慢性前列腺炎厌氧菌感染的研究

本文对１０６例前列腺标本进行了细菌学研究。慢性前列腺炎厌氧菌检出率为２７．３％（２９／１０６）。厌氧菌阳性者中６８．９％（２０／２９）与需氧菌组成混合感染３１％（９／２９）为单纯厌氧菌感染。研究还提示：厌氧菌感染是慢性前列腺炎不可忽视的原因,氟呱酸对厌氧菌有强大杀灭作用。     

Na+, K+, Cl− cotransport and its regulation in Ehrlich ascites Tumor cells. Ca2+/Calmodulin and protein kinase C dependent pathways

Summary Net Cl^– uptake as well as unidirectional³⁶Cl influx during regulatory volume increase (RVI) require external K⁺. Half-maximal rate of bumetanide-sensitive³⁶Cl uptake is attained at about 3.3mm external K⁺. The bumetanide-sensitive K⁺ influx found during RVI is strongly dependent on both Na⁺ and Cl^–. The bumetanide-sensitive unidirectional Na⁺ influx during RVI is dependent on K⁺ as well as on Cl^–. The cotransporter activated during RVI in Ehrlich cells, therefore, seems to transport Na⁺, K⁺ and Cl^–. In the presence of ouabain and Ba⁺ the stoichiometry of the bumetanide-sensitive net fluxes can be measured at 1.0 Na⁺, 0.8 K⁺, 2.0 Cl^– or approximately 1 : Na, 1 : K, 2 : Cl. Under these circumstances the K⁺ and Cl^– flux ratios (influx/efflux) for the bumetanide-sensitive component were estimated at 1.34 ±0.08 and 1.82 ± 0.15 which should be compared to the gradient for the Na⁺, K⁺, 2Cl^– cotransport system at 1.75 ± 0.24.Addition of sucrose to hypertonicity causes the Ehrlich cells to shrink with no signs of RVI, whereas shrinkage with hypertonic standard medium (all extracellular ion concentrations increased) results in a RVI response towards the original cell volume. Under both conditions a bumetanide-sensitive unidirectional K⁺ influx is activated. During hypotonic conditions a small bumetanide-sensitive K⁺ influx is observed, indicating that the cotransport system is already activated.The cotransport is activated 10–15 fold by bradykinin, an agonist which stimulates phospholipase C resulting in release of internal Ca²⁺ and activation of protein kinase C.The anti-calmodulin drug pimozide inhibits most of the bumetanide-sensitive K⁺ influx during RVI. The cotransporter can be activated by the phorbol ester TPA. These results indicate that the stimulation of the Na⁺, K⁺, Cl^– cotransport involves both Ca²⁺/calmodulin and protein kinase C.     

Coupling Among Energy Failure, Loss of Ion Homeostasis, and Phospholipase A2 and C Activation During Ischemia

Abstract— The objective of the present experiments was to correlate changes in cellular energy metabolism, dissipative ion fluxes, and lipolysis during the first 90 s of ischemia and, hence, to establish whether phospholipase A₂or phospholipase C is responsible for the early accumulation of phospholipid hydrolysis products. Ischemia was induced for 15–90 s in rats, extracellular K⁺ (K⁺_e) was recorded, and neocortex was frozen in situ for measurements of labile tissue metabolites, free fatty acids, and diacylglycerides. Ischemia of 15-and 30-s duration gave rise to a decrease in phosphocreatine concentration and a decline in the ATP/free ADP ratio. Although these changes were accompanied by an activation of K⁺ conductances, there were no changes in free fatty acids until after 60s, when free arachidonic acid accumulated. An increase in other free fatty acids and in total diacylglyceride content did not occur until after anoxic depolarization. The results demonstrate that the early functional changes, such as activation of K⁺ conductances, are unrelated to changes in lipids or lipid mediators. They furthermore suggest that the initial lipolysis occurs via both phospholipase A₂ and phospholipase C, which are activated when membrane depolarization leads to influx of calcium into cells.     

Bacterial Disproportionation of Elemental Sulfur Coupled to Chemical Reduction of Iron or Manganese

A new chemolithotrophic bacterial metabolism was discovered in anaerobic marine enrichment cultures. Cultures in defined medium with elemental sulfur (S⁰) and amorphous ferric hydroxide (FeOOH) as sole substrates showed intense formation of sulfate. Furthermore, precipitation of ferrous sulfide and pyrite was observed. The transformations were accompanied by growth of slightly curved, rod-shaped bacteria. The quantification of the products revealed that S⁰ was microbially disproportionated to sulfate and sulfide, as follows: 4S⁰ + 4H₂O → SO₄^2- + 3H₂S + 2H⁺. Subsequent chemical reactions between the formed sulfide and the added FeOOH led to the observed precipitation of iron sulfides. Sulfate and iron sulfides were also produced when FeOOH was replaced by FeCO₃. Further enrichment with manganese oxide, MnO₂, instead of FeOOH yielded stable cultures which formed sulfate during concomitant reduction of MnO₂ to Mn²⁺. Growth of small rod-shaped bacteria was observed. When incubated without MnO₂, the culture did not grow but produced small amounts of SO₄^2- and H₂S at a ratio of 1:3, indicating again a disproportionation of S⁰. The observed microbial disproportionation of S⁰ only proceeds significantly in the presence of sulfide-scavenging agents such as iron and manganese compounds. The population density of bacteria capable of S⁰ disproportionation in the presence of FeOOH or MnO₂ was high, > 10⁴ cm^-3 in coastal sediments. The metabolism offers an explanation for recent observations of anaerobic sulfide oxidation to sulfate in anoxic sediments.     

Iron-bound phosphorus in marine sediments as measured by bicarbonate-dithionite extraction

A sequential five-step extraction scheme for phosphorus pools in freshwater sediment was modified for use in marine sediments. In the second step phosphate bound to reducible forms of iron and manganese (iron-bound P) is extracted by a bicarbonate buffered dithionite solution (BD-reagent). The extraction scheme was tested on sediment from 16 m water depth in Aarhus Bay, DK and used in two other marine sediments: Kattegat at 56 m and Skagerrak at 695 m depth. By comparing the BD-extractable P-pool with both the pool of iron in the BD-fraction and the pool of oxidized, amorphous or poorly crystalline iron (am.FeOOH), highly significant correlations (p < 0.001) were observed in all three sediments. Thus, we conclude that the BD-reagent was very specific for iron-bound P. Further evidence for this came from two experiments: 1) Enhanced BD treatment did not result in additional phosphate extraction and 2) by sequential extraction of phosphorus pools in pure cultures of diatoms and cyanobacteria no phosphate was recovered in the BD-fraction. The pool of am.FeOOH was very important for controlling porewater phosphate concentration which was inferred from the significant inverse relationships between the two parameters (p < 0.001) in all sediments studied. Further, an isotopic exchange experiment with ³²PO_f4/^p3– revealed that BD-extractable P was by far the most exchangeable P-pool even deep in the sediment where the pool size was small. Iron-bound P made up 33–45% of total P in the surface sediments. The ratio between iron-bound phosphate and am.FeOOH was 8–11 in Aarhus Bay and Kattegat. In Skagerrak the ratio was 17, which may indicate that the iron mineral extracted from this sediment is less capable of adsorbing phosphate or less saturated with phosphate.     

Reactions Catalyzed by Peg-Modified α-Chymotrypsin in Organic Solvents. Influence of Water Content and Degree of Modification

-Chymotrypsin was modified with cyanuric chloride activated monomethoxypolyethylene glycol (MPEG) with molecular weights 1900 and 5000. Using the higher molecular weight MPEG a product that was soluble in benzene at moderate levels of modification was obtained, whereas with MPEG 1900 almost all the enzyme's amino groups had to be modified for dissolving the conjugate. The catalytic activity decreased with increasing degree of substitution. Apparent V_max was considerably higher for the less modified enzyme preparation than for the more modified one, while K_m,app stayed almost constant. The modified enzyme was used for peptide synthesis. The reaction was dependent on the content of dissolved water. Both V_max,app and K_m,app increased with increasing water content. It was possible to achieve a process with complete conversion of substrate to dipeptide.     

山医群体近交系中国地鼠(Cricetulus griseus)的研究——Ⅲ.生物学特性

山医群体近交系中国地鼠的红细胞、白细胞、网织红细胞、血红蛋白及血清蛋白量均与人类相近。血小板数高于人类,但低于小鼠。嗜中性与淋巴细胞的比值与人类相反而与小鼠近似。血清尿素氮及谷丙转氨酶高于人类生理值,低于SD大鼠。心率为658±102次/min,呼吸率20±30次/min。心电图除T波低平外,其余与人类相近。颈动脉血压为13.47±1.01/12.48±1.09kPa。染色体数为2n=22。以上各项在近交系地鼠和野生地鼠间未见明显差异。     

南极乔治王岛冰锥洞微生物培养探索

【目的】南极洲具备独特的环境和相对的生物地理隔离,南极洲各类生境中蕴藏了大量尚未培养和难培养的微生物,也是新颖微生物物种的重要来源之一。本研究以南极冰锥洞这类特殊生境为研究对象,通过培养条件的多样化提升南极微生物的培养率和多样性,揭示南极冰锥洞可培养微生物类群多样性,为该环境可培养微生物功能研究奠定基础,也为南极极端环境未培养微生物的培养方法提供借鉴。【方法】通过采用不同培养基添加复苏促进因子(resuscitation promoting factor, Rpf)的方式,提高南极柯林斯冰盖冰锥洞生境中微生物的可培养率,探究该生境中微生物的多样性。采用4种不同营养水平的培养基,平行添加Rpf进行菌株培养,经分离纯化与16S rRNA基因鉴定,分析冰锥洞可培养微生物的多样性及培养条件对多样性的影响。【结果】本研究共分离培养细菌407株,涵盖5个门、18个科、29个属,其中：放线菌门(Actinomycetota)为优势门,占72.73%;微杆菌科(Microbacteriaceae)为优势科,占69.78%;Lacisediminihabitans属为优势属,占45.70%。从培养基效果...     

Rice ubiquitin-conjugating enzyme OsUbc13 negatively regulates immunity against pathogens by enhancing the activity of OsSnRK1a

Ubc13 is required for Lys63-linked polyubiquitination and innate immune responses in mammals, but its functions in plant immunity still remain largely unknown. Here, we used molecular biological, pathological, biochemical, and genetic approaches to evaluate the roles of rice OsUbc13 in response to pathogens. The OsUbc13-RNA interference (RNAi) lines with lesion mimic phenotypes displayed a significant increase in the accumulation of flg22- and chitin-induced reactive oxygen species, and in defence-related genes expression or hormones as well as resistance to Magnaporthe oryzae and Xanthomonas oryzae pv oryzae. Strikingly, OsUbc13 directly interacts with OsSnRK1a, which is the α catalytic subunit of SnRK1 (sucrose non-fermenting-1-related protein kinase-1) and acts as a positive regulator of broad-spectrum disease resistance in rice. In the OsUbc13-RNAi plants, although the protein level of OsSnRK1a did not change, its activity and ABA sensitivity were obviously enhanced, and the K63-linked polyubiquitination was weaker than that of wild-type Dongjin (DJ). Overexpression of the deubiquitinase-encoding gene OsOTUB1.1 produced similar effects with inhibition of OsUbc13 in affecting immunity responses, M. oryzae resistance, OsSnRK1a ubiquitination, and OsSnRK1a activity. Furthermore, re-interfering with OsSnRK1a in one OsUbc13-RNAi line (Ri-3) partially restored its M. oryzae resistance to a level between those of Ri-3 and DJ. Our data demonstrate OsUbc13 negatively regulates immunity against pathogens by enhancing the activity of OsSnRK1a.     

有机肥施用对红壤原生生物与微生物互作的影响

为明确不同施肥处理对土壤原生生物群落、微生物碳代谢活性的影响,以南方典型旱地红壤为研究对象,基于中国科学院鹰潭红壤生态实验站玉米单作系统有机培肥长期定位试验,选取不施肥(M0)、低量猪粪(M1)、高量猪粪(M2)、高量猪粪+石灰(M3)4个处理,利用高通量测序技术研究不同猪粪处理下红壤原生生物多样性、群落结构的变化,揭示原生生物与微生物互作对土壤微生物碳代谢活性和玉米产量的影响。结果表明：(1)长期施用猪粪处理下,土壤pH、有机质(SOM)、全氮(TN)、全磷(TP)、速效磷(AP)和速效钾(AK)的含量显著提高;(2)与M0处理相比,施肥处理显著提高了原生生物生物量和多样性,并且显著改变了其群落结构,其中土壤TP、pH、AP、TN、SOM和AK是原生生物群落结构变化的重要驱动因子;(3)施肥处理显著提高了土壤细菌和真菌生物量,增加了微生物碳代谢活性(Average well color development, AWCD);(4)土壤pH和AP通过影响原生生物多样性和群落结构,间接提高了微生物碳代谢活性和玉米产量。本研究结果为提升旱地红壤的生物多样性,保障土壤健康和维持生态系统服务功...