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Faba bean-wheat intercropping controls the occurrence of faba bean Fusarium wilt by improving the microecological environment of rhizosphere soil 蚕豆-小麦间作通过改善根瘤土壤的微生态环境控制蚕豆镰刀菌枯萎病的发生
IF 3.7 2区 农林科学 Q1 ECOLOGY Pub Date : 2024-12-01 Epub Date: 2024-10-13 DOI: 10.1016/j.ejsobi.2024.103685
Yiran Zheng , Jing Zhang , Dongsheng Wang, Siyin Yang, Zixuan Cen, Yan Dong

Background

Fusarium wilt is a severe soil-borne disease that affects faba bean production. Faba bean-wheat intercropping is often used to control the occurrence of Fusarium wilt in faba bean.

Aims

To evaluate the effects of faba bean-wheat intercropping on the occurrence of faba bean Fusarium wilt and soil microecology.

Methods

We established two planting patterns, faba bean monocropping (M) and faba bean-wheat intercropping (I), to investigate Fusarium wilt occurrence and plant dry weight and assess changes in soil enzyme activities, microbial diversity, and community composition during different stages of disease onset.

Results

Intercropping effectively controlled faba bean Fusarium wilt at the three disease stages and increased the dry weight of faba bean plants. Intercropping promoted the activities of catalase (CAT), urease, sucrase, and acid phosphatase in the rhizosphere soil of faba bean at three disease stages. Bacterial and fungal diversity decreased with disease progression, and intercropping mitigated this trend. Compared with monocropping, intercropping increased the abundance of beneficial bacteria such as Proteobacteria, Actinobacteriota, Gemmatimonadota, Gemmatimonas, Conexibacter, and Sphingomonas, while reducing the abundance of pathogenic fungi such as Alternaria, Cladosporium, and Fusarium. Intercropping also increased the abundance of arbuscular mycorrhiza, soil saprophytes, and undefined saprophytes while decreasing the abundance of plant pathogens.

Conclusion

Faba bean-wheat intercropping enhanced soil enzyme activities, effective nutrient content, and alpha diversity indices of bacteria and fungi in the rhizosphere soil of faba bean, while promoting the abundance of beneficial bacteria, arbuscular mycorrhizal fungi, as well as both soil and undefined humus. Simultaneously, intercropping reduced the abundance of plant pathogens, facilitated nutrient cycling in the soil, provided sufficient nutrients for crop uptake, and mitigated the toxic effects of hydrogen peroxide on cells. Ultimately, this resulted in a reduced occurrence of Fusarium wilt.
背景镰刀菌枯萎病是一种严重影响蚕豆生产的土传病害。目的 评估蚕豆-小麦间作对蚕豆镰刀菌枯萎病发生和土壤微生态的影响。方法我们建立了两种种植模式,即蚕豆单作(M)和蚕豆-小麦间作(I),调查镰刀菌枯萎病的发生情况和植株干重,并评估发病不同阶段土壤酶活性、微生物多样性和群落组成的变化。在三个发病阶段,间作能提高蚕豆根瘤土壤中过氧化氢酶(CAT)、脲酶、蔗糖酶和酸性磷酸酶的活性。细菌和真菌的多样性随着病害的发展而减少,而间作减轻了这一趋势。与单作相比,间作增加了有益细菌的数量,如蛋白细菌、放线菌、革马提那菌、革马提那菌、锥菌和鞘氨单胞菌,同时降低了致病真菌的数量,如交替孢霉、多孢霉和镰刀菌。结论蚕豆-小麦间作提高了蚕豆根圈土壤中的土壤酶活性、有效养分含量以及细菌和真菌的α多样性指数,同时促进了有益菌、丛枝菌根真菌以及土壤和未确定腐殖质的丰度。同时,间作减少了植物病原体的数量,促进了土壤中的养分循环,为作物吸收提供了充足的养分,并减轻了过氧化氢对细胞的毒性作用。最终减少了镰刀菌枯萎病的发生。
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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 : 2024-12-01 Epub 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
Bacteria contribute more than fungi to SOC decomposition in a paddy field under long-term free-air CO2 enrichment 在长期自由空气二氧化碳富集条件下,细菌比真菌对稻田中 SOC 分解的贡献更大
IF 3.7 2区 农林科学 Q1 ECOLOGY Pub Date : 2024-12-01 Epub Date: 2024-10-02 DOI: 10.1016/j.ejsobi.2024.103682
Meiling Xu , Feifan Zhang , Ling Zhang , Hongze Zhang , Caixian Tang , Xiaozhi Wang , Jing Ma , Qiao Xu
Microbial responses to future climate change are important in determining soil organic carbon cycling and evaluating carbon-climate feedback. Paddy soils from a 15-year free-air CO2 enrichment (FACE) experiment were incubated and analyzed to reveal the responses of soil microbial activity, community diversity and composition to the soil depth and elevated CO2. Network topology analysis was conducted to determine microbial complexity and stability, and Mantel tests were used to analyze the correlation between bacteria and fungi and soil respiration. Elevated CO2 stimulated cumulative soil respiration (topsoil 6.2 %, subsoil 21.8 %), which was positively correlated with bacterial diversity. The elevated CO2 effects on the microbial community were greater in the topsoil than in the subsoil, namely, bacterial diversity was increased by 2.1 % in the topsoil (0–15 cm). Elevated CO2 also increased the abundance of Nitrospirota in the top- but not in the subsoil. Fungal diversity and phyla were not affected by elevated CO2, but fungal diversity was significantly correlated with the contents of soil DOC, total dissolved N, and total P in the subsoil. Compared to the subsoil, bacterial richness was higher in topsoil, and more Ascomycota was found but fewer Mortierellomycota; the microbial network had a greater number of nodes and edges. These results suggested that 1) depth was a major factor affecting soil properties that determine microbial community and function; 2) bacterial taxa were more sensitive to elevated CO2 than fungal taxa; 3) elevated CO2 increased SOC decomposition directly via enhanced soil C availability and altered bacterial diversity and microbial complexity and stability.
微生物对未来气候变化的反应对于确定土壤有机碳循环和评估碳-气候反馈非常重要。对一项为期 15 年的自由空气二氧化碳富集(FACE)实验中的稻田土壤进行了培养和分析,以揭示土壤微生物活动、群落多样性和组成对土壤深度和高浓度二氧化碳的响应。通过网络拓扑分析确定了微生物的复杂性和稳定性,并使用曼特尔检验分析了细菌和真菌与土壤呼吸作用之间的相关性。高浓度二氧化碳刺激了累积土壤呼吸作用(表土 6.2%,底土 21.8%),这与细菌多样性呈正相关。二氧化碳升高对表层土壤微生物群落的影响大于底层土壤,即表层土壤(0-15 厘米)的细菌多样性增加了 2.1%。二氧化碳浓度升高也增加了表层土壤中硝化螺菌的数量,但没有增加底层土壤中硝化螺菌的数量。真菌多样性和真菌门类不受二氧化碳升高的影响,但真菌多样性与底土中土壤 DOC、总溶解氮和总磷的含量显著相关。与底土相比,表层土壤的细菌丰富度更高,发现的子囊菌群更多,而毛霉菌群更少;微生物网络的节点和边缘数量更多。这些结果表明:1)深度是影响土壤特性的主要因素,而土壤特性决定了微生物群落和功能;2)细菌类群比真菌类群对升高的 CO2 更敏感;3)升高的 CO2 通过提高土壤 C 的可用性直接增加了 SOC 的分解,并改变了细菌多样性和微生物的复杂性和稳定性。
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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 : 2024-12-01 Epub 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。
{"title":"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","authors":"Yuxuan Zhang ,&nbsp;Mengya Lu ,&nbsp;Zhiquan Wang ,&nbsp;Kun Zhang ,&nbsp;Bin Zhang ,&nbsp;Reziwanguli Naimaiti ,&nbsp;Shangyuan Wei ,&nbsp;Xueli Ding","doi":"10.1016/j.ejsobi.2024.103695","DOIUrl":"10.1016/j.ejsobi.2024.103695","url":null,"abstract":"<div><div>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 <sup>13</sup>C-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<sup>−1</sup> soil) with no-nutrient (S + Nu<sub>0</sub>), low nutrient (S + Nu<sub>low</sub>, 42 mg N kg<sup>−1</sup>, 10 mg P kg<sup>−1</sup>), and high nutrient (S + Nu<sub>high</sub>, 126 mg N kg<sup>−1</sup>, 30 mg P kg<sup>−1</sup>) supply increased total CO<sub>2</sub> 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 + Nu<sub>low</sub> and tripled in the S + Nu<sub>high</sub> compared to the S + Nu<sub>0</sub>. 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 + Nu<sub>low</sub> S + Nu<sub>high</sub>. A greater proportion of straw-derived C incorporation into SOC (indicated by higher levels <sup>13</sup>C-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.</div></div>","PeriodicalId":12057,"journal":{"name":"European Journal of Soil Biology","volume":"123 ","pages":"Article 103695"},"PeriodicalIF":3.7,"publicationDate":"2024-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142652449","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 : 2024-12-01 Epub 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
Planting Chinese milk vetch with phosphate-solubilizing bacteria inoculation enhances phosphorus turnover by altering the structure of the phoD-harboring bacteria community 在种植中国牛奶面包时接种磷酸盐溶解菌,通过改变噬磷菌群落的结构提高磷周转率
IF 3.7 2区 农林科学 Q1 ECOLOGY Pub Date : 2024-12-01 Epub Date: 2024-09-16 DOI: 10.1016/j.ejsobi.2024.103678
Danna Chang , Yarong Song , Hai Liang , Rui Liu , Cheng Cai , Shuailei Lv , Yulin Liao , Jun Nie , Tingyu Duan , Weidong Cao

This study aimed to reveal how planting Chinese milk vetch (CMV) as green manure in combination with phosphate-solubilizing bacteria-based biofertilizer can enhance phosphorus (P) utilization in CMV-rice crop rotations. The pot experiment included two factors: the presence of Acinetobacter calcoaceticus (ACC) inoculation, and the variety of CMV (six varieties), resulting in 12 treatments. The experiment lasted for 190 d and soil and plants were analyzed thereafter. ACC inoculation increased the average shoot dry weight by 37.1 % and P uptake by 73.9 % of CMV, and increased the average content of soil labile P by 9.2 %; decreased the average content of moderately labile P by 6.9 % and stable P by 5.4 %, compared to control. ACC inoculation increased the average concentrations of acetic acid, gluconic acid, oxalic acid, citric acid, acid phosphatase and alkaline phosphatase. Structural equation model showed that organic acid and phosphatase correlated with soil labile and moderately labile P pools. The average abundance and diversity of the alkaline phosphatase gene (phoD) and the proportion of dominant species in the mineralization of organic P (Streptomycetaceae) increased under ACC inoculation. Thus, planting CMV with ACC inoculation increased the average concentrations of organic acid and alkaline phosphatase, activating insoluble inorganic P and organic P. However, their combination enhanced the average abundance and altered the structure of the phoD-harboring bacteria community, which in turn promoted organic P mineralization. Planting Chinese milk vetch with Acinetobacter calcoaceticus inoculation can effectively utilize P in paddy soil, which can enhance P availability for subsequent rice crops.

本研究旨在揭示将中国乳牛(CMV)作为绿肥种植并结合磷溶解菌生物肥料如何提高中国乳牛-水稻轮作中磷(P)的利用率。盆栽试验包括两个因素:是否接种钙化醋酸杆菌(ACC)和 CMV 的品种(6 个品种),共 12 个处理。实验持续了 190 天,之后对土壤和植株进行了分析。与对照组相比,接种 ACC 使 CMV 的平均芽干重增加了 37.1%,钾吸收量增加了 73.9%,土壤中可溶性钾的平均含量增加了 9.2%;中度可溶性钾的平均含量减少了 6.9%,稳定钾的平均含量减少了 5.4%。接种 ACC 增加了乙酸、葡萄糖酸、草酸、柠檬酸、酸性磷酸酶和碱性磷酸酶的平均浓度。结构方程模型显示,有机酸和磷酸酶与土壤中的可溶性和中度可溶性磷库相关。在 ACC 接种条件下,碱性磷酸酶基因(phoD)的平均丰度和多样性以及有机钾矿化优势物种(链霉科)的比例都有所增加。因此,在接种 ACC 的同时种植 CMV 会增加有机酸和碱性磷酸酶的平均浓度,激活不溶性无机磷和有机磷,但二者的结合提高了 phoD 依赖细菌群落的平均丰度并改变了其结构,从而促进了有机磷的矿化。在种植中国牛奶草的同时接种卡氏不动杆菌,可有效利用稻田土壤中的钾,从而提高后续水稻作物对钾的利用率。
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引用次数: 0
Fire alters soil bacterial and fungal communities and intensifies seasonal variation in subtropical forest ecosystem 火灾改变了土壤细菌和真菌群落,加剧了亚热带森林生态系统的季节性变化
IF 3.7 2区 农林科学 Q1 ECOLOGY Pub Date : 2024-12-01 Epub Date: 2024-09-18 DOI: 10.1016/j.ejsobi.2024.103677
Ziyue Shi , Yaru Chen , Aogui Li , Mengjun Hu , Weixing Liu

Soil microbes stand as pivotal constituents and perform important ecological functions in forest ecosystems due to their extensive diversity. The increasing frequency of forest fire, coupled with the accelerating global warming, has resulted in changes in environmental conditions and forest structure, consequently influencing soil microbial communities. Despite this, there is a lack of comprehensive understanding regarding the impacts of fire on soil bacterial and fungal communities. Based on a fire experimental study in subtropical forest ecosystem, we investigated the alterations in soil properties and microbial community across two seasons. The results showed that soil bacterial richness remained unchanged by fire in both seasons. In contrast, soil fungal richness decreased in spring but increased in autumn at burnt sites, indicating the amplified seasonal variation induced by fire. In addition, fire had a significant impact on soil microbial community composition. Specifically, it elevated the relative abundance of Actinobacteriota but reduced that of Acidobacteriota and Verrucomicrobiota, which was related to increased temperature, pH, and decreased nitrogen resulting from fire. The relative abundance of Ascomycota increased following fire, whereas the relative abundance of Basidiomycota decreased. These shifts in soil fungal community were mainly related to lower soil carbon:nitrogen ratio. Furthermore, bacterial community was more responsive to environmental changes than fungal community. Overall, our study demonstrates soil microbial diversity and community structure in response to forest fire and the driving factors, advancing our comprehension of soil microbial dynamics in forest ecosystems under environmental perturbations.

在森林生态系统中,土壤微生物以其广泛的多样性成为重要的组成成分,并发挥着重要的生态功能。森林火灾日益频繁,加上全球变暖加速,导致环境条件和森林结构发生变化,进而影响土壤微生物群落。尽管如此,人们对火灾对土壤细菌和真菌群落的影响还缺乏全面的了解。基于亚热带森林生态系统的火灾实验研究,我们调查了两个季节中土壤性质和微生物群落的变化。结果表明,土壤细菌丰富度在两个季节都没有受到火灾的影响。相比之下,火灾现场土壤真菌丰富度在春季下降,但在秋季上升,这表明火灾引起的季节性变化扩大了。此外,火灾对土壤微生物群落组成也有显著影响。具体而言,火灾提高了放线菌群的相对丰度,但降低了酸性杆菌群和蛭石微生物群的相对丰度,这与火灾导致的温度升高、pH 值升高和氮素减少有关。火灾后,子囊菌群的相对丰度增加,而担子菌群的相对丰度下降。土壤真菌群落的这些变化主要与土壤碳氮比降低有关。此外,细菌群落比真菌群落对环境变化的反应更灵敏。总之,我们的研究证明了土壤微生物多样性和群落结构对森林火灾的响应及驱动因素,从而加深了我们对环境扰动下森林生态系统土壤微生物动态的理解。
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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 : 2024-12-01 Epub 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。
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引用次数: 0
Differences in succession of bacterial communities during co-cultivation of corn straw with different soils 玉米秸秆与不同土壤共耕期间细菌群落演替的差异
IF 3.7 2区 农林科学 Q1 ECOLOGY Pub Date : 2024-12-01 Epub Date: 2024-10-13 DOI: 10.1016/j.ejsobi.2024.103683
Shuang Liu, Qingxin Meng, Yujia Li, Zhigang Wang, Weihui Xu, Yingning Sun, Zhidan Yu, Yunlong Hu
Managing carbon inputs from straw can pave the way towards carbon neutrality and climate change mitigation. Straw decomposition by cooperative microbial actions is an important process of carbon cycling in nature, and in this process, microbial communities are constantly in succession. Soil is rich in microorganisms and can be a source of microbial for straw degradation. In this study, corn straw was mixed with different soil types and incubated in conical flasks for 70 days. Bacterial diversity and community structure were determined using 16S rRNA sequencing. Then, the effects of physicochemical parameters and enzyme activities on the composition of bacterial communities at different stages were evaluated. The results showed that bacterial diversity decreased during co-cultivation. The differences in bacterial communities between all treatments were greater in the later stages, with Pseudomonadota, Actinomycetota, and Bacillota as the major phyla. Among them, the biomarkers at different times for different treatments included Sphingomonas, Mycobacterium, Oceanobacillus, Streptomyces, Pseudomonas, Flavobacterium, and Saccharomonospora. All of them showed cellulose degradation capacity; thus, the organic matter gradually decreased during the co-cultivation. Canonical correspondence analysis (CCA) showed that pH, organic matter (OM), electrical conductivity (EC), cellulase, β-glucosidase, and filter paper (FPase) activities had a significant effect on bacterial communities at different stages. Our findings suggested that soil microbial communities can be an effective source of cellulose-degrading microorganisms, and corn straw co-cultivation with different soil types increased the abundance of cellulose-degrading bacteria, which provides the theoretical basis for efficient cellulose-degrading agent screening.
管理来自秸秆的碳输入可以为实现碳中和和减缓气候变化铺平道路。微生物合作分解秸秆是自然界碳循环的一个重要过程,在此过程中,微生物群落不断更替。土壤中含有丰富的微生物,可以作为秸秆降解的微生物源。本研究将玉米秸秆与不同类型的土壤混合,并在锥形瓶中培养 70 天。使用 16S rRNA 测序测定了细菌多样性和群落结构。然后,评估了不同阶段理化参数和酶活性对细菌群落组成的影响。结果表明,细菌多样性在共培养过程中有所下降。所有处理之间的细菌群落差异在后期阶段都较大,主要以假单胞菌、放线菌和芽孢杆菌为主。其中,不同处理不同时间的生物标志物包括鞘氨单胞菌、分枝杆菌、海洋杆菌、链霉菌、假单胞菌、黄杆菌和酵母菌。它们都具有降解纤维素的能力,因此在共培养过程中有机物质逐渐减少。典型对应分析(CCA)表明,pH 值、有机质(OM)、电导率(EC)、纤维素酶、β-葡萄糖苷酶和滤纸酶(FPase)活性对不同阶段的细菌群落有显著影响。我们的研究结果表明,土壤微生物群落可作为纤维素降解微生物的有效来源,玉米秸秆与不同类型土壤共培养可提高纤维素降解菌的丰度,这为高效纤维素降解剂的筛选提供了理论依据。
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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 : 2024-12-01 Epub 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
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European Journal of Soil Biology
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