南岭栲叶多酚类化学成分的分离与鉴定

采用Sephadex LH-20、MCI gel CHP 20P和Toyopearl Butyl-650C等柱色谱及半制备液相色谱技术,从壳斗科(Fagaceae)锥属(Castanopsis)植物南岭栲(Castanopsis fordii Hance)叶子乙醇提取物中分离得到18个多酚类化合物,运用波谱学方法解析鉴定为:没食子酸(1)、没食子酸甲酯(2)、没食子酸乙酯(3)、莽草酸-3-O-没食子酸酯(4)、3,3'-二甲基鞣花酸(5)、3,3'-二甲氧基鞣花酸-4'-O-α-D-吡喃木糖苷(6)、3-甲氧基-4'-鼠李糖鞣花酸(7)、6-O-没食子酰基熊果苷(8)、龙胆酸5-O-β-D-(6'-O-没食子酰基)-吡喃葡萄糖(9)、4-hydroxy-3-methoxyphenol 1-O-β-D-(6'-O-galloyl)glucoside(10)、1,6-二-O-没食子酰基-β-D-葡萄糖苷(11)、gallic acid 3-O-β-D-(6'-Ogalloyl)-glucopyranoside(12)、benzyl 6-O-galloyl-β-D-glucopyranoside(13)、2,3-di-O-galloyl-D-glucose(14)、gemin D(15)、特里马素(16)、丁香素(17)、viburnolide A(18)。所有化合物均为首次从该植物中分离得到。     

秋枫化学成分的研究

利用各种色谱技术从秋枫(Bischofia javanica)的根中分离得到11个化合物。通过波谱学方法鉴定为3,4-二羟基苯乙醇(1),2-(3,4-dihydroxy)-phenylethyl-O-β-D-glucopyranoside(2),tachioside(3),isotachioside(4),儿茶素(5),表儿茶素(6),没食子儿茶素(7),4-羟基-2-甲氧基苯酚1-O-β-D-(6’-O-没食子酰基)葡萄糖苷(8),4-hydroxy-3-methoxyphenol-β-D-[6-O-(4-hydroxy-3,5-dimethoxylbenzoate)]glucopyranoside(9),maesopsin-6-O-glucopyranoside(10),β-香树脂醇乙酸酯(11)。所有化合物均为首次从该种植物中分离得到。     

刺桑皮正丁醇部位化学成分研究

为研究刺桑(Taxotrophis ilicifolia)皮正丁醇部位的化学成分，该研究采用硅胶、ODS、Sephadex LH-20、反相半制备高效液相等色谱法对刺桑皮正丁醇萃取部位进行分离纯化，并综合理化性质及波谱数据鉴定其化合物的结构。结果表明：从刺桑皮正丁醇萃取物中分离得到16个化合物，分别鉴定为icariside E5 (1)、裂环异落叶松脂醇-9-O-β-吡喃葡萄糖苷(2)、2,4,6-三甲氧基苯酚-1-O-β-D-葡萄糖苷(3)、9-O-β-glucopyranosyl trans-cinnamyl alcohol (4)、3,4,5-三甲氧基苯酚-1-O-β-呋喃芹糖基-(1″→6′)-β-吡喃葡萄糖苷(5)、3-羟基-4,5-二甲氧基苯酚-β-D-吡喃葡萄糖苷(6)、2,6-二甲氧基-4-羟基苯酚-1-O-β-D-吡喃葡萄糖苷(7)、isotachioside (8)、ficuscarpanoside A (9)、uridine (10)、methyl syringate 4-O-β-D-glucopyranoside (11)、3,4,5-三甲氧基苯酚-β-D-吡喃...     

珍珠菜的化学成分研究(英文)

从珍珠菜(Lysimachia clethroides)根部分离得到8个化合物,通过波谱数据结合理化性质分别鉴定为山奈素-3-O-β-D-吡喃葡萄糖苷(1),山奈素-3-O-β-D-(2-O-β-D-吡喃葡萄糖)吡喃葡萄糖苷(2),(+)-儿茶素(3),(-)-表儿茶素(4),(+)-没食子儿茶素(5),(-)-表没食子儿茶素(6),(E)-2,3,5,4′-tetrahydroxystilbene-2-O-β-D-glucopyranoside(7)和2,3,5,4′-tetrahydroxystilbene-3-O-β-D-glucopyranoside(8)。所有化合物均为首次从该植物中分离得到。     

鸡血藤中的酚酸类化合物

为了解鸡血藤(Spatholobus suberectus Dunn)的化学成分,从鸡血藤的95%乙醇提取物中分离出15个酚酸类单体成分,经波谱学分析分别鉴定为:没食子酸(1)、tachioside(2)、isotachioside(3)、canthoside D(4)、3,5-二甲氧基-4-羟基苯基-1-O-β-D-吡喃葡萄糖苷(5)、2,6-二甲氧基-4-羟基-苯酚-1-O-β-D-吡喃葡萄糖苷(6)、4-羟甲基-2,6-二甲氧基苯基-β-D-吡喃葡萄糖苷(7)、丁香酸葡萄糖苷(8)、3-甲氧基苯乙醇-4-O-β-D-葡吡喃糖苷(9)、2-(4-hydroxy-3,5-dimethoxyphenyl)ethyl-β-D-glucopyranoside(10)、4,6-二羟基-2-O-(β-D-吡喃葡萄糖苷)苯乙酮(11)、松香(12)、顺式紫丁香苷(13)、(–)-(7R,8S)-guaiacylglycerol 8-O-β-Dglucopyranoside(14)和l-threo-guaiacylglycerol-8-O-β-glucopyranoside(15)。其中,化合物2~8和10~15为首次从密花豆属植物中分离得到。     

朝鲜蓟叶中的酚性糖苷化合物

从朝鲜蓟（Cynara scolymus）叶中分离得到2个酚性糖苷化合物,其中一个是新化合物,通过波谱学方法确定其结构为2-甲氧基-4-（2,3-二羟基-丙酰基）-苯基-1—O-（6′-O-没食子酰基）-β-D-吡喃葡萄糖苷（1）。     

紫娟茶化学成分及其抗炎抗氧化活性研究

本文对紫娟茶的化学成分进行分离纯化及其抗炎、抗氧化活性进行考察。实验采用现代分离纯化方法,从紫娟茶中共分离得到12个化合物,根据波谱学数据进行结构鉴定为:山柰酚(1)、(+)-表儿茶素(2)、(-)-表儿茶素-3-O-没食子酸酯(3)、杨梅素(4)、表没食子儿茶素-3-O-(3″-O-甲基)没食子酸酯(5)、槲皮素(6)、没食子酸(7)、表没食子儿茶素没食子酸酯(8)、3-O-没食子酰基奎宁(9)、小木麻黄素(10)、1,4,6-三-O-没食子酰基-β-D-葡萄糖(11)、咖啡因(12),其中化合物9为首次从紫娟茶中分离得到。化合物11表现出良好的抗氧化活性,化合物1、3、4、6、8～11均具有显著的抗炎活性。     

中华山蓼化学成分研究

bk中华山蓼(Dxyria sinensis Hemsl.)全草中首次分离得到十四个化合物,通过波谱学方法分别鉴定为(-)-表没食子儿茶素(1)、(-)-儿茶素没食子酸酯(2)、(-)-表儿茶素(3)、(-)-表儿茶素-3-没食子酸酯(4)、槲皮素-3-O-α-L-鼠李糖苷(5)、tiliroside(6)、山萘酚-3-O-β-D-吡喃葡萄糖苷(7)、桷皮素(8)、2,4-二羟基-6-甲氧基-乙酰基苯-4-O-β-D-吡喃葡萄糖苷(9)、反-N-(4-羟基苯乙基)阿魏酸酰胺(10)、顺-N-(4-羟基苯乙基)阿魏酸酰胺(11)、icariol A2(12)、(+)-松脂素(13)、Helonioside B(14).     

玫瑰红景天化学成分研究

采用大孔吸附树脂、硅胶柱、ADS-5C反相柱和制备HPLC色谱技术对新疆产玫瑰红景天根茎中的植物化学成分进行提取分离和纯化研究,从中分离得到15个化合物。通过理化方法及1H、13C NMR等方法鉴定为:对-O-β-吡喃葡萄糖基-苯-2-丁酮(1)、6’-O-没食子酰-红景天苷(2)、对-O-β-吡喃葡萄糖基-苯丙烯酸(3)、7-甲氧基香豆素(4)、表没食子儿茶素-3-没食子酸酯(5)、苯乙基-6-O-β-葡萄糖苷(6)、对羟基苯甲酸(7)、红景天苷(8)、肉桂醇-6’-O-α-吡喃阿拉伯糖基-O-β-吡喃葡萄弹苷(9)、肉桂醇-6’-O-α-吡喃木糖-O-β-吡喃葡萄弹苷(10)、肉桂醇-6’-O-α-呋喃阿拉伯糖基-O-β-吡喃葡萄弹苷(11)、肉桂醇-O-β-D-吡喃葡萄弹苷(12)、对-羟基-苯乙醇(13)、3,7-二甲基-2,6-二烯-1,4-二辛醇(14)、3,7-二甲基-2,6-二烯-1,4-二辛醇-O-β-吡喃葡萄糖苷(15)。其中化合物1～4为首次在玫瑰红景天发现。     

黄刺玫果实化学成分及其体外延长凝血酶原时间研究

对黄刺玫(Rosa xanthina Lindl)果实的化学成分及其体外延长凝血酶原时间(PT)进行研究。采用硅胶、Sephadex LH-20、MDS柱色谱以及半制备高效液相色谱等方法进行分离纯化,并运用NMR、MS等波谱方法对所分离的化合物进行结构鉴定。结果从黄刺玫果实75%乙醇提取物中分离鉴定6个化合物,分别为槲皮素-3-O-α-L-鼠李吡喃糖苷(1)、槲皮素-3-O-(6″-O-反式香豆酰基)-β-D-葡萄糖苷(2)、山奈酚-4'-O-β-D-吡喃葡萄糖苷(3)、槲皮素-4'-O-β-D-吡喃葡萄糖苷(4)、1,2-二(4-羟基-3-甲氧基苯基)-1,3-丙二醇(5)、2,3-二羟基-1-(3-羟基-4-甲氧基苯基)-1-丙酮(6)。其中化合物6是首次从本属植物中分离得到,化合物1~5为首次从黄刺玫中分离得到。体外血浆PT测定结果表明,化合物1~4与空白对照相比(P0.05)均显示具有延长凝血酶原时间作用,进一步对化合物1的延长凝血酶原时间(PT)进行量效关系研究,结果显示在浓度不小于27 m M时,化合物1显示明显延长凝血酶原时间作用。     

32种杜鹃花属植物在迁地保育条件下的自交研究

迁地保育条件下的杜鹃花属植物自交可育性一直缺乏系统的比较研究,该文对5亚属13亚组32种杜鹃花属植物的自交进行了数据采集与分析,初步揭示了迁地保育条件下杜鹃花属植物自交育性特征。结果表明:(1)自交可育与不育是杜鹃花属植物有性生殖中的两个并存现象,自交能育型种类或多于不育型。在受试的32种杜鹃花中,自交不育型10种、弱可育型5种、可育型7种、高可育型10种,其中27种的自交育性为首次报道,涵盖包括杜鹃亚属杜鹃组(sect.Rhododendron)和马银花亚属(subgen.Azaleastrum)及常绿杜鹃亚属(subgen.Hymenanthes)中银叶杜鹃亚组(subsect.Argyrophylla)等5个亚组在内的未被研究的类群。(2)通过与自然授粉有关育性指标的比较,发现不同种类的自交可育性指标有大幅度降低及增高这两类截然不同的现象,从而提出了自交可能是部分杜鹃花属植物的适应策略,或者对不利环境及其媒介条件的主动响应。(3)在云锦杜鹃亚组(subsect.Fortunea)这个被认为最原始的杜鹃花类群中,具备从自交不育到高可育的所有类型,并可能由此奠定整个杜鹃花属的遗传基础,而类群与种类分布的不同区域气候环境长期直接的或通过影响传粉媒介间接的作用,则可能是最终塑造该属植物自交育性多样化的外部动力。(4)该文还依据有关自交的研究结果,对杜鹃花属植物的迁地保育、育种、相关学科发展进行了讨论,并认为后合子期败育的理论不能完美地解释自交不能坐果的现象,而多倍体似不会导致自交不育。     

Astragalar morphology of late Eocene anthropoids from the Fayum Depression (Egypt) and the origin of catarrhine primates

The phylogenetic relationships of the late Eocene anthropoids Catopithecus browni and Proteopithecus sylviae are currently a matter of debate, with opinion divided as to whether these taxa are stem or crown anthropoids. The phylogenetic position of Catopithecus is of particular interest, for, unlike the highly generalized genus Proteopithecus, this taxon shares apomorphic dental and postcranial features with more derived undoubted catarrhines that appear in the same region 1-2 Ma later. If these apomorphies are homologous and Catopithecus is a stem catarrhine, the unique combination of plesiomorphic and apomorphic features preserved in this anthropoid would have important implications for our understanding of the crown anthropoid morphotype and the pattern of morphological character transformations that occurred during the early phases of stem catarrhine evolution.Well-preserved astragali referrable to Proteopithecus, Catopithecus, and the undoubted early Oligocene stem catarrhine Aegyptopithecus have provided additional morphological evidence that allows us to further evaluate competing hypotheses of interrelationships among Eocene-Oligocene Afro-Arabian anthropoids. Qualitative observations and multivariate morphometric analyses reveal that the astragalar morphology of Proteopithecus is very similar to that of early Oligocene parapithecids and living and extinct small-bodied platyrrhines, and strengthens the hypothesis that the morphological pattern shared by these taxa is primitive within crown Anthropoidea. In contrast, Catopithecus departs markedly from the predicted crown anthropoid astragalar morphotype and shares a number of apomorphic features (e.g., deep cotylar fossa, laterally projecting fibular facet, trochlear asymmetry, mediolaterally wide astragalar head) with Aegyptopithecus and Miocene-Recent catarrhines. The evidence from the astragalus complements other independent data from the dentition, humerus and femur of Catopithecus that support this taxon's stem catarrhine status, and we continue to maintain that oligopithecines are stem catarrhines that constitute the sister group of a clade containing propliopithecines and Miocene-Recent catarrhines.     

Paleosols and paleoenvironments of the middle Miocene,Maboko Formation,Kenya

The middle Miocene (15 Ma) Maboko Formation of Maboko Island and Majiwa Bluffs, southwestern Kenya, has yielded abundant fossils of the earliest known cercopithecoid monkey (Victoriapithecus macinnesi), and of a kenyapithecine hominoid (Kenyapithecus africanus), as well as rare proconsuline (Simiolus leakeyorum, cf. Limnopithecus evansi) and oreopithecine apes (Mabokopithecus clarki, M. pickfordi), and galagids (Komba winamensis). Specific habitat preferences can be interpreted from large collections of primate fossils in different kinds of paleosols (pedotypes). Fossiliferous drab-colored paleosols with iron-manganese nodules (Yom pedotype) are like modern soils of seasonally waterlogged depressions (dambo). Their crumb structure and abundant fine root-traces, as well as scattered large calcareous rhizoconcretions indicate former vegetation of seasonally wet, wooded grassland. Other fossiliferous paleosols are evidence of nyika bushland (Ratong), and early-successional riparian woodland (Dhero). No fossils were found in Mogo paleosols interpreted as saline scrub soils. Very shallow calcic horizons (in Yom, Ratong, and Mogo paleosols) and Na-montmorillonite (in Mogo) are evidence of dry paleoclimate (300-500 mm MAP=mean annual precipitation). This is the driest paleoclimate and most open vegetation yet inferred as a habitat for any Kenyan Miocene apes or monkeys. Victoriapithecus was abundant in dambo wooded grassland (Yom) and riparian woodland (Dhero), a distribution like that of modern vervet monkeys. Kenyapithecus ranged through all these paleosols, but was the most common primate in nyika bushland paleosols (Ratong), comparable to baboons and macaques today. Mabokopithecus was virtually restricted to riparian woodland paleosols (Dhero), and Simiolus had a similar, but marginally wider, distribution. Habitat preferences of Mabokopithecus and Simiolus were like those of modern colobus monkeys and mangabeys. A single specimen of Komba was found in dambo wooded grassland paleosol (Yom), a habitat more like that of the living Senegal bushbaby than of rainforest galagids. A shift to non-forest habitats may explain the terrestrial adaptations of Victoriapithecus, basal to the cercopithecid radiation, and of Kenyapithecus, basal to the hominoid radiation. Both taxa are distinct from earlier Miocene arboreal proconsulines, oreopithecines and galagids.     

Stratigraphy, artefact industries and hominid associations for Sterkfontein, member 5

A revised stratigraphy for the early hominid site of Sterkfontein (Gauteng Province, South Africa) reveals a complex distribution of infills in the main excavation area between 2.8 and 1.4 m.y.a, as well as deposits dating to the mid to late Pleistocene. New research now shows that the Member 4 australopithecine breccia (2.8-2.6 Ma) extends further west than was previously thought, while a late phase of Member 4 is recognized in a southern area. The artefact-bearing breccias were defined sedimentologically as Member 5, but one supposed part of these younger breccias, the StW 53 infill, lacks in situ stone tools, although it does appear to post-date 2.6 Ma when artefacts first appear in the archaeological record. The StW 53 hominid, previously referred to Homo habilis, is here argued to be Australopithecus. The first artefact-bearing breccia of Member 5 is the Oldowan Infill, estimated at 2-1.7 Ma. It occupies a restricted distribution in Member 5 east and contains an expedient, flake-based tool industry associated with a few fossils of Paranthropos robustus. An enlarged cave opening subsequently admitted one or more Early Acheulean infills associated in Member 5 west with Homo ergaster. The artefacts attest to a larger site accumulation between ca. 1.7 and 1.4 Ma, with more intensive use of quartzite over quartz and a subtle but important shift to large flakes and heavier-duty tools. The available information on palaeoenvironments is summarized, showing an overall change from tropical to sub-tropical gallery forest, forest fringe and woodland conditions in Member 4 to more open woodland and grassland habitats in the later units, but with suggestions of a wet localized topography in the Paranthropus -bearing Oldowan Infill.     

基于分子证据确认秦岭藤属与驼峰藤属(夹竹桃科)的系统位置

秦岭藤属(Biondia Schltr.)是中国特有属,约13种,驼峰藤属(Merrillanthus Chun & Tsiang)是仅在我国与柬埔寨分布的单种属,目前两个属均被归并到白前属(Vincetoxicum Wolf),由于取样和系统发育分析尚存一些欠缺,因此其系统位置和归属尚需进一步确认。该文使用2个核糖体基因序列片段(ITS、ETS)、5个叶绿体基因序列片段(psbA-trnH、trnG、trnL、trnL-F、trnT-L),以及二者的合并数据,重建娃儿藤亚族(Tylophorinae)(包含属的模式秦岭藤 [B. chinensis Schltr.=V. shaanxiense(Schltr.)Meve & Liede]与驼峰藤 [M. hainanensis Chun & Tsiang=V. hainanense(Chun & Tsiang)Meve, H. H. Kong & Liede])的系统发育树。结果表明:秦岭藤属与驼峰藤属均包含在白前属中,秦岭藤与青龙藤 [B. henryi(Warb.)Tsiang & Li=V. henryi(Warb.)Meve & Liede]互为姐妹类群,并与V. kawaroense Meve & Liede聚为一支,而黑水藤 [B. insignis Tsiang=V. insigne(Tsiang)Meve, H. H. Kong & Liede]在另一分支中(亚热带分支Subtropical Clade); 驼峰藤属与V. cissoides(Blume)Kuntze和V. philippicum Meve, Omlor & Liede聚为一支。核糖体和叶绿体基因数据均支持秦岭藤属与驼峰藤属归并入白前属,但秦岭藤属为多系,尚需收集更多种类和数据合并分析,深入探讨归并后白前属的种间系统关系和位置。     

荨麻科三新种

该文描述了荨麻科三新种:(1)自中国重庆市发现的荨麻科荨麻属一新种,城口荨麻。此种与异株荨麻有亲缘关系,区别特征为此种的茎被少数刺毛,叶片多为心形,雄、雌花序均不分枝,瘦果在中央稍凹陷。(2)自中国广西发现的荨麻科赤车属一新种,来宾赤车。此种与特产云南东南部的富宁赤车相近缘,与后者的区别在于本种茎的毛开展或向上弯曲,叶片长椭圆形,基部斜楔形,雌花具3~4枚花被片,其中1~2枚较大花被片在背面顶端具一长筒状突起。(3)自缅甸北部发现的荨麻科楼梯草属一新种,克钦楼梯草。此种在体态上与骤尖楼梯草甚为相似,与后者的区别在于本种的每一茎节具正常叶和一退化叶,托叶狭披针状条形和无脉,雌总苞苞片无角状突起,雌小苞片较大,呈楔状长圆形,雌花具一小花被片,以及雌蕊具一宽倒卵球形柱头。     

中国西藏兰科植物新资料

中国西藏东南地区位于东喜马拉雅和印缅的交接处,是全球生物多样性的热点地区,尤其是位于该地区的墨脱,由于巨大的海拔高差,使该地区的植被类型呈显著的垂直地带性,且植物种类繁多、植被结构复杂。该文报道了西藏野生兰科植物新记录属3个,即线柱兰属(Zeuxine)、爬兰属(Herpysma)和槽舌兰属(Holcoglossum);新记录种27个,即白肋线柱兰(Zeuxine goodyeroides)、爬兰(Herpysma longicaulis)、小花槽舌兰(Holcoglossum himalaicum)、西南齿唇兰(Anoectochilus elwesii)、窄唇蜘蛛兰(Arachnis labrosa)、短足石豆兰(Bulbophyllum stenobulbon)、尖角卷瓣兰(B. forrestii)、南方虾脊兰(Calanthe lyroglossa)、泰国牛角兰(Ceratostylis siamensis)、金唇兰(Chrysoglossum ornatum)、格力贝母兰(Coelogyne griffithii)、云南贝母兰(C. assamica)、斑舌兰(Cymbidium tigrinum)、梳唇石斛(Dendrobium strongylanthum)、狭叶金石斛((D. angustifolium)、厚唇兰(D. mariae)、粗茎苹兰(Pinalia amica)、垂叶斑叶兰(Goodyera pendula)、绿花斑叶兰(G. viridiflora)、狭叶羊耳蒜(Liparis perpusilla)、小花羊耳蒜(L. platyrachis)、三裂羊耳蒜(L. mannii)、镰叶鸢尾兰(Oberonia falcata)、阔瓣鸢尾兰(O. latipetala)、凹唇石仙桃(Pholidota convallariae)、大苞兰(Sunipia scariosa)、滇南矮柱兰(Thelasis khasiana)。这些植物新资料的发现,对于丰富西藏植物种类以及对该地区物种多样性的保护和研究具有重要意义。     

利用DNA片段测序方法探究枳属和富民枳的分类地位

富民枳(Poncirus polyandra)属于芸香科(Rutaceae)枳属(Poncirus Raf.)。自发表以来,分类地位一直备受争议,其中在Flora of China中认为富民枳为柑橘杂交种(Poncirus polyandra),把枳属归并于柑橘属(Citrus)。该研究选取枳属的富民枳、枳(Poncirus trifoliata)及柑橘属下8个种共10个种47个个体作为研究材料,以九里香(Murraya exotica)为外类群,利用3个叶绿体片段(trn L-trn F、trn S-trn G、rbc L)、ITS片段和1个单拷贝核基因(Chr 5)数据构建系统发育树,探究枳属和富民枳的分类地位。结果表明:基于3个叶绿体片段数据构建的最大似然树(ML)和贝叶斯树(BI)的拓扑结构基本一致,10个物种聚为两大分支,即柑橘属的8个物种聚为一大分支,富民枳和枳聚为另一大分支。其中,富民枳所有个体聚为一小单系分支,枳的所有个体聚为一小单系分支,支持枳属和富民枳独立存在。2个核DNA片段数据结果显示,枳属的两个种与柑橘属的8个物种聚在一个大分支里,无法确立枳属的单系地位,但富民枳的9个个体聚在一起,暗示富民枳在遗传上是一个独立的类群。综上研究认为,无论是叶绿体DNA数据还是核DNA数据均支持富民枳是一个独立的物种,但核DNA数据不支持枳属成立。     

Reconstructing the history of Campanulaceae with a Bayesian approach to molecular dating and dispersal–vicariance analyses

We reconstruct here the spatial and temporal evolution of the Campanula alliance in order to better understand its evolutionary history. To increase phylogenetic resolution among major groups (Wahlenbergieae–Campanuleae), new sequences from the rbcL region were added to the trnL-F dataset obtained in a previous study. These phylogenies were used to infer ancestral areas and divergence times in Campanula and related genera using a Bayesian approach to molecular dating and dispersal–vicariance analyses that takes into account phylogenetic uncertainty. The new phylogenetic analysis confirms Platycodoneae as the sister group of Wahlenbergieae–Campanuleae, the two last ones inter-graded into a well-supported clade. Biogeographic and dating analyses suggest that Western Asia and the Eastern Mediterranean have played a major role as centers of migration and diversification within the Campanula alliance, probably in relation to the intense orogenic activity that took place in this region during the Late Neogene, and that could have promoted isolation and allopatric speciation within lineages. Diversification rates within several Campanula lineages would have increased at the end of the Miocene, coinciding with the Messinian Stage. Strong selective pressures from climate changes and the expansion of mountainous regions during this period are suggested to explain the adaptation to drought, cold or disturbed environments observed in many Campanula species. Several independent long-distance dispersal events to North America are inferred within the Rapunculus clade, which seem to be related to high ploidy levels.     

毛茛科六新种

该文描述了毛茛科六新种：(1)托里乌头,与阿尔泰乌头近缘,区别为其茎和叶无毛,总状花序极密集,雄蕊花丝多有1或2小齿。(2)门源翠雀花,与大通翠雀花近缘,区别为其茎极短,花序总状,退化雄蕊瓣片不分裂。(3)云台山铁线莲,与裂叶铁线莲近缘,区别为其叶为二回羽状复叶,花较小,雄蕊花丝呈黑色,无脉。(4)黑丝铁线莲,与前种云台山铁线莲在亲缘关系上极为相近,区别为其小叶较小,多呈狭卵形或披针形,聚伞花序也较小,通常只具3花。(5)五台山毛茛,与砾地毛茛相似,区别为其基生叶被柔毛,花瓣蜜槽具鳞片,心皮具短而粗的花柱和小柱头。(6)靖西铁线莲,与宝岛铁线莲在亲缘关系上接近,区别为其茎疏被短柔毛,小叶卵形或狭卵形,不分裂,聚伞花序有1~3花,萼片较大(长1.7~2 cm,宽0.5~0.7 cm)。