古田山大样地木本植物根萌现状及优势种群根萌空间格局分析

　　已有研究表明，萌生现象对森林恢复和植被演替等生态过程中具有及其重要的意义，作为一种可以和种子繁殖“抗衡”的直接的再生方式，森林萌生更新已受到越来越多的关注。近年来萌生生态学的研究主要针对于萌生的生态功能如对个体生活史策略的影响、在植被演替中的作用、对物种多样性影响等方面，研究的切入点大多注重相关的环境因子、遗传因子或自然和人为干扰如砍伐、火烧、大风等引起的萌生现象，针对原始森林演替的研究相对较少，针对“长期动态监测样地”的萌生现象则更少。由于长期动态观测样地具有固定和长期观察的特有优点，这对物种共存、格局及维持机制、植被演替等生物多样性热点问题的研究带来了难得的机遇和条件。 我国是地球上亚热带常绿阔叶林分布面积最广，发育最为典型的区域，我国亚热带常绿阔叶林的生物多样性极高,仅次于热带雨林。目前对亚热带常绿阔叶林物种共存、分布格局、群落演替等的研究相对较少。参照美国史密森热带研究所的热带森林研究中心(Center for tropical forest science，CTFS)森林动态样地的操作规范，中国森林生物多样性研究网络在中国从南到北按主要森林类型建立了5块20～25hm2的森林大样地。作为中国森林生物多样性长期监测网络的重要组成部分，古田山样地分布着典型的中亚热带常绿阔叶林。本论文在24hm2古田山中亚热带常绿阔林长期监测样地调查的基础上，重点从古田山大样地木本植物根萌现状及优势种群根萌空间格局等方面进行具体分析，试图了解古田山大样地根萌植物的种类组成、个体大小、数量、地理区系成分特点等基础特征，同时选择大样地乔灌木层的优势树种，重点分析优势种群根萌的空间分布格局及其特点，以便加深了解优势物种根萌的种内、种间的共存关系，也将对优势植物根萌植物的分布和样地生境的关系作出有益尝试。本文最后通过比较优势物种的主干和根萌空间分布格局等方面的相关性进一步揭示根萌在群落组成中的地位和作用。本研究将为亚热带常绿阔叶林根萌植物的长期动态研究积累基础资料，对了解常绿阔叶林根萌植物现状以及空间分布格局等方面起到积极的探索意义，同时对揭示根萌现象在亚热带常绿阔叶林物种多样性维持机制中的地位和作用也将起到一定的推动作用。

遥感研究南海台风引起的冷迹特征

海表面温度（Sea Surface Temperature, SST）是海洋生态环境变化的重要因子，也是海洋观测研究的最重要的因子之一。海表温度场表征了海洋热力、动力过程和海洋与大气相互作用的综合结果，是反映海气热量、动力和水汽交换的重要参量，也是气候变化及海洋营养盐浓度和初级生产力的重要影响因子。台风过后通常会在上层海洋引起冷迹，即台风路径附近的海表温度降低。海表温度的变化是台风与海洋之间能量交换的关键，对于台风的产生，演化和强度变化有非常重要的作用。因此，研究上层海洋对台风的响应，特别是海表温度对台风的响应过程有非常重要的科学意义。本研究主要利用微波SST逐日数据资料统计研究了海表面温度对南海台风的响应过程，并分析了中尺度涡（特别是气旋性涡）对台风所引起的降温幅度和降温位置的影响作用。在此研究基础上初步尝试提出了一种新的量化台风降温效应的方法。 首先，本研究以1998-2009年总共12年内经过中国南海的92个台风为研究对象，利用逐日连续的微波TMI及TMI-AMSER海表温度数据资料分析了92个台风所引起的最大降温幅度以及冷迹位置的分布特征。统计结果表明有64个（69.6%）台风引起了海表温度明显的降低（降温≥2oC），而对最大降温出现的位置进行分析发现：有超过半数（56个）的台风引起的最大降温位于台风路径的附近或路径右侧，同时还有8个（8.7%）台风引起的最大降温明显位于路径的左侧。文中选取了冷迹相对于台风路径出现在不同位置（左、右、附近）的4个台风为例来说明台风引起的降温特征。通过量化降温中心到台风路径的距离发现台风所引起的最大降温出现的位置主要集中分布在路径左右两侧100km范围内。另外，通过对比台风来之前的海平面高度距平发现先于台风之前处在于上层海洋环境的冷涡，特别是强冷涡，在台风引起的海表面降温幅度和位置分布中可能起着重要的作用，其中冷涡的位置与台风所引起的最大降温中心出现的位置有很好的相关性。 其次，本研究提出一个新的描述降温效应的指数。台风所经过的海域往往会出现海表温度的降低，而海表温度的变化对海洋生态系统有很重要的影响。台风的降温效应因台风、背景温度场和台风前的海洋环境条件而异。目前，海表温度对台风的响应效应主要是通过三个物理量来描述，降温幅度、冷迹范围、冷迹持续时间。但是还没有一个综合的量来对台风的降温效应进行定量的描述。本研究利用遥感微波SST数据尝试初步

南海北部区域表层水微生物多样性及其分布特点研究

海洋中的微生物多样性是十分丰富的。南海北部区域表层水的微生物群落结构及物种多样性情况仍不十分清楚。本研究，采用构建基因克隆文库的方法，对该区域内表层水中的微生物多样性及分布特点进行研究。获得了8000多个细菌16S rDNA基因、真核微生物ITS 区基因及光合微型生物 psbA 基因单克隆。本研究结果表明：在南海北部区域表层水中存在两种不同微生物类群，即近海岸带海洋微生物类群和开阔海域海洋微生物类群。 16S rDNA基因克隆文库中，确定了507个OTUs。93.7% 的16S rDNA 序列定义在同一种水平上，1.4 %的16S rDNA序列定义在同一属的水平上，2.7%的16S rDNA序列定义在同一纲的水平上，1.2%的16S rDNA序列定义在同一门的水平上。值得一提的是有0.7%的南海表层水样品的16S rDNA 序列，属于目前数据库中的未知序列。系统育树分析表明这类序列可归属于4个不同的分枝群。与Venter’s Sorcerer II 海洋科考（马尾岛海域）的结果不同，南海北部区域表层水中，并没有发现SAR11分支细菌、丝状杆菌（Fibrobacter）和Rheinheimera细菌序列，但南海北部区域却发现了马尾岛海域未检测到的物种，如酸杆菌门、恐球菌-栖热菌门、厚壁菌门，硝化螺旋菌门，浮霉菌门以及疣微菌类细菌。除疣微菌外，其他5种细菌都是海洋环境样品中较为常见的细菌。变形菌门、蓝细菌及厚壁菌门细菌序列是南海北部表层样品16S rDNA基因克隆文库中的主要类群。 真核生物如浮游植物和海洋真菌是海洋表面生物质的主要组成部分之一。现有的研究多集中在环境样品的原核微生物的群落结构研究上，很少关注海洋微型真核生物的多样性及群落结构分布。本研究通过构建ITS基因克隆文库的方法，得到了3044条ITS序列，最终定义了1288个OTUs。其中，329个OTUs序列定义在同一种水平上，310个OTUs序列定义在同一属或纲的水平上，123个OTUs序列定义在同一门的水平上。值得注意的是有339个OTUs的序列，属于目前数据库中的未知序列。系统发育树分析表明它们分别归属于4个不同的分枝群。这表明以往对海洋真核微型生物的多样性仍知之甚少。盘菌亚门、体腔动物门和担子菌纲是南海北部表层样品ITS基因克隆文库中的主要类群。此外，在南海北部区域还发现了少数归属于绿藻、链形植物、定鞭金藻类、放射虫类、Stramenopiles、Typhlocoela、壶菌类、多孢囊霉目、子囊菌门、地位未定的物种、 酵母、领鞭毛虫门、不可培养的后生动物和海绵动物的ITS序列。 海洋初级生产力主要是依靠光合微型浮游生物进行光合作用完成的。利用新设计的psbA通用引物，对南海北部33个表层水样滤膜进行基因克隆文库建库分析，最终获得了南海北部区域表层水微生物多样性及其分布特点研究3062条部分psbA基因序列，并将其划分为957个 OTUs。其中蓝细菌和未培养的病毒序列在psbA基因库中的数量最多。本研究还发现了南海北部区域存在11个独立分支的新型psbA类群。研究证实psbA基因可以作为一种研究海洋光合微型浮游生物群落结构的指示基因。 克隆文库相似性分析发现，在所有的16S rDNA克隆文库中没有任意两个站点的克隆文库相似性超过50%。虽然N401和N420站点的16S rDNA克隆文库相似性最大，但它们在地理位置上并不接近。一些地理位置接近的站点，其16S rDNA克隆文库之间相似性比较接近。比如，海南岛区域的克隆文库之间就比较相似，且在同一分支。大多数地理环境相似的站点的16S rDNA克隆文库都聚在同一大分支上。例如，来自于珠江口区域站点的克隆文库之间的相似性比较接近，而且分布在一个大分支中；开阔海洋区域的16S rDNA克隆文库，也大多聚类在同一分支中。但也有例外的情况：比如 N107 和N400 站点的16S rDNA克隆文库，就聚类到一起，分析发现这两个文库中所处的环境都是甲烷产生区，其中都含有相似的与甲烷代谢相关的菌群。不过从整体来看，整个南海北部的细菌群落，大致分为两大类：中国大陆近海岸微生物群落和开阔海域微生物群落。33个ITS克隆文库的相似性分析发现：相似性在10%以下的类群，可以分成两大分支，而且该分类，比细菌群落的分布情况更接近南海北部的地理环境特征。对psbA基因克隆文库的相似性分析也验证了在南海北部区域表层水中存在两种不同微生物生态系统。 此外，本研究针对分子生态专业软件DOTUR程序在处理大量克隆文库数据时所遇到的

Bacillus pallidus sp nov., isolated from forest soil

A Gram-positive bacterium, designated strain CW 7(T), was isolated from forest soil in Anhui Province, south-east China. Cells were strictly aerobic, motile with peritrichous flagella and rod-shaped. The strain grew optimally at 30-37 degrees C and pH 7.0-8.0. The major fatty acids of strain CW 7(T) were anteiso-C-15:0, iso-C-15:0 and anteiso-C-17:0. The predominant menaquinone was MK-7. The cell-wall peptidoglycan contained meso-diaminopimelic acid. The G + C content of the genomic DNA was 42.3 mol%. Phylogenetic analysis indicated that strain CW 7(T) belonged to a monophyletic cluster within the genus Bacillus and showed 16S rRNA gene sequence similarities of less than 96.5% to recognized species of the genus Bacillus. The results of the polyphasic taxonomic study, including phenotypic, chemotaxonomic and phylogenetic analyses, showed that strain CW 7(T) represents a novel species of the genus Bacillus, for which the name Bacillus pallidus sp. nov. is proposed. The type strain is CW 7(T) (=KCTC 13200(T)=CCTCC AB 207188(T)=LMG 24451(T)).

Polychlorinated dibenzo-p-dioxin and dibenzofurans (PCDD/Fs), polybrominated diphenyl ethers (PBDEs), and polychlorinated biphenyls (PCBs) monitored by tree bark in an E-waste recycling area

To investigate the environmental levels and profiles of polychlorinated dibenzo-p-dioxins and dibenzofurans (PCDD/Fs), polybrominated diphenyl ethers (PBDEs), and polychlorinated biphenyls (PCBs), tree bark samples (n = 22) were collected from Luqiao, an E-waste recycling area, in east China in July 11-13, 2006. The average concentrations of PCDD/Fs, PBDEs, and PCBs determined by isotope dilution-high resolution gas chromatography (HRGC) coupled with high resolution mass spectrometer (HRMS) were 0.1 +/- 0.0, 1.4 +/- 0.2, and 6.5 +/- 0.8 lg g (1) lipid weight, respectively. PCDD/F-toxic equivalent (TEQ, WHO-1998), PCB-TEQs, and total dioxin-like TEQs were 1.3 +/- 0.1, 0.5 +/- 0.0, and 1.8 +/- 0.2 ng g (1) lipid weight, respectively. The profiles of these pollutants in the tree bark were also discussed. Tetra-CDFs, deca-BDE and tri-CBs were the main homologues and accounted for 47% of total PCDD/Fs, 79.3% of total PBDEs, and 33.2% of total PCBs, respectively; As for TEQs, 2,3,4,7,8-PeCDF and PCB126 were the main contributors and accounted for 36% of the total PCDD/F-TEQs and 81.2% of the total PCB-TEQs, respectively. High accumulation of PCDD/Fs, PBDEs, and PCBs detected in the tree bark indicated heavy contaminations of these pollutants in Luqiao area. (C) 2008 Elsevier Ltd. All rights reserved.

Elevated levels of urinary 8-hydroxy-2'-deoxyguanosine in male electrical and electronic equipment dismantling workers exposed to high concentrations of polychlorinated dibenzo-p-dioxins and dibenzofurans, polybrominated diphenyl ethers, and polychlorinated biphenyls

To investigate the occupational exposure levels to polychlorinated dibenzo-p-dioxins and dibenzofurans (PCDD/Fs), polybrominated diphenyl ethers (PBDEs), and polychlorinated biphenyls (PCBs), indoor dust (n = 3) in workshops and hair samples from male workers (n = 64) were collected at two electrical and electronic equipment waste (E-waste) dismantling factories located in the LQ area in east China in July 11-13, 2006. Pre- and postworkshift urines (64 of each) were also collected from the workers to study oxidative damage to DNA using 8-hydroxy-2'-deoxyguanosine (8-OHdG) as a biomarker. The concentrations of PCDD/Fs, PCDD/F-WHO-TEQs, PBDEs, PCBs and PCB-WHO-TEQs were (50.0 +/- 8.1) x 10(3), 724.1 +/- 249.6, (27.5 +/- 5.8) x 10(6), (1.6 +/- 0.4) x 10(9), (26.2 +/- 3.0) x 10(3) pg/g dry weight (dw) in dust, and (2.6 +/- 0.6) x 10(3), 42.4 +/- 9.3, (870.8 +/- 205.4) x 10(3), (1.6 +/- 0.2) x 10(6), 41.5 +/- 5.5 pg/g dw in hair, respectively. The homologue and congener profiles in the samples demonstrated that high concentrations of PCDD/Fs, PBDEs, and PCBs were originated from open burning of E-waste. The 8-OHdG levels were detected at 6.40 +/- 1.64 mu mol/mol creatinine in preworkshift urines. However, the levels significantly increased to 24.55 +/- 5.96 mu mol/mol creatinine in postworkshift urines (p < 0.05). Then, it is concluded that there is a high cancer risk originated from oxidative stress indicated by the elevated 8-OHdG levels in the E-waste dismantling workers exposed to high concentrations of PCDD/Fs, PBDEs, and PCBs.

The methane hydrate formation and the resource estimate resulting from free gas migration in seeping seafloor hydrate stability zone

It is a typical multiphase flow process for hydrate formation in seeping seafloor sediments. Free gas can not only be present but also take part in formation of hydrate. The volume fraction of free gas in local pore of hydrate stable zone (HSZ) influences the formation of hydrate in seeping seafloor area, and methane flux determines the abundance and resource of hydrate-bearing reservoirs. In this paper, a multiphase flow model including water (dissolved methane and salt)-free gas hydrate has been established to describe this kind of flow-transfer-reaction process where there exists a large scale of free gas migration and transform in seafloor pore. In the order of three different scenarios, the conversions among permeability, capillary pressure, phase saturations and salinity along with the formation of hydrate have been deducted. Furthermore, the influence of four sorts of free gas saturations and three classes of methane fluxes on hydrate formation and the resource has also been analyzed and compared. Based on the rules drawn from the simulation, and combined information gotten from drills in field, the methane hydrate(MH) formation in Shenhu area of South China Sea has been forecasted. It has been speculated that there may breed a moderate methane flux below this seafloor HSZ. If the flux is about 0.5 kg m-2 a-1, then it will go on to evolve about 2700 ka until the hydrate saturation in pore will arrive its peak (about 75%). Approximately 1.47 109 m3 MH has been reckoned in this marine basin finally, is about 13 times over preliminary estimate.

Energy level analyses of even-parity J=1 and 2 Rydberg states of Sn I by multichannel quantum defect theory

This paper analyzes the energy levels along the even-parity J=1 and 2 Rydberg series of Sn I by multichannel quantum defect theory. A good agreement between theoretical and experimental energy levels was achieved. Below 59198 cm~(-1), a total of 85 and 23 new energy levels, respectively, in the J=1 and J=2 series, which cannot be measured previously by experiments, are predicted in this work. Based on the calculated admixture coefficients of each channel, interchannel interactions were discussed in detail. The results are helpful to understand the characteristics of configuration interaction among even-parity levels in Sn I.

中国南海深海沉积物中的微生物资源

由于采样条件和培养条件的限制，深海微生物研究的较少，因此目前海洋微生物资源的研究主要集中在近海和浅海。而深海独特的生态环境，使微生物形成了独特的代谢体系，成为新颖化合物的重要来源，具有很好的开发应用前景。本文首次较为系统的研究了深度为1758-3600m南海海底沉积物中深海微生物资源的分离和活性菌株的筛选情况，旨在为探索我国南海深海微生物资源提供一定的科学依据。 采用多种分离培养基从6个不同深度（1758、2620、3200、3500、3587和3600m）的南海深海沉积物样品中，分离到225株深海微生物，包括40株放线菌和185株细菌。以分离得到的225株深海微生物为研究对象，从产蛋白酶、抗真菌、杀虫三个方面进行活性菌株的筛选，研究南海深海沉积物中的微生物资源状况： （1）.将分离到的225株深海微生物，同时在10℃、28℃、45℃三个温度下进行产低温蛋白酶、中温蛋白酶、高温蛋白酶的筛选。初筛结果表明：这225株深海微生物大都有大小不同的产蛋白酶能力。10℃有产蛋白酶的有109株，28 ℃产蛋白酶的有160株，45℃产蛋白酶的有117株。筛选到一株在45℃下有较强产蛋白酶能力的菌株B1394，其酶活可达873U/ml，有一定的应用前景。通过形态观察、生理生化测定、16SrDNA序列测定，将B1394定名为枯草芽孢杆菌（Bacillus subtilis）。其粗酶液性质研究发现：最适酶活温度60℃，最适pH 8.0， 40℃、50℃和60℃热稳定性较好， Mn2+ 、Mg2+ 、Ca2+对该蛋白酶有激活作用，Hg2+ 、Fe3+ 、Cu2+ 、Zn2+ 、 Fe2+对其有抑制作用，苯甲基磺酰氟（PMSF）几乎完全抑制其活性，推断为丝氨酸蛋白酶。 （2）.对其中100株深海细菌和40株深海放线菌，以立枯丝核菌（ Rhizoctonia solani）和白色念珠菌（Candida albicans）为靶菌进行了抗真菌活性的筛选。初筛结果表明：分别有37株和35株深海细菌对立枯丝核菌和白色念珠菌有抑菌活性，分别占被检测细菌数目的37%和35%；有18株深海放线菌对立枯丝核菌有抑制作用，占被检测放线菌总数的45%。筛选到一株有较强抗真菌活性的深海放线菌SHA6，其发酵液对包括尖孢镰刀菌（Fusarium oxysporum）在内的10种植物病原菌有明显的抑制作用。对其发酵液的理化性质进行初步研究发现SHA6发酵液具有良好的热稳定性和酸碱稳定性, 对SHA6进行分子生物学鉴定后将其初步定名为为橙色单胞菌（Aurantimonas altamirensis）。 （3）.以卤虫为初步筛选模型，对其中的20株深海放线菌进行了杀虫方面的筛选，结果发现有5个深海放线菌菌株表现有较强的杀虫活性。其中深海放线菌SHA4发酵液的乙酸乙脂提取物杀卤虫的活性最强，在浓度为100μg/ml时杀卤虫活性为83%,而在浓度400ppm时，48h可以杀死38%的甜菜夜娥。对SHA4进行分子生物学鉴定后将其初步定为拟诺卡氏菌属（Nocardiopsis sp）。 总之，本论文阐明了我国南海深海沉积物中微生物资源状况的初步研究结果，为进一步开发利用我国南海深海微生物资源奠定了基础。

Optimizing the formation of in vitro sponge primmorphs from the Chinese sponge Stylotella agminata (Ridley)

The establishment and optimization of in vitro primmorph formation from a Chinese sponge, Stylotella agminata (Ridley), collected from the South China Sea, were investigated. Our aims were to identify the key factors affecting primmorph formation in this species and to optimize the technique for developing an in vitro primmorph culture system. The size of dissociated cells from S. agminata is relatively small, in the range between 5 and 10 mum. Round-shaped primmorphs of less than 100 gm were formed 3 days after transferring the dissociated cells into seawater containing Ca2+ and Mg2+. The effect of various cell dissociation conditions, inoculum. cell density, concentration of antibiotics, pH, and temperature was further investigated upon the formation of primmorphs. The time required for primmorph formation, primmorph size distribution, and the proliferating capability were microscopically documented. Healthy sponge S. agminata, inoculum. cell density and culture temperature play a critical role for the successful formation of primmorphs and that the microbial contamination will have to be controlled. (C) 2002 Elsevier Science B.V. All rights reserved.

Web-based spatiotemporal visualization of marine environment data

With long-term marine surveys and research, and especially with the development of new marine environment monitoring technologies, prodigious amounts of complex marine environmental data are generated, and continuously increase rapidly. Features of these data include massive volume, widespread distribution, multiple-sources, heterogeneous, multi-dimensional and dynamic in structure and time. The present study recommends an integrative visualization solution for these data, to enhance the visual display of data and data archives, and to develop a joint use of these data distributed among different organizations or communities. This study also analyses the web services technologies and defines the concept of the marine information gird, then focuses on the spatiotemporal visualization method and proposes a process-oriented spatiotemporal visualization method. We discuss how marine environmental data can be organized based on the spatiotemporal visualization method, and how organized data are represented for use with web services and stored in a reusable fashion. In addition, we provide an original visualization architecture that is integrative and based on the explored technologies. In the end, we propose a prototype system of marine environmental data of the South China Sea for visualizations of Argo floats, sea surface temperature fields, sea current fields, salinity, in-situ investigation data, and ocean stations. An integration visualization architecture is illustrated on the prototype system, which highlights the process-oriented temporal visualization method and demonstrates the benefit of the architecture and the methods described in this study.

Polyaniline as marine antifouling and corrosion-prevention agent

Conductive polyaniline was found to have special marine antifouling property. The coating from conducting polyaniline and epoxy resin(or polyurethane) can last 6-9 months in Southern China sea, i.e., less than 10% of the coating surface was fouled during this period. The conducting polyaniline has special synergetic antifouling effect on other antifouling agents like cuprous oxide or 4, 4'-dichlorodiphenyltrichloroethane. The conductivity of the polyaniline was found to be extremely important for its antifouling effect. Moreover, employing aliphatic polyamine as solvent of emeraldine base and curing agent of epoxy resin, a new technique to process corrosion prevention coating containing emeraldine base was developed, therefrom the emeraldine base and epoxy resin was in molecular level blending. This technique was solvent free and extremely effective, i.e., only 1wt% of emeraldine base in the coating can have good corrosion prevention property.

Cultivation of the brown alga Sargassum horneri: sexual reproduction and seedling production in tank culture under reduced solar irradiance in ambient temperature

As a large conspicuous intertidal brown alga, individuals of Sargassum horneri can reach a length of more than 7 m with a fresh weight of 3 kg along the coasts of the Eastern China Sea. The biomass of this alga as a vital component in coastal water ecology has been well documented. In recent years, a steady disappearance of the algal biomass along the once densely populated coastal areas of the Eastern China Sea has drawn attention in China. Efforts have been made to reconstruct the subtidal algal flora or even to grow the alga by use of long-lines. As part of the efforts to establish an efficient technique for producing seedlings of S. horneri, in this investigation a series of culture experiments were carried out in indoor raceway and rectangular tanks under reduced solar irradiance at ambient temperature in 2007-2008. The investigation demonstrated that: (1) sexual reproduction of S. horneri could be accelerated in elevated temperature and light climates, at least 3 months earlier than in the wild; (2) eggs of S. horneri had the potential to be fertilized up to 48 h, much longer than that of known related species; (3) suspension and fixed culture methods were both effective in growing the seedlings to the long-line cultivation stage; and (4) the life cycle of S. horneri in culture could be shortened to 4.5 months, thus establishing this alga as an appropriate model for investigating sexual reproduction in dieocious species of this genus.

Using otolith weight to predict the age of Pennahia macrocephalus in the mouth of the Beibu Gulf

The relation between otolith weight (OW) and the age of marine fish is studied. A total of 222 individuals of bighead white croaker, Pennahia macrocephalus were sampled seasonally in the mouth of the Beibu Gulf, the South China Sea, in 2007. Since there are no significant differences in sagittal OW between otolith in pairs (Pa parts per thousand yen0.05), the undamaged left sagittal otolith is used for age determination. The highest correlations among standard length, OW and fish ages are confirmed by linear, exponential and multinomial regression. Results show that sagittal OW overlaps only occasionally among age groups, and to individuals with similar standard length, the older and slower-growing fish has a heavier otolith because of the continued otolith material deposition. There are differences in sagittal OW among different age groups and significant positive linear relationship with age (P < 0.05). The age readings can be verified by plotting the sagittal OW versus the standard length for age groups, and the individuals with similar standard length but in different ages can be separated by sagittal OW frequency analysis. Mostly, the predicted ages using the regression between sagittal OW and ages are closed to the observed ages by counting annulus on scale. It indicates that the sagittal OW analysis is a useful technique for validating the accuracy of age determination by annuli counts, especially for individuals of similar size. Furthermore, the technique is applied for Pennahia macrocephalus with discussion in this paper.

Research on crustal structure and lithosphere property in the Okinawa Trough area

A mass of geological, geophysical and geochemical data and information from the Okinawa Trough area are collected for comprehensive research in the study area from East China to Okinawa Trough and then to Ryukyu Island Are region. According to the seismic tomography result (P and S wave) and the processing result of free-air and Bouguer gravity anomaly and magnetic anomaly data in the study area, the comprehensive interpretation is carried out. The Moho depth distribution of the study area is obtained by the inversion calculation based on gravity data using the Harmonious Series method. The crust properties are analyzed. Meantime, some Cenozoic basalt data from Kuandian (NE China), Hannuoba (North China), Minxi (South China), Penghu Islands (Taiwan Strait), Okinawa Trough and Japan Island Arc regions are chosen to make the comparison research on element- isotopes. The result indicates that the lithosphere thickness in the Okinawa Trough area has obviously decreased, where a Low -velocity layer of upper-mantle has reached the Moho interface and the metasometized asthenosphere has formed. The research result on element- isotopes shows that the characteristic of the crust in the Okinawa Trough area is different from that in East China area and the Ryukyu Island Arc area. It is considered that the crust in the Okinawa Trough area belongs to the transition type, which is quite similar to the feature of the oceanic crust.