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1.
盘波  温放 《广西科学》2019,26(1):89-94
报道了湘桂粤地区8种苦苣苔科植物的省级分布新记录。包括:湖南省级分布新记录的皱边马铃苣苔Oreocharis crispate W. H. ChenY. M. Shui、革叶石山苣苔Petrocodon coriaceifolius (Y. G. Wei) Y. G. WeiMich.M?ller;广东省级分布新记录的多花石山苣苔Pet. multiflorus Fang WenY. S. Jiang、弯果奇柱苣苔Deinostigma cyrtocarpa (D.FangL.Zeng) Mich.M?llerH.J. Atkins;广西省级分布新记录的粉花半蒴苣苔Hemiboea roseoalba S.B. Zhou,Xin HongF. Wen、江华小花苣苔Primulina jianghuaensis K.M. LiuX.Z.Cai、封开报春苣苔P. fengkaiensis Z.L. NingM. Kang、密花石山苣苔Petrocodon confertiflorus H.Q. LiY.Q. Wang,并提供了这些省级分布新记录种的标本引证和地理分布信息。  相似文献   

2.
牟村  彭春良  张帆 《广西科学》2019,26(1):141-145
通过对中国湖南省苦苣苔科植物野外调查以及文献资料整理,从苦苣苔科植物的属种组成、区系成分及地理分布特征等方面,阐述湖南省苦苣苔植物多样性现状。湖南省内共有苦苣苔科植物17属81种(含种下单位,下同),无特有属;特有种23种,占总种数28.40%。省内苦苣苔科植物主要分布于湘西北和湘西南地区。种数排前五的属为广义报春苣苔属(24种)、广义马铃苣苔属(17种)、半蒴苣苔属(9种)、石山苣苔属(6种)、长蒴苣苔属(5种)及吊石苣苔属(5种)。地理成分以热带成分为主。在种的分类水平上,特有成分所含种数32种,占总种数的45.07%,表明湖南省苦苣苔科植物特有性较高。针对苦苣苔科植物分布特性以及湖南苦苣苔科植物多样性现状,本文给出了合理保护与开发利用省内野生资源的建议。  相似文献   

3.
贵州地处中国西南,苦苣苔科植物资源丰富,近年来有若干个新种在贵州被发现,并被合格发表。为了让研究贵州省植物的高校、研究单位的师生和科研人员更好地了解、认知这些新分类群,现逐步将这些新类群的形态描述翻译成中文,并辅以引自原文的配图。本篇收录了无毛光叶苣苔Glabrella leiophylla(Fang WenY.G.Wei) Fang Wen,Y.G.WeiMich.M?ller、盘州马铃苣苔Oreocharis panzhouensis Lei Cai,Y.GuoF.Wen、锯缘报春苣苔Primulina serrulata R.B.ZhangF.Wen、长筒石山苣苔Petrocodon longitubus Cong R.LiYang Luo。  相似文献   

4.
贵州地处中国西南,苦苣苔科植物资源丰富,近年来有若干个新种在贵州被发现,并被合格发表。为了让研究贵州省植物的高校、研究单位的师生和科研人员更好地了解、认知这些新分类群,现逐步将这些新类群的形态描述翻译成中文,并辅以引自原文的配图。本篇收录了兴义石蝴蝶Petrocosmea xingyiensis Y.G.Wei et F.Wen、凹柱苣苔Litostigma coriaceifolium Y.G.Wei,F.Wen et M.Mller、文采后蕊苣苔Opithandra wentsaii Z.Y.Li以及红花大苞苣苔Anna rubidiflora S.Z.He,F.WenY.G.Wei。  相似文献   

5.
《贵州科学》2021,39(4)
报道了产自贵州省的2个新记录植物,分别是富源杜鹃Rhododendron fuyuanenseZ.H.Yang(杜鹃花科)和江西半蒴苣苔Hemiboeasubacaulis Hand.-Mazz.var.jiangxiensis Z.Y.Li(苦苣苔科)。  相似文献   

6.
贵州地处中国西南,苦苣苔科植物资源丰富,近年来有若干个新种在贵州被发现,并被合格发表。为了让研究贵州省植物的高校、研究单位的师生和科研人员更好地了解、认知这些新分类群,现逐步将这些新类群的形态描述翻译成中文,并辅以引自原文的配图。本篇收录了桐梓石山苣苔Petrocodon tongziensis R.B.ZhangF.Wen、都匀马铃苣苔Oreocharis duyunensis Z.Y.Li,X.G.XiangZ.Y.Guo、绥阳半蒴苣苔Hemiboea suiyangensis Z.Y.Li,S.W.LiX.G.Xiang、齿瓣马铃苣苔Oreocharis odontopetala Q.FuY.Q.Wang。  相似文献   

7.
以苦苣苔科植物半蒴苣苔(Hemiboea henryi Clarke)、温州长蒴苣苔(Didymocarpus cortusifolius(Hance)W.T.Wang)、牛耳朵(Chirita eburnea Hance)和大花旋蒴苣苔(Boea clarkeana Hemsl.)为材料,测定并比较了它们的生理生态因子、光合作用和叶绿素荧光参数.结果表明:4种苦苣苔科植物的净光合速率日变化曲线均为双峰曲线,峰形也相似;4种苦苣苔科植物均有较低的光补偿点和光饱和点,以及较高的CO2补偿点和CO2饱和点,说明低光照(600~750μmol·m-2·s-1)和高CO2浓度(1277—1965mg/m3)可以有效促进植物的生长和发育.叶绿素荧光参数的测定结果显示:随着光合有效辐射从0μmol·m-2·s-1增加到1400μmol·m-2·s-1,4种苦苣苔科植物的光系统Ⅱ实际光化学量子产量和光化学猝灭值逐渐下降,表观电子传递速率和非光化学猝灭值则增加;光化学量子产量、表观电子传递速率和光化学猝灭的大小顺序为温州长蒴苣苔〉牛耳朵〉半蒴苣苔〉大花旋蒴苣苔,非光化学猝灭均值的大小顺序为牛耳朵〉半蒴苣苔〉温州长蒴苣苔〉大花旋蒴苣苔.表明4种苦苣苔科植物中,牛耳朵同时具有较高的光利用能力和光适应能力,是引种开发的优选品种.  相似文献   

8.
《贵州科学》2021,39(3)
贵州地处中国西南,苦苣苔科植物资源丰富,近年来有若干个新种在贵州被发现,并被合格发表。为了让研究贵州省植物的高校、研究单位的师生和科研人员更好的了解、认知这些新分类群,现逐步将这些新类群的形态描述翻译成中文,并辅以引自原文的配图。本篇收录了白云岩蛛毛苣苔Paraboea dolomiticaZ.Y.Li, X.G.XiangZ.Y.Guo、赤水石山苣苔Petrocodon chishuiensisZ.B.Xin, F.WenS.B.Zhou以及卵瓣马铃苣苔Oreocharis ovatilobata Q.FuY.Q.Wang、小黄花石山苣苔Petrocodon luteoflorus Lei CaiF.Wen。  相似文献   

9.
贵州地处中国西南,苦苣苔科植物资源丰富,近年来有若干个新种产自贵州。为了方便贵州植物学老师、学生知道、认识这些新种,现将其形态描述翻译成中文,并配有图片。本篇收录了Oreocharis brachypodus J.M.LiZ.M.Li短柄马铃苣苔(暂定)、Petrocodon lancifolius Fang WenY.G.Wei披针叶石山苣苔(暂定)、Petrocodon retroflexus Q.ZhangJ.Guo反瓣石山苣苔(暂定)、Petrocosmea viridis M.Q.HanYan Liu青翠石蝴蝶。  相似文献   

10.
在我国第一批公布的《国家重点保护野生植物名录》中,苦苣苔科引人注目。该科有4种一级保护植物,即:单座苣苔(Metabriggsiaovalifolia)、瑶山苣苔(Dayaoshaniacotinifolia),辐花苣苔(Thamnocharisesquiroli)和报春苣苔(Primulinatabucum);还有1种二级保护物种,即  相似文献   

11.
杨丽华 《广西科学》2019,26(1):83-85
本研究报道了广东苦苣苔科(Gesneriaceae)4个新记录种:遂川报春苣苔Primulina suichuanensis X. L.YuJ. J. Zhou、假烟叶报春苣苔P. pseudoheterotricha (T.J. Zhou,B. PanW.B. Xu) Mich. M?llerA. Weber、黄花牛耳朵P. lutea (Yan LiuY.G. Wei) Mich. M?llerA. Weber、龙南后蕊苣苔Oreocharis burttii (W.T.Wang) Mich.M?llerA.Weber。  相似文献   

12.
无肋树平藓(Homaliodendron pulchrum L.Y.PeiY.Jia)是2011年报道的新种,先前记载于中国四川、湖南和广西.发现了该种在中国贵州的新记录,并详细描述了采自贵州茂兰国家自然保护区该种的形态特征,绘制了墨线图,编制了贵州省境内树平藓属的分种检索表.  相似文献   

13.
以河池石山苣苔Petrocodon hechiensis (Y.G.Wei,Yan LiuF.Wen) Y.G.WeiMich.M?ller、靖西石山苣苔Pet. jingxiensis (Yan Liu,H.S.GaoW.B.Xu) A.WeberMich.M?ller这2种石山苣苔属植物的叶片为试验材料,在不同基质上进行扦插繁育,并对3种基质组合的扦插效果进行对比分析,比较各扦插基质的优劣,筛选高效的扦插繁育方法。结果表明,在喷施0.2%多菌灵并对插穗经100 mg/L IAA溶液浸泡1 h后,采用水苔作为扦插基质时,2种石山苣苔属植物扦插生根情况较好,生根率也最高(河池石山苣苔为59%,靖西石山苣苔为62%),但出芽阶段会由于营养不良导致部分插穗出现死亡的现象;而采用水苔+蛭石+珍珠岩+泥炭土(体积比0.5∶1∶1∶1)为基质时,插穗成苗率较高(河池石山苣苔为50%,靖西石山苣苔为60%)。可见,河池石山苣苔与靖西石山苣苔的叶插繁殖可以将水苔作为生根基质,待插穗出芽后,以水苔+蛭石+珍珠岩+泥炭土(体积比0.5∶1∶1∶1)作为移栽基质,可获得较好的成苗效果。  相似文献   

14.
Two types of granitoids, highly deformed eugen grenitoids end undeformed fine-grained grenitoids, ere widely distributed in Gangou area, Central Tianshen Mountains, Northwest China. The augen grenitoids are high-K calc-alkaline characterized by high K20, Rb, Y and Th, and low Sr and Sr/Y. They also have high contents of large ion lithophile elements (LILE), such as Be, Rb, K and Th, and relatively low contents of high field strength elements (HFSE), such as Zr, Y and Nb. The fine-grained granitoids are calc-alkaline cherecterlzed by high Sr, low Y and HREE, similar to adakitic rocks, and with Na20/K20〈2 (1.76-1.91), high/sr (0.70689--0.70981), and negative εNd(t) (-2.4-5.3). High-precision SHRIMP U-Pb zircon dating results indicate that the Gangou augen greniUods were formed at 428 ± 10 Me, and the fine-grained granitoids were emplaced at 361 -368 Me. These geochemical and U-Pb zircon data have significant implications for the timing of closure of the Mishigou-Gangou Ocean and the evolution of the Central Tianshan orogenic belt.  相似文献   

15.
Emplacement ages of lamproites that comprise lamproite and olivine lamproite in Zhenyuan County, Guizhou Province, China, have been constrained by the whole-rock Sm-Nd and Rb-Sr isochron methods and the whole rock K-Ar method. Intrusive activities of lamproites in the Sinantang area of Zhenyuan County, Guizhou Province, took place during the Late Cambrian, as indicated by the Sm-Nd isochron ages ( t ) = (503 ± 17) (2σ) Ma and by the Rb-Sr isochron ages ( t ) = (501.2 ± 4.6) (2σ) Ma. Intrusive activities of olivine lamproites at the Maping with Ⅱ-type diamond and Xitou in Zhenyuan County, Guizhou Province, took place from the Late Cambrian to the Early Ordovician, as evidenced by the Sm-Nd isochron ages ( t ) = (502 ± 27) (2σ) Ma and by the Rb-Sr isochron age ( t ) = (502 ± 27) (2σ) Ma. This suggests that the upwelling hot materials derived from the deep mantle were emplaced from the Late Cambrian to the Early Ordovician (503-497 Ma), while the time terminal of cooling of the geothermal event of magmatism-tectonism probably was at 442.64-435.54 Ma, as dated by the whole rock K-Ar method.  相似文献   

16.
Preserving many kinds of rice resources and rich variations, Guizhou Province is one of the districts with the highest genetic diversity of cultivated rice (Oryza sativa L.) in China. In the current research, genetic diversity and structure of 537 accessions of cultivated rice from Guizhou were studied using 36 microsetellite markers and 39 phenotypic characters. The results showed that the model-based genetic structure was the same as genetic-distance-based one using SSRs but somewhat different from the documented classification (mainly based on phenotype) of two subspecies. The accessions being classified into indica by phenotype but japonica by genetic structure were much more than that being classified into japonica by phenotype but indica by genetic structure. Like Ding Ying's taxonomic system of cultivated rice, the subspecific differentiation was the most distinct differentiation within cultivated rice. But the differentiation within indica or japonica population was different: japonica presented clearer differentiation between soil-watery ecotypes than indica, and indica presented clearer differentiation between seasonal ecotypes than japonica. Cultivated rices in Guizhou revealed high genetic diversity at both DNA and phenotypic levels. Possessing the highest genetic diversity and all the necessary conditions as a center of genetic diversity, region Southwestern of Guizhou was suggested as the center of genetic diversity of O. sativa L. from Guizhou.  相似文献   

17.
Suppose that P=(p\-1, p\-2, ..., p\-M)\% is a probability vector with p\-i>0 and Y={1, 2, ..., M}. Let (Y, 2\+Y, μ) be a probability space with μ(i)=p\-i, i=1, 2, ..., M, and (∑\-M, B, m)= Π \+∞\-0(Y, 2\+U, μ). It is shown that for any a \%(0≤a ≤1) \%, there exists a set U∈B such that m(U)=a and the Julia set associated with U is equal to the Julia set associated with ∑\-M\%. Moreover repelling fixed points with respect to U are dense in the Julia set associated with U.  相似文献   

18.
LetX be a complex quasi-Banach space and Φ:[0,∞)→[0,∞) an increasing convex function with Φ(0)=0, and Φ∈Δ2. ThenL Φ * (X) is a quasi-Banach space with continuous quasi-norm andL Φ * (X) has the ARNP if and only ifX does. Supported by the National Natural Science Foundation of China Liu Peide: born in 1943, Professor  相似文献   

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