广东种子植物区系地理成分研究

广东种子植物区系共有２１９科１４３４属４９８６种。其中：①热带区系成分占有较大的比例,约占非世界属的６２．３％,表明广东区系受到热带区系的强烈渗透,次之为亚热带（至亚热带山地）成分约占３２．２％,及中国特有分布占５．６％;②以单型属（７２属）,单种属（５８５属）和寡种属（５６２属）占绝对优势,共占８５．０％,充分显示了广东区系的古老性和过渡性特点;③从区系组成和植被结构的特征成分来看,以华夏植物区系成分为主,包括：亚热带分布,亚热带山地分布,中国特有分布,东亚—北美间断分布,及一些亚洲热带分布中以亚热带为主的属：④在这些属中有东亚特有属１３２属,中国特有属７５属以及华南—西南—中南半岛特有属６８属等;这些属的存在毫无疑问地说明,广东区系是华夏植物区系的核心地区之一,同时也显示了热带区系与亚热带区系有着不可分隔的统一性。     

河南金岗台山区的植被及其垂直分布

根据样方中的种类统计,组成金岗台山区植被的种子植物计有１０５科,３４９属,５６６种;其区系特征为：地理成分复杂,有１４个分布区类型;温带区系特征较为明显,其成分占４２．２％,热带成分占３３．６％;且有一定的古老和特有成分。植被的生活型谱为高位芽植物占３９．６％,地面芽植物占３１．４％,地上芽植物占１０％,地下芽植物占１２％,一年生植物占７％。主要植被类型计有５个植被型,５个植被亚型和３９个群系。垂     

中国珍稀濒危植物—栌菊木区系性质的评价

栌菊木是菊科的单型属。Ｎｏｕｅｌｉａｉｎｓｉｇｎｉｓ是中国特有的珍稀濒危植物,分布于北纬２４°－３０°和东经９９°４０′－１０３°５０′的康滇地区。关于它的起源和区系性质,许多作者都进行过研究。本文分析了分布区的历史及栌菊木与近缘属Ｇｏｃｈｎａｔｉａ的系统关系,得出结果为：１．栌菊木是康滇地区的特有属,而非金沙江河谷特有;２．它是一个生存在亚热带气候环境中的温带成分,但非热带成分;３．其起源地应是康滇古陆的南部──滇中高原,而不是古地中海地域;４．起源时间大约在中新世末或更晚,当时气候条件与现代滇中地区相似。综上所述：栌菊木是一个（起源于晚第三纪）比较年青的属,并不是起源古老的区系成分。     

贡嘎山东坡植物区系的垂直分布格局

为了探讨贡嘎山植物区系的垂直分化特征及其与周边地区植物区系的联系,结合样带法与样方法,对贡嘎山东坡垂直植被带进行了调查,统计得出各垂直植被带的科、属的物种数量,分析了科、属、种级区系成分的构成及其沿海拔梯度的分布格局,并对各垂直植被带区系的相似性进行了聚类分析。结果表明：1)贡嘎山植物区系在整体上具有温带性质,但在干旱河谷地带,热带和温带区系成分的比例相当：热带成分的构成和分布反映古热带和古地中海区系的残遗性影响;2)东亚(含亚型)和东亚-北美成分对贡嘎山中部森林植物区系的影响最大,这些成分以温带古老性质为主;3)北温带成分是贡嘎山植物区系的主体之一,对青藏高原隆升以来贡嘎山植物区系进化类群和特有成分的发展有主要贡献,代表区系的年轻组分;4)中国特有种类型多样,占不同垂直植被带物种数量的40％-65％,其比例随海拔上升而增大。各类型比例的垂直变化突出反映了贡嘎山及横断山脉中海拔地段的植物区系与华中地区的联系,以及高海拔地段与青藏高原及东喜马拉雅的区系之间的联系。本文还就贡嘎山在生物地理分布上的意义以及贡嘎山和横断山脉植物区系特有性的性质进行了讨论。     

元谋干热河谷植物区系研究

元谋是我国著名的干热河谷之一。在元谋干热河谷1600米以下的山坡上主要分布着稀树灌草丛植被。经研究计有种子植物78科、266属、399种,其中绝大部分为草本和灌木种类。从种子植物的地理成分分析这里的区系成分带有明显的热带性质,其中出现在元谋的热带属占属总数(不包括世界分布属)的72.3％,温带分布属占26.4％,中国特有分布属占1.3％。这里的区系成分除了与其所处的滇中高原邻近地区关系很密切外,与印度等地的稀树草原也有联系,表现出了区系成分的古老联系和稀树草原植被的残余性。     

西北地区木本植物区系多样性研究

西北地区在中国植物区系上属于泛北极植物区,其南部基本上控制在中国-日本植物亚区的华中地区内,区系成分以北亚热带成分占优势,中、东部主要控制在中国-日本植物亚区内的华北地区中的黄土高原地区内,以华北区系成分占优势,西南部主要属青藏高原植物亚区和中国-喜马拉雅植物亚区,区系成分以唐古特和横断山区系成分占优势,北部主要是亚洲荒漠植物亚区,区系成分是以古地中海成分占优势。本区有木本植物(不包括栽培植物)103科338属1729种(含种下等级),其中裸子植物6科17属57种,被子植物97科321属1672种,另外,具有中国特有属26个,土著特有种173个(含种下等级)。大科、大属在区系组成中起着非常重要的作用,该区木本植物区系包含有15个分布区类型及其17个变型,其中北温带分布、泛热带分布、东亚至北美间断分布、东亚分布等成分占有重要地位。其木本植物区系的主要特征为:种类比较丰富;分布不均,区域差异大;地理成分复杂,具有明显的温带性质;起源古老;土著特有种较多;区系联系广泛,多种区系成分的汇集、混杂和过渡。     

广西元宝山植被种子植物区系初步研究

组成元宝山植被的种子植物共有118科337属732种,区系统计分析表明:(1)科级和属级的区系成分都表现为热带性质稍强于温带性质,亚热带区系性质明显。在元宝山植被区系中,热带亚热带成分与温带成分相互交融,这正是亚热带山地植物区系的一个基本特征。(2)泛热带分布、热带亚洲分布、北温带分布、东亚和北美洲间断分布和东亚分布的属为该植被区系主要构成成分。(3)元宝山植被中存在许多区系上孑遗、古老、孤立的植物类群,并且特有成分丰富,具有重要的保护价值。(4)裸子植物丰富,针叶林群落类型多样,是元宝山植被组成的突出特点。     

中国西南干旱河谷植被的区系地理成分与空间分异

根据对云南、四川、甘肃三省九条主要河流干旱河谷的植物群落调查数据, 对我国西南干旱河谷维管束植物区系的科、属分布区类型进行划分, 并分析其地理分布格局。结果表明: (1)西南干旱河谷区的植物区系地理成分复杂, 联系广泛, 共包含11个科级和15个属级分布区类型; 总体上, 科、属两级热带/温带成分比例分别为3.06和1.77, 显示了强烈的热带区系亲缘及温带区系的后期影响; 与地中海-西亚至中亚植物区系存在一定联系; 其东亚成分和中国特有成分比例低于亚热带区系平均水平, 且中国-喜马拉雅成分比例高于中国-日本成分。(2)从西南向东北方向, 植物区系的热带性质逐渐减弱, 温带性质逐渐增强; 科、属水平区系成分与古地中海-中亚区系的相似性逐渐增强; 东亚和中国特有成分比例增加; 南盘江与元江的干旱河谷植物区系之间存在中国-日本和中国-喜马拉雅成分的分界线。(3)根据干旱河谷植物属区系成分的比例构成将怒江、澜沧江和元江与其他流域分开, 显示了长江溯源侵蚀和水系合并对西南诸河流植物区系发育的影响。     

云南药山自然保护区种子植物区系的垂直分布格局

通过野外植被调查,结合文献资料,探讨了云南药山自然保护区种子植物区系的垂直分布格局.结果表明,温带区系成分所占比重,随着海拔的升高,总体上呈单调递增趋势,而热带区系成分所占比重呈单调递减格局;区系平衡点出现在海拔2000 m 左右.在平衡点之下,植物区系以热带、亚热带区系成分为主,而在此之上,则以温带区系成分为主.区系成分的聚类分析表明,研究区域内植被垂直带谱主要由1500 m以下的干热河谷植被、1500～2000 m左右的云南松林、2000～2600 m的常绿阔叶林、2600～3100 m的硬叶常绿阔叶林、3100～3600 m的亚高山灌丛和3600 m以上的高寒草甸构成,这与传统的植被类型划分方法的结果基本一致.     

福建武夷山的锈菌

福建武夷山锈菌区系基本上属于温带性质,温带型的种占60％以上,也有不少亚热带和热带型的种,本地区是温带和热带锈菌的交汇处。区系成分以东亚成分占显著地位,约占总种数的38.7％;中国特有种有14种,占9.3％;世界广布种占14％;尚有广布整个北半球的泛北极种类,分布欧亚大陆的种类以及亚洲和美洲间断分布的种类。本地区锈菌在种属组成上与日本和我国台湾省相近,已知种中分别有74％和60％以上与日本和我国台湾的种相同,说明它们同属一个区系。寄生在蕨类上被称作“活化石”的原始类型如拟夏孢锈(Uredinopsis)和明痂锈(Hyalopsora)在武夷山各采到了若干种,据此推测第四纪冰期武夷山地区可能也是古老生物的天然避难所之一。     

Distribution of N,P, K,Ca, Mg,S, Zn,Fe, Mn and Cu in groundnut

Summary Concentration of N, P, K, Ca, Mg and S in summer groundnut crop was higher than in kharif while Zn, Fe, Mn and Cu contents were higher in summer crop. Kernel's N, P and Zn; Leaflet's Ca and Mn; Stem's K and Fe; Root's S and Cu and Petiole's Mg contents were highest. Shell's N, P, K, Mg, S, Zn and Cu; Kernel's Ca, Fe and Mn contents were the least. N, P, K, S, Zn and Cu concentrations decreased linearly as the crop grew. Ca, Mg, Fe and Mn concentrations did not display any distinct pattern. Ca concentration was positively correlated with pod yield in both the seasons.     

Simultaneous measurement of the trace elements Al, As, B, Be, Cd, Co, Cu, Fe, Li, Mn, Mo, Ni, Rb, Se, Sr, and Zn in human serum and their reference ranges by ICP-MS

The goal of this article was to establish reference ranges of the concentration of trace elements in human serum and to compare these results with those reported by other authors. We describe the sample preparation and measurement conditions that allow the rapid, precise, and accurate determination of Al, As, B, Be, Cd, Co, Cu, Fe, Li, Mn, Mo, Ni, Rb, Se, Sr, and Zn in human serum samples (n=110) by inductively coupled plasma-mass spectrometry (ICP-MS). Accuracy and precision were determined by analyzing three reconstituted reference serum samples by comparison with other methods and by the standard addition procedure. The advantages of the ICP-MS method include short time of analysis of the elements mentioned, low detection limit, high precision, and high accuracy. Disadventages include a high risk of contamination due to the presence of some of the elements of interest in the environment, the relatively delicate sample handling, and the high cost of the equipment.     

Reference values for the concentrations of As,Cd, Co,Cr, Cu,Fe, I,Hg, Mn,Mo, Ni,Pb, Se,and Zn in selected human tissues and body fluids

This report attempts to formulate reference ranges of elemental concentrations for 15 trace elements in selected human tissues and body fluids. A set of samples consisting of whole blood, blood serum, urine, milk, liver, and hair were chosen and considered for 15 elements of biological significance: As, Cd, Co, Cr, Cu, F, Fe, I, Hg, Mn, Mo, Ni, Pb, Se, and Zn. The results represent wholly or partially data received from 40 countries of the global regions of Africa, Asia, Europe, North, South, and Central America, Australia, and New Zealand. This survey, even if qualitative, has been useful in demonstrating certain trends of trace-element scenarios around the world. It is of course recognized that both diet and environment exert a strong influence on the distribution pattern of several elements, such as As, Cd, Mn, Pb, Se, and Zn. A limited comparison of the available information on soil status of different countries reflected some interesting associations for elements, such as Mn and Zn. Importantly, this study revealed that only a few countries were in a position to identify a reasonable amount of data on samples requested for this project. Regretably, for a number of countries, any dependable data for even such essential elements as Cu, Fe, and Zn were not available. In view of the nutritional importance of many elements, the time is ripe for concerted efforts by intergovernmental agencies to initiate investigations or commission task forces/projects to generate reliable reference data for selected global regions, which sadly lack data of any kind at present.     

Monovalent Cation Permeation through the Connexin40 Gap Junction Channel : Cs,Rb, K,Na, Li,TEA, TMA,TBA, and Effects of Anions Br,Cl, F,Acetate, Aspartate,Glutamate, and NO3

The unitary conductances and permeability sequences of the rat connexin40 (rCx40) gap junction channels to seven monovalent cations and anions were studied in rCx40-transfected neuroblastoma 2A (N2A) cell pairs using the dual whole cell recording technique. Chloride salt cation substitutions (115 mM principal salt) resulted in the following junctional maximal single channel current-voltage relationship slope conductances (γ_j in pS): CsCl (153), RbCl (148), KCl (142), NaCl (115), LiCl (86), TMACl (71), TEACl (63). Reversible block of the rCx40 channel was observed with TBA. Potassium anion salt γ_j are: Kglutamate (160), Kacetate (160), Kaspartate (158), KNO₃ (157), KF (148), KCl (142), and KBr (132). Ion selectivity was verified by measuring reversal potentials for current in rCx40 gap junction channels with asymmetric salt solutions in the two electrodes and using the Goldman-Hodgkin-Katz equation to calculate relative permeabilities. The permeabilities relative to Li⁺ are: Cs⁺ (1.38), Rb⁺ (1.32), K⁺ (1.31), Na⁺ (1.16), TMA⁺ (0.53), TEA⁺ (0.45), TBA⁺ (0.03), Cl⁻ (0.19), glutamate⁻ (0.04), and NO₃− (0.14), assuming that the monovalent anions permeate the channel by forming ion pairs with permeant monovalent cations within the pore thereby causing proportionate decreases in the channel conductance. This hypothesis can account for why the predicted increasing conductances with increasing ion mobilities in an essentially aqueous channel were not observed for anions in the rCx40 channel. The rCx40 effective channel radius is estimated to be 6.6 Å from a theoretical fit of the relationship of relative permeability and cation radius.     

Crystal structure, detonation performance, and thermal stability of a new polynitro cage compound: 2, 4, 6, 8, 10, 12, 13, 14, 15-nonanitro-2, 4, 6, 8, 10, 12, 13, 14, 15-nonaazaheptacyclo [5.5.1.13, 11. 15, 9] pentadecane

A new polynitro cage compound 2, 4, 6, 8, 10, 12, 13, 14, 15-nonanitro-2, 4, 6, 8, 10, 12, 13, 14, 15-nonaazaheptcyclo [5.5.1.1(3,11).1(5,9)] pentadecane (NNNAHP) was designed in the present work. Its molecular structure was optimized at the B3LYP/6-31 G(d,p) level of density functional theory (DFT) and crystal structure was predicted using the Compass and Dreiding force fields and refined by DFT GGA-RPBE method. The obtained crystal structure of NNNAHP belongs to the P-1 space group and the lattice parameters are a = 9.99 ?, b = 10.78 ?, c = 9.99 ?, α = 90.01°, β = 120.01°, γ = 90.00°, and Z = 2, respectively. Based on the optimized crystal structure, the band gap, density of state, thermodynamic properties, infrared spectrum, strain energy, detonation characteristics, and thermal stability were predicted. Calculation results show that NNNAHP has detonation properties close to those of CL-20 and is a high energy density compound with moderate stability.     

Reliability of Analyses of Hg,Fe, Ca,K, P,pH, Alkalinity,Conductivity, Hardness and Colour from Lakes

The aim of this report has been to present results concerning analytical quality controls of Hg analysis of fish and sediment, analyses of Fe, Ca, total-P, K, pH, alkalinity, conductivity, colour and hardness (Ca + Mg) of lake water samples. Despite the fact that these are standard parameters in many regular water control programs, there are major differences in the reliability with which these parameters can be determined. The focus here is on an overall inter-laboratory comparison between the parameters. Six laboratories have been involved in the analysis. Selected results: pH gives the lowest (average) relative standard deviation (error), about 2 %; conductivity gives an error of about 5–7 %; alkalinity yields an average error of as much as 13–25 %, which is the largest among the parameters studied here; colour also gives a high error, 9–15 %; hardness gives a relative standard deviation of about 6–7 %. Of the other parameters (i. e., Hg, Fe, Ca and P), Hg gives the best reliability and Fe and P the lowest. To have knowledge of the reliability of the analytical data is of paramount importance in most control programs and research projects.     

Competitive inhibition and selectivity enhancement by Ca in the uptake of inorganic elements (Be, Na, Mg, K, Ca, Sc, Mn, Co, Zn, Se, Rb, Sr, Y, Zr, Ce, Pm, Gd, Hf) by carrot (Daucus carota cv. U.S. harumakigosun)

We investigated the uptake of inorganic elements (Be, Na, Mg, K, Ca, Sc, Mn, Co, Zn, Se, Rb, Sr, Y, Zr, Ce, Pm, Gd, and Hf) and the effect of Ca on their uptake in carrots (Daucus carota cv. U.S. harumakigosun) by the radioactive multitracer technique. The experimental results suggested that Na, Mg, K, and Rb competed for the functional groups outside the cells in roots with Ca but not for the transporter-binding sites on the plasma membrrane of the root cortex cells. In contrast, Y, Ce, Pm, and Gd competed with Ca for the transporters on the plasma membrane. The selectivity, which was defined as the value obtained by dividing the concentration ratio of an elemental pair, K/Na, Rb/Na, Be/Sr, and Mg/Sr, in the presence of 0.2 and 2 ppm Ca by that of the corresponding elemental pair in the absence of Ca in the solution was estimated. The selectivity of K and Rb in roots was increased in the presence of Ca. The selectivity of Be in roots was not affected, whereas the selectivity of Mg was increased by Ca. These observations suggest that the presence of Ca in the uptake solution enhances the selectivity in the uptake of metabolically important elements against unwanted elements.     

Relations of the Al,B, Ba,Br, Ca,Cl, Cu,Fe, K,Li, Mg,Mn, Na,P, S,Si, Sr,and Zn mass fractions to morphometric parameters in pediatric and nonhyperplastic young adult prostate glands

The variation with age of the 18 trace element mass fractions and some histological characteristics of intact prostate glands of 50 subjects aged 0–30 years was investigated by instrumental neutron activation analysis, inductively coupled plasma atomic emission spectrometry, and a quantitative morphometric analysis. Mean values ± standard error of the mean (M ± SΕΜ) for the mass fractions (in milligrams per kilogram wet tissue) of these trace elements in pre-puberty were: Al 28.5 ± 9.0, B 0.40 ± 0.11, Ba 1.48 ± 0.44, Br 10.5 ± 1.5, Ca 241 ± 30, Cl 3,203 ± 278, Cu 3.51 ± 0.89, Fe 33.7 ± 4.1, K 2,364 ± 145, Li 0.020 ± 0.004, Mg 153 ± 23, Mn 0.46 ± 0.06, Na 2,286 ± 130, P 1,391 ± 100, S 1,698 ± 132, Si 62 ± 11, Sr 0.38 ± 0.08, and Zn 27.6 ± 2.3. During puberty and postpuberty, when there is a significant increase in circulating androgens, the mean values were: Al 7.2 ± 1.4, B 0.21 ± 0.05, Ba 0.25 ± 0.06, Br 5.8 ± 1.0, Ca 433 ± 81, Cl 2,314 ± 201, Cu 1.77 ± 0.13, Fe 20.9 ± 1.6, K 2,585 ± 118, Li 0.0088 ± 0.0014, Mg 232 ± 27, Mn 0.34 ± 0.04, Na 1,875 ± 107, P 1,403 ± 98, S 1,673 ± 73, Si 22.2 ± 3.1, Sr 0.22 ± 0.03, and Zn 93.3 ± 8.9. Mean values (M ± SΕΜ) of percent volumes (%) of the stroma, epithelium and lumen in the prostate before puberty were 73.4 ± 2.6, 20.4 ± 1.7, and 4.45 ± 0.94, respectively, versus 46.5 ± 2.5, 38.5 ± 1.9, and 14.9 ± 1.2 during puberty and postpuberty. This work’s results confirm that the Zn mass fraction in prostate tissue is an androgen-dependent parameter. For the first time it has been demonstrated that the glandular lumen is a main pool of Ca, Mg, and Zn accumulation and that the stroma is a main pool of Al, B, Ba, Br, Cl, Cu, Fe, Mn, Na, and Si accumulation in the normal human prostate, for the age range 0–30 years. It was concluded that the Ca, Mg, and Zn binds tightly within the prostatic fluid, because the volume of glandular lumen reflects the volume of prostatic fluid.     

The Effect of Age and Gender on Al, B, Ba, Ca, Cu, Fe, K, Li, Mg, Mn, Na, P, S, Sr, V, and Zn Contents in Rib Bone of Healthy Humans

The effect of age and gender on major, minor, and trace element contents in the intact rib bone of 80 relatively healthy 15–55-year-old women and men was investigated. Contents or upper limit of contents of 16 chemical elements in the rib bone were determined by inductively coupled plasma atomic emission spectrometry (ICP-AES). Mean values (M?±?SΕΜ) for the mass fraction of Ba, Ca, Cu, Fe, K, Li, Mg, Na, P, S, Sr, and Zn (milligram per kilogram of dry bone) were as follows: 2.54?±?0.16, 171,400?±?4,050, 1.35?±?0.22, 140?±?11, 1,874?±?71, 0.049?±?0.011, 2,139?±?38, 5,378?±?88, 75,140?±?1,660, 1,881?±?51, 291?±?20, and 92.8?±?1.5, respectively. The upper limits of contents of Al, B, Mn, and V were <7.20, <0.65, <0.36, and <0.03, respectively. Statistically significant tendency for the Ca, Mg, and P content to decrease with age was found in the human rib bone, regardless of gender. The mass fraction of Fe in the male rib bone increases with age. It was shown that higher Ca, Mg, Na, P, and Sr mass fractions as well as lower Fe content were typical of female ribs as compared to those in male ribs.