不同大豆连作年限对黑土细菌群落结构的影响

大豆连作导致作物产量下降、病原微生物富集和土壤退化等问题日趋严重。然而,目前关于大豆连作对土壤细菌群落结构组成及多样性分布的影响及发生机制尚不清楚。采用高通量测序技术,对大豆连作(不同年限)和大豆-玉米轮作下的黑土细菌16S rRNA基因进行测序分析。结果表明:轮作5年(CR5)和13年长期连作(CC13)处理显著增加了土壤pH、全氮(TN)、全磷(TP)和速效养分(AN、AP和AK)含量。与短期连作相比,CR5和CC13处理均提高了细菌群落的OTUs数量、PD值、Chao1指数和Shannon指数。聚类分析图谱结果显示细菌群落结构组成受到轮作和连作年限的双重影响,而土壤pH、TN、TP、AN、AP和AK是细菌群落结构发生变化的主要驱动因子(P0.05)。此外,VPA分析发现上述土壤因子中,土壤pH对细菌群落结构变化的贡献度最大。本研究证明大豆长期连作提高了土壤养分含量和细菌群落的丰富度和多样性指数,从分子生物学的角度证实大豆长期连作在一定程度上改善了土壤环境,为大豆连作障碍的研究提供了理论依据。     

超声心动图与血浆BNP、和肽素、hs-CRP对慢性心力衰竭患者心功能的评估价值分析

目的:研究超声心动图与血浆脑钠肽(BNP)、和肽素及超敏C反应蛋白(hs-CRP)对慢性心力衰竭(CHF)患者心功能的评估价值。方法:将我院从2017年3月～2020年3月收治的100例CHF患者纳入研究。将其按照美国纽约心脏病协会(NYHA)分级标准分成Ⅰ级33例,Ⅱ级21例,Ⅲ级25例,Ⅳ级21例。对所有患者均进行超声心动图检查,分析相关参数的差异。检测并对比所有患者血浆BNP、和肽素以及hs-CRP水平。采用Pearson相关性分析超声心动图相关参数与血浆BNP、和肽素及hs-CRP水平的关系。结果:心功能分级Ⅰ～Ⅳ级患者的左室射血分数(LVEF)呈逐渐降低趋势,而左房内径(LAD)及左室舒张末期内径(LVEDD)均呈逐渐升高趋势(P0.05),血浆BNP、和肽素及hs-CRP水平均呈逐渐升高趋势(P0.05)。经Pearson相关性分析可得:CHF患者LVEF与血浆BNP、和肽素及hs-CRP均呈负相关(r=-0.621、-0.534、-0.635,P0.05),而LAD、LVEDD与血浆BNP、和肽素及hs-CRP均呈正相关(r=0.582、0.602、0.511,r=0.547、0.592、0.615,P0.05)。结论:超声心动图及血浆BNP、和肽素、hs-CRP用于评估CHF患者心功能均效果显著,且联合检测具有协同互补的作用,实现对CHF患者病情严重程度更为精准的评估。     

荷叶离褶伞子实体化学成分

本文对祁连山野生荷叶离褶伞Lyophyllum decastes子实体的化学成分和生物活性进行研究。采用硅胶色谱、高效液相色谱等多种方法进行分离纯化得到8个化合物,通过MS、NMR和电子圆二色谱 （ECD）等方法确定了化学结构,其中有4个为聚炔类化合物。化合物1作为天然产物系首次报道,其相绝对构型是通过比较ECD的方法确定。对所得聚炔类化合物应用细胞模型进行抗氧化活性（CAA）指标检测,化合物1-4均呈现一定抗氧化活性,其中化合物1的抗氧化活性最强,其EC₅₀为(24.73±6.12)μmol/L。聚炔类化合物1-4为荷叶离褶伞首次报道成分,可作为祁连山野生荷叶离褶伞HPLC-DAD化学表征参考化合物。     

挂榜山小鲵早期胚胎发育初步观察

2005年1～2月,在Nikon体视镜下对挂榜山小鲵的早期胚胎发育过程进行了观察,对不同发育时期进行了数码拍照。根据胚胎发育的外部形态及典型特征将挂榜山小鲵早期胚胎发育过程分为21个时期。在水温6．5～10℃的条件下,受精卵历时1134h孵化出膜,初孵幼鲵全长约16．50mm。     

关于三氧化二砷（As2O3）联合药物治疗肝癌的研究进展

实验与临床研究已证实,As2O3能有效治疗急性早幼粒细胞性白血病（APL）。在此基础上．As2O3抗肝癌作用的研究报告日益增多。研究表明As2O3的抗肝癌效力呈剂量一时间效应关系,但作用时间越长及药物浓度越大,As2O3的毒副作用越大。为实现As2O3低毒高效的抗肿瘤目的,联合用药引起关注。本文通过查阅94年至今国内外有关As2O3药物联合治疗肝癌的文献,对As2O3联合药物治疗肝癌予以综述。     

过表达热休克蛋白70提高CHO细胞表达抗体的能力

通过在中国仓鼠卵巢细胞(CHO)中过表达热休克蛋白70以提高其表达抗体的能力。首先从中国仓鼠基因组DNA中扩取HSP70基因,构建真核表达质粒pcDNA3.1-HSP70,再将重组质粒稳定转染到CHO/dhfr-细胞中,筛选获得稳定的细胞系,运用RT-qPCR检测和Western blot分析HSP70基因的过表达。在过表达HSP70的CHO细胞组和对照细胞组(转染空载体pcDNA3.1的CHO细胞组)中分别转染表达抗-HBs的质粒,应用ELISA检测两组细胞表达抗-HBs的能力。RT-qPCR结果显示实验组CHO细胞中HSP70基因的表达量明显高于对照组细胞;ELISA检测结果表明过表达HSP70的CHO细胞组抗-HBs表达量高于对照组细胞(P<0.05)。研究揭示HSP70能有效促进细胞内分泌性蛋白的表达。     

闽江河口湿地不同植被带土壤全硅的含量及分布特征

硅是湿地系统元素循环所关注的重要内容之一,土壤全硅的分布特征与湿地土壤-植物系统活跃程度密切相关。于2016年1—12月,以闽江河口鳝鱼滩湿地为研究对象,通过野外原位采样及室内实验分析,对短叶茳芏、短叶茳芏与互花米草交错带、互花米草3种植物类型湿地的土壤全硅含量和储量的变化特征进行观测。结果表明:短叶茳芏、短叶茳芏与互花米草交错带、互花米草湿地土壤全硅的年平均含量依次为197.67、201.21、210.33 mg/g,表现为由陆向海方向逐渐增加的趋势;季节上均呈现秋冬高于春夏的趋势;土壤全硅含量和储量均表现为上部土层(0—30cm)高于下部土层(30—60cm)。经统计分析发现,湿地土壤全硅含量与有机质显著负相关(P<0.05),与含水率和pH有极显著正相关关系(P<0.01)。除短叶茳芏湿地外,其余2种湿地土壤全硅含量与有效硅含量显著负相关(P<0.05)。研究闽江河口湿地不同植被带土壤全硅含量和储量及其分布特征,旨在揭示湿地土壤全硅水平在不同类型湿地植被生长影响下的变化过程,为本研究区的硅素研究补充关键数据。     

Role of the Dinaric Karst (western Balkans) in shaping the phylogeographic structure of the threatened crayfish Austropotamobius torrentium

1. This study examines phylogeography and phylogeny of the threatened stone crayfish, Austropotamobius torrentium, in order to elucidate the role of the Dinaric Karst geology in shaping the evolutionary history and genetic diversity of aquatic fauna in the western Balkans. Mitochondrial 16S rRNA and COI genes were partially sequenced from 188 and 159 crayfish, respectively, sampled from 70 localities. Phylogenetic relationships were reconstructed using four methods of phylogenetic inference. Divergence times between phylogroups were estimated in a Bayesian framework, and their demographic history was examined using neutrality tests and mismatch distribution analysis. 2. Seven geographically localised phylogroups separated by pronounced genetic gaps were found. Five of them have a distribution range within the northern‐central Dinaric (NCD) region, while the remaining two include populations from the southern Balkans (SB) and central and south‐eastern Europe (CSE). The oldest divergence event separated two NCD lineages from the rest of populations in the Late Miocene or Early Pliocene. Divergences amongst the five NCD phylogroups and SB + CSE occurred in the Pliocene. The most recent split separated SB and CSE phylogroups during the Late Pliocene. For both genes, uncorrected pairwise divergences between most of the phylogroups (4.1–8.7% for COI and 1.6–4.8% for 16S rRNA) were of the same range as, or higher than, some of the interspecific distances previously reported for the genus Austropotamobius. 3. Geographically isolated and deeply divergent cryptic monophyletic phylogroups within A. torrentium in the NCD region arose in the course of intensification of Neotectonic movements during the Pliocene and the beginning of the Pleistocene and the development of karstification that has heavily fragmented the palaeohydrography of the area. The results confirm a gradual north–south expansion of stone crayfish during the pre‐Pleistocene that preceded the rapid northward post‐glacial re/colonisation of central Europe (CSE phylogroup) through the Danube drainage. 4. Austropotamobius torrentium comprises morphologically cryptic but molecularly distinct taxa. Considering the relatively small geographical areas they inhabit, the NCD phylogroups of stone crayfish should be given the highest conservation priority.     

Soil inorganic carbon storage pattern in China

Soils with pedogenic carbonate cover about 30% (3.44 × 10⁶ km²) of China, mainly across its arid and semiarid regions in the Northwest. Based on the second national soil survey (1979–1992), total soil inorganic carbon (SIC) storage in China was estimated to be 53.3±6.3 PgC (1 Pg=10¹⁵ g) to the depth investigated to 2 m. Soil inorganic carbon storages were 4.6, 10.6, 11.1, and 20.8 Pg for the depth ranges of 0–0.1, 0.1–0.3, 0.3–0.5, and 0.5–1 m, respectively. Stocks for 0.1, 0.3, 0.5, and 1 m of depth accounted for 8.7%, 28.7%, 49.6%, and 88.9% of total SIC, respectively. In contrast with soil organic carbon (SOC) storage, which is highest under 500–800 mm yr⁻¹ of mean precipitation, SIC storage peaks where mean precipitation is <400 mm yr⁻¹. The amount and vertical distribution of SIC was related to climate and land cover type. Content of SIC in each incremental horizon was positively related with mean annual temperature and negatively related with mean annual precipitation, with the magnitude of SIC content across land cover types showing the following order: desert, grassland >shrubland, cropland >marsh, forest, meadow. Densities of SIC increased generally with depth in all ecosystem types with the exception of deserts and marshes where it peaked in intermediate layers (0.1–0.3 m for first and 0.3–0.5 m for latter). Being an abundant component of soil carbon stocks in China, SIC dynamics and the process involved in its accumulation or loss from soils require a better understanding.