瑞香狼毒根的抑菌活性研究（Ⅰ）

以苹果干腐病菌、小麦赤霉病菌、番茄早疫病菌、南瓜枯萎病菌、玉米大斑病菌、烟草赤星病菌和辣椒疫霉病菌为供试菌,采用生物活性跟踪法、生长速率测定法和系统溶剂提取法对瑞香狼毒根中的杀菌活性物质进行了筛选和分离。结果表明,杀菌活性物质主要集中在乙酸乙酯提取物和甲醇粗提物中。从乙酸乙酯提取物中分离出两种杀菌活性物质AF1-4和AF1-5,同时还发现瑞香狼毒根中还存在增菌物质。     

湖北第二批国家珍稀濒危保护植物

本文经调查记述了湖北第二批国家重点保护植物16种,分属12科16属,可为我省珍稀濒危植物资源的保护及合理利用提供参考。     

水氮互作对冬小麦田氨挥发损失和产量的影响

2015-2017年利用水肥渗漏研究池,以‘石麦15’(SM15)为材料,采用随机区组设计,设置2个氮肥类型(尿素和有机肥牛粪)、2个施氮水平(180和90 kg·hm^-2)、2个灌溉水平(500和250 mm)进行试验,探讨水、氮及其互作对冬小麦田土壤氨挥发损失量和籽粒产量的影响.结果表明: 施肥以后土壤氨挥发持续7 d左右.2015-2016年施肥后各处理土壤氨挥发损失总量为13.36～46.04 kg·hm^-2,氨挥发氮肥损失率为8.9%～41.1%,2016-2017年各处理土壤氨挥发损失总量为14.78～52.99 kg·hm^-2,氨挥发氮肥损失率为9.2%～45.8%;两年试验内氨挥发损失量最多的处理为W₂U₁(施尿素N 180 kg·hm^-2,灌溉量250 mm),氨挥发损失率最高的处理为W₂U₂(施尿素N 90 kg·hm^-2,灌溉量250 mm),合理的水氮管理可以显著降低土壤氨挥发损失率,施用尿素造成的土壤氨挥发损失为有机肥的2～3倍.两年试验均以W₁M₁(施牛粪N 180 kg·hm^-2,灌溉量500 mm)的小麦产量最高,灌溉量、肥料类型和施氮量互作对冬小麦产量影响极显著.综合氨挥发损失量和冬小麦籽粒产量,本试验条件下,水氮互作效应显著,冬小麦生育期内总灌溉量500 mm、施有机肥180 kg·hm^-2时冬小麦季土壤氨挥发损失率较低,产量最高,施用有机肥的增产效果优于尿素,可作为黄淮海地区冬小麦实际生产中增产增效的水肥优化管理方式.     

Distribution patterns of ammonia-oxidizing archaea and bacteria in sediments of the eastern China marginal seas

Ammonia-oxidizing archaea (AOA) and bacteria (AOB) vary in their contribution to nitrification in different environments. The eastern China marginal seas (ECMS) are featured by complex river runoffs and ocean currents, forming different sediment patches. Here, via quantitative PCR and clone library analysis of the amoA genes, we showed that AOB were more abundant than AOA in ECMS sediments. The abundance, diversity and richness of AOA, but not AOB, were higher in the East China Sea (ECS) than in the Yellow Sea (YS) and Bohai Sea (BS). Nitrosopumilus (AOA) and Nitrosospira (AOB) were predominant lineages, but their abundances varied significantly between ECS, and BS and YS. This was mainly attributed to salinity and dissolved oxygen of the bottom water. The discovery of a high abundance of Nitrosophaera at estuarine sites suggested strong terrigenous influence exerted on the AOA community. In contrast, variations in ocean conditions played more important roles in structuring the AOB community, which was separated by bottom water dissolved oxygen into two groups: the south YS, and the north YS and BS. This study provides a comprehensive insight into the spatial distribution pattern of ammonia-oxidizing prokaryotes in ECMS sediments, laying a foundation for understanding their relative roles in nitrification.     

Screening of high α-arbutin producing strains and production of α-arbutin by fermentation

A mutant Xanthomonas maltophilia BT-112 with high α-anomer-selective glycosylation activity was screened by a series of mutation methods including UV light, N-methyl-N-nitro-N-nitroso-guanidine treatment and quick neutron mutation. The α-arbutin titer increased 15-folds compared with the parent strain. The optimal conditions for culture medium and the operational conditions for lab-scale fermenter were investigated. Under optimized conditions, the maximal hydroquinone (HQ) tolerance of cells and yield of α-arbutin were 120 mM and 30.6 g/l, respectively. The molar conversion yield of α-arbutin based on the amount of HQ supplied reached 93.6 %. The product was identified as α-arbutin by ¹³C NMR and ¹H NMR analysis. In conclusion, the results in this work provide a one-step and cost-effective method for the large-scale production of α-arbutin.     

High-resolution crystal structure reveals a HEPN domain at the C-terminal region of S. cerevisiae RNA endonuclease Swt1

Swt1 is an RNA endonuclease that plays an important role in quality control of nuclear messenger ribonucleoprotein particles (mRNPs) in eukaryotes; however, its structural details remain to be elucidated. Here, we report the crystal structure of the C-terminal (CT) domain of Swt1 from Saccharomyces cerevisiae, which shares common characteristics of higher eukaryotes and prokaryotes nucleotide binding (HEPN) domain superfamily. To study in detail the full-length protein structure, we analyzed the low-resolution architecture of Swt1 in solution using small angle X-ray scattering (SAXS) method. Both the CT domain and middle domain exhibited a good fit upon superimposing onto the molecular envelope of Swt1. Our study provides the necessary structural information for detailed analysis of the functional role of Swt1, and its importance in the process of nuclear mRNP surveillance.     

南洋臀纹粉蚧雌成虫主要器官及其蜡泌物的扫描电镜观察

为明确南洋臀纹粉蚧Planococcus lilacinus(Cockerell)雌成虫及其蜡泌物的结构特征,利用扫描电镜观察该虫体表主要器官、蜡质及泌蜡腺体的超微结构.结果表明:南洋臀纹粉蚧雌成虫外覆白色粉状厚蜡被,体缘具18对蜡棒,触角8节、口器和足发达且分布有不同长度的毛形和刺形感受器,眼为单眼,腹脐和背孔唇形、...     

Rainfall manipulation experiments as simulated by terrestrial biosphere models: Where do we stand?

Changes in rainfall amounts and patterns have been observed and are expected to continue in the near future with potentially significant ecological and societal consequences. Modelling vegetation responses to changes in rainfall is thus crucial to project water and carbon cycles in the future. In this study, we present the results of a new model‐data intercomparison project, where we tested the ability of 10 terrestrial biosphere models to reproduce the observed sensitivity of ecosystem productivity to rainfall changes at 10 sites across the globe, in nine of which, rainfall exclusion and/or irrigation experiments had been performed. The key results are as follows: (a) Inter‐model variation is generally large and model agreement varies with timescales. In severely water‐limited sites, models only agree on the interannual variability of evapotranspiration and to a smaller extent on gross primary productivity. In more mesic sites, model agreement for both water and carbon fluxes is typically higher on fine (daily–monthly) timescales and reduces on longer (seasonal–annual) scales. (b) Models on average overestimate the relationship between ecosystem productivity and mean rainfall amounts across sites (in space) and have a low capacity in reproducing the temporal (interannual) sensitivity of vegetation productivity to annual rainfall at a given site, even though observation uncertainty is comparable to inter‐model variability. (c) Most models reproduced the sign of the observed patterns in productivity changes in rainfall manipulation experiments but had a low capacity in reproducing the observed magnitude of productivity changes. Models better reproduced the observed productivity responses due to rainfall exclusion than addition. (d) All models attribute ecosystem productivity changes to the intensity of vegetation stress and peak leaf area, whereas the impact of the change in growing season length is negligible. The relative contribution of the peak leaf area and vegetation stress intensity was highly variable among models.