Lernanthropus antofagastensis sp. nov. (Copepoda: Lernanthropidae) parasitic on Anisotremus scapularis in Chilean waters,and new records of Lernanthropus trachure (Brian, 1903)

Lernanthropus antofagastensis sp. nov., parasitic on Anisotremus scapularis, and inshore fish of Antofagasta, Chile, is described and illustrated. It resembles five other species of Lernanthropus in its dorsal plate and third leg, but can be distinguished from them by a combination of characters. L. trachuri Brian, 1903, is recorded, its male described and illustrated from specimens collected from Seriolella violacea and Trachurus murphy, taken in the same locality.     

第四代管理系统在优化机舱管理中的应用(英文)

机舱被誉为船舶的心脏,为船舶提供主要动力来源.优化机舱管理将对航运效率和安全提供有效保障.结合机舱管理实际,讨论如何运用第四代管理系统的理论进行轮机管理的优化.     

Swedish nemerteans (phylum Nemertea), with description of a new hoplonemertean genus and species

A survey of the nemertean fauna along the Swedish west coast found specimens of 20 genera and 32 species, of which one genus and species is new to science (Tetraneuronemertes lovgreni gen. et sp. n.). The proportions of the three taxa Hoplonemertea, Heteronemertea, and Palaeonemertea are 34, 55, and 11%, respectively, with respect to specimen numbers, and the proportions for species within these taxa are 53, 31 and 16%, respectively. The most common species encountered during the survey were the heteronemerteans Lineus bilineatus, Micrura fasciolata, and Micrura purpurea, the hoplonemertean Nipponnemertes pulcher, and the palaeonemertean Cephalothrix rufifrons.     

广西涉海工程项目建设对海洋环境的影响分析

分析广西涉海工程项目建设现状及其对海洋环境的影响,提出海洋环境保护建议,为广西海洋资源的可持续利用和海洋经济的可持续发展提供参考.     

长江水下三角洲沉积特征与发展趋势

长江水下三角洲是一个以径、潮流相互作用为主的沉积体。野外调查、分析资料证明,在三角洲前缘,沉积物由灰、黄色细、粉沙组成,分选较好。构造见波痕交错层理等,另夹似丘状交错层理风暴沉积层。由于受径流影响,有孔虫、超微属种、个数稀少,随着离河口距离增加,水体加深,前三角洲中沉积物颗粒变细,以粉沙质泥占优,分选变差。有机炭含量较高,潜穴发育。水平、波状层理中,经常出现风暴浊积层。有孔虫属种增至30种,个数几千枚。超微含量以大洋桥石为主,>50％。前三角洲向海,颗粒变为泥质沙,分选差。波痕交错层理。有孔虫属种多于40种,个数上万枚。它反映了三角洲一陆架过渡的浅海沉积环境特点。由于科氏力、径、潮流及苏北沿岸流的作用,长江水下三角洲沉积主体目前正逐步偏向东南,这导致北部不断受改造、废弃。     

船用螺旋桨盘前方诱导速度计算

提出了计算船用螺旋桨盘前方诱导速度场的计算模型及方法。假定桨前方诱导速度可由三部分组成，即ｕ＝ｕＬ＋ｕｂ－ｕＦ，ｕＬ为由 Ｌｅｒｂｓ诱导因子法所计算的诱导速度；ｕＦ为由场点至桨盘处自由涡系在场点处所产生的诱导速度；ｕｂ为桨盘处附着涡在场点处所产生的诱导速度。这三部分诱导速度计算均十分简单，从而避免了由桨盘处开始向后泄向无穷远处自由涡系在场点处所产生的诱导速度计算时所必须进行的一无限数值积分，计算方法中计入了桨叶有限叶数的影响。所作实例计算与试验结果比较，吻合良好。     

细粒泥沙颗粒分析中的反絮凝技术

本文分析了导致细粒泥沙水中絮凝的因素,探讨了絮凝和分散的机理,给出了一个反絮凝的物理模型.在大量科学实验基础上,文章提出了一整套包括化学分散和物理分散方法的反絮凝技术,补充和纠正了现行细粒泥沙颗分方法的不足.本文的反絮凝技术已为许多工程部门完成了总数以万计的沙样颗分,其有效性经受了充分考验.     

长江水下三角洲沉积特征与发展趋势

长江水下三角洲是一个以径、潮流相互作用为主的沉积体。野外调查、分析资料证明,在三角洲前缘,沉积物由灰、黄色细、粉沙组成,分选较好。构造见波痕交错层理等,另夹似丘状交错层理风暴沉积层。由于受径流影响,有孔虫、超微属种、个数稀少,随着离河口距离增加,水体加深,前三角洲中沉积物颗粒变细,以粉沙质泥占优,分选变差。有机炭含量较高,潜穴发育。水平、波状层理中,经常出现风暴浊积层。有孔虫属种增至30种,个数几千枚。超微含量以大洋桥石为主,>50％。前三角洲向海,颗粒变为泥质沙,分选差。波痕交错层理。有孔虫属种多于40种,个数上万枚。它反映了三角洲一陆架过渡的浅海沉积环境特点。由于科氏力、径、潮流及苏北沿岸流的作用,长江水下三角洲沉积主体目前正逐步偏向东南,这导致北部不断受改造、废弃。     

近海沉积物二组分吸附模式与有机物的吸附

将天然沉积物视为有机质和无机质组成的二组分吸附剂，提出了二组分吸附模式。用该模式研究了大连近海沉积物对六氯乙烷和邻苯二甲酸二正丁酯的吸附行为，分别得出大连近海只物中的有机质和无机质对两种有机物的吸附规律、吸附能力和对吸附贡献大小。通过实测数据和模式计算数据的比较，评价了该模式的合理性和可靠性。     

Re-evaluation of the phylogenetic position of the genus Dexiotrichides (Protozoa, Ciliophora, Scuticociliatida) inferred from stomatogenetic and molecular information for Dexiotrichides pangi

The divisional process and systematic position of the marine scuticociliate Dexiotrichides pangi are studied. Based on both stomatogenetic data and 18S rDNA gene sequences, the phylogeny and morphogenetic characteristics of this taxon, and of other related genera, are analyzed and discussed. Both the divisionary events and the molecular biological data indicate that this speciesgenus, together with certain other genera in the Dexiotricha-complex, occupies an intermediate position between the tetrahymenids and the “typical” scuticociliate, which suggests that the Dexiotricha-like taxa should be excluded from the “true” scuticociliates. As a further contribution, the process of stomatogenesis in D. pangi can be summarized as follows: (1) The oral primordia in the opisthe are formed only by the proliferation of basal bodies in the scutica field, which subsequently develop into three membranelles, while the new paroral membrane seems to be generated by the sub-anterior portion of somatic kinety 1 (the 1st postoral intercalary kinety). The latter character exhibits a mode similar to Tetrahymena. (2) In the proter the parental membranelles are retained and remain unchanged throughout the entire division process; only the old paroral membrane is disassembled and differentiated into the anlage, which then gives rise to the new paroral membrane and the scutica of the proter. The 18S rRNA gene sequence reported here is the first one for a ciliate in the Dexiotricha-complex.