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。     

从花粉形态特征试论壳斗科的系统分类及其演化

本文通过采用光学显微镜、扫描电镜、透射电镜对中国壳斗科,包括三个亚科、6属、103种植物的花粉形态,做了较全面的研究,认为壳斗科植物花粉分为四个类型,分别归于三个亚科。根据花粉形态特征笔者支持将Cyclobalanopsis作为 Quercus的亚属处理,并对三棱栎的分类位置及壳斗科各属的亲缘关系及演化进行了讨论。     

地质时期樟科植物花化石及其系统演化意义

该研究对地质时期樟科植物花化石的主要类群,即Androglandula、Lauranthus、Mauldinia、Neusenia、Perseanthus和Potomacanthus属分别从属和种的形态特征、分布、地层以及系统意义进行了论述,并结合现代樟科植物从地层和分布、花序类型、花部形态特征和显微构造特征进行了分析。结果表明:(1)樟科植物在中晚白垩纪期,已经起源于劳亚古陆的中纬度区域。(2)樟科植物的花序类型为Mauldinia属的侧生花序类型和假伞形花序类型。(3)花为3基数的两性花,花被片6枚排列为2轮,雄蕊12或6,排列为4、3或2轮,最内轮雄蕊不育,第三轮雄蕊基部常见一对附属腺体,雄蕊药室瓣裂,4或2药室,雌蕊为单心皮。(4)花被片上常有大量的油细胞、并列型气孔器和单细胞毛。该研究结果中樟科花化石的发现,为樟科植物的系统演化提供了古生物学的证据和资料。     

壳斗演化的假说及分子系统学和化石证据

壳斗作为壳斗科Fagaceae的重要特征, 其起源、演化和多样性形成长期以来为系统学家们所关注, 有众多的观点和假说。本文在综合这些假说的基础上, 结合分子系统学和大化石证据, 讨论了壳斗演化的规律。研究结果支持壳斗具枝性性质, 来源于二歧聚伞花序最外侧小枝的假说。在比较3个壳斗演化模型的基础上, 根据4种分子系统关系的一致性重建了壳斗的演化历史: 壳斗是单系起源; 水青冈属的2果4裂瓣壳斗是最早分化的壳斗类型, 三棱栎型壳斗是较晚分化的类型; 并支持具有内裂瓣的金鳞果类型壳斗可能与其他横切面为圆形的壳斗有较近的共同祖先。这一结果也得到了多个大化石证据的支持。壳斗科多个分子系统关系的一致性和壳斗化石证据共同证实了壳斗演化的规律是从开裂向裂瓣融合、逐步简化、多向发展; 支持开裂壳斗、坚果三角形、较小、具棱或狭翅是祖征, 融合壳斗、坚果圆形、较大、不具棱是衍征。这些结果为进一步探索壳斗科的演化历史和系统发育提供了新的证据。     

中国东属植物花粉形态及其系统学意义

从系统学分类学的角度出发,对国产栎属31个种的花粉进行了光学显微镜和扫描电镜观察。研究结果表明栎属的花粉萌发孔对该属的系统与分类无太大的参考价值;但栎属的花粉纹饰有颗粒状,聚粒状两种主要类型,具有重要的系统学分类学价值。花粉形态的研究结果支持将栎属植物划分为常绿类与落叶类的观点,栎属巴东栎组植物的花粉纹饰在种间存在分化,花粉形态的研究结果支持将巴东栎组至少划分为两个不同类群的观点;在佐以其他证据的情况下,栎属植物的花粉纹饰还具有重要的分类学价值。     

中国栎属植物花粉形态及其系统学意义

从系统学分类学的角度出发 ,对国产栎属 31个种的花粉进行了光学显微镜和扫描电镜观察。研究结果表明栎属的花粉萌发孔对该属的系统与分类无太大的参考价值 ;但栎属的花粉纹饰有颗粒状、聚颗粒状两种主要类型 ,具有重要的系统学分类学价值。花粉形态的研究结果支持将栎属植物划分为常绿类与落叶类的观点 ;栎属巴东栎组植物的花粉纹饰在种间存在分化 ,花粉形态的研究结果支持将巴东栎组至少划分为两个不同类群的观点 ;在佐以其他证据的情况下 ,栎属植物的花粉纹饰还具有重要的分类学价值     

主成分分析法在壳斗科植物化石鉴定中的应用*

壳斗科化石是北半球新生代地层的优势分子,然而由于其属种众多,叶片属种间特异性不明显,该科叶片化石的鉴定是古植物学研究的难点之一。面对化石标本不完整的性状特征信息,如何剔除冗余特征,重点考虑具有鉴定意义的标本特征,就显得非常必要。本研究通过调研多种降维算法,考虑到植物特征编码及赋值的数值特性,选用主成分分析法,以壳斗科青冈亚属植物叶片为例,对可能在化石叶片上观察到的22个性状特征(变量)进行降维处理,挑选出对于壳斗科化石叶片分类鉴定起主要作用的10个性状特征,并将其应用于化石鉴定进行验证。结果表明,仅考虑经过主成分分析法压缩挑选的10个主要性状特征,仍然能够实现壳斗科化石植物的准确鉴定。主成分分析法应用于壳斗科性状特征的降维处理效果良好,剔除冗余特征对标本鉴定结果没有影响。     

金缕梅科:地理分布、化石历史和起源

本文利用系统发育与地理分布相结合的方法,探讨金缕梅科各属植物的系统位置和分布式样,并结合化石、古地理及古气候等证据,讨论该科的分布中心,可能的起源时间和地点以及现代分布式样形成的原因。研究结果表明：全世界金缕梅科植物共30属144种,间断分布于亚洲西部、东部、东南部,非洲东部、南部,大洋洲的澳大利亚东北部以及中美洲和北美洲的东南部,欧洲和南美洲尚无现代类群分布的记载。它基本上是一个热带和亚热带山地分布的科。通过对该科30个属的系统位置及其分布式样的分析,将金缕梅科属的分布归纳为：A．热带分布类型(18属),包括(1)热带亚洲分布(11属),(2)热带中美洲分布(2属),(3)热带非洲分布(2属),(4)热带大洋洲分布(3属),B．温带分布类型(12属),包括(5)东亚分布(7属),(6)西亚分布(2属),(7)西亚-东亚-北美间断分布(1属),(8)东亚-北美间断分布(1属),(9)北美分布(1属)。东亚区南部到印度支那区北部(即中国长江以南至中南半岛北部地区)是它的现代分布区中心;根据化石证据、原始类型分布和外类群分布分析,提出该科植物起源于劳亚古陆,并曾经有一个很长的白垩纪历史,至少在早白垩纪金缕梅科植物的先驱就已经出现。最后,从地质和气候的变迁等方面探讨了金缕梅科现代分布区形成的原因。     

壳斗科植物的化学成分及生物活性研究进展

本文综述了1970年以来壳斗科植物的化学成分及生物活性的研究进展。     

On the Middle Miocene avifauna of Maboko Island,Kenya

The Middle Miocene sediments of Maboko Island (Lake Victoria) in western Kenya yielded numerous avian bones, which remained, however, little studied. The significance of this material is shown by the recent identification of an opisthocomiform bird. In the present study, further avian remains from Maboko Island are described. Most of the specimens belong to aquatic or semi-aquatic groups, of which some are closely related to taxa known from Early and Middle Miocene European avifaunas, that is, Nectornis cormorants (N. africanus nov. sp.) and Laricola-like Laromorphae. The fossil material also includes Ciconiidae (cf. Ciconia), Pelecanidae, Phoenicopteridae (Leakeyornis aethiopicus), Musophagidae, and a species of Ardeidae, which closely resembles the taxon Pikaihao from the Early Miocene of New Zealand. Some avian remains from Maboko Island belong to higher-level taxa unknown from the Middle Miocene of Europe. The occurrence of a giant Jacanidae (?Nupharanassa mabokoensis nov. sp.) is of particular interest, because these are globally absent in extant avifaunas and were previously only known from the Late Eocene/Early Oligocene of Egypt. Further unknown from contemporaneous European sites are small representatives of Jacanidae, Bucerotidae, and Alcedinidae, with the fossils of the latter two taxa being among the earliest published records of their respective groups. Several of the taxa that are common in contemporaneous European avifaunas have not been found in Maboko, and in spite of less pronounced climatic differences, Middle Miocene Afrotropical avifaunas already appear to have been distinct from contemporaneous European ones.     

A phylogenetic analysis of the major groups of catfishes (Teleostei: Siluriformes) using rag1 and rag2 nuclear gene sequences

Higher-level relationships among catfishes were investigated by parsimony, maximum likelihood and Bayesian analyses of two nuclear genes across 110 catfish species representing 36 of 37 families and Conorhynchos (family incertae sedis). Analysis of 3660 aligned base pairs from the rag1 and rag2 genes confirms monophyly of Siluriformes, of most siluriform families and of a number of multifamily groups, some recognized, some novel. South American Loricarioidei are recovered as the sistergroup to other catfishes which are divided into Diplomystidae and Siluroidei. This result contrasts with the prevailing hypothesis that Diplomystidae is the sister to all other catfishes. Monophyly of Siluroidei is supported by rag data including a unique three-codon deletion from rag1. Deep within Siluroidei are 12 large, strongly supported groups with poorly resolved interrelationships. Five are single families: Cetopsidae, Plotosidae, Chacidae, Siluridae and Pangasiidae. Four others are monophyletic taxa ranked here as superfamilies: Clarioidea (Clariidae, Heteropneustidae), Arioidea (Ariidae, Anchariidae), Pimelodoidea (Pimelodidae, Pseudopimelodidae, Heptapteridae, Conorhynchos), Ictaluroidea (Ictaluridae, Cranoglanididae). South American Doradoidea (Doradidae, Auchenipteridae) and Aspredinidae are a sistergroup pair. Sisoroidea (without Aspredinidae), Ailia+Laides, Horabagridae, and Bagridae (without Rita) form a large, predominantly Asian clade, "Big Asia." Mochokidae, Malapteruridae, Amphiliidae, Claroteidae, and African schilbids are united as a species-rich African clade, "Big Africa." The three large continental clades, "Big Asia," "Big Africa" and Neotropical Loricarioidei suggest a prevalence of intracontinental diversification of catfishes. South America is the home of the Gymnotiformes, putative sistergroup of catfishes, plus two of the deepest siluriform clades, Loricarioidei and Diplomystidae, thus suggesting an ancient siluriform presence if not origin there. The rag phylogeny does not identify any African-South American catfish clade. The well-known African-Asian relationships within families Clariidae and Bagridae are confirmed, as is the recently found North American-Asian relationship between Ictaluridae and Cranoglanididae.     

竹亚科系统学和生物地理学研究进展及存在的问题

对近年来在竹亚科作为一个单系类群的界定、其系统位置的确定、内部系统演化趋势以及地理分布和起源方面研究所取得的进展进行了评述。竹亚科作为一个单系类群仅包括了木本的竹族（Bambuseae)和一个草本的莪利竹族（Olyreae),其中莪利竹族分布在新几内亚的伊里安竹（Buergersiochloa)处于Olyreae最基部。禾本科12个亚科中除了3个亚科为基部类群以外,其余9个亚科分成PACCAD（包括黍亚科,狭义的芦竹亚科,广义的虎尾草亚科,假淡竹叶亚科,三芒草亚科和扁芒草亚科）和BOP单系分支（包括竹亚科,稻亚科和早熟禾亚科）。在BOP支中,竹亚科与早熟禾亚科相近缘,共同组成稻亚科的姐妹群。竹亚科分成草本和木本两个单系类群,木本竹子又分成热带和温带支系,热带支系进一步分成新世界热带和旧世界热带两个单系类群。从现有的化石证据和基部类群的地理分布推断,竹亚科很可能起源于晚白垩纪的冈瓦纳古陆。最后,本文就竹亚科研究尚存在的问题做了初步探讨。     

Trois nouvelles especes du genre mixtacandona (ostracoda,cyprididae, candoninae)

The authors describe Mixtacandona elegans n. sp.,M. pietrosanii n. sp., M. tabacarui n. sp. and present new data on the systematics and biogeography of the following Mixtacandona groups: ljovuschkini,hvarensis and riongessa. Mixtacandona elegans n. sp. belongs to the group ljovuschkini. The carapace is very elongated and has markedly assymetrical valves. The species has been found in a porous aquifer in southeastern Bulgaria. M. pietrosanii n. sp. belongs to the group hvarensis. The 3rd antennular segment and the 2nd endopodial segment of the cleaning leg have each two setae. The species lives in porous aquifers in the Danube plain in Roumania. M. tabacarui n. sp. (gr. riongessa) has a triangular left valve with a pointed dorsal protuberance. The species has been found in wells fed by karstic water in southern dobrodgea (Roumania), on the Black Sea coast.     

木兰科的化石记录

通过整理和分析木兰科植物的化石记录发现：不论是植物大化石还是花粉,迄今为止在白垩纪以前地层中尚无可靠的记录,自白垩纪以来,木兰科的许多种广泛发生于北半球,如亚洲,欧洲及北美等地,但非洲和大洋洲至今尚未发现木兰科的化石记录。该科最早的化石记录为中国东北延吉地区早白垩世大拉子组的喙柱始木兰Archimagnolia rostrato-stylose Tao et Zhang. 根据现有化石记录,并结合木兰科现代植物的地理分布,推测：1）木兰科的起源时间不迟于早白垩世Aptian-Albian期;2）木兰科起源地点可能是东亚,后来经过欧洲进入北美,再从北美迁移到达南美洲;3）在地质历史时期,木兰属的出现比鹅掌楸属早,从而支持根据形态学与分子系统学研究得出的木兰属较鹅掌楸属原始的结论。     

木兰科的化石记录

通过整理和分析木兰科植物的化石记录发现：不论是植物大化石还是花粉,迄今为止在白垩纪以前地层中尚无可靠的记录,自白垩纪以来,木兰科的许多种广泛发生于北半球,如亚洲,欧洲及北美等地,但非洲和大洋洲至今尚未发现木兰科的化石记录。该科最早的化石记录为中国东北延吉地区早白垩世大拉子组的喙柱始木兰Archimagnolia rostrato-stylose Tao et Zhang. 根据现有化石记录,并结合木兰科现代植物的地理分布,推测：1）木兰科的起源时间不迟于早白垩世Aptian-Albian期;2）木兰科起源地点可能是东亚,后来经过欧洲进入北美,再从北美迁移到达南美洲;3）在地质历史时期,木兰属的出现比鹅掌楸属早,从而支持根据形态学与分子系统学研究得出的木兰属较鹅掌楸属原始的结论。     

New material of Pleistocene cats (Carnivora, Felidae) from Southern South America, with comments on biogeography and the fossil record

In this paper the systematic position and age of several Pleistocene cat remains found in southern South American are studied, in an attempt to more fully document the scarce record of the group and clear up their obscure Quaternary history. The fossils are compared with a large sample of recent specimens by means of qualitative and quantitative characters, as well as multivariate methods (discriminant analysis). The age of previous records is restricted using recent chronostratigraphic and biostratigraphic studies. Ly. colocolo is recorded in the late Ensenadan (0.78-0.5 Ma BP) and Bonaerian/Lujanian (0.5 Ma-8.5 Ka BP) ages of the Pampean Region (Argentina) and in the late Pleistocene or Holocene of Tierra del Fuego (Chile). An incomplete hemimandible found in the Bonaerian of the Pampean Region is referred to cf. Herpailurus and could be the earliest record of this lineage. Two other remains could belong to On. geoffroyi, but their incompleteness and some differences prevent their assignation to this recent species. The age of “Felis” vorohuensis is restricted to the late Ensenadan. The fossil record of the Ocelot Lineage is very fragmentary, but it is at least as old as late Ensenadan. Taphonomic biases are responsible for this poor fossil record and this fact could partially explain the hiatus with respect to the timing estimated by molecular divergence. The combination of data suggests that Ly. colocolo, On. guigna, On. geoffroyi and Oreailurus jacobita speciated in South America, supporting previous opinions. If the molecular divergence dates are right the recent diversity of this group could be explained by a minimum of five to six immigrations.     

基于细胞核rDNA ITS片段的水青冈属的分子系统发育

对山毛榉科水青冈属6种、1亚种、1栽培变种的ITS区片段进行了测序和分析,并对其中2个具有ITS序列多态性的分类群进行了ITS区克隆。水青冈属ITS系统发育树聚成两支,位于基部的是分布于北美的大叶水青冈,另一分支则包括了欧洲和东亚的类群。在欧洲和东亚分支中,又包括两支,其中日本北部的波叶水青冈位于基部,台湾水青冈和欧亚大陆的水青冈形成另外一支。ITS区分析与现行的水青冈属基于形态学性状的属下分类系统有一定差异,而与本属现存物种的地理分布格局较为一致。各类群间TIS区序列差异较小,显示属内现存物种的分化时间不是太长。     

Genetic and morphologic variation of the Pecos assiminea,an endangered mollusk of the Rio Grande region,United States and Mexico (Caenogastropoda: Rissooidea: Assimineidae)

Assiminea pecos is an endangered species of amphibious gastropod that occupies four widely separated portions of the Rio Grande region in the southwestern United States (Pecos River basin) and northeastern Mexico (Cuatro Cienegas basin). Our statistical and discriminant function analyses of shell variation among the disjunct populations of this species indicate that Mexican specimens differ in their morphometry from those of the United States and can be diagnosed by several characters. We also analyzed variation in the mitochondrial genome by sequencing 658 bp of mitochondrial COI from populations of A. pecos, representatives of the other three North American species of Assiminea, and several outgroups. Our results indicated substantial divergence of the Mexican population of A. pecos, which was consistently depicted as a monophyletic unit nested within or sister to the shallowly structured group comprised of American members of this species. Consistent with our findings, we describe the Mexican population as a new species, which is provisionally placed in the large, worldwide genus Assiminea pending further study of the phylogentic relationships of the North American assimineids. Our molecular data suggest that the Rio Grande region assimineids, which are among the few inland members of the otherwise estuarine subfamily Assimineinae, diverged from coastal progenitors in the late Miocene, with subsequent Pleistocene vicariance of Mexican and American species perhaps associated with development of the modern, lower course of the Rio Grande. Handling editor: K. Martens