烙铁头蛇毒C-型凝集素样蛋白的生物活性及其作用机制研究

蛇毒C一型凝集素样蛋白一般是由两个相似亚基组成的异构二聚体或由多个异构二聚体组成的多聚体。烙铁头蛇毒血小板活化素TMVA是一个高分子量的C一型凝集素样蛋白。本文研究了烙铁头蛇毒C一型凝聚素样蛋白的生物活性及其作用机制。同时还从烙铁头蛇毒中分离到一个抗凝蛋白（mucroqucetin）。TMVA呈量效关系地诱导P好和洗涤血小板聚集，提示其活化血小板并不调节v从下或不依赖于vWF。抗人血小板糖蛋白（GP）Ib单克隆抗体HIPI呈剂量依赖性特异性抑制TMVA诱导的血小板聚集。抗人GPllb单克隆抗体PZ也抑制血小板聚集。单克隆抗体和流式细胞术分析显示，FITC一TMVA特异性地、剂量依赖性地结合到福尔马林固定的人血小板上，在FIIC-TMVA4O砚浓度时达到饱和性结合状态，这种结合被HIPI特异性地抑制，并呈剂量依赖性。TMVA不结合血小板GPIX、GPllb、GPllla、GPIa、GPlla和GPIV。Mocarhagin仅能部分阻断TMVA诱导的血小板聚集，然而TMVA却能诱导mocarhagin阻断的血小板聚集。以上结果显示TMVA在GPIbQ上的主要受体位于富含亮氨酸第二次重复区氨基酸残基59一81，除此之外，TMVA可能还有其他结合位点。小鼠体内首次给予TMVA后，在短时间内（15min-30min）引起循环血小板数及网织血小板百分率暂时性减低、血小板膜表面P-seleetin的表达暂时性增加，但循环血液中血小板一白细胞复合物未增加；抗鼠血小板单克隆抗体P一selectin、GPllb、GPlll。免疫组化染色显示脾和肺的组织巨噬细胞呈阴性反应，提示TMVA导致循环血小板减少不是巨噬细胞系统对血小板的清除所致。可能是由于TMVA．通过GPIb活化血小板后使P-selectin暴露于胞浆膜表面，这些脱颗粒的血小板在补体的参与下自身溶破，而导致快速的暂时性血小板减少。给予TMVA．后组织病理学显示，肝、脾、肺、肾、胰、大肠及小肠血管未血栓形成；TMVA不影响内源性和外源性凝血系统；TMVA呈剂量依赖性延长小鼠的出血时间，但在TMvA25p眺g时小鼠的出血时间未延长、仍小于5分钟，是一个安全的剂量。以上结果充分证明TMVA具有体内抗血栓作用，血小板自身溶破导致血小板减少在体内抗血栓中可能也起到重要的作用。体内外实验显示TMVA在动物体内外都具有抗补体活性作用。TMVA上调血小板上DAF和CD59的表达，不同程度地上调白细胞上D胚和CDS夕的表达。TMVA在补体系统中的作用可能与其在异种器宫移植中抗IIAR的发生相关。Mucroqucetin是一个由Q链和p链组成的异二聚体蛋白质，其分子量为25KD。。N一末端氨基酸序列与其它该类蛇毒C一型凝集素样蛋白有很高的同源性。Mucroqucetin呈量效关系延长部分凝血活酶时间（APTT），几乎不影响凝血酶原时间（PT）。因子IX和X的抑制试验显示，该纯化蛋白呈量效关系抑制工X因子的凝血活性，不影响X因子，提示mucroqucetin的抗凝活性主要通过结合FIX而实现，是一个血液凝固IX因子结合蛋白。

五步蛇出血毒结构和功能的研究

通过Sephadex-G-100分子筛层析，QAE-Sephadex-A-50阴离子交换层析和两次Poly-buffer-exchanger离子交换层析，分得两个出血毒蛋白，分别称之为HF-1和HF-2。通过碱性PAGE，等电聚焦（IEF），SDS-PAGE和线性密度梯度PAGE，证实两出血蛋白为电泳均一。它们均为三聚体蛋白，分别含有三个相同亚基。HF-1含3 x 113个氨基酸位点，而HF-2含3 x 104个氨基酸位点。EDTA可抑制两者的活性，而碘代乙酸部份抑制HF-2的活性而不抑制HF-1的活性。从氨基酸组成分析发现，HF-1不含有Cys，而HF-1的激光喇曼光谱也没有Cys的特征峰，这在出血毒中是少见的。HF-1和HF-2均属#alpha#－纤溶酶类，同时兼有出血活性和蛋白水解酶活性。还实验了出血HF-2对血小板聚焦的抑制活性，证实HF-2抑制血小板聚集依赖于其对血浆纤原的降解。

Mass spectrometry study on snake venoms and enzymes

In this paper, three kinds of snake venoms and lour kinds of enzymes (phospholipase A(2), fibrinolytic enzyme, arginine esterase and L-amino acid oxidase) isolated from the snake venom were analyzed. As the snake venom was different, the MALDI/TOF/MS showed difference, The MALDI/TOF/MS determination results could be affected Ly the concentrations of snake venom enzymes, And the mechanisms of desorption and ionization was also given in this study, By using MALDI/TOF/MS we obtained the accurate molecular weights and homogeneities of the enzymes. The apparent characteristics of the positive MALDI/TOF/MS of enzymes composed by two subunits were also given out, The results showed that MALDI/TOF/MS is an effective analytic method for discovering new components from snake venom complexes. And it is reliable to use this method to determine the molecular weights and purifies of protein molecules.

Geochemical properties of the variolitic andesite from Susong in the Dabie orogenic belt, China

The variolitic andesite from the Susong County in the Dabie Mountains implies that it was erupted in water. The mineralogy of the varioles is primarily radiate plagioclase (albite sind oligoclase), with little pyroxene, hornblende and quartz (derived from alteration). The pyroxene, hornblende and quartz are in the interstices between plagiocalse. The matrix consists of glass, hornblende, chlorite, epidote and zoisite. It is clearly subjected an extensive alteration. The andesite has an uncommon chemical composition. The SiO2 content is about 56.8%, TiO2 = 0.9%, MgO = 6.4%, Fe2O3 (tot) = 6.7%similar to 7.6%, 100Mg/(Mg + Fe) = 64.1 similar to 66.2. Mg-# is significantly high. The andesite has high abundances of large-lithophile trace elements (e.g. K, Ba. Sr, LREE), e.g. La/Nb = 5.56 similar to 6.07, low abundances of high-strength-field elements (HFSE e.g. Ta, Nb, P, Ti), particularly Ta and Nb strongly depleted. These are consistent with the characteristics of subduction-related magmas. In the spider diagram of trace elements, from Ce to right hand, the abundances of elements decrease quickly, showing a character of the continental margins. There has a strong punishment of light-rare-earth elements, with a significant diffraction of REEs (the mean value of (La/Yb)(N) is 32.84). No Eu anomaly, but there are anomaly high (La/Yb)(N) = 28.63 similar to 36.74, (La/Y)(N) = 70.33 similar to 82.4. The elements Y and Yb are depleted greatly, Y<20 g/g, Y-N = 2.74 similar to 2.84, Yb-N = 2.18 similar to 2.35. From the La-(La/Sm) diagram, the andesite is derived from partial melting. But the epsilone value of Nd is - 18.7 similar to -19.2, so that the material source may be the mantle materials affected by the crustal materials. The Nd model age is 1.9 Ga indicating that the variolitic basaltic andesite was resulted from the mantle wedge of North China block, which had the Nd model age of 2.5Ga, when the Yangze block which had the Nd model age of 1.7Ga subducted beneath it. So the variolitic andesite has characteristics of the island-are volconic rocks oil a continental basement in the vicinity of the destructive continental margin.

水母刺丝囊毒素的提取，溶血活性和毒性的研究

本文研究了水母毒性细胞—刺丝囊的性质、刺丝囊毒素的提取及刺丝囊毒素的溶血活性和毒性等方面的内容。 通过显微镜、扫描电镜及透射电镜分别对霞水母、海蜇、沙蜇触手中所含刺丝囊的形态特点进行了分析，发现三种水母触手中含有不同形状和大小的刺丝囊。应用珠磨式组织研磨器破碎刺丝囊，可有效提取刺丝囊毒素。 霞水母刺丝囊毒素具有明显的溶血活性。4-37°C范围内毒素的溶血活性与温度变化密切相关。毒素溶血活性对pH敏感。胰蛋白酶和鞘磷脂能明显抑制毒素的溶血活性。毒素的溶血活性具有二价金属离子依赖性，Ca2+可能是毒素溶血活性的重要活化剂。EDTA，NaCl及GSH对毒素的溶血活性具有稳定作用。 水母刺丝囊毒素与触手中提取的毒素含有明显不同的蛋白组成，刺丝囊毒素的溶血活性强于触手中提取的毒素。 霞水母刺丝囊毒素表现出明显的神经毒性作用。毒素对草鱼的毒性具有剂量依赖性。霞水母刺丝囊毒素的致死毒性对热的稳定性要比已报道的其它水母毒素强。毒性对pH敏感，胰蛋白酶对毒素的毒性具有明显的抑制作用。毒素的毒性在-80°C稳定。通过DEAE-Sepharose Fast Flow和Sephadex G-100分离霞水母刺丝囊毒素，主要得到两条蛋白谱带，分子量分别为60kDa和47kDa。毒素中的溶血活性成分不具有致死毒性。

Studies on the hemolytic activity of tentacle extracts of jellyfish Rhopilema esculentum Kishinouye: Application of orthogonal test

The present work is first reporting the hemolytic activity of venom from jellyfish Rhopilema esculentum Kishinouye extracted by different phosphate buffer solutions and incubated at different temperature according to the orthogonal test L6(1) x 3(6). Of the seven controllable independent variables, incubated temperature and phenylmethylsulfonyl fluoride (PMSF) had strongest effect on the hemolytic activity. (c) 2006 Elsevier B.V. All rights reserved.

晚中生代松辽盆地形成的大地构造环境及成因机制

Directed by the theory of "Collision Tectonic Facies", the tectonic setting and dynamic mechanism of the formation of Songliao basin in late Mesozoic (J_3-K_1) are studied in the present thesis with the methods of petrology, petrochemistry, geochemistry and isotopic geochronology. The research contents in this paper include as followings. Firstly, the general tectonic frame is made up of different tectonic facies formed from Mid-late Proterozoic to Mesozoic, which are Huabei plate, the Chengde-Siziwangqi melange (Pz_1), the Wenduermiao magmatic arc (Pz_1), the Hegenshan-Chaogenshan melange (Pz_2), the accretion arec (Pz_1-P), the Raohe-Hulin melange (Mz), the magmatic arc (Mz) and the pull-apart basin on the magmatic arc (Mz). Secondly, the volcanic rock assemblages of Songliao basin and its adjacent area in late Mesozoic is the typical calc-alkaline of the magmatic arc. The types of volcanic rocks in the study area include basalts, basaltic andesites, andesites, dacites and rhyolites, and basic-intermediate volcanic rocks have higher alkalinity. The volcanic rock series in this area is the high-K calc-alkaline series. Thirdly, the total REE of volcanic rocks in Songliao basin and its adjacent area is higher than that of the chondrite. The pattern of the REE normalized by the chondrite shows the characteristics similar to that of the typical island arcs or the active continental margins in the earth, that is enrichment of LREE and depletion of Eu. The spider-diagram of the trace element normalized by the primitive mantle also expresses the similar features to that of the typical island arcs or the active continental margins, it has distinctive valleies of Nb, Ta, Sr, P, and Ti, as well as the peaks of La, Ce, Th, U, and K. The incompatible elements show that the high field strength elements, such as Nb, Ta, Ti, and P, are depletion while the low field strength elements, such as K, U, Pb, and Ba, are enrichment. These features are similar to those of orogenic volcanic rocks and imply the formation of the volcanic rocks in this area is related to the subduction. The degrees of both the enrichment of the HFS elements and depletion of the LFS elements become more obvious from basic to acid volcanic rocks, which suggests crustal contamination enhances with the magmatic crystallization and fractionation. The concentration of the compatible elements is W-shape, and anomalies in Cr and Ni suggest there is the contamination during the magmatic crystallization and fractionation. Fourthly, the isotopic age data prove the volcanic activity in the Songliao basin and its adjacent area started in the early-middle Jurassic, and ended in the end of the early Cretaceous-the beginning of the Cretaceous. The volcanism summit was the late Jurassic-the early Cretaceous (100 - 150Ma). Finally, the tectonic setting of volcanism in the late Mesozoic was magmatic arc, which originated the subduction of Raohe-Hulin trench to the northwest Asian plate. The subduction began in the middle Jurassic, and the collision orogenesis between the Sikhote-Alin arc and Asian continent was completed in the end of the early Cretaceous-the beginning of the late Cretaceous. The results of above tectonic processes were finally to format Nadanhada orogenic belt symbolized by the Raohe-Hulin suture or melange belt. The violently oblique movement of the Izanagi plate toward Asian plate in the late Mesozoic was the dynamic mechanism of above tectonic processes. At the same tome, the left-lateral strike-slip shear caused by the oblique movement of the Izanagi plate produced a series of strike-slip faults in east Asian margin, and the large scale displacements of these strike-slip faults then produced the pull-apart basing or grabens on the magmatic arc. Conclusively, the tectonic setting during the formation of the grabens of Songliao basin in the late Mesozoic was magmatic arc, and its dynamic mechanism was the pull-apart. In a word, there was a good coupling relation among the oblique subduction of the oceanic plate, collisional orogene between island arc and continental plate, strike-slip shear of the faults and the formation of the grabens in Songliao basin and its adjacent area in late Mesozoic. These tectonic processes were completed in the unoin dynamic setting and mechanism as above description.

大别山岩石圈有效弹性厚度初步研究

As powerful tools to study the lithosphere dynamics, the effective elastic thickness (Te) as well as the envelope of yielding stress of lithosphere have been attracted great attention of geoscientists in the past thirty years. The oceanic lithosphere, contrary to the continental lithosphere, has more fruits for its simple structures and evolution process. In continent, the lithosphere commonly is complex and variable in the rheological, thermal structures, and has a complicated history. Therefore, the application of the effective elastic thickness in continent is still a subject to learn in a long time. Te, with the definition of the thickness of an elastic plate in theory flexured by the equal benging of the real stress in the lithosphere plate (Turcotte, 1982), marks the depth of transition between elastic and fluid behaviors of rocks subjected to stress exceeding 100 MPa over the geological timescales (McNutt, 1990). There are three methods often adapted: admittance or isostatic response function, coherence and forwarding. In principle, the models of Te consist of thermal-rheological, non-linear Maxwell, non-linear work hardening and rheological layered models. There is a tentative knowledge of Te that it is affected by the following factors: crustal thickness, crust-mantle decoupling, plate bending, boundary conditions of plate (end forces and bending moments), stress state, sedimentary layer, faulting effect, variation in the mountain belts' strike, foreland basin, inheritance of tectonic evolution, convection of mantle, seismic depth and lithosphere strength. In this thesis, the author introduces the geological sketch of the Dabie collisional orogenic belt and the Hefei Basin. The Dabie Mts. is famous for the ultra-high pressure metamorphism. The crustal materials subducted down to the depth of at least 100 km and exhumed. So that the front subjects arise such as the deeply subduction of continent, and the post-collisional crust-mantle interaction. In a geological journey at June of 1999, the author found the rarely variolitic basaltic andesite in the Dabie Mts. It occurs in Susong Group, near Zhifenghe Countryside, Susong County, Anhui Province. It is just to the south of the boundary between the high-grade Susong melange and the ultra-high grade South Dabie melange. It has a noticeable knobby or pitted appearance in the surface. The size of the varioles is about 1-4 mm. In hand-specimen and under microscope, there are distinct contacts between the varioles and the matrice. The mineralogy of the varioles is primarily radiate plagioclase, with little pyroxene, hornblende and quartz. The pyroxene, hornblende and quartz are in the interstices between plagioclase. The matrix is consisted of glass, and micro-crystals of chlorite, epidote and zoisite. It is clearly subjected and extensive alteration. The andesite has an uncommon chemical composition. The SiO_2 content is about 56.8%, TiO_2 = 0.9%, MgO = 6.4%, (Fe_2O_3)_(Total) = 6.7% ～ 7.6%, 100 Mg/(Mg+Fe) = 64.1 ～ 66.2. Mg# is significantly high. The andesite has higher abundances of large-lithophile trace elements (e.g. K, Ba, Sr, LREE), e.g. La/Nd = 5.56-6.07, low abundances of high-strength-field elements (HFSE, e.g. Ta, Nb, P, Ti), particularly Ta and Nb strongly depleted. These are consistent with the characteristics of subducted-related magmas (Pearcce, 1982; Sun and McDonaugh, 1989). In the spider diagram of trace elements, from Ce to right hand, the abundances of elements decrease quickly, showing a characteristic of the continental margins (Pearce, 1982). There has a strongly enrichment of light-rare-earth elements, with a significant diffraction of REEs (the mean value of (La/Yb)_N is 32.84). No Eu anomaly, but there are anomaly high (La/Yb)_N = 28.63-36.74, (La/Y)_N = 70.33 - 82.84. The elements Y and Yb depleted greatly, Y < 20 ppm, Y_N = 2.74-2.84, Yb_N = 2.18 - 2.35. From the La-(La/Sm) diagram, the andesite is derived from partial melting. But the epsilone value of Nd is -18.7 ～ -19.2, so that the material source may be the mantle materials affected by the crustal materials. The Nd model age is 1.9 Ga indicating that the basaltic andesite was resulted from the post-collisional crust-mantle interaction between the subducted Yangze carton and the mantle of Sino-Korea carton. To obtain the Te of the lithosphere beneath the Dabie Mts. and the Hefei Basin, the author applies the coherence method in this thesis. The author makes two topography-gravity profiles (profiles 7~(th) and 9~(th)) across the Dabie Mts. and the Hefei Basin, and calculates the auto-coherence, across coherence, power spectrum, across power spectrum of the topography and gravity of the two profiles. From the relationships between the coherence and the wave-number of profiles. From the relationships between the coherence and the wave-number of profiles 7~(th) and 9~(th), it is obtained that the characteristic wavelengths respectively are 157 km and 126 km. Consequently the values of effective elastic thickness are 6.5 km and 4.8 km, respectively. However, the Te values merely are the minimum value of the lithosphere because the coherencemethod in a relative small region will generate a systemic underestimation. Why there is a so low Te value? In order to check the strength of the lithosphere beneath the Dabie Mts., the authore tries to outline the yielding-stress envelope of the lithosphere. It is suggested that the elastic layers in the crust and upper mantle are 18 km and 35 km, respectively. Since there exist a low viscosity layer about 3-5 km thickness, so it is reasonable that the decoupling between the crust and mantle occurred. So the effective thickness of the lithosphere can be estimated from the two elastic layers. Te is about 34 km. This is the maximum strength of the lithosphere. We can make an approximately estimation about the strength of the lithosphere beneath the Dabie Mts.: Te is about 20-30 km. The author believes that the following factors should be responsible for the low Te value: (1) the Dabie Mts. has elevated strongly since K_3-J_1. The north part of the Dabie Mts. elevates faster than the south part today; (2) there occur large active striking faults in this area. And in the east, the huge Tan-Lu striking fault anyway tends to decrease the lithosphere strength; (3) the lithosphere beneath the Dabie Mts. is heter-homogeneous in spatio-temporal; (4) the study area just locates in the adjacent region between the eastern China where the lithosphere thickness is significantly reduced and the normal western China. These factors will decrease the lithosphere strength.

山东西部中生代碳酸岩和火山岩的地球化学特征及其成因研究

On account of some very peculiar features, such as extremely high Sr and Nd contents which can buffer their primary isotopic signatures against crustal contamination, deep-seated origin within mantle, and quick ascent in lithosphere, carbonatites are very suitable for deciphering the nature of sub-continental lithospheric mantle(SCLM) and receiving widespread attentions all around the world. The Mesozoic carbonatites located in western Shandong was comprehensively investigated in this dissertation. The extremely high REE concentrations, similar spider diagrams to most other carbonatites around the world and high Sr. low Mn contents of apatite from carbonatites confirm their igneous origin. The K depletion of carbonatites from this studies reflect the co-existing of carbonatite melts with pargasite+phlogopite lherzolite rather than phlogopite lherzolite. Geological characteristics and their occumng without associated silicate rocks argue against their origin of fractionation of or liquid immisibility with carbonated silicate melts. In contrast to the low S7Sr/86Sr and high l43Nd/l44Nd of other carbonatites in the world, carbonatites of this studies show EMU features with high S7Sr/86Sr and low l4jNd/144Nd ratios, which imply that this enriched nature was formed through metasomatism of enriched mantle preexisted beneath the Sino-korean craton by partial melts of subducted middle-lower crust of Yangtze craton. In addition to carbonatites, the coeval Mesozoic volcanic rocks from western Shandong were also studied in this dissertation. Mengyin and Pingyi volcanic rocks, which located in the south parts of western Shandong are shoshonite geochemically. while volcanic rocks cropped out in other places are high-K calc-alkaline series. All these volcanic rocks enriched in LREE and LILE. depleted in HFSE, and show TNT(strong negative anomalies in Ta, Nb. Ti) patterns in spider diagrams which are common phenomena in arc-related volcanic rocks. The Sr-Nd-Pb isotopic systematics reveal that the volcanic rocks decrease gradually in 87Sr/86Sr, 206Pb/204Pb, 20SPb/204Pb and increase in TDM from south to north, suggesting the distinction of SCLM beneath Shandong in Mesozoic is more explicit in south-north trending than in east-west trending. The variable features of SCLM can be attributed to the subduction of Yangtze craton beneath Sino-Korean craton, and subsequent metasomatism of SCLM by partial melts of Yangtze lower crust in different extent.

矾山杂岩体成因及其与磷（铁）矿的成矿关系

The Fanshan complex consists of layered potassic ultramafic-syenite intrusions. The Fanshan apatite (-magnetite) deposit occurs in the Fanshan complex, and is an important style of phosphorus deposit in China. The Fanshan complex consists of three (First- to Third-) Phases of intrusion, and then the dikes. The First-Phase Intrusive contains ten typical layered rocks: clinopyroxenite, biotite clinopyroxenite, coarse-grained biotite clinopyroxenite, pegmatitic orthoclase-biotite clinopyroxenite, variegated orthoclase clinopyroxenite, interstitial orthoclase clinopyroxenite, biotite rock, biotite-apatite rock, biotite rock and magnetite-apatite rock. This layered intrusive consists of nine rhythmic units. Each rhythmic unit essentially comprises a pair of layers: clinopyroxenite at the bottom and biotite clinopyroxenite at the top. The apatite (-magnetite) deposit is situated near the top of rhythmic Unit no. 6 of the First-Phase Intrusive. The Second-Phase Intrusive contains three typical rocks: coarse-grained orthoclase clinopyroxenite, . coarse-grained salite syenite and schorlomite-salite syenite. The Third-Phase Intrusive includes pseudo-trachytic salite syenite, porphyritic augite syenite, fine-grained orthoclase clinopyroxenite and fine-grained salite syenite. The origin of the Fanshan complex is always paid attention to it in China. Because most layered igneous intrusion in the world not only have important deposit in it, but also carry many useful information for studying the formation of the intrusion and the evolvement of magma. Two sketch maps were drawn through orebodies along no. 25 cross-cut on 425 mL and no. 1 cross-cut on 491 mL in the Fanshan mine. Through this mapping, a small-scaled rhythmic layering (called sub-rhythmic layering in the present study) was newly found at the top of the rhythmic Unit no. 6. The concept of sub-rhythmic layering is defined in this article. The sub-rhythmic layering is recognized throughout this apatite-rich part, except for magnetite-apatite rock. Presence of the layered magnetite-apatite rock is one of the characteristics of the Fanshan apatite (-magnetite) deposit. Thus, from this layer downwards six units of sub-rhythmic layering are recognized in the present study. Each unit consists of biotite clinopyroxenite (or biotite rock and biotite-apatite rock) layer at the bottom and apatite rock layer at the top. To study this feature in detail is an important work for understanding the origin of the Fanshan complex and apatite (-magnetite) deposit. The origin of the Fanshan complex and the relation of the formation of the apatite(-magnetite)deposit will be interpreted by the study of sub-rhythmic layering on the basis of previous research works. The magma formed the Fanshan complex was rich in K2O, early crystallized pyroxene, and after this phase more biotite crystallized, but no amphibole appeared. This indicated that the activity of H2O in the magma was low. Major element compositions of biotite and clinopyroxene (on thin sections) in the sub-rhythmic layering were analyzed using electron microprobe analyzer. The analytical results indicate Mg/(Mg+Fe*+Mn) atomic ratios (Fe*, total iron) of these two minerals rhythmically changed in sub-rhythmic layering. The trends of Mg/(Mg+Fe*+Mn) atomic ratio (Fe*, total iron) of biotite and clinopyroxene indicate that the magma evolved markedly from relatively magnesian bottom layer to less magnesian top layer in each sub-rhythmic unit. A general trend through the sub-rhythmic layering sequence is both minerals becoming relatively magnesian upwards. The formation temperatures for sub-rhythmic layering yield values between 600 and 800 ℃, were calculated using the ratio of Mg/(Mg+Fe+Mn) in the salite and biotite assemblage. The equilibrium pressures in the rhythmic layers calculated using the contents of Al in the salite were plotted in the section map, shown a concave curve. This indicates that the magma formed the First-Phase Intrusive crystallized by two vis-a-vis ways, from its bottom and top to its centre, and the magnetite-apatite rock was crytallized in the latest stage. The values of equilibrium pressures in the sub-rhythmic layering were 3.6-6.8(xlO8) Pa with calculated using the contents of Al in the salite. The characteristics of geochemistry in various intrusive rocks and the rocks or apatite of sub-rhythmic layers indicated that the Fanshan complex formed by the comagmatic crystallization. The contents of immiscible elements and REEs of apatite rock at the top of one sub-rhythmic unit are more than biotite clinopyroxenite at the bottom. The contents of immiscible elements and REEs of apatite of biotite clinopyroxenite at the bottom of one sub-rhythmic unit are higher than apatite rock at the top. The curves of rocks (or apatite) in the upper sub-rhythmic units are between two curves of the below sub-rhythmic unit in the primitive mantle-normalized trace element abundance spider diagram and the primitive mantle-normalized REE pattern. The trend for the contents of immiscible elements and REEs inclines to the same contents from the bottom to the top in sub-rhythmic layering. These characteristics of geochemistry of rocks or apatites from sub-rhythmic layering indicate that the latter sub-rhythmic unit was produced by the residual magma after crystallization of the previous sub-rhythmic unit. The characteristics of petrology, petrochemistry, geochemistry in the Fanshan complex and sub-rhythmic layers and the trends of Mg/(Mg+Fe+Mn) atomic ratio of biotite and clinopyroxene in sub-rhytmic layering rejected the hypotheses, such as magma immiscibility, ravitational settling and multiple and pulse supplement of magma. The hypothesis of differentiation by crystallization lacks of evidences of field and excludes by this study. On the base of the trends of formation temperatures and pressures, the characteristics of petrology, petrochemistry, geochemistry for the Fanshan complex and the characteristics of geochemistry for the rocks (or apatites), the trends of Mg/(Mg+Fe+Mn) atomic ratio of biotite and clinopyroxene in sub-rhytmic layering, and the data of oxygen, hydrogen, strontium and neodymium isotopes, this study suggests that the magma formed the Fanshan complex was formed by low degree partial melting of mantle at a low activity of H2O, and went through the differentiation at the depth of mantle, then multiply intruded and crystallized. The rhythmic layers of the First-Phase Intrusive formed by the magma fractional crystallized in two vis-a-vis ways, from the bottom and top to the centre in-situ fractional crystallization. The apatite (-magnetite) deposit of the Fanshan complex occurs in sub-rhythmic layering sequence. The the origin of the sub-rhythmic layering is substantially the origin of the Fanshan apatite (-magnetite) deposit. The magma formed the rhythmic layers of First-Phase Intrusive was rich in H2O, F and P at the later stage of its in-situ fractional crystallization. The Fanshan apatite (-magnetite) deposit was formed by this residual magma in-situ fractional crystallization. The magnetite-apatite rock was crystallized by two vis-a-vis ways at the latest stage in-situ fractional crystallization in the rhythmic layers. The result was light apatite layer below heavy the magnetite-apatite layer, formed an "inversion" phenomenon.

安多地区早中侏罗世岩浆岩岩石地球化学和同位素年代学研究及其对构造演化的制约

Anduo area is located in the Central Tibet, the middle segment of the Bangonghu-Nujiang suture. Anduo Block is the northern part of Lhasa terrane. The relationships among the different geological bodies were determined during the 1: 250000 regional geological surveying. Petrography, petrologic geochemistry, isotopic geochemistry and geochronology of igneous rocks from the suture and granitoids from Anduo Block were analyzed systematically as a whole for the first time. Then, their tectonic setting and history are discussed.Anduo ophiolitic melange consists of metamorphic peridotites, cumulates, plagiogranites, sheeted dykes swarm, pillow lava and radiolarian cherts. The concentration of Cr and Ni in the metamorphic peridotites is very high, with Mg# about 0.94 ~ 0.97, higher 87Sr/86Sr and Pb isotopic ratios, and lower 143Nd/i44Nd ratio. LREE is enriched relative to HREE and positive Eu anomaly is very clear. The REE distribution curve is U shape. Nb and Ta anomalies from cumulate gabbro and sheeted dyke swarm are not clear, while that are slightly negative from pillow lava. Plagiogranite belongs to strong calc-alkaline series with high Si, middle Al, low Fe, Mg and low K contents. Eu anomaly (~ 1.23) from plagiogranites is slightly positive. The character of all components of ophiolite is similar to that of the MORB, while to some extent the ophiolite was influenced by crustal material. Anduo ophiolite formed in a mature back-arc basin. Additionally, intermediate acidity volcanic rocks within Anduo phiolite melange are island arc calc-alkline rocks related to ocean subduction.The early-middle Jurassic plutonic rocks are tonalite, granodiorite bearing-phenocryst, magaporphyritic hornblende monzogranite, magaporphyritic monzogranite, monzogranite bearing-phenocryst and syenogranite in turn. They belong to calc-alkaline series which developed from middle K to high K series temporally. REE distribution curves of all plutonic rocks are similar and parallel to each other. SREE and negative Eu anomaly values decrease. In the multi-element spider diagram, the curves of different plutons are similar to each other, but troughs of Nb, Sr, P and Ti from young plutons become more evident. This suggests that thereare some closely petrogenetic affinities among plutonic rocks which make up amagma plutonism cycle of the early-middle Jurassic. Magma source is mainly crustal,but abundant mafic microgranular enclaves within granitoids indicate that crastalmagma should be mixed with mantle-derived magma and the mantle-derived magmadecreased subsequently. Tonalite has features of I-type granite, magaporphyriticmonzogranite is transition type, and monzogranite bearing-phenocryst is S-typegranite. The characteristic of granitoids from Anduo Block suggest that the formingtectonic setting is active continental margin.Reliable zircon U-Pb SHRIMP ages are obtained in the study area firstly. Plagiogranite from the Anduo ophiolite of the Bangonghu-Nujiang suture is 175.1 Ma, and granitoids from Anduo Block is 172.6-185.4 Ma. Additionally, plagioclase from the plagiogranite dates a 40Ar/39Ar age of 144 Ma, while biotite and hornblend from granitoids of Anduo Block give a 163-165 Ma.Similar cooling ages of plagiogranite from the Anduo ophiolitic melange and granitoids from Anduo Block and the spatial distribution of the ophiolitic rocks between Anduo, Naqu, and Shainzha area suggest that bilateral subduction of the Bangonghu-Nujiang oceanic basin took place in the early-middle Jurassic. During this subduction, Anduo ophiolitic rocks were related to north subduction of the Bangonghu-Nujiang oceanic basin and Anduo back-arc basin spreading, while granitoids from Anduo Block were related to south subduction.

Resumos...

Análise dos custos de produção de soja nos estados do Paraná e Santa Catarina para a safra 2007/08; Resumo das exportações do complexo da soja em 2007; Atuação da Embrapa e instituições parceiras no programa de difusão de cultivares e tecnologias associadas a cultura da soja, nos estados do Paraná, Santa Catarina, Mato Grosso do Sul e São Paulo - safra 2007/08; Desenvolvimento de cultivares de soja em pré-lançamento da parceria Embrapa e Fundação Meridional nos estados do Paraná, Santa Catarina e São Paulo - safra 2007/2008; Caracterização dos produtores de soja da região de Unaí - MG; Resultados de produtividade de soja obtidos em unidades demonstrativas e de observação, na safra 2007/08, em Mato Grosso do Sul; Secagem de resíduo do leite de soja "Okara" em secador de cilindro rotativo assistido a microondas; Rendimento de grãos de soja em sucessão a espécies forrageiras solteiras ou consorciadas com milho safrinha; Interações entre forrageiras tropicais e a soja em sistemas de integração lavoura-pecuária no arenito paranaense; Plantio direto de cultivares de soja RR na renovação de cana crua em condição de argissolo; Efeito de diferentes sistemas de manejo sobre o crescimento inicial de duas cultivares da soja; Influência da insolação e do horário de aplicação de glifosato sobre a fitotoxidez na soja BRS Valiosa RR; Teores de óleo e de proteína de genótipos de soja em duas épocas de plantio e dois tipos de solo em Frutal- MG; Leitura SPAD e teor de e proteína nos grãos de genótipos de soja obtidos em quatro épocas de plantio em Viçosa -MG; Influência da época e da população de plantas no rendimento de soja hortaliça; Avaliação de cultivares de soja semeadas em duas épocas em Rolim de Moura - RO; Avaliação regional de cultivares de soja no estado de São Paulo em 2007/08: região do médio Paranapanema; Avaliação regional de cultivares de soja no estado de São Paulo em 2006/07: região do médio Paranapanema; Avaliação regional de cultivares de soja no estado de São Paulo em 2005/06: região do médio Paranapanema; Avaliação regional de cultivares de soja no estado de São Paulo em 2004/05: região do médio Paranapanema; Comparação dos níveis de danos de larvas de Liogenys fuscus (Coleoptera: Melolonthidae) na produção de massa seca de soja; Avaliação da eficiência de inseticidas, em tratamento de sementes, no manejo do coró Liogenys fuscus, em soja; Eficiência do tratamento de sementes com inseticidas no controle da lagarta-elasmo Elasmopalpus lignosellus, na cultura da soja; Tratamento de sementes e a população de percevejos fitófagos na fase vegetativa da soja; Impacto de fungicidas aplicados contra a ferrugem asiática da soja sobre populações da lagarta da soja, Anticarsia gemmatalis Hubner; Eficácia biológica do Chorantraniliprole & Lambdacialotrina no controle de Spodoptera eridania (Lepidoptera: Noctuidae) na cultura da soja no sudoeste goiano; Eficácia biológica do Chorantraniliprole & Lambdacialotrina no controle da lagarta enroladeira (Omiodes indicatus) (Lepidoptera: Cydnidae) na cultura da soja na região sudoeste do estado de Goiás; Avaliação de inseticidas no controle da lagarta falsa medideira (Pseudoplusia includens Walker, 1857) na cultura da soja; Avaliação de inseticidas/acaricidas no controle do ácaro vermelho Tetranychus desertorum (Banks, 1900) na cultura da soja; Eficiência de acaricidas no controle do ácaro rajado Tetranychus urticae (Koch, 1836) na cultura da soja; Estudos de eficiência e praticabilidade agronômica do produto Abamectin Nortox (Abamectin), no controle de Tetranychus urticae (ácaro rajado) na cultura da soja; Avaliação da eficiência de inseticidas e acaricidas para controle do ácaro verde, em soja; Expansão de uso do inseticida teflubenzuron e de sua mistura de pronto uso com o inseticida alfacipermetrina para o controle de lagartas de Spodoptera frugiperda (Smith, 1797) na cultura da soja; Eficácia de inseticidas no controle de ninfas de mosca-branca Bemisia tabaci (Genn, 1889) e validação do método de amostragem; Controle químico de Bemisia tabaci biótipo B na cultura da soja em Chapadão do Sul (MS); Manejo da mosca-branca Bemisia tabaci biotipo B, na cultura da soja na região dos Chapadões; Controle químico da mosca-branca, na cultura da soja, e o impacto dos inseticidas em Encarsia sp.; Estudos de seletividade de inseticidas a parasitóides de ovos, realizados para a cultura da soja; Estudos de seletividade de herbicidas e fungicidas a parasitóides de ovos, realizados para a cultura da soja; Avanços no uso do parasitóide de ovos Trichogramma pretiosum Riley (Hymenoptera:Trichogrammatidae) na cultura da soja; Ação de alguns manejos químicos no controle de pragas na cultura da soja; Efeito de doses de herbicidas e sistemas de semeadura na incidência de retenção foliar e haste verde, em cultivares de soja, no Maranhão e Tocantins; Avaliação da reação de genótipos de soja ao nematóide das lesões radiculares (Pratylenchus brachyurus); Reação de cultivares de soja a Pratylenchus brachyurus em área naturalmente infestada; Efeito do espaçamento entrelinhas na severidade da ferrugem da soja; Curva populacional de Phakopsora pachyrhizi, agente causal da ferrugem asiática da soja, através de armadilha caça-esporos na safra 2007-08, em Costa Rica, MS; Efeito curativo de fungicidas triazóis no controle da ferrugem asiática da soja -Phakopsora pachyrhizi Sydow; Efeito de fungicidas triazóis no controle do oídio da soja; Efeito de fungicidas no controle da ferrugem da soja; Eficiência de controle químico de doenças da soja no Maranhão - safra 2007/08; Efeito do fungicida opera associado a adjuvantes no controle de Phakopsora pachyrhizi, agente causal da ferrugem asiática da soja, em Uberlândia, MG, na safra 2007-08; Efeito de adjuvantes oleosos (Assist e Adash) ao fungicida Piraclostrobina + epoxiconazole no controle da ferrugem da soja; Informações preliminares sobre lesão de causa desconhecida (LCD) em soja; Eficiência de Picoxistrobina + Ciproconazole no controle da ferrugem asiática da soja; Cultivar de soja BRS 278RR: indicação para cultivo nas regiões sul do Maranhão, sudoeste do Piauí e norte do Tocantins; Cultivar de soja BRS 279RR: indicação para cultivo nas regiões sul do Maranhão, sudoeste do Piauí e norte do Tocantins; BRS 282: nova cultivar de soja resistente a nematóides de galha; Cultivar de soja BRS 283: indicação para os estados do PR, de SP, de SC e sul do estado do Mato Grosso do Sul; Cultivar de soja BRS 284: indicação para os estados do PR, SP, SC e sul do estado do Mato Grosso do Sul; BRS 285: nova cultivar de soja convencional indicada para o estado de Mato Grosso do Sul; Extensão da cultivar de soja CD 225RR para as regiões sul do estado do Mato Grosso do Sul, oeste e sul do estado de São Paulo; Extensão da cultivar de soja CD 226RR para as regiões oeste e sul do estado de São Paulo; Recomendação da cultivar de soja CD 228 para os estados de Goiás, Minas Gerais, região norte do estado do Mato Grosso do Sul e região sul do estado do Mato Grosso; Recomendação da cultivar de soja CD 229RR para o estado de Goiás, região norte do estado do Mato Grosso do sul e região sul do estado do Mato Grosso; Recomendação da cultivar de soja CD 231RR para os estados do Paraná, São Paulo e região sul do estado do Mato Grosso do Sul; Recomendação da cultivar de soja CD 232 para os estados do Paraná, São Paulo e região sul do estado do Mato Grosso do Sul; NK7074 RR: cultivar de soja recomendada para a região centro do Brasil; NK 7059RR: cultivar de soja de excelente desempenho nos estados do sul do Brasil e nas regiões sul do MS e centro-sul de SP; Cultivar de soja BRSMG 752S; Cultivar de soja BRSMG 811CRR; Cultivar de soja BRSMG 790A; Cultivar de soja BRSGO 7960: indicação para os estados de Goiás e Minas Gerais; Indicação da cultivar BRSGO 7961 para os estados de Goiás, Distrito Federal e Minas Gerais; Indicação da cultivar de soja BRSGO 7962 para os estados de Goiás e Minas Gerais; Indicação da cultivar BRSGO 7963 para os estados de Goiás, Distrito Federal e Minas Gerais; Indicação da cultivar de soja BRSGO 8060 para os estados de Goiás, Distrito Federal, Minas Gerais e Mato Grosso do Sul; Cultivar de soja BRSGO 8360 indicação para os estados de Minas Gerais, Mato Grosso, Mato Grosso do Sul, Goiás e Distrito Federal; Indicação da cultivar de soja BRSGO 7760RR para o estado de Goiás; Cultivar de soja BRS 7860: indicação para o estado de Goiás e Distrito Federal; Cultivar de soja BRS 7860RR: indicação para o estado de Minas Gerais; Cultivar de soja BRS 7860RR: indicação para os estados de São Paulo e Mato Grosso do Sul; Cultivar de soja BRS 8160RR: indicação para o estado de Minas Gerais; Cultivar de soja BRS 8160RR: indicação para o estado de Goiás (sul e leste) e Distrito Federal; Cultivar de soja BRS 8160RR: indicação para o estado do Mato Grosso do Sul; Indicação da cultivar de soja BRS 8460RR, para os estados de Goiás e Distrito Federal; Indicação da cultivar de soja BRS 8560RR para os estados de Goiás(região sul e leste), Mato Grosso, Mato Grosso do Sul, Minas Gerais e Distrito Federal; Indicação da cultivar de soja EMGOPA 313RR para os estados de Goiás e Tocantins; Cultivar de soja BRS Gisele RR: extensão de indicação para os estados da Bahia, do Tocantins e do Maranhão; Cultivar de soja BRS Juliana RR: extensão de indicação para os estados da Bahia, do Tocantins e do Maranhão; UFU capim branco: nova cultivar para o estado de Mato Grosso; Indicação da nova cultivar UFU Carajás para o estado de Mato Grosso; Extensão de indicação da cultivar UFU Imperial para o estado de Minas Gerais; Indicação da cultivar UFU Mineira para o estado de Minas Gerais; UFU Guará: nova cultivar para a região sul e leste de Mato Grosso; Indicação da cultivar UFU Tikuna para cultivo em Goiás; Eficiência de novos descritores na caracterização de soja pela análise multivariada; Agrupamento de cultivares de soja para o caráter tipo de crescimento; Avaliação de cultivares de soja na região centro-sul do estado do Tocantins - safra 2007/08; Comportamento de cultivares de soja em Palmas-TO, safra 2007/08; Produtividade de cultivares de soja sob épocas e densidades de semeadura no nordeste maranhense; Avaliação de cultivares de soja no cerrado de Rondônia nas safras 2006/07 e 2007/08; Indicação da cultivar de soja BRSGO Luziânia RR para o estado de Goiás e o Distrito Federal; Indicação da cultivar de soja BRSGO Mineiros RR para o estado de Goiás e o Distrito; Tolerância de linhagens de soja a diferentes doses de glifosate; Produtividade e componentes de produção da soja após a aplicação de gesso agrícola incorporado e em superfície; Formas de antecipação da adubação na cultura da soja; Produção de grãos e controle de plantas daninhas em pós-emergência com a utilização de fontes de manganês junto ao glifosato em pós-emergência; Produtividade da soja em resposta a aplicação de micro nutrientes; Avaliação do efeito de aplicação foliar de soluções contendo ácidos humicos sobre a produtividade e a absorção de nutrientes pela soja; Faixas de suficiência de nutrientes em folhas de soja, em Mato Grosso do Sul e Mato Grosso, definidas pelo uso do método DRIS de diagnose do estado nutricional; Alterações na nutrição mineral da soja induzidas pela transgenia e o manejo com herbicidas; Níveis críticos de manganês, em três solos de cerrado; Efeito da população de células na nodulação e rendimento da soja; Avaliação do herbicida Spider aplicado na dessecação na cultura da soja resistente ao herbicida glifosato; Efeito do 2,4 d no controle de plantas voluntárias de soja Roundup Ready®; Controle químico de buva resistente ao glyphosate, com herbicidas aplicados na operação de manejo, em pré-semeadura da cultura da soja; Manejo de soja voluntária resistente ao glyphosate; Identificação de biótipo de picão-preto (Bidens subalternans) resistente a atrazine; Qualidade e produtividade de sementes de soja produzidas em área de cerrado de Roraima, em plantio direto sobre braquiária; Qualidade de sementes de dois genótipos de soja hortaliça cultivados em cerrado de Roraima 2007/2008; Qualidade de sementes de soja produzidas em área de cerrado de Roraima em função de manejos do solo - 2007; Qualidade e produtividade de sementes de soja em função de doses de potássio produzidas em cerrado de Roraima 2007; Qualidade de sementes de soja BRS Candeia e BRS Tracajá produzidas em cerrados de Roraima, em função do tamanho; Tamanho da semente de soja: efeito sobre o desenvolvimento e produtividade; Influência do tamanho da semente na produtividade da cultura da soja; Dano por embebição em sementes de soja em função do teor de água inicial, cultivar e local de produção; Velocidade de hidratação de sementes de soja em função de características do tegumento; Pré-condicionamento e qualidade fisiológica de lotes de semente de soja armazenados sob condições de baixa umidade relativa do ar; Qualidade da semente de soja tolerante ao glifosato; Efeito da aplicação de glyphosate como dessecante em pré-colheita em semente de soja sobre a produtividade; Efeito do teor de lignina no potencial fisiológico de sementes de diferentes cultivares de soja.

Invertebrate diversity in Irish and British forests

Ireland and Britain were once covered in natural forest, but extensive anthropogenic deforestation reduced forest cover to less than 1% and 5 %, respectively, by the beginning of the 20th century. Large-scale afforestation has since increased the level of forest cover to 11% in Ireland and 12% in Britain, with the majority of planted forests comprising small monoculture plantations, many of which are of non - native conifer tree species. At present the forest cover of Ireland and Britain generally consists of small areas of remnant semi-natural woodland and pockets of these plantation forests within a predominantly agricultural landscape. Invertebrates comprise a large proportion of the biodiversity found within forested habitats. In particular, spiders and carabid beetles play an important role in food webs as both predators and prey and respond to small-scale changes in habitat structure, meaning they are particularly sensitive to forest management. Hoverflies play an important role in control and pollination and have been successfully used as indicators of habitat disturbance and quality. This research addressed a number of topics pertinent to the forest types present in the contemporary Irish and British landscapes and aimed to investigate the invertebrate diversity of these forests. Spiders and carabid beetles were sampled using pitfall trapping and hoverflies were sampled using Malaise net trapping. Topics included the impacts of afforestation, the importance of open space, the choice of tree species, and the use of indicators for biodiversity assessment, as well as rare native woodlands and the effect of grazing on invertebrate diversity. The results are discussed and evidence-based recommendations are made for forest policy and management to protect and enhance invertebrate biodiversity in order to promote sustainable forest management in Ireland and Britain.

Distribution, ecology, life history, genetic variation, and risk of extinction of nonhuman primates from Costa Rica

We examined the association between geographic distribution, ecological traits, life history, genetic diversity, and risk of extinction in nonhuman primate species from Costa Rica. All of the current nonhuman primate species from Costa Rica are included in the study; spider monkeys (Ateles geoffroyi), howling monkeys (Alouatta palliata), capuchins (Cebus capucinus), and squirrel monkeys (Saimiri oerstedii). Geographic distribution was characterized accessing existing databases. Data on ecology and life history traits were obtained through a literature review. Genetic diversity was characterized using isozyme electrophoresis. Risk of extinction was assessed from the literature. We found that species differed in all these traits. Using these data, we conducted a Pearson correlation between risk of extinction and ecological and life history traits, and genetic variation, for widely distributed species. We found a negative association between risk of extinction and population birth and growth rates; indicating that slower reproducing species had a greater risk of extinction. We found a positive association between genetic variation and risk of extinction; i.e., species showing higher genetic variation had a greater risk of extinction. The relevance of these traits for conservation efforts is discussed.

A coprological survey of parasites of wild mantled howling monkeys, Alouatta palliata palliata.

Fecal samples from 155 mantled howling monkeys (Alouatta palliata palliata) examined at Centro Ecologico La Pacifica, Guanacaste Province, Costa Rica, revealed 75 (48%) had parasitic infections. A sampling of nine howling monkeys from Santa Rosa National Park. Costa Rica indicated only one infected animal (11%). Only three of 19 (16%) spider monkeys (Ateles geoffroyi) also from Santa Rosa were infected. Controrchis biliophilus, Trypanoxyuris minutus, unidentified strongylid eggs and Isospora sp. oocysts were found. Three monkeys from La Pacifica died and were examined for adult helminths. They were infected with Ascaris lumbricoides, C. biliophilus and T. minutus.