difference, with increased macropores (>100 μm) and mesopores (30–100 μm), Ferralsols exhibited a significantly higher net N mineralization rate from day 0 to day 7, while Mollisols extended the mineralization after day 21. Soil dissolved organic carbon (DOC) had a similar temporal trend to the net N mineralization rate, suggesting DOC was the product of mineralization. Soil microbial biomass carbon (MBC) showed an opposite temporal trend to the net N mineralization rate in Mollisols, suggesting microbial biomass as a key N source for mineralization. Soil pores distribution did not affect nitrification under waterlogged conditions, but it affected nirK, nirS and nosZ genes by altering redox potential and substrates availability in the pore micro-environment. Overall, soil pores over 30 μm were the key pore size ranges affecting the intensity and duration of N mineralization, with different effects on DOC, MBC, and N cycling functional genes in Mollisols and Ferralsols. These findings emphasized the role of pore size in regulating N transformation in waterlogged conditions, contributing to the understanding of the N availability in compacted paddy soils from typical geographic rice-growing regions.
土壤孔隙分布会影响气体、水和溶质的渗透性,从而影响氮(N)矿化等微生物活动。了解土壤孔隙分布对氮矿化及后续氮转化的影响对于治理板结水稻土至关重要。本研究对中国典型水稻区的两种水稻土--东北草甸钙质软土和南方钙质软土--在三种容重(1.0 g cm-3、1.2 g cm-3 和 1.4 g cm-3)下进行了培养实验,以研究土壤孔隙度对氮矿化和氮循环功能基因的影响。虽然累积矿化氮没有显著差异,但随着大孔(100 μm)和中孔(30-100 μm)的增加,Ferralsols 在第 0 天到第 7 天的净氮矿化率明显更高,而 Mollisols 在第 21 天后矿化率延长。土壤溶解有机碳(DOC)与净氮矿化率的时间趋势相似,表明 DOC 是矿化的产物。土壤微生物生物量碳(MBC)与 Mollisols 中净氮矿化率的时间趋势相反,表明微生物生物量是矿化的关键氮源。土壤孔隙分布并不影响积水条件下的硝化作用,但会通过改变孔隙微环境中的氧化还原电位和基质可用性而影响 nirK、nirS 和 nosZ 基因。总体而言,30 μm 以上的土壤孔隙是影响氮矿化强度和持续时间的关键孔隙大小范围,对软质土和铁质土中的 DOC、MBC 和氮循环功能基因具有不同的影响。这些发现强调了孔隙大小在调节涝渍条件下氮转化中的作用,有助于了解典型水稻种植区压实水稻土中氮的可用性。
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引用次数: 0
Soil microbial resistance and resilience to drought under organic and conventional farming 有机耕作和传统耕作下土壤微生物的抗旱性和复原力
IF 3.7 2区 农林科学 Q1 ECOLOGY Pub Date : 2024-11-05 DOI: 10.1016/j.ejsobi.2024.103690
Elena Kost , Dominika Kundel , Rafaela Feola Conz , Paul Mäder , Hans-Martin Krause , Johan Six , Jochen Mayer , Martin Hartmann
The impacts of climate change, such as drought, can affect soil microbial communities. These communities are crucial for soil functioning and crop production. Organic and conventional cropping systems can promote distinct soil microbiomes and soil organic carbon contents, which might generate different capacities to mitigate drought effects on these cropping systems. A field-scale drought simulation was performed in long-term organically and conventionally managed cropping systems differing in fertilization and pesticide application. The soil microbiome was assessed during and after drought in bulk soil, rhizosphere, and roots of wheat. We found that drought reduced soil respiration and altered microbial community structures, affecting fungi in the bulk soil and rhizosphere more strongly than prokaryotes. Microbial communities associated with crops (i.e. rhizosphere and root) were more strongly influenced by drought compared to bulk soil communities. Drought legacy effects were observed in the bulk soil after harvesting and rewetting. The extent of the structural shifts in the soil microbiome in response to severe drought did not differ significantly between the organic and conventional cropping systems but each cropping system maintained a unique microbiome under drought. All cropping systems showed relative increases in potential plant growth-promoting genera under drought but some genera such as Streptomyces, Rhizophagus, Actinomadura, and Aneurinibacillus showed system-specific drought responses. This agricultural field study indicated that fungal communities might be less resistant to drought than prokaryotic communities in cropping systems and these effects get more pronounced in closer association with plants. Organic fertilization and the associated increase in soil organic carbon, or the reduction in pesticide application might not have the proposed ability to buffer severe drought stress on soil microbial taxonomic diversity. Yet, it remains to be elucidated whether the ability to maintain system-specific soil microbiomes also during drought translates into different functional capabilities to cope with the stress.
干旱等气候变化的影响会影响土壤微生物群落。这些群落对土壤功能和作物生产至关重要。有机种植系统和常规种植系统可以促进不同的土壤微生物群落和土壤有机碳含量,这可能会对这些种植系统产生不同的缓解干旱影响的能力。在施肥和施用农药不同的长期有机和常规管理种植系统中进行了田间尺度的干旱模拟。在干旱期间和之后,对小麦的大块土壤、根瘤层和根部的土壤微生物组进行了评估。我们发现,干旱降低了土壤呼吸作用,改变了微生物群落结构,对大块土壤和根圈中真菌的影响比对原核生物的影响更大。与块状土壤群落相比,与作物相关的微生物群落(即根瘤菌圈和根部)受干旱的影响更大。收获和复湿后,在大体积土壤中观察到了干旱遗留效应。土壤微生物群对严重干旱的结构变化程度在有机种植系统和常规种植系统之间没有显著差异,但每种种植系统在干旱条件下都保持了独特的微生物群。在干旱条件下,所有种植系统中潜在的促进植物生长的菌属都相对增加,但一些菌属,如链霉菌属、根霉菌属、放线菌属和Aneurinibacillus菌属,则表现出系统特异性的干旱反应。这项农田研究表明,在种植系统中,真菌群落对干旱的抵抗力可能不如原核生物群落,而在与植物关系更密切的情况下,这些影响会更加明显。有机肥和相关土壤有机碳的增加,或杀虫剂施用量的减少,可能无法缓冲严重干旱对土壤微生物分类多样性的压力。然而,在干旱期间保持系统特异性土壤微生物组的能力是否会转化为应对压力的不同功能能力,还有待进一步阐明。
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引用次数: 0
Plantation conversion of Eucalyptus promotes soil microbial necromass C accumulation 桉树的种植转化促进了土壤微生物坏质碳的积累
IF 3.7 2区 农林科学 Q1 ECOLOGY Pub Date : 2024-11-03 DOI: 10.1016/j.ejsobi.2024.103691
Min Wang , Chang Liao , Weili Lai , Songyi Huang , Shihong Xiao , Caiqiong Deng , Xianhua Gan , Qing Ma , Mengyun Liu
<div><h3>Context</h3><div>Stand conversion in subtropical regions has altered soil physicochemical properties and microbial communities, leading to changes in microbially mediated processes, such as microbial necromass C (MNC) formation and accumulation. However, previous studies on the effects of stand conversion on MNC are lacking, leading to gaps in our understanding regarding the influence of long-term stand conversion on MNC accumulation in different soil layers and the relative importance of soil properties for regulating MNC.</div></div><div><h3>Aims</h3><div>In this study, we used field surveys and soil analysis to assess the effects of converting a <em>Eucalyptus</em> forest into other planted forest (broadleaf mixed forest [BM] and <em>Acacia mangium</em> × <em>Acacia auriculiformis</em> forest [AM]) on soil properties, enzyme activity, microbial community composition, and MNC after conversion 20 years in Guangdong, South China.</div></div><div><h3>Results</h3><div>We found that the content of soil organic C (SOC) in the surface soil (0–10 cm after litter removal) increased by 64.9 % when <em>Eucalyptus</em> was converted to AM, whereas there was no significant difference in the subsurface soil (10–20 cm). β-1,4-glucosidase (BG) and β-1,4-N-acetaminophen glucosidase (NAG) activity increased significantly, while leucine aminopeptidase (LA) activity decreased significantly in the surface soil. In the subsurface soil, BG activity did not change significantly; nonetheless, acid phosphomonoesterase (AP) activity decreased. The fungal, bacterial, and gram-negative bacterial biomass did not significantly differ among the different forests in the surface soil, but the fungal, bacterial, gram-positive, and gram-negative bacterial biomass decreased significantly in the subsurface soil. The ratio of fungi to bacteria was highest in the BM, whereas the ratio of gram-positive to gram-negative bacteria was highest in the AM. Soil fungal and microbial necromass C and the ratio of fungal to bacterial necromass C increased significantly in the surface soil when <em>Eucalyptus</em> was converted to AM. The contribution of MNC and fungal necromass C to SOC content significantly increased by 22.20 % and 26.23 %, respectively, when <em>Eucalyptus</em> was converted to AM. The main controlling factors of MNC accumulation in the surface soil were pH and total N, whereas soil enzyme activity (BG related to C-acquisition) was the dominant determinant of MNC accumulation in the subsurface soil.</div></div><div><h3>Conclusion</h3><div>Our study provides evidence that converting <em>Eucalyptus</em> to AM may promote MNC accumulation in the surface soil by changing soil pH and TN content to affect soil enzyme activity and microbial community structure, and ultimately changed MNC accumulation. Therefore, developing effective forest management practices, such as reasonable stand conversion may help to enhance forest SOC accumulation by increasing MNC accumulation.</d
背景亚热带地区的林分转换改变了土壤理化性质和微生物群落,导致微生物介导的过程发生变化,如微生物坏死物质 C(MNC)的形成和积累。然而,以前缺乏有关林分转换对 MNC 影响的研究,导致我们对长期林分转换对不同土层中 MNC 积累的影响以及土壤特性对调节 MNC 的相对重要性的认识存在差距。目的 在本研究中,我们利用实地调查和土壤分析评估了在中国南方广东将桉树林改造成其他人工林(阔叶混交林 [BM] 和芒果相思树 × 金合欢林 [AM])20 年后对土壤性质、酶活性、微生物群落组成和 MNC 的影响。结果我们发现,当桉树转化为 AM 后,表层土壤(去除枯落物后 0-10 厘米)的土壤有机碳(SOC)含量增加了 64.9%,而表层下土壤(10-20 厘米)则无显著差异。表层土壤中,β-1,4-葡萄糖苷酶(BG)和β-1,4-N-乙酰氨基酚葡萄糖苷酶(NAG)活性显著增加,而亮氨酸氨肽酶(LA)活性显著降低。在地下土壤中,BG 活性没有明显变化;但酸性磷单酯酶(AP)活性有所下降。在表层土壤中,不同森林的真菌、细菌和革兰氏阴性菌生物量没有显著差异,但在表层下土壤中,真菌、细菌、革兰氏阳性菌和革兰氏阴性菌生物量显著下降。真菌与细菌的比例在 BM 中最高,而革兰氏阳性菌与革兰氏阴性菌的比例在 AM 中最高。当桉树转化为 AM 时,表层土壤中的土壤真菌和微生物坏死物质 C 以及真菌与细菌坏死物质 C 之比显著增加。桉树转化为 AM 后,MNC 和真菌坏死物质 C 对 SOC 含量的贡献率分别大幅增加了 22.20 % 和 26.23 %。表层土壤中 MNC 积累的主要控制因素是 pH 值和全氮,而土壤酶活性(与 C 获取有关的 BG)是表层下土壤中 MNC 积累的主要决定因素。因此,制定有效的森林管理措施,如合理的林分转换,可能有助于通过增加 MNC 积累来提高森林 SOC 积累。
{"title":"Plantation conversion of Eucalyptus promotes soil microbial necromass C accumulation","authors":"Min Wang ,&nbsp;Chang Liao ,&nbsp;Weili Lai ,&nbsp;Songyi Huang ,&nbsp;Shihong Xiao ,&nbsp;Caiqiong Deng ,&nbsp;Xianhua Gan ,&nbsp;Qing Ma ,&nbsp;Mengyun Liu","doi":"10.1016/j.ejsobi.2024.103691","DOIUrl":"10.1016/j.ejsobi.2024.103691","url":null,"abstract":"&lt;div&gt;&lt;h3&gt;Context&lt;/h3&gt;&lt;div&gt;Stand conversion in subtropical regions has altered soil physicochemical properties and microbial communities, leading to changes in microbially mediated processes, such as microbial necromass C (MNC) formation and accumulation. However, previous studies on the effects of stand conversion on MNC are lacking, leading to gaps in our understanding regarding the influence of long-term stand conversion on MNC accumulation in different soil layers and the relative importance of soil properties for regulating MNC.&lt;/div&gt;&lt;/div&gt;&lt;div&gt;&lt;h3&gt;Aims&lt;/h3&gt;&lt;div&gt;In this study, we used field surveys and soil analysis to assess the effects of converting a &lt;em&gt;Eucalyptus&lt;/em&gt; forest into other planted forest (broadleaf mixed forest [BM] and &lt;em&gt;Acacia mangium&lt;/em&gt; × &lt;em&gt;Acacia auriculiformis&lt;/em&gt; forest [AM]) on soil properties, enzyme activity, microbial community composition, and MNC after conversion 20 years in Guangdong, South China.&lt;/div&gt;&lt;/div&gt;&lt;div&gt;&lt;h3&gt;Results&lt;/h3&gt;&lt;div&gt;We found that the content of soil organic C (SOC) in the surface soil (0–10 cm after litter removal) increased by 64.9 % when &lt;em&gt;Eucalyptus&lt;/em&gt; was converted to AM, whereas there was no significant difference in the subsurface soil (10–20 cm). β-1,4-glucosidase (BG) and β-1,4-N-acetaminophen glucosidase (NAG) activity increased significantly, while leucine aminopeptidase (LA) activity decreased significantly in the surface soil. In the subsurface soil, BG activity did not change significantly; nonetheless, acid phosphomonoesterase (AP) activity decreased. The fungal, bacterial, and gram-negative bacterial biomass did not significantly differ among the different forests in the surface soil, but the fungal, bacterial, gram-positive, and gram-negative bacterial biomass decreased significantly in the subsurface soil. The ratio of fungi to bacteria was highest in the BM, whereas the ratio of gram-positive to gram-negative bacteria was highest in the AM. Soil fungal and microbial necromass C and the ratio of fungal to bacterial necromass C increased significantly in the surface soil when &lt;em&gt;Eucalyptus&lt;/em&gt; was converted to AM. The contribution of MNC and fungal necromass C to SOC content significantly increased by 22.20 % and 26.23 %, respectively, when &lt;em&gt;Eucalyptus&lt;/em&gt; was converted to AM. The main controlling factors of MNC accumulation in the surface soil were pH and total N, whereas soil enzyme activity (BG related to C-acquisition) was the dominant determinant of MNC accumulation in the subsurface soil.&lt;/div&gt;&lt;/div&gt;&lt;div&gt;&lt;h3&gt;Conclusion&lt;/h3&gt;&lt;div&gt;Our study provides evidence that converting &lt;em&gt;Eucalyptus&lt;/em&gt; to AM may promote MNC accumulation in the surface soil by changing soil pH and TN content to affect soil enzyme activity and microbial community structure, and ultimately changed MNC accumulation. Therefore, developing effective forest management practices, such as reasonable stand conversion may help to enhance forest SOC accumulation by increasing MNC accumulation.&lt;/d","PeriodicalId":12057,"journal":{"name":"European Journal of Soil Biology","volume":"123 ","pages":"Article 103691"},"PeriodicalIF":3.7,"publicationDate":"2024-11-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142572269","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Longitudinal distributions of CO2-fixing bacteria in forest soils and their potential associations with soil multifunctionality 森林土壤中固氮细菌的纵向分布及其与土壤多功能性的潜在联系
IF 3.7 2区 农林科学 Q1 ECOLOGY Pub Date : 2024-10-24 DOI: 10.1016/j.ejsobi.2024.103689
Ying Wang , Yimei Huang , Na Li , Qian Huang , Baorong Wang , Shaoshan An
Autotrophic microorganisms can fix carbon dioxide (CO2) into organic carbon (C), potentially offering a natural mechanism to mitigate global climate change. Forest soils, recognized as vast and critical C repositories with significant microbial CO2 fixation rates, remain understudied, particularly regarding the spatial variations of autotrophic bacteria and their relationship to soil functions in arid regions. In this study, we systematically investigated soil multifunctionality, along with the spatial distribution of autotrophic bacterial communities identified by the RubisCO cbbL and cbbM genes, and the driving factors across a longitudinal gradient in the Loess Plateau forest soils. The investigation spanned an ∼850 km west-east transect with precipitation below 600 mm. The alpha diversity of cbbL-containing bacteria, as measured by the Chao1 index, was correlated with climatic variables such as precipitation and elevation instead of local soil characteristics. In contrast, the alpha diversity of cbbM-containing bacteria was associated with soil properties. The community composition of autotrophic bacteria, based on cbbL and cbbM genes, showed greater similarity in soils from the eastern Loess Plateau and was distinct from those in the western region. The cbbL- and cbbM-containing generalist taxa were subject to differential selection and promotion between the eastern and western regions. Temperature, soil pH and spatial variables were key drivers influencing the community composition of cbbL- and cbbM-containing bacteria. The diversity and communities of soil autotrophic bacteria significantly affected soil multifunctionality. The study demonstrates that soil autotrophic bacteria in forest soils are intricately connected to climatic conditions, soil pH and spatial factors, significantly impacting soil multifunctionality. These insights provide evidence that can be instrumental in predicting and potentially enhancing the functional capacity of forest ecosystems in the Loess Plateau.
自养微生物可以将二氧化碳(CO2)固定为有机碳(C),可能为减缓全球气候变化提供一种自然机制。森林土壤被认为是巨大而重要的碳储存库,具有显著的微生物二氧化碳固定率,但对其研究仍然不足,特别是关于自养细菌的空间变化及其与干旱地区土壤功能的关系。在本研究中,我们系统地研究了黄土高原森林土壤的多功能性、RubisCO cbbL 和 cbbM 基因鉴定的自养细菌群落的空间分布及其纵向梯度上的驱动因素。调查横跨降水量低于 600 毫米的西-东横断面达 850 公里。用 Chao1 指数测量的含 cbbL 细菌的α多样性与降水量和海拔等气候变量相关,而与当地土壤特性无关。相比之下,含 cbbM 细菌的α多样性与土壤特性相关。基于 cbbL 和 cbbM 基因的自养细菌群落组成在黄土高原东部的土壤中表现出更大的相似性,而与西部地区的土壤不同。含 cbbL 和 cbbM 的普通类群在东部和西部地区受到不同的选择和促进。温度、土壤pH值和空间变量是影响含cbbL和cbbM细菌群落组成的主要因素。土壤自养细菌的多样性和群落对土壤多功能性有显著影响。该研究表明,森林土壤中的土壤自养细菌与气候条件、土壤酸碱度和空间因素密切相关,对土壤多功能性有重要影响。这些见解为预测和潜在地提高黄土高原森林生态系统的功能能力提供了证据。
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引用次数: 0
Continuous measurement of red wood ant (Formica rufa) outdoor behaviour using passive acoustic monitoring 利用被动声学监测连续测量红木蚁(Formica rufa)的户外行为
IF 3.7 2区 农林科学 Q1 ECOLOGY Pub Date : 2024-10-22 DOI: 10.1016/j.ejsobi.2024.103687
L. Vang Sørensen , S. Rodríguez-Martínez , M. Rollo , J. Klaminder
Ants serve as ecosystem engineers that maintain important ecological processes within forests. Given their ecological importance, it is a clear scientific shortcoming that we lack non-invasive methods to survey their behaviour inside common opaque habitats such as mounds, litter, and soil. In this study, we assess if acoustic signals from red wood ant (Formica rufa) mounds are useful to infer temporal changes in ant activity within forested ecosystems. We found that acoustic indices used previously as a proxy for soil fauna in soil ecological studies (Acoustic Complexity Index, Bioacoustic Index) can indeed separate sounds generated by the ant's daily routines (biophony) from other forest sounds. Yet, we also show that these indices are problematic proxies for soil diversity as they increase not only due to an increased number of species but also due to an increased number of the same species. Acoustic measures that incorporated the strength of acoustic signals, Average Power Density (APD) and Peak Power Density (PPD) also increased with increasing ant abundance and constituted the conceptually best proxy for ant activity. For example, the PPD could i) track diurnal changes in Formica rufa activity with a high temporal resolution (minutes) and ii) detect altered behavioural responses to temperature changes. We conclude that microphones detecting biophony can provide high-resolution information about in situ ant behaviours in forested ecosystems. Thus, passive acoustics monitoring offers a promising avenue as a non-invasive monitoring tool for soil macrofauna studies.
蚂蚁是维持森林重要生态过程的生态系统工程师。鉴于蚂蚁在生态方面的重要性,我们缺乏非侵入式方法来调查蚂蚁在土丘、垃圾和土壤等常见不透明栖息地内的行为,这是一个明显的科学缺陷。在这项研究中,我们评估了来自红木蚁(Formica rufa)蚁丘的声学信号是否有助于推断森林生态系统中蚂蚁活动的时间变化。我们发现,以前在土壤生态研究中用作土壤动物群替代物的声学指数(声学复杂性指数、生物声学指数)确实可以将蚂蚁日常活动产生的声音(生物声音)与其他森林声音区分开来。然而,我们也发现,这些指数是有问题的土壤多样性代用指标,因为它们的增加不仅是由于物种数量的增加,也是由于相同物种数量的增加。声学指标包括声信号强度、平均功率密度(Average Power Density,APD)和峰值功率密度(Peak Power Density,PPD),它们也随着蚂蚁数量的增加而增加,在概念上是蚂蚁活动的最佳代表。例如,PPD 可以 i) 以较高的时间分辨率(分钟)跟踪 Formica rufa 活动的昼夜变化;ii) 检测对温度变化的行为反应变化。我们的结论是,探测生物声音的麦克风可以提供有关森林生态系统中蚂蚁现场行为的高分辨率信息。因此,被动声学监测作为一种非侵入式监测工具,为土壤大型底栖动物研究提供了一条前景广阔的途径。
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引用次数: 0
Pinus radiata seedlings rhizobiome shifts in response to foliar and root phosphite application 辐射松幼苗根生物群对叶面和根部施用亚磷酸的响应变化
IF 3.7 2区 农林科学 Q1 ECOLOGY Pub Date : 2024-10-16 DOI: 10.1016/j.ejsobi.2024.103688
Frederico Leitão , Glória Pinto , Isabel Henriques
Soil health is an emerging concern in agriculture and is dependent on the microbial communities in the rhizosphere (rhizobiome). Phosphite-based products are used as bio-stimulants and/or fungicides. However, there is a lack of studies evaluating the impact of these products in nurseries, especially at the level of the rhizobiome. This work aims to assess the impact of phosphite (Phi) application on the rhizobiome of Pinus radiata seedlings. Two application modes (foliar and irrigation) were compared in an experimental setup with control treatments. Gas exchange parameters were evaluated to assess plant physiological performance. Bacterial rhizobiome analysis was performed using next generation sequencing targeting the 16S rRNA gene. Results showed that Phi application did not significantly affect plant photosynthetic performance. However, Phi irrigation led to a significant decrease in rhizobiome richness and diversity compared to control. Beta diversity analysis confirmed distinct microbial communities in the irrigated group. At the genus level, several acidophilic taxa, including Burkholderia and Aciditerrimonas, were significantly enriched in phosphite-irrigated samples, while others like Mucilaginibacter were reduced. The study reveals that Phi application, especially through irrigation, alters the structure of the rhizobiome in pine seedlings, leading to a decrease in richness and bacterial diversity. These findings highlight the importance of understanding the effects of commercial products, such as phosphite. This understanding is crucial to ensure sustainable plant growth and maintain soil health.
土壤健康是农业领域新出现的一个问题,它取决于根瘤菌圈(根瘤生物群)中的微生物群落。亚磷酸盐类产品被用作生物刺激剂和/或杀菌剂。然而,目前还缺乏对这些产品在苗圃中的影响进行评估的研究,尤其是在根瘤生物群层面。这项研究旨在评估施用亚磷酸(Phi)对黑松幼苗根生物体的影响。在实验设置中比较了两种施用模式(叶面施肥和灌溉施肥)和对照处理。通过评估气体交换参数来评估植物的生理表现。利用针对 16S rRNA 基因的新一代测序技术对细菌根生物群进行了分析。结果表明,施用 Phi 对植物的光合作用没有明显影响。然而,与对照组相比,Phi 灌溉导致根瘤生物群的丰富度和多样性显著下降。Beta 多样性分析证实,灌溉组的微生物群落与对照组截然不同。在属的层面上,几个嗜酸类群,包括伯克霍尔德氏菌(Burkholderia)和Aciditerrimonas,在亚磷酸盐灌溉的样本中明显富集,而其他类群,如粘菌(Mucilaginibacter)则有所减少。该研究揭示了磷的应用,尤其是通过灌溉,改变了松树幼苗根瘤生物群的结构,导致丰富度和细菌多样性的降低。这些发现强调了了解亚磷酸等商业产品影响的重要性。这种了解对于确保植物可持续生长和维护土壤健康至关重要。
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European Journal of Soil Biology
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