基于.NET的事务处理

介绍了事务处理的基本原理,讨论了.NET中的事务处理,说明了ADO.NET和消息队列中的手动事务处理,以及ASP.NET、XML Web service、.NET Framework类中的自动事务处理,并对.NET中的各种事务处理给出了实施的方法,为利用.NET构建具有事务处理的企业应用提供了参考.     

A new species of Cerithium （Gastropoda： Cerithiidae） from the South China Sea

Specimens of a new species of Cerithiidae, Cerithium mangrovum n. sp., were collected during two surveys along the coasts of Hainan and Guangdong Province, China. Usually associated with potamidid snails, this species often occurs in large populations between the mid-high tidal zones in a range of habitats, including mangroves, grass beds, silt, mud, and coral reefs. C. mangrovum n. sp. has a slender and tapering shell and the straight-sided whorl bears three aligned beaded spiral cords. The thick outer lip has a wide posterior sinus. It morphologically resembles C. coralium Kiener, 1841. The shell of C. coralium is usually larger and wider and the spiral cords are not as beaded as in C, mangrovum n. sp. Its radula has a rachidian tooth with a shallow, wide, median basal projection while the rachidian tooth of C. mangrovum n. sp. has a moderately long, median basal projection.     

Identification of Species in Genus Platycephalus from Seas of China

Platycephalus in Chinese sea area has a high commercial value.However,there were mis-identifications in previous records.In this study,we fully distinguished and diagnosed all five species,Platycephalus indicus,P.cultellatus,Platycephalus sp.,Platycephalus sp.1 and Platycephalus sp.2.The results revealed that P.cultellatus was overlooked by previous ichthyologists.Platycephalus sp.1 was misidentified as P.indicus in reality,and Platycephalus sp.2 only existed in the seas of Japan.Furthermore,morphological,especially phylogenetic analysis indicated that Platycephalus sp.from South China Sea differs from all former known species,which might be a new species.We identified all Platycephalus species in China seas for the first time,which will contribute to local species identification,biodiversity conservation and sustainable exploitation of Platycephalus species.     

Medusa consumption and prey selection of silver pomfret Pampus argenteus juveniles

The current study explored Aurelia aurita and Rhopilema esculent um consumption by silver pomfret juveniles, as well as their prey selection between the two jellyfi sh species. Silver pomfret juveniles weighing 1±0.1 g actively preyed on both the species. Their daily A. aurita consumption was 11.6 times their own body weights regardless of the size of A. aurita medusae. Their daily R. esculent um consumption was 13, 9.1, 5, and 4.1 times their own body weights when the R. esculentum medusae were 10, 20, 30, and 40 mm in bell diameter, respectively. The survival rates of the R. esculent um were higher than those of the A. aurita. When the R. esculent um medusae were more than 30 mm in bell diameter, their survival rate exceeded 92%. Silver pomfrets serve as a type of potential predators on A. aurita in coastal waters, and they have little infl uence on R. esculent um with a size exceeding 30 mm. Besides, A. aurita may be able to be used as fi sh prey in silver pomfret artifi cial breeding.     

Ciliates in the Marsh Wetlands of Chongming Island: Taxonomy of Five Species and a Species List

To clarify the confusion surrounding species identification and state intraspecific variations, this research studied the morphological taxonomy of five species, Kentrophyllum cf. setigerum Petz et al., 1995; Zosterodasys shumerica Aliev, 1990; Frontonia tchibisovae Burkovsky, 1970; Neourostylopsis orientalis Chen et al., 2013; and Apoholosticha cf. sinica Fan et al., 2014, which were collected from Chongming Island's marsh wetlands. Kentrophyllum cf. setigerum possesses less somatic kineties than K. setigerum(19–26 right and 18–25 left kineties vs 35–40 right and 30 left kineties). Whether Z. shumerica is identical to Z. transversa Foissner et al., 1994, which was presented in a previous report, was negated. The improved diagnosis for the species is provided. Frontonia tchibisovae was confirmed to have three or four micronuclei, and the number of kinetosome rows in its peniculus 3 varied between China and Russia populations. The new population of N. orientalis bears cortical granules, which differs from the original population that has an arrangement of rows across the dorsal bristles. For A. cf. sinica, there are colorless cortical granules on the ventral side of the new population, whereas in the previously reported populations bright orange, spherical granules were clustered around dorsal cilia. Additionally, we sequenced the small-subunit(SSU) rRNA genes of K. cf. setigerum, N. orientalis, and A. cf. Sinica, and compared the new and reported populations. For the first time, we also provide a species list, including 33 ciliates collected from the wetlands based on living observation and silver staining.     

Effects of temperature and salinity on the development of the amphipod crustacean Eogammarus sinensis

The amphipod crustacean Eogammarus sinensis has useful features that make it suitable for use in the aquaculture of fish and large decapod crustaceans.In this study,we investigated the effects of temperature and salinity on the development,fecundity,survival,and growth rate of E.sinensis.The results show that temperature significantly affected E.sinensis development,but salinity.As temperature increased,the duration of E.sinensis embryonic development decreased.Fecundity was affected significantly by temperature and the combination of temperature and salinity,but by salinity alone.In addition,high temperatures accelerated E.sinensis juvenile growth rates,whereas high salinity reduced it.Therefore,our data suggest that E.sinensis tolerates a wide range of salinities and that temperature has more significant effects than salinity on the embryonic development,fecundity,and growth of E.sinensis.Our results shall be useful for mass production of this species for use in aquaculture.     

矿山储量动态监测后的新问题探讨

2008年度的矿山储量动态监测工作,业已结束.通过对矿山的储量动态监测,各地暴露出诸多新问题.给我们的矿政管理带来新困惑.本文就此作一分析、探讨,努力促使我市的矿政管理更加规范、科学和合法. 一、概述 今年参加矿山储量动态监测的矿山共有30多家.根据各县(市、区)反映的情况,主要存在以下几类问题.一是采矿权有效期已届满但累计总量未采完,故矿山企业仍然在生产.二是采矿权有效期未满但企业提前采完核定资源量,矿山仍然在生产.三是采矿权有效期未满,法定储量也未采完,但有越界开采现象.四是采矿权有效期未满,划定资源量也采完,存在越界现象.五是采矿权有效期已届满,划定资源量也采完.且有越界现象.六是矿山企业超年度规模开采矿产资源.     

“三保”促和谐 统筹显智慧——2009年广西开展耕地保护和节约集约用地保卫战扫描

引言 (重耳)出于五鹿,乞食于野人,野人与之块.公子怒,欲鞭之.子犯日:"天赐也."稽首,受而载之. --<左传> 中国人历来敬重土地,爱护土地. 在古老的自然崇拜中,土地崇拜占据着重要位置.几千年前,土地常常作为国家的象征,所以国家也叫社稷,这里的"社"为土地神,"稷"为谷神.土地神和谷神构成了一个农耕国家的主干.在漫长的农业文明中,土地的崇拜情结成为深厚、凝重的中国历史文化的一个底蕴和特征.     

浙江大桥坞铀矿床斑岩体的“双层结构”与铀矿化

大桥坞斑岩型铀矿床产于中生代蒙山破火山口中一石英斑岩体的内外接触带及其隐爆角砾岩筒中。铀成矿主要与斑岩体的“双层结构”有关,即”双层结构”成矿模式。浅部石英斑岩为含矿岩体,深部花岗斑岩为矿源岩体。矿化以裂隙型、角砾型为主,矿体的形态主要呈细脉状、浸染状,与围岩界线不清。成岩物质来源于壳幔混源的富铀钙碱性岩浆。成矿物质主要来源于该深部富铀花岗岩浆冷凝结晶分异产生的富铀岩浆期后热液。其成矿过程主要是富铀岩浆期后热液流体沿断裂构造系统上升、运移,在浅部石英斑岩体内外接触带发生隐爆,成岩成矿。早期铀-赤铁矿化阶段形成贫铀矿化,晚期铀-金属硫化物矿化阶段,形成富铀矿化,两期叠加作用致富。     

山东省莱州市寺庄金矿床地质特征

“焦家式”金矿(即破碎带蚀变岩型金矿)是山东胶西北地区重要的矿床类型。莱州寺庄金矿床位于焦家成矿带的南段,矿化特征表现出与该成矿带上诸金矿的共同特征。矿区内划分了3个赋矿岩性带(黄铁绢英岩化碎裂岩带、黄铁绢英岩化花岗质碎裂岩带、黄铁绢英岩化花岗岩带),圈出3个矿体群(共180余个矿体)。其中在黄铁绢英岩化花岗岩带内发现了规模较大的矿体,取得了重大的找矿突破。     

强力侵位花岗岩体与金矿的关系——以丹东三股流岩体为例

辽宁丹东五龙金矿、四道沟金矿位于五龙背—大堡花岗岩体与三股流花岗岩体之间,成矿作用与三股流岩体密切。据分析,这两个岩体的岩浆来源相同,岩石化学性质相似,岩体侵位时间相当,且同处于丹东北东向韧性剪切带内,但由于岩体侵位时受控的局部构造环境不同,导致岩体以不同的方式侵位。三股流岩体在韧性推覆剪切带发展演化过程中沿剪切面理以气球膨胀式强力侵位;而五龙背—大堡岩体则是沿该剪切带晚期发育的北西向脆性张裂面被动侵位。不同方式侵位的岩体具有不同的成岩环境,从而在一定程度上控制岩浆气水溶液的分离和聚集。强力侵位的花岗岩体在成岩过程中具有较好的封闭条件,因此可能有利于成矿热液的分泌、聚集和保存,而被动侵位的花岗岩体则不具备这种有利的成矿条件。     

浙西石耳山超单元花岗岩演化特征及成因浅析

本文介绍近年来在浙西石耳山花岗岩区引进“花岗岩超单元─单元”理论进行的1：5万区域地质调查工作取得的成果。按同源岩浆演化序列的观点，通过野外工作和室内研究，解体了晋宁期石耳山复式花岗岩体。对划分出的30个侵入体，归并建立了四个单元，并进一步建立了石耳山超单元。通过对石耳山超单元花岗岩的岩石矿物学、岩石化学、地球化学等地质特征的分析研究，初步总结其演化特征，并同时探讨其成因类型，指出石耳山超单元花岗岩相当于S型花岗岩，应属上地壳硅铝层重熔岩浆的产物。     

法库地区十间房超单元花岗岩岩石成因及侵位机制探讨

法库地区十间房片麻状二长花岗岩过去被认为是大古代或元古代混合岩和混合花岗岩．１：５万地质调查表明，该花岗岩是与印支－海西期韧性剪切构造同期侵位的花岗岩，同位素年龄测试属中三叠世．该岩体属复式岩体，是上部地壳沉积物质局部熔融的花岗岩浆沿剪切带被动侵位的“Ｓ”型大型岩床．     

Petrogenesis and tectonic setting of granite porphyry in Keyouzhongqi area,Inner Mongolia

The authors studied the geochemistry, zircon U-Pb ages, Hf isotope of the granite porphyry and its petrogenesis and tectonic setting in the studied area. The zircon U-Pb dating indicates the formation of the granite porphyry is in Early Cretaceous （ 125.1 ± 1.5 Ma）. The granite porphyry has high-SiO2 and alkali-rich features, which belongs to high-K talc-alkaline series rocks （ A/CNK = 0. 95%-1. 25% ）. The analyses of trace elements show the characteristics of a swallow-shaped REE distribution pattern with enrichment in LREEs and most of LILEs and HFSEs, depletion in Ba, Sr, Nb, P and Ti, and especially strong depletion in Eu, which indicates the granite porphyry belongs to the aluminous A-type granite. Their εHf（t） range from 5.94 to 8.80 with Hf two-stage model ages （TDM2 ） of 620 Ma to 803 Ma. Combining with the regional tectonic background, we conclude that the source of the rocks is the new crust materials accreted from depleted mantle in Neoproterozoic and is the product of partial melting of middle and lower crustal rocks, which may be suffered from the dual impact of the subduction of the Palaeo-Pacific Ocean and the closure of the Mongol-Okhotsk Ocean.     

山东省招远市上庄矿区陈家矿段深部金矿床地质特征

“焦家式”金矿是胶西北地区重要的矿床类型。陈家矿段位于焦家成矿带的北段,矿化特征表现出与焦家成矿带诸多的相同特征。研究区共有3种赋矿岩性即绢英岩化碎裂岩、绢英岩化碎裂状二长花岗岩、绢英岩化碎裂状花岗闪长岩。在-500～-800m共圈定4个矿体,发现了新的金矿体,实现了深部找矿的目的。     

千山花岗岩地球化学特征及其成因探讨

千山花岗岩位于辽宁省鞍山地区,形成于中生代,为一由多种岩石类型组成的花岗岩套。千山花岗岩体的地球化学特征表明,其某些特殊成分含量及某些特征值同澳大利亚东南部晚泥盆世的 A 型花岗岩相似,因此,千山花岗岩具有 A 型花岗岩的特征。它是部分熔融的产物,其岩浆熔体的母岩成分大致相当于富含角闪石的中性火成岩。     

新疆西准噶尔哈图岩体地球化学特征及其地质意义

哈图岩体侵位于西准噶尔南部早-中泥盆世海相火山-沉积地层中,主要岩性为二长花岗岩、正长花岗岩及少量碱长花岗岩,是研究西准噶尔晚石炭世构造环境的理想对象。哈图岩体花岗岩中SiO2含量(质量分数,下同)为72.06%~76.53%,全碱(Na2O+K2O)为7.80%~8.57%,CaO为0.20%~1.58%,MgO为0.07%~0.42%,明显具有高Si、富碱、贫Ca、低Mg的特征;这些花岗岩的Al2O3含量为12.55%~14.06%,A/CNK值为1.06~1.15,A/NK值为1.15~1.36,显示其为弱过铝质-强过铝质花岗岩。此外,哈图岩体具有较低的稀土元素总含量((88.14~139.53)×10-6)和高的轻、重稀土元素比值((La/Yb)N值为3.04~6.50),在球粒陨石标准化稀土元素配分模式中显示为典型的右倾"V"字形且具有强烈的负Eu异常,表明源区可能有斜长石残留或出现斜长石的分离结晶作用;在原始地幔标准化微量元素蛛网图中,这些花岗岩明显富集Rb、Th、U、K、Pb等大离子亲石元素,相对富集Zr、Hf,强烈亏损Sr、Ti、P,相对亏损Ba、Nb。以上特征及主量、微量元素特征和图解表明,哈图岩体为典型的弱过铝质-强过铝质A2型花岗岩,其形成于造山后伸展阶段,是由洋壳和岛弧组成的新生地壳受上涌的幔源物质加热,在浅部低压条件下发生部分熔融,再经分离结晶作用的产物。     

鲁西太古代徂徠山杂岩体花岗质岩石成因探讨

鲁西太古代徂徕山杂岩体主要由片麻状花岗岩和钾长花岗岩构成,此外尚发育少量小规模的中粗粒、细粒闪长岩。本文着重讨论花岗质岩石的成因。徂徕山杂岩体岩石地球化学研究表明,片麻状花岗岩为深源(下地壳)花岗质岩浆侵位结晶的产物;钾长花岗岩是片麻状花岗岩在区域变质作用过程中部分熔融形成的,两者具有密切的成因联系。