有机溶剂对缢蛏碱性磷酸酯酶分子构象和催化活力的影响

本文初步研究了三种有机溶剂甲醇、二甲基甲酰胺、二氧六环对缢蛏碱性磷酸酯酶(ALP)分子构象和催化活力的影响。发现在有机溶剂作用下,ALP的荧光发射光谱、紫外差光谱、园二色光谱都发生了显著的变化,而酶经甲醇、二甲基甲酰胺预处理后酶活力提高,经二氧六环预处理后活力下降,但当测活体系中有三种有机溶剂存在时,酶的活力却被大大抑制。     

钙调蛋白的自旋共振研究:拮抗剂和它的相互作用

利用碘乙酰胺氮氧自由基标记钙调蛋白研究了它与三氟拉嗪(TFP)、酸枣仁皂甙A(JuA)的相互作用。结果表明,每分子CaM分别至少可以结合两分子的TFP及JuA,它们的作用影响了CaM上的Met残基(主要是71,72和76)的环境,使反应自由基运动自由度的旋转相关时间τR值下降。据τR变化的趋势,推测TFP和JuA都是通过疏水作用结合到CaM上的疏水沟区,但两者的结合位点可能不同。     

Carbon uptake in Eurasian boreal forests dominates the high-latitude net ecosystem carbon budget

Arctic-boreal landscapes are experiencing profound warming, along with changes in ecosystem moisture status and disturbance from fire. This region is of global importance in terms of carbon feedbacks to climate, yet the sign (sink or source) and magnitude of the Arctic-boreal carbon budget within recent years remains highly uncertain. Here, we provide new estimates of recent (2003–2015) vegetation gross primary productivity (GPP), ecosystem respiration (R_eco), net ecosystem CO₂ exchange (NEE; R_eco − GPP), and terrestrial methane (CH₄) emissions for the Arctic-boreal zone using a satellite data-driven process-model for northern ecosystems (TCFM-Arctic), calibrated and evaluated using measurements from >60 tower eddy covariance (EC) sites. We used TCFM-Arctic to obtain daily 1-km² flux estimates and annual carbon budgets for the pan-Arctic-boreal region. Across the domain, the model indicated an overall average NEE sink of −850 Tg CO₂-C year⁻¹. Eurasian boreal zones, especially those in Siberia, contributed to a majority of the net sink. In contrast, the tundra biome was relatively carbon neutral (ranging from small sink to source). Regional CH₄ emissions from tundra and boreal wetlands (not accounting for aquatic CH₄) were estimated at 35 Tg CH₄-C year⁻¹. Accounting for additional emissions from open water aquatic bodies and from fire, using available estimates from the literature, reduced the total regional NEE sink by 21% and shifted many far northern tundra landscapes, and some boreal forests, to a net carbon source. This assessment, based on in situ observations and models, improves our understanding of the high-latitude carbon status and also indicates a continued need for integrated site-to-regional assessments to monitor the vulnerability of these ecosystems to climate change.     

Hyposensitive canopy conductance renders ecosystems vulnerable to meteorological droughts

Increased meteorological drought intensity with rising atmospheric demand for water (hereafter vapor pressure deficit [VPD]) increases the risk of tree mortality and ecosystem dysfunction worldwide. Ecosystem-scale water-use strategy is increasingly recognized as a key factor in regulating drought-related ecosystem responses. However, the link between water-use strategy and ecosystem vulnerability to meteorological droughts is poorly established. Using the global flux observations, historic hydroclimatic data, remote-sensing products, and plant functional-trait archive, we identified potentially vulnerable ecosystems, examining how ecosystem water-use strategy, quantified by the percentage bias (δ) of the empirical canopy conductance sensitivity to VPD relative to the theoretical value, mediated ecosystem responses to droughts. We found that prevailing soil water availability substantially impacted δ in dryland regions where ecosystems with insufficient soil moisture usually showed conservative water-use strategy, while ecosystems in humid regions exhibited more pronounced climatic adaptability. Hyposensitive and hypersensitive ecosystems, classified based on δ falling below or above the theoretical sensitivity, respectively, achieved similar net ecosystem productivity during droughts, employing different structural and functional strategies. However, hyposensitive ecosystems, risking their hydraulic system with a permissive water-use strategy, were unable to recover from droughts as quickly as hypersensitive ones. Our findings highlight that processed-based models predicting current functions and future performance of vegetation should account for the greater vulnerability of hyposensitive ecosystems to intensifying atmospheric and soil droughts.     

结晶麦胚凝集素的制备及其性质研究

<正> 1963年,Aub 等人发现麦胚脂酶具有凝集肿瘤细胞能力。Nagata等人用离子交换色谱法由麦胚脂酶制备出麦胚凝集素,而后经两次结晶,获得结晶麦胚凝集素(Crystalline wheat germ ag glutinin,CWGA)。本文采用亲和层析法由麦胚直接制得CWGA。CWGA经7.5％PAGE检测为一条谱带、SDS-PAGE检测表现分子量18,6kD,其等电点pH6.2,对2％A型人红细胞最低凝集浓度为4μg/mL。     

Litter and soil biodiversity jointly drive ecosystem functions

The decomposition of litter and the supply of nutrients into and from the soil are two fundamental processes through which the above- and belowground world interact. Microbial biodiversity, and especially that of decomposers, plays a key role in these processes by helping litter decomposition. Yet the relative contribution of litter diversity and soil biodiversity in supporting multiple ecosystem services remains virtually unknown. Here we conducted a mesocosm experiment where leaf litter and soil biodiversity were manipulated to investigate their influence on plant productivity, litter decomposition, soil respiration, and enzymatic activity in the littersphere. We showed that both leaf litter diversity and soil microbial diversity (richness and community composition) independently contributed to explain multiple ecosystem functions. Fungal saprobes community composition was especially important for supporting ecosystem multifunctionality (EMF), plant production, litter decomposition, and activity of soil phosphatase when compared with bacteria or other fungal functional groups and litter species richness. Moreover, leaf litter diversity and soil microbial diversity exerted previously undescribed and significantly interactive effects on EMF and multiple individual ecosystem functions, such as litter decomposition and plant production. Together, our work provides experimental evidence supporting the independent and interactive roles of litter and belowground soil biodiversity to maintain ecosystem functions and multiple services.     

Accelerated organic matter decomposition in thermokarst lakes upon carbon and phosphorus inputs

Mineralization of dissolved organic matter (DOM) in thermokarst lakes plays a non-negligible role in the permafrost carbon (C) cycle, but remains poorly understood due to its complex interactions with external C and nutrient inputs (i.e., aquatic priming and nutrient effects). Based on large-scale lake sampling and laboratory incubations, in combination with ¹³C-stable-isotope labeling, optical spectroscopy, and high-throughput sequencing, we examined large-scale patterns and dominant drivers of priming and nutrient effects of DOM biodegradation across 30 thermokarst lakes along a 1100-km transect on the Tibetan Plateau. We observed that labile C and phosphorus (P) rather than nitrogen (N) inputs stimulated DOM biodegradation, with the priming and P effects being 172% and 451% over unamended control, respectively. We also detected significant interactive effects of labile C and nutrient supply on DOM biodegradation, with the combined labile C and nutrient additions inducing stronger microbial mineralization than C or nutrient treatment alone, illustrating that microbial activity in alpine thermokarst lakes is co-limited by both C and nutrients. We further found that the aquatic priming was mainly driven by DOM quality, with the priming intensity increasing with DOM recalcitrance, reflecting the limitation of external C as energy sources for microbial activity. Greater priming intensity was also associated with higher community-level ribosomal RNA gene operon (rrn) copy number and bacterial diversity as well as increased background soluble reactive P concentration. In contrast, the P effect decreased with DOM recalcitrance as well as with background soluble reactive P and ammonium concentrations, revealing the declining importance of P availability in mediating DOM biodegradation with enhanced C limitation but reduced nutrient limitation. Overall, the stimulation of external C and P inputs on DOM biodegradation in thermokarst lakes would amplify C-climate feedback in this alpine permafrost region.     

异叶三宝木的二萜成分及抗菌活性研究

为研究异叶三宝木(Trigonostemon heterophyllus)的二萜成分及其抗菌活性,采用硅胶柱层析、凝胶柱层析、高效液相色谱对萃取物进行分离纯化,结合现代波谱技术对所得化合物进行结构鉴定,并通过牛津杯法和2倍稀释法检测化合物对革兰氏阴性菌大肠杆菌(Escherichia coli)以及革兰氏阳性菌肺炎双球菌(Pneumococcus)的生长抑制活性和MIC值。从异叶三宝木中分离得到了6个化合物,包括5个二萜类, 1个木脂素类,分别鉴定为trigonochinene E (1)、neoboutomannin (2)、6,9-O- dedimethyltrigonostemone (3)、stelltian B (4)、3,4-secosonderianol (5)、biondinin A (6)。化合物1、2、3、5对大肠杆菌有抑制作用,MIC值分别为9.375、18.75、18.75、18.75 μg/mL。化合物2、3、4、6为首次从该种植物中分离得到,化合物4为首次从该属植物中分离得到。除化合物4外,其他化合物都有一定的抗菌活性,且化合物1、2、3对大肠杆菌抑制作用强于阳性对照硫酸卡那霉素。     

芝麻病毒病害研究：Ⅱ.芝麻黄花叶病病原鉴定

继对芝麻矮化坏死病源研究之后,又对普遍发生的芝麻黄花叶病害分离物(YMo—I)进行了系统鉴定。该分离物普遍存在于各芝麻主产区,普通年份发病率为1～5％。YMo—I侵染芝麻引起叶片褪绿及黄绿相间花叶。摩擦接种能够侵染4科12种(品种)植物。局部侵染苋色藜、昆诺藜;系统侵染大豆、花生、望江南、克氏烟等。该病毒能够由桃蚜、花生蚜、大豆蚜以非持久性方式进行传播。ELISA检测其病株种子带毒率为0.5％,但尚未发现种生病苗。病毒在组织汁液中存活期3天;钝化温度55～60℃,稀释限点4×10~(-3)。提纯病毒为弯曲线状粒体,大小约为13×730nm。并有极易凝聚的趋势。病组织中诱导大量典型PVY第一亚组的风轮形和卷筒状细胞质内含体和少数多边形结晶核内含体。血清学上该病毒与花生条纹病毒(PStV)、西瓜花叶病毒—2(MMV—2)密切相关,与花生斑驳病毒、大豆花叶病毒弱相关;与芜菁花叶病毒不相关。但它不侵染WMV—2的寄主—黄瓜,并且该病害田间的发生流行与芝麻、花生的间作方式以及PStV在花生田间的流行密切相关。根据上述结果,YMo—I分离株被鉴定为花生条纹病毒的一芝麻分离株。     

石菖蒲中一新倍半萜

石菖蒲（Acorus gramineus Soland）的精油经GC/MS/DS检测,硅胶加压柱层分离,得到一新的倍半萜,其在精油中的含量达60.30％,通过波谱方法确定了结构,并命名为石菖蒲酮（gramenone）。