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| 1 | Finding of ancient materials in Cathaysia and implication for the formation of Precambrian crust显示文摘在 Nanxiongarea 从帕拉片麻岩为 56 由岩屑形成的锆石标明日期的 U-Pb,北广东省,显示在 Cathaysiahinterland 的最近的 Neoproterozoic 沉积由众多的 Grenvillian 和 Neoarchaean 组成碎屑状的材料,以及 someMesoproterozoic 岩屑。次要的 Paleoarchaean (3.76 Ga ) 和 Mesoarchaean (3.0—3.2 Ga ) 锆石,是在华南的最旧的锆石,第一也在沉积被发现,建议卡赛西亚·布洛克可以包含很旧的材料。thirty-sevenzircons 的 Hf 同位素作文表明这些碎屑状的材料有不同起源。次要的锆石从产生从的岩浆结晶相对少年外壳,当大多数锆石的父母岩浆从古老的外壳被导出时。U-Pb 标明日期和这些锆石的 Hf 同位素分析的集成建议在 Cathaysia 块的少年外壳的产生主要发生在 2.5 点—2.6Ga。Mesoarchaean (3.0—3.3 Ga ) ,迟了的 Paleoproterozoic (~ 1 .8 Ga ) 和 Paleoarchaean (~ 3 .7 Ga ) 可以也是外壳的生长的重要事件。Grenvillian magmatism 是极其强烈的,但是它主要涉及与少年外壳的很少形成古老的外壳的部件再循环。~ 2 .1 Ga Hf 模型年龄的 Themarked 存在和有结晶化的锆石的缺席在~ 2 .1 Ga 变老建议许多锆石的父母岩浆可能从由 Neoarchaean 和迟了的 Paleoproterozoic 材料组成的混合来源被导出。 | YU JinHai Y S O'REILLY WANG LiJuan W L GRIFFIN JIANG ShaoYong WANG RuCheng XU XiSheng | 2007 | Chinese Science Bulletin2007，52，1： | 47 |
| 2 | Formation history and protolith characteristics of granulite facies metamorphic rock in Central Cathaysia deduced from U-Pb and Lu-Hf isotopic studies of single zircon grains显示文摘The petrochemical as well as zircon U-Pb and Lu-Hf isotopic studies of granulite facies metamorphic rock from the Taoxi Group in eastern Nanling Range, Central Cathaysia indicate that its protolith is the sedimentary rock with low maturation index. The clastic materials are mostly from middle Neoproterozoic (~736 Ma) granitoid rocks with minor Neoarchaean and Paleoproterozoic rocks. The timing of this Neoproterozoic magmatism is in agreement with the second period of magmatism widespread surrounding the Yangtze Block. Hf isotopic data indicate that the Neoproterozoic granitoids resulted from the recycled Paleoproterozoic mantle-derived crustal materials. The sedimentary rock was deposited in Late Neoproterozoic Era, and carried into low crust in Early Paleozoic. The partial melting of the meta-sedimentary rock took place at about 480 Ma and subsequently granulite facies metamorphism occurred at ca. 443 Ma. The zircons forming during this time interval (Early Paleozoic) show large Hf isotope variations, and their -Hf(t) values increase from -13.2 to +2.36 with decreasing age, suggesting the injection of mantle-derived materials during partial melting and metamorphism processes in the Early Paleozoic. Calculation results show that this metamorphic rock, if evolved to Mesozoic, has similar isotopic composition to the nearby Mesozoic high Si peraluminous granites, implying that this kind of granulite facies metamorphic rock is probably the source material of some Mesozoic peraluminous granitoids in eastern Nanling Range. | YU Jinhai ZHOU Xinmin Y. S. O'Reilly ZHAO Lei W. L. Griffin WANG Rucheng WANG Lijuan CHEN Xiaomin | 2005 | Chinese Science Bulletin2005，50，18： | 35 |
| 3 | Grenvillian orogeny in the Southern Cathaysia Block:Constraints from U-Pb ages and Lu-Hf isotopes in zircon from metamorphic basement显示文摘Metamorphic basement rocks in the Cathaysia Block are composed mainly of meta-sediments with different ages. New zircon U-Pb geochronological results from the meta-sedimentary rocks exposed in the Zengcheng and Hezi areas, southern Cathaysia Block, show that they consist dominantly of early Neoproterozoic (1.0―0.9 Ga) materials with minor Paleo- to Mesoproterozoic and late Neoproterozoic (0.8―0.6 Ga) components, suggesting that the detritus mostly come from a Grenvillian orogen. The youngest detrital zircon ages place a constraint on the deposition time of these sediments in Late Neoproterozoic. Zircon Hf isotopic compositions indicate that the Grenvillian zircons were derived from the reworking of Mesoproterozoic arc magmatic rocks and Paleoproterozoic continental crust, implying an arc-continent collisional setting. Single-peak age spectra and the presence of abundant euhedral Grenvillian zircons suggest that the sedimentary provenance is not far away from the sample location. Thus, the Grenvillian orogen probably preexisted along the southern margin of the Cathaysia Block, or very close to the south. Similarity in the ages of Grenvillian orogeny and the influence of the assembly of Gondwana in South China with India and East Antarctic are discussed, with suggestion that South China was more likely linked with the India-East Antarctica continents in Early Neoproterozoic rather than between western Laurentia and eastern Australia. | WANG LiJuan YU JinHai S.Y. O'REILLY W.L. GRIFFIN SUN Tao WEI ZhenYang JIANG ShaoYong SHU LiangShu | 2008 | Chinese Science Bulletin2008，53，19： | 21 |
| 4 | Prevention and treatment of hepatic artery thrombosis after liver transplantation显示文摘BACKGROUND: Hepatic artery thrombosis (HAT) which is a serious complication after orthotopic liver transplanta- tion (OLT) remains a significant cause of graft loss. The purpose of this study was to sum up our experiences in the prevention, diagnosis and management of HAT after liver transplantation. METHODS: From April 1993 to September 2003, a total of 198 patients underwent OLT at our hospital. The hepatic artery was anastomosed using 7/0 prolane with running continuous suture in 96 patients (group 1) and with inter- rupted suture in 102 (group 2). Ultrasonography was per- formed every day in two weeks after operation and selec- tively afterwards. RESULTS: HAT occurred in 6 patients (6.3%, 6/96) of group 1, and in 1 (1%, 1/102) of group 2 (x2=4.027, P= 0.045). Six patients received emergency thrombectomy, and 1 conservative therapy but died from tumor recurrence eventually. Biliary complication developed in 3 patients af- ter thrombectomy of whom 2 died of liver failure and one waited for retransplantation. In the other 3 patients after thrombectomy, 1 died of renal failure, and 2 survived. The mortality of patients with HAT was 57.1% (4/7). CONCLUSIONS: The technique of hepatic arterial anasto- mosis is the key factor for the prevention of HAT. Routine ultrasonography is very important in early detection of HAT after OLT. Biliary complication is a severe outcome secondary to HAT. | Shu-Sen Zheng, Zhi-Yong Yu, Ting-Bo Liang, Wei-Lin Wang, Yan Shen, Min Zhang, Xiao Xu and Jian Wu Hangzhou, China Centre of Organ Transplantation and Department o Hepatobiliary and Pancreatic Surgery, First Affiliated Hospital of Medica College, Zhcjiang University, Hangzhou 310003, China | 2004 | Hepatobiliary & Pancreatic Diseases International2004，3，1： | 18 |
| 5 | Genetic lineage tracing identifies in situ Kit-expressing cardiomyocytes显示文摘 | Qiaozhen Liu Rui Yang Xiuzhen Huang Hui Zhang Lingjuan He Libo Zhang Xueying Tian Yu Nie Shengshou Hu Yan Yan Li Zhang Zengyong Qiao Qing-Dong Wang Kathy O Lui Bin Zhou | 2016 | Cell Research2016，26，1： | 12 |
| 6 | Paleoproterozoic basement beneath the southern Jiangxi Province:Evidence from U-Pb ages and Lu-Hf isotopes in zircons from the Doushui lamprophyre显示文摘这篇论文论述侵入的煌斑岩的 geochemical 分析在 Shangyou 县的古苏格兰的 Doushui 花岗石身体,南部的江西省。U-Pb 标明日期和 Hf 同位素分析特别从它为锆石被执行。Petrological 和 geochemical 特征证明煌斑岩属于 high-K,弱碱的辉石黑云母煌斑岩。它被 Mg #(0.74 ) , Ni (253 μg/g ) 和 Cr (893 μg/g ) 满足的高度描绘,并且也在不兼容的元素充实,例如 REE, Rb, Sr, Ba 和 K。它的原语融化,这被建议可能由 non-crust-derived 源于充实的披风 metasomatized 代理人。在煌斑岩标明日期锆石的结果的形态学和 LAM-ICPMS 显示他们是从深外壳的岩石捕获的 xenocrysts。在 ∼1.86 Ga 形成的大多数 xenocrystic 锆石,和在不同 Phanerozoic 时期的一些。Paleoproterozoic 锆石具有 magmatic 起源并且有类似的 176Hf/177 Hf 和 176Lu/177 Hf 比率,显示他们可能从一样的火的地下室岩石。年龄和从这地下室岩石的锆石的 Hf 同位素作文类似于在南部的浙江省的 Paleoproterozoic Danzhu 花岗石的那些,但是极其与 Nanling 地下室区分开来,建议学习区域可能是一向西在东方卡赛西亚·布洛克的 Paleoproterozoic Wuyishan 岩层的延期部分。这些 Paleoproterozoic 锆石有低 Hf 同位素作文,外壳的来源特征。这些锆石的 Hf 模型年龄和在他们以内的更旧的继承核心的存在,结合了可得到的其它数据由以前的研究报导了,建议 Paleoproterozoic 岩浆的来源是 Neoarchaean 外壳,在 Wuyishan 岩层暗示更旧的地下室的存在。U-Pb 年龄和五 Phanerozoic 锆石的 Hf 同位素显示那个 Paleoproterozoic 地下室经历了多重做的发生在古苏格兰, Indosinian 和早 Yanshanian 分别地。古苏格兰的 magmatism 也涉及少年外壳重做。 | YU JinHai WANG LiJuan O'REILLY S Y SHU LiangShu SUN Tao | 2009 | Chinese Science Bulletin2009，54，9： | 10 |
| 7 | Fibroblasts in an endocardial fibroelastosis disease model mainly originate from mesenchymal derivatives of epicardium显示文摘 | Hui Zhang Xiuzhen Huang Kuo Liu Juan Tang Lingjuan He Wenjuan pu Qiaozhen Liu Yan Li Xueying Tian Yue Wang Libo Zhang Ying Yu Hongyan Wang Ronggui Hu Fengchao Wang Ting Chen Qing-Dong Wang Zengyong Qiao Li Zhang Kathy O Lui Bin Zhou | 2017 | Cell Research2017，27，9： | 6 |
| 8 | The MRE11 GAR motif regulates DNA double-strand break processing and ATR activation显示文摘MRE11/RAD50/NBS1 建筑群是很快招募到 DNA 双海滨裂缝(DSB ) 的主要传感器。MRE11 被知道是由在它的 glycine-arginine-rich (长嘴硬鳞鱼) 以内的 PRMT1 的精氨酸 methylated 主题。在这研究,我们报导在 GAR 主题与离氨酸代替精氨酸并且产生 MRE11 缺乏 methylated 精氨酸的 RK 蛋白质。Mre11 RK/RK 老鼠对 γ 过分敏感;照耀(红外) 和从这些老鼠的房间显示了房间周期检查点缺点和染色体不稳定性。而且, Mre11 RK/RK MEF 展出了在 RPA 和 RAD51 的招募表明缺点和缺陷到损坏地点的 ATR/CHK1。M RK 形成的 RN 建筑群并且对 DNA 损坏并且通常的地点局部性响应红外激活 ATM 小径。M RK RN 建筑群在为响应红外在 vivo 观察的损害 DNA 结束切除术和 ATR 激活负责的 vitro 展出了 exonuclease 和 DNA 有约束力的缺点。我们的调查结果在 DSB 修理为 MRE11 长嘴硬鳞鱼主题的关键角色提供基因证据,并且在 MRE11 长嘴硬鳞鱼表明在 translational 以后修正之间的一个机械学的连接主题并且 DSB 处理,以及发信号的 ATR/CHK1 检查点。 | Zhenbao Yu Gillian Vogel Yan Coulombe Danielle Dubeau Elizabeth Spehalski Josee Hebert David O Ferguson Jean Yves Masson Stephane Richard | 2012 | Cell Research2012，22，2： | 5 |
| 9 | 聚酰亚胺薄膜热膨胀系数的不稳定性研究显示文摘测量了聚酰亚胺薄膜在冷热循环过程中各温度点的热膨胀系数。结果表明:聚酰亚胺薄膜的热膨胀系数具有不稳定性。 | 王晓燕 耿洪滨 何世禹 刘勇 Yu O Pokhyl K V Koval | 2005 | 绝缘材料2005，38，2： | 4 |
| 10 | 灰鹤在天山木扎提河湿地越冬及行为观察显示文摘于2017年10月—2019年5月,采用直接计数法、瞬时扫描取样法、卫星跟踪和最小凸多边形法(MCP),对新疆阿克苏地区拜城县木扎提河流域灰鹤(Grus grus)的种群特征、活动范围、行为时间分配和行为节律进行调查和分析。结果表明,2019年越冬灰鹤种群数量超过4700只,较2016年增加1倍多,种群发展动态呈上升趋势。灰鹤主要以家庭群为主(63.90%),聚集群次之(28.62%),孤鹤最少(7.48%)。家庭群主要以2成鸟1幼鸟为主(占46.82%),聚集群以5~8只个体为主(占65.91%)。整个越冬期持续140~160 d,灰鹤越冬期活动距离为1058 km,活动区域相对固定,活动区域面积为125 km^2。日活动面积和活动距离随着气温的变化而变化,温度降低,日活动范围和活动距离降低;反之,则增加。因此,活动面积和活动距离呈凹形变化,即先增加(10—11月),再逐渐减少(12—1月),然后增加(2—3月)的变化趋势。取食和警戒是灰鹤的主要越冬行为。灰鹤的46.8%日间时间用于取食,17.8%的日间时间用于警戒,用于休息、走动、理羽和其他行为的日间时间分别占13.4%、11.4%、7.4%和3.2%。日取食高峰呈双凸型,出现在8:00—9:00和17:00—18:00,分别达到57.0%和58.5%。休息高峰出现在11:00—15:00,占24.6%,呈单峰型。研究区灰鹤种群面临着放牧、农耕、天敌、道路车辆、低温和人为驱赶等诸多威胁因素。 | 李军伟 马鸣 孟凡娟 E I Ilyashenko V Yu Ilyashenko O V Belyalov A E Gavrilov S Kh Zaripova N Batbayar 曹垒 | 2020 | 生态与农村环境学报2020，36，5： | 4 |
| 11 | Dissociation behavior of “dry water” C_3H_8 hydrate below ice point:Effect of phase state of unreacted residual water on a mechanism of gas hydrates dissociation显示文摘The results on a dissociation behavior of propane hydrates prepared from 'dry water' and contained unreacted residual water in the form of ice inclusions or supercooled liquid water(water solution of gas) were presented for temperatures below 273 K.The temperature ramping or pressure release method was used for the dissociation of propane hydrate samples.It was found that the mechanism of gas hydrate dissociation at temperatures below 273 K depended on the phase state of unreacted water in the hydrate sample.Gas hydrates dissociated into ice and gas if the ice inclusions were in the hydrate sample.The samples of propane hydrates with inclusions of unreacted supercooled water only(without ice inclusions) dissociated into supercooled water and gas below the pressure of the supercooled water-hydrate-gas metastable equilibrium. | Andrey O Drachuk Vladimir P Melnikov Nadezhda S Molokitina Anatoliy N Nesterov Lev S Podenko Aleksey M Reshetnikov Andrey Yu Manakov | 2015 | Journal of Energy Chemistry2015，24，3： | 2 |
| 12 | Late Paleozoic magmatism in South China:Oceanic subduction or intracontinental orogeny?显示文摘A gneissic granite with an U-Pb age of 313±4 Ma was found in northeastern Fujian Province,South China.It is an S-type granite characterized by high K2O,Al2O3 and low SiO2,Na2O contents with high A/CNK ratio of 1.22 for the whole rock.Zircons with stubby morphology from the gneissic granite yield 206 Pb/238 U ages ranging from 326 to 301 Ma with a weighted average age of 313±4 Ma,and negative εHf(t) values from -8.35 to -1.74 with Hf model ages (TCDM) of 1.43 to 1.84 Ga.This S-type granite probably originated from late Paleoproterozoic crust in intracontinental orogeny.Integrated with previous results on paleogeographic reconstruction of South China,the nature of Paleozoic basins,Early Permian volcanism and U-Pb-Hf isotope of detrital zircons from the late Paleozoic to early Mesozoic sedimentary rocks,we suggest the occurrence of a late Paleozoic orogeny in the eastern Cathaysia Block,South China.This orogenic cycle includes Late Carboniferous (340-310 Ma) orogeny (compression) episode and Early Permian (287-270 Ma) post-orogenic or intraplate extension episode.Therefore,the late Paleozoic magmatism in the southeastern South China probably occurred during the intraplate orogeny rather than the arc-related process. | YU JinHai LIU Qian HU XiuMian WANG Qin O'REILLY Suzanne Y | 2013 | Science China(Technological Sciences)2013，56，3： | 2 |
| 13 | Twist Regulates Cytokine Gene Expression through a Negative Feedback Loop that Represses NF-κB Activity显示文摘 | Dra?en ?o?i? James A. Richardson Kai Yu David M. Ornitz Eric N. Olson | 2003 | Cell2003，，2： | 2 |
| 14 | CD44 Variant Regulates Redox Status in Cancer Cells by Stabilizing the xCT Subunit of System xc ? and Thereby Promotes Tumor Growth显示文摘 | Takatsugu Ishimoto Osamu Nagano Toshifumi Yae Mayumi Tamada Takeshi Motohara Hiroko Oshima Masanobu Oshima Tatsuya Ikeda Rika Asaba Hideki Yagi Takashi Masuko Takatsune Shimizu Tomoki Ishikawa Kazuharu Kai Eri Takahashi Yu Imamura Yoshifumi Baba Mitsuyo O | 2011 | Cancer Cell2011，，3： | 2 |
| 15 | Glucose-6-phosphate dehydrogenase (G6PD) variants in Malaysian Malays显示文摘 | Ainoon O Yu YH Amir Muhfiz AL et a2 | 2003 | Hum Mutat2003，21，1： | 1 |
| 16 | Solid and soft nano -structured materials:Fundamentals and applications 显示文摘 | WILLANDER M NUR O LOZOVIK Yu E | 2005 | Micro electronics Journal2005，，7： | 1 |
| 17 | Factors affecting Agrobactcrium-mediated transformation and regeneration of sweet orange and citrange 显示文摘 | Yu C H Huang S Chen C X Deng Z A Ling P and Gmitter F O J | 2002 | Plant Cell Tissue and Organ Culture2002，71，： | 1 |
| 18 | Dynamic knowledge inference and learning under adaptive fuzzy Petri net framework显示文摘 | LI X O YU W FELIPE LARA-ROSANO | 2000 | IEEE Trans on System Man and Cybernetics Part C:Applications and Reviews2000，30，4： | 1 |
| 19 | Evidence for an important role of WRKY DNA binding proteins in the regulation of NPR1 gene expression 显示文摘 | Yu O Chen C Chert Z | 2001 | The Plant Cell2001，13，7： | 1 |
| 20 | A Computer-aided System to Retrieve Tribological Data显示文摘 | Kholodilov O V Kirpichenko Yu E | 1994 | Trenie Iznos1994，15，4： | 1 |
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