THREE NEW SPECIES OF RHODODENDROH FROM SZECHUAN

Rhododendron Hoii Fang,spec.nov.Plate1.Frutex0.6-1 m.altus;ramuli nigrescenti-lepidoti,hornotini sicco brunnei,annotini cinerei vel nigrescenti-cinerei.Folia coriacea,elliptica,1.5-2 cm.rarius 2.5cm.longa,1—1.2 cm.lata,apice brevissime acuta et mucronulata,basi subrotundatavel late cuneata,margine paullo recurvata,supra atroviridia,nitidula,non-lepidota,subtus cinnamomo-brunnea,lepidota,squamulis (glandulis) contiguis     

湖南树木三新种

<正> 1.石门鹅耳枥 新种 图版I∶1 Carpinus shimenensis C. J. Qi, sp. nov. Species insignis, ab omnibus speciebus generis foliis late ellipticis, vel late ovatooblongis, minoribus, 3-5 cm longis, 2-3 cm latis, margine acute dentato-duplica-to-serratis, nervis lateralibus 11-13 jugis, supra manifeste impressis, subtus conspicueelevatis, dense villosis, bracteis frucferis semiovatis vel semiovato-rotundis, extra marginedentato-lobatis, intra margine basi auritis facile distinguibilis. Arbor decidua alta 5 m, trunco 20 cm diametro; ramuli juvenales atro-grisei, deindelaete brunnei, internodiis brevissimis. Folia papyracea, elliptica, vel ovato-elliptica, 3-5cm longa, 2-3 cm lata, apice abrupte acura, obtusa vel aliquantum rotunda, basi cordata,aliquantum obliqua, supra adpresse byssaceo-villosa, nervis lateralibus utrinsecus 11-13,distantioni nervi 2-3 mm, cum costis supra impressis, subtus manifeste elevatis, margineirregulariter dentato-duplicato-serratis, serraturis abrupte acutis; petioli breves, crassi,4-11 mm longi, dense villosi; stipulae persistentes, circ. 7 mm longae, rubrobrunneae.Spica fructifera 3-3.5 cm longa, in rhachidi villosae; nuculae ovato-rotundae, circ. 4 mm     

内蒙古西部黄芪属一新种

中戈壁黄芪新种图版Ⅰ Astragalus centrali-gobicus Z. Y. Chu et Y. Z. Zhao sp. nov. Species A. leasanico Ulbr. similis, sed foliolis 3—9, lanceolato-ellipticis vel lanceolato-ovatis, 10—30 mm longis, 5—15 mm latis; corollis flavis, apice leviter roseolis; leguminibus mature circ. 4.5 cm longis differt. Species A. hamiensi S. B.     

贵州树木新分类群及新分布(续)

<正>长柄核果木 新种(图1) Drypetis longipes X. H. Song, sp, nov. Species foliis intergris, pedicellis fructuum 3～4cm. longis instractis. Arbuscula sempervirens, 8 m. alta, tranco 14 cm diam., cortice cineracei, levi,tenuiramis cernuis cinereis vel flavidi-inereis, lenticellis suberosis leviter elevatis,ramulis hornotinis interdum pubescentibus, deinde glabris. Folia alterna tenuicoriacea vel crassi-chartacea, elliptica vel ovato-elliptica, 7～10cm. longa et 3～4cm. lata, apice acuminata vel brevicaudata, acumine obtusis, basi cuneata, obliqua,utringque glabra, nitide, costa media supra elevata vel plana subtus elevata, nervis alteralibus utrinsecus 7～8(～9), curvis, prope marginem consutis, nervulis,subparallelis, subtus elevatis, manifestis, petiolis 3～5mm. longis, purpureis interdum pubescentibus. Fructus juvenes plerumque singulares, globosis viridis,dense brevipubescentis, stylis brevissimis 2-lobatis, persistentibus, stigmatibus latissimis, reniformibus, pedicellis 3～4cm. longis.     

中国肥皂荚属一新种

<正>我们在《中国树木志》苏木科的编写过程中,在广西发观肥皂荚属一新种,观报道于下: 广西肥皂荚 新种 图版Ⅰ Gymnocladus guangxiensis P. C. Huang et Q. W. Yao, sp. nov. Affinis Gymnocladi chinensi Baill., sed pinnis trijugatis, rhachibus rhachillisque glabris seve vix puberulis, foliolis 12 vel 14, maioris, 3.4—7cm. longis, 1.8—2.8cm.latis, leguminibus purpureofuscis, nitidis differt. Guangxi: Xingan, Tabianxiang, Xingan Exp. 158 (Typus fr. in Herb. coll. Indust. Silv. Nank. Conserv. ) ; Jinxiu, S. Y. Liang et al, 294.     

云南木兰科新植物

1 显脉木兰新种 Magnolia phanerophlebia B. L. Chen, sp. nov. Arbor parva glaberrima, c. 3 m alta. 6 cm in diam., cortice incano laevi: ramuli junniores virides in sicco cinerascentes et pruinosi. Folia sempervirentia, lamina rigide coriacea, obovata vel obovato-elliptica'35-43cm longa, 10-17 cm lata, apice acuta vel breviter acuminata, basi anguste cuneata, supra nitidissima     

Two New Varieties of Stipa (Gramineae) from Nei Mongol

1 Stipa glareosa P.Smirn.var.langshanica Y.Z.Zhao,var.nov.(Fig.1)Species S.glareoeae P.Smirn.affinis,sed aristis inferne tortilibus 3～5mm longis;lemmatis 5～7mmlongis,glabris vel minute pilosis.Herba perennis,dense caespitosa,10～20cm alta.Vaginae pubescentes,margine pilosae;ligulae ad1mm longae,margine dense villosae;laminae 0.3～0.8mm in diam.,extus (subtus) et intus (supra)pubescentes;folia caulina 2～3cm longa,radicalia 4～9cm longa.Paniculae comnactae,in vaginis termi-nalibus;glumae 18～23mm lonsae,3 nerviae,apice longissime acutatae;lemmata 5～7mm longa,glabravel margine et dorso infera medium secus costam pilosa,apice glabra vel minute pilosa,callo circ.1mm lon-go dense pilosis;aristae 3～4.5cm lonsae,unigeniculatae,segmento infimo torto,3～5mm longo,pilis ad     

Post-collisional extensional and thrust-nappe structures in northern part of Dabie Mountains

Thrust-nappe structures and extensional structures simultaneonsly occur in the northern part of the Dabie Mountains. The systematic structural study reveals that extensional structures along the Mozitan-Xiaotian fault and thrust-nappe structures that take the Jinzhai-Shucheng fault as their frontal thrust share the same shear sense, and display a transitional relationship from the ductile extensional structure of deep level in the south to the ductile-brittle and brittle thrust-nappe structure of shallow level in the north. The extensional and thrnst-nappe structures in the region are explained to result from post-collisional processes by the continuous subduction of the Yangtze continental block and the extension induced by the uplifting of the core part of the Dabie Mountains, which are components of the exteasional structures produced in the exhumation process of the ultrahigh pressure metamorphic rocks in the Dabie Mountains. Because of the frontal blocking in the process of the north-westward spreading, the extension and detachment of the low-grade metamorphic rocks along the Mozitan-Xiaotian fault was transformed into the northwestward thrustiag, resulting in the thrust-nappe structures. They developed in the period of 200-170 Ma, maybe last till the late Jurassic.     

放牧和封育条件下金露梅灌丛草地群落动态变化的研究

对放牧和封育条件下金露梅灌丛群落动态变化进行了研究.结果表明：金露梅灌丛群落种类数量在放牧条件下不会发生明显的改变（P＞0.05）,在封育条件下出现轻微的先增后减的变化格局;盖度和地上生物量在放牧条件下6-7月无明显的差异,到9月上旬呈现下降趋势,显著地低于前期（P＜0.05）;在封育条件下7月下旬后趋于稳定状态,且明显地高于6月底的数值（P＜0.05）.群落的平均高度在放牧条件下无明显变化（P＜0.05）,在封育条件下呈现逐步增高的趋势,不同时期有明显的差异（P＜0.05）.     

河南省栾川县梅花石资源特征及开发利用研究

河南省栾川县潭头镇—秋扒乡一带是栾川梅花石的主产区.为了研究其资源特征,开展了栾川梅花石资源野外勘查,并对其物理性质、化学性质进行了测试分析.研究结果表明,其原岩为中元古界熊耳群中酸性火成岩,包括杏仁状安山岩、杏仁状粗安岩、杏仁状流纹岩、杏仁状英安岩及杏仁状玄武安岩.栾川梅花石储量丰富,无放射性污染,抗压强度高,具极高的观赏价值和收藏价值.最后,对栾川梅花石的合理开发及利用提出了一些建议.     

甘南亚高寒草甸金露梅叶片氮磷化学计量学动态

通过甘南地区金露梅的研究,以营养元素的不同水平供给为外部驱动因素,有无繁殖过程为内部因素,比较分析了金露梅叶片氮磷化学计量学的变化特征.研究结果表明:施肥显著影响了叶片的w(N)和w(P),施肥后叶片的w(N)依次为17.8,18.9,20.1,22.6 mg/g,w(P)依次为1.92,2.05,2.19,2.58 mg/g,但施肥对w(N):w(P)的影响不显著.繁殖显著降低了叶片的w(N)和w(N):w(P),而对w(P)影响不显著.外部和内部因素对金露梅叶片的化学计量学的影响不相同.不同的施肥水平显著影响金露梅叶片的w(N)和w(P),而对w(N):w(P)影响不显著.证明繁殖过程导致了氮的大量消耗和w(N):w(P)的显著降低.金露梅在内外因素的影响下分别表现了w(N):w(P)的趋同和分异.     

35 ka BP climate simulations in East Asia and probing the mechanisms of climate changes

Interglacial or postglacial climates are all of charac-teristic of warmer conditions. However, if condition asso-ciated with the warm feature is wetter or drier than today,it would produce different impacts on natural environ-ments and human society. Quaternary studies found thatclimate with warm-dry or warm-wet conditions had oc-curred in China during the last 40—30 ka BP[1]. For ex-ample, it was warmer than the present during themid-Holocene (3—8 ka BP) and the late phases of MarineIsot…     

Simulation of sea surface temperature changes in the Middle Pliocene warm period and comparison with reconstructions

The Middle Pliocene (ca 3.12–2.97 Ma) is a recent warm period in the Earth’s history. In many respects, the warmth of the Middle Pliocene is similar to the probable warm situation of the late 21st century predicted by climate models. Understanding the Middle Pliocene climate is important in predicting the future climate with global warming. Here, we used the latest reconstructions for the Middle Pliocene—Pliocene Research Interpretation and Synoptic Mapping (PRISM) version 3—to simulate the Middle Pliocene ...     

Timing and history of marine hydrocarbon accumulation in Tarim craton

<正> Based on the analyses of hydrocarbon inclu-sions, K-Ar dating of authigenic illites and oil/gas-watercontact retrospection as well as other methods, the marineprimary reservoirs in the cratonic region of the Tarim Basinare found to have been formed in the late Caledonian toearly Hercynian, late Hercynian, and Himalayan, and oil andgas adjusted and redistributed in the Yanshanian (Jurassic toCretaceous) and Himalayan (Tertiary). The analyses alsoshow that the remaining primary oil accumulations aremostly formed in the late Hercynian, and the secondary oilreservoirs resulted from the adjustment and redistribution ofthe earlier accumulations during the Yanshanian and Hima-layan (especially late Himalayan), of which the Himalayan isalso the major stage of gas accumulation. The primary oilreservoirs formed in the late Hercynian mostly occur withinthe Paleozoic formation, whereas the secondary reservoirsformed in the Himalayan in the Mesozoic. The late adjust-ment and redistribution of reservoirs in the craton region ofthe Tarim Basin is ubiquitous because of the intensified tec-tonic movements since the Mesozoic, especially Cenozoic andintrusion of the high- to over-mature gas. Furthermore, thelower amplitude of reservoirs in the craton region also makesthem easier to be adjusted and redistributed. Therefore, theremaining paleo-uplift and palaeo-slope developed in rela-tively stable tectonic regions are the main potential areas forthe middle-large marine reservoirs in the Tarim Basin.     

中国槭属一新种

<正> 利川械 新种图1 Acer lichuanense C.D.Chu et G.G.Tang Species A.huiani Fanf et Hsieh et A.thomsonii Miq.subsimilis,ab illo lobis lateralibus foliorum minoribus vel inconspicuis,nervis secundariis paucioribus 7-9 jugis,petiolis pubescentibus,a hoc basi foliorum trinervis non quinquenervis non quinquenervis,pedicellis fructuum brevioribus,samaris minoribus differt.     

Decadal northward shift of the Meiyu belt and the possible cause

The feature of the decadal movement of the Meiyu belt and their association with East Asia atmospheric circulation for the period of 1979―2007 is examined in this study. It is shown that the Meiyu belt of China has a decadal shift in the late 1990s. There is a remarkable difference between the periods before and after 1999, with the Meiyu belt mainly located to the south of the Yangtze River valley before 1999, but afterward mainly located in the Huaihe River valley. At the same time, a distinctive tropospheric warming and stratospheric cooling trend is found in the mid-latitudes of East Asia, which causes the upper tropospheric pressure surfaces upward bulging and the tropoause elevated in the subtropics and associated widening of the subtropical area over East Asia. Accompanying the subtropics widening, the subtropical westerly jet over East Asia shifts northward and the East Asia tropical Hadley circulation expands poleward, which results in the northward shift of the Meiyu belt.     

Hydrocarbon charging histories of the Ordovician reservoir in the Tahe oil field, Tarim Basin, China

The Ordovician reservoir of the Tahe oil field went through many tectonic reconstructions, and was characterized by multiple hydrocarbon chargings. The aim of this study was to unravel the complex charging histories. Systematic analysis of fluid inclusions was employed to complete the investigation. Fluorescence observation of oil inclusions under UV light, and microthermometry of both oil and aqueous inclusions in 105 core samples taken from the Ordovician reservoir indicated that the Ordovician reservoir underwent four oil chargings and a gas charging. The hydrocarbon chargings occurred at the late Hercynian, the Indo-Sinian and Yanshan, the early Himalaya, the middle Himalaya, and the late Himalaya,respectively. The critical hydrocarbon charging time was at the late Hercynian.     

青竹梅果浆对H_2O_2溶血及离体肝匀浆脂质过氧化的拮抗

本文建立H_2O_2红细胞氧化溶血及肝匀浆振荡引发脂质过氧化模型以进一步考察青竹梅的抗氧化活性。实验发现,H_2O_2对红细胞有直接溶血的作用,随H_2O_2浓度增加,溶血度递增,相关极显著(P<0.01),本文选用2mMH_2O_2浓度建立溶血模型。青竹梅浆对氧化溶血有拮抗作用,当加入10—100μl 50％果浆(相当果肉量5.0—50.0μg)到2mMH_2O_2溶血系统时见溶血度递降,下降率从20.7％—55.8％。又见青竹梅浆具有明显的抗肝匀浆脂质过氧化作用,且随浆量增加,抑制率加大,该抑制效果与公认的抗氧化剂——五味子比约强6—7倍。     

对若干影响青竹梅果浆营养成份和抗氧化活性因素的考察

青竹梅果浆具有高酸度(5%)、高蛋白(1.6%)和低糖(1.5%)特征.果浆含16—17种氨基酸,其中天门冬氨酸含量很高,几乎占总氨基酸量的60—70%.发现果浆酸度对抗氧化活性有一定影响,但无线性关系,测试了外源柠檬酸的抗氧化活性,发现其抑制率仅占果浆总活性的三分之一.分析了在制备果浆中几种辅料的影响,其中只有 NaCl 有较大干扰.采用不同温度处理果浆未见抗氧化活性的显著变化,证明果浆热稳定性好,同时又观察室温与低温贮存八周果浆的变化,未见其抗氧化活性的明显衰减。     

Neural correlates of moral judgment of lying： An event-related-potential study

The present study investigated neural mechanisms of moral judgment of lying in adults using high-density event-related potentials (ERPs). Participants were recruited to do moral judgment of 200 stories including two types of lying and their corresponding truth-telling. The results showed that both types of lying were judged more negative than their corresponding truth-telling, and moral judgment of black lying was more negative than that of modest lying. There were two main components of the ERPs evoked by the test stimuli. One was an early component, peaking at about 200 ms, and the other was a late component, peaking at about 400 ms. Over the frontal scalp sites, the early component was positive and the late component was negative, while they both reversed over the posterior sites. The ERPs of both types of lying was more positive than that of their corresponding truth-telling in the time window of 600—900 ms at the posterior sites.