中国的石松科植物

本文对国产石松科(狭义)进行了分类学研究,共记载本科植物6属15种3变型。文中引用新建 立的1属,即拟小石松属Pseudolycopodiella Holub,并包含1个新命名：Lycopodium neopungens H．S．Kung et L．B．Zhang,1个新变型：Palhinhaea hainanensis C．Y. Yang f．glabra H．S．Kung et L．B．Zhang和9个新 异名：Lycopodium annotinum L．var．brevifolium Christ(=L ．zonatum),L．annotinum L．var．aciculare Christ (=L．zonatum),L.alticola Ching(=L．zonatum),L．simulans Ching et H．S．Kung ex Ching(=L．japoni- cum),L．interjectum Ching et H．S．Kung ex Ching(=L．japonicum),L. taliense Ching(=L．japonicum),L．pseudoclavatum Ching(：=L．japonicm．),L． pseudoclavatum Ching var．yunnanense Ching(=L．japonicum),及L. centro-chinense Ching(=L. japonicum)．本文还记述了有关分类群的地理分布,并认为中国没有Dipha- siastrum wightianum(Wall．ex Grev．et Hook．)Holub的分布。     

甘肃省被子植物分布新记录

报道了甘肃省分布的玄参科(Scrophulariaceae)水茫草属(Limosella Linn.)1个新记录属,以及玄参科(Scrophulariaceae)、木兰科(Magnoliaceae)、蓼科(Polygonaceae)、胡颓子科(Elaeagnaceae)、百合科(Liliaceae)5个新记录种——水茫草(Limosella aquatica Linn.)、峨眉含笑(Michelia wilsonii Finet et Gagnep.)、叉分蓼(Polygonum divaricatum L.)、棱果沙棘(Hippophae goniocarpa Y.S.Lian et al.ex SwensonBartish)、青海黄精(Polygontum qinghaiense Z.L.Wu et Y.C.Yang)。其中,峨眉含笑是国家二级重点保护野生植物。     

中国(竹思)簩竹属(Schizostachyum Nees)的研究及其它

对国产(竹思)(竹劳)竹属(Schizostachyum Nees)进行了系统整理。对属的范围进行了修订,认为本属应包括乔草竹属(Dendrochloa Parkinson),薄竹属(Leptocanna Chia et H.L.Fung),长穗竹属(Teinostachyum Munro)和李海竹属(Neohouzeaua A.Camus),并首次建立了本属的属下分类系统。此外,对二种竹子起了新名:甲竹(Bambusa austro-sinensis Xia)和毛环单竹(B.yunnanensis Xia);作了4个新组合,即Schizostachyum coradatum(Wen et Dai)Xia, S.dumetorum(Hance)Munro var.xinwuense(Wen et J. Y Chin)Xia, Bambusa glaucescens glaucescens(Willd)Sieb. ex Munro var.annulata(W.T.Lin et Z.J.Feng)Xia和B.glaucescens (Willd)Sieb.ex Munro var.pubivagina(W.T.Lin et Z.J.Feng)Xia.     

中国(竹思)簩竹属(Schizostachyum Nees)的研究及其它

对国产(竹思)(竹劳)竹属(Schizostachyum Nees)进行了系统整理。对属的范围进行了修订,认为本属应包括乔草竹属(Dendrochloa Parkinson),薄竹属(Leptocanna Chia et H.L.Fung),长穗竹属(Teinostachyum Munro)和李海竹属(Neohouzeaua A.Camus),并首次建立了本属的属下分类系统。此外,对二种竹子起了新名:甲竹(Bambusa austro-sinensis Xia)和毛环单竹(B.yunnanensis Xia);作了4个新组合,即Schizostachyum coradatum(Wen et Dai)Xia, S.dumetorum(Hance)Munro var.xinwuense(Wen et J. Y Chin)Xia, Bambusa glaucescens glaucescens(Willd)Sieb. ex Munro var.annulata(W.T.Lin et Z.J.Feng)Xia和B.glaucescens (Willd)Sieb.ex Munro var.pubivagina(W.T....     

秦岭植物分布3新记录属

报道了秦岭植物分布3新记录属:鹿蹄草科(Pyrolaceae)的沙晶兰属(Monotropastrum Andres)、列当科(Orobanchaceae)的藨寄生属(Gleadovia Gamble et Prain)和爵床科(Acanthaceae)的十万错属(Asystasia Blume)。相应的新记录种或变种为无毛沙晶兰[M.humile(D.Don)H.Hara var.glaberrimum H.Hara]、藨寄生(G.ruborum Gamble et Prain)和白接骨[A.neesiana(Wallich)Nees]。     

云南叉蕨属(Tectaria Cav.)的增补与订正

叉蕨属是蕨类植物的大属之一,全世界约150种,分布于世界热带及亚热带地区。据记载,中国 有27种、2变种,分布在长江以南,仅有2种北达长江以北四川境内,而大部分种类集中分布在云南。近 来,笔者主要对保存在中国科学院昆明植物研究所标本室的标本进行了清理,也参考了中国科学院植物 研究所标本馆的标本,这些标本不少是近年来所采集,其中,发现1新种并有1种和1变种为中国新记 录,1种为云南新记录,1种为贵州新记录,有4个种名是新异名,即Tectaria cosimilis Ching et C．H．Wang, T．decurrenti-calata Ching et C．H．Wang,T．fengii Ching et C. H．Wang,T．Simaoensis Ching et C.H．Wang。至此,所知云南产叉蕨属有22种、2变种。     

广东省种子植物分布新资料(三)

报道广东省种子植物分布新记录 5 种,即土佐景天(Sedum tosaense Makino.)、浙江木蓝(Indigofera parkesii Craib)、墙草(Parietaria micrantha Ledeb.)、寻乌阴山荠[Yinshania sinuata subsp. qianwuensis (Y. H. Zhang) Al-Shehbaz et al.]和浙江乳突果[Biondia microcentra (Tsiang) P. T. Li],其中墙草属(Parietaria L.)为新分布属,均发现于广东丹霞山国家级自然保护区。新记录的发现丰富了广东省种子植物种质资源,同时为丹霞山的植物多样性与区系发生研究提供依据。     

中国马尾杉属拟石杉组(新组)的分类研究及马尾杉属的属下分类

1964年J．Holub建立马尾杉属Phlegmariurus(Herter)Holub之后,植物学界有各种不同的反映。 本文在研究中国种类基础上将这个属看作不同于石杉属Huperzia Bernh．的独立的属,其特殊性尤表现 在附生习性和热带分布两方面。本文将该属中国种类划分为三个组,列出其分组检索表。对其中新组 拟石杉组Sect. Huperzioides(sect. nov．)作了分类学研究,共记载了该组植物13种,内含4个新组合： Ph．petiolatus(Clarke)H．S．Kung et L. B．Zhang,Ph．cryptomerianus (Maxim．)Ching,Ph．ovatifolius (Ching)W. M. Chu, Ph. nylamensis (Ching et S. K. Wu)H. S. Kung et L. B. Zhang; 7个新异名: Hu- perzia formoana Holub [ = Ph. taiwanensis Ching], H. austrosinica Ching [ ＝ Ph. petiolatus ], Lycopodi- um minchegense Ching [ = Ph. mincheensis Ching ], Ph. mincheensis var. angustifolius C. Y. Ma [ ＝ Ph. mincheensis ], Ph. longyangensis C. Y. Ma [ = Ph. fordii ], Ph. nanus C. Y. Ma [ = Ph. fordii ], Ph. yangdongensis Ching et C. F. Zhang [ = Ph. fordii ]; 以及1个中国分布新记录种: Ph. hamiltonii。     

中国石杉属(狭义)小杉兰组的分类学研究

本文将石杉科石杉属(狭义)分为两组,即小杉兰组Sect．Huperzia和蛇足石杉组Sect．Serratae (Rothm．)Holub,对小杉兰组的概念进行了修订并对国产有关种类进行了分类学研究。共记载国产小杉 兰组植物12种1变种,并包括1个新组合:Huperzia quasipolytrichoides(Hayata)Ching var. rectifolia (J．F．Cheng)H．S．Kung et L．B．Zhang,2个新异名:H．hupehensis Ching和H．whangshanensisChing et P．C．Chiu．     

西藏十字花科新记录植物

报道了西藏十字花科一新记录属芝麻菜属(Eruca)和一新记录种山西异蕊芥(Dimorphostemon shanxiensis R.L.Guo et T.Y.Cheo).     

Neogene Corylopsis seeds from eastern Tennessee

A new fossil species of Corylopsis (Hamamelidaceae), C. grisea Quirk & Hermsen sp. nov, based on seeds from the early Pliocene Gray Fossil Site (GFS), eastern Tennessee, USA, is described. The assignment of the seeds to Hamamelidaceae, subfamily Hamamelidoideae, is based on the overall size of the seeds, smooth testa, lack of a seed wing, and the presence of a terminal hilar scar. The assignment to the genus Corylopsis is based on seed size as well as the presence of a hilar facet, in addition to the hilar scar. Although Corylopsis persists only in East Asia today, its fossil record indicates that the genus was widespread across the Northern Hemisphere in the past. Prior to its discovery at GFS, Corylopsis was only known from the Paleogene in North America. The presence of C. grisea at GFS extends the fossil record of Corylopsis in North America to the Neogene and reinforces the interpretation of GFS as a forested refugium that provided a relatively moist, equable environment where subtropical to warm temperate plants could persist during a time of cooling and drying in the continental interior of North America. Its presence provides additional evidence for the biogeographic connection between the GFS paleoflora and the modern flora of eastern Asia.     

Fossil Records in the Lythraceae

The Lythraceae (Myrtales) are a family of 28 genera and ca. 600 species constituting with the Combretaceae and sister family Onagraceae a major lineage of the Myrtales and including the former Sonneratiaceae, Duabangaceae, Punicaceae, and Trapaceae. The fossil record of the family is extensive and significant new discoveries have been added to the record in recent years. This review provides a vetted summary of fossils attributed to the Lythraceae, their geographic distributions, and their stratigraphic ranges. It anticipates the use of the information to generate robustly dated molecular phylogenies to accurately reconstruct the evolutionary and biogeographic history of the family. Fossils of 44 genera or form genera have been attributed to the Lythraceae; 24 are accepted here as lythracean. Fourteen of the 28 modern genera have fossil representatives: Adenaria, Crenea, Cuphea, Decodon, Duabanga, Lafoensia, Lagerstroemia, Lawsonia, Lythrum, Pemphis, Punica, Sonneratia, Trapa, and Woodfordia. Ten extinct genera are recognized. The most common kinds of fossil remains are seeds and pollen. The only fossil flower confidently accepted in the family is the extinct genus Sahnianthus from the Early Paleocene of India. The oldest confirmed evidence of the Lythraceae is pollen of Lythrum/Peplis from the Late Cretaceous (early Campanian, 82?81 Ma) of Wyoming. Seeds of Decodon from the late Campanian (73.5 Ma) of northern Mexico are next oldest. Sonneratia, Lagerstroemia, and extinct Sahnianthus first appear in the Paleocene of the Indian subcontinent; extinct Hemitrapa fruits first occur in the Paleocene of northwestern North America. Diversification of the Lythraceae occurred primarily during two major periods of global temperature change, during the Paleocene-Eocene Thermal Maximum and from the middle Miocene forward when temperatures decreased markedly and seasonality and dry-adapted vegetation types became more prominent. Fossils of the Lythraceae from South America and Africa are limited in number. The few dates available for South American genera are comparatively young and diversification of the largest genus, Cuphea (ca. 240 species), was mainly a Quaternary event. A phylogeny of the family is briefly explored and examples of specialized characters occurring in the oldest known genera are noted. The fossil record of the Lythraceae is presently too fragmentary to confidently reconstruct the early history of the family. The record indicates, however, that the family was well-diversified and widely dispersed globally over a wide latitudinal range by the end of the Paleocene.     

The geologic history of the Lythraceae

The known fossil record of the Lythraceae has been amplified by recent studies in northern Latin America. A total of 18 genera is recognized in geologic strata ranging in age from lower Eocene to Recent, and among the 22 or 23 modern genera, seven have a documented geologic history. The oldest remains are from an Indo-Malayan Old World warm-temperate to subtropical vegetation preserved in the lower Eocene London Clay flora. The most ancient of extant genera isLagerstroemia and the most recent (among those with an adequate fossil record) isCuphea (middle Miocene to Recent). These represent, respectively, primitive and advanced members of the family, and the paleobotanical record supports current concepts concerning phylogenetic relationships among genera of the Lythraceae. The family apparently had an Old World origin and became differentiated into a distinct modern taxon during Paleocene and early Eocene time.     

New observations on the tontoniid ciliate Spirotontonia grandis (Suzuki and Han, 2000) Agatha, 2004 (Ciliophora, Oligotrichida, Tontoniidae); comparison with the similar Laboea strobila

Spirotontonia grandis (Suzuki and Han, 2000) Agatha, 2004 belongs to the family Tontoniidae Agatha, 2004 because it has a contractile tail. It is the type of the genus Spirotontonia Agatha, 2004, which is characterized by a sinistrally spiralled girdle kinety. Supplementary observations on protargol-impregnated and, especially, live specimens of S. grandis from the Irish Sea are provided. These new findings are included in an improved species diagnosis. Furthermore, they contribute to a better separation of the tontoniid S. grandis from the strombidiid Laboea strobila, which also has a screw-like appearance, a sinistrally spiralled girdle kinety, and multiple macronuclear nodules, but lacks the tontoniid tail. Since the tail of S. grandis, the main distinguishing feature between the two species, is highly contractile and easily lost, further differences are emphasized, e.g., the lower number of girdle kinety whorls (3.0–3.5 vs. 4.5–5.0), the larger cell size (110–170×55–80 μm vs. 80–110×40–60 μm after protargol impregnation), the relatively larger size of the ventral portion of the membranellar zone (51% vs. 40% of body length), and the overlapping cortical platelets (present vs. absent). The record of S. grandis from the Irish Sea is the first record outside the East China Sea and the second worldwide.     

Palaeopalynological Evidence of Phylogeny in Hamamelidaceae

This paper deals with evolution, classification and pollen morphology of the Hamamelidaceae, an important family in phylogeny of angiosperms. I. Pollen morphology and systematics of modern Hamamelidaceae. The pollen morphology of the family may be divided into the following four types: (1) Tricolpate: Hamamelis, Loropetalum, Mytilaria, Corylopsis, Sysopsis, and Distylum etc.; (2) Tricolpate with operculum: Disanthus; (3) Tricolporate: Rhodoleia; (4) Pantoporate: Liquidambar. The tricolpate pollen of the Hamamelidaceae is a primitive type in angiosperms, but the most ancient type is monocolpate pollen. Therefore, the family might have evolved from the Magnoliaceae of the monocolpate pollen. The pantoporate pollen is an evolutionary type in the family. It might have evolved from the tricolpate pollen. II.The fossil pollen of the Hamamelidaceae 1 .General introduction of the fossil pollen of the family Hamamelidaceae The most’ancient fossil pollen belonging to the family was found in the middle-late Early Cretaceous. Palynologists call the fossil pollen of the Hamamelidaceae Retitricolpites, which consists of three genera: Hamamelis L.,Corylopsis Sieb. et Zucc and Fothergilla Murr. Liquidambar is of an advanced type in the fossil pollen of the Hamamelidaceae. It was found in the period from the Palaeogene to the Neogene in China. 2. The geological history of the Hamamelidaceae may be divided into the following four stages: (A) The Early Cretaceous stage or origination stage. The family may be evolved from Magnoliales in the middle-late Early Cretaceous. (B)the Late Cretaceous stage or formation stage. The family is much developed in the period. (C) The Tertiary stage or development stage. The family was a much developed one among angiosperms. (D)The Neogene to modern stage or perfection stage. The evolutionary type, the Liquidambar type of the Hamamelidaceae, was much developed in the Neogene. III. The palaeopalynological evidence of evolution of the Hamamelidaceae The earliest fossil pollen of angiosperms was found in the Barremian (Early Cretaceous) in England, Israel, the United States of America etc., and was named as Clavatipollenites by Couper (1953). In recent years, Clavatipollenites was also found in the middle-late Early Cretaceous in Nei Monggol and Jiangxi Province of China. We also found Retitricolpites in the middle-late Early Cretaceous in Nei Monggol and Jiangxi Province. Retitricolpites, belonging to the Hamamelidaceae, is a primitive type among angiosperms, but it is younger than Clavatipollenites. Therefore, the pollen of Hamamelidaceae may have evoloved fromClavatipollenites, which may have evoloved in turn from that of Magnoliales.     

武夷山中亚热带常绿阔叶林样地的群落特征

武夷山保存了典型的中亚热带原生性森林生态系统。由于以往研究的空间和时间尺度较小, 方法规范性不强, 该地区尚缺少大型的、规范的综合性观测和研究平台。本文依托环境保护部南京环境科学研究所等单位按照CTFS调查技术规范建立的武夷山中亚热带常绿阔叶林9.6 ha动态监测样地开展植物群落调查, 从物种组成、区系特征、径级结构和空间分布格局等方面分析了其群落特征。结果表明: 样地内有维管植物68科135属232种, 其中乔木层内胸径≥ 1 cm的植物有44科86属171种。热带性质的科和属分别占总科数和总属数的68.58%和58.83%, 热带特征明显。珍稀濒危物种较多, 有4种国家II级重点保护野生植物、2种《中国生物多样性红色名录——高等植物卷》中的“近危”物种、1种《濒危野生动植物种国际贸易公约》(CITES)附录II物种以及72种中国特有物种, 具有较高的保护和研究价值。稀有种29种, 占总树种数的16.96%。重要值最大的科是壳斗科和山茶科, 二者的重要值之和大于40%。米槠(Castanopsis carlesii)、毛锥(C. fordii)、甜槠(C. eyrei)和少叶黄杞(Engelhardtia fenzlii)的重要值较大, 但没有明显的优势种。小径木较多, 所有个体的平均胸径为5.10 cm, 整体径级分布呈倒J形。乔木层可分为两个亚层, 米槠、毛锥、甜槠等在第I亚层中占优势。米槠和毛锥呈均匀分布, 甜槠、少叶黄杞、赤楠(Syzygium buxifolium)和木荷(Schima superba)呈聚集分布。     

The family prosthogonimidae (Trematoda) in Australia

The family Prosthogonimidae (Trematoda) in Australia. International Journal for Parasitology 3: 853–862. The family Prosthogonimidae has previously been known in Australia by three species of Prosthogonimus Lühe, 1899 (from birds) and by Coelomotrema Angel, 1970 (from marsupials). Two new genera are now proposed: Cylindrotrema cygni from Cygnus atratus (Latham) (caecum), and Mawsonotrema eudyptulae from Eudyptula minor (Forster) (liver). Prosthogonimus vitellatus Nicoll, 1914 is recorded from three new hosts, Gymnorhina tibicen leuconota (Latham), Phalacrocorax melanoleucos (Vieillot) and Chlidonias hybrida (Pallas), and the species is redescribed from 11 specimens from the first of these. The life history, not known for any Australian species, is discussed.

The only plump-bodied genera in the family are Coelomotrema, Cylindrotrema and Mawsonotrema, all of which are confined to Australia.

Mawsonotrema differs from all other members of the family in the position of the genital pore, which is away from the anterior end of the body, lying against the anterior border of the acetabulum.     

PALYNOLOGY AND SYSTEMATICS OF THE LYTHRACEAE. III. GENERA PHYSOCALYMMA THROUGH WOODFORDIA,ADDENDA, AND CONCLUSIONS

Pollen of the 27 genera presently recognized as comprising the family Lythraceae have been surveyed with light microscopy and scanning and transmission electron microscopy. Results for five genera (Physocalymma, Pleurophora, Rotala, Tetrataxis, Woodfordia), in addition to Duabanga, Sonneratia, and Punica (assigned to the Lythraceae in some classifications), are presented here; the remaining genera were treated previously in the series. The family is revealed as the most diverse palynologically of the order Myrtales. The most simple pollen type and the one common to the largest number of genera is prolate-spheroidal to prolate; tricolporate, without pseudocolpi; psilate, scabrate or finely verrucate; and 16–28 μm or less in length. Specializations include oblate grains, development of pseudocolpi (three or six in number), diversification of exine sculpturing, broadening of the colpal and pseudocolpal areas, and reduction in the conspicuousness of the colpi. Pollen evidence provides qualified support for inclusion of Punica in the Lythraceae, the generalized nature of the pollen tempering the conclusion, and little support for inclusion of Sonneratia and Duabanga in the family. Completion of the survey provides a data base of pollen characters that will be integrated in future studies with other evidence into an overall phenetic and cladistic assessment of the family leading to production of a more natural classification.     

The diversification of the northern temperate woody flora – A case study of the Elm family (Ulmaceae) based on phylogenomic and paleobotanical evidence

Ulmaceae is a woody family widespread in northern temperate forests. Despite the ecological importance of this family, its phylogeny and biogeographic history are poorly understood. In this study, we reconstruct phylogenetic relationships within the family and infer spatio-temporal diversification patterns based on chloroplast genome (complete cpDNA) and nuclear ribosomal DNA sequences (nrDNA). The seven Ulmaceae genera are resolved in two main clades (temperate vs. tropical) by both cpDNA and nrDNA sequences. The temperate clade includes four genera, Hemiptelea, Zelkova, Planera, and Ulmus. The relationships among Planera and other genera are controversial because of inconsistent topologies between plastid and nuclear data. The tropical clade includes three genera ((Ampelocera, Phyllostylon), Holoptelea). Molecular dating and diversification analyses show that Ulmaceae originated in the Early Cretaceous (ca. 110–125 Ma) with the main lineages establishing from the Late Cretaceous to the early Eocene. The diversification rate slowed during the middle to the late Paleogene (ca. 23–45 Ma), followed by a rapid diversification of the East Asian temperate group in the Neogene, congruent with a global cooling event. The ancestral state optimization analysis suggests an East Asian origin of the temperate Ulmaceae clade during the Paleocene, which is consistent with the fossil record. Both phylogenomic and fossil evidence support East Asia as a center of origin and diversification for the temperate woody lineages.     

A Revaluation of the Systematic Positions of the Cercidiphyllaceae and Daphniphyllaceae Based on rbcL Gene Sequence Analysis,with Reference to the Relationship in the “Lower” Hamamelidae

The rbcL gene sequences of six species representing five subfamilies of the Hamamelidaceae and the Platanaceae were determined and used in the phylogenetic analysis on the “lower” Hamamelidae sensu Endress (1989) and its allies newly suggested. Four most parsimonious trees were obtained, all having 893 steps with CI = 0.558 and RI = 0.591. The families Cercidiphyllaceae, Daphniphyllaceae, Hamamelidaceae and Saxifragaceae are closely located, while the relationships among them remain unsolved even if more representatives of the Hamamelidaceae were further added in this parsimony analysis. Our results confirm the phylogenetic trees revealed by Chase et al. (1993) and Soltis et al. (1997), instead of those of Hoot and Crane (1996). Considering the morphological features they share, it is suggested that the Cercidiphyllaceae and Daphniphyllaceae be placed into the Hamamelidales. The relationship between the Platanaceae and the Hamamelidaceae shown in our analysis is not so closed as suggested by the cladistic analyses by using morphological characters only(e.g. Lu et al., 1991), while those among the Platanaceae, Trochodendraceae and Tetracentraceae are close as indicated by this study. The Eupteleaceae falls into the Ranunculales. The Eucommiaceae seems to show closer relationship with the Hamamelidaceae, the “core” family of the “lower” Hamamelidae, than with the other members except the Cercidiphyllaceae. The rbcL gene trees imply that the “lower” Hamamelidae is a heterogeneous group,composed of isolated ancient families.