小鲵属分子系统发育研究

小鲵属为亚洲特有的有尾两栖类，是小鲵科之模式属。现记载小鲵属动物有29种，占全科物种数一半以上（Frost, 2007），为小鲵科第一大属。该属分布跨越古北界和东洋界，分布于中国、朝鲜、韩国、日本等地区，其系统学研究一直以来颇为中外学者所关注。澄清该属的物种分类问题，阐明其种间的系统发育关系对整个小鲵科的系统演化与分布格局关系的研究具有关键性意义。 本论文以中国及周边地区的小鲵属物种为主要对象，主要利用分子生物学实验与生物信息学途径相结合的手段，运用支序系统学与分子进化生物学理论及分析方法，展开系统发育的研究。在此基础上诠释现存的分类问题，并探讨该属系统发育关系。 研究材料上，本研究采用野外采集与网络下载数据相结合的方法，获取了较为全面的小鲵属物种DNA序列资料。技术手段上，选取了线粒体DNA的Cytb、12S、16S、NADH 2、COI等多个基因部分片段序列，对小鲵属开展了较为全面系统的研究。分析方法上，针对小鲵属物种各类群的具体情况，运用了处于领域前沿的多种分析方法。应用PAUP、MrBayes、Modeltest、Mega等软件，采用了最大简约法（MP）、邻接法（NJ）、贝叶斯推断（BI）及K2P遗传距离分析等方法。 本研究对小鲵属进行了较为全面的系统发育研究，弥补了有关小鲵属系统发育研究的不足，并得出了以下结果： （1）关于豫南小鲵Hynobius yunanicus的有效性，基于细胞色素b序列的系统发育关系联合形态和染色体组型等证据证明了豫南小鲵是商城肥鲵的同物异名。 （2）获得了较为全面的小鲵属物种系统发育树，并以此解释了北海道滞育小鲵、东北小鲵、中国小鲵与义乌小鲵等存在的分类问题。 （3）本研究利用DNA条形码技术对小鲵属及小鲵科物种进行了鉴定，再次证明豫南小鲵为商城肥鲵的同物异名；并认为猫儿山小鲵与挂榜山小鲵为同物异名。 综上，本研究较为完整地勾勒了小鲵属的系统发育关系全貌，并对小鲵属物种的起源进行了推测。 Hynobius, the type genus of the Family Hynobiidae, is the only exclusively Asian salamander genus. This genus which contains 29 species (beyond half of total Family), is the key group in Hynobiidae. The genus distributed across Palaearctic and Oriental Realm, and was found in China, Korea, and Japan. Systematics of genus Hynobius draws attention of researchers all the times. Resolving the taxonomic and phynogenetic questions of Hynobius is very important to the evolutionary research of Family Hynobiidae. Firstly, studies on systematics of genus Hynobius based on morphology, karyotype and molecular phylogeny of Hynobius are reviewed along with existing questions of this genus. The sequential reaserch project of phylogenetics is perspectively outlined. Using molecular data, we compared Hynobius yunanicus with a sympatric species Pachyhynobius shangchengensis. Our cytb sequences associating with karyotypic and morphological data supportted that H. yunanicus is not a valid species, but a synonym of P. shangchengensis. Because of phenotypic plasticity, some morphological characters are not even suitable for identifying hynobiids. The taxonomy of hynobiids is still controversial to a certain extent (Zhao et al. 1993; Fei, 1999; Chen et al. 2001; Zeng et al. 2006) and needs to be resolved by a new method. Here we examined the utility of COI barcoding for the discrimination of hynobiids. Meantime, the taxonomy of this Family was looked-over again. Our result show that the DNA Barcoding based on COI is easier and more rapidly than classic methods. And the DNA Barcodes data supported the actual taxonomy of Hynobiidae. Based on the achievements of our research, the phylogeny of Hynobius was reconstructed including some new species (H. maoershanensis, H. guabangshanensis, etc). Besides the phylogenetics of Hynobius was outlined, some questions and the hypothesis about the origin of genus Hynobius was put out.

南海新生代碱性玄武岩的特征及其地球动力学意义

南海是西太平洋最大的边缘海之一，位于欧亚板块、印-澳板块以及太平洋板块之间。南海海底扩张停止(15.5Ma, Briais et al., 1993) 后的板内火山作用，影响着中国南部、中南半岛、大洋基底和分裂的微大陆片段的广大地区。对南海新生代玄武岩进行地球化学研究，不仅对于理解南海板内火山作用的深部地幔过程有着重要意义，而且对南海形成演化及含油气盆地形成的深部动力学机制有着深远意义。 南海新生代玄武岩K-Ar/Ar-Ar年龄为3.8-7.9Ma, 表明为晚中新世以来的岩浆活动产物，与周边地区的碱性火山岩在年龄上的一致性。岩石学特征表明，南海新生代玄武岩的矿物组合为橄榄石、单斜辉石、斜长石，与特征的碱性玄武岩的矿物组合一致。由橄榄石所计算的南海底潜在地幔温度(Tp)平均值为1661℃, 暗示南海地区下的地幔可能存在热量异常，为海南地区存在地幔柱的观点提供了证据。单斜辉石富钙、钛，由单斜辉石-熔体平衡温压计计算的岩浆房深度分别为：碱玄岩岩浆房深度约49km（对应压力为1.46～1.48 GPa）；粗面玄武岩岩浆房约25km（对应压力为0.76 GPa）；玄武岩岩浆房约15km（对应压力为0.44GPa）。由碱玄岩→粗面玄武岩→玄武岩，平衡温度(K)依次降低:从1535～1498→1429→1369。由斜长石微晶所计算的岩浆喷出地表的温度为989℃。 主量元素特征表明，岩石类型主要为碱玄岩，有少量的粗面玄武岩和玄武岩，属于碱性系列。微量元素方面，大离子亲石元素(LILE)以及高场强元素（HFSE）特别是Nb、Ta、Ti、Y等元素均呈现富集现象，Yb、Sc、Sr以及K、U、Th等生热元素相对亏损，微量元素及稀土元素分布岩石类似板内OIB微量元素的全球平均值。同位素地球化学研究表明，源区存在两个混合端员并具Dupal Pb异常：一个为DMM，位于软流圈或岩石圈地幔中；另一个为EM2源区，可能来自位于核-幔边界处的海南地幔柱而非大陆底岩石圈地幔。研究表明，南半球Dupal异常不存在全球范围内的地区专属性，本区存在的Dupal异常与南半球Dupal异常可能不存在联系。在南海新生代玄武岩的成因过程中，海南地幔柱在为岩石圈地幔的部分熔融作用提供所需的热量同时，也在物质上作出了贡献。南海盆新生代碱性玄武岩由不同程度的部分熔融作用，以及岩浆在上升期间或者在高位岩浆房中的橄榄石等矿物分离结晶作用所形成，同时还可能发生了堆晶作用。构造环境判别表明，玄武岩浆在上升到地表过程中几乎未受到地壳混染。 南海新生代玄武岩的地球化学研究表明，在玄武质岩浆的深部地幔演化过程中，海南地幔柱可能起着重要的作用。通过引入海南岛地幔柱这个概念，本文建立了一个新的有关南海形成演化的初步的概念性模型：（1）50-32Ma，印度洋板块-欧亚板块碰撞及其所导致的太平洋板块后退的综合效应为南海地区提供了一个伸展环境，此伸展环境为地幔柱物质的上升提供了通道；（2）32-21Ma，当地幔柱柱头到达软流圈时, 通过侧向物质流开始同扩张中心发生相互作用，促进了南海的扩张，并在26-24Ma期间发生了洋脊重新就位事件，使扩张中心从原来的18°N附近(即现今西北海盆的中心)调整到15.5°N附近（即现今的东部亚盆）；（3）21-15.5Ma, 随着地幔柱效应的逐渐增强，热点-洋脊相互作用越来越强烈，在大约21Ma发生了洋脊的再次重新就位事件，诱发了西南海盆的扩张；（4）15.5-现在，由于印澳板块前缘与巽他大陆碰撞，使得南海大约在15.5Ma停止扩张,并沿着南沙海槽及吕宋海沟向菲律宾岛弧及巴拉望地块之下俯冲，而南海热点继续活动，在地表处直到第四纪还有碱性玄武岩喷出。

甘肃鼢鼠粪尿气味对侵占行为的影响

气味是哺乳动物个体识别的主要途径，动物气味能传达个体、种、性别和优势地位等化学信息。对地面鼠个体气味识别的研究已有较多报道(Johnston et al., 1993; Johnston et al., 1994; Tang-Martinez et al., 1993)，对地下鼠气味识别研究仅见对鼹形鼠的报道(Heth et al., 1996a, 1996b; Heth et al., 1997; Todrank et al., 1996)。营地下生活的鼠类，如甘肃鼢鼠(Myospalax cansus)、鼹形鼠(Spalax ehrenbergi)等，常独居，终生栖息在自己的洞道内，从不离开并具有领域性和攻击行为。

Adult personality inconsistency and problems with parents: uncovering the roots of the false self

Research has established that individuals who tend to vary their personality depending on who they are with, show a variety of signs of psychological maladjustment in comparison to those who do not; they show more negative affect (Baird, Le and Lucas, 2006), lower life satisfaction (Suh, 2002), lower self-esteem (Sheldon et al., 1997), lower role-satisfaction (Donahue et al., 1993), higher rates of depression (Lutz and Ross, 2003), more anxiety (Diehl, Hastings and Stanton, 2001) and poorer physical health (Cross, Gore and Morris, 2003). It has also been shown that personality variability is positively related to the experience of inauthenticity and falsity (Sheldon et al., 1997). Donahue, Roberts, Robins and John (1993) found that personality inconsistency of this type is related to tension within the family. Psychoanalytic theory has also linked the operation of an adult false self to experiences with parents, particularly in early life (Winnicott, 1960). It was hypothesized that personality variability and the adult experience of falsity in social situations would be related to an emotionally unstable relationship with parents. The method to test this comprised a questionnaire-based survey given to a non-clinical population. The final sample comprised 305, with 193 women and 112 men, aged from 19 to 55. The first questionnaire asked participants to rate personality traits, including emotional stability, in three social contexts - with parents, with friends and with work colleagues. The second part involved 3 questions; participants were asked to select in which of the aforementioned three social contexts they felt “most themselves”; in which they were “most authentic” and in which they “put on a front”. It was found, consistent with predictions, that an index of overall personality variability calculated from the personality questionnaire correlated strongly with emotional instability around parents (r = 0.46, p<0.001), while not correlating with emotional instability in either of the other two contexts measured. This suggests a specific link between a person’s relationship with their parents and their overall personality integration. Furthermore, it was found that participants who cited one of the three social contexts (parents, friends, work colleagues) as being one in which they were “more themselves” or “more authentic” had significantly higher ratings of emotional instability with parents than those participants who found that they were equally authentic across settings (F = 9.8, p<0.005). The results suggest a clear link between a person’s relationships with their parents and their adult personality integration. An explanation is that individuals who experience an anxious or ambiguous attachment with their parents in childhood may fear rejection or abandonment in later life, and so habitually adapt their personality to fit in to social contexts as adults, in order to be accepted by others and to minimize the possibility of social rejection. These individuals meanwhile retain an emotionally unstable relationship with their parents in adulthood. This interpretation is speculative but is open to empirical testing. Clinicians should be aware that attachment problems with parents may underlie poor personality integration in adulthood.

Development and validation of a shipboard system for measuring high-resolution vertical profiles of aqueous dimethylsulfide concentrations using chemical ionization mass spectrometry

A sampling and analytical system has been developed for shipboard measurements of high-resolution vertical profiles of the marine trace gas dimethylsulfide (DMS). The system consists of a tube attached to a CTD with a peristaltic pump on deck that delivers seawater to a membrane equilibrator and atmospheric pressure chemical ionization mass spectrometer (Eq-APCIMS). This allows profiling DMS concentrations to a depth of 50 m, with a depth resolution of 1.3-2 m and a detection limit of nearly 0.1 nmol L-1. The seawater is also plumbed to allow parallel operation of additional continuous instruments, and simultaneous collection of discrete samples for complementary analyses. A valve alternates delivery of seawater from the vertical profiler and the ship�s underway intake, thereby providing high-resolution measurements in both the vertical and horizontal dimensions. Tests conducted on various cruises in the Mediterranean Sea, Atlantic, Indian, and Pacific Oceans show good agreement between the Eq-APCIMS measurements and purge and trap gas chromatography with flame photometric detection (GC-FPD) and demonstrate that the delivery of seawater from the underway pump did not significantly affect endogenous DMS concentrations. Combination of the continuous flow DMS analysis with high-frequency hydrographic, optical, biological and meteorological measurements will greatly improve the spatial/temporal resolution of seagoing measurements and improve our understanding of DMS cycling.

El significado de la prosopopeya de las Leyes en el "Critón" de Platon

El objeto de este trabajo es realizar un estudio iusfilosófico sobre la aparición de las Leyes (nómoi) personificadas de Atenas en el Critón de Platón. La prosopopeya de las Leyes resulta ser un aspecto central para poder comprender la obra, ya que éstas entablan un diálogo imaginario con Sócrates en el cual instalan diversos argumentos filosóficos para fundamentar la autoridad de la pólis. A los fines de identificar el valor argumentativo de este recurso en la obra, analizaré el significado del nómos en la Atenas del siglo V a. C. y la naturaleza de las Leyes en el contexto general del diálogo. Se busca demostrar la importancia que tienen aquéllas para explicar la decisión de Sócrates de beber la cicuta.

A survey of molecular line emission towards ultracompact HII regions

We have used the JCMT to survey molecular line emission towards 14 ultracompact HII regions (G5.89, G9.62, G10.30, G10.47, G12.21, G13.87, G29.96, G31.41, G34.26, G43.89, G45.12, G45.45, G45.47, and G75.78). For each source, we observed up to ten 1 GHz bands between 200 and 350 GHz, covering lines of more than 30 species including multiple transitions of CO isotopes, CH3OH, CH3CCH, CH3CN and HCOOCH3, and sulphuretted molecules. The number of transitions detected varied by a factor of 20 between sources; which were chosen following observations of high-excitation ammonia (Cesaroni et al. 1994a) and methyl cyanide (Olmi et al. 1993). In half our sample (the line-poor sources), only (CO)-O-17: (CO)-O-18, SO, (CS)-S-34 and CH3OH were detected. In the line-rich sources, we detected over 150 lines, including high excitation lines of CH3CN, HCOOCH3; C2H5CN, CH3OH, and CH3CCH. We have calculated the physical conditions of the molecular gas. To reproduce the emission from the line-rich sources requires both a hot, dense compact core and an ambient cloud consisting of less dense, cooler gas. The hot cores, which are less than 0.1 pc in size; reach densities of at least 10(8) cm(-3) and temperatures of more than 80 K. The line-poor sources can be modelled without a hot core by a 20-30 K, 10(5) cm(-3) cloud. We find no correlation between the size of the HII region and the current physical conditions in the molecular environment. A comparison with chemical models (Millar et al. 1997) confirms that grain surface chemistry is important in hot cores.