云南元谋盆地上新世甘棠组植物和孢粉组合及其古气候意义

云南元谋盆地湾堡甘棠组植物群的叶化石和孢粉化石合计107种类型,分属86属,47科。植物叶化石包括18科,24属,35种。除一种裸子植物外,其它均为被子植物。被子植物中,榆科、桦木科、豆科无论属种或者化石数量都是最多;杨柳科、槭科、蔷薇科次之;壳斗科、樟科、杨梅科、鼠李科、忍冬科、胡颓子科、杜鹃科、香蒲料、禾本科均有代表。甘棠组的孢粉植物群也相当丰富,合计97个类型,分属72属,44科。以松科、榆科、禾本科及蕨类植物的水龙骨科最为丰富,胡桃科、壳斗科、金缕梅科及蕨类植物的凤尾蕨属也很常见。被子植物花粉占孢粉总数的50%--60%,以禾本科和榆属花粉含量最高,多在10%以上。裸子植物绝大部分为松科花粉,占孢粉总数的20%-30%。孢子以水龙骨科和凤尾蕨属为主,二者各占孢粉总数的5%-10%。发现于元谋盆地湾堡甘棠组的植物叶化石以及孢子花粉组合在成分上都是混合的类群。组合中既有相当多的湿润亚热带常绿阔叶林成分,也有耐干旱的胡颓子、杨梅、旱蕨等灌木、小乔木或草本分子,同时还有含量很高的、在半干旱环境下也能生存的禾本科、榆科花粉。据此推测甘棠组的植物群和孢粉组合反映了上新世时元谋地区的植被已经分化,盆地的周围山地生长有松科、壳斗科、樟科、胡桃科、金缕梅科为主的常绿和落叶阔叶树木或林块,可能有少许杜鹃科小乔木混杂其中,属于地带性植被。而在盆地内则是以禾本科、蔷薇科等为主,杂以大戟科、豆科、忍冬科、杨梅科等灌木或草本植物以及榆科、桦木科等树木组成的稀树灌丛草原型植被。盆地内的植被所反映的气候和周边地区相比,显得明显干旱。因此推测元谋盆地在2-3百万年前的中晚上新世已经发育成为金沙江流域的干热河谷盆地之一。     

A Floristic Study of Flora of Seed Plants of the Chaqia-GongheBasin and Its Contiguous Zone in Qinghai,China

The Chaqia-Gonghe Basin and its contiguous zone is situated in eastern Qinghai of China, between latitude 34°45′- 37°00′N and longitude 98°45′- 101°30′E . Ranging from 2 800m to 5 305 m in altitude, the total area is about 38 300km2 . Its climate is continental or plateau-continental one . There are 854 species of native seed plants belonging to 59 families and 277 genera there , which occupied 37. 37% of the total species, 54 . 53% of the total genera and 65. 56% of the total families in Qinghai respectively . The floristic characteristics of the native seed plants are as follows : ( 1) Number of species and woody ones there are poor . (2) At generic level, the flora is temperate in nature, dominated by north temperate elements especially the typical elements from the warm and cold zone of Eurasia , but also with some elements of warm, cold warm and alpine ones . (3 ) The area is a margin of distribution for many species or genera especially for tropical ones, and thus , the flora of the area is clearly marginal in nature . (4) Floristic-geographically , it is a converged and transitional region for the Qinghai-Tibetan Plateau Alpine Flora , Loess Plateau Warm Flora , as well as East Asia Alpine Desert Flora. (5 ) It is a part of the Tangute Flora . (6 ) It is a key area to divide the subregions in the flora of Qinghai on the Tangute Area .     

Vegetation, climate and palaeoaltitude reconstructions of the Eastern Alps during the Miocene based on pollen records from Austria, Central Europe

Aim To reconstruct the flora, vegetation, climate and palaeoaltitude during the Miocene (23.03–5.33 Ma) in Central Europe. Location Six outcrop sections located in different basins of the Central Paratethys in Austria. Methods Pollen analysis was used for the reconstruction of the vegetation and climate. The altitude of the Eastern Alps that are adjacent to the Alpine Foreland and Vienna basins has been estimated using a new quantification method based on pollen data. This method uses biogeographical and climatological criteria such as the composition of the modern vegetation belts in the European mountains and Miocene annual temperature estimates obtained from fossil pollen data. Results Pollen changes from Early to Late Miocene have been observed. The vegetation during the Burdigalian and Langhian (20.43–13.65 Ma) was dominated by thermophilous elements such as evergreen trees, typical of a present‐day evergreen rain forest at low altitudes (i.e. south‐eastern China). During the Serravallian and Tortonian (13.65–7.25 Ma) several thermophilous elements strongly decreased, and some disappeared from the Central European region. This kind of vegetation was progressively substituted by one enriched in deciduous and mesothermic plants. Middle‐altitude (Cathaya, Cedrus and Tsuga) and high‐altitude (Abies and Picea) conifers increased considerably during the Langhian and later on during the Serravallian and Tortonian. Main conclusions Pollen changes are related to climatic changes and to the uplift of the Alpine massifs. The vegetation during the Burdigalian and Langhian reflects the Miocene climatic optimum. The decrease in thermophilous plants during the Serravallian and Tortonian can be interpreted as a climatic cooling and can be correlated with global and regional climatic changes. This study shows that the palaeoaltitude of the eastern part of the Eastern Alps during the Burdigalian was not high enough for Abies and Picea to form a forest. Therefore, we inferred that the summits of most of the mountains would have been less than 1800 m. The substantial increase of middle‐ and high‐altitude conifers in the pollen spectra suggests that the uplift rate increased during the Langhian in this region. Based on higher palaeoaltitude estimations for the pollen floras from the studied sections of Austria, we infer that the uplift of the easternmost part of the Alpine chain continued during the Serravallian and Tortonian.     

中国现代花粉数据集

孢粉是重建古植被、古气候的重要基础数据。孢粉数据库对研究样点至区域和全球尺度上的古环境演变规律、古气候变化特征反演和古生物地球化学循环模拟等具有重要意义。该文收集整理了中国1960-2020年间发表和部分未发表的现代花粉数据记录, 包括样品编号、采样位置、采样地经纬度和海拔高度、样品类型、数据来源、数据类型、周边植被信息、参考文献、花粉类群及其含量等信息; 并对数据进行筛选和标准化等处理, 由此整合为中国现代花粉数据集。该数据集由4 497个现代花粉采样点的数据信息组成, 包括660个来自中国第四纪孢粉数据库数据, 1 763个前期整理发表的数据和2 074个近期收集的数据, 涵盖772个花粉类群。样品类型以土壤表层样品(3 332个)为主, 苔藓样品以及湖泊、海洋表层样品等为辅, 广泛分布于全国不同地理区域和植被类型中, 其中以温带荒漠区域(24.91%)和亚热带常绿阔叶林区域(24.02%)最丰富, 其次为温带草原区域(16.14%)和青藏高原高寒植被区域(15.83%)。数据按照来源可分为原始数据(58%)和数值化数据(42%); 按照数据类型可分为原始统计粒数的样点(59%)和以花粉百分比表达的样点(41%)。半个多世纪以来, 科研人员开展了大量的表层现代花粉取样和研究。本数据集虽然仅获取部分记录, 但样点覆盖了我国绝大多数地区, 可有效地用于古植被与古气候重建的现代孢粉与现代植被校验, 并将为中国孢粉数据库的建立与更深入的孢粉研究提供数据支撑。     

澜沧江源区种子植物区系研究

澜沧江源区位于青海省的南部,约处于北纬31°30′～33°53′,东经92°35′～97°35′。海拔3500～5900m,面积约50590km2,属于高原大陆性气候类型。本区共有野生种子植物61科、279属、996种。分别占青海省总科数的67．78％、总属数的54．92％、总种数的43．59％。区系特征如下：（1）种类相对丰富,木本较少;（2）就属的层面而言,本区属于以北温带成分,特别是欧亚大陆温、寒地带典型成分和东亚的中国．喜马拉雅高山成分为优势的高寒类型的温带区系性质;（3）许多属和多数种均以横断山地区和西藏东北部高原为传播通道而与喜马拉雅关系密切;（4）为青藏高原主体区系与横断山区系的交汇过渡区,区系的过渡性质明显;（5）是青藏高原植物亚区唐古特地区的一部分;（6）是青海植物区系或“唐古特植物地区”中植物分化比较活跃的地区之一。     

Mapping of key bee flora of upper Gangetic region of India – a palynological assessment through regional honeys

Fifty‐one regional honey samples, collected mainly from Uttarakhand and Uttar Pradesh districts, were studied to determine the pollen composition. Pollen spectra of the local honeys varied according to the vegetation type utilized by the bees within this floristically diverse region. Eight pollen types from Uttarakhand and seven from Uttar Pradesh were the predominant pollen types in honey and included both local naturalized flora as well as cultivated crops. The investigation revealed that in addition to already known bee forage (e.g. Brassica, Coriandrum, and Litchi) some other species including Eucalyptus, Callistemon that are planted for social forestry programs, are also heavily utilized as pollen and nectar sources by honey bees in urban and semi urban areas. Naturalized flora including Myrica, Rumex, Erigeron are also utilized and therefore are important for apiculture in these regions.     

Botanical origin of honey from south of Calde´n district (Argentina)

We performed palynological analysis of 75 honey samples from the south of Caldén district, which is the part of the phytogeographical province del Espinal. Prosopis caldenia , "caldén" (Fabaceae) is the dominant arboreal species in this region. 79 pollen types that belong to 36 plant families were identified. Honeydew elements are absent or present in negligible amounts. Native flora is intensely utilized. Main nectar sources that characterize monofloral honey samples, are these natives Condalia microphylla (Rhamnaceae), Prosopis sp. and Vicia sp. (Fabaceae), Larrea divaricata (Zygophyllaceae) and Brassicaceae, which are foreign to the area. The pollen from these plants along with the pollen of Trichocline sp. (Asteraceae) and Prosopidastrum globosum (Fabaceae), Schinus fasciculatus (Anacardiaceae), Astereae and Lycium sp.(Solanaceae), characterize honey from Caldén.     

Pollen Types Used by the Native Stingless Bee, <Emphasis Type="Italic">Tetragonisca angustula</Emphasis> (Latreille), in an Amazon-Chiquitano Transitional Forest of Bolivia

Samples of corbicular and stored pollen gathered by Tetragonisca angustula (Latreille, 1811) in an Amazon-Chiquitano transitional forest during the dry season were analyzed. The pollen spectrum was established as well as the dynamics of the relationship between the stingless bee and the surrounding flora. Pollen samples obtained from three rational hives were subjected to acetolysis and 55 pollen types were identified, the most frequent being from Anadenanthera (Fabaceae), Chenopodiaceae, and Dydimopanax (Araliaceae). Significant differences in pollen families used between hives along the months of collection were found in stored pollen and non-significant differences in corbicular pollen. Mean values of alpha diversity (H′) showed T. angustula as a generalist while beta diversity qualitatively showed that pollen composition was similar between two hives both of which differed from the third hive. Pollen types in corbicular and stored pollen were in general related with richness of flowering plants in the foraging area; the pollen offer was less diverse than the pollen collected, and a trend to prefer the collection of pollen from the most abundant flowering species could be discerned. T. angustula showed polylectic feeding habits and a capacity to adapt to food availability.     

Leaf functional traits vary with the adult height of plant species in forest communities

Aims Within-community variation accounts for a remarkable proportion of the variation in leaf functional traits. Plant height may be used to explain within-community variances of leaf traits because different microenvironments, especially light intensity, may occur at different heights. This study determines whether or not leaf nitrogen (N) and phosphorus (P) contents as well as leaf mass per area (LMA) are interspecifically correlated with the adult height of forest woody species. We also discuss these relationships with respect to community structure and functions of the ecosystem.Methods A total of 136 dicotyledonous woody species from 6 natural forests (3 evergreen and 3 deciduous ones) in East China (18°44′–45°25′N, 108°50′–128°05′E) were investigated. For each of the 157 species–site combinations, 6 traits were measured: plant adult height relative to the forest canopy (H R), leaf N and P contents per unit area (N area and P area), N and P contents per unit dry mass (N mass and P mass) and LMA. The total variances of each leaf trait across sites were partitioned in a hierarchical manner. The relationships between leaf traits and H R within forest communities were then analyzed using both standardized major axis regression and Felsenstein's phylogenetic independent contrasts. Relationships between evergreen and deciduous forests were compared by linear mixed models.Important findings H R is a robust predictor of leaf N area, P area and LMA, explaining 36.7, 39.4 and 12.0% of their total variations across forests, respectively. Leaf N area, P area and LMA increased with H R in all of the studied forests, with slopes that were steeper in evergreen forests than in deciduous ones. Leaf N mass and P mass showed no significant relationship with H R generally. The increase in leaf N area, P area and LMA with H R across species is assumed to maximize community photosynthesis and may favor species with larger H R .     

粤北通天箩石灰岩阱洞的植物及其与生态条件的关系

 通天箩在广东北部乳源县的岩溶地区,是一个陷入地中达95m深的大型垂直阱洞,阱口直径73m,阱底最大直径140m,阱壁陡峭,各种证据表明,自古以来没有人下过阱。我们经过3次探险下阱调查,发现阱底中部生长着面积约3500m2的常绿阔叶林,还有不少藤本植物和蕨类植物,共有蕨类植物6科、8属、12种,被子植物46科、61属、80种(包含变种);这些植物区系是在光照不足和石灰岩基质发育的土壤上存在和发展起来,从未受过人类的干扰。     

安徽大别山分水岭地带植物花粉形态研究

应用光学显微镜和扫描电镜对安徽大别山分水岭鹞落坪自然保护区7月份开花的32科52种3变种植物的花粉形态进行了观察和研究,提供了花粉图谱、植物生长习性和地理分布范围,为地层中的化石花粉鉴定提供标准图谱和相关信息。对该区域植物的生态因子,包括地理位置、分布范围、海拔高度、年降水量、年积温和生境进行归纳总结,确定该区域的花粉形态综合特征与气候和环境之间可能的联系,为地层孢粉研究提供现代孢粉学依据。     

An Analysis of the Flora of Qinling Mountain Range: Its Nature,Characteristics, and Origins

The Qinling Mountain Range, which covers an area of ca. 76500km² and ranges from 32°05′ to 34°45′ N and from 104°30′ to 115°52′ E, is a major watershed of the Huanghe and Chang jiang rivers with the highest peak about 3767 m above sea level. The flora comprises ca. 3124 species in 892 genera, of which 51.9% of species and 4.4% of the genera are endemic to China. Evoluated in this paper is the importance of the 20 larger fami lies which together contain 65.2% of the total number of species. The phytogeographical affinities of genera of seed plants in the flora are analyzed and briefly discussed. Among the native genera of the flora of the Qinling Mountain Range, 220 (26.8%) are tropical, 563 (68.5%) temperate, and 39 (4.7%) endemic to China. It is clear from the figures that temperate genera play an important role in the flora and vegetation of the Qinling Mountain Range. The features of the flora include the unusually high proportion of endemic species, a wealth of Sino-Japanese elements and prominant temperate nature in compsition. On the ba sis of analysis of paleobotanical materials in the Qinling Mountain Range and adjacent areas, historical distribution of dominant species, and the origin and relationships of Chinese en demic genera occurring there, the flora is of outstanding originality. No doubt, the rich and diverse flora have evolved gradually and autochthonously at least since the latest Cretaceous.     

Early Tertiary fossil plants and paleoclimate of Lanzhou Basin

Fossil plants from the lower part of Xianshuihe Formation in the Lanzhou Basin, Gansu Province were studied. The flora contains 29 species, representing 20 genera and 12 families, which include Lauraceae ( Daphnogene ), Lardizabalaceae ( Akebia ), Berberidaceae ( Berberis ), Ulmaceae ( Planera, Ulmus, Zelkova ), Betulaceae ( Alnus, Carpinus ), Myricaceae( Myrica ), Salicaceae ( Populus, Salix), Myrsinaceae(Ardisia), Rosaceae ( Prunus, Sorbus, Sorbaria, Spiraea ), Leguminosae ( Gleditsia, Sophora), Anacardiaceae (Rhus), Caprifoliaceae(Viburnum). An analysis of the floristic elements and their foliar physiognomy shows that most members of the flora are deciduous broad-leaved trees or shrubs with a few evergreen shrubs. The most noteworthy species is Rhus turcomanica which was present in the Middle Eocene to Late Eocene of Central Asia (Kazakhstan, Turkmenistan). Generally, Rhus turcomanica occurred at the same beds as Palibinia, an extinct fossil plant whose presence indicates a subtropical dry climate. Another species, Sorbaria callicomifolia Kornilova was present from the Early Oligocene to Early Miocene of Central Asia (Kazakhstan and Turkmenistan). According to an analysis of spores and pollen, this flora contains over 20 species. It is predominated by the angiosperm pollen. There appeared Ephedripites and Nitrariadites which were important elements in the dry area. Ephedripites was found from the Upper Cretaceous to Early Tertiary. Nitrariadites occurred in the Late Miocene, whereas Rhus turcomanica and Sorbaria callicomifolia were both reported in the subtropical dry area from the Middle Eocene to Early Oligocene. The latest record of Rhus turcomanica is from the Middle Eocene to Early Oligocene of Central Asia. The presence of this element in the lower part of Xianshuihe Formation may indicate that itsage is the latest stage of the Early Oligocene.     

兰州盆地早第三纪植物及古气候意义

化石采自甘肃省兰州盆地咸水河组底部,经研究认为有29种,归属20属12科。它们是：樟科 Lauraceae (Daphnogene),木通科Lardizabalaceae(Akebia),小檗科Berberidaceae(Berberis),榆科Ulmaceae (Planera,Ulmus,Zelkova),桦木科Betulaceae(Alnus,Carpinus),杨梅科Myricaceae(Myrica),杨柳科Sali- caceae(Populus,Salix),紫金牛科Myrsinacese(Ardisia),蔷薇科Rosaceae (Prunus,Sorbus,Sorbaria,Spir- aea),豆科Leguminosae(Gleditsia,Sophora),漆树科 Anacardiaceae(Rhus),忍冬科Caprifoliaceae(Viburnum) 等。经植物区系组成与叶相分析显示,该植物区系的大多数成员是落叶阔叶乔、灌木,少数为常绿灌木。其中特殊的分子是 Rhus turcomanica Korov．ex Vassilvesk,该成分是早第三纪中、晚期的标志化石植物。另一化石植物 Sorbaria callicomifolia Kornilova曾出现在中亚的早渐新世,最晚至早中新世。同一层位采集的孢粉样分析结果显示：该组合仅约20种,种类相对贫乏,并以被子植物的花粉占优势。其中出现裸子植物的麻黄粉,被子植物的白刺粉及蒿粉等,这几个类型均指示沉积时期经历干旱气候。综合植物大化石及孢粉分析研究,均出现一些指示气候为亚热带干旱或周期性干旱气候的特点,并据Rhus turcomanica出现的最晚记录,推测咸水河组底部的地质时代大约是早渐新世晚期。     

云南地区种子植物区系成分的地理分布格局及其聚类分析

以覆盖云南地区全境的种子植物分布信息为基础,结合GIS和聚类分析的方法探讨了云南地区植物区系成分的地理分布格局.结果表明,随着纬度的升高,世界分布成分所占的比重呈递增趋势,热带区系成分所占比重呈递减趋势,而温带区系成分所占比重则呈递增格局.聚类分析结果表明,在24.5°N左右,研究区域可分为南北两个部分.分界线以南,热带区系成分占优势地位,植被类型主要为热带区系性质强烈的山地雨林、季节雨林、季雨林和季风常绿阔叶林等;分界线以北,温带区系成分所占比重相对较高,甚至占主导地位,植被类型主要为具较强温带区系性质的硬叶常绿阔叶林、温性针叶林、针阔混交林和高寒草甸以及具强烈区系过渡性质的半湿润、湿性常绿阔叶林.该分界线与"田中线"不同,可能源于研究目标和内容的差异.

Abstract：

Based on all-around floristic information,and by using geographical information system and cluster analysis,this paper studied the spatial pattern of seed plant floristic elements in Yunnan Province of China.It was indicated that the proportions of cosmopolitan and temperate elements increased with increasing latitude,while those of tropical elements had a decreasing trend.Cluster analysis showed that the study area could be divided into two parts,with the latitude about 24.5°N as a division line.To the south of the line,the dominant flora was tropical elements,and the vegetation was dominated by tropical mountain rainforest,seasonal rain forest,monsoon rain forest,and monsoon evergreen broadleaved forest.To the north of the line,there were much greater proportions of temperate elements,and the vegetation was dominated by the evergreen,hard and broadleaved forest,temperate coniferous forest,coniferous and broadleaved mixed forest,alpine meadow,and evergreen broadleaved forest(moist or semi-moist,showing strong floristic transition).This division line was different from "Tanaka Line",possibly due to different study aims and contents.     

禄丰古猿化石地点地层概述

本文较详尽地记述了云南禄丰古猿化石地点附近的地质、地貌、地层情况以及产出古猿及大量脊椎动物化石的剖面。     

Numerical Characteristics of Pollen Assemblages of Surface Samples from the West Kunlun Mountains

A total of 31 suface sediment samples were collected from West Kunlun Mountain in south Xinjiang Autonomous Region in northwest China. These samples are from seven types of vegetation: Picea schrenkiana Fisch. et Mey. forest, Sabina Spach. woodland, sub-alpine steppe, alpine meadow, desert vegetion, cushion-vegetation and vegetation adjancent to glaciers. Pollen percentages and pollen concentrations were calculated in all samples. The dominant pollen types in the region are Chenopodiaceae, Artemisia, Picea, Ephedra, Gramineae, Cyperaceae, Rosaceae, Leguminosae, Compositae etc. In order to reveal the relationship between pollen composition and the vegetation type from which the soil sample was collected, principal component analysis and group average cluster analysis were employed on the pollen data. The results revealed that the major vegetation types in this region could be distinguished by pollen composition: a. Samples from desert vegetation were dominated by pollen of Chenopodiaceae (about 60195%). The percentages of all other pollen types were low. b. Picea forest samples were rich in Picea pollen (about 20%) Sabina forest had more Sabina pollen grains than other vegetation types (about 5%, others <1%). Pollen percentages of Artemisia, Chenopodiaceae and Ephedra were comparatively higher (each about 20%) in these samples from the two types of vegetations. C. Pollen percentages of Artemisia, Cyperaceae, Gramineae and Chenopodiaceae were high in both sub-alpine steppe and alpine meadow. But steppe containal more Artemisia and Chenopodiaceae (steppe 33.75% and 32.30%, meadow 15.57% and 19.48% in average), less Cyperaceae and Gramineae (steppe 2.58% and 7.60%, meadow 22.35% and 12.93% in average) than meadow. d. Samples from cushion-vegetation and vegetation adjacent to glaciers were mainly composed of pollen grains transported from other sites. It was not easy to distinguish them from other vegetation types. Principal component analysis and cluster analysis distinguish samples from Picea forest, Sabina woodland, sub-alpine steppe, alpine meadow and desert vegetation. Therefore we think it will be possible to apply the module to reconstruct past vegetation in this region and other similar regions. Regression analysis was also applied to reveal the relationships between pollen and plant percentages of Artemisia, Chenopodiaceae, Cyperaceae and Gramineae. The results indicated that a linear relationship existed between pollen and plant percentages for Artemisia, Chenopodiaceae and Cyperaeeae.     

滦河流域及周边地区花粉与植被关系的研究

滦河流域及周边地区空气中的花粉组合基本上反映了当地的植被面貌, 与植物的花期相对应, 乔木植物的花期多在春季, 草本植物的花期多在夏秋季, 该地冬季基本上无植物开花, 冬季空气中的花粉应是当年或多年春、夏、秋季散落在地上又被风吹到空气中的表土花粉和一些外来花粉 ;表土花粉随海拔高程的降低依次出现山地草甸、针阔混交林或以针叶树为主的针阔混交林、山地灌草丛、滨海平原草甸和滨海草甸或滨海盐生草甸的等 5个花粉组合带, 分别为蒿 (Artemisia)唐松草 (Thalictrum)松(Pinus)桦 (Betula) 孢粉组合带、松桦栎 (Quercus) 蒿孢粉组合带、藜科 (Chenopodiaceae)蒿禾本科 (Gramineae)中华卷柏 (Selaginellasinensis) 孢粉组合带、藜科蒿菊科 (Com positae)香蒲 (Typha) 孢粉组合带和藜科蒿莎草科 (Cyperaceae)禾本科孢粉组合带 ;由于花粉在河水中是以悬移质颗粒被搬运, 因此在不同时期沉积物花粉组合存在着一定的差异, 其中洪水期间河水对孢粉的分选作用最为明显。     

陕西种子植物区系地理初步研究

陕西约有种子植物３９０７种,隶属于１７７科１１１５属,其中热带属３２８属（２９４４％）,温带属６４５属（５８１１％）,中国特有属５３属（４７５％）。区系地理成分分析表明,北温带分布属是其植物区系的核心,反映出区系的温带性质。然而这些温带区系成分并非起源于北方,而是亚热带山区起源,是华夏植物区系的北向延伸,其与亚热带和热带植物区系成分有着共同的起源,是华夏植物区系的组成部分。由于特殊的地理位置,决定了其成为多种地理成分的汇集之地,并表现出由亚热带向温带过渡的区系特点。此外区系中单、少种科、属及古特有属相对丰富,体现出区系的古老性。