安息香科的系统位置及地理分布

安息香科为柿目的一成员,包括１１个属,为一自然的分类群．它与山茶科很接近,并可能是从它的祖先类群演化而来的．本文分析其形态特征的演化趋势,认为子房上位,花冠裂片覆瓦状排列,雄蕊为花冠裂片两倍,花序圆锥花序为原始性状,而子房下位．花冠裂片镊合状排列,雄蕊与花冠裂片的同数,花序少花或单花为进化性状．安息香属为本科最大的属,形态变异多样化,既具有最原始性状,为本科原始类群代表,同时又有较多进化性状．其他各属可能是以它作为基干演化而来．从分析各属的分布区类型,本科有７属分布于热带地区,但仅有３属真正分布于热带,其余４属分布于亚热带或其边缘地区．因此,安息香科基本上是一个热带科,但不典型,它可能是从古热带山区的亚热带地区演化而来的．根据全科的属和种的统计,有１１属,１５０余种,间断分布于欧亚和美洲两大陆块上,亚洲有１０属,５７种,主要分布于东亚,在这一地区,以我国秦岭和长江以南至南岭以北及华西南种类最丰富,包括有最原始类群和系统演化各阶段类群;热带南美洲有２属８３种,这一带种类虽丰富,但仅２属及缺乏原始类群．因此,我们称东亚为安息香科的分布和分化中心,而热带南美洲为第二分布中心．根据化石记载结合本科现代分布格局,我们     

Notes on three Japanese Agaricales

Three species of Agaricales from Japan are treated here. 1) From the examination of the types and additional specimens,Lyophyllum nigrescens is conspecific withHydropus nigrita from Cuba. 2)Hydropus kansaiensis sp. nov. from Otsu appears close toTrogia mellea from Malaysia. 3)Alnicola lactariolens sp. nov. from Otsu is a distinctive species in this genus because of the purple color of its spore print.This work has been supported by a grant to one of us (H. C.) by the Japanese Society for the Promotion of Science in 1988/89.     

Prediction of individual oxygen uptake on-step transients from frequency responses

Power-oxygen uptake ( ) frequency responses can be used to predict responses to arbitrary exercise intensity patterns. It is still an open question for which range of exercise intensities such computed response patterns yield valid predictions. In the present study, we determined the power- frequency response of nine sports students by means of pseudo-randomised switching between 20 W and 80 W during upright and supine cycle exercise. Starting from a baseline of 20 W each subject also performed sustained step increases to 40 W, 80 W, 120 W, and 160 W in both positions. The individual step responses were then compared with the expected time-courses predicted on the basis of the individual frequency responses. The comparison showed a close agreement for the 20 W–40 W and 20 W–80 W steps in both positions. With larger step amplitudes the kinetics became increasingly slower than the predicted time course in both positions. During additional ramp tests (10 W · 30 s^–1) whole blood lactic acid concentration [1a^–]_b tended to be higher in the supine position at exercise intensities higher than 160 W. The mean power at 4 mmol · 1^–1 [la^–]_b amounted to 234 (SD 32) W and 253 (SD 44) W (P<5%) in the supine and the upright position, respectively. The maximal oxygen uptake relative to body mass was not found to be significantly different [upright, mean 57 (SD 10) ml · (min · kg)^–1;supine, mean 54 (SD 10) ml · (min · kg)]. These findings would suggest that for a range of mild exercise intensities kinetics are not appreciably influenced by the step amplitude or by cardiovascular changes associated with the upright and the supine position.     

Monitoring wetlands in a salinizing landscape: case studies from the Wheatbelt region of Western Australia

Three elements of wetland biodiversity (aquatic invertebrates, waterbirds and overstorey vegetation of the wetland edge) have been monitored since 1998 at Lake Eganu and Paperbark Swamp in the Western Australian Wheatbelt to provide information about the changes occurring in wetland biodiversity in a landscape that is severely affected by dryland salinization. Changes in extent of wetland vegetation since the 1960s were examined using historical aerial photographs and waterbird use of Lake Eganu during the early 1980s was compared with recent waterbird survey results. Lake Eganu, which is within a major drainage line, started to become salinized in the mid-1960s, about 70 years after land clearing began in the catchment, and its salinity has increased an order of magnitude. The extent of wetland overstorey vegetation and the richness of freshwater aquatic invertebrates have both declined about 80%. Waterbird richness has also declined over the past 20 years, with changes in species composition. Salinization has not occurred at Paperbark Swamp, which is in a small catchment off the main drainage line, and there has been no consistent change in the biodiversity elements monitored.     

Significance of ozone exposure for inter-annual differences in primary metabolites of old-growth beech (Fagus sylvatica L.) and Norway spruce (Picea abies L.) trees in a mixed forest stand

The influence of long-term free-air ozone fumigation and canopy position on leaf contents of total glutathione, its redox state, non-structural proteins (NSP), soluble amino compounds, and total soluble sugars in old-growth beech (FAGUS SYLVATICA) and spruce (PICEA ABIES) trees were determined over a period of five years. Ozone fumigation had weak effects on the analysed metabolites of both tree species and significant changes in the contents of total glutathione, NSP, and soluble sugars were observed only selectively. Beech leaves were affected by crown position to a higher extent than spruce needles and exhibited lower contents of total glutathione and NSP and total soluble sugars, but enhanced contents of oxidised glutathione and amino compounds in the shade compared to the sun crown. Contents of total soluble sugars generally were decreased in shade compared to sun needles of spruce trees. Interspecific differences between beech and spruce were more distinct in the sun compared to the shade crown. Contents of total glutathione were increased whilst contents of amino compounds and total soluble sugars were lower in spruce needles compared to beech leaves. The metabolites determined showed individual patterns in the course of the five measurement years. Contents of total glutathione and its redox state correlated with air temperature and global radiation, indicating an important role for the antioxidant at low temperatures. Correlations of glutathione with instantaneous ozone concentrations seem to be a secondary effect. Differences in proteins and/or amino compounds in the inter-annual course are assumed to be a consequence of alterations in specific N uptake rates.     

Increased temperatures may safeguard the nutritional quality of crops under future elevated CO2 concentrations

Iron (Fe) and zinc (Zn) deficiencies are a global human health problem that may worsen by the growth of crops at elevated atmospheric CO₂ concentration (eCO₂). However, climate change will also involve higher temperature, but it is unclear how the combined effect of eCO₂ and higher temperature will affect the nutritional quality of food crops. To begin to address this question, we grew soybean (Glycine max) in a Temperature by Free‐Air CO₂ Enrichment (T‐FACE) experiment in 2014 and 2015 under ambient (400 μmol mol^?1) and elevated (600 μmol mol^?1) CO₂ concentrations, and under ambient and elevated temperatures (+2.7°C day and +3.4°C at night). In our study, eCO₂ significantly decreased Fe concentration in soybean seeds in both seasons (?8.7 and ?7.7%) and Zn concentration in one season (?8.9%), while higher temperature (at ambient CO₂ concentration) had the opposite effect. The combination of eCO₂ with elevated temperature generally restored seed Fe and Zn concentrations to levels obtained under ambient CO₂ and temperature conditions, suggesting that the potential threat to human nutrition by increasing CO₂ concentration may not be realized. In general, seed Fe concentration was negatively correlated with yield, suggesting inherent limitations to increasing seed Fe. In addition, we confirm our previous report that the concentration of seed storage products and several minerals varies with node position at which the seeds developed. Overall, these results demonstrate the complexity of predicting climate change effects on food and nutritional security when various environmental parameters change in an interactive manner.     

SVMyr: A Web Server Detecting Co- and Post-translational Myristoylation in Proteins

Myristoylation (MYR) is a protein modification where a myristoyl group is covalently attached to an exposed (N-terminal) glycine residue. Glycine myristoylation occurs during protein translation (co-translation) or after (post-translation). Myristoylated proteins have a role in signal transduction, apoptosis, and pathogen-mediated processes and their prediction can help in functionally annotating the fraction of proteins undergoing MYR in different proteomes.Here we present SVMyr, a web server allowing the detection of both co- and post-translational myristoylation sites, based on Support Vector Machines (SVM). The input encodes composition and physicochemical features of the octapeptides, known to act as substrates and to physically interact with N-myristoyltransferases (NMTs), the enzymes catalyzing the myristoylation reaction.The method, adopting a cross validation procedure, scores with values of Area Under the Curve (AUC) and Matthews Correlation Coefficient (MCC) of 0.92 and 0.61, respectively. When benchmarked on an independent dataset including experimentally detected 88 medium/high confidence co-translational myristoylation sites and 528 negative examples, SVMyr outperforms available methods, with AUC and MCC equal to 0.91 and 0.58, respectively.A unique feature of SVMyr is the ability to predict post-translational myristoylation sites by coupling the trained SVMs with the detection of caspase cleavage sites, identified by searching regular motifs matching upstream caspase cleavage sites, as reported in literature.Finally, SVMyr confirms 96% of the UniProt set of the electronically annotated myristoylated proteins (31,048) and identifies putative myristoylomes in eight different proteomes, highlighting also new putative NMT substrates.SVMyr is freely available through a user-friendly web server at https://busca.biocomp.unibo.it/lipipred.     

干热河谷区不同坡位土壤水分对降雨的响应特征

研究干热河谷地区土壤水分在降雨过程中的短时动态变化,有助于揭示该地区的土壤水文功能。本研究选取贵州花江干热河谷作为研究区,运用原位监测法,获取不同坡位的高频土壤水分监测数据,分析土壤水分对降雨的短时动态响应特征。结果表明: 在整个监测期间,无论是坡上还是坡中,研究区各层土壤水分均为中等变异水平(15.2%≤变异系数CV≤29.7%),坡上土壤水分的波动幅度(CV=21.1%)大于坡中(CV=19.1%),0～5 cm土层(CV=26.2%)大于20～40 cm土层(CV=16.5%)。与坡中相比,坡上土壤水分对降雨的响应速度更快,降雨对土壤水分的补给量大、补给速率快;坡上的土壤水分补给速率与消退速率之差(2.3%·h^-1)大于坡中(1.8%·h^-1)。随土层深度增加,下层土壤水分对降雨的响应早于或同步于上层,降雨对土壤水分的补给量减少、补给速率减慢,土壤水分的消退速率也减慢。与坡中相比,坡上土壤水分入渗能力更强,保水能力更优。干热河谷的微观环境和小气候影响土壤水分对降雨的响应特征,而岩-土界面优先流的快速补给则会加快下层土壤水分对降雨的响应速度,使得该地区的坡面更容易形成混合产流机制。