春小麦新品种高原314及其栽培技术

高原314是中国科学院西北高原生物研究所农业中心通过有性杂交培育的春小麦新品种，2001年12月通过青海省农作物品种审定委员会审定，品种原代号为95-314，现定名为高原314，属小麦Var. graecum Korn的变种。品种组合为：高原602 * {[ST142 * [(82宁182 * 82原11) * 47-2]] * [(78-17-3 * 83-228-3) * (Chanal * 338)]}F_3。

南亚和东南亚龙胆属(龙胆科)的新名称、新组合及分类注释(英文)

本文提出了龙胆属两个种的新名称 (GentianamembranuliferaT .N .Ho,G .nudicaulis Kurz var.as samensisT .N .Ho )和 5个变种的新组合 [(Gentianalateriflora Hemsl.var.uncifolia (H.J.Lam)T.N.Ho,G.sumatranaRidl.var.humifusa (S .Moore)T .N .Ho ,G .quadrifariaBl.var.wightii(Kusnez.)T .N .Ho,G .loerzingiiRidl.var.timida (Kerr)T .N .Ho ,G .membranuliferaT .N .Hovar.recurvata (Kusnez.)T .N .Ho) ]。

青海南部七种翠雀属植物的核型

报道了采自青海南部７ 种翠雀属（Delphiniun L.） 植物的染色体数目和核型。大通翠雀花D.pylzowii 的核型公式为２ｎ＝ １６ ＝ ２ｍ ＋ ４ｓｍ ＋ １０st； 毛翠雀花D.trichophorum的核型公式为２ｎ＝ １６ ＝ ２ｍ ＋ ４ｓｍ ＋ １０st； 蓝白翠雀花D.albocoerelum 的核型公式为２ｎ ＝ １６ ＝ ２ｍ ＋ ４ｓｍ（２ＳＡＴ） ＋ １０st； 囊谦翠雀花D.nangchienense的核型公式为２ｎ ＝ １６ ＝ ２ｍ ＋ ６ｓｍ ＋ ８ｓｔ； 唐古拉翠雀花D.tangkulaense 的核型公式为2ｎ＝１６＝２ｍ（２ＳＡＴ）＋６ｓｍ＋８ｓｔ；单花翠雀花D.candelabrum var.monanthum 的核型2n=16=2m+6sm+8st;展毛翠雀花D.kamaoense var.glabrescens的核型公式为2n=16=2m+6sm+8st；前5种植物的染色体数目和核型为首次报道。

青藏高原毛茛科3种特有植物核型和进化研究

对青藏高原高山冰缘地区毛茛科3 种特有植物的核型进行了分析。它们的核型公式(K)、染色体相对长度组成(C. R. L. ) 和核型不对称系数(A s. K% ) 分别为: 青藏金莲花 T rollius pumilus var. tangu ticus: K (2n) = 6m + 8sm (2SA T ) + 2st, C. R. L. = 4L + 4M 2+ 4M 1+ 4S,A s. K% = 63. 57, 核型属2B型; 甘青乌头A conitum tanguticum 为K (2n) = 6m + 10sm ,C. R. L. = 4L + 8M 1+ 4S,A s. K% = 62. 54, 2B 型; 单花翠雀花Delphinium candelabrum var.monanthum 为K (2n) = 6m + 8sm + 2st, C. R. L. = 4L + 4M 2+ 4M 1+ 6S,A s. K% = 64. 34, 属3B 型。经同相关近缘种核型资料比较, 青藏金莲花核型不对称性和进化程度比金莲花T.ch inensis 低; 甘青乌头的核型不对称性和进化程度在其近缘类群(乌头组Sect. Aconitum ) 已报道的种之内最低; 单花翠雀花核型不对称性和进化水平比翠雀组(Sect. Delphinastrum ) 已报道的展毛翠雀花D. kamaoense var. glabrescens、多枝翠雀花D. maxim owiczii 和蓝翠雀花D. caeruleum 都低。这与该3 种植物在王文采先生(1979) 中国毛茛分类系统中的位置是一致的。

赖草属资料

禾本科赖草属二新种及一新变种,即芒颖赖草Leymus aristiglumus L . B .Cai ,伊吾赖草Leymus yiwuensis L. B. Cai ex N. R. Cui 和疏节赖草Leymus secalinus var. laxinodis L . B . Cai 。

鹅观草属的几个新组合

本文报道了禾本科鹅观草属的三个种级新组合和四个变种级新组合。即大丛鹅观草Roegneria magnicaespis (D. F. Cui) L. B. Cai ; 新疆鹅观草Roegneria si nkiangensis (D. F. Cui) L. B. Cai ; 阿尔泰鹅观草Roegneria al taica(D. F. Cui) L. B. Cai ; 短芒鹅观草Roegneria glaberrima var. breviarista (D.F. Cui) L. B. Cai ;林缘鹅观草Roegneria mutabilis var. nemoralis (D. F. Cui)L. B. Cai ; 多花鹅观草Roegneria aboli nii var. pl urif lora (D. F. Cui) L. B. Cai 和曲芒鹅观草Roegneria tschimganica var. glabrispicula (D. F. Cui) L. B. Cai

中国以礼草属新分类群

本文报道了禾本科以礼草属二新种及二新变种，即稀穗以礼草Kengyilia laxistachya L.B.Cai et D. F. Cui，和静以礼草Kengyilia hejingensis L.B.Cai et D. F. Cui，显芒以礼草Kengyilia hirsute var. obviaristata L. B. Cai和毛鞘以礼草Kengyilia rigiadula var. trichocolea L. B. Cai.

辽宁卷耳属（石竹科）一新变种

本文发表了卷耳属一新变种，即短果卷耳Cerastium glomeratum Thuill. Var. bbrachycarpum L. H. Zhou et Q. Zh. Han

中国西部高山8种龙胆属植物的染色体数目

本文报道了我国西部高山上的8种龙胆属植物的染色体数目。其中宽街龙胆（Gentianaampla）的染色体数目为Zn＝48，提钟龙胆（G．stipitataSubsp．timensis）的染色体数目为2n=26）小齿龙胆（G．microdonta）和四数龙胆（G．lineolata）的染色体数目为2n=24，南山龙胆（G．grumil）的染色体数目为2n=18，上述5种植物的染色体数目为首次报道。其余蓝玉簪龙胆（G．veitchiorum）的染色体数目为2n=24，线叶龙胆（G．lawrenci Burk．var���farrei）的染色体数目为2n＝48，钻叶龙胆的染色体数目为2n＝18。

马先蒿属6个种的核型与进化研究

分析和报道了马先蒿属（Pedicularis Linn.）分布于青藏高原东北部６个特有种的核型，并根据核型及其有关参数，分析和比较了该６种马先蒿核型的不对称性和相对进化程度。６个种的体细胞染色体数目都是２ｎ＝１６。核型分别为：绵德马先蒿P.pilostachya Maxim.，核型公式Ｋ（２ｎ）＝１６＝４ｍ＋１２ｓｍ，染色体相对长度组成２Ｌ＋６Ｍ２＋６Ｍ１＋２Ｓ，核型不对称系数Ａｓ·Ｋ＝６５．２９％，属于２Ａ型；青海马先蒿P.przewalskii Maxim.，Ｋ（２ｎ）＝１６＝８ｍ（ＳＡＴ）＋４ｓｍ＋２ｓ＋２ｔ，２Ｌ＋８Ｍ２＋２Ｍ１＋４Ｓ，Ａｓ·Ｋ＝６５．０２％，２Ｂ型；华马先蒿P.oederi Vahl.var.sinensis(Maxim.)Hurus.，K(2n)=16=12m+4sm，2L+4M2+8M1+2 S，As·K=59.89%，2B型；粗野马先蒿P.rudis Maxim.，K(2n)=16=4m+10sm+2st，4L+4M2+4M1+2 S，As·K=68.10%，2B型；甘肃马先蒿P.kansuensis Maxim. Subsp. kansuensis，K(2n)=16=6m+6sm+2st+2t，2L+6M2+6M1+2 S，As·K=68.92%，2A型；藓生马先蒿P.muscicola Maxim. K(2n)=16=8m(SAT)+8sm，2L=8M2+4M1+2S，As·K=62.64%，2B型。根据这6个种的核型和已有资料，认为该属的染色体基数x=8，极少数种有多倍体。通过对以上6种核型及进化程度的比较，该属核型变异较大，以中部着丝粒染色体为组成基础（较原始的种类，如华马先蒿和绵穗马先蒿），端部或近端部着丝粒染色体存在与否与该属内种的进化程度有关。核型不对称性所表示的进化程度似乎与花冠的演化有联系。

Notes on grasses (Poaceae) for the Flora of China, VI. New combinations in Stipeae and Anthoxantham

When Oryzopsis is confined to the type species, Chinese species are placed in Achnatherum and Piptatherum. This necessitates the following new combinations: Piptatherum grandispiculum, Piptatherum aequiglume var. ligulatum, Piptatherum tibeticum var. psilolepis.. Piptatherum. munroi var. parviflorum, Achnatherum henryi. and Achnatherum henryi var. acutum. Achnatherum henryi is lectotypified. The new name Piptatherum kuoi replaces the illegitimate name Piptatherum obtusum, and this species is lectotypified. Hierochloe potaninii is transferred to Anthoxanthum as A. potaninii, as Hierochloe is regarded as a synonym of Anthoxanthum. All the grass taxa (Poaceae) listed are endemic to China.

New taxa, names, and combinations in Saxifraga (Saxifragaceae) for the Flora of China

The following new species, new variety, new name, and four new combinations are published for the forthcoming account of Saxifraga L. in the Flora of China, Volume 8: S. epiphylla Gornall & H. Ohba, sp. nov., S. gemmigera Engler var. gemmuligera (Engler) J. T. Pan & Gornall, comb. nov., S. heterotricha Marquand & Airy-Shaw var. anadena (H. Smith) J. T. Pan & Gornall, comb. et stat, nov., S. hypericoides Franchet var. aurantiascens (Engler & Irmscher) J. T. Pan & Gornall, comb. nov., S. hypericoides var. rockii (Mattfeld) J. T. Pan & Gornall, comb. et stat. nov., S. sinomontana J. T. Pan & Gornall, nom. nov., and S. sinomontana var. amabilis H. Smith ex J. T. Pan, var. nov. In addition, the names S. mengtzeana Engler & Irmscher and S. mengtzeana var. cordatifolia Engler & Irmscher are lectotypified here.

中国南方热带地区田洋玛珥湖24万年以来的气候变化及湖泊演变

A continuous long (224m) and high-resolution core TY2 was recovered from paleo-maar-lake Tianyang, tropical South China. Based on the diatom records of the upper 130-m core, this paper focuses on exploring climate change and the lake evolution history in tropical South China during the past 240ka. The most typical and unique characteristics of the diatom assemblages is that, Aulacoseira granulata was dominant or absolutely dominant species (80-90%) during most parts of the 130-m core, while Cyclotella stelligera var. tenuis and Fragilaria construens var. venter were subdominant species in only limited parts of the lower and upper core, respectively. Time scale is always the biggest problem for the study of TY2 core, so although diatom is seldom used for establishing time scale, here we attempt this by correlating the diatom-reconstructed temperature sequence with the time scale of ODP core 806B from Equatorial Western Pacific. Verified by the few most reliable ages from TY2 core and the parallel core TYl, a rather reasonable and reliable time scale was established. 01S 7/6 falls at the depth of 100m (ca. 194kaBP), OIS 6/5 at 75m (ca. 132kaBP), OIS 5/4 at 46m (ca. 75kaBP), OIS 4-3 at 35m (ca. 60kaBP). Qualitative and quantitative environmental reconstructions are made on the basis of diatom assemblage ecotype and EDDI dataset. Correlation of diatom-reconstructed temperature and moisture changes of Core TY2 with pollen-reconstructed temperature and rainfall sequence of Core TYl proves that the results are quite consistent in most periods. Thus the reconstruction results from diatom are quite reliable, and probably have a much higher resolution than pollen results. Combined with lithological and magnetic susceptibility variations, the diatom analysis reveals that, the general climate in tropical South China during the past 240ka was warm and wet. On the time scale of glacial-interglacial, warm and wet, cool and dry are not always synchronous. It was relatively warm-wet during the penultimate interglacial, cool-dry during the penultimate glacial, warm-dry during the last interglacial, and cooler-drier during the last glacial. In contrast, on the time scale of subglacial-subinterglacial scales, warm and dry, cool and wet corresponds very obviously, showing very clear 21-23 ka precession cycle. Analysis also shows that, the water of Tianyang paleo-maar-lake was generally warm, turbulent, turbid, meso-trophic, slightly alkaline, low conductivity and fresh during the past 240 kaBP, with small variations in some parts. Tianyang paleolake experienced shallow to semi-deep lake in OIS7d, open shallow lake in OIS7c-OIS5b, shallow coastal lake in OIS5a-OIS4c, swamp in OIS4b, and then completely dried up in OIS3c. The lake evolution was mainly controlled by temperature and precipitation changes in tropical China. While temperature and precipitation changes were probably controlled by the migrations of monsoon rainband and the evaporation rate, which was in turn controlled by the evolution of East Asian monsoon. Therefore, when the summer monsoon was strongest the climate was warm-dry, when stronger the climate was warm-wet; when the winter monsoon was strongest the climate was cool-dry, stronger cool-wet. This mechanism caused the warm-dry sub interglacial and cool-wet subglacial climate in the tropical South China.

喀斯特峡谷区常见植物叶片δ^13C值与环境因子的关系研究

通过对贵州花江峡谷喀斯特石漠化区4种典型石漠化植物群落中11种常见植物种叶片的δ^13C值测定,研究了各植物种对影响植物碳同位素分馏的主要环境因子（土壤储水量、大气相对湿度、光照强度、土壤厚度）的响应,分析了石漠化梯度中不同土层土壤储水量、大气相对湿度、土壤有机质、年均气温、光照强度等环境因子梯度变化与植物叶片δ^13C值的关系。结果表明,大部分物种的δ^13C值对环境因子的变化趋势表现为随环境水分好转呈下降趋势,即水分利用效率下降；也有部分物种呈稳定不变或逆势上升趋势。相关性分析表明,清香木（Pistacia weinmannifolia）、石岩枫（Mallotus repandus）、红背山麻杆（Alchornea trewioides）的主导因子是土层储水量；肾蕨（Nephrolepis cordifolia）、野桐（Mallotus japonicus var���floccosus）的主导因子是土壤厚度；肾蕨、八角枫（Alangium chinense）、构树（Broussonetia papyrifera）的主导因子是光照强度；而广西密花树（Rapanea kwangsiensis）、圆叶乌桕（Sapium rot undifolium）和灰毛浆果楝（Cipadessa cinerascens）则分辨不出主导因子,即环境影响因素更为综合。总体而言,叶片高δ^13C值是对低水分、高光、低资源环境的适应.

喀斯特山区先锋植物叶片解剖特征及其生态适应性评价——以贵州花江峡谷区为例

通过研究贵州西南部典型喀斯特植被退化区花江峡谷植被现状，选取具一定经济价值和推广价值的先锋植物，采用生物显微制片技术与数理统计方法相结合，报导了6科10种分属不同生活型的植物叶片的解剖结构特征，并进行了比较和解剖因子分析。结果表明研究区喀斯特先锋植物叶片在不同种类之间具有明显差异，这些差异除受遗传因子控制外，环境因子(主要为光照和水分)也有重要作用；生活型不同对先锋植物叶片特征有一定影响，但未表现出规律性。根据叶片适应特征的差异，10种先锋植物可分为3种类型，即旱生或阳生叶类型的构树(Broussonetia papyrifera)、火棘(pyracantha fortuneana)、刺槐(Robinia pseudoacacia)、白三叶(Trifolium repens)；偏中生叶类型(香椿的Toona sirensis)、顶坛花椒(Zanthaxylum pinum var���dingtanensis)、黔滇木蓝(In-digofera esquirolii)、忍冬(Lomicera japonica)、紫云英(Astragalus sinicus)；偏阴生叶类型的繁缕(Stellaria media)。