简介：小四是我从小玩到大的好朋友．从小就特别喜欢看一些漫画书籍，人送外号“漫迷”，上了大学她简直对漫画就到了一种痴迷的状态，天天登录一些在线漫画网站，搜索寻找一部部漫画作品，看起来没完没了，于是叉升级为“漫痴”。不过，这位“漫迷＆漫痴”近期情绪越来越不对头了，总是在抱怨：在线漫画看起来不爽，网页广告太多，花花绿绿尽是骚扰；漫画图片下载太慢，

简介：FieldinvestigationsofmarinemacrobenthoswereconductedattensitesintheBeringSeainJuly2010.Altogether90speciesofmacrobenthosbelongingto59familiesand78generawereidentified.Amongthem,41polychaetes,16mollusks,23crustaceans,threeechinoderms,twocnidarians,onenemertean,onepriapulid,twosipunculids,andoneechiuranwereidentified.Theaveragedensityandbiomassoftotalmacrobenthoswere984ind./m2and1207.1g/m2ofwetweight,respectively.ThepredominantspeciesinthestudyareawereScoloplosarmiger,Eudorellapacifica,Ophiurasarsii,Heteromastusfiliformis,Ennuculatenuis,andHarpiniopsisvadiculusbyabundance,whilethepredominantspeciesinthisareawasEchinarachniusparmabybiomass.Hierarchicalclusteranalysis(Bray–Curtissimilaritymeasure)revealedthattwoimportantbenthicassemblagesinthestudyareawereCommunityAandCommunityB.CommunityAwasstableandCommunityBwasunstable,asshownbytheAbundance/BiomassComparisons(ABC)approach.ThemacrobenthiccommunitystructureintheshelfoftheBeringSeawascharacterizedbyitshighabundanceandbiomass,highproductivitybutgreatheterogeneity.

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简介：北华南海架上的沙波浪被认为寡妇床形式同样稳定。为在车站LF13-2和LF13-1之间的海床的工业使用，探索的一个新回合被进行。沙波浪的间距和振幅都系统地与水深度正在改变的最新获得的数据表演。自从2003～2004证明海床当前是活跃的，重复了观察。由于表面沉积的强壮的侵蚀自从Dongsha()高举，Dongsha的架上有几乎不现代的沉积区域。在学习区域的沙材料主要从床沉积形成的侵蚀发源。水深度增长由更健全的数据主要由于侵蚀的重复回响揭示了。底部水流在Dongsha的区域是相当复杂的在水下高原。在地点9MKII，向南方退电流比强壮，向北方在地点AEM-HR充满电流，WNW病房洪水水流比ESE病房稍微强壮退当前。在地点9MKII，最大的底部水流速度是48cm/s，并且22%观察底部水流速度比20cm/s大，它遇见为沙波浪的创造要求的最小的底部水流速度。这篇文章指出今日的海洋学的状况与沙波浪形态学联合很好，并且沙飘动，这是在很大程度上在有进行中的今日的海洋学的底部水流的平衡调节并且活跃。

简介：ThemainactivitiesinthejointexpeditionbetweenCHINAREandANAREonAmeryiceshelfareintroduced.Five-daycontinuousGPSobservationdatacollectedonthesitewhichlocatesatthefrontalpartofAmeryiceshelfwasprocessedwithprecisepointpositioning(PPP)technologybasedonpreciseproductsfromIGS.VelocityofthesurfaceiceflowonAmerycanbederivedfromthePPPsolution.Preliminaryresultshowsthatthesurfaceiceflowvelocityofthesiteis2.25metersperday,themotiondirectionisnortheastward.SemidiurnaloceanictideanddiurnaloceanictidesignalofthatsitecanberecoveredfromtheheightvariationseriesofPPPsolution.Theseabovesolutionscanbeusedtotheconsequentmassbalancecalculation.

简介：AmarinestratigraphicsequenceacrossthePliocene/Pleistoceneboundaryhasbeenfoundinthenorth-erncontinentalshelfoftheSouthChinaSea.ThemarineQuaternarydepositsintheYinggehaiBasinmayex-ceed2,000minthickness,probablyprovidingthebestsectionforstudyingthelowerboundaryofthemarinePleistoceneinSouthChina.TheverticalsuccessionwithplanktonicforaminifersandnannofossilsrevealedinboreholesinthebasinhasbeenwellcorrelatedwiththatintheinternationalstratotypesectionofthePliocene/PleistoceneboundaryatVrica,Italy,resultingintheacquirementofabiostratigraphicboundaryat1.64Ma.Thisboundary,however,doesnotcoincidewithanyprominentlithologicalpalaeoenvironmentalchangesinthestudyareaandcanhardlybeusedingeologicalpractice.Thereare,incontrast,significantchangesatthelevelofLADofGloborotaliamulticameratasensulatolocatedbelowtheabove-mentionedboundary.Thepercentageofplanktonicforaminifersinthetotalpopulationandpreservationofforaminiferaltestsdisplaygreatchangesatthislevelcorrespondingtoaclearonlapontheseismicprofilesandindicatingadepositionalhiatusatca.2.0-2.5Ma.SincethelevelcanbewidelytracedinthePearlRiverMouthBasinandtheBeibuGulfBasinandwellcorrespondswiththemarkeddepositionalenvironmentalchangesrecordedinthewestPacificandotherregions,itisrecommendedthatthePlio/PleistoceneboundarybedrawnatthelevelofGr.multicameratasensulatoLAD,roughlyconcurrentwiththeGauss/Matuyamaturn.

简介：TheavailabledataontidalcurrentsspanningperiodsgreaterthansixmonthsforthecontinentalshelfoftheEastChinaSea(26°30.052′N,122°35.998′E)wereanalyzedusingseveralmethods.TidalCurrentHarmonicAnalysisresultsdemonstratedthatsemi-diurnaltidesdominatedthecurrentmovement.Thetidalcurrentsoftheprincipaldiurnalandsemidiurnalrotatedclockwisewithdepth,withthedeflectionofthemajorsemi-axestotherightintheupperlayerandtotheleftinthelowerlayer.Theverticalstructuresoftwoprincipalsemi-diurnalconstituents-M2andS2-weresimilar,whichindicatesthatthetidalcurrentsaremainlybarotropicinthisarea.Themainfeaturesofthevariationofthefourprincipaltidalconstituentswithdepthdemonstratethatthecurrentsinthisregionareinfluencedbytheupperandlowerboundarylayers.Therefore,thetidalconstituentsoftheshallowwateraresimilar.DifferentverticalmodeswerecalculatedbasedontheEmpiricalOrthogonalFunction(EOF)analysisoftheEasternandNortherncomponentsofthetidalcurrents,withavariancecontributionforthezero-ordermodelofatleast90%.Thevariancecontributionofthebaroclinicmodelisminimal,whichfurtherrevealsastrongbarotropiccharacterforthetidalcurrentsofthisregion.

简介：根据在2009的冬季和夏天的CTD数据和当模特儿的结果，在西方的华东海架区域的水群众的季节的特征用一个簇分析方法被分析。结果证明在学习区域的水群众的分布和温度咸度特征具有不同季节的差别。在西方的华东海架区域，在冬季期间有三水群众，即，沿海的水(CCW)，台湾温暖的当前的表面水(TWCSW)和混合的黄海浇的大陆人(YSMW)，而是四在夏天期间，即，CCW，TWCSW，台湾温暖的当前的深水(TWCDW)和YSMW。都所有，CCW，TWCSW和TWCDW中是主导的水群众。CCW，首先由低咸度描绘了，在冬季有更低的温度，更高的咸度和更小的空间程度比在里面夏天。TWCSW在比在冬季的夏天更温暖、更新鲜、更小，并且它在冬季期间从台湾海峡水台湾，中国和更少向东北主要从自台湾东面的菲律宾海流向日本的暖流表面水(KSW)发源，但是它在夏天期间由海峡水和KSW组成。TWCDW被低温度和高咸度描绘，并且台湾向东北在自台湾东面的菲律宾海流向日本的暖流表面下的水里完全发源。

简介：Shelf-lifeextensionofaquaticproductsisofsignificanteconomicalimportance.Todeterminethepotentialeffectofchitosanontheshelf-lifeoffilletedtilapia,thisstudyanalyzedthebacterialcommunitydiversityinfreshandspoiledtilapiafilletsstoredat(4±1)℃andexaminedtheantimicrobialactivityofchitosanagainstrelevantbacteriaisolates.ResultsshowedthatPseudomonas(20%)andAeromonas(16%)wereabundantinfreshtilapiafillets,whereasPseudomonas(52%),Aeromonas(32%)andStaphylococcus(12%)weredominantinthespoiledsamples.Chitosanshowedwide-spectrumantibacterialactivityagainstbacteriaisolatedfromtilapiaand5.0gL-1chitosanwasselectedforapplicationinpreservation.Wefurtherdeterminedtheshelf-lifeofchitosan-treated,filletedtilapiastoredat(4±1)℃basedonmicrobiological,biochemicalandsensoryanalyses.Resultsshowedthattheshelf-lifeofchitosan-treated,filletedtilapiawasextendedto12d,whereasthatofuntreated,controlsampleswas6d.Theseindicatethatchitosan,asanaturalpreservative,hasgreatapplicationpotentialintheshelf-lifeextensionoftilapiafillets.

简介：OnthebasisoftheinsitudataofDO2,pH,SiO2.PO4-P,NO3-NandNO2-NcollectedinthenorthoftheEastChinaSeaduring1987-1988,thefollowingpointsaremainlyexpounded.1.TheinorgonicnutrientsareobviouslyaffectedbycontinentrunoffinthenorthoftheEastChinaSea.Theirdistributionsarecharacteristicofitsdistributionofterrigenousmaterials.2.TherearethreetransportpathsofnutrientsfromtheshelftotheKuroshioarea.Thefirstismixing-diffusing-advec-tionandupwellingprocess,theprocessofbiologyandbiochemistrybelongstothesecond,andthesinkingprocessisthelastone.3.TheswingoftheKuroshioaxisaffectesboththerangeofthemigrationofsubstancesthroughmixing-diffusing-advec-tionprocessandtheupwellingdegreeofthesubsurfaceKuroshiowatertotheshelf.4.MostpartofthesubstancessinkasmacroparticlestothedeeplayerbeforereachingtheKuroshioarea.

简介：appendicularians上的桡脚类的动物的潜在的抑制在领域和试验性的条件里被发现。appendicularians和planktonic桡脚类的动物的丰富和分发在华南海(SCS)的西北大陆人架上在夏天期间与他们的关联的参考被学习。基于地形学和调查区域的水质量，它被划分成三个分区：区域我(东方Leizhou半岛的沿海的水)与低温度，咸度和高叶绿素一(Chl一)集中，有低温度的区域II(东方的沿海的水和东南海南岛)，高咸度和中等Chl集中和区域III(近海从Leizhou半岛流水到海南岛)与高温度，高咸度和低Chl集中。appendicularians和桡脚类的动物的种类丰富增加了从对沿海近海水，和高价值在区域III被观察。appendicularian和桡脚类的动物丰富的分发通常减少了从对沿海近海水，与最高的价值在区域我。我们的结果建议appendicularians和桡脚类的动物的分发模式显著地不同，由于物理、生物的因素的影响。appendicularians上的远洋的桡脚类的动物的否定影响没被发现基于在在SCS的西北大陆人架中的situ数据。

简介：TheEastChinaSeawhichcoversatotalareaof750,000squarekilometersisasemi-closedsealyingbetweentheeasterncoastofChina’smainlandandthePacificOcean,boundedonthewestbyChina,ontheeastbytheKyushuandtheRyukyuIslandsofJapan,andonthenorthbyJichuIslandoftheRepublicofKorea(ROK)andtheYellowSea,andconnectedwiththeSouthChinaSeabytheTaiwanStraiton

简介：根据通过台湾海洋研究院的领域观察的历史的吝啬的海洋水流数据在19912005期间并且在2006的夏天的华东海(ECS)的大陆人架上的营养素的调查数据，从台湾海峡和自台湾东面的菲律宾海流向日本的暖流的滋养的流动表面下的水用一个格子插值方法被估计，它两个都是台湾温暖的水流的来源。二水群众的滋养的流动也被比较。结果显示出那磷酸盐(PO4-P),硅酸盐(SiO3-Si)和硝酸盐(没有到从自台湾东面的菲律宾海流向日本的暖流upwelling水的ECS大陆人架的3-N)流动比稍微高那些在2006的夏天从台湾海峡流水。相反由于它的更低的速度，滋养的流动密度(即，滋养的流动由特定的节的区域划分了)自台湾东面的菲律宾海流向日本的暖流，表面下的水比台湾海峡水的低。另外，台湾温暖的当前的深水，被自台湾东面的菲律宾海流向日本的暖流表面下的水主要组成，可能直接在ECS到达高周波的有害水藻花蕾的区域。

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简介：Lishui下垂在华东海架盆，富于烃，与是的主要的忍受烃的层古新的Mingyuefeng碎屑状的岩石。用petrological和geochemical方法的这些古新的碎屑状的岩石的含蓄的地质的背景资料的分析有重要实际重要性。这些古新的沙岩主要是锂的arenite，锂的arkose和greywacke，K长石，斜长石，authigenic泥土，硅石和碳酸盐镇静。作为大陆人存款，Yueguifeng碎屑状的岩石有高铝矽酸盐和mafic岩屑内容，当Lingfeng和Mingyuefeng形成由于震荡富于硅石时主要元素这些古新的沙岩满足的沿海的海洋的depositional环境是低的并且有集中的分布，显示geochemical作文是non-epigenetic，由沉积过程和成岩作用转变了。Yueguifeng岩屑包括再循环的沉积，由中等捱过和侵蚀控制了，当Lingfeng和Mingyuefeng岩屑由于低化学捱过作为首先第一周期的材料被解释时。在迟了的白垩纪到早古新，和平的板在欧亚的板下面开始了subducting，由于融化subducted由板碰撞和岩浆爆发引起一个造山运动海洋的外壳这导致了“activemargin”的双构造背景并且“continental岛arc”在华东海架盆。在期间晚古新，与菲律宾的海洋板的开发一起东方的移植的和平的板边缘，和Lishui的构造设置逐渐地下垂变成了被动大陆人边缘。由岩屑形成的来源包括了两orogenic大陆人块和大陆人岛弧，和父母岩石主要是felsic暴烈的岩石和花岗石。

简介：Grainsizeandmineralcompositionofcoresedimentswereusedtoinvestigateinfluencesofvariousterrestrialandmarineconditions,whichhaveprevailedonthesouthwesternBlackSeashelfduringtheHolocene.Siliciclasticmudwithsmallamountsofsandandgravelfromnearbycoastalhinterlandistheprincipalsedimenttype,whereassedimentsdepositedneartheshelfedgeandthe(I)stanbulStraitandofftheDuruLake(apaleo-rivermouth)constituedlargequantitiesofsandandgravelofbothbiogenicandterrigenicorigin.Variableamountsofaragonite,1nm-micas,quartz,feldspars,calciteanddolomiteconstitutethedominantnon-claymineralsinbulksediments.Theclaymineralassemblageinthe＜2μmfractionismadeupofsmectite,illite,kaoliniteandchlorite.Aragoniteandcalcitearemainlyderivedfrombenthicaccumulations,whereasfeldspars(mainlyplagioclase)andsmectitereflectmagmaticvolcanicprovenanceandthedistributionof1nm-micasandchloritecorrelatewithnearbymetamorphicsourcesonland.Nevertheless,grainsizeandmineraldistributiongenerallyindicateacombinationofeffectsofwindandwaveclimate,longshoreandoffshorecycloniccurrents,changingsea-levelstandsandnearbysourcerockandmorphologicalconditions.ItisalsosuggestedthatatleastpartofclaymineralscouldbederivedfromthenorthwesterlyDanubeRiverinput.

简介：无

简介：渐新世Huagang形成是在Xihu的主要沙岩水库下垂，位于华东海架盆的东方。与薄节的岩相学，紫外线荧光显微镜学，扫描电子显微镜学，和同位素地球化学的一条综合途径，不同diagenetic特征被识别，典型diageneticparasequences被建立，并且diagenetic液体进化历史为渐新世Huagang被重建在Xihu的南方的形成沙岩水库下垂。Huagang形成沙岩水库现在在mesodiagenesis的时期B，它经历了象机械压缩，毛孔衬里绿泥石水泥，长石溶解，石英硬化和溶解那样的重要diagenetic改变，并且焦化硬化。碳酸盐水泥(早陨铁，中等ferrocalcite和迟了的ankerite)的三种类型在Huagang形成沙岩水库被识别。碳和氧而迟了的碳酸盐水泥是，碳酸盐水泥的同位素的作文证明早方解石从碱的湖的环境猛抛仔细与器官的酸有关。到Huagang形成沙岩水库，它在成岩作用期间经历了溶解的二个主要事件。早溶解是象长石，锂的碎片，和碳酸盐水泥那样的不稳定的部件被酸的水溶解。第二溶解是石英和其它硅酸盐矿物质在碱的条件下面被溶解。烃收费的二个主要阶段发生在这个学习区域。第一个烃炮兵阵地在中等碳酸盐硬化以前但是对长石溶解和在结束的石英硬化的发作以后中新世。收费的第二烃在迟了的碳酸盐降水以后发生在第四级的时期。