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1.
【背景】昆虫是世界上种类最多、肠道菌群资源最丰富且多样的动物类群之一。昆虫肠道微生物具有产生活性次级代谢产物的能力,是活性天然产物的重要来源。【目的】研究药用昆虫喙尾琵琶甲(Blaps rynchopetera)成虫肠道来源链霉菌(Streptomyces sp.) BPA71的次级代谢产物及其生物活性。【方法】利用正相硅胶柱色谱、葡聚糖凝胶Sephadex LH-20柱色谱等方法分离纯化该菌株的发酵粗提物,采用牛津杯法进行抗菌活性追踪,确定抗菌活性部位,通过ESI-MS、NMR等波谱数据分析对化合物结构进行鉴定,采用微量肉汤稀释法测定最低抑菌浓度(minimal inhibitory concentration, MIC),采用MTS法测定抗肿瘤活性。【结果】从Streptomyces sp. BPA71的固体发酵提取物中共分离得到4个已知化合物,通过对比核磁数据确定为糠酸甲酯(1)、吡咯甲酰胺A (2)、吡咯甲酰胺B (3)和吲哚-3-乙酸甲酯(4)。抗菌活性结果显示化合物2具有广谱抗菌活性。此外,化合物2对宫颈癌细胞HeLa、肺癌细胞A549、肝癌细胞SMMC-7721、乳腺癌细胞MDA-MB-231和结肠癌细胞SW480这5株肿瘤细胞均有明显的抑制活性。【结论】喙尾琵琶甲肠道来源Streptomyces sp. BPA71可产生丰富的生物活性物质,该研究结果为进一步挖掘喙尾琵琶甲肠道链霉菌的活性天然产物奠定了基础,同时丰富了人们对喙尾琵琶甲肠道微生物的认识。 相似文献
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泥炭地是主要的甲烷(CH4)排放源,甲烷循环过程对水位变化响应敏感。研究选取两块具有水位差异的泥炭地土壤,通过厌氧培养实验探究水位变化对泥炭地甲烷产生和甲烷厌氧氧化(Methane Anaerobic Oxidation,AOM)潜势的影响,并分析影响其潜势大小的生物地球化学因子。结果显示,高水位泥炭地(0 cm) CH4产生累积量为(0.89±0.01)μg/g,要显著高于低水位(-30 cm:(0.70±0.03)μg/g)泥炭地甲烷产生量,但低水位AOM累积量要显著高于高水位泥炭地(0 cm:(2829.93±35.99)μg/g),低水位泥炭地AOM量为(3588.06±24.78)μg/g。通过相关性分析发现甲烷产生潜势与含水量和DOC具有显著相关性,AOM潜势与含水量、pH、DOC具有显著相关性,含水量和DOC是影响若尔盖泥炭地甲烷产生及AOM潜势大小的重要因子。此外,发现高水位泥炭地甲烷产生潜势对温度升高的响应较为明显,特别是表层土壤(0-20 cm)。本研究明确了水位变化对若尔盖泥炭地甲烷产生及AOM潜势的影响特征,估算了全国泥炭地甲烷产生及AOM潜势的大小,以期为减缓全球气候变暖提供一定的理论支撑。 相似文献
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Dongxin Zhao Zhongxian Huang Jie Liu Li Ma Juan He 《Preparative biochemistry & biotechnology》2013,43(10):914-919
AbstractZinc finger protein ZNF191(243–368), the zinc finger region of ZNF191, is potentially associated with cell proliferation in hepatocellular carninoma. A His-tag expression system was used to express and purify proteins with mutations in the zinc finger 3 of ZNF191(243–368) for analysis of protein properties, structure, and functions. The purification of the His-tag fusion proteins was simpler and faster than that of the ZNF191(243–368) inclusion bodies. The properties and structures of the His-tag fusion mutant proteins were investigated using spectrographic techniques and DNA hydrolysis experiment. The His6-tag system could be used to express ZNF191(243–368). The presence of the His6-tag at the N-terminus of ZNF191(243–368) did not evidently affect its properties and structure. However, the site-directed mutations in zinc finger 3 affected the structure of the protein. The DNA hydrolase activity of His6-ZF-F3/H4 suggested that four histidines in zinc finger 3 might form a structure similar to that of the active center in a hydrolase. This work reports that continuous histidines need to form a certain structure for specific functions, and provides new insights into the design of an artificial nuclease. 相似文献
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Huai Chen Qiuan Zhu Changhui Peng Ning Wu Yanfen Wang Xiuqing Fang Yongheng Gao Dan Zhu Gang Yang Jianqing Tian Xiaoming Kang Shilong Piao Hua Ouyang Wenhua Xiang Zhibin Luo Hong Jiang Xingzhang Song Yao Zhang Guirui Yu Xinquan Zhao Peng Gong Tandong Yao Jianghua Wu 《Global Change Biology》2013,19(10):2940-2955
With a pace of about twice the observed rate of global warming, the temperature on the Qinghai‐Tibetan Plateau (Earth's ‘third pole’) has increased by 0.2 °C per decade over the past 50 years, which results in significant permafrost thawing and glacier retreat. Our review suggested that warming enhanced net primary production and soil respiration, decreased methane (CH4) emissions from wetlands and increased CH4 consumption of meadows, but might increase CH4 emissions from lakes. Warming‐induced permafrost thawing and glaciers melting would also result in substantial emission of old carbon dioxide (CO2) and CH4. Nitrous oxide (N2O) emission was not stimulated by warming itself, but might be slightly enhanced by wetting. However, there are many uncertainties in such biogeochemical cycles under climate change. Human activities (e.g. grazing, land cover changes) further modified the biogeochemical cycles and amplified such uncertainties on the plateau. If the projected warming and wetting continues, the future biogeochemical cycles will be more complicated. So facing research in this field is an ongoing challenge of integrating field observations with process‐based ecosystem models to predict the impacts of future climate change and human activities at various temporal and spatial scales. To reduce the uncertainties and to improve the precision of the predictions of the impacts of climate change and human activities on biogeochemical cycles, efforts should focus on conducting more field observation studies, integrating data within improved models, and developing new knowledge about coupling among carbon, nitrogen, and phosphorus biogeochemical cycles as well as about the role of microbes in these cycles. 相似文献
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Xiaoju He Yinyan He Binrong Xi Jiusheng Zheng Xiaoming Zeng Qinhua Cai Yu OuYang Chen Wang Xiaofei Zhou Huiying Huang Wei Deng Siming Xin Qixiang Huang Huai Liu 《PloS one》2013,8(11)