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21.
Plant roots and soil microorganisms contain significant quantities of low molecular weight (MW) phosphorylated nucleosides and sugars. Consequently, upon death these can represent a significant input of organic-P to the soil. Some of these organic-P substrates must first be dephosphorylated by phosphatases before being assimilated by the soil microbial community while others can be taken up directly from soil solution. To determine whether sorption or phosphatase activity was limiting the bioavailability of low MW organic-P in soil we compared the microbial uptake and C mineralization of a range of 14C-labeled organic-P substrates [glucose-6-phosphate, adenosine monophosphate (AMP), adenosine diphosphate (ADP) and adenosine triphosphate (ATP)] to that of the parent compounds (adenosine and glucose). In a fertile grassland soil we showed that at low organic-P substrate concentrations (<0.5 mM) phosphatase activity did not limit microbial uptake or mineralization in comparison to their non-phosphorylated counterparts. However, at high substrate concentrations (1-10 mM) the mineralization of the organic-P compounds was significantly lower than that of the non-phosphorylated compounds suggesting that phosphatase activity or microbial transporter capacity limited bioavailability. Sorption to the solid phase followed the series glucose<adenosine<G-6-P<AMP<ADP=ATP. However, sorption of the organic-P compounds to the solid phase did not appear to greatly affect bioavailability. The high adenosine mineralization capacity of the microbial biomass suggests that nucleosides may represent a significant source of C and N to the soil microbial biomass. We conclude that at low organic-P substrate concentrations typical of those in soil, neither phosphatase activity nor sorption greatly limits their bioavailability.  相似文献   
22.
以新疆巩留县和新源县2个居群下的7个新疆野苹果群体当年生枝条为材料,应用EIS法对各群体抗寒性进行测定,并与电导率法进行对比分析。结果表明:巩留和新源2个居群内群体间的半致死温度差异不显著,2个居群间的差异显著,巩留居群的半致死温度显著低于新源居群,证明巩留居群的抗寒性高于新源居群。电阻抗图谱法单-DCE模型中6个参数(τ,ψ,r,r1,re,ri)中,r1,re,τ3个参数可以得出供试样品的半致死温度,其中r1,re所得的半致死温度与电导率法相关系数达到极显著水平,说明参数r1,re适用于新疆野苹果的抗寒性测定。电阻抗图谱法(EIS)与电导率法的抗寒性测定结果基本一致,但省时、不需温育,具有更大优越性。  相似文献   
23.
Deposition of anthropogenic nitrogen (N) alters the decomposition of organic matter in forest ecosystems by changing the expression of key microbial enzymes. We investigated the effects of experimental N deposition on dissolved organic matter (DOM) in soils of three forest ecosystems representative of the upper Great Lakes region: the sugar maple/basswood (SMBW), sugar maple/red oak (SMRO) and white oak/black oak (WOBO) ecosystems. Mineral soil samples were collected on five dates from ambient and N-amended plots (80 kg N ha−1 yr−1) in three replicate stands of each forest type. DOM was extracted (2:1, water:soil) from each soil sample and analyzed for dissolved organic carbon (DOC). DOC concentration was significantly greater in the N-amended soils (on average: 24% higher for SMBW, 9% for SMRO, and 40% for BOWO). In June and October 2002, bioassays were performed to assess N treatment effects on the composition of DOM and its interacting bacterial community. Within each site, DOM extracts from the ambient and N-amended plots were reciprocally inoculated with bacteria from each plot. After a 48 h incubation at 20 °C, community activity in each microcosm was profiled by measuring 10 extracellular enzyme activities (EEA). MANOVA showed that ecosystem type, sampling date, DOM source (ambient or N-amended plot) and inoculum source (ambient or N-amended plot) all had significant effects on bioassay EEA. Post hoc tests (Tukey's HSD) found significant reductions in oxidative enzyme activity as a result of the N treatment. In general, the bioassay results corroborated a previous report describing losses in soil oxidative enzyme activity in response to N saturation. However, it is not clear whether increased DOC concentration is the direct result of reduced oxidative activity.  相似文献   
24.
溶藻细菌胞外溶藻活性物质分离的研究进展   总被引:1,自引:0,他引:1  
王飞  李燕 《安徽农业科学》2008,36(17):7071-7073
利用溶藻细菌治理水华引起了人们越来越多的关注。通过间接方式释放特异性或非特异性的胞外物质是溶藻细菌溶藻的主要方式。总结了国内外在溶藻细菌胞外溶藻活性物质方面的最新分离进展,探讨了研究的趋势和应用前景。  相似文献   
25.
AIM: To investigate the correlation between extracellular signal-regulated kinase 5 ( ERK5 ) -322G/T polymorphism (rs3866958) and the susceptibility to sporadic colorectal cancer (CRC) in southern Chinese population. METHODS: ERK5 -322G/T genotypes were determined by Taqman-MGB probes in 835 CRC cases and 908 healthy controls. RESULTS: No significance of ERK5 -322G/T genotype distribution between CRC patients and controls was observed, but -322G/T decreased the susceptibility to CRC in fat people whose BMI was ≥ 24 kg/m2. Compared to GG genotypes, the carriers with GT and TT genotypes had a significant decrease in the risk of CRC(OR=0.576,95%CI 0.413-0.804, P<0.01). CONCLUSION: ERK5 -322G/T polymorphism (rs3866958) has no significant relevance with sporadic CRC susceptibility, but decrease, the risk of CRC in people with fatness. The T variant genotype is an independent protective factor against sporadic CRC of overweight patients in southern Chinese population.  相似文献   
26.
While soil extracellular enzyme assays (EEAs) are frequently used to infer soil microbial function, the data typically reflect a small number of sampling points across a season, and it is unclear to what extent soil EEA may vary on the time scale of days to weeks. Rain events, in particular, may cause rapid shifts in EEA, and fine scale temporal data are needed to properly assess the generality of EEA data collected at coarser time scales. We examined soil EEA 2-3 times per week in the field from June to November in the context of natural rain events and temperature fluctuations, and explored how long-term water addition altered EEA responses. We also tested the short-term effects of water addition on the distribution of EEA in intact soil mesocoms and leachate. There was little temporal variation in EEA for the hydrolases phosphatase, N-acetyl-glucosaminidase and β-glucosidase, despite the occurrence of multiple large rain events and large soil temperature fluctuations. Phenol oxidase activity correlated significantly with seasonal trends in temperature and soil moisture, but was highly variable at short time scales, and the latter did not correlate significantly with short-term changes in soil microclimate. EEA generally increased in response to long-term water addition, and in soil mesocosms water addition did not significantly redistribute EEA among the upper and lower soil layers, and leachate EEA was three orders of magnitude lower than soil EEA. Overall, our results reveal relatively minor short-term variation in EEA for hydrolase enzymes, and no discernable response to temperature fluctuations or precipitation over the short term. However, high short-term variation in phenol oxidase activity suggests that it may be difficult to infer temporal trends in EEA for this enzyme from a limited number of sampling points.  相似文献   
27.
水稻白叶枯病菌是一种引起水稻白叶枯病的植物病原细菌,水稻白叶枯病是世界水稻生产中最严重的细菌性病害之一。本研究采用携带同源序列的自杀质粒pK18MobGⅡ整合的办法构建了水稻白叶枯病菌中国菌株13751编码6-磷酸葡糖酸内酯酶的基因XOO2193的非极性突变体GNM2193。对突变体的表型分析发现其毒力在杂交水稻品种特优63上显著减弱,突变体在非寄主植物蓖麻上不能引起过敏反应。此外,突变体胞外多糖的产量是野生型的43.4%。用一段含有XOO2193基因的DNA片段对GNM2193进行功能互补,互补菌株在水稻上的毒力、引起过敏反应的能力和胞外多糖产量恢复到野生型水平。说明XOO2193基因与病菌的毒力和胞外多糖的产生有关。  相似文献   
28.
The fate of extracellular DNA in the environment concerns both the fate of transgenes from genetically modified organisms and the evolution of active bacteria capable of incorporating this DNA into their genomes. This study addressed the possibility that DNA, like other organic molecules, could move vertically in the capillary fringe of groundwater aquifers. The targeted gene fragment used here was the 35S-nptII sequence, which was below detection levels in controls. Initial microcosm studies detected the DNA target molecule by PCR during the entire experiment. The vertical advection of water and DNA were monitored for a period of 3 days in soil columns. DNA was added as a water solution at the bottom of the unsaturated soil column, and then DNA-free water was added at the bottom after 12 and 24 h. After the addition of the DNA solution, capillary water rose 4 cm within the soil column and the target DNA was detected up to that height. After 60 min, the entire soil column (10 cm) was wetted and the target sequence was detected up to a height of 7.5 cm. After the second wetting (12 h later), the target sequence was detected up to the top of the soil column (10 cm). However, after the third wetting (24 h later), the marker sequence was only found at heights from 0.5 to 4 cm. Results clearly show the vertical movement of DNA due the capillary rise and suggest the possibility of DNA degradation within the soil column.  相似文献   
29.
Enzyme activities have been used as indicators of soil quality and changes in biogeochemical function due to management or perturbations. The objective of this study was to answer a number of methodological questions regarding sampling schemes, sample handling recommendations, and assay procedures to facilitate the use of enzyme assays in the tropical highlands of East Africa. We used para-nitrophenol (pNP) based substrates for five enzymes: β-glucosidase, cellobiohydrolase, chitinase, acid phosphatase, and alkaline phosphatase. In the first experiment, we examined sampling procedures and compared the results of determining enzyme activities on a plot using composite or discrete samples. Composite samples usually had higher activities than the means of individual cores (P<0.05), but relative ranking of sites was the same if analyses were based on composite or discrete samples. In the second experiment, we examined the effects of storage time and conditions on enzyme activity. Enzyme activity degraded rapidly in frozen samples, but was better maintained in samples stored at 4 °C. Phosphatase and cellobiohydrolase activity declined after 14 days of storage, while the activity of the other enzymes remained close to the values of fresh samples for 28 or more days. In the third experiment, we examined the effect of the addition of an antiseptic, toluene, to prevent bacterial growth during the assay. We found no consistent toluene effect (P>0.4), probably because the assays were of short duration and microbial growth was minimized. Finally, we looked at the incubation time necessary to produce reliable results. Phosphatases, with relatively high activities could reliably be determined in 2 h incubations, but the other enzymes had much lower activities and required longer incubation times for reliable determination. For the enzymes we looked at, 4 h was a good standard time for determining the activity of even the lowest activity enzymes. The results of this study provide practical guidelines for applying these enzyme assays in the degraded tropical soils.  相似文献   
30.
Declining rates of soil respiration are reliably observed during long-term laboratory incubations. However, the cause of this decline is uncertain. We explored different controls on soil respiration to elucidate the drivers of respiration rate declines during long-term soil incubations. Following a long-term (707 day) incubation (30 °C) of soils from two sites (a cultivated and a forested plot at Kellogg Biological Station, Hickory Corners, MI, USA), soils were significantly depleted of both soil carbon and microbial biomass. To test the ability of these carbon- and biomass-depleted (“incubation-depleted”) soils to respire labile organic matter, we exposed soils to a second, 42 day incubation (30 °C) with and without an addition of plant residues. We controlled for soil carbon and microbial biomass depletion by incubating field fresh (“fresh”) soils with and without an amendment of wheat and corn residues. Although respiration was consistently higher in the fresh versus incubation-depleted soil (2 and 1.2 times higher in the fresh cultivated and fresh forested soil, respectively), the ability to respire substrate did not differ between the fresh and incubation-depleted soils. Further, at the completion of the 42 day incubation, levels of microbial biomass in the incubation-depleted soils remained unchanged, while levels of microbial biomass in the field-fresh soil declined to levels similar to that of the incubation-depleted soils. Extra-cellular enzyme pools in the incubation-depleted soils were sometimes slightly reduced and did not respond to addition of labile substrate and did not limit soil respiration. Our results support the idea that available soil organic matter, rather than a lack microbial biomass and extracellular enzymes, limits soil respiration over the course of long-term incubations. That decomposition of both wheat and corn straw residues did not change after major changes in the soil biomass during extended incubation supports the omission of biomass values from biogeochemical models.  相似文献   
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