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neo
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     Seven compounds (A 1—A 7) were isolated from the seeds of Annona squamosa L.Three of them, A 2, A 3, and A 5, are new compounds of annonaceous acetogenins, and they were name neo desacetyluvaricin (A 2), neo annonin B (A 3) and neo reticulatacin A (A 5), respectively.
     从番荔枝(Annona squam osa L.)的种子中分离到A1—A7共7个化合物,其中A2、A3和A5为的番荔枝内酯,分别命名为-去乙酰紫玉盘素(neo-desacetyluvaricin, A2)、阿诺宁乙(neo-annonin B, A3)和牛心番荔枝素甲(neo-reticulatacin A, A5)。
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     Construction of pMCLacⅠ/Neo plasmid and a new strategy for studying gene mutation
     pM CLacⅠ/Neo质粒的构建和基因突变研究的策略
短句来源
     FUJI New Middle Type NEO SC Series Electromagnetic Contactor
     富士中型NEO SC系列电磁接触器
短句来源
     They are β sitosterol,β sitosterol β D glucoside,apigenin,hesperetin rutinoside,18,19 dihydroxy 5α,10β neo cleroda dien butenolide,18 O β D glucopyranosyl 19 hydroxy neo cleroda dien butenolide.
     它们分别为 :β 谷甾醇 ,β 胡萝卜甙 ,芹菜素 ,18,19 二羟基 5α ,10 β 克罗烷 二烯 丁烯羟酸内酯 ,橙皮甙 ,18 O β D 吡喃葡萄糖 19 羟基 克罗烷 二烯 丁烯羟酸内酯。
短句来源
     Results Eight compounds were isolated and identified as: tanshinone II A (I), crypotanshinone (II), przewaquinone A (III), sugiol (IV), ursolic acid (V), 2α,3α dihydroxy urs 12 ene 28 acid (VI), oleanolic acid (VII), and neo przewaquinone A (VIII).
     结果 获得并鉴定了 8个化合物结构 :丹参酮II A(I) ,隐丹参酮 (II) ,紫丹参甲素(III) ,柳杉酚 (IV) ,熊果酸 (V) ,2α ,3α 二羟基乌苏 1 2 烯 2 8 酸 (VI) ,齐墩果酸 (VII) ,甘西鼠尾酮A(VIII)。
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  “neo”译为未确定词的双语例句
     After being treated with adriamycin for 24 h,the percentages of apoptotic cells in BIU87 and BIU87/neo were (23.75±3.72)%,(21.94±1.27)% respectively,but those in the BlU87/bcl-2 cells were(3.38±0.95)%(P<0.01).
     ADR作用24 h后,BIU87、BIU87/neo细胞凋亡率分别为(23.75±3.72)%、(21.94±1.27)%,而BIU87/bcl-2细胞为(3.38±0.95)%(P<0.01);
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     The intracellular ROS levels of BIU87,BIU87/neo and BIU87/bcl-2 were (90.45±1.96)%,(88.41±3.88)% and(77.00±3.86)% respectively,and those of BIU87/bcl-2 cells were lower significantly than those of BIU87,BIU87/neo(P<0.01).
     ROS分别为(90.45±1.96)%、(88.41±3.88)%和(77.00±3.86)%,BIU87/bcl-2细胞较前两者明显降低(P<0.01)。
短句来源
     RT-PCR results demonstrated bcl-2 mRNA levels of BIU87/bcl- 2 cells were significantly higher than those of BIU87 and BIU87/neo(P<0.01).
     RT-PCR BIU87/bcl-2细胞的bcl-2 mRNA水平显著高于BIU87、BIU87/neo(P<0.01)。
短句来源
     Group II (N0.015M) received NEO 0. 015mg/kg with MOR 0.025 mg/kg caudally.
     Ⅱ组(N_(0.015)M组),NEO 0.015mg/kg+MOR 0.025mg/kg;
短句来源
     Group III(N0.02M) received NEO 0.02 mg/kg with MOR 0.025 mg/kg caudally.
     Ⅲ组(N_(0.02)M组),NEO 0.02mg/kg+MOR 0.025mg/kg。
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  相似匹配句对
     Neo-localization
     通信大鳄的“新本地化”
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     On Neo-Terrorism
     试论新恐怖主义
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  neo
The relict genera once occupied huge areas in the northern hemisphere in the Tertiary or the late Cretaceous, while neo-endemism mostly originated in the late Tertiary.
      
These results suggest that upon exposure of DNA to 1O2, neo-epitopes are generated, which may be one of the factors for the induction of circulating autoantibodies in the three diseases.
      
In pCI.ARS-neo, ARS was from autonomously replicating stable transgene pr8a of silkworm Bombyx mori.
      
In pCI.ori-neo, chromosomal ori was from the human c-myc locus.
      
Analysis of the maintenance of pCI.ARS-neo and pCI.ori-neo in transgenic mice and in cultured immortalized human T cells revealed the interplay of transcription and replication, as the CMV element suppressed autonomous replication of both plasmids.
      
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In recent years, the geotectonic problem of China engages the attentionof many Chinese and Soviet geologists, but different opinions are confessed by different authors. After studying the structural characters of the fundamentalfloor and its later geological development, theauthor of this paper agrees withthe statement of the Soviet geologist, B. M. Синицын. In 1952 he pointed outthat the Chinese platform in eastern China, may bs divided into: (1) theSine-Korean platform; and (2) the Southern-Chinese platform,...

In recent years, the geotectonic problem of China engages the attentionof many Chinese and Soviet geologists, but different opinions are confessed by different authors. After studying the structural characters of the fundamentalfloor and its later geological development, theauthor of this paper agrees withthe statement of the Soviet geologist, B. M. Синицын. In 1952 he pointed outthat the Chinese platform in eastern China, may bs divided into: (1) theSine-Korean platform; and (2) the Southern-Chinese platform, consolidatedas a result of the Luliang movement. This Chinese platform especially in its southern part shows a very peculiarphenomenon as it is called "Activization" of the platform. During Sinian andPaleozoic, its sediments belonged to the pronounced epi-continental type, duringthe mesozoic the south-eastern part of the Southern-Chinese platform wasneither a stable shelf nor a geosyncline, but an intermediate type between them.Its characters were really not geosynclinal, but sometimes showed geosynclinalaffinities, as for instances, the immense granitic intrusions, the eruptions oflavas, and the rather strongly folded geosynclinal structures. These imply thelimited mobility or the incomplete consolidation of the underground. Accor-dingly, referred to the structural type of this region, P. Misch called it"Sinotype". Furthermore, in the Southern-Chinese platform, two strong "Activizingunits" are recognized as follows: 1) The Hunan-Kwangsi activizing andsubsiding region; 2) The Cathaysian activizing oldland. The "Activization"of these regions lasted for a long geological time. It began in Sinian, throughCaledonian, Variscian, Indo-Sinian, Yenshanian and even Himalayan. BeforeMesozoic, the Caledonian was the most intensive and widely distributed one.But as pointed out by A. H. Мазарович, the Caledonian of the Southern-Chineseplatform was merely a fold-belt within the platform. According to its geotectonic history, its character of sedimentation, itsregional metamorphism, its igneous activity and its geotectonic systems, suchas "Kwangsi ∈ system", "North-Kwangtung ∈ system", "Meso and Neo-Cathaysiansystem", and the "Nanling eastwest tectonic zone", it is the author's opinionthat the "Imtermediate type (Sinotype)" of the Southern-Chinese platform wasdeveloped gradually through a long "Activizing process". This "Sinotype" is anintermediate type between the stable shelf and the geosynclinal region.

作者同意B.M.西尼村的意见,认为中国地台是中国东部的一个大的构造单位,它是在吕梁运动后造成的。中国地台由两个主要部分构成,它的北部称中朝地台,南部称华南地台。中国地台有一很重要的特征,就是一个“活化”的地台。华南地台的东南部“活化”尤其强烈而显著,在中生代的太平洋运动时,差不多具有类似地槽的特征。但是它的“活化”是有悠久历史的,即开始於震旦纪,所以加里东运动给与很大的影响,但加里东运动只是地台内部的褶皱。地台“活化”直到中生代太平洋运动才得到高度发展,产生巨大的火成活动以及“中国式”的构造型式。新生代时地台还有中等强度的运动和火成活动。自第四纪冰期之后,地台仍在较弱的升降运动中。华南地台无论从沉积岩相、区域变质及火成活动,或从山字型、华夏式及南岭东西褶皱的构造体系等构造型式发育史的研究,都可以看到它的“活化”过程,在这过程里发育了“过渡类型”的构造形态,这都是不同放地槽或地台的构造形态的。本文是作为学习心得性质的初步尝试,文中不成熟和谬误之处尚多,希望得到大家的指正。如果能在集体的讨论和研究之下将我国大地构造研究清楚的话,这是作者所衷心期望的。

A greatly enhanced extraction (synergism) has been shown to exist in the system M(111)/H2Sal/TBP/diluent, where M(111) denotes lanthanum, praseodyniurn or neo-dynium, H2Sal is salicylic acid, TBP is tributyl phosphate. Benzene, cyclohexane, kerosene and carbon tetrachloride have been used as diluents. The distribution coefficient increases by a factor of > 104 - 105 in comparison with that when either TBP or salicylic acid is added alone as extracting agent. The extractable species is found to be M(HSal)3...

A greatly enhanced extraction (synergism) has been shown to exist in the system M(111)/H2Sal/TBP/diluent, where M(111) denotes lanthanum, praseodyniurn or neo-dynium, H2Sal is salicylic acid, TBP is tributyl phosphate. Benzene, cyclohexane, kerosene and carbon tetrachloride have been used as diluents. The distribution coefficient increases by a factor of > 104 - 105 in comparison with that when either TBP or salicylic acid is added alone as extracting agent. The extractable species is found to be M(HSal)3 (TBP)2, using benzene as diluent. The temperature dependency of the distribution coefficient has also been determined.

1.以水杨酸和磷酸三丁酯混合萃取鐧、镨、钕的硝酸盐时,在PH6.20左右有协同效应产和。 2.温度变化对协同效应有很大影响,随着温度升高萃取率显著下降。 3.以苯为稀释剂时被萃取络合物的组成为M(HSal)_3(TBP)_2,其中M=La(Ⅲ),Pr(Ⅲ),Nd(Ⅲ)。 4.在研究过的八种不同稀释剂中,四种“惰性稀释剂”卽环己烷,煤油,四氯化碳及苯中有协同效应产生,其中以在环己烷中的分配比为最大。

The foraminifera described and figured in this paper were collected from theChanghsing formation in Western Guizhou.They were found together with Palaeofu-sulina and Brachiopods in calcareous siltstone and light grey limestone.12 generaand 13 species(including 7 new species)are here listed below:Nodosaria delicatasp.nov.,Lingulina strigata sp.nov.,Frondicularia inflata(K.M.-Maclay),Colaniellanana K.M.-Maclay,Colaniella cylindrica K M.-Maclay,Geinitzina tcherdynzevi K.M.-Maclay,Padangia cf.perforata Lange,Pachyphloia...

The foraminifera described and figured in this paper were collected from theChanghsing formation in Western Guizhou.They were found together with Palaeofu-sulina and Brachiopods in calcareous siltstone and light grey limestone.12 generaand 13 species(including 7 new species)are here listed below:Nodosaria delicatasp.nov.,Lingulina strigata sp.nov.,Frondicularia inflata(K.M.-Maclay),Colaniellanana K.M.-Maclay,Colaniella cylindrica K M.-Maclay,Geinitzina tcherdynzevi K.M.-Maclay,Padangia cf.perforata Lange,Pachyphloia pigmobesa sp.nov.,Hemigordiusplautus sp.nov.,Agathammina ovata sp.nov.,Multidiscus semiconcavus sp.nov.,Neo-discus qinglongensis sp.nov.and Robuloides acutus Reichel.So far as the faunal featuresis concerned,the genera Colaniella and Robuloides are known to be widely distributedin the Tethyan region.The genus Colaniella may be regarded as one of zonefossils for the Changhsing limestone in Sichuan,Shanxi,Jiangxi and Hunan of China.Frondicularia inflata(K.M.-Maclay),Colaniella nana K.M.-Maclay,Colaniella cylind-rica K.M.-Maclay and Geinitzina tcherdynzevi K.M.-Maclay,etc.have been knowncommonly from the Upper Permian of N.Csucasus,U.S.S.R..Robuloides acutus Rei-chel has been reported from the foraminiferal limestone of Greece.Accordingly,theforaminiferal fauna from the Changhsing formation in Western Guizhou,accepted asbelonging to late Upper Permian in age,may be correlated with that from the Nikitinformation in N.Caucasus.

本文描述的有孔虫化石计12属、13种,其中包括7新种。多数化石是根据分离出来的完整壳体和做定向切片的观察和研究的。讨论了Angulodiscus 和Multidiscus 两个属的归属,并讨论了含有孔虫化石的地层时代应属晚二叠世。

 
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