Biogeography,timing, and life-history traits in the PPAM clade: Coleanthinae (syn. Puccinelliinae), Poinae,Alopecurinae superclade,Miliinae, and Avenulinae and Phleinae (Poaceae,Pooideae, Poeae)

We conducted a biogeographic analysis of the PPAM clade of Poeae Plastid DNA Group 2, which includes 12 subtribes of C₃ grasses. One hundred and eighty-four species sampled represent 42 of 43 accepted genera and taxonomic diversity in large genera. We analyzed plastid sequences of matK, trnC-rpoB, and trnT-trnL-trnF using BEAST to produce a dated tree and MrBayes to produce a Bayesian tree, on which we ran Bayesian-Binary-Markov-Chain analyses on a worldwide biogeographic data set of 12 areas. PPAM split in southwestern Asia into subtribe Coleanthinae and PAM clades in the Early Miocene. PAM diversified rapidly in the Middle Miocene in southwestern Asia into four monogeneric lineages, Avenulinae, Phleinae, Miliinae, Poinae, and the Alopecurinae superclade (seven subtribes with 27 genera). In the Late Miocene, Pliocene, and mostly Pleistocene, the latter four lineages diversified and dispersed across Eurasia and established in North America. Dispersals to the southern hemisphere occurred in the Pliocene and Pleistocene. Annuals occur in 15 Mediterranean and southwestern Asia genera, but in few genera in other regions. Beyond phylogenetically isolated annual species dating to the Miocene, all other annuals evolved in the Pliocene and Pleistocene. Cold tolerance is high among perennial species, many occurring in the alpine, nine genera ranging into the Arctic. We suggest that alpine and subalpine habitats were ancestral. High tolerance of saline and alkaline conditions arose between the Pliocene and Pleistocene in Coleanthinae, Alopecurinae, Poinae, Hookerochloinae, Beckmanniinae, and Arctopoa. Combinations are proposed for Cornucopiae alopecuroides in Alopecurus and for Paracolpodium colchicum in Hyalopodium. A nothogenus × Catanellia is proposed for Catabrosa × Puccinellia.     

Biogeographical Divergence of the Flora of Yunnan,Southwestern China Initiated by the Uplift of Himalaya and Extrusion of Indochina Block

The floral composition of Yunnan is conspicuously linked to the biogeographical history of this extremely species-rich province in southwestern China. The floristic compositions of three representative regions in Yunnan were compared to reveal their variation with geography. From southern Yunnan, 4150 native species (including subspecies and varieties) from 1240 genera and 183 families of seed plants were recognized. From central Yunnan 3389 native species from 1095 genera and 167 families of seed plants were recognized. From northwestern Yunnan 6807 native species from 1296 genera and 166 families of seed plants were recognized. Although these three floras across Yunnan are similar in familial composition, similarities between the floras of southern and northwestern Yunnan are low at the generic and specific levels. The flora of northwestern Yunnan is dominated by families and genera with cosmopolitan and north temperate distributions, while the flora of southern Yunnan is dominated by tropical families and genera. Northwestern Yunnan is composed largely of temperate genera, of which the highest proportion has a north temperate distribution. In contrast, southern Yunnan has mainly tropical genera, of which most have a tropical Asian distribution. The flora of central Yunnan is a combination of southern and northwestern Yunnan. These three floras might be derived from a common Tertiary tropical or subtropical East Asian flora, but the geological history of each region has influenced its flora, and they have remained divergent since the late Tertiary. The flora of northwestern Yunnan has evolved with the uplift of the Himalayas and by gradual proliferation of mainly cosmopolitan and north temperate floristic elements, while the flora of southern Yunnan has evolved with extrusion of the Indochina block and the influence of mainly tropical Asian elements.     

Diversification and extinction patterns among Neogene perimediterranean mammals

The best mammalian fossil record during the Neogene of Western Europe is that of the rodents, the most successful and diversified mammal order. The study of origination and extinction during the Neogene (24-3 Ma BP) in one of the best-documented areas, Spain and southern France, gives an insight into the dynamics of these communities and indicates the possible nature of the driving forces. Three main periods of time show a high rate of origination: the late Burdigalian (17.5 Ma BP), the early Vallesian (11.5-11 Ma BP) and the early Pliocene (4.2-3.8 Ma BP). Two of these high origination-rate periods are immediately followed by important extinction events during which all cohorts are deeply affected (11.5-11 Ma BP and 4.2-3.8 Ma BP). The most important extinction event seems to occur during the early Vallesian (11.5-11 Ma BP), which probably includes the middle/late Miocene boundary. At the Miocene/Pliocene boundary, and during the early Pliocene, the faunal turnover seems to become faster, inducing a strong decrease of the mean species duration. Whereas the main immigration event, which occurs at 17.5 Ma BP, can be related to other faunal migrations in terms of the closure of the Tethys, as it occurs also in eastern Africa and in southwest Asia, the middle/late Miocene boundary event may have been related to a period of ice growth in the Southern Hemisphere. The extinction event that affects the planktonic foraminifera at 12 Ma BP cannot be chronologically correlated to this southwestern European land-mammal extinction event, because the calibration of the marine fossil record during that time-span has to be precise. Some limited terrestrial faunal exchanges that occur during the Messinian between southwestern Europe and northwestern Africa do not deeply affect the general faunal dynamics. Both allochthonous cohorts of immigrants become rapidly extinct. Several endemic rodent faunas, indicating insular conditions, have been reported from the southern edge of the western European continent from the middle Miocene up to the Pliocene. All show low taxonomic diversity, strong endemism and short survival. Some of them, like those of the Gargano Islands during the late Miocene, underwent peculiar morphological changes and also speciation. The large number of rodent genera coevolving in the Gargano Islands is indicative of the large surface areas of these islands. The general geographic pattern of southwestern Europe during the Neogene may therefore correspond to a large continental province including Spain and southern France with some kind of fast-modifying archipelago on its southern rim.     

云南石林地区石灰岩山地种子植物区系成分的研究

云南石林是我国为数不多的世界地质公园。分析了云南石林地区石灰岩山地植物区系从科到种的 组成特征。调查统计分析的植物共有维管植物147科533属889种,其中种子植物占133科508属846种。 种子植物科级区系成分中,以亚热带科为主,暖温带科次之。属级区系成分中,热带分布属占优势,占总属数 的56．2％,温带分布属也占近三分之一,这表明该植物区系的过渡性即亚热带性质。在其种级区系组成中,中 国特有种有328种,占总种数的40％,其次是东亚分布种和热带亚洲分布种。石林石灰岩山地种子植物区系, 从科到种的组成都充分说明了该植物区系的亚热带性质及组成上的独特性。     

云南蕨类植物的物种多样性和区系组成

在一定实地调查和分类的基础上,采用统计分析及区系地理分析法,对云南地区蕨类植物进行研究。结果表明:云南地区共有蕨类植物60科193属1 530种(包括变种和变型),科、属、种分别占中国蕨类植物科总数的58.8%,属的83.9%和种的95.2%;在这60个科中含30种以上的有13个,含5个属以上的有11个,分别占该蕨类植物区系属、种数的56.5%和79.2%,特别是鳞毛蕨科、蹄盖蕨科、水龙骨科和金星蕨科,这4个科共拥有70属761种,分别占总属数、总种数的36.3%、49.7%;193属中含30种以上的有11个,分别占总属、总种数的5.7%和41.7%,最具优势的是鳞毛蕨属和耳蕨属、蹄盖蕨属、铁角蕨属、卷柏属,这5个属共有403种,占总种数的26.3%;该区系中无云南特有科,但具有4个亚洲特有科:雨蕨科、稀子蕨科、柄盖蕨科和骨碎补科;该区系以热带、亚热带性质为主,科的区系成分中热带亚热带分布的科占66.6%,热带成分的属有112个,占68.7%(除世界分布类型);该区系是东亚地区蕨类植物区系的重要组成部分,东亚分布31属和中国特有分布6属,分别占总属数(除世界分布属外)的19.0%和3.7%;该地区蕨类植物区系与西藏、台湾具有共同的区系起源和物种分化形成的背景,属的相似性系数约为70%,种的相似性系数约为30%,均起源于热带亚热带地区;属的热带区系成分与温带区系成分所占比例分别为68.7%和27.6%,存在一定的区系过渡性;该区系科的分化强度为3.2,属的分化强度为7.9,在科、属水平上均表现出较强的区系分化特征。     

大中山自然保护区种子植物区系研究

云南省大中山自然保护区有种子植物749种,隶属于137科396属。区系成分中,世界分布33属,占全部总属数的8.33%;热带分布206属,占除世界分布属以外的56.75%(下同),温带分布148属,占40.77%,中国特有9属,占2.48%。该地区植物种类丰富,种子植物区系起源古老,地理成分复杂,具有明显的亚热带特性。从区系成分和植物类群多样性所占比例上看,是一个需要重点保护的区域。     

A unique record of Cercis from the late early Miocene of interior Asia and its significance for paleoenvironments and paleophytogeography

The climatic impacts of the Tibetan Plateau since the Neogene and the phytogeographic pattern changes of formerly widely-distributed forest communities on the plateau remain poorly constrained. Today, Cercis L. (Fabaceae) is a well-known arborescent genus typically distributed in subtropical to warm temperate zones of the Northern Hemisphere, and Paleogene fossil occurrences from Eurasia and North America show a long history of the genus in mid-low latitudes of the Northern Hemisphere. Here, we describe a fossil species, Cercis zekuensis sp. nov. based on well-preserved fruits from the early Miocene of the northeastern Tibetan Plateau. Detailed morphological comparison (e.g., ventral margin with a veinless wing) of extant and fossil members of Cercis and other genera confirmed validity of the present taxonomic identity. Based on the comparison with extant relatives and their climate preferences, this unexpected occurrence of thermophilic Cercis in northeastern Tibetan Plateau indicates this area had higher temperature and precipitation in the Miocene than today. Integrated with inferred (paleo-)temperature lapse rates, this indicates a low paleoelevation of less than 2.4 km. In contrast with the present-day alpine climate here (~3.7 km), such a low elevation facilitated a more favorable habitat with comparatively high biodiversity and warm temperate forests at that time, as were evidenced by co-occurring megafossils. Moreover, the present existence of Cercis implies the genus was widespread in interior Asia during the early Neogene and shows its modern disjunction or diversification between eastern and central Asia was possibly shaped by the late Cenozoic regional tectonic uplift and consequential environmental deterioration.     

云南常绿阔叶林的植被地理研究

云南具有极其丰富的生物多样性和以常绿阔叶林为优势的植被类型。该研究利用6个基于样方层面的1 hm²样地资料, 以及通过对整个植被类型的植物区系的调查, 对云南常绿阔叶林植被型的3个植被亚型(季风常绿阔叶林、半湿润常绿阔叶林和中山湿性常绿阔叶林)的生态外貌特征、植物区系组成及其生物地理演化进行了研究。在样方层面, 尽管这3个常绿阔叶林在树种组成上优势种均为壳斗科、樟科和山茶科植物, 但它们在种类组成、多样性、生态外貌和生物地理特征上呈现多样化。分布在南部及西南部的季风常绿阔叶林物种组成极其丰富, 具有热带森林的生态外貌, 并以热带亚洲分布种为优势种。主要分布在云南高原的半湿润常绿阔叶林和云南中部和北部山地的中山湿性常绿阔叶林具有亚热带常绿阔叶林的生态外貌特征和以中国-喜马拉雅及中国特有种占优势, 是中国西南独特的植被类型。在植被亚型层面, 这3个常绿阔叶林的植物区系(包括所有生活型的种子植物)中种数最多的科, 按地理成分均为世界分布型的科, 含种数较少的科则为其他各种分布型的科。半湿润常绿阔叶林和中山湿性常绿阔叶林的植物区系, 热带分布属分别占总属数的44.91%和44.04%, 温带分布属占46.29%和48.19%, 其中北温带分布属比例最高, 分别为18.36%和19.95%。季风常绿阔叶林植物区系则显示了不同的地理成分格局: 热带分布属占总属数的78.05%, 并以热带亚洲分布属占最高比例。通过对这3个常绿阔叶林的比较发现, 半湿润常绿阔叶林和中山湿性常绿阔叶林除生态外貌特征有一定区别外, 在植物区系组成和地理成分上很接近, 它们在种的组成上, 与季风常绿阔叶林的类似性仅为17.1%和15.4%。季风常绿阔叶林因其在植物区系和生态外貌上与后二者区别明显, 建议在云南植被分类上划分一个独立的植被型, 它是东南亚低山常绿阔叶林分布在中国西南部热带北缘山地的一个植被类型。结合云南的地质历史和古植物学资料, 认为云南的常绿阔叶林及其植物区系受晚中新世以来的地质历史事件深刻影响。半湿润常绿阔叶林是中国西南独特而特有种丰富的植被类型, 由于严重的人为干扰破坏, 现已片段化或成为萌生灌丛状, 应给予优先保护。     

Hemiasterid echinoids (Echinodermata: Spatangoida) from the Cretaceous Tethys to the present-day Mediterranean

Hemiasterid echinoids form one of the oldest and most varied spatangoid groups. Current data on stratigraphical and geographical distribution pattern show that their biogeographical history is closely related to Mediterranean-Tethyan structural and climatic changes. The group first appeared in the Aptian in the central Tethys (southwestern Europe) and developed and diversified remarkably in the Late Cretaceous through the subgenera Hemiaster (Hemiaster), H. (Bolbaster) and H. (Leymeriaster). Marked morphological changes arose in the early Paleogene when new Tertiary forms H. (Trachyaster), Opissaster and Ditremaster, originating in the Caribbean and Madagascan regions, respectively, replaced H. (Bolbaster) which partly survived and H. (Hemiaster) and H. (Leymeriaster) which disappeared entirely. These new forms achieved their greatest diversity during the Eocenee and thrived in the Mediterranean basin until it was sealed off from the Indo-Pacific in the Middle Miocene. Then Late Neogene climatic and structural events reduced hemiasterids to only a few Mediterranean species. The survivors of modern groups persisted in refuge areas of the western Mediterranean until middle Messinian times before being reduced to only one species, the last fossil one, during the Pliocene. Then, the Cenozoic groups H. (Trachyaster) and Opissaster definitively disappeared. Outside the Mediterranean basin primitive H. (Bolbaster) and modern Ditremaster, which colonized deep-water Atlantic environments from the Late Cretaceous and Middle Miocene respectively, survived the Messinian and Plio-Pleistocene climatic crises. They flourished in the northern Atlantic where their present-day descendants Ditremaster (Sarsiaster) griegii and H. (Bolbaster) expergitus still survive. H. (Bolbaster) expergitus spread worldwide and colonized the western Mediterranean in the Plio-Pleistocene via the Straits of Gibraltar.     

云南景谷盆地晚第三纪介形类

该文首次报道景谷盆地介形类化石13属30种(其中19新种,1未定种)并建立3个介形类化石组合,三号构组以Potamocypris-Candoniella为代表的介形类化石组合,时代为中新世早期;回环组以Herpetocyprella-Metacypris为代表的组合,时代为中新世中晚期;大红猫村组以Leucocythere-Ily-ocypris组合为代表,时代为上新世。     

Age and implications of the Forest Bed, Falkland Islands, southwest Atlantic Ocean: Evidence from fossil pollen and spores

Diverse pollen and spore assemblages (microfloras) are preserved in organic clays and lignites associated with fossil tree remains in the Forest Bed. At present, these microfloras provide the only reliable basis for determining the age, composition, structure and affinity of the Forest Bed community. The Bed is suggested to be Middle? Miocene to Early Pliocene (age range Oligocene–Early Pliocene) based on the time distribution of a number of rare pollen types and the present-day ecology of their nearest living relatives in central–southern America and the southwest Pacific. The wet forest community whose remains form the Forest Bed was a form of broadleaf-gymnosperm temperate rainforest in which Dacrydium, Lagarostrobos and Podocarpus are likely to have formed an overstorey above a closed canopy dominated by Nothofagus (Nothofagus) spp. The latter subgenus is now endemic to ±uniformly wet regions in southern South America whilst two of the tall gymnosperms (Dacrydium, Lagarostrobos) are now endemic to the southwest Pacific region. An extinct, probable shrub-sized, conifer (Podosporites microsaccatus) appears to have formed the ground cover. Ferns and fern allies were very rare, in contrast to most living Nothofagus-gymnosperm communities. Fossil pollen and spore types produced by uncommon subcanopy tree, shrub and fern species potentially provide a means for more accurately dating the deposit once their time of first occurrence and extinction at subantarctic latitudes in the southwest Atlantic region is established (nearest living equivalents given in parentheses) — Clavatipollenites cf glarius (Hedyosmum), Thymelaepollis sp. (Ovidia-type) and Cyatheacidites annulatus (Lophosoria). This will require palynostratigraphic analysis of Late Palaeogene–Neogene sediments recovered from basins surrounding the Falkland Islands, for example from DSDP Site 329 drilled on the Maurice Ewing Bank at the eastern margin of the Falkland Plateau.     

云南临沧晚中新世邦卖组植物群

云南临沧中寨晚中新世邦卖组植物群总计37科59属71种（含37新种）。其中,蕨类植物仅有1科1属1种（新种）;裸子植物有2科2属2种;被子植物有34科55属67种[其中双子叶植物32科53属65种（含35新种）和单子叶植物2科2属2种];另有分类位置不明的果实1属1种（新种）。这个植物群属于常绿和落叶阔叶混交林植被,它...     

高黎贡山北段种子植物区系研究

高黎贡山北段种子植物种类十分丰富,共记载野生种子植物172科,778属,2514种及302变种(亚种),是植物多样性最为丰富的地区之一。区系成分分析表明:1)本区种子植物区系的性质具有鲜明的温带性,并深受热带植物区系的影响,区系地理成分复杂、联系广泛;2)现代种子植物区系是在古南大陆热带亚洲植物区系的基础上,由古南大陆成分及古北大陆成分在漫长的地质历史过程中融合发展而来,许多源于印度-马来、北温带(特别是东亚)的成分在此都产生了较为丰富的特有类群,它们共同演变成今天的植物区系外貌;3)种子植物区系具有明显的水平和垂直替代现象,间断现象也较为显著,主要表现为滇西北-滇东南间断分布或在此线西南侧连续分布;4)种子植物区系的特有现象十分丰富,物种分化强烈,新老兼备,而以新生的进化成分为主,由此表明高黎贡山北段在保存古老成分的同时,又分化出许多新生成分,它是一个孕育新特有现象的重要舞台。     

Late Pliocene diversity and distribution of Drynaria(Polypodiaceae) in western Yunnan explained by forest vegetation and humid climates

The palaeodiversity of flowering plants in Yunnan has been extensively interpreted from both a molecular and fossil perspective. However, for cryptogamic plants such as ferns, the palaeodiversity remains poorly known. In this study, we describe a new ferny fossil taxon, Drynaria lanpingensis sp. nov. Huang,Su et Zhou(Polypodiaceae), from the late Pliocene of northwestern Yunnan based on fragmentary frond and pinna with in situ spores. The frond is pinnatifid and the pinnae are entirely margined. The sori are arranged in one row on each side of the primary vein. The spores have a semicircular to bean-shaped equatorial view and a tuberculate surface. Taken together with previously described fossils, there are now representatives of three known fossil taxa of Drynaria from the late Pliocene of western Yunnan.These finds suggest that Drynaria diversity was considerable in the region at that time. As Drynaria is a shade-tolerant plant, growing preferably in wet conditions in the understory of forests, its extensive existence may indicate forest vegetation and humid climates in western Yunnan during the late Pliocene.This is in line with results from floristic investigations and palaeoclimatic reconstructions based on fossil floras.     

云南地区种子植物多样性分布格局和多样性分化特点研究

利用大尺度的植物分布信息结合地理信息系统和数理统计分析,探讨了云南种子植物多样性的地理分布格局和多样性分化特点。结果表明,从科到属和种,植物多样性和区系分化强度的数据集离散程度均呈递增趋势。相对属和种而言,科的多样性的空间分异和高值区域并不明显,这可能与科、属、种所代表的不同地质历史时期有关;南部地区属和种的多样性明显高于除滇西北以外的大部分地区。种的多样性分布中心主要集中在滇西北地区、云南南部地区、哀牢山、无量山地区和昆明地区,这可能与生境异质性和热量条件有关。相对科而言,属的区系分化强度的空间分异更为明显,并与物种多样性的分布格局比较接近,暗示着植物多样性与区系分化之间的密切联系。相对科而言,属的区系分化中心高值区域更为明显。总体上,云南地区植物多样性的分布格局及其分化可能与其生境、热量条件和地质历史有关。     

福建梁野山国家级自然保护区种子植物区系研究

通过野外调查、采集标本和查阅相关文献资料,编制福建梁野山自然保护区野生种子植物名录,进行植物区系组成和分布区类型的分析,并将其与周边相邻2个保护区的植物区系进行比较。结果表明:(1)梁野山自然保护区共有野生种子植物154科662属1 498种,种类丰富。(2)区系地理成分以热带分布型为主,其中在科级水平上热带分布型所属科共有85科,占总科数的69.67%;在属级水平上热带性质分布型的属有371属,占总属数的60.82%。但相当数量温带成分的存在,体现了亚热带植物区系的特点。(3)对梁野山保护区与周边相邻的武夷山和南靖南亚热带雨林保护区的植物区系比较发现,梁野山种子植物区系属数的热带属数/温带属数(R/T值,1.66)高于武夷山的R/T值(1.10)而低于南靖南亚热带雨林保护区的R/T值(2.68),梁野山种子植物区系与该相邻2个保护区的相似性系数非常接近,但在区系成分上,梁野山既有与武夷山共有而南靖南亚热带雨林保护区没有分布的温带成分,也有与南靖南亚热带雨林保护区共有而武夷山没有的热带成分,说明梁野山植物区系与其地处武夷山脉南端的地理位置相一致,具有明显的从南亚热带向中亚热带过渡的特点。     

一些东亚特有种子植物的化石历史及其植物地理学意义

特有植物在植物区系地理的研究中有重要意义,不同等级的特有植物往往成为不同等级植物区系分区的重要依据。查明东亚特有植物的地史渊源对于揭示东亚植物区的特征与性质,理解中国植物区系及东亚植物发生和演变都有重要的意义。本文在现有资料的基础上,分析总结了东亚植物区系中有化石记录的银杏科、杜仲科、连香树科、大血藤科和昆栏树科等5个特有科,水杉等21个特有属的化石历史。从这些特有植物化石历史的分析可以发现,东亚植物的特有植物从来源上可以分为北极-第三纪,北热带,和就地起源等3种类型,特有植物的来源表明东亚植物区系是一个来源复杂的植物区系。尽管各种特有类群的地质历史各不相同,但是都经历了从广布到分布区逐步缩小,最后形成特有的过程。大部分特有类群形成特有的时间是在上新世末到第四纪初。根据特有类群划分区系等级的原则,东亚现代植物区系最终形成的时间应该是上新世末到第四纪初。     

Extent and timing of floristic exchange between Australian and Asian rain forests

Aim We tested an entrenched concept – that the Australian rain forest flora is essentially a Gondwanan relict. We also assessed the role of regional‐level source–sink dynamics in the assembly of this flora. Location Eastern Australia. Methods To avoid potential biases inherent in selective studies undertaken to date, we used an analytical, whole‐of‐flora approach integrated with the fossil record. We identified disjunctions between woody Australian rain forest plant taxa and relatives on other land masses. To test the strength of the fossil evidence for the regional antiquity of this flora, we evaluated the proportion of these disjunct clades represented in the Australian fossil record, and to minimize the effects of biases in this record, we compared late Quaternary (i.e. late Pleistocene and Holocene, 126–0 ka), Pliocene and late Oligocene–early Miocene Australian pollen records interpreted as tropical rain forest. Using within‐species disjunctions as a proxy, we assessed the role of recent immigration from Asia into Australia. To assess the role of source–sink dynamics, we performed comparative analyses of disjunctions in major rain forest categories representing a north–south/climatic gradient. Results Southern Australian, cool temperate (microthermal) rain forests contain many floristic disjunctions with Gondwanan fragments and most of these clades have Gondwanan fossils. Disjunct clades in Australian mesothermal rain forest mostly occur in Asia/Malesia and a low proportion of these clades show pre‐Neogene records. Many clades in lowland tropical and ‘dry’ rain forest show disjunctions with Asia/Malesia and few have Australian fossil records. Rates of recent immigration from Asia/Malesia are high in these northern forests, and outweigh rates of recent emigration approximately nine‐fold. The late Quaternary fossil record has many more rain forest angiosperms than Oligocene–Miocene and Pliocene floras, consistent with extensive late Cenozoic immigration. Main conclusions The microthermal rain forests are largely Gondwanan relicts, but there is progressively greater, and more recent contribution from Asia/Malesia into more northern, and more lowland tropical rain forests. This variation reflects a strong gradient in geographic and ecological proximity between these forests and source floras in Asia/Malesia, and is consistent with a source–sink size model of immigration driven by late Cenozoic contractions and expansions of Australian rain forest.     

香港长洲岛野生植物物种多样性与植被的研究

长洲岛共有野生维管植物237种,隶属于73科184属.植被类型以次生常绿阔叶林为主,其次为灌丛群落.植物区系以热带亚热带植物地理成分占优势,热带性质明显.该岛的植物区系与邻近岛屿植物区系具有极大的相似性,在香港植物区系组成中占有一定地位.由于人为活动和外来植物的影响,其植物多样性及植被的保护应引起注意.     

青藏高原特有种子植物区系特征及多样性分布格局

青藏高原拥有丰富的种子植物, 但对该地区特有植物的区系特征以及多样性还鲜有报道。本文通过植物志(书)以及在线数据库, 整理了只分布于青藏高原地区的种子植物名录及其地理分布, 分析了它们的科属特征、区系成分以及多样性空间分布格局。结果表明: 青藏高原共有特有种子植物3,764种, 隶属113科519属, 多数为草本植物(76.3%); 包含100种以上的科有菊科、毛茛科、列当科等15个, 属有马先蒿属(Pedicularis)、杜鹃花属(Rhododendron)、紫堇属(Corydalis)等7个; 从属的区系成分来看, 温带成分占主导(67.5%)。青藏高原特有植物多样性格局呈现从高原东南部向西北部逐渐递减的趋势, 其中东喜马拉雅-横断山脉的物种多样性非常丰富, 而且多数物种分布在高原的中海拔地带。理解青藏高原特有物种的特征及多样性格局对探讨高原植物区系的演化历史和物种保护有重要启示。