酯酶同工酶在食用菌菌种选育中的应用研究

采用聚丙烯酰胺凝胶电泳 ,分析了不同培养时间和不同培养基种类对平菇、杏鲍菇、白灵菇酯酶同工酶的影响 ,结果表明在不同培养时间和不同培养基条件下 ,酯酶同工酶酶谱的酶带呈现不同的多态性 ,由此提示同工酶在食用菌菌种选育的应用上应固定最佳培养时间及最适培养基种类 ,并在所有操作条件一致的情况下 ,才能得到稳定准确的分析结果     

Environmental stress response limits microbial necromass contributions to soil organic carbon

The majority of dead organic material enters the soil carbon pool following initial incorporation into microbial biomass. The decomposition of microbial necromass carbon (C) is, therefore, an important process governing the balance between terrestrial and atmospheric C pools. We tested how abiotic stress (drought), biotic interactions (invertebrate grazing) and physical disturbance influence the biochemistry (C:N ratio and calcium oxalate production) of living fungal cells, and the subsequent stabilization of fungal-derived C after senescence. We traced the fate of ¹³C-labeled necromass from ‘stressed’ and ‘unstressed’ fungi into living soil microbes, dissolved organic carbon (DOC), total soil carbon and respired CO₂. All stressors stimulated the production of calcium oxalate crystals and enhanced the C:N ratios of living fungal mycelia, leading to the formation of ‘recalcitrant’ necromass. Although we were unable to detect consistent effects of stress on the mineralization rates of fungal necromass, a greater proportion of the non-stressed (labile) fungal necromass C was stabilised in soil. Our finding is consistent with the emerging understanding that recalcitrant material is entirely decomposed within soil, but incorporated less efficiently into living microbial biomass and, ultimately, into stable SOC.     

Fungal and bacterial N2O production regulated by soil amendments of simple and complex substrates

Fungal N₂O production results from a respiratory denitrification that reduces NO₃⁻/NO₂⁻ in response to the oxidation of an electron donor, often organic C. Despite similar heterotrophic nature, fungal denitrifiers may differ from bacterial ones in exploiting diverse resources. We hypothesized that complex C compounds and substances could favor the growth of fungi over bacteria, and thereby leading to fungal dominance for soil N₂O emissions. Effects of substrate quality on fungal and bacterial N₂O production were, therefore, examined in a 44-d incubation after soils were amended with four different substrates, i.e., glucose, cellulose, winter pea, and switchgrass at 2 mg C g⁻¹ soil. During periodic measurements of soil N₂O fluxes at 80% soil water-filled pore space and with the supply of KNO₃, substrate treatments were further subjected to four antibiotic treatments, i.e., no antibiotics or soil addition of streptomycin, cycloheximide or both so that fungal and bacterial N₂O production could be separated. Up to d 8 when antibiotic inhibition on substrate-induced microbial activity and/or growth was still detectable, bacterial N₂O production was generally greater in glucose- than in cellulose-amended soils and also in winter pea- than in switchgrass-amended soils. In contrast, fungal N₂O production was more enhanced in soils amended with cellulose than with glucose. Therefore, fungal-to-bacterial contribution ratios were greater in complex than in simple C substrates. These ratios were positively correlated with fungal-to-bacterial activity ratios, i.e., CO₂ production ratios, suggesting that substrate-associated fungal or bacterial preferential activity and/or growth might be the cause. Considering substrate depletion over time and thereby becoming limited for microbial N₂O production, measurements of soil N₂O fluxes were also carried out with additional supply of glucose, irrespective of different substrate treatments. This measurement condition might lead to potentially high rates of fungal and bacterial N₂O production. As expected, bacterial N₂O production was greater with added glucose than with added cellulose on d 4 and d 8. However, this pattern was broken on d 28, with bacterial N₂O production lower with added glucose than with added cellulose. In contrast, plant residue impacts on soil N₂O fluxes were consistent over 44-d, with greater bacterial contribution, lower fungal contribution, and thus lower fungal-to-bacterial contribution ratios in winter pea- than in switchgrass-amended soils. Real-time PCR analysis also demonstrated that the ratios of 16S rDNA to ITS and the copy numbers of bacterial denitrifying genes were greater in winter pea- than in switchgrass-amended soils. Despite some inconsistency found on the impacts of cellulose versus glucose on fungal and bacterial leading roles for N₂O production, the results generally supported the working hypothesis that complex substrates promoted fungal dominance for soil N₂O emissions.     

间作栽培对宁夏南部山区马铃薯根际土壤真菌菌群结构的影响

根据宁夏南部山区气候和作物的生长特点,设计马铃薯‖玉米（P‖M,行比分别为4∶1,3∶2, 2∶3）、马铃薯‖蚕豆（P‖F,行比同前）、马铃薯不同品种（A‖B‖C,行比1∶1∶1）间作栽培模式,以马铃薯连作为对照,研究马铃薯根际土壤真菌多样性和菌群结构的变化,探寻能够减轻宁夏南部山区马铃薯连作障碍的有效栽培模式。采用基于18S rDNA的末端标记限制性片段长度多态性 (Terminal restriction fragment length polymorphism,T-RFLP) 技术研究不同间作栽培模式下马铃薯根际土壤真菌的菌群结构和多样性变化,构建真菌ITS克隆文库,利用Genbank数据库比对各栽培模式中ITS序列的测序结果,并作群落结构组成和功能分析。结果表明,马铃薯间作栽培后真菌Shannon-Wiener指数和Simpson指数均有不同程度降低;马铃薯与玉米、蚕豆间作后根际土壤真菌的物种丰富度在门、纲和目的分类学水平上与连作相比明显下降,菌群结构发生较大变化,成熟期马铃薯‖玉米3∶2行比间作模式与连作的差异最大,属的比例下降67.74%。间作栽培后,黑孢属（Nigrospora）、地丝霉属（Geomyces）、圆盘菌属（Orbilia）、枝顶孢属（Acremonium）、四枝孢属（Tetracladium）等9个属的真菌消失,同时新增刺盘孢属（Colletotrichum）、毛壳属（Chaetomium）、巨孢囊霉属（Gigaspora）、小球腔菌属（Pleosporineae）等13个属的真菌,其中马铃薯‖玉米3∶2行比间作后巨孢囊霉属比例高达60.35%。可见,马铃薯‖玉米间作栽培能有效改善马铃薯根际土壤的真菌菌群结构,使其微环境得以改善,缓解宁夏南部山区马铃薯连作障碍。     

迷迭香精油对几种植物病原菌的抑菌活性研究

采用生长速率法和抑菌圈法测定了迷迭香精油对甜瓜蔓枯病菌、西瓜炭疽病菌、甜瓜灰霉病菌、甜瓜枯萎病菌、梨树腐烂病菌、柑橘黑腐病菌、油菜菌核病菌、蚕豆轮纹病菌和桃细菌性穿孔病菌的抑菌活性.结果表明:迷迭香精油对8种病原真菌都具有很好的抑菌活性,其EC50分别为843.9914、1 084.2372、483.9457、1 735.5866、1 011.7869、901.2150、356.8803、1 197.3657 μL/L;对桃细菌性穿孔病菌也具有一定的抑菌活性,浓度为100 mL/L时,抑菌圈直径为1.00 cm,最低抑菌浓度为1 000 μL/L.     

印度梨形孢真菌促进芝麻生长并提高芝麻抗旱性

将印度梨形孢（Piriformospora indica,Pi）真菌接种芝麻幼苗根部,分别在大田及温室条件下研究供试真菌对芝麻生长和抗旱性的效应。大田试验主要调查产量性状,温室试验在芝麻初花期进行15d的持续干旱处理,测定株高等形态性状、过氧化氢酶活性等生理指标。结果表明,接种及未接种Pi真菌的芝麻植株在干旱处理前后叶长、叶宽差异达到极显著水平,株高、全展叶片数、基部茎粗、叶绿素含量、根颈粗差异达到显著水平;在人工干旱胁迫条件下,接种Pi真菌后芝麻植株能维持较高的过氧化氢酶（CAT）活性和较高含量的脯氨酸（Pro）,降低丙二醛（MDA）含量,从而减轻干旱胁迫伤害。在千粒重及单株籽粒重两个产量性状上,大田和温室接种的芝麻与未接种的差异均达到显著水平。接种Pi真菌不仅能促进芝麻的生长,而且在干旱条件下,使得芝麻表现出较强的抗旱性,显著提高芝麻产量。     

不同程度重金属污染对稻田土壤真菌群落结构的影响

为了研究土壤真菌群落结构在不同程度重金属污染中的变化,本文用Illumina Hi Seq高通量测序技术分析了苏南地区某金属冶炼厂和加工产业区的重金属污染水稻土的真菌群落结构,发现不同程度重金属污染对水稻季土壤真菌丰度和群落结构均有显著影响。经过真菌主成分分析发现,PC1影响因素对样品处理差异的贡献率是35.96%,PC2影响因素对样品处理差异的贡献率是21.48%;通过真菌冗余度分析发现,重金属Pb和Cu污染对土壤真菌群落结构的影响显著;通过对真菌属水平的相对丰度分析表明,重金属污染会显著降低敏感真菌的丰度,如被孢霉属相对丰度最高降低了87.50%、木霉属最高降低了99.46%、离壳菌属和菇属最高降低了100.00%,同时耐性真菌的相对丰度会提高,如类球囊霉属的相对丰度最高增加了98倍、四枝孢霉属最高增加了56倍、根囊壶菌属最高增加了2.62倍。综上所述,不同程度重金属污染对稻田土壤真菌群落结构有显著影响,且随着污染程度的增加,抗逆真菌相对数量和种类显著增加,敏感真菌的相对数量急剧减少,真菌群落结构随着重金属污染程度增加进一步分化。     

高氮和NO2-对中亚热带森林土壤N2O和NO产生的影响

利用15N同位素标记方法,研究在两种水分条件即60％和90％ WHC下,添加硝酸盐(NH4NO3,N 300 mg kg-1)和亚硝酸盐(NaNO2,N 1 mg kg-1)对中亚热带天然森林土壤N2O和NO产生过程及途径的影响.结果表明,在含水量为60％ WHC的情况下,高氮输入显著抑制了N2O和NO的产生(p＜0.01);但当含水量增为90％ WHC后,实验9h内抑制N2O产生,之后转为促进.所有未灭菌处理在添加NO2-后高氮抑制均立即解除并大量产生N2O和NO,与对照成显著差异(p＜0.01),在60％ WHC条件下,这种情况维持时间较短(21 h),但如果含水量高(90％ WHC)这种情况会持续很长时间(2周以上),说明水分有效性的提高和外源NO2-在高氮抑制解除中起到重要作用.本实验中N2O主要来源于土壤反硝化过程,而且加入未标记NO2-后导致杂合的N2O(14N15NO)分子在实验21 h内迅速增加,表明这种森林土壤的反硝化过程可能主要是通过真菌的“共脱氮”来实现,其贡献率可多达80％以上.Spearman秩相关分析表明未灭菌土壤NO的产生速率与N2O产生速率成显著正相关性(p＜0.05),土壤含水量越低二者相关性越高.灭菌土壤添加NO2-能较未灭菌土壤产生更多的NO,但却几乎不产生N2O,表明酸性土壤的化学反硝化对NO的贡献要大于N2O.     

Fungal biomass in pastures increases with age and reduced N input

Previous studies have shown that soil fungal biomass increases towards more natural, mature systems. Shifts to a fungal-based soil food web have previously been observed with abandonment of agricultural fields and extensification of agriculture. In a previous field experiment we found increased fungal biomass with reduced N fertilisation. Here, we explore relationships between fungi, bacteria, N input and grassland age on real dairy farms in the Netherlands. We hypothesised that also in pastures that are still in production there is a negative relationship between fungal biomass and fertilisation, and that fungal biomass increases with grassland age in pastures that are still in production. We expected the fungal/bacterial biomass ratio to show the same responses, as this ratio has often been used as an indicator for management changes. We sampled 48 pastures from eight organic dairy farms. Sites differed in age and fertilisation rate. We determined fungal and bacterial biomass, as well as ergosterol (a fungal biomarker). Fungal and bacterial biomass and ergosterol, showed a negative relationship with N application rate, and correlated positively with organic matter percentage. In old pastures, fungal biomass and ergosterol were higher than in younger pastures. Because bacterial biomass responded in the same way as fungal biomass, the F/B ratio remained constant, and can therefore—in our data set—not be used as an indicator for changing management. We conclude that the changes in fungal and bacterial biomass were driven by changes in organic matter quality and quantity. The negative relationship we found between N application rate and fungal biomass adds to earlier work and confirms the presence of this relationship in pastures with relatively small differences in management intensities. Earlier studies on shifts in fungal biomass focused on ex-agricultural fields or restoration projects. Here we show that fungal biomass is also higher in older agricultural pastures.     

Microbial populations,enzyme activities and nitrogen-phosphorus-potassium enrichment in earthworm casts and in the surrounding soil of a pineapple plantation

Summary Total populations of bacteria and fungi, dehydrogenase activity (as a measure of total potential microbial activity), and urease and phosphatase activities were determined in earthworm casts and surrounding laterite soils planted to pineapple. The casts contained higher microbial populations and enzyme activities than the soil. Except for fungal populations, statistically significant (P = 0.05) increases were found in all other parameters. Microbial populations and enzyme activities showed similar temporal trends with higher values in spring and summer and lower values in winter. The earthworm casts contained higher amounts of N, P, K and organic C than the soil (P = 0.05). Selective feeding by earthworms on organically rich substrates, which break down during passage through the gut, is likely to be responsible for the higher microbial populations and greater enzyme activity in the casts.