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Morphological and molecular analyses of a Philine kinglipini outbreak in summer of 2022 in Jiaozhou Bay,china

Journal of oceanology and Limnology 2024年第3期42卷 831-848页

作者： Zelin DUAN Yanan YU Jing WANG Junlong zhang Nansheng CHEN CAS key laboratory of marine Ecology and environmental sciences Institute of OceanologyChinese Academy of SciencesQingdao 266071China laboratory of marine Ecology and environmental Science Laoshan LaboratoryQingdao 266237China Center for Ocean Mega-Science Chinese Academy of SciencesQingdao 266071China laboratory of marine Organism Taxonomy and Phylogeny Qingdao Key Laboratory of Marine Biodiversity and ConservationInstitute of OceanologyChinese Academy of SciencesQingdao 266071China marine Biological Museum Chinese Academy of SciencesQingdao 266071China Department of Molecular Biology and Biochemistry Simon Fraser UniversityBurnabyBritish ColumbiaV5A 1S6Canada

A sudden and unprecedented outbreak of molluscan Philine kinglipini occurred in summer 2022 in Jiaozhou Bay,Shandong,china,causing substantial damage to local mariculture industry of the Manila clam Ruditapes *** *** has been found in many coastal regions of china,the molecular research of *** has not been extensively studied,making it difficult to accurately identify and track *** samples in field using molecular *** were collected during the outbreak and their morphological features and molecular sequences were *** show that the causative species of the outbreak was *** mitochondrial genome(mt DNA)of *** was constructed for the first time,based on which phylogenetic analysis of the mt DNAs of *** and related species in the order Cephalaspidea was carried *** revealed by metabarcoding analysis of 18S rDNA V4,the seasonal change of *** and closely related Philine species was striking with peaks between April and ***,metabarcoding analysis is applicable tool for monitoring the bloom development of *** and related *** study generated for the first time essential molecular marker sequences and mtDNA of ***,which provided a reference for future characterization and monitoring of its outbreaks and for phylogenetic analysis of Philine species.

关键词： marine species outbreaks metabarcoding analysis mitochondrial genome Philine kinglipini phylogenetics spatial-temporal dynamics

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南海北部陆缘构造属性研究进展

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海洋地质前沿 2012年第7期28卷 1-9页

作者：万志峰夏斌施秋华蔡嵩蔡周荣国土资源部海洋油气资源与环境地质重点实验室青岛266071 中国科学院边缘海地质重点实验室广州510640 中山大学海洋学院广州510275

南海北部陆缘位于特提斯与古太平洋两大构造域的叠合部位,构造特征十分复杂,其构造属性一直是国内外学者争论的焦点,从主动陆缘到被动陆缘,火山型被动陆缘到非火山型被动陆缘等均有表述。南海复杂的形成机制以及东、西部构造差异性所引... 详细信息

南海北部陆缘位于特提斯与古太平洋两大构造域的叠合部位,构造特征十分复杂,其构造属性一直是国内外学者争论的焦点,从主动陆缘到被动陆缘,火山型被动陆缘到非火山型被动陆缘等均有表述。南海复杂的形成机制以及东、西部构造差异性所引起的地球物理、岩浆活动等认识的异同,是造成南海北部陆缘构造属性认识差异的主要原因。通过与全球典型地区的比较研究,进一步加强对南海形成演化过程分析,开展大洋钻探与多学科综合分析,揭示南海海盆的多期扩张与多盆张裂特征,是认识南海北部陆缘构造属性的关键。探讨了南海三叉裂谷张裂模式,初步认为南海第1次扩张具有非火山型被动陆缘性质,第2次扩张具有火山型陆缘性质。

关键词：大陆边缘陆缘构造研究进展南海

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东海陆架北部表层有用重砂资源形成条件及成矿远景

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海洋地质前沿 2012年第7期28卷 10-16页

作者：黄龙张志珣杨慧良国土资源部海洋油气资源和环境地质重点实验室青岛266071 青岛海洋地质研究所青岛266071

对2007年取自东海陆架北部海域336个表层沉积物样品进行了重矿物研究,计算了钛铁矿、石榴石、锆石、金红石4种有用重砂矿物的品位,其异常品位值主要富集在研究区的北部和东南部。形成条件分析表明,古长江等陆源河流供给形成的陆架残留... 详细信息

对2007年取自东海陆架北部海域336个表层沉积物样品进行了重矿物研究,计算了钛铁矿、石榴石、锆石、金红石4种有用重砂矿物的品位,其异常品位值主要富集在研究区的北部和东南部。形成条件分析表明,古长江等陆源河流供给形成的陆架残留沉积物为重砂矿物的富集提供了物质来源;粉砂质砂、砂质粉砂和砂等粗粒沉积物类型也有利于重砂矿物的保存;冰后期海侵过程中的水动力和现代水动力条件都有利于重砂矿物的进一步富集,且现代水动力条件对已富集的区域起到重要的保护作用。综合品位分布情况、离岸距离、水深和沉积物类型等条件,将东海陆架北部海域重砂矿物资源划分为5个成矿远景区,为将来开发提供了科学依据。

关键词：重砂异常品位形成条件成矿远景东海陆架

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Geochemical constraints on CO2-rich mantle source for the Kocebu Seamount,Magellan Seamount chain in the western Pacific

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Journal of oceanology and Limnology 2020年第4期38卷 1201-1214页

作者： LIU Yuhao zhang guoliang zhang Ji WANG Shuai Center of Deep Sea Research&key laboratory of marine geology and environment Institute of OceanologyChinese Academy of SciencesQingdao 266071China laboratory for marine geology Qingdao National Laboratory for Marine Science and TechnologyQingdao 266000China University of chinese academy of sciences Beijing 100049China Center for Ocean Mega-Science Chinese Academy of SciencesQingdao 266071China

The alkaline oceanic island basalts(OIBs)with under-saturated SiO2 and high contents of CaO and alkaline are usually attributed to mantle sources different from typical tholeiitic *** on the results of high pressure and temperature experiment study,the genesis of silica under-saturated alkaline basaltic melts could be explained by the role of CO2,thus,the genetic relationship of alkaline basalts with CO2 has become a topic of relevance because it is closely related to the deep carbon *** Magellan Seamount chain in the West Pacific Seamount Province has wide distribution of alkali *** the first time,we collected alkaline basalt samples from the Kocebu Seamount of the Magellan Seamount chain and found that magmatic apatites widely occur in the less evolved volcanic rock samples,and the high contents of phosphorus should be a feature of the alkaline OIBs of the Magellan *** with typical OIBs,these alkaline volcanic rocks have higher CaO and P2O5,lower SiO2 content,negative anomaly of high field strength elements(HFSEs),more distinctly negative anomaly of potassium(K)and the ubiquity of titanaugite,indicating a CO2-rich mantle *** on the relatively high K2O and TiO2 contents and La/Yb ratio and low MgO content of these alkaline rocks,we suggest that the volcanic rocks of the Magellan Seamounts are originated from carbonated eclogites derived possibly from ancient subducted altered oceanic crust.

关键词： alkaline oceanic island basalts(OIBs) carbonatite geochemistry mantle source Magellan Seamounts

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Control of subduction rate on Tonga-Kermadec arc magmatism

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Journal of oceanology and Limnology 2018年第3期36卷 687-699页

作者： LUO Qing zhang guoliang key laboratory of marine geology and environment Institute of OceanologyChinese Academy of SciencesQingdao 266071China University of chinese academy of sciences Beijing 100049China laboratory of marine geology Qingdao National Laboratory for Marine Science and TechnologyQingdao 266071China Deep-Sea Extreme environment and Life Processes Center Institute of OceanologyChinese Academy of SciencesQingdao 266071China

Dehydration/melting of oceanic crusts during returning to the mantle in subduction zones are related to origin of arc lavas. The factors that influence arc magmatism include compositions of the subducting slabs, mantle wedge and subduction rates. However, distinguishing these factors remains difficult and highly debated. Subducting rate is related to the total mass of inputs and controls thermal structure, thus plays a crucial role in arc magmatism. Here we explore the relationships between geochemical variations of arc lavas and convergence rates(increasing from 46 mm/a to the south to 83 mm/a to the northward) in the Tonga-Kermadec arc system. Data of geochemistry for lava samples from nine islands of this arc system are collected and compiled to investigate the role of subduction rate in arc magmatism. Lavas from the northern Tonga arc with a faster subduction rate show broadly lower concentrations of TiO_2 and highfield-strength elements(HFSEs, e.g. Nb, Ta, Zr, Hf), and higher Ba/Th, U/Th ratios than the Kermadec Arc to the south. Some of the Kermadec lavas show the highest values of Th/Nb ratio. We suggest that the northern Tonga arc with a higher subduction rate has been influenced by a stronger role of subductionreleased fluid, which results in stronger large-ion-lithophile elements(LILEs) and relatively weaker HFSEs contribution. It is interpreted that faster subduction rate tend to create a cooler subduction zone, leading to stronger dehydration subduction slab contribution with, thus, higher LILE/HFSE ratios of arc lavas. The conclusion contributes to a better understanding of arc magmatism, and ultimately the long-term chemical differentiation of the Earth. More supplementary geochemical data along Tonga-Kermadec arc and tests in other arcs are needed.

关键词： subduction rate arc magmatism Tonga-Kermadec Arc

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Unique double-layer solid electrolyte interphase formed with fluorinated ether-based electrolytes for high-voltage lithium metal batteries

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Journal of Energy Chemistry 2024年第1期88卷 532-542,I0012页

作者： Ruo Wang Jiawei Li Bing Han Qingrong Wang Ruohong Ke Tong zhang Xiaohu Ao Guangzhao zhang Zhongbo Liu Yunxian Qian Fangfang Pan Iseult Lynch Jun Wang Yonghong Deng Department of Materials Science&Engineering School of Innovation and EntrepreneurshipSouthern University of Science and TechnologyShenzhen 518055GuangdongChina School of Geography Earth and Environmental SciencesUniversity of BirminghamEdgbastonBirmingham B152TTUK key laboratory of marine environmental Corrosion and Bio-Fouling Institute of OceanologyChinese Academy of SciencesQingdao 266071ShandongChina Shenzhen CAPCHEM Technology Co. Ltd.Shenzhen 518118GuangdongChina CALB Group Co. Ltd.Changzhou 213200JiangsuChina

Li metal batteries using high-voltage layered oxides cathodes are of particular interest due to their high energy ***,they suffer from short lifespan and extreme safety concerns,which are attributed to the degradation of layered oxides and the decomposition of electrolyte at high voltage,as well as the high reactivity of metallic *** key is the development of stable electrolytes against both highvoltage cathodes and Li with the formation of robust interphase films on the ***,we report a highly fluorinated ether,1,1,1-trifluoro-2-[(2,2,2-trifluoroethoxy)methoxy]ethane(TTME),as a cosolvent,which not only functions as a diluent forming a localized high concentration electrolyte(LHCE),but also participates in the construction of the inner solvation *** TTME-based electrolyte is stable itself at high voltage and induces the formation of a unique double-layer solid electrolyte interphase(SEI)film,which is embodied as one layer rich in crystalline structural components for enhanced mechanical strength and another amorphous layer with a higher concentration of organic components for enhanced *** Li||Cu cells display a noticeably high Coulombic efficiency of 99.28%after 300 cycles and Li symmetric cells maintain stable cycling more than 3200 h at 0.5 mA/cm^(2) and 1.0m Ah/cm^(2).In addition,lithium metal cells using LiNi_(0.8)Co_(0.1)Mn_(0.1)O_(2) and Li CoO_(2) cathodes(both loadings~3.0 m Ah/cm^(2))realize capacity retentions of>85%over 240 cycles with a charge cut-off voltage of 4.4 V and 90%for 170 cycles with a charge cut-off voltage of 4.5 V,*** study offers a bifunctional ether-based electrolyte solvent beneficial for high-voltage Li metal batteries.

关键词： Lithium metal batteries High-voltage layered oxides Fluorinated ether-based electrolytes Solid electrolyte interphase Cathode electrolyte interphase

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晚侏罗世裂谷运动对北海盆地油气富集的控制作用

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海洋地质前沿 2012年第3期28卷 34-39页

作者：龚建明雷宝华李桂海张生银廖晶国土资源部海洋油气资源与环境地质重点实验室青岛266071 海南省海洋地质调查局海口570206 中国科学院油气资源研究重点实验室兰州730000

为了探讨北海盆地油气富集的控制因素,对前人在该区的大量研究成果进行了整理和分析,结果显示,北海盆地三叉裂谷所在的3个地堑具有上下2层不同的结构特征,即晚侏罗世末期的裂谷拉伸运动造就了北海盆地的下构造层,而早白垩世之后的热沉... 详细信息

为了探讨北海盆地油气富集的控制因素,对前人在该区的大量研究成果进行了整理和分析,结果显示,北海盆地三叉裂谷所在的3个地堑具有上下2层不同的结构特征,即晚侏罗世末期的裂谷拉伸运动造就了北海盆地的下构造层,而早白垩世之后的热沉降作用塑造了北海盆地的上构造层;断层主要分布在下白垩统之下的老地层中。北海盆地油气成藏组合主要受下构造层的控制,成藏模式主要表现为中生代砂岩断—背斜油气藏,因此,可以认为,北海盆地油气富集的主要控制因素是晚侏罗世—早白垩世的裂谷拉伸运动。

关键词：晚侏罗世裂谷运动油气富集北海盆地

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日本囊对虾基因组小卫星的特征分析

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水产学报 2007年第2期31卷 137-144页

作者：栾生孔杰王清印高焕王伟继张庆文中国水产科学研究院黄海水产研究所农业部海洋渔业资源可持续利用重点开放实验室中国水产科学研究院黄海水产研究所农业部海洋渔业资源可持续利用重点开放实验室山东青岛2.6071

为了分析日本囊对虾基因组中小微星序列的分布特征并开发小卫星标记,构建了日本囊对虾随机基因组文库,对其中片段长度为400-1 000bp的3 395个克隆测序,共获得总长度为1 606 711bp的DNA序列。在序列拼接后的2 815个克隆中,筛选到487个小... 详细信息

为了分析日本囊对虾基因组中小微星序列的分布特征并开发小卫星标记,构建了日本囊对虾随机基因组文库,对其中片段长度为400-1 000bp的3 395个克隆测序,共获得总长度为1 606 711bp的DNA序列。在序列拼接后的2 815个克隆中,筛选到487个小卫星序列,其序列总长度占测序序列总长度的3.97%。小卫星序列中,以12bp重复单位的序列数量最多(8.62%),总体趋势表现为重复单位越长,相应的重复序列数目越少(R=-0.826,P1)。小卫星重复单位拷贝数分布范围以8bp重复单位最广(3.1-47.6),其次是10bp(2.5-44),再次是12bp(2.2-28)。平均拷贝数最高的三种重复类型分别为8bp重复单位(13.45),32bp(9.32)和7bp(9.28)。小卫星序列重复单位的拷贝数分布范围2-48,集中分布在2-30,且表现为拷贝数目越大,其相应的重复序列数目越低的趋势。小卫星序列中,AT含量大于50%的序列占66%小卫星AT含量与相应的序列数目不相关(R=0.063,P1,P1),小卫星序列的产生与其两端侧翼序列的碱基组成可能存在一定的关系。

关键词：日本囊对虾串联重复序列小卫星重复单位拷贝数

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Structural features in the mid-southern section of the Kyushu–Palau Ridge based on satellite altimetry gravity anomaly

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Acta Oceanologica Sinica 2024年第4期43卷 50-60页

作者： Feifei zhang Dingding Wang Xiaolin Ji Fanghui Hou Yuan Yang Wanyin Wang School of Geological Engineering and Geomatics Chang’an UniversityXi’an 710054China qingdao institute of marine geology China Geological SurveyQingdao 266071China Information and Navigation College Air Force Engineering UniversityXi’an 710077China National Engineering Research Center of Offshore Oil and Gas Exploration Beijing 100028China key laboratory of marine geology and environment Institute of OceanologyChinese Academy of SciencesQingdao 266071China

The Kyushu–Palau Ridge(KPR),an anti-S-shaped submarine highland at the center of the Philippine Sea Plate(PSP),is considered the residual arc of the Izu–Bonin–Mariana Island Arc,which retains key information about the cessation of the Western Philippine Basin(WPB)expansion and the Parece Vela Basin(PVB)***,using the new generation of satellite altimetry gravity data,high-precision seafloor topography data,and newly acquired ship-borne gravity data,the topographic and gravity characteristics of the KPR mid-southern section and adjacent region are *** distribution characteristics of the faults were delineated using the normalized vertical derivative–total horizontal derivative method(NVDR-THDR)and the minimum curvature potential field separation *** Moho depth and crustal thickness were inverted using the rapid inversion method for a double-interface model with depth *** on these results,the crust structure features in the KPR mid-southern section,and the“triangular”structure geological significance where the KPR and Central Basin Rift(CBR)of the WPB intersect are *** KPR crustal thickness is approximately 6–16 km,with a distinct discontinuity that is slightly thicker than the normal oceanic *** KPR mid-southern section crust structure was divided into four segments(S1–S4)from north to south,formed by the CBR eastward extension joint action and clockwise rotation of the PVB expansion axis and the Mindanao fault zone blocking effect.

关键词： structural features satellite altimetry gravity data Kyushu-Palau Ridge Central Basin Rift faults Moho depth

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声管中双水听器法估算反射系数及降低干扰的方法研究

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山东科学 2009年第5期22卷 63-67,88页

作者：张颖张颖颖山东省科学院海洋仪器仪表研究所山东省海洋环境监测重点实验室山东青岛266001

借助数学模型研究声管中干扰的形成和传输路径,估算薄空气层的干扰级和声反射系数。研究发现,声源和管壁的机械连接导致的管壁振动决定了反射系数的估算精度。可以采用两种方法降低干扰:(1)合理设计声管结构,保持声管下端面和柱状换能... 详细信息

借助数学模型研究声管中干扰的形成和传输路径,估算薄空气层的干扰级和声反射系数。研究发现,声源和管壁的机械连接导致的管壁振动决定了反射系数的估算精度。可以采用两种方法降低干扰:(1)合理设计声管结构,保持声管下端面和柱状换能器后垫片的机械连接松动;(2)测量标准水听器所在位置的管壁径向速度来估算反射系数。大量试验和计算的结果表明,采用小弹性弹簧可以降低干扰。

关键词：双水听器法反射系数降噪

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