三棱栎的幼苗形态解剖及系统位置

对三棱栎幼苗的形态和解剖学研究表明,三棱栎幼苗与壳斗科其它属区别明显,并与水青冈属及南水青冈属较为接近,而与栎属关系甚远,最后提出了三棱栎属与水青冈属,南水青冈属共同组成水青冈亚科,为壳斗科中较原始的类群。     

中国壳斗科栎亚科花粉形态研究

本文应用光学显微镜与扫描电子显微镜观察了壳斗科所属栎亚科2属26种2变种的花粉形态,并以本科其它属一些代表种作对比,试图从孢粉学方面为栎亚科的系统分类提供依据。 花粉外壁纹饰在扫描电镜下可分三种类型,即水青冈型(含水青冈属),栎型(含栎属和三棱栎属),栗型(含栗属、锥属和柯属),花粉的类型与植物形态分类的三个亚科一致。 栎亚科的花粉外壁纹饰在扫描电镜下为颗粒聚集成的种种形状。栎属可区分为四种类型,即颗粒状、颗粒——蠕虫状、聚颗粒及芽孢状,其中类型一、二、三为常绿种类,类型四为落叶种类。花粉纹饰在常绿与落叶种类之间有较明显的差异,而青冈亚属和栎亚属之间却没有界线。因此,栎属仍以包含两个亚属为宜。三棱栎属花粉纹饰则介于栎属的类型二与三之间。     

论山毛榉科植物的系统发育

本文运用分支分类学方法,对山毛榉科植物进行了系统发育的分析。山毛榉科作为单元发生群包括柯属、锥属、粟属、三棱栎属、水青冈属和栎属。桦木科和南山毛榉属被选择作为外类群。对大量的性状进行评估之后,选择了25对性状作为建立数据矩阵的基本资料。性状极化以外类群比较为主,同时也采用了化石证据和通行的形态演化的基本原则。数据矩阵由7个分类群、2个外类群和25个性状组成。采用最大同步法、演化极端结合法和综合分析法对该数据矩阵进行了分析。在得到的3个树状分支图中按照最简约的原则,选出演化长度最短的谱系分支图作为本文讨论山毛榉科属间的系统演化关系的基础。关于山毛榉科植物的系统发育,作者的观点如下：(A)现存的山毛榉科的6个属形成了4条平行进化的分支路线,它们分别被处理作4个亚科,即：栗亚科,三棱栎亚科,水青冈亚科和栎亚科;(B)平行进化是山毛榉科植物系统发育过程中的主要形式。生殖过程中的一些特征,如：果实第二年成熟,胚珠通常败育等,是影响山毛榉科植物属间基因交流的主要原因。在现存的山毛榉科植物中,柯属是最原始的类群。三棱栎属和锥属的起源也较早,而栗属、水青冈属和栎属是特化的类群。     

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。     

壳斗科原始植物轮叶三棱栎在云南西双版纳的发现及其生物地理意义

于云南西双版纳发现了壳斗科植物的原始类群——轮叶三棱栎（Trigonobalanus verticillata Forman）。轮叶三棱栎被认为是栎属（Quercus L.）和水青冈属（Fagus L.）植物的祖先之一,原纪录分布于印度尼西亚和马来西亚,后来在我国海南岛被发现,其分布格局的形成一直未能合理解释。本次在云南新发现轮叶三棱栎,不仅可以解释它在海南岛的分布,也为海南岛历史上可能曾经连接着越南北部和广西西南部的假设提供了科学支持,具有重要的科研价值和生物地理学意义。     

中国栎属(壳斗科)基于叶表皮及叶结构特征的分支分析

以三棱栎为外类群,基于叶表皮及叶结构特征对中国栎属进行初步的分支分析,结果显示了栎属内稳定的“支”结构及其种间关系。栎亚属可划分为5个组,分别为巴东栎组,高山栎组,Jiang子栎组,麻栎组和槲栎组,Jiang子栎组是栎亚属常绿栎类与落叶栎类之间的过渡类群;高山栎组应为栎亚属常绿栎类中的特化类群,而非最原始类群,5个组中,仅巴东栎组不是单系类群,而是一个多系类群,青冈亚属较栎亚属早分支,可划分为3大类;无毛类,简单被毛类和复杂被毛类;无毛类最原始,复杂被毛类与栎亚属关系最近,因此,叶表皮及叶结构特征对解决栎亚属组间亲缘关系有重要的分类学意义。     

姜科植物地理

本文讨论了姜科的分类系统、起源、进化和地理分布．姜科为一还热带分布科,按Ｂｕｒｔｔ［８］的系统分２亚科４族．全世界有５２属,约１３７７种,其中姜亚科含４８属,１２６８种．主要分布于热带亚洲．其现代分布中心在印度－马来西亚。闭鞘姜亚科含４属,１０９种,主要分布于热带美洲及非洲。本文在化石资料及现代分布资料的基础上,讨论了姜科的早期分化时间、地点及现代分布格局形成。化石记录表明．欧洲、北美及印度的白垩纪、早第三纪均发现过姜科的化石,据此姜科植物的起源时间应不晚于早白垩纪。姜亚科的早期分化中心推论在劳亚古陆的南部．欧洲和北美没有现代姜科的分布是因为第三纪冰期的影响．而亚洲热带地区现代姜科植物繁盛是因为气候适宜．且相对稳定所致．南美的姜亚科种类应是由非洲传人．而大洋洲的姜亚科种类则是由马来西亚传入．闭鞘姜亚科的早期分化中心推论在西冈瓦纳古陆．亚洲及大洋洲的闭鞘姜亚科的种类应是随印度板块飘向亚洲时传入。中国姜科植物有２２属．２０９种（占全世界属的４２％．种的１５％）．主要分布于马来西亚亚区（占全国属的９０％）．其次为中国喜马拉雅亚区（占全国属的６８％）。最少为中国－日本亚区（占全国属的４５％）。统计数字表明．马来西亚     

北温带水青冈属的间断分布及其泛生物地理学解释

水青冈属(Fagus L.)在北温带呈间断分布, 已发现的丰富的第三纪化石为讨论其起源和演化提供了证据。该文采用泛生物地理学的轨迹分析方法对水青冈属的分布进行了研究, 试图分析水青冈属的分布格局, 进而讨论其进化问题。结果表明, 水青冈属在中国、日本、北美、欧洲的分布是完全间断的, 没有一个共有轨迹连接它们, 即使在毗邻的、且有植物亲缘关系的中国和日本, 也没有一个共有轨迹连接。完全间断的轨迹对分析水青冈属的起源、演化和扩散学说, 没有提供任何信息。仅有两条共有轨迹分别分布在中国东南部和日本, 分别代表了中国4种和日本3种水青冈属种类的连接, 说明水青冈属经历了漫长的历史演化, 扩散能力是有局限性的, 仅在分化和多样性中心进行了一些分化和演化, 整个属并未进行长距离的扩散, 或者长距离扩散早已销声匿迹了, 现代的分布格局完全是以间断为最主要特征的。间断分布的动力解释为古地中海西撤、青藏高原隆起、东亚季风活动等地质历史事件, 第三纪以来特别是第四纪冰期活动等气候波动, 以及水青冈属植物的生物学特性(特别是喜温喜湿)。     

中国壳斗科植物属的空间多样性及差异

该文采用地理信息系统技术,以县为空间数据的基本单元,以壳斗科植物为研究对象,制作属的空间分布图,计算空间相似性系数,分析壳斗科各属的空间多样性及其差异。结果表明,三棱栎属为连续分布,与其他属的空间分布最不相似,其他属均为间断分布,其中锥属、青冈属、柯属空间分布最相似,这3个属的多样化中心均有云南南部,水青冈的多样化中心比前3个属偏北,栎属多样化中心是四川西南部和云南西北部,西北地区东南部是联系南方与北方栎属植物的重要通道。     

槲栎叶复合群及其地史学和系统学意义

根据槲栎叶复合群研究的最新成果订正了国产槲叶栎属 (Dryophyllum)的化石。通过对该属 9种化石的整理 ,将 Dryophyllum dewalquei、D.parvum、D.relongtanense、D.yunnanensis和 D.sp.等 5种分别归入 Berryophyllum dewalquei、B.parvum、B.relongtanense、B.yunnanensis和 B.sp.;将 D.fushunense归入 Castaneophyllum fushunense;将 D.nervosaum归入 Quercusnervosum;将 D.relongtanense的一部分归入Q.lantenoisii;D.subfalcatum尚不能确定归属 ,但可以肯定不属槲栎叶复合群。同时 ,还讨论了槲栎叶复合群的地史学意义。该复合群是原始壳斗科向现代壳斗科过渡的中间类群 ,壳斗科各现代属出现的时间不早于古新世     

Fossils of the Fagaceae and their implications in systematics and biogeography

The fossil history of the Fagaceae from China and its systematic and biogeographic implications are discussed based on revisionary studies of the fossil records. No creditable macrofossil record of the Fagaceae exists in the Cretaceous deposits and all the Cretaceous microfossil reports remain equivocal and require further study. The Paleocene fossils show the appearance and diversification of the two groups corresponding to the subfamilies Fagoideae and Castaneoideae sensu Nixon. By the Eocene, all modern genera had been present. The oldest fagaceous fossils represent subfamily Fagoideae with affinities to the extant genus Trigonobalanus. The leaf fossil genus Berryophyllum, with affinities to Quercus subg. Cyclobalanopsis, has been documented by the early Eocene and might have occurred earlier than other fossils assignable to Quercus. The appearance of evergreen sclerophyllous Ouercus with entire leaves might have occurred earlier than those with toothed leaves. Deciduous, urticoid-leaved oak fossils (Quercus subg. Quercus sect. Quercus) had not appeared until the Miocene. Fossil equivalents of Trigonobalanus, Castanopsis and Lithocarpus had occurred in Europe and North America by the early Tertiary, suggesting that continuous distributions were achieved via the northern hemisphere land bridges. Three groups of evergreen sclerophyllous oaks of apparent close phylogenetic relationships occurred in the Hengduan mountains, the Mediterranean area and northwestern North America. Their fossil forms have become dominant elements of those vegetation zones since the Miocene. A shared fossil history indicates a possible biogeographic boundary formed by the ancient Mediterranean. The evidence suggests that the oaks might arrive in North America during two distinct geologic periods: evergreen sclerophyllous entire-leaved oaks appeared by the Early Tertiary, whereas thedeciduous oaks with urticoid leaves appeared in the Late Tertiary.     

EXTINCT TRANSITIONAL FAGACEAE FROM THE OLIGOCENE AND THEIR PHYLOGENETIC IMPLICATIONS

Fruits, catkins, and associated leaves of at least two extinct trigonobalanoid taxa have been discovered at an Oligocene fossil plant locality rich in fagaceous remains. These fossils exhibit a mosaic of fruit and pollen characters found in the two extant subfamilies Castaneoideae and Fagoideae of Fagaceae. Comparison with cladograms based on modern taxa suggests that these extinct taxa were similar to the ancestors of subfamily Fagoideae and may have been intermediate between Fagus and the modern trigonobalanoid genera. Pollen types isolated from the fossil staminate catkins provide unique character states that are transitional between modern pollen types in Fagaceae and are important in understanding the evolution of exine micromorphology within the family. This analysis provides a striking example of the use of character data from fossils to determine character-state adjacency prior to polarization of characters using outgroup comparison. Because of the mosaic nature of their character complexes, these fossils support monophyly in both the family Fagaceae and the subfamily Fagoideae. In addition, the occurrence of trigonobalanoid fossils in the Oligocene of North America has interesting biogeographic implications and provides insights into the nature of North American Fagaceae during the Tertiary.     

An early Oligocene fossil acorn,associated leaves and pollen of the ring‐cupped oaks (Quercus subg. Cyclobalanopsis) from Maoming Basin,South China

The ring‐cupped oaks (Quercus subg. Cyclobalanopsis) characterized by united and concentric ring‐cupped acorns, are mainly distributed in broad‐leaved evergreen forests in tropical and subtropical regions of East and Southeast Asia. Their geological history has been traced from the middle Eocene to Pleistocene. Most reports of the subgenus have been on the basis of leaves, whereas the acorns or cupules, more valuable evidence for the inter‐ and intrageneric classifications, have been relatively poorly documented. Here, we describe a new species, Quercus shangcunensis sp. nov., based on a ring‐cupped fossil acorn and pollen on the acorn, as well as Quercus sp. associated leaves, recovered from the early Oligocene Shangcun Formation of Maoming Basin, Guangdong Province, South China. The morphological and anatomical structures of these fossils confirm their attribution to the subg. Cyclobalanopsis. Quercus shangcunensis sp. nov. represents the world's first Oligocene fossil acorn and the earliest fossil acorn in China for the subgenus, indicating that the subg. Cyclobalanopsis arrived in the low latitude area of South China at least by the early Oligocene. Our fossil provides evidence that the subgenus was present in one of its modern distribution centers in the Oligocene, suggesting that the modern distribution patterns of the subg. Cyclobalanopsis most likely originated during or prior to the Oligocene.     

A Taxonomical Revision of Fossil Evergreen Sclerophyllous Oaks from China

Evergreen sclerophyllous oaks (Quercus subg. Quercus sect. Brachylepides and part of sect. Engleriana) were dominant in Hengduan Mt., south west China, since the Late Tertiary. About 17 species from China have been recorded hitherto. However, some mistakes and confusion were made in their taxonomy and nomenclature. Therefore the nomenclature of the fossil would also be incorrect. An attempt is made in present paper, to revise such mistakes and contusion. 14 species of sect. Brachylepides were reduced to 7 and 3 species of sect Engleriana to one. In addition, the key to these fossil species was made.     

禄丰古猿化石地点的植物叶化石

1987年,在云南禄丰古猿化石地点D剖面第4层(薄层黑色炭质粘土与灰色细砂互层)发现植物叶部印痕化石,经鉴定属壳斗科绝灭的雷龙潭檞叶(Dryophyllum relongtanense Colani),该种植物常参与组成亚热带至暖温带的常绿阔叶林或常绿与落叶阔叶混交林。     

禄丰古猿化石地点的植物叶化石

1987年,在云南禄丰古猿化石地点D剖面第4层(薄层黑色炭质粘土与灰色细砂互层)发现植物叶部印痕化石,经鉴定属壳斗科绝灭的雷龙潭槲叶(Dryophyllum relongtanense Colani),该种植物常参与组成亚热带至暖温带的常绿阔叶林或常绿与落叶阔叶混交林。     

Phylogeny, biogeography, and molecular dating of cornelian cherries (Cornus, Cornaceae): tracking Tertiary plant migration

Data from four DNA regions (rbcL, matK, 26S rDNA, and ITS) as well as extant and fossil morphology were used to reconstruct the phylogeny and biogeographic history of an intercontinentally disjunct plant group, the cornelian cherries of Cornus (dogwoods). The study tests previous hypotheses on the relative roles of two Tertiary land bridges, the North Atlantic land bridge (NALB) and the Bering land bridge (BLB), in plant migration across continents. Three approaches, the Bayesian, nonparametric rate smoothing (NPRS), and penalized likelihood (PL) methods, were employed to estimate the times of geographic isolations of species. Dispersal and vicariance analysis (DIVA) was performed to infer the sequence and directionality of biogeographic pathways. Results of phylogenetic analyses suggest that among the six living species, C. sessilis from western North America represents the oldest lineage, followed by C. volkensii from Africa. The four Eurasian species form a clade consisting of two sister pairs, C. mas-C. officinalis and C. chinensis-C. eydeana. Results of DIVA and data from fossils and molecular dating indicate that the cornelian cherry subgroup arose in Europe as early as the Paleocene. Fossils confirm that the group was present in North America by the late Paleocene, consistent with the DIVA predictions that, by the end of the Eocene, it had diversified into several species and expanded its distribution to North America via the NALB and to Africa via the last direct connection between Eurasia and Africa prior to the Miocene, or via long-distance dispersal. The cornelian cherries in eastern Asia appear to be derived from two independent dispersal events from Europe. These events are inferred to have occurred during the Oligocene and Miocene. This study supports the hypothesis that the NALB served as an important land bridge connecting the North American and European floras, as well as connecting American and African floras via Europe during the early Tertiary.