The Equation of State and Petrogenesis of Komatiite

(1) Equation of State of Komatiite

The equation of state (EOS) of a molten komatiite (27 wt% MgO) was detennined in the 5 to 36 GPa pressure range via shock wave compression from 1550°C and 0 bar. Shock wave velocity, U_S, and particle velocity, U_P, in km/s follow the linear relationship U_S = 3.13(±0.03) + 1.47(±0.03) U_P. Based on a calculated density at 1550°C, 0 bar of 2.745±0.005 glee, this U_S-U_P relationship gives the isentropic bulk modulus K_S = 27.0 ± 0.6 GPa, and its first and second isentropic pressure derivatives, K'_S = 4.9 ± 0.1 and K"_S = -0.109 ± 0.003 GPa^-1.

The calculated liquidus compression curve agrees within error with the static compression results of Agee and Walker [1988a] to 6 GPa. We detennine that olivine (FO₉₄) will be neutrally buoyant in komatiitic melt of the composition we studied near 8.2 GPa. Clinopyroxene would also be neutrally buoyant near this pressure. Liquidus garnet-majorite may be less dense than this komatiitic liquid in the 20-24 GPa interval, however pyropic-garnet and perovskite phases are denser than this komatiitic liquid in their respective liquidus pressure intervals to 36 GPa. Liquidus perovskite may be neutrally buoyant near 70 GPa.

At 40 GPa, the density of shock-compressed molten komatiite would be approximately equal to the calculated density of an equivalent mixture of dense solid oxide components. This observation supports the model of Rigden et al. [1989] for compressibilities of liquid oxide components. Using their theoretical EOS for liquid forsterite and fayalite, we calculate the densities of a spectrum of melts from basaltic through peridotitic that are related to the experimentally studied komatiitic liquid by addition or subtraction of olivine. At low pressure, olivine fractionation lowers the density of basic magmas, but above 14 GPa this trend is reversed. All of these basic to ultrabasic liquids are predicted to have similar densities at 14 GPa, and this density is approximately equal to the bulk (PREM) mantle. This suggests that melts derived from a peridotitic mantle may be inhibited from ascending from depths greater than 400 km.

The EOS of ultrabasic magmas was used to model adiabatic melting in a peridotitic mantle. If komatiites are formed by >15% partial melting of a peridotitic mantle, then komatiites generated by adiabatic melting come from source regions in the lower transition zone (≈500-670 km) or the lower mantle (>670 km). The great depth of incipient melting implied by this model, and the melt density constraint mentioned above, suggest that komatiitic volcanism may be gravitationally hindered. Although komatiitic magmas are thought to separate from their coexisting crystals at a temperature =200°C greater than that for modern MORBs, their ultimate sources are predicted to be diapirs that, if adiabatically decompressed from initially solid mantle, were more than 700°C hotter than the sources of MORBs and derived from great depth.

We considered the evolution of an initially molten mantle, i.e., a magma ocean. Our model considers the thermal structure of the magma ocean, density constraints on crystal segregation, and approximate phase relationships for a nominally chondritic mantle. Crystallization will begin at the core-mantle boundary. Perovskite buoyancy at > 70 GPa may lead to a compositionally stratified lower mantle with iron-enriched mangesiowiistite content increasing with depth. The upper mantle may be depleted in perovskite components. Olivine neutral buoyancy may lead to the formation of a dunite septum in the upper mantle, partitioning the ocean into upper and lower reservoirs, but this septum must be permeable.

(2) Viscosity Measurement with Shock Waves

We have examined in detail the analytical method for measuring shear viscosity from the decay of perturbations on a corrugated shock front The relevance of initial conditions, finite shock amplitude, bulk viscosity, and the sensitivity of the measurements to the shock boundary conditions are discussed. The validity of the viscous perturbation approach is examined by numerically solving the second-order Navier-Stokes equations. These numerical experiments indicate that shock instabilities may occur even when the Kontorovich-D'yakov stability criteria are satisfied. The experimental results for water at 15 GPa are discussed, and it is suggested that the large effective viscosity determined by this method may reflect the existence of ice VII on the Rayleigh path of the Hugoniot This interpretation reconciles the experimental results with estimates and measurements obtained by other means, and is consistent with the relationship of the Hugoniot with the phase diagram for water. Sound waves are generated at 4.8 MHz at in the water experiments at 15 GPa. The existence of anelastic absorption modes near this frequency would also lead to large effective viscosity estimates.

(3) Equation of State of Molybdenum at 1400°C

Shock compression data to 96 GPa for pure molybdenum, initially heated to 1400°C, are presented. Finite strain analysis of the data gives a bulk modulus at 1400°C, K'_S. of 244±2 GPa and its pressure derivative, K'_OS of 4. A fit of shock velocity to particle velocity gives the coefficients of U_S = C_O+S U_P to be C_O = 4.77±0.06 km/s and S = 1.43±0.05. From the zero pressure sound speed, C_O, a bulk modulus of 232±6 GPa is calculated that is consistent with extrapolation of ultrasonic elasticity measurements. The temperature derivative of the bulk modulus at zero pressure, θK_OSθT|_P, is approximately -0.012 GPa/K. A thermodynamic model is used to show that the thermodynamic Grüneisen parameter is proportional to the density and independent of temperature. The Mie-Grüneisen equation of state adequately describes the high temperature behavior of molybdenum under the present range of shock loading conditions.

精确测量1／4波片相位延迟量的新方法

提出了一种精确测量1／4波片相位延迟量的新方法。测量光路由激光器、起偏器、被测1／4波片、光弹调制器、检偏器和光电探测器构成。起偏器和检偏器的透光轴相互垂直。被测1／4波片的快轴与光弹调制器的振动轴平行，且与起偏器和检偏器的透光轴分别成±45°夹角。准直激光束依次经过起偏器、被测1／4波片、光弹调制器和检偏器的探测光强由光电探测器接收。利用探测信号的直流分量与二次谐波分量精确计算出被测1／4波片的相位延迟量。实验验证了这种测量方法的有效性，改变初始光强过程中相位延迟量测量结果的复现性为0．012°，检偏器

Impacto da terapia mecânica não cirúrgica em pacientes com periodontite crônica e agressiva generalizadas

O objetivo deste estudo foi avaliar o impacto do tratamento periodontal não cirúrgico sobre a atividade de elastase e o volume de fluido gengival nos pacientes portadores de periodontite crônica e agressiva generalizadas. Foram avaliados 18 pacientes com periodontite crônica (idade média 48,6 DP 7,5 anos), e 11 com periodontite agressiva (idade média 27,9 DP 6,54 anos). Foram utilizados os parâmetros clínicos de avaliação de profundidade de bolsa à sondagem (PB) (mm), nível de inserção (NI) (mm) e sangramento à sondagem (SS). As medidas clínicas e as amostras de fluido gengival foram colhidas a partir dos cinco sítios mais profundos (P) e de cinco sítios rasos com gengivite (G) de cada paciente, antes e 90 dias após o término do tratamento. As etapas clínicas obedeceram ao seguinte cronograma: seleção e exame periodontal; coleta de fluido gengival; tratamento periodontal; reavaliação, compreendendo o exame periodontal e coleta de fluido gengival. O tratamento levou, em média, 4 sessões de 40 minutos cada por paciente, com intervalo de 1 semana entre elas. As consultas para reavaliação foram feitas 90 dias após o término do tratamento. O teste de Wilcoxon foi utilizado para comparar os dados antes e depois do tratamento e o teste não pareado de Mann-Whitney U-test foi utilizado para comparar os grupos de periodontite crônica e agressiva. A amostra analisada antes e após o tratamento não apresentou diferenças significativas entre o grupo com periodontite crônica e agressiva, que responderam de forma similar a todos os indicadores avaliados, exceto para a profundidade de bolsa à sondagem nos sítios rasos com gengivite (p = 0,039) e para o sangramento à sondagem (p = 0,021) nos sítios profundos, ambos mais reduzidos na periodontite crônica após o tratamento. A elastase apresentou, após o tratamento, redução significativa nos sítios profundos, para a periodontite crônica (p = 0,012) e agressiva (p = 0,02). Em relação ao volume de fluido gengival, houve significativa redução após o tratamento nos pacientes com periodontite crônica e agressiva, tanto nos sítios rasos (p = 0,03 e p = 0,03) como nos profundos (p ˂ 0,001 e p = 0,003), respectivamente. Concluindo, os grupos com periodontite crônica e agressiva generalizadas comportaram- se de maneira semelhante frente à terapia mecânica não cirúrgica. Ainda, a terapia periodontal mecânica não cirúrgica mostrou redução significativa do volume de fluido gengival em todos os sítios analisados, e da atividade neutrofílica, nos sítios profundos, associada a reduções significativas em todos os indicadores clínicos analisados após o tratamento.

An investigation of wind tunnel wall effects at high Mach numbers

This paper presents the results of an investigation of wind tunnel wall interference in a two-dimensional wind tunnel at high Mach numbers. The results are presented in the form of curves of lift coefficient versus the ratio of model chord to tunnel height, as functions of Mach number and angle of attack. The investigation was carried out by the authors at the Guggenheim Aeronautical Laboratory of the California Institute of Technology during the school year 1944-45.

Tests were carried out on the NACA low drag airfoil section 65,1-012 at Mach numbers from .60 to .80, and angles of attack of from 1 to 3 degrees. Models were 1", 2", 4" and 6" chord, giving values of the chord to tunnel height ration of .1 to .6. Schlieren photographs were made of shock waves where they occurred.

一种检测光刻机激光干涉仪测量系统非正交性的新方法

提出一种精确检测光刻机激光干涉仪测量系统非正交性的新方法。将对准标记曝光到硅片表面并进行显影;利用光学对准系统测量曝光到硅片上的对准标记理论曝光位置与实际读取位置的偏差;由推导的位置偏差与非正交因子、坐标轴尺度比例、过程引入误差的线性模型,根据最小二乘原理计算出干涉仪测量系统的非正交性。实验结果表明,利用该方法使用同一硅片在不同旋转角下进行测量,干涉仪测量系统非正交因子的测量重复精度优于0.01 μrad,坐标轴尺度比例的测量重复精度优于0.7×10-6。使用不同的硅片进行测量,非正交因子的测量再现性优于

基于基频分量消光的1/4波片快轴标定方法

提出了一种基于基频分量消光的波片快轴标定方法,并利用琼斯矩阵对其标定原理进行了分析。激光器、起偏器、相位调制器、待标定1/4波片、检偏器和光电探测器构成标定光路,起偏器、检偏器的透光轴与相位调制器的振动轴分别成+45°和0°夹角。准直激光束依次经过起偏器、相位调制器、待标定1/4波片和检偏器,由光电探测器接收。理论分析表明该标定方法标定精度主要取决于检偏器的定位误差。实验验证了该标定方法的有效性,1/4波片快轴标定结果的最大偏差为0.043°,标准差为0.012°,标定精度为0.05°。

Efeito da intervenção dietética individualizada no diagnóstico nutricional e no controle metabólico de diabéticos tipo 2 sedentários

Objetivo: Avaliar o efeito da intervenção dietética individualizada sobre o diagnóstico nutricional e controle metabólico em diabéticos tipo 2 sedentários Casuística e Métodos: Trata-se de um ensaio clínico controlado e prospectivo com 80 adultos, de ambos dos sexos, com Diabetes Mellitus tipo 2 divididos em GI (grupo intervenção: 40 indivíduos submetidos à intervenção dietética e a utilização de hipoglicemiante) e GC (grupo controle: 40 indivíduos submetidos à medicação hipoglicemiante). Foi realizada intervenção dietética individualizada por três meses baseando-se nas recomendações da American Diabetes Association (2002). Foram analisadas as variáveis antropométricas: massa corporal total (MCT), estatura com determinação do Índice de Massa Corporal (IMC) e perímetro da cintura (PC); as variáveis bioquímicas glicemia, colesterol total, LDL-colesterol, HDL-colesterol, triglicerídeos (TG) e hemoglobina glicada (HbA1c) e as variáveis dietéticas energia, proteínas, carboidratos, lipídeos, colesterol e fibras alimentares. Para estatística inferencial foi utilizado o Anova two-way com nível de significância de 95%. Resultados: Na análise intergrupos, o GC apresentou aumento nas variáveis: MCT (Δ%=0,78; p=0,014), IMC (Δ%=0,76; p=0,012), PC (Δ%=0,75; p=0,019) enquanto que o GI apresentou redução nas variáveis: MCT (Δ%=-3,71; p<0,001), IMC (Δ%=-3,77; p<0,001), PC (Δ%=-3,98; p<0,001). Na comparação da média do IR intergrupos, observou-se diferença nas variáveis: energia (p<0,001), lipídeos (p=0,012), gorduras saturadas (p<0,001); colesterol dietético (p=0,006); fibras alimentares (p=0,001); glicemia (p<0,001), colesterol total (p<0,001), LDL-colesterol (p<0,001) e HbA1c (p<0,001).Conclusão: A intervenção dietética foi eficiente em melhorar o perfil antropométrico e o controle metabólico dos diabéticos tipo 2 sedentários.

Estudo multicêntrico nacional para avaliação da incidência de autoanticorpos e eventos adversos em pacientes com diferentes enfermidades em uso de infliximabe

Introdução: O infliximabe é um anticorpo monoclonal quimérico que inibe o fator de necrose tumoral, sendo usado em doenças autoimunes e/ou inflamatórias, tais como a artrite reumatóide (AR), a espondilite anquilosante (EA), a psoríase e a artrite psoriásica (AP) e as doenças inflamatórias intestinais (DII). Objetivos: Avaliar se o infliximabe induz à formação de autoanticorpos e verificar a ocorrência de eventos adversos, sobretudo o lúpus induzido por este medicamento. Metodologia: Trata-se de um estudo aberto, prospectivo, de fase IV, onde dosamos os autoanticorpos antes e depois do tratamento (das doenças citadas anteriormente), o qual teve duração mínima de 6 meses (5 infusões). Resultados: No total, 286 pacientes foram avaliados para o fator anti-nuclear (FAN) por imunofluorescência indireta em células Hep2, sendo significativo o aumento de número de indivíduos (p = 0,0001), antes e depois da medicação. Além do FAN, foram dosados, em 146 pacientes, 17 outros autoanticorpos pelo método multiplex, sendo que o anti-DNA de dupla hélice (anti-dsDNA) e o anticardiolipina IgM (aCL IgM) tiveram um aumento significativo (p = 0,003 e 0,0024, respectivamente). Pacientes com AR tiveram uma variação significativa nos títulos do anticorpo anti-proteína citrulinada (ACPA) (antes e depois do tratamento) (p = 0,012). De todos os pacientes avaliados (n = 286), somente 1 (0,35%) apresentou sinais clínicos e laboratoriais de lúpus induzido pelo infliximabe. Conclusão: O estudo demonstrou que o infliximabe interferiu na formação de autoanticorpos (FAN, anti-dsDNA, aCL IgM e ACPA), sendo rara a indução de lúpus pelo medicamento.

毛乌素沙地两种固沙禾草种子萌发和幼苗生长与环境的关系

干旱区和半干旱区生长的植物具有复杂的生存机制，以确保其能够在特定的环境中生存和发展。植物在干旱的荒漠条件下的生存，与其特殊的种子萌发机制密切相关，这种机制能够确保植物在合适的时间与地点进行种子萌发与幼苗生长发育。在植物的生活史中，种子对极端环境具有最大的忍耐力，而萌发的幼苗对环境胁迫的忍耐程度最小。在干旱区生长的植物往往具有特殊的萌发机制使萌发出的幼苗能够度过对外界的敏感期，对于植物的生存具有重要意义。 毛乌素沙地是我国的四大沙地之一，该地区具有水分短缺，蒸发强烈，风沙剧烈和生境异质性高的特征。本文假设生长在这种极端环境中的植物也发展出了“适时适地”的种子萌发和幼苗生长的适应对策。为了验证以上的假设，本文选取毛乌素沙地不同生境中生长的两种优势固沙禾草——流动沙丘上生长的沙鞭(Psammochloa villosa)和固定沙丘上生长的赖草(Leymus secalinus)为研究材料，通过野外调查、温室控制实验和实验室控制实验的方法，从生理生态学的角度探讨这两种植物的种子萌发和幼苗生长过程对沙丘环境的适应对策，主要对比它们在种子休眠、萌发和幼苗早期生长过程中对沙丘生境适应性的异同点。研究结果表明： （1）新成熟的沙鞭和赖草的种子为适应冬季低温而发展出生理性的内生休眠——非深度生理休眠。沙鞭和赖草的种子分别需要经过4周和8周的低温层积处理(3－5ºC)来完全打破休眠。另外，划破种皮或者部分切除胚乳也能够促进种子的萌发，这进一步证明两种植物的种子具有非深度生理休眠。然而，切除胚乳在不同程度上影响它们的幼苗生长。由非深度生理休眠、温度和损伤种皮/胚乳调节的部分萌发机制能够确保两种植物的种子即使在条件适宜的情况下只有部分种子萌发，从而分散植物生存的风险性。 （2）毛乌素沙地的小量降水（无法触发萌发）使种子经常遭受湿润－干燥的交替胁迫过程。种子先在湿润条件下吸涨1d或者2d，然后在室温下干燥0-8天。尽管在经历反复吸涨和自然干燥脱水后仍能够保持萌发能力，沙鞭和赖草种子的萌发特性却发生了不同的变化：和各自的对照相比，沙鞭种子萌发率相同而萌发速率降低;赖草种子的萌发率和萌发速率都降低，部分种子进入休眠状态。沙鞭和赖草萌发出的幼苗可能由于没有后续降雨或者因沙蚀而遭受干燥胁迫，但是其幼苗在生长早期能够忍耐一定程度的干燥，再次湿润后部分幼苗能够恢复生长。沙鞭和赖草幼苗的耐干燥的“极限点”不同：当幼根长度为1 mm时，它们的幼苗忍耐干燥的时间分别是60d和30d;当幼根长度为4 mm时，它们的幼苗忍耐干燥的时间分别是14d和7d。沙鞭和赖草的种子和生长早期的幼苗的耐干燥性特性可能是它们对降雨量和降雨时间都不可预测的沙地生境的生存策略之一。 （3）不同的沙埋深度影响沙鞭和赖草的种子萌发和出苗。这两种植物的种子萌发和出苗都需1－2 cm的浅层沙埋。随着沙埋深度的增加，两种植物的种子萌发率和出苗率逐渐降低，强迫休眠率逐渐升高;萌发率与出苗率和沙埋深度呈负相关关系而休眠率和沙埋深度呈正相关关系。但是，沙鞭种子出苗的最大沙埋深度是8 cm，而赖草的则为4 cm。因强迫休眠而没有萌发的种子对维持一个长期的土壤种子库来说具有生态学优势，这些种子暴露在合适的萌发土壤深度时具有生长出幼苗的潜能。 （4）沙鞭和赖草的种子都具有大小的差异性，种子大小对沙鞭和赖草的种子在不同沙埋深度的出苗具有不同的影响。沙鞭的三种不同大小种子的平均质量分别为小，4.489 ± 0.012 mg (4 – 4.9 mg);中，5.457 ± 0.012 mg (5 – 5.9 mg)和大，6.415 ± 0.011 mg (6 – 6.9 mg)。赖草的两种不同大小种子的平均质量分别为小，3.083 ± 0.026 mg (3 – 3.5 mg)和大3.955 ± 0.028 mg (3.6 – 4.0 mg)。在相同的沙埋深度下，两种植物的大种子的出苗率都显著高于小种子。和小种子相比，两种植物的大种子由于贮藏更多的能量，所以在相同深度的沙埋中具有出苗率更高的生态优势，而大量小种子在沙埋中不能萌发，可以作为种子库保存在沙层中，这样就分散了一次性大量萌发给植物带来的冒险性。 （5）沙鞭和赖草的幼苗在生长过程中会遭受沙埋，其幼苗忍耐沙埋的能力与沙埋的相对深度（沙埋比例）和幼苗年龄有关。沙鞭和赖草幼苗的耐沙埋能力不同：沙鞭的2周龄幼苗可以忍耐达到株高100%的沙埋，而其1周龄幼苗只能忍耐75%的沙埋。赖草的1周龄和2周龄幼苗都只能忍耐75%的沙埋。沙埋之后，沙鞭和赖草幼苗的生物量，根/茎比以及根和茎的长度都受到不同程度的影响。赖草幼苗不能忍耐完全沙埋可能是限制它在流动沙丘上分布的一个原因。 （6）降雨量和降雨频率能够不同程度地影响沙鞭和赖草在不同沙层的萌发和出苗。这两种植物的种子萌发和出苗需要的最小降雨量不同：在一次浇水相当于5 mm降雨量后，沙鞭和赖草种子的萌发率都超过50%;但是使沙鞭和赖草的出苗率能够达到50%的降雨量分别为10 mm和15 mm。沙埋中的沙鞭和赖草种子的出苗对降雨的响应具有以下特征：两种植物种子的出苗随降雨量或者降雨频率的增加而增加;沙鞭的出苗率受到降雨量和降雨频率的显著影响，但是二者交互作用的影响不显著;赖草的出苗率受到降雨量、降雨频率以及二者交互作用的显著影响。 由非深度生理休眠，种子大小，干燥－湿润循环，沙埋和降雨调节的种子萌发和出苗机制确保了自然条件下沙鞭和赖草每次只有少量种子萌发和出苗，从而分散了两种植物在沙丘上的生存风险。 根据沙鞭和赖草在沙丘上的种子萌发和幼苗生长特性，本文为毛乌素沙地通过植物固沙恢复受损的沙地生态系统的种子飞播实践提出了几点建议。

Present status and future scope of fisheries in the Andaman group of islands

The coastal area of approximately 2000 km and the water-bodies in between the Andaman and Nicobar islands are rich in fishery potential which range from 0.012-0.47 million tonnes. The fishery is dominated by catches of sardines, perches, carangids, mackerels, Leiognathus elasmobranchs, seerfish, mullets and tunas. About 2050 fishermen, with 1150 country craft, 113 mechanised boats and 1367 different kinds of nets and lines are engaged in active fishing in the island. Numerous bays, lagoons and creeks are available among the group of islands for mariculture activities. The mangroves of these islands provide feeding and nursery grounds for juveniles of penaeid prawns, crabs and finfishes.

黄河口滨岸潮滩湿地系统氮生物循环特征与循环模式研究

潮滩湿地处于海陆相互作用地带，是响应全球变化和人类活动较为敏感的生态系统 之一。潮滩湿地是海岸带一个非常重要的生态类型，作为陆地和海洋过渡区的重要组成 部分，承接来自陆地人类活动带来的大量含氮物质。潮滩湿地氮的生物循环特征不但影 响湿地系统自身的调节机制，而且其在环境介质中的特殊动力学过程也与一系列全球环 境问题息息相关。为了更深入的理解潮滩湿地氮的生物循环特征及其关键机制，论文以 黄河口滨岸潮滩翅碱蓬湿地为研究对象，通过野外样品采集、原位实验、微区试验，研 究了湿地土壤氮的时空分布与化学转化特征，探讨了湿地植物生物量与氮累积季节变化 特征以及湿地植物残体分解及分解过程氮动态特征，建立了湿地植物-土壤系统氮循环 分室模式，主要结论如下：（1）潮滩湿地土壤氮含量具有明显的水平变异和空间结构， TN、NO3 --N 和C/N 具有明显空间分布格局，其空间变异性均以向低潮滩延伸且受潮汐 涨落影响较大的方向最大；微地貌特征和潮汐微域物理扰动是导致空间异质性的两个重 要随机因素，水盐条件、土壤类型和潮汐物理扰动是三个重要结构因素；（2）潮滩湿地 土壤氮含量在不同时期的垂直分布均存在较高变异性，主要与有机质分布、潮汐影响、 水分条件以及陆源影响程度有关；潮滩湿地土壤的氮含量具有明显季节变化特征，主要 与水分状况及受潮汐影响的程度有关；（3）潮滩湿地土壤氮的净矿化/硝化速率均呈波动 变化，并受生物固持、反硝化、温度、水分、C/N 和pH 等因素影响；潮滩湿地0~15cm 土壤的净矿化量和净硝化量分别介于0.33~27.81kg·hm-2 和1.19~15.99kg·hm-2，高潮滩湿 地维持无机氮的能力明显强于中潮滩和低潮滩湿地；（4）两种表现型翅碱蓬的生物量 均具有明显季节变化和空间结构分形特征，二者的地上生物量具有自相似性，分别遵从 D=2.012 和2.366 的分形生长过程；（5）沉积强度显著影响翅碱蓬种子的出苗和幼苗存 活，适度沉积可刺激幼苗生长，重度沉积对幼苗生长则具有抑制作用；沉积可促使幼苗 被埋部分发育为根系，反映了其对潮滩较强沉积环境的特殊适应对策；（6）两种表现 型翅碱蓬根、茎和枯落物的TN 含量均呈递减变化，符合指数衰减模型，叶是二者重要 氮储库，分配比高达46.91±16.97%和55.21±9.79%；中潮滩植被的N/P 为9.87±3.47＜14， 其生长受N 限制，低潮滩植被的N/P 为15.73±5.00＜16，其生长同时受N、P 限制，但 更受P 限制；（7）潮滩湿地植物残体在水盐含量较高或沉积较强条件下的失重率和分解 速率一般较高，反之则较低；温度、水分、盐分和pH 是影响残体相对分解速率的重要 摘 要 II 因素；（8）当分解环境的养分状况不发生较大改变时，残体相对分解速率在很大程度上 取决于基质质量，当养分状况因潮汐养分交换、潮汐物理扰动、沉积物矿化等发生较大 改变时，残体相对分解速率在很大程度上取决于分解环境养分供给状况；（9）潮滩湿地 植物残体在不同水盐梯度和沉积强度下的氮含量、C/N 的变化模式整体较为一致，水盐 条件和沉积强度对残体氮绝对量的变化具有重要影响，C/N 对分解过程中氮养分的调控 作用更为重要；（

GENETIC DIVERSITY IN THE CHINESE PANGOLIN (MANIS-PENTADACTYLA) - INFERRED FROM RESTRICTION ENZYME ANALYSIS OF MITOCHONDRIAL DNAS

Two different forms of Chinese pangolins can be recognized according to the color of their scales, i.e., brown and dusky. We analyzed mitochondrial DNA (mtDNA) purified from the livers of seven dusky and six brown Chinese pangolins from the same locality, using cleavage patterns from 19 restriction enzymes. From the 19 6-bp recognition enzymes used, 51-56 sites were observed. By combining the cleavage patterns for each enzyme, the 13 samples were classified into four restriction types: two in dusky and two in brown Chinese pangolins. The estimated number of nucleotide substitutions per site in dusky and brown types is 0.002, and that between dusky and brown types is 0.012. Divergence between brown and dusky forms began 0.6 Myr ago, provided the mean rate of sequence divergence is 0.02 per Myr in mtDNA. Our results suggest that there is considerable divergence in Chinese pangolins, and brown and dusky Chinese pangolins may be quite different forms or, at least, belong to different maternal groups.

The study of biological characteristic and population dynamic of Caspian vimba (Vimba vimba persa), in coastal waters of Caspian Sea (Mazandaran Province)

This study was conducted to determine reproduction characteristics, diet regime, age structure and population dynamics parameters of the vimba vimba persa (Pallas, 1811) in Mazandaran waters of the Caspian Sea, from October 2008 to September 2009. A total of 994 specimens were monthly collected by beach seine and cast net from six fish landings of Ramsar, Tonekabon, Chaloos, Mahmood Abad, Sari and Behshahr. Biometric characters were measured for each specimen at the laboratory. Scales were used for age determination. Sex determination and fecundity were determined. Population dynamic parameters as well as stock assessment including cohort analysis were estimated using FISAT software. The finding showed that the mean of fork length and body weight of the Caspian Vimba were 168.4±2.6 mm and 71.94±32.24 g respectively. Strong correlation was found between these two variables (a= 0.012; b = 3.047; r2 = 0.955). 92 specimens were studied from the fecundity point of view. This species was found to have more abundance in spring (esp. Apr-May). The samples composed of 397(42.6%) male, 537(57.4%) female; Overall sex ratio (M: F =1: 1.35) was significantly different from the expected 1:1 ratio (p ≤0.05). The advanced stages of maturity (4th & 5th) were found in April and May. The highest Gonadosomatic Index in female was in May and the lowest one was in July. This fish is therefore a spring spawner. The maximum absolute and relative fecundities were 34640 and 260.9, respectively; the minimum absolute and relative fecundities were 5400 and 94.5 respectively. The averages of absolute and relative fecundities were 17198±7710 and 171.85±48.8, respectively. Coefficient vacuity index was 59.2% which indicates that this fish is mesophagous. Among of living creature consumes by Caspian Vimba mollusks, 76 arthropods, worms, plants, detritus and fishes were found 32.9% , 26.7% , 13.4% , 17% , 4.4% and 1.6% respectively. The infinite fork lengths were 261 mm for females, 25mm for males and 261 mm for both sexes respectively. For population growth and mortality parameters; K ( 0.28 per year for both sexes, 0.3 per year for males, 0.33 per year for females); t0 ( -0.65 year for both sexes, -0.23 year in females, -0.51 year in males ); Φ' ( 2.28 ); Z ( 0.98 per year ); M ( 0.59 per year); F ( 0.39 per year) and Exploitation coefficient was 0.4. The analysis showed that total biomass and MSY were 1336 and 528.8 tonnes respectively.