迟缓爱德华氏菌基因组fosmid文库的构建、opp基因簇的克隆及aroA基因缺失突变株的构建

本研究构建了迟缓爱德华氏菌(Edwardsiella tarda)LSE40 基因组fosmid文库，该文库共包含2 500个克隆，插入片段平均大小为33.6kb，文库总容量约84Mb，覆盖E.tarda LSE40基因组（按5Mb计算）超过16倍。随机挑取1 000个fosmid克隆进行双末端测序共得到1 741条高质量的序列，序列平均长度546 bp，全长949 997bp，约为E.tarda基因组的19％。将这些序列提交到KEGG自动注释服务器KAAS对所得序列进行代谢途径分析，得到E.tarda LSE40的KO (KEGG Orthology) 注释。分析结果表明，与代谢途径相关的基因有932条序列，与环境信息处理相关基因283条，与遗传信息处理相关基因220条，与细胞进程和人类疾病相关的基因分别为64条和16条。同时将序列进行BlastX，按照微生物致病性共同主题找到61个毒力相关基因。Fosmid文库的建立和部分基因组序列的生物信息学分析为进一步研究E.tarda LSE40的致病机制、代谢机制和生理生态机制提供了丰富的物质基础。 通过比较基因组的方法，从E.tarda LSE40 fosmid文库克隆到编码寡肽透过酶的opp基因簇，该基因簇全长6 741bp，含有5个ORF，依次编码OppA-B-C-D-F 5个蛋白；位于oppA和oppB的间隔区和oppF之后的非编码区各有一个茎环结构，推测分别为oppA和opp基因簇的转录终止子。以细菌OppA的保守结构域SBP_bac_5构建系统发生树，结果显示E.tarda LSE40与同属细菌E.ictaluri的亲缘关系最近，与肠杆菌科细菌的亲缘关系较近，与革兰氏阳性细菌的亲缘关系较远，表明OppA的SBP_bac_5结构域可作为细菌分类鉴定的依据。 从E.tarda LSE40 fosmid文库克隆aroA基因全序列，该序列全长1 287bp，编码428个氨基酸，与鲶鱼爱德华氏菌(E. ictaluri)氨基酸相似性在94%，与其他肠杆菌科菌如Escherichia coli和Yersinia enterocolitica相似性在73%-74%。通过In-frame deletion构建了E.tarda LSE40 aroA缺失突变株。与野生型相比，aroA突变株的半数致死量LD50提高了62倍。在牙鲆接种~106cfu/ml的E.tarda细菌时，接种野生型细菌的牙鲆在6天内全部死亡，濒死鱼的细菌数达7.97×108cfu/ 100mg；而接种aroA突变株的牙鲆没有出现死亡，28天后检测不到细菌的存在。实验结果为进一步评价aroA突变株作为减毒活疫苗打下了基础。

真鲷(Pagrosomus major)胚胎冷冻保存损伤机理及冷冻精子遗传物质稳定性研究

本文对真鲷心跳期胚胎对5种常用渗透性抗冻剂（DMSO、甘油、甲醇、丙二醇、乙二醇）和3种非渗透性抗冻剂（PVP、PEG-8000、蔗糖）的耐受性进行了研究。渗透性抗冻剂分6个浓度梯度（5%；10%；15%；20%；25%；30%）和3个时间组（10min；30min；1h）。非渗透性抗冻剂中，PVP、PEG-8000分3个浓度梯度（5%、10%、15%）和2个时间组（10min、30min），蔗糖为4个浓度梯度（5%、10%、15%、20%）和2个时间组（10min、30min）。实验结果表明，在渗透性抗冻剂组中，浓度为5%的处理组的孵化率（>90%）与对照组差异均不显著，随着抗冻剂浓度增大及处理时间的延长，真鲷心跳期胚胎的孵化率显著下降（P<0.05），在最高浓度的最长处理时间中胚胎孵化率均降到了0。总体上，真鲷心跳期胚胎对五种渗透性抗冻剂的耐受性从小到大依次为：甲醇 < 甘油 < 乙二醇 < DMSO < 丙二醇。对影响胚胎孵化率的三个因素（抗冻剂、浓度、时间）进行的因素效应分析结果表明，三种因素对孵化率的影响显著（P<0.05），并且浓度效应 > 时间效应 > 抗冻剂效应。在非渗透性抗冻剂组中，蔗糖组胚胎孵化率未呈显著变化；PVP组随着浓度及时间的增大，孵化率显著下降（P<0.05）；PEG-8000组随着浓度增大孵化率显著下降（P<0.05），但在两个时间组间差异不显著。相同处理情况下PEG-8000对真鲷心跳期胚胎的毒性要小于PVP。因素效应分析比较结果表明仅时间效应不显著，且抗冻剂效应 > 浓度效应 > 时间效应。 对所用各种抗冻剂进行了渗透压测量，实验中使用的渗透性抗冻剂（5%-30%）的渗透压值在959-7980mOsm/kg之间，均高于使用海水的渗透压值（919mOsm/kg）；使用的非渗透性抗冻剂的渗透压值在316-1040mOsm/kg之间，除20%蔗糖渗透压值（1040mOsm/kg）高于海水外，其他非渗透性抗冻剂的渗透压值均要低于海水。对孵化率与相应的溶液渗透压值进行相关回归分析结果表明，渗透性抗冻剂的渗透压与孵化率呈显著的负相关（P<0.05），而非渗透性抗冻剂的渗透压与孵化率相关不显著。渗透性抗冻剂组的回归分析结果表明，二次方程的曲线拟合度最高，得到的回归方程分别为：Y10min = -2×10-8X2 10min - 6×10-5 X 10min + 1.5635 （R2 = 0.713），Y30min= 5×10-8X2 30min－0.0007 X 30min + 2.097（R2 = 0.681），Y1h = 7×10-8X2 1h－0.0008 X 1h+ 2.0397（R2= 0.725）。 在真鲷胚胎对抗冻剂耐受性实验的基础上，挑选五种抗冻剂--10%DMSO、5%甘油、10%甲醇、20%丙二醇、10%乙二醇，浸泡真鲷心跳期胚胎30min后，分别以超速（130℃/min）、快速（20℃/min）、慢速（3℃/min）的速度降温并使用低温显微镜进行观察，依次记录Toif（油球结冰）、Teif（胚胎外部结冰）、Tiif（胚胎内部结冰）等结冰点，Toif值在-9~-23℃之间；Teif值在-21~-35℃之间；Tiif值在-21~-52℃之间。结冰顺序为先油球结冰，然后胚胎外部结冰随之内部马上瞬间变黑形成内部冰晶。随着降温速度的提高，各结冰温度值显著下降。各抗冻剂之间的Teif及Tiif值不同，Toif值之间没有显著差异。对两种玻璃化冷冻方法进行模拟观察，发现胚胎冰晶形成的顺序与非玻璃化过程不同--先内部结冰然后逐渐蔓延至外部形成外部冰晶，而且模拟玻璃化的内部结冰温度Tiif值（-52.56℃）显著（P<0.05）低于使用低浓度的同种抗冻剂超速降温组的Tiif值（-40.11℃）。在快速及慢速降温组中，20%丙二醇组的Tiif要显著的低于其他组（P<0.05）；在超速降温中，甲醇组的Tiif值要显著的低于其他组（P<0.05）。在Tiif小于30℃的实验组中获得形态完整胚胎的比例平均仅有30.77%；在Tiif大于30℃的实验组中获得形态完整胚胎的平均比例高达70.37%，模拟玻璃化组达到100%。各抗冻剂之间，复温后胚胎形态完整率10%甲醇组最高（77.78%）；其次依次为10%乙二醇（66.67%）、20%丙二醇（55.56%）和10%DMSO（55.56%）；5%甘油组最低（11.11%）；推测甲醇的对胚胎的渗透效果要好于其他组。综上推测：使用丙二醇、甲醇作为抗冻剂以及玻璃化冷冻保存方法对真鲷心跳期胚胎超低温保存也许较为合适。 我们对低温保存的真鲷精子核DNA损伤进行了研究以期为下一步胚胎遗传物质稳定性研究提供参考依据。研究方法为单细胞凝胶电泳（SCGE），针对研究对象，在实验过程中对传统的碱性单细胞凝胶电泳在铺胶方法、电泳条件等进行了改进。对精子细胞进行预处理，在碱性电泳液中使核DNA双链解链变性后电泳，EB染色lOmin后，在荧光显微镜下观察，每次随机观察50个左右的核DNA。结果表明，对荧光显微镜下观察到的精子核按彗尾长度及荧光强度划分等级，出现损伤的精子核DNA的损伤程度主要为轻度损伤和中度损伤，很少见有完全损伤的真鲷精子核。经5%、10%、18%、20%、25%、30%DMSO冷冻保存后的精子彗星率分别为33.47％ ± 8.95％; 35.91％ ± 19.44％; 48.95％ ± 8.90％; 43.33％ ± 11.19％; 55.80％ ± 38.94％。鲜精彗星率为31.43 ％ ± 2.68％。对比真鲷冷冻精液与新鲜精液的精子DNA的损伤状况，表明仅用30％ DMSO冷冻精子DNA损伤状况与鲜精差异显著(P<0.05)。 综上所述，渗透性抗冻剂对胚胎的毒性与其渗透压值呈显著的负相关关系。丙二醇对真鲷心跳期胚胎毒性最小，甲醇较其他抗冻剂能更好的渗透入胚胎；玻璃化方法能显著降低Tiif值并能更好的保持超低温保存后胚胎的形态完整性，因此，使用丙二醇、甲醇作为抗冻剂以及玻璃化冷冻保存方法对真鲷心跳期胚胎超低温保存也许较为合适。常规使用的用于超低温保存真鲷精子的DMSO（浓度<15%）不会对精子核物质稳定性造成明显影响。由于胚胎较精子结构要复杂许多，对于真鲷胚胎损伤机理的研究还有大量工作可以开展。

高位虾池水色及其它环境因子变化对凡纳滨对虾生长的影响

本文研究了16口虾塘的饲料投喂量、水位、盐度、透明度、水温、pH、溶解氧浓度、NH3-N浓度、水色、对虾体长及浮游植物的种类和数量等水体理化因子和生物因子的变化。经过统计分析结果如下： 在养殖前4个月饲料的日平均投喂量基本上呈一个倒“U”型。即随着养殖时间的推移，饲料日平均投喂量逐渐增大，到养殖60 d左右，饲料日平均投喂量达到了最大值，然后进入一个平台期，平台期大约维持30 d左右，随后饲料日平均投喂量逐渐减少。在120 d~130 d饲料日平均投喂量降到最低点后又逐渐回升。 水位平均值变化趋势基本相同，均为前浅后深，即随着养殖时间的推移养殖水位平均值逐渐加深 。 盐度变化趋势基本相同，均为前低后高，即随着养殖时间的推移养殖水体盐度逐渐升高。 透明度的总体变化趋势为：早上透明度比下午大，前期透明度比后期大。 水温基本上是随着养殖时间的推移而逐渐下降。6:30的水温比17:30的水温低。且6:30水温与17:30水温基本上呈平行趋势。 pH变化的总体趋势为：前期较高，随着养殖时间的推移pH逐渐下降，到中期（90d左右）pH降到最低点，尔后又逐渐上升，略呈“V”字形。早上的pH比下午的低。且早上的pH与下午的pH基本上呈平行趋势，间或有较大波动。 6:30时溶解氧浓度的平均值随着养殖时间的推移而逐渐增高。17:30时溶解氧浓度的平均值在整个养殖过程中比较平稳。同时，17:30时溶解氧浓度的平均值高于6:30，养殖前期（前90d）这种趋势更明显。 NH3-N浓度的平均值随着养殖时间的推移而逐渐增高。在养殖后期NH3-N浓度的波动较大。同时，养殖过程中17:30时NH3-N浓度的平均值高于6:30。 6:30时出现9~21号水色，它们出现的比例分别为：9号占0.1%，10号占0.3%，11号占1.1%， 12号0.6%，13号1.5%，14号占3.7%，15号占7.1%，16号占17.5%，17号占22.0%，18号占15.9%，19号占13.7%，20号10.9%，21号占5.8%；17:30时出现11~21号水色，它们出现的比例分别为11号占0.1%， 12号占0.3%，13号占1.2%，14号占4.0%，15号占6.0%，16号占17.8%，17号占24.7%，18号占18.1%，19号占11.8%，20号占9.7%，21号5.7%。 在11种典型水色中共检出浮游植物67种。其中11号水色检出16种，优势种为诺马斜纹藻（占总数47.1%）和菱形海线藻（占总数29.8%）。12号水色共检出16种，优势种为原甲藻（占总数40.85%）和圆筛藻（占总数20.73%）。13号水色共检出16种，优势种为颤藻（占总数45.58%）。14号水色共检出18种，优势种为拟货币直链藻（占总数56.73%）和膝沟藻（占总数12.87%）。15号水色共检出18种，优势种为诺马斜纹藻（占总数64.76%）。16号水色共检出16种，优势种为拟货币直链藻（占总数69.93%）。17号水色共检出14种，优势种为诺马斜纹藻（占总数62.56%）和膝沟藻（占总数15.76%）。18号水色共检出21种，优势种为拟货币直链藻（占总数71.19%）。19号水色共检出18种，优势种为圆筛藻（占总数94.99%）。20号水色共检出18种，优势种为圆筛藻（占总数87.14%）。21号水色共检出15种，优势种为拟货币直链藻（占总数59.80%）和萎软几内亚藻（占总数17.57%）。 相关分析结果表明高位池理化因子中对水色的主要影响因素：17:30PH值、养殖生物量、17:30NH3-N、17:30 透明度、水交换量。 对体长的主要影响因素为 6:30溶解氧、水交换量、17：30水色、饲料投喂量、盐度、17:30透明度、17:30水温、6:30NH3-N。 对对虾本身生物学形状对体重的影响研究表明体长、头胸甲长、胸宽、额剑下缘刺数目对体重的通径系数达到显著水平，它们是直接影响体重的重要指标，其中体长对体重的直接影响（0.428**）最大，是影响体重的最主要因素，其次为头胸甲长（0.290**）和胸宽（0.245**），额剑下缘刺数对体重的直接影响（0.070*）较小；胸高与体重的相关程度很大（0.7923），但它与额剑上缘刺数对体重的直接影响都非常小，主要通过其他性状间接影响活体重，是影响体重的次要因素。

Study on growth factors of intermetallic layer within hot-dipped 25% Al-Zn alloy coating on steel

25%Al-Zn alloy coating performs better than hot dip galvanized coating and 55%Al-Zn-Si coating with regard to general seawater corrosion protection. This study deals with the interfacial intermetallic layer's growth, which affects considerably the corrosion resistance and mechanical properties of 25%Al-Zn alloy coatings, by means of three-factor quadratic regressive orthogonal experiments, The regression equation shows that the intermetallic layer thickness decreases rapidly with increasing content of Si added to the Zn-Al alloy bath, increases with rise in bath temperature and prolonging dip time. The most effective factor that determined the thickness of intermetallic layer was the amount of Si added to Zn-Al alloy bath, while the effect of bath temperature and dip time on the thickness of intermetallic layer were not very obvious.

Effect of nano-TiO(2)on MP-25 resin

MP-25 resin is a chlorine-containing polymer widely used in coatings. The effects of two types of nano-TiO2 (P-25 and RM301 LP) on MP-25 were studied with saline immersion, UV irradiation, and electrochemical impedance spectroscopy. UV irradiation was evaluated in terms of gloss change and X-ray photoelectron spectroscopy (XPS). The results indicate that, compared to pigment R-930 TiO2, P-25 reduced the immersion resistance and accelerated UV aging of the MP-25 coating, whereas RM301 LP showed the opposite effects. XPS analysis showed that MP-25 resin degraded under UV irradiation via dechlorination and C-C bond breakage, similarly to poly(vinyl chloride), but RM301 LP could inhibit the aging of MP-25 to a certain extent. A skin effect of oxygen and chlorine was identified in MP-25 resin by XPS. RM301 LP could improve the impedance of the MP-25 coating because of its excellent fill capacity. Hence, rutile nano-TiO2 RM301 LP represents an excellent additive for MP-25 resin. (c) 2007 Wiley Periodicals, Inc.

开垦对海北高寒草甸土壤有机碳的影响

在中国科学院海北高寒草甸生态系统定位站地区,选择高寒草甸开垦后形成的农田(种植春油菜)作为研究对象,开垦年限分别为0、10、20和30年,利用土壤有机碳密度分组法,对0～10 cm、10～20 cm、20～30 cm、30～40 cm土层土壤有机碳(SOC)及不同组分(轻组有机碳LFOC,重组有机碳HFOC)含量及随开垦年限变化关系进行了研究.结果表明,高寒草甸开垦后土壤有机碳及其组分的变化主要发生在0～10 cm土层,LFOC下降最快,其次为HFOC和SOC,至30年时分别下降了48.63%、43.97%、37.64%.而0～40 cm土体内,SOC、LFOC和HFOC亦呈下降趋势,开垦30年,它们的下降速率分别为785.77、16.79和460.29 kg C•hm-2•yr-1.开垦将大大降低高寒草甸作为碳汇的功能,土壤碳库的总贮量由143 516.94 kg C•hm-2•yr-1下降至114 298.34 kg C•hm-2•yr-1,使其逆转为碳源.

藏羚寄生蠕虫卵粪检调查初报

2004年12月25日-2005年1月5日对位于青藏公路楚玛尔河大桥附近集群的藏羚（Pantholops hodgsoni），随机拣取其新鲜粪便共计36份带回实验室。利用漂浮法、沉淀法对粪样进行寄生虫蠕虫卵检查，结果显示，粪样中存在有细颈属（Nematodirus）、马歇尔属（Marshallagia）线虫卵和莫尼茨属（Moniezia）绦虫卵，其感染率在19．4％-94．4％之间，感染强度（EPG）分别为5．58、5．11和2．86。结果表明，冬季藏羚的寄生蠕虫感染率高，但感染种类少和感染强度低。

高产节水春小麦新品种--高原448

高原448是中国科学院西北高原生物研究所采用有性杂交方法选育而成的,其系谱是:青春533/高原602.原代号为94-448,1999年11月通过青海省农作物品种审定委员会审定,定名为高原448.该品种现已成为青海省灌区种植的主要品种之一,是青海省农作物品种审定委员会指定的全省灌区小麦区域试验和生产试验的对照品种.

牦牛放牧率对小嵩草高寒草甸暖季草场植物群落组成和植物多样性的影响

两年的牦牛放牧试验结果表明:在暖季草场,随着放牧率的提高,禾草和莎草类功能群的盖度、生物量及其组成与高度减小,它们与放牧率呈显著的负相关(P<0.05);可食杂草和毒杂草类功能群的盖度、生物量及其组成与高度增加,它们与放牧率呈显著的正相关(P<0.05);各功能群的盖度与生物量之间是显著的正相关关系(P<0.05).对照草地由于没有牦牛的采食,群落由少数优势种植物所统治,群落结构趋于简单,物种组成贫乏,物种多样性和均匀度指数最小;轻度放牧牦牛选择采食对植物群落的影响较小,群落的物种丰富度指数、均匀度指数和多样性指数均不高;中度放牧提高了资源的利用效率,增加了群落结构的复杂性,草地的物种丰富度指数、均匀度指数和多样性指数均最高,该结果支持"中度干扰理论";重度放牧由于牦牛采食过于频繁,改变了植物的竞争能力,导致植物种的均匀度下降,多样性减少.不同放牧率草地群落的物种数(S)、丰富度指数(Ma)、多样性指数(Shannon-Wiener指数H′和Simpson指数D)、均匀度指数(Pielow指数J′)的排序为:对照<轻度放牧<重度放牧<中度放牧,优势度指数(Berger-Parke指数Ⅰ)的变化趋势则与之相反.

Pre-column derivatization of amines with 1,2-benzo-3,4-dihydrocarbazole-9-isopropyl chloroformate followed by LC-fluorescence and LC-APCI-MS

A pre-column derivatization method for the sensitive determination of amines using the labeling reagent 1,2-benzo-3,4-dihydrocarbazole-9-isopropyl chloroformate (BCIC-Cl) followed by high-performance liquid chromatography with fluorescence detection has been developed. Identification of derivatives is carried out by high performance liquid chromatography/atmospheric pressure chemical ionization (LC-APCl-MS-MS). The chromophore of 2-(9-carbazole)-ethyl chloroformate (CEOC) reagent is replaced by 1,2-benzo-3,4-dihydrocarbazole-9-isopropyl functional group, which results in a sensitive fluorescence derivatizing reagent BCIC-Cl. BCIC-Cl can easily and quickly label amines. Derivatives are stable enough to be efficiently analyzed by high-performance liquid chromatography and show an intense protonated molecular ion corresponding m/z [MH](+) under APCl in positive-ion mode. The collision-induced dissociation of protonated molecular ion formed a product at m/z 260 corresponding to the cleavage of CH2-OCO bond. Studies on derivatization demonstrate excellent derivative yields over the pH 9.0-10.0. Maximal yields close to 100% are observed with a 3 to 4-fold molar reagent excess. In addition, the detection responses for BCIC derivatives are compared with those obtained using CEOC and FMOC as derivatization reagents. The ratios of l(BCIC)/l(CEOC) and l(BCIC)/l(FMOC) are, respectively, 1.23-3.14 and 1.25-3.08 for fluorescent (FL) responses (here, l is relative fluorescence intensity). Separation of the derivatized amines had been optimized on reversed-phase Eclipse XDB-C-8 column. Detection limits are calculated from 1.0 pmol injection, at a signal-to-noise ratio of 3, are 10.6-37.8 fmol. The mean interday accuracy ranges from 94 to 105% for fluorescence detection with the largest mean %CV < 7.5. The mean interday precision for all standards is < 6.0% of the expected concentration. Excellent linear responses are observed with coefficients of > 0.9997.

Capillary electrophoretic analysis of pharmacologically active xanthone compounds from Swertia przewalskii pissjauk extract

Pharmacologically active xanthone compounds isolated from Swertia przewalskii pissjauk were well separated by capillary electrophoresis (CE) within 5 min, using a running buffer of 25 mM disodium tetraborate at pH 9.0. Quantitative determination was shown to be possible because regression equations revealed a linear relationship between the peak area of each constituent and its concentration, with correlation coefficients of 0.9972-0.9994. The relative standard deviations were between 0.44%-0.73% for migration times and 2.52%-4.28% for peak areas. The dissociation constant of 1,7-O-beta-D-glucopyranosyl-8-hydroxy-3,7-dimethoxyxanthone, 1,8-dihydroxy-3, 7-dimethoxy-xanthone and 1,7-dihydroxy-3,8-dimethoxyxanthone were also measured by the CE method, giving a value of 9.04, 8.94, and 8.59, respectively.

湖南、广西泥盆纪硅岩地球化学与沉积构造背景

During the Devonian, a complicated carbonate platform-basin configuration was created through transtensional rifting in the context of opening of Devonian South China Sea; extensive bedded chert, commonly interbedded with tuffaceous beds, occurred in the narrow, elongate interplatform basins (or troughs) in South China, where they occurred earlier (Early Devonian) in southern Guangxi and later (early Late Devonian) in northern Guangxi-south central Hunan. In order to unravel the origin and distribution of the bedded chert successions, and their relationships to basement faulting activities during the opening of the Devonian South China Sea, studies of element (major, minor and REE) geochemistry and Rb-Sr, Sm-Nd isotopic systematics are carried out upon the chert deposits. These chert deposits commonly have high SiO2 contents and (average 94.01%) and low TFe2O3 (average 0.55%), together with other geochemical parameters, suggestive of both biogenic and hydrothermal origins. However, Fe/Ti ratio are high along the elongate interplatform basins(troughs) to the northwest along Wuxiangling-Zhaisha-Chengbu, and to the southeast along Xiaodong-Mugui-Xinpu, suggesting relatively intense hydrothermal activities there. They generally contain very low total REE contents (∑REE average 31.21ug/g) with mediate negative Ce anomalies (mean Ce/Ce*=0.83) and low Lan/Cen values (average 1.64), indicating an overall continental margin basin where they precipitated. The northward increases in Ce/Ce* values, particularly along the elongate troughs bounded both to the east and west of the Guangxi-Huanan rift basin, suggest a northward enhancement of terrigenous influences, thereby reflecting a gradual northward propagation of open marine setting. Generally low positive Eu anomalies in the chert, except for the apparently high Eu anomalies in the chert from Chengbu (Eu/Eu* up to 4.6), suggest mild hydrothermal venting activities in general, except for those at Chengbu. The initial 87Sr/86Sr (0) ratios of chert generally vary from 0.712000 to 0.73000 , suggesting influences both from terrigenous influx and seawater. The Nd isotopic model ages (tDM or t2DM) and initial εNd (0) values of chert vary mostly from 1.5 to 2.1 Ga, and from –16 to –21, respectively, implying that the silica sources were derived from the provenances of the Palaeoproterozoic crust relics at depth. The high εNd (0) values of chert (-0.22 to 14.7) in some localities, mostly along the elongate troughs, suggest that silica sources may have been derived from deeper-seated mantle, being channeled through the interplate boundary fault zones extending downwards to the mantle. At Wuxiangling, Nanning, chert occurs extensively from the Emsian through the Frasnian strata, both U/Th ratios and tDM ages of chert reached up to a maximum in the early Frasnian corresponding to the extensive development of chert in South China, pointing to a maximum extensional stage of Devonian South China basin, which is supported by the Ce/Ce* values as is opposed to the previous datasets as the coeval minimum values.

压力和铁含量对铁方镁石(Mg1-xFex)O(x<=0.25)弹性常数影响的第一性原理研究

By first principle methods based on density functional theory (DFT),the equation of state(EOS) and elastic constants of both periclase and ferropericlase are calculated. The pressure and iron doping effects on the elastic constants of ferropericlase are investigated systematically. Firstly, we calculate the elastic constants of periclase and compare the obtained results with experimental data and other theoretical calculations, which shows a encouraging consistence and demonstrates the practicability of first-principle methods. Secondly, by adding iron into periclase crystal model, we build up ferropericlase with iron contents ranging from 0% to 25% mole percent. The corresponding elastic constants are calculated in a large pressure range(0~120GPa). Emphatically, the strong correlation of 3d electrons in transitional elements, such as iron, is difficult to treat in first-principle methods for a long time. The current solution is to make additional correction. During the initial stage of this study, the strong correlation of 3d electrons in iron is not considered, and we observed that addition of iron decreases the volume of ferropericlase, which is totally contradictory to the experimental data. By applying LDA+U approximation in order to solve the strongly correlated 3d electron of iron, we observed the expansion of volume by iron as expected. On the basis of the LDA+U approximation, the elastic constants of ferropericlase are calculated. After a detailed analysis of data obtained from theoretical calculations, we have reached the following conclusions:(1)pressure imposes positive effects on all elastic constants, and the degree of effects is C11>C12>C44. (2) Iron has no distinctive effects on C11 and C12, although some fluctuations are observed around 60GPa. However, iron has obvious softening effects on C44 The softening effects on C44 are intensified as pressure increases. Above the 100GPa, the effects increase greatly, even surpasses the pressure's positive effects in ferropericlase crystal models with iron mole percent of having 12.5%, 18.75% and 25% iron content. (3)As to the modulus deprived from elastic constants, iron has no effect on the adiabatic bulk module BS, only a little fluctuation around 60GPa. We find iron's softening effects on shear modulus G. (4)We find out that, compared with low iron content, elastic constants with iron content approaching 25mole% is consistently fluctuated，which may be caused by the limitations of the LDA+U approximation method itself. (5)We investigate the pressure and Fe doping effects on elastic anisotropy factor（A=(2C44+C12-C11)/C11） of ferropericlase and find out that iron contents will lower the critical isotropic pressure. At the same pressure, when the pressure is below the isotropic pressure, iron softens the anisotropy factor ; when pressure surpasses the isotropic pressure, iron increases the anisotropy factor.

班公湖带多不杂超大型富金斑岩铜矿床的成岩成矿年代学、岩石学及高氧化岩浆¬流体-成矿作用

Duobuza copper deposit, newly discovered typical gold-rich porphyry copper deposit with superlarge potential, is located in the Tiegelong Mesozoic tectonic -magmatic arc of the southern edge of Qiangtang block and the northern margin of Bangonghu-Nujiang suture. Quartz diorite porphyrite and grandiorite porphyry, occurred in stock, are the main ore-bearing porphyries. As the emplacement of porphyry stock, a wide range of hydrothermal alteration has developed. Within the framework of the ore district, abundant hydrothermal magnetite developed, and the relationship between precipitation of copper and gold and hydrothermal magnetite seems much close. Correspondingly, a series of veinlets and network veinlets occurred in all alteration zones. Therefore, systematic research on such a superlarge high-grade Duobuza gold-rich porphyry copper deposit can fully revealed the metallogenic characteristics of gold-rich porphyry copper deposits in this region, establish metallogenetic model and prospecting criteria, and has important practical significance on the promotion of regional exploration. In addition, this research on it can enrich metallogenic theory of strong oxidation magma-fluid to gold-rich porphyry copper deposit, and will be helpful to understand the metallogenic characteristics in early of subduction of Gangdese arc stages and its entire evolution history of the Qinghai-Tibet Plateau, the temporal and spatial distribution of ore deposits and their geodynamics settings. Northern ore body of Duobuza copper deposit have been controlled with width (north-south) about 100 ~ 400 m, length (east-west) about 1400 m, dip of 200 °, angle of dip 65 °~ 80 °. And controlled resource amount is of 2.7 million tons Cu with grade 0.94% and 13 tons Au with 0.21g/tAu. Overall features of ore body are large scale, higher grade copper, gold-rich. Ore occurred in the body of granodiotite porphyry and quartz diorite porphyrite and its contact zone with wall rock. Through the detailed mapping and field work studies, some typies of alteration are identificated as follows: albitization, biotititation, sericitization, silication, epidotization, chloritization, carbonatization, illitization, kaolinization and so on. The range of alteration is more than 10km2. Wall alteration zone can be divided into potassic alteration, moderate argillization alteration, argillization, illite-hydromuscovite or propylitization from ore-bearing porphyry center outwards, but phyllic alteration has not well developed and only sericite-quartz veins occurred in local area. Moreover, micro-fracture is development in ore district , and correspondingly a series of veinlets are development as follows: biotite vein (EB type), K-feldspar-biotite-chalcopyrite-quartz vein, magnetite-antinolite-K-feldspar vein, quartz-chalcopyrite-magnetite veins (A-type), quartz-magnetite-biotite-K-feldspar vein, chalcopyrite veinlets in potassic alteration zone; (2) chalcopyrite occurring in the center vein–quartz vein (B type), chalcopyrite veinlets, chalcopyrite-gypsum vein in intermediate argillization alteration; (3) chalcopyrite- pyrite-quartz vein, pyrite-quartz vein, chalcopyrite-gypsum veins, quartz-gypsum- molybdenite-chalcopyrite vein in argillization alteration; (4) gypsum veins, quartz-(molybdenite)-chalcopyrite vein, quartz-pyrite vein, gypsum- chalcopyrite vein, potassium feldspar veinlets, Carbonate veins, quartz-magnetite veins in the wall rock. In short, various veins are very abundant within the framework of the ore district. The results of electronic probe microscopy analysis (EMPA) indicate that Albite (Ab 91.5~99.7%) occurred along the rim of plagioclase phenocryst and fracture, and respresents the earliest stages of alteration. K-feldspar (Or 75.1~96.9%) altered plagioclase phenocryst and matrix or formed secondary potassium feldspar veinlets. Secondary biotite occurred mainly in phenocryst, matrix and veinlets, belong to magnesium-rich biotite formed under the conditions of high-oxidation magma- hydrothermal. Chloritization developed in all alteration zones and alterd iron- magnesium minerals such as biotite and hornblende and then formed chlorite veinlets. As the temperature rises, Si in the tetrahedral site of chlorite decreased, and chlorite component evolved from diabantite to ripiolite. The consistent 280℃~360℃ of formation temperature hinted that chlorite formed on the same temperature range in all alteration zones. However, formation temperature range of chlorite from the gypsum-carbonate-chlorite vein was 190℃~220℃, and it may be the product of the latest stage of hydrothermal activity. The closely relationship between biotite and rutile indicate that most of rutiles are precipitated in the process of biotite alteration and recrystallization. In addition, the V2O3 concentration of rutile from ore body in Duobuza gold-rich porphyry copper deposit is >0.4％, indicate that V concentration in rutile has important significance on marking main ore body of porphyry copper deposit. Apatites from Duobuza deposit all are F-rich. And apatite in the wall rock contained low MnO content and relatively high FeO content, which may due to the basaltic composition of the wall rocks. The MnO in apatite from altered porphyry show a strong positive correlation with FeO. In addition, Cl/F ratio of apatite from wall rock was highest, followed by the potassic alteration zone and potassic alteration zone overprinted by moderate argillization alteration was the lowest. SO2 in Apatite are in the scope of 0 to 0.66%, biotite in the apatite has the highest SO2, followed by the potassic alteration zone, potassic alteration zone overprinted by moderate argillization alteration, and the lowest in the surrounding rocks, which may be caused by the decrease of oxygen fugacity of hydrothermal fluid and S exhaust by sulfide precipitation in potassic alteration. Magnetite in the wall rock have higher Cr2O3 and lower Al2O3 features compared with altered porphyry, this may be due to basalt wall rock generally has high Cr content. And magnetites have higher TiO2 content in potassic alteration than moderate argillization alteration overprinted by potassic alteration, argillization and wall rock, suggested that its formation temperature in potassic alteration was the highest among them. The ore minerals mainly are chalcopyrite and bornite, and Au contents of chalcopyrite, bornite, and pyrite are similar with chalcopyrite slightly higher. The Eu* negative anomaly of disseminated chalcopyrite was relatively lower than chalcopyrite in veinlets. Within a drill hole, the Eu* negative anomaly of disseminated chalcopyrite was gradually larger from bottom to top. Magnetite has the same distribution model, with obvious negative Eu* abnormal, and ΣREE in great changes. The gypsum has the highest ΣREE content and the obvious negative anomaly, and biotite obviously has the Eu* abnormal. Based on the petrographic and geochemical characteristics, five series of magmatic rocks can be broadly classified; they are volcanic rocks of the normal island arc, high-Nb basaltic rocks, adakites, altered porphyry and diorite. The Sr, Nd, Hf isotopes and geochemistry of various series of magmatic rock show that they may be the result of mixing between basic magma and various degrees of acid magma coming from lower crust melted by high temperature basic underplating from partial melting of the subduction sediment melt metasomatic mantle wedge. Furthermore S isotope and Pb isotope of the sulfide, ore-bearing porphyries and volcanic rocks indicated ore-forming source is the mantle wedge metasomatied by subduction sediment melt. Oxygen fugacity of magma estimated by Fe2O3/FeO of whole rock and zircon Ce4+/Ce3+ indicated that the oxidation of basalt-andesitic rocks is higher than ore-forming porphyry, and might imply high-oxidation characteristics of underplated basic magma. Its high oxidative mechanism is likely mantle sources metasomatied by subduction sediment magma, including water and Fe3+. And such high oxidation of basaltic magma is conducive to the mantle of sulfides in the effective access to melt. And the An component of dark part within plagioclase phenocryst zoning belong to bytownite (An 74%), and its may be a result of magma composition changes refreshment by basaltic magma injection. SHRIMP zircon U-Pb and LA-ICP-MS zircon U-Pb geochronology study showed that the intrusions and volcanic rocks from Duobuza porphyry copper deposit belong to early Cretaceous magma series (126~105Ma). The magma evolution series are as follows: the earliest diorite and diorite porphyrite → ore-bearing porphyry and barren grandiorite porphyry →basaltic andesite → diorite porphyrite → andesite → basaltic andesite, and magma component shows a evolution trend from intermediate to intermediate-acid to basic. Based on the field evidences, the formation age of high-Nb basalt may be the latest. The Ar-Ar geochronology of altered secondary biotite, K-feldspar and sericite shows that the main mineralization lasting a interval of about 4 Ma, the duration limit of whole magma-hydrothermal evolution of about 6 Ma, and possibly such a long duration limit may result in the formation of Duobuza super-large copper deposit. Moreover, tectonic diagram and trace element geochemistry of volcanic rocks and diorite from Duobuza porphyry copper deposit confirm that it formed in a continental margin arc environment. Zircon U-Pb age of volcanic rocks and porphyry fall in the range of 105~121Ma, and Duobuza porphyry copper deposit locating in the north of the Bangonghu- Nujiang suture zone, suggested that Neo-Tethys ocean still subducted northward at least early Cretaceous, and its closure time should be later than 105 Ma. Three major inclusion types and ten subtypes are distinguished from quartz phenocrysts and various quartz veins. Vapor generally coexisting with brine inclusions, suggest that fluid boiling may be the main ore-forming mechanism. Raman spectrums of fluid inclusions display that the content of vapor and liquid inclusion mainly contain water, and vapor occasionally contain a little CO2. In addition, the component of liquid inclusions mainly include Cl-, SO42-, Na+, K+, a small amount of Ca2+, F-; and Cl- and Na+ show good correlation. Vapor mainly contains water, a small amount of CO2, CH4 and C2H6 and so on. The daughter minerals identified by Laman spectroscopy and SEM include gypsum, chalcopyrite, halite, sylvite, rutile, potassium feldspar, Fe-Mn-chloride and other minerals, and ore-forming fluid belong to a complex hydrothermal system containing H2O-NaCl-KClFeCl2CaCl2. H and O isotopic analysis of quartz phenocryst, vein quartz, magnetite, chlorite and gypsum from all alteration zones show that the ore-forming fluid of Duobuza gold-rich porphyry copper deposit consisted mainly of magmatic water, without addition of meteric water. Duobuza gold-rich porphyry copper deposit formed by the primary magmatic fluid (600-950C), which has high oxidation, ultra-high salinity and metallogenic element-rich, exsolution direct from the magma, and it is representative of the typical orthomagmatic end member of the porphyry continuum. Moreover, the fluid evolution model of Duobuza gold-rich porphyry copper deposit has been established. Furthermore, two key factors for formation of large Au-rich porphyry copper deposit have been summed up, which are ore-forming fluids earlier separated from magma and high oxidation magma-mineralization fluid system.

新疆谢米斯台中段地区火山岩特征及其含矿性研究

Central Xiemisitai is located on the northwest edge of the Junggar Basin, bounded on the north by Sawuer Mountain, and southward Junggar Basin. Geotectonically, it is within the Chengjisi-Ximisitai-Santanghu island arc of Late Paleozoic, between Siberian and Junggar plates. The volcanics in this area mainly consist of acidic volcanic lava, rock assemblage of esite, dacite, and rhyolite, and the transitional phase is comparatively developed. Besides, Si2O of volcanics here covers a large range of 53.91-79.28t %, K2O of 1.71-6.94t%, and Na2O of 2.29-5.45t%, which is a set of metaluminous- peraluminous high K calc-alkaline to calc alkaline mid-acidic volcanic series. In addition, the volcanics are potassic to high-potassic assemblage, with slight shoshonite in. The REE curve of volcanics in central Xiemisitai is rightward and smooth, inclining to LREE enrichment, which reveals the characteristics of island-arc volcanics. Through the lithology changing from neutral to acidic, the negative anomaly of Eu is increasing. The volcanics here deplete HFSE such as Nb, Ti, P, etc., but relatively rich in LILE like Rb, K, Th, etc., possessing geochemistry characteristics of arc volcanics, which means that the lava source region is watery, under the meta-somatic contamination of subducted components. Moreover, high Ba and Sr show volcanics in epicontinental arc environment, and their contemporaneous granitoid rocks are also marked with the characteristics of volcanic arc granite. In central Xiemisitai, the volcanics zircon age of volcanic rhyolite is 422.5Ma± 1.9Ma, mid-late Silurian. Only one sample zircon has been measured for the present, not very convincing, so volcanics here might not come from Devonian volcanism. Consequently, further confirming the volcanic age will play a key role in the research on the beginning of volcanism in Xiemisitai area and even North Xinjiang. This area includes three copper mineralization types: a) from andesite fracture; b) from rhyolite fracture broken zone, with the copper mineralization distributed by veins along the fissure; and c) from quartz veins. The mineralization of earth surface in S24 ore spot is intensive, and the primary geochemistry reconnaissance anomaly is fairly good. According to display data, the maximum content of Cu is as high as 0.9% and as low as 0.05%. Also, ore-control fracture structure is having a considerable scale in the strike of fracture both horizontally and vertically downwards, and the result of the geophysics stratagem EH-4 system reveals obvious low-resistivity anomaly. As a result, we believe that the S24 plot is expected to be a volcanic copper deposit target area.