贵州省宽阔水亮叶水青冈林的数量分类

亮叶水青冈(Fagus lucido) 是我国水青冈属植物中分布较广的一种,常与一些耐寒的常绿阔叶树种构成落叶、常绿阔叶混交林,或形成单优群落镶嵌于落叶、常绿阔叶混交林带内,在较高的山体上亦与常绿针叶,常绿、落叶阔叶树种形成针阔混交林。各种亮叶水青冈林是亚热带山地植被垂直带谱的一个重要组成分子。贵州省宽阔水林区保存有集中连片,面积较大,原生性较强的亮叶水青冈林,是该林区森林植被的主体。本文是应用聚类分析和极点排序的数量分类方法对宽阔水林区亮叶水青冈林类型进行划分并对类型的分布规律、优势种的分布格局和生境梯度的变化进行分析的初步研究。     

贵州亮叶水青冈林的结构和动态

贵州的亮叶水青冈林主要分布在黔北宽阔水和黔东北梵净山林区。通过对其结构和动态的分析,说明亮叶水青冈林有稳定的组成和结构,虽然有些亮叶水青冈林下仅有少量的幼苗、幼树,但是亮叶水青冈的长寿命和一直保持着的繁殖潜力以及对光照的广泛适应性,则是保证其世代更替连续性的有利条件,因此它是这些地区的较稳定的群落类型。     

贵州省宽阔水国家级自然保护区亮叶水青冈群落结构及多样性

以贵州省宽阔水国家级自然保护区亮叶水青冈（Fagus lucida）群落为研究对象,基于野外实地调查,应用数量生态学的方法,对保护区内亮叶水青冈群落特征及物种多样性进行了研究,对保护区内植物群落动态变化监测以及对亮叶水青冈群落的保护和管理都具有一定的理论指导意义。结果表明：设置样地共11700m²,调查样地内维管束植物62科,111属,165种,其中蕨类植物4科,6属,6种,种子植物58科,105属,159种。其中以单种科和寡种科（2-5种）占优势,两者的比例之和超过总科数的85％,蔷薇科共有植物6属15种,为所有科中最多,其他属数较多的科有樟科和壳斗科。属的结构中以单种属占据绝对优势,达到70.27％,山矾属和悬钩子属种数最多,各有6种。亮叶水青冈在群落中虽占优势,但龄级结构出现双峰值的异常趋势,种群呈衰退趋势。从总体趋势上来看,群落物种多样性指数均为乔木层 > 灌木层 > 草本层;物种丰富度指数灌木层 > 乔木层 > 草本层;均匀度指数乔木层 > 草本层 > 灌木层。亮叶水青冈幼苗和幼树除在局部区域较集中分布外,其余大部分区域数量均少,且受林下金佛山方竹（Chimonobambusa utilis）干扰较强,大径级植株比重大,年龄结构总体呈衰退型,在未来种群稳定性维持较为困难。应加强对保护区亮叶水青冈的保护,建议合理抚育管理亮叶水青冈幼苗,在森林的经营和管理上,对亮叶水青冈林可在其生长到一定阶段时适度进行人为干扰,会更有利于亮叶水青冈林的更新和生长发育。     

生物多样性 第14卷 总目录

第1期(2006年1月)1四川盆地西缘湿性常绿阔叶林不同恢复阶段物种多样性响应朱万泽蔡小虎何飞王金锡13鄂尔多斯高原植物群落多样性时空变化特点黄永梅张明理21中国北方典型草地物种丰富度与生产力的关系马文红方精云29亚热带山地亮叶水青冈林的群落分类及物种组成与更新汪正祥雷     

金佛山方竹对亮叶水青冈幼树种群数量结构的影响

为探索贵州省宽阔水保护区亮叶水青冈(Fagus lucida)种群的更新维持机制,采用样方法研究金佛山方竹(Chimonobambusa utilis)对亮叶水青冈种群数量结构的影响。结果表明,较高的金佛山方竹密度降低了亮叶水青冈种群数量,亮叶水青冈株数随径级和高度级增加都呈现递减趋势;金佛山方竹密度增加有利于亮叶水青冈小径级向中径级个体的转化,而方竹密度减少则有利于中径级向大径级个体的转化;金佛山方竹密度增大降低了亮叶水青冈种群平均胸径,但增加了平均高度。这表明金佛山方竹能够影响亮叶水青冈个体数量和形态建成,亮叶水青冈通过降低胸径和增加高度来适应竹丛环境。     

八大公山中亚热带山地常绿落叶阔叶混交林物种组成与结构

山地常绿落叶阔叶混交林在我国主要分布在中亚热带1000～2000 m中山地带。八大公山位于武陵山系北端,中亚热带北缘,具有保护较好的典型山地常绿落叶阔叶混交林。为了研究常绿落叶阔叶混交林动态和川东-鄂西植物多样性形成及维持机制,按照CTFS（Center for Tropical Forest Science）样地建设标准,中国科学院武汉植物园于2010-2011年在湖南八大公山（Badagongshan,BDGS）国家级自然保护区建立了一个25 hm2（500 m×500 m）中亚热带山地常绿落叶阔叶混交林动态监测样地（Forest Dynamic Plot）。本研究以样地内所有胸径（DBH）≥1 cm的木本植物（不含竹藤）为研究对象,分析该样地区系成分、群落组成、垂直结构、径级结构和空间分布。结果表明：八大公山样地属于典型的山地常绿落叶阔叶混交林,植物以泛热带分布科（24.50%）和北温带分布属（24.56%）占优势,包括9种珍稀濒危植物。样地内木本植物合计53科、114属、238种（含种下分类单位）,186556株存活个体。落叶树144种,常绿树94种。壳斗科（Fagaceae）、杜鹃花科（Ericaceae）、樟科（Lauraceae）和山茶科（Theaceae）占据优势;个体数超过1000的有38个物种,以常绿树种（63.16%）为主;稀有种（〈25株）103个（占样地物种总数43.28%）。群落垂直结构可分为乔木层（优势树种多脉青冈Cyclobalanopsis multinervis和亮叶水青冈Fagus lucida）、亚乔木层（优势种长蕊杜鹃Rhododendron stamineum和黄丹木姜子Litsea elongata）和灌木层（优势种短柱柃Eurya brevistyla和薄叶山矾Symplocos anomala）。个体数超过1000的树种和稀有种主要来自灌木层。由于生长型限制,样地内树种平均胸径较小（5.41 cm）,DBH〈5 cm的个体占优势（68.40%）。主要优势树种的径级结构呈现倒J型。     

贵州梵净山森林树干附生尖叶拟船叶藓分布格局研究*

通过使用双向指示种分析( TWINSPAN) 和无偏对应分析( DCA) 两种方法进行研究的结果表明, 梵净山
树干附生尖叶拟船叶藓在群落水平上的分布与森林群落类型相对应, 其所在群落可以分成贵州青冈- 箭竹群落、
贵州青冈+ 巴东栎+ 雷公鹅耳枥- 箭竹群落、贵州青冈- 短柱柃群落、大钟杜鹃+ 多脉青冈- 野八角群落、亮
叶水青冈+ 多脉青冈+ 贵州青冈- 箭竹群落和贵州青冈- 尖叶山茶- 野八角群落6 类树附生苔藓植物群落类型。
尖叶拟船叶藓在梵净山的垂直分布范围为海拔1 650~ 2 080 m; 在树干垂直分布表现为下部显著多于中部, 中部
显著多于上部; 在不同树种间的分布存在显著差异。分析了影响树附生尖叶拟船叶藓生态分布的相关因素。     

贵州梵净山森林树干附生尖叶拟船叶藓分布格局研究

通过使用双向指示种分析（TWINSPAN）和无偏对应分析（DCA）两种方法进行研究的结果表明,梵净山树干附生尖叶拟船叶藓在群落水平上的分布与森林群落类型相对应,其所在群落可以分成贵州青冈-箭竹群落、贵州青冈＋巴东栎＋雷公鹅耳枥-箭竹群落、贵州青冈-短柱柃群落、大钟杜鹃＋多脉青冈-野八角群落、亮叶水青冈＋多脉青冈＋贵州青冈-箭竹群落和贵州青冈-尖叶山茶-野八角群落6类树附生苔藓植物群落类型。尖叶拟船叶藓在梵净山的垂直分布范围为海拔1650～2080m;在树干垂直分布表现为下部显著多于中部,中部显著多于上部;在不同树种间的分布存在显著差异。分析了影响树附生尖叶拟船叶藓生态分布的相关因素。     

贵州月亮山不同演替阶段亮叶水青冈林碳储量及其分配格局

林龄对森林生态系统碳储量及其在不同碳组分(植被、木质残体、凋落物和土壤)中的分配有着重要影响。亚热带森林在陆地生态系统碳循环中起着重要作用, 水青冈属(Fagus)植物是我国亚热带广泛分布的重要树种, 而有关水青冈林碳储量随林龄变化的研究在我国鲜有报道。该研究选取贵州月亮山3个演替阶段(林龄分别为33年、82年和208年)的亮叶水青冈(Fagus lucida)林为研究对象, 对其生态系统全组分的碳储量及其分配格局进行了调查与估算。研究发现, 随林龄增加, 亮叶水青冈林生态系统碳储量显著增加, 33年、82年和208年林分别为(186.9 ± 46.0)、(265.8 ± 82.3)和(515.1 ± 176.4) Mg·hm ^-2, 且生态系统碳储量的增加主要由植被碳储量(占比由32%增长至79%)贡献。凋落物与木质残体碳储量随林龄增加亦呈增加趋势, 但二者占生态系统碳储量的比例很小(<1%)。而不同林龄土壤碳储量无显著差异, 其占比由33年林的67%降至208年林的20%。这些结果验证了林龄对森林生态系统各组分碳储量及其分配的重要影响, 同时指出干扰和土地利用历史等对森林植物残体和土壤碳积累的重要作用。     

Ecosystem carbon stock and within-system distribution in successional Fagus lucida forests in Mt. Yueliang,Guizhou, China

林龄对森林生态系统碳储量及其在不同碳组分(植被、木质残体、凋落物和土壤)中的分配有着重要影响。亚热带森林在陆地生态系统碳循环中起着重要作用, 水青冈属(Fagus)植物是我国亚热带广泛分布的重要树种, 而有关水青冈林碳储量随林龄变化的研究在我国鲜有报道。该研究选取贵州月亮山3个演替阶段(林龄分别为33年、82年和208年)的亮叶水青冈(Fagus lucida)林为研究对象, 对其生态系统全组分的碳储量及其分配格局进行了调查与估算。研究发现, 随林龄增加, 亮叶水青冈林生态系统碳储量显著增加, 33年、82年和208年林分别为(186.9 ± 46.0)、(265.8 ± 82.3)和(515.1 ± 176.4) Mg·hm ^-2, 且生态系统碳储量的增加主要由植被碳储量(占比由32%增长至79%)贡献。凋落物与木质残体碳储量随林龄增加亦呈增加趋势, 但二者占生态系统碳储量的比例很小(<1%)。而不同林龄土壤碳储量无显著差异, 其占比由33年林的67%降至208年林的20%。这些结果验证了林龄对森林生态系统各组分碳储量及其分配的重要影响, 同时指出干扰和土地利用历史等对森林植物残体和土壤碳积累的重要作用。     

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.     

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.     

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.     

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.     

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.     

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.     

Caprine blood groups. 2. The C,G, H,I, J,K, L,N, and Q systems

Nine blood group systems of goats were identified using 12 caprine reagents produced by absorption of alloimmune antisera. The caprine C blood group system, possibly homologous to the ovine C blood group system, was characterized by two reagents and shown to be controlled by three alleles,C ¹²,C ²⁵, andC ⁻. A more complex blood group system of goats, designated G, was identified using three reagents and shown to be controlled by six codominant alleles (G ^10.19.20,G ^10.19,G ^10.20,G ¹⁰,G ¹⁹,G ²⁰) and a recessive allele (G ⁻). A further seven one-factor two-allelic systems were identified by seven reagents. The nine genetic systems provided exclusion probabilities of 0.479, 0.492, 0.548, and 0.572 in Australian Angora, Dairy, Cashmere, and Texan Angora goat breeds, respectively. This work was supported by a grant from the Australian Stud Book, Alison Road, Randwick, New South Wales 2031, Australia.