人胃癌BGC-823细胞中去甲斑蝥素抑癌作用机理的蛋白质组学研究

去甲斑蝥素是我国自行研制的抗肿瘤药物,在临床上主要用于消化道肿瘤的治疗．实验表明,去甲斑蝥素可引起人胃癌BGC-823细胞发生 M期阻滞及细胞凋亡．进一步利用双向电泳和质谱技术,筛选出了去甲斑蝥素抑癌作用相关蛋白．研究显示,线粒体热休克蛋白CH60、线粒体ATP合酶d亚单位、内质网葡萄糖调节蛋白GRP78、线粒体Hsp70的辅助因子GRPE1、SH3L3以及染色质组装因子1小亚基RBBP4参与了去甲斑蝥素的抑癌作用．研究提示,去甲斑蝥素可能通过促进线粒体热休克蛋白及p53的表达进而激活caspase-3依赖的凋亡通路,并且去甲斑蝥素在引发内质网协迫之后,可通过抑制胞外信号调节激酶(extracellular signal regulated kinase, ERK)的活性促进肿瘤细胞的凋亡．进一步分析了去甲斑蝥素与线粒体ATP合酶抑制剂寡霉素A的联合用药对人胃癌细胞生长的影响,结果表明,联合用药的抑瘤效果比单独用药的抑瘤效果显著,提示去甲斑蝥素可能通过抑制线粒体ATP合酶功能抑制BGC-823生长．上述结果为优化去甲斑蝥素的联合用药方案提供了新线索．     

Effects of temperature on simultaneous nitrification and denitrification via nitrite in a sequencing batch biofilm reactor

A laboratory scale experiment was described in this paper to enhance biological nitrogen removal by simultaneous nitrification and denitrification (SND) via nitrite with a sequencing batch biofilm reactor (SBBR). Under conditions of total nitrogen (TN) about 30 mg/L and pH ranged 7.15–7.62, synthetic wastewater was cyclically operated within the reactor for 110 days. Optimal operation conditions were established to obtain consistently high TN removal rate and nitrite accumulation ratio, which included an optimal temperature of 31 °C and an aeration time of 5 h under the air flow of 50 L/h. Stable nitrite accumulation could be realized under different temperatures and the nitrite accumulation ratio increased with an increase of temperature from 15 to 35 °C. The highest TN removal rate (91.9%) was at 31 °C with DO ranged 3–4 mg/L. Process control could be achieved by observing changes in DO and pH to judge the end-point of oxidation of ammonia and SND.     

杂交-渐渗进化理论在转基因逃逸及其环境风险评价和研究中的意义

转基因作物的商品化生产和大规模环境释放, 引起了全球对生物安全问题的广泛关注和争议, 其中转基因通过花粉介导的基因漂移逃逸到非转基因作物及其野生近缘种, 进而带来不同类型的环境风险就是备受争议的生物安全问题之一。有效的生物安全评价和研究能够为转基因作物的安全持久利用保驾护航。按照风险评价的原则, 对于转基因逃逸及其潜在环境风险的评价应包括两个重要步骤: (1)检测转基因向野生近缘种(包括杂草类型)群体逃逸的频率; (2)确定逃逸后的转基因能否通过遗传渐渗在野生近缘种群体中存留和扩散。杂交－渐渗是进化生物学中非常重要的科学命题和普遍的自然现象, 杂交－渐渗的进化理论与转基因逃逸及其潜在环境风险的研究和评价有密切的关系。杂交－渐渗过程往往导致物种形成、适应性进化和自然群体的濒危与灭绝, 这是因为在杂交－渐渗过程中, 不同的机制如遗传同化作用、群体湮没效应以及群体的选择性剔除效应等都会在很大程度上影响群体的进化过程。转基因通过杂交－渐渗进入野生群体, 使这一过程更加复杂化。如果转基因能提高群体的适合度, 则更有利于其渐渗速率, 从而在群体中迅速扩散并带来一定的生态后果。杂交－渐渗的进化理论和思想将有益于指导转基因逃逸及其潜在环境风险的研究和评价。     

空心莲子草性可塑性影响下的克隆整合

植物的生活史由其有性生殖构件和营养体构件相互作用共同完成,克隆整合作为克隆植物的重要特征,其与有性生殖特征的相互作用关系却所知很少。该研究通过同质园种植实验,分析了空心莲子草的分株表型、生理、性别等与克隆整合的关系。结果表明:(1)克隆整合以及分株间是否连接对空心莲子草的表型特征、气体交换等生理性状和性别特征均有显著影响。(2)克隆整合显著缩小了雌雄同花和雄蕊心皮化两种性别植株间表型特征的差距,后代的性别特征与营养体表型特征显著相关。(3)在贫瘠的沙土基质中克隆整合明显增加了空心莲子草的营养体生长特征和气体交换等光合生理指标,但这种增加在富含有机质的塘泥基质中不明显。(4)居于不同土壤基质分株间的联系会减少分株表型特征和气体交换对生长环境的响应,并保持母体性别特征不受环境的影响,但单独居于沙土或塘泥单一土壤基质的分株性别特征却因受到环境影响而改变。因此,克隆整合有利于空心莲子草性别特征的稳定。     

Root microbiota shift in rice correlates with resident time in the field and developmental stage

Land plants in natural soil form intimate relationships with the diverse root bacterial microbiota. A growing body of evidence shows that these microbes are important for plant growth and health. Root microbiota composition has been widely studied in several model plants and crops; however, little is known about how root microbiota vary throughout the plant's life cycle under field conditions. We performed longitudinal dense sampling in field trials to track the time-series shift of the root microbiota from two representative rice cultivars in two separate locations in China. We found that the rice root microbiota varied dramatically during the vegetative stages and stabilized from the beginning of the reproductive stage, after which the root microbiota underwent relatively minor changes until rice ripening. Notably, both rice genotype and geographical location influenced the patterns of root microbiota shift that occurred during plant growth. The relative abundance of Deltaproteobacteria in roots significantly increased overtime throughout the entire life cycle of rice, while that of Betaproteobacteria, Firmicutes, and Gammaproteobacteria decreased. By a machine learning approach, we identified biomarker taxa and established a model to correlate root microbiota with rice resident time in the field(e.g., Nitrospira accumulated from 5 weeks/tillering in field-grown rice). Our work provides insights into the process of rice root microbiota establishment.     

过表达亚甲基四氢叶酸脱氢酶对高山被孢霉脂质合成的影响

高山被孢霉是一种富含多不饱和脂肪酸的丝状真菌,但其脂质过程中NADPH的来源还没有研究透彻。以高山被孢霉(尿嘧啶营养缺陷型)作为出发菌株,研究亚甲基四氢叶酸脱氢酶(MTHFD1)对高山被孢霉脂质合成的影响。首先构建了过表达载体pBIG2-ura5s-MTHFD1,采用根癌土壤杆菌介导转化真菌的方法,将二元表达载体转化进高山被孢霉CCFM501中,在筛选培养基SC-CS平板上进行筛选,进而得到稳定遗传MTHFD1基因的过表达菌株(MA-MTHFD1);其次提取MA-MTHFD1菌株基因组进行PCR鉴定,并结合qPCR分析结果,表明MTHFD1基因成功在高山被孢霉中实现了过量表达;最后通过对MA-MTHFD1中的脂肪酸含量、NADPH含量及NADPH合成途径中相关基因转录水平进行分析,研究MTHFD1基因过表达对脂质合成的影响。实验结果表明,过表达MTHFD1基因可以提高高山被孢霉脂质合成能力。与原养型高山被孢霉相比,MA-MTHFD1菌株中脂肪酸含量提高了40.13%,NADPH的含量提高了26.45%,而且NADPH合成途径中其他相关基因苹果酸酶(ME)和异柠檬酸脱氢酶(IDH)的转录水平也发生了上调。这一系列研究结果表明,在高山被孢霉脂质合成还原力形成中,MTHFD1基因起到了关键作用。这为解析高山被孢霉中NADPH来源及深入研究脂质合成机制,从而对其胞内脂肪酸代谢通路进行分子水平上的改建提供了一定的理论依据。     

热带假丝酵母脂肪醛脱氢酶基因CtAld1和CtAld2的功能评价

【目的】热带假丝酵母是发酵法生产二元酸的重要工业菌株,具有较高的ω-氧化活性。脂肪醛脱氢酶在ω-氧化途径中起重要作用,催化脂肪醛生成脂肪酸,但其具体催化功能及对细胞生理影响还未被系统研究。本文通过删除脂肪醛脱氢酶基因CtAld1和CtAld2鉴定了其在ω-氧化途径中的功能。【方法】通过基因组信息挖掘获得热带假丝酵母脂肪醛脱氢酶基因CtAld1和CtAld2序列,在此基础上,通过同源重组敲除CtAld1和CtAld2基因。考察突变株的生长和胞内脂肪醛脱氢酶活性变化,并评价CtAld1和CtAld2基因敲除对细胞二元酸合成能力的影响。【结果】分别获得了热带假丝酵母突变株XZX-1(ΔCtAld1/ΔCtAld1)、XZX-2(ΔCtAld2/ΔCtAld2)和XZX-12(ΔCtAld1/ΔCtAld1,ΔCtAld2/ΔCtAld2)。在以十二烷为唯一碳源的培养基中,敲除CtAld2基因显著抑制细胞的生长,胞内脂肪醛脱氢酶活性降低为出发菌株的30%;敲除CtAld1基因尽管会使细胞损失一部分醛脱氢酶活性,但能够一定程度地提升细胞在十二烷中的生长性能。敲除CtAld1或CtAld2会降低菌株二元酸产量,组合敲除CtAld1和CtAld2严重削弱菌株十二碳二元酸的合成能力。【结论】CtAld2对热带假丝酵母细胞的生长和十二碳二元酸的合成具有重要作用,缺失CtAld1或CtAld2基因降低细胞的二元酸合成能力。CtAld1和CtAld2可作为热带假丝酵母ω-氧化途径代谢工程改造的潜在靶点。     

云南中度退化的喀斯特天坑草地植物群落优势种种间关系

喀斯特天坑作为独特的宏大地表负地形,其坑底生境与外界环境相互独立,呈现出独特的植物群落格局及特征.本研究选取云南沾益天坑群中可进入性较强的中度退化天坑--巴家陷塘为对象,筛选出重要值大于1的优势种,结合总体关联性分析、χ²检验、AC联结系数及Spearman秩相关系数对巴家陷塘退化天坑植物群落中11种优势种的种间关联性和相关性进行研究.结果表明: 巴家陷塘退化天坑植物群落种间联结指数VR=1.377>1,总体呈显著正关联,但正负关联差异较大,阳生型植物和阴生型植物呈极显著负关联,现阶段仍具有独立的分布格局,但呈逐渐趋于稳定的趋势;Spearman分析中种间正相关对数(26对)少于种间负相关对数(29对),结合天坑微环境的差异,将退化天坑的优势物种划分为3个生态种组,群落总体呈现出一定的圈层分布规律.     

Depositional facies and cyclic patterns in a subtidal-dominated ramp during the Early-Middle Ordovician in the western Tarim Basin (NW China)

Due to a long-term transgression since the Early Cambrian, an extensive shallow-water carbonate platform was developed in the entire Tarim Basin (NW China). During the deposition of the Yingshan Formation (Early-Middle Ordovician), a carbonate ramp system was formed in the intrashelf basin in the Bachu-Keping area of the western basin. Four well-exposed outcrop sections were selected to investigate their depositional facies, cycles, and sequences, as well as the depositional evolution. Detailed facies analyses permit the recognition of three depositional facies associations, including peritidal, semi-restricted subtidal, and open-marine subtidal facies, and eleven types of lithofacies. These are vertically arranged into meter-scale, shallowing-upward peritidal, semi-restricted subtidal, and open-marine subtidal cycles, in the span of Milankovitch frequency bands, suggesting a dominant control of Earth’s orbital forcing on the cyclic sedimentation on the platform. On the basis of vertical facies (or lithofacies) and cycle stacking patterns, as well as accommodation changes illustrated graphically by Fischer plots at all studied sections, six third-order depositional sequences are recognized and consist of lower transgressive and upper regressive parts. In shallow depositional settings, the transgressive packages are dominated by thicker-than-average, shallow subtidal cycles, whereas the regressive parts are mainly represented by thinner-than-average, relatively shallow subtidal to peritidal cycles. In relatively deep environments, however, the transgressive and regressive successions display the opposite trends of cycle stacking patterns, i.e., thinner-than-average subtidal cycles of transgressive packages. Sequence boundaries are mainly characterized by laterally traceable, transitional zones without apparent subaerial exposure features. Good correlation of the long-term changes in accommodation space inferred from vertical facies and cycle stacking patterns with sea-level fluctuations elsewhere around the world suggests an overriding eustatic control on cycle origination, platform building-up and evolution during the Early-Middle Ordovician, although with localized influences of syndepositional faulting and depositional settings.