银杉的遗传多样性及系统位置的研究一兼论松科的分子系统学

银杉属Cathaya是我国著名植物学家陈焕镛和匡可任建立的松科单型属，该属是否成立及该属在松科中的系统位置至今仍众说不一。银杉Cathazyaargyro phylla是银杉属的唯一幸存种，被誉为第三纪的活化石，并被列为我国一级保护的濒危植物，也是世界植物红皮书所列少数几种濒危裸子植物之一，保护区虽已设立数个，但该物种的濒危原因仍为未解之谜。本文针对上述问题开展了松科植物的分子系统学研究，探讨了银杉属的系统位置及松科的属间关系，并通过遗传多样性的研究探讨了银杉的濒危机制及保护策略。 1．松科的分子系统学研究 为选取合适的分子标记，本文先探讨了ITS-1在松科等裸子植物中的系统学价值。对1 6种裸子植物（其中含松科10属12种）的ITS-1的扩增结果如下：ITS-1在裸子植物属闻存在极大的长度变异(约600-2600bp)，因而不适用于属级以上的系统学研究;在同属种中，ITs-1的长度虽较一致，但与被子植物的ITS-1相比，裸子植物的ITS-1太长(如在松属中超过2600bp)，难以进行大规模研究。银杉属ITS-1的扩增产物中，一个片段的长度与松属ITS-1的长度相当，另一个片段的长度与云杉属ITS-l的长度相当，这三属间的关系值得进一步研究。此外，在松科植物ITS-1的研究中必须注意真菌“污染”这一问题。 由于ITS不适用于裸子植物属间关系的研究，因而本文运用rbcL-accD基因片段及trnK基因的PCR-RFLP分析探讨银杉属的系统位置及松科的属间关系。rbcL和trnK虽然都是叶绿体基因，但位于trnK内含子区的natK基因与rbcL基因在所受的选择压及进化速率上相差甚远，通过这两个基因研究结果的比较有助于评价系统树的可靠性。此外，考虑到松科的10个属中有9个属的rbcL基因序列已被测定，我们补测了银杉属的rbcL基因序列，进而对松科10个属的rbcL基因序列进行了全面分析。PCR -RFLP分析及rbcL基因的序列分析结果如下： A. PCR扩增的松科rbcL-accD基因片段均长约2550bp，属间没有明显的长度变异，1 8种限制性内切酶的单酶切及7种组合双酶切共获得86个酶切位点，其中54个为变异位点。PAUP和MEGA软件分析均表明：银杉属、松属、黄杉属和落叶松属构成一个单系群，且银杉属与松属的关系似乎近于它与另外二属的关系，但这一结果来得到bootstrap分析的较强支持;黄杉属近缘于落叶松属;冷杉属近缘于油杉属。 B．PCR扩增出的松科trnK基因均长约2557bp，在属间也没有明显的长度变异。16种限制性内切酶的单酶切及7种组合双酶切共获得92个酶切位点，其中68个为变异位点。变异位点中的35个具有系统发育信息，其中28个位于matK基因上。分布于整个trnK基因上的informative位点和仅分布于matK基因上的informative位点分别用于PAUP(version 3.1.1)分析，且PAUP分析中分别用Wagner简约法和Dollo筒约法构建系统树。总体看来，Wager简约树和Dono简约树的结构基本一致（Cedrus的位置除外）：Abies、Keteleeria、Tsuga和Pseudolarix分为一支，且这一支在所有的简约树中均得到分辨;Pseudotsuga近缘于Larix,而Abkes相对近缘于Keteleeria; Cathaya与Ables-Keteleeria-Pseudolarix-Tsuga这一支的关系较远，它与松科的其它属聚在一起，但b∞tstrap分析也不支持它与任何一个属有很近的关 系，说明Cathaya是比较孤立的一个属。Cedrus的位置较特殊，在Wagner简约树中它位于松属以外的其它8个属的基部（因松属为外类群），而在Dollo筒约树中它位于Al}ies-Kete~eer uz-Pseudo/zr/x- Tsuga达一支的基部，并且它与这一支的关系得到了bootstrap分析的较强支持。 C．银杉的rbeL基因长1425bp，其序列与松科其它9个属的rbcL基因序列均有较大差异，从遗传距离(Mega软件中的P-distance)上看，银杉属作为一个属是无可非议的。PAUp和Mega软件分析均表现：Abies、Keteleeria、Pseudolter和Tsuga分为一支，且Cathaya与这一支的关系较远;Pseuaiotsuga近缘于Larix,且这二属间的关系得到了bootstrap分析的强烈支持;Abies近缘于Keteleeria，Pseudolarix近缘于Tsuga，且这两支也得到了bootstrap分析的较强支持;Cathaya与Pinus聚为一支，但支持强度不高。Cetirus的位置与trnK基因的PCR-RFLP分析结果极为相似。 根据rbcL-accD基因片段及trnK基因的PCR-RFLP分析以及rbcL基因的序列分析可以得出如下结论：<1> Cathaya作为一个属不仅是成立的，而且是一个较为孤立的属，将它置于其它任何属内都是不正确的，该属与Abies-Keteleer ia-Pseudolarx-Tsuga这一支的关系较远，相对而言Cathaya与Pinus的关系可能稍近一些。<2>松科主要分为两大支：一支含Abies、KeteZeera、Pseudolarx和Tsuga，该支中Abies近缘于KetelaeriaPseudolarix近缘于Tsuga;另一支含Pseudotsuga、Larix、Cathaya、Pinus和Picete，该支中Pseudotsuga明显近缘于Larix;Cedrus可能更近于Abies-Keteleeria-Pseudolarix-Tsuga这一支。 2．银杉的遗传多样性研究 本研究运用随机扩增多态DNA(RAPD)方法对银杉的1 1 3个个体（分别采自现存全部4个居群：金佛山、花坪、大瑶山和八西山)进行了遗传多样性检测。21个1O-mer的寡核苷酸引物共检测11个位点，其中42个位点是多态的，占37%，这一多态位点百分率仅为裸子植物多态位点百分率平均值的一半左右，说明银杉的遗传多样性水平很低。对多态位点的分析发现银杉屠群内发生了十分严重的遗传漂变，因而导致屠群间的强烈分化。AMOVA分析表明：银杉的遗传变异中，34.7%的变异存在于居群闻，这一数值是裸子植物GST平均值(6。8%)的5倍多;在金佛山屠群中，17%的遗传变异存在于亚居群间，这一数值也是裸子植物GsT平均值的两倍多。银杉的这一居群遗传结构与其它裸子植物的居群遗传结构截然不同。此外，我们提出了度量遗传多样性水平的分化指数概念及其计算方法，并发现遗传多样性水平的高低与生境的复杂程度有一定的相关性。 银杉的遗传多样性水平很低，其适应幅必然很窄，且由于严重的遗传漂变导致居群间的强烈分化，使基因流受阻，进而产生严重的近交，近交又使银杉的适应能力进一步下降，并使极为有限的遗传多样性进一步丧失，这种恶性循环会导致银杉濒危程度的加剧，甚至绝灭。 鉴于银杉独特的居群遗传结构，即有相当大一部分遗传变异存在于居群之间，取样保护时，不仅要在每个居群中取足够多的个体，而且要在尽可能多的居群中取样。就原地保护而言，由于每个居群和亚居群都有独特的基因型，因而都具有保护价值。另外，人工加强居群间的基因流（如人工授粉）对提高银杉各居群的适应能力肯定是有益的。

昆明地区花卉害虫及天敌

1997 年5～ 8 月至1998 年4～ 8 月, 对昆明地区的花卉害虫及天敌进行了考 察和标本采集, 共采到花卉害虫及天敌标本4500 多号, 经鉴定分14 目, 65 科, 158 属, 205 种。标本保存在中国科学院昆明动物研究所。

Effects of molecular structures on the olfactory responses of phospholipid membranes to four alcohols

In order to understand the relationship between phospholipid molecular structures and their olfactory responses to odorants, we designed and synthesized four phosphatidylcholine analogues with different long hydrocarbon (CH) chains and selected three natural phospholipids with different head-groups. By using interdigital electrodes (IEs) as olfactory sensors (OSs), we measured the responses of the Ifs coated with these seven different lipid membranes to four alcohol vapors in a gas flow system. The Ifs voltage changes were recorded and the voltage-relative saturate vapor pressure (V-P/P degrees) curves were also plotted. It was found that with a methyl (-CH3) placed at the C-8 position in the 18-carbon chain, the olfactory responses could be improved about ten times and with conjugated double bonds (C=C) in the long chains, the sensitivity could be increased by 3 similar to 4 orders of magnitude. As to head-groups, choline is preferred over ethanolamine and serine in phospholipid structures in terms of high olfactory sensitivity: These results are expected to be useful in further designing and manufacturing lipid-mimicking OSs. (C) 1998 Elsevier Science Ireland Ltd. All rights reserved.

LIPID MICRORESISTOR AS MIMICKING OLFACTORY SENSOR - THE RULE OF THE RESPONSE OF LIPIDS TO C-1-C-4 ALCOHOLS

Phosphatidylcholine (PC) and six other PC-similar lipids are coated on interdigital electrodes, IEs, as sensitive membranes. Eight alcohols (C-1-C-4) are tested in a flow system at room temperature. It is found that all responses are log(response)-log(concentration) linear relations. These results agree with Steven's law in psychophysics. Moreover, the thresholds of the sensors are coincident with human olfactory thresholds. The authors have analysed the data of the lipid hypothesis suggested by Kurihara et al. We have found that this hypothesis is also in agreement with Steven's law. Lipid microresistors are real mimicking olfactory sensors. A definition of an olfactory sensor is suggested.

低碳钢在海底沉积物中的腐蚀行为

海底沉积物环境下钢铁的腐蚀和防护问题由于人们对海洋的广泛的开发和利用而逐渐引起人们的注意。本文对钢在海底沉积物中的腐蚀行为进行了模拟海底沉积物环境下的失重实验和电化学测量，以探讨海底沉积物环境下的钢的腐蚀行为和作用机制。失重法埋片实验表明，在没有微生物影响的海底沉积物中，钢的腐蚀速度与海洋腐蚀环境的其它区带相比是较低的。A3钢在砂型海底沉积物中的腐蚀速度约是其在粘土型海底沉积物中腐蚀速度的2倍。另外，主要用电化学方法研究了A3钢在海底沉积物中的腐蚀行为，包括线性极化阻力测量，弱极化区的动电位扫描测量和电化学交流阻抗谱（EIS）测量，计算了A3钢在海底沉积物中腐蚀的有关电化学参数，探讨了A3钢在两种类型海底沉积物中的腐蚀行为差异。认为A3钢在砂型和粘土型海底沉积物中腐蚀速度大小的差别主要是由于作为阴极去极化剂的氧在不同类型海底沉积物中的扩散速度不同。通过弱极化数据拟合和IES测量的结果表明，A3钢在海底沉积物中的腐蚀机制主要是受阴极去极化剂的氧扩散控制作用。并提出了初期腐蚀过程的等效电路和腐蚀模式图。本文较系统的研究了A3钢在海底沉积物中的电化学腐蚀行为，并首次将弱极化曲线拟合技术应用于海底沉积物腐蚀研究，得到了一些有意义的结果。结合A3钢在不同类型海底沉积物中的阻抗谱特征，提出了相应的等效电路和腐蚀模型。

扬子板块西部大陆地幔地球化学特征及壳幔演化－有关基性岩超基性岩的地球化学研究

The continental mantle geochemical characteristics and crust-mantle evolution in the west of Yangtze Plate was discussed through the study of some within-plate basic-ultrabasic rocks from Lower Proterozoic to Later Paleozoic in this paper. In the Lower Proterozoic, the plate subduction between the pre-Tethys Proterozoic Ocean Plate and paleo-Yangtze Plate induced some basic volcanic formed in the island arc-back arc surrounding, which were represented by Ailaoshan Group-Dibadu Formation-Dahongshan Group, and there existed EM I component in the mantle source. The Middle Proterozoic Caiziyuan peridotite was formed in the epicontinental basin at the ocean-land boundary or within-continent rift basin. Its mantle source could be metasomatized by the dehydration fluid of subducted plate, and much initial radioactive ~(143)Nd was added to the source. In the Later Proterozoic, some rifts at the epicontinent or within-continent was formed due to the pre-Tethys oceanic plate subduction, and within-plate hot-spot Dahongshan diabase came into being. The whole-rock isochronal age of diabase is 1066±110Ma, and its mantle source was enriched Nd isotope and trace element which was related to the primary volatile component from asthenosphere and mantle plume. Its mantle source was included "FOZO" component representing mantle plume. The layer ultramafic rocks located at the Panxi Rift in the Middle-Later Paleozoic were resulted from different period and source. The early ultramafic indicated the incipient action of Panxi Rift, which is residue of continental lithospheric partial melting. Its mantle source involved subducted material and had distinct EM II component. The Emeishan basalt in the Later Paleozoic was typical continental flood basalt and its source also contained EM II component. The subduction of paleo-Tethys Ocean Plate provided essential dynamic condition for the large-scale opening of Panxi Rift, while the mantle plume supplied much material for Emeishan basalt. However, the plume was contaminated by the metasomatized continental mantle lithosphere in its upwelling process, which resulted in the Sr isotopic and incompatible elemental enrichment, and the Nd isotope kept down the weak-depleted character of mantle plume. The magmatic history in the west of Yangtze Plate is the tectonic process between pre-Tethys, paleo-Tethys Oceanic Plate and Yangtze Plate in a long history. Due to the subduction of oceanic plate, the crustal source material took part in the crust-mantle evolution widely. the continental mantle lithosphere in the west of Yangtze Plate was metasomatized by the fluid released by the subducted plate and the primary volatile from deeper mantle, and the mantle source include obvious enriched component.

地球化学新方法在隐状矿床找矿预测中的应用研究

With the progress of prospecting, the need for the discovery of blind ore deposits become more and more urgent. To study and find out the method and technology for the discovery of blind and buried ores is now a priority task. New geochemical methods are key technology to discover blind ores. Information of mobile components related to blind ores were extracted using this new methods. These methods were tested and applied based on element' s mobile components migrating and enriched in geophysical-geochemical process. Several kinds of partial extraction techniques have tested based on element' s occurrence in hypergenic zone. Middle-large scale geochemical methods for exploration in forest and swamp have been tested. A serious of methods were tested and applied effetely about evaluation of regional geochemical anomaly, 1:25000 bedrock or soil geochemical methods sampling based on the net in dendritic water system instead of the normal net. 1. Element related with ores can be mobiled to migrate upwards and be absorpted by surface soil. These abnomal components can be concentrated by natural or artificial methods. These trace metalic ions partially exist in dissovlvable ion forms of active state, and partially have been absorbed by Fe-Mn oxide, soil and organic matter in the soil so that a series of reaction such as complex reaction have take place. Employing various partial extraction techniques, metallic ions related with the phase of the blind ores can be extracted, such as the technique of organic complex extraction, Fe-Mn oxide extraction and the extraction technique of metallic ions of various absorption phases. 2.1:200000 regional geochemical evaluation anomaly methods: Advantageous ore-forming areas were selected firstly. Center, concentration, morphological feature, belt of anomaly were choosed then. Geological and geochemical anomalies were combined. And geological and geochemical background information were restrained. Xilekuduke area in Fuyun sheet , Zhaheba area in Qiakuerte sheet, the west-north part in Ertai sheet and Hongshanzui anomaly in Daqiao sheet were selected as target areas, in Alertai, in the north of Xinjiang. in Xilekuduke area, 1:25000 soil geochemical methods sampling based on the net in dendritic water system was carried out. Cu anomaly and copper mineralization were determined in the center area. Au , Cu anomalies and high polarization anomaly were determined in the south part. Prospecting by primary halo and organic complex extraction were used to prognosis blind ore in widely rang outcrop of bedrock. 1:25000 bedrock or soil geochemical methods sampling based on the net in dendritic water system were used in transported overburden outside of mining area. Shallow seismic method and primary halo found a new blind orebody in mining area. A mineralization site was fou and outside of Puziwan gold mine, in the north of Shanxi province. Developing middle-large scale geochemical exploration method is a key technique based 1:200000 regional geochemical exploration. Some conditions were tested as Sampling density , distribution sites of sample, grain size of sample and occurrence of element for exploration. 1:50000 exploration method was advanced to sample clast sediment supplement clast sediment in valley. 1:25000 bedrock or soil geochemical methods sampling based on the net in dendritic water system was applied to sample residual material in A or C horizon. 1:2000 primary or soil halo methods used to check anomalies and determine mineralization. Daliang gold mineralization in the northern Moerdaoga was found appling these methods. Thermomagnetic method was tested in miniqi copper-polymetallic ore. Process methods such as grain size of sample, heated temperature, magnetic separating technique were tested. A suite of Thermomagnetic geochemical method was formed. This method was applied in Xiangshan Cu~Ni deposit which is cover by clast or Gobi in the eastern Xinjiang. Element's content and contrast of anomaly with Thermomagnetic geochemical method were higher than soil anomaly. Susceptibility after samples were heated could be as a assessment conference for anomaly. In some sectors thermo-magnetic Cu, Ni, Ti anomalious were found outside deposits area. There were strong anomal ies response up ore tested by several kind of partial extraction methods include Thermomagnetic, enzyme leach and other partial extractions in Kalatongke Cu-Ni deposit in hungriness area in the northern of Xinjiang. Element's anomalies of meobile were mainly in Fe-Mn oxide and salt. A Copper mineralization site in Xilekuduke anomaly area had been determined. A blind ore was foung by shallow seismic and geochemical method and a mineralization site was found outside this mining area in Puziwan gold deposit in shanxi province. A Gold mineralization site was found by 1:50000 geochemical exploration in Daliang, Inner Mongolia.