我国某些苏铁类生殖器官化石的发现兼论苏铁类起源

本文对苏铁类化石的系统分类作了概要的介绍。重点报道了笔者在近廿年来所采集的苏铁类生殖器官化石,各别是中晚石炭世的一枚苏铁大孢子叶化石的发现,将苏铁类起源的时间大大地推前了,并指出其起源地应在中国西北的甘肃地区。所有这些生殖器官的发现将推动苏铁化石生殖生物学的发展,对其起源、分布、演化和苏铁植物区系的形成和发展提供了极为重要的材料。     

我国某些苏铁类生殖器官化石的发现兼论苏铁类起源

本文对苏铁类化石的系统分类作了概要的介绍。重点报道了笔者在近廿年来所采集的苏铁类生殖器官化石,特别是中晚石炭世的一枚苏铁大孢子叶化石的发现,将苏铁类起源的时间大大地推前了,并指出其起源地应在中国西北的甘肃地区。所有这些生殖器官的发现将推动苏铁化石生殖生物学的发展,对其起源、分布、演化和苏铁植物区系的形成和发展提供了极为重要的材料。     

苏铁类植物传粉生物学研究进展(综述)

苏铁类植物是现存最古老的种子植物,研究其传粉特点,对于研究种子植物的起源与演化、植物与动物的协同进化以及苏铁类植物的繁殖机制、濒危机制有重要意义。本文从苏铁雌雄株开花物候学、传粉媒介及传粉机制等方面,对苏铁类植物传粉生物学相关研究进行综述,并提出今后该类植物传粉生物学研究的建议：对更多苏铁属种类未知的传粉机制进行研究;更广泛地应用排除法研究苏铁类特别是苏铁属植物的传粉媒介,进一步探讨传粉昆虫与苏铁类的共生关系问题。     

椭圆斜羽叶的解剖研究及斜羽叶的系统分类位置

本文根据对椭圆斜羽叶(Plagiozamites oblongifolius)钙质石化化石的研究,认为其主要特征如下:羽状复叶,叶肉无海绵组织和栅栏组织分化。羽片叶脉维管束外韧式,木质部外始式,与现代苏铁属叶脉特征相近。羽轴维管束为“U”形,外始式木质部、梯状纹孔管胞,与现代苏铁属的羽轴维管束相似。根据上述特征,目前可将斜羽叶属归入原始苏铁类植物。但是,如果斜羽叶的生殖器官同 Noeggerathia 一样,为异孢型孢子囊穗,则斜羽叶可能为一种与苏铁类起源有关的原裸子植物。     

云南海口早寒武世褐藻化石新知

主要报道了产自云南海口耳材村早寒武世筇竹寺组玉案山段澄江生物群中的褐藻化石－拟点叶藻（Punctariopsis latifolia gen.et sp.nov.)简单拟点叶藻（Punctariopsis simplex gen.etsp.nov.)和古德带藻（Vendotaenia cf.antiqua Gnilovskaya)3种。这些化石丰富了澄江生物群物种的多样性,为研究该群生物爆发性演化提供了新的证据。同时通过对现生褐藻和褐藻化石形态学的比较研究,表明化石属和现代属在系统演化上可能有较密切的亲缘关系,并进一步证明了澄江生物群在云南海口地区发生于一个潮间带和亚潮带的海水环境。     

中国苏铁

苏铁家族溯源 苏铁又名铁树,这里讲的苏铁不只限于狭义的苏铁一个物种,而是指广义的苏铁类植物(CYCADS)。苏铁类是现存地球上最原始的一类种子植物。据化石记录,它最早出现在地球上是在古生代二迭纪约2.5亿年前,到侏罗纪约1.5—1.9亿年时期,苏铁类植物发展达到顶峰,多种多样的古苏铁植物类群遍布于世界各大陆,与当时动物界的兽王——恐龙并驾称霸地球。至今发现的苏铁类化石至少有30属,     

内蒙古道虎沟中侏罗世小蝎蛉科(昆虫纲,长翅目)昆虫化石

描述小蝎蛉科化石1新属2新种:多脉原始小蝎蛉Protochoristella polyneura gen.et sp.nov.,美丽原始小蝎蛉P.formosa gen.et sp.nov..简要讨论了小蝎蛉科的起源与演化.所有化石标本均采于内蒙古宁城道虎沟中侏罗世九龙山组地层,模式标本现保存于首都师范大学生命科学学院.     

龙凤山藻在澄江早寒武世生物群中的发现

主要报道了产自云南昆明海口耳材村早寒武世筇竹寺组玉案山段澄江生物群中可能为自由漂浮生长的宏观藻类化石--心型龙凤山藻(新种)(Longfengshania cordata sp. nov.)和中华豆芽藻(新属、新种)(Plantulaformis sinensis gen. et sp. nov.).这些化石的发现进一步显示了澄江生物群物种多样性,为揭示该生物群爆发性演化提供了新的证据.通过对龙凤山藻属亲缘关系的深入比较研究,进一步证明该类化石应归属宏观藻类以及它们遗传上的稳定性、演化上的保守性和环境上的适应性.     

准苏铁果属(Cycadocarpidium)在吉林汪清县晚三叠世地层的发现

本文记述了吉林汪清县天桥岭地区晚三叠世地层中准苏铁果属(Cycadocarpidium)的发现和该属的两个新种:巨大准苏铁果(C.giganteum sp.nov.)和雅致准苏铁果(C.elegans sp.nov.),并讨论了它们在确定地层时代、恢复古地理古气候等方面的意义。     

辽宁早白垩世化石木一新属——原始金松型木（Protosciadopityoxylon）

报道了辽宁早白垩世化石木的一个新属—原始金松型木 (Protosciadopityoxylongen .nov .)。该属化石以辽宁原始金松型木 (Protosciadopityoxylonliaoningensegen .etsp .nov .)为代表。文中对新属新种进行了描述 ;讨论了新属与现存金松属 (Sciadopitys)及化石金松型木属 (Sciadopityoxylon)的关系 ;并与其相似的原始叶枝杉型木属 (Protophyl locladoxylon)、原始圆孔木属 (Protocircoporoxylon)及异木属 (Xenoxylon)作了比较。     

The Cuticles of Two Fossil Cycads and Epiphytic Fungi

Cuticles of two fossil cycads and seven epiphytic fungi are described in this paper. They are Nilssonia sinensis Yabe et Oishi, Ctenis lyrata Li et Ye; Perisporiacites shaheziensis sp. nov., Notothyrites haizhouensis sp. nov., Microthyriacites pilcatus sp. nov., M. fuxinensis sp. nov., Stigmateacites polymorphus gen. et sp. nov., S. simplex gen. et sp. nov., Liaoningnema multinoda gen. et sp. nov. Materials were collected from the Shahezi Formation of Changtu district and the Haizhou Formation in Haizhou mine-field of Li- aoning Province, China. The age of these tossils is Early Cretaceous.     

中国内蒙古中侏罗世脉翅目昆虫化石—新科(英文)

建立脉翅目昆虫化石新科———Grammolingiidaefamnov .,并描述该科化石 3新属 6新种 :Grammolingiaboigen .nov .ofsp .nov .,Litholingiarhoragen .nov .ofsp .nov .,Litholingiaeumorphagen .nov .ofsp .nov .,Litholing iapolychotomagen .nov .ofsp .nov .,Leptolingiajurassicagen .nov .ofsp .nov .,Leptolingiatianyiensisgen .nov .etsp .nov ..给出了新科的属级检索表 ,描述的所有模式标本均采自于内蒙古自治区宁城县中侏罗世九龙山组地层中。标本分别保存在义县博物馆和首都师范大学生物系。本次发现再次表明目前关于脉翅目昆虫的认识仍然十分贫乏。     

A NEW LACEWING FAMILY (NEUROPTERA)FROM THE MIDDLE JURASSIC OF INNER MONGOLIA, CHINA

Abstract  A new family, Grammolingiidae of fossil lacewings is erected, of which 3 new genera and 6 new species are described and illustrated: Grammolingia boi . gen. nov. et sp. nov., Lithlingia rhra gen. nov. et sp. nov., Litholingia eumopha gen. nov. et sp. nov. and Litholingiu polychotom gen. nov. et sp. nov., Leptolingia jurassica gen. nov. et sp. nov. and Leptolingia tianyiensis gen. noc. et sp. nov. A key to genera within this new family is provided. All specimens described were collected from the Middle Jurassic Jiulongshan Formation of Eastern Inner Mongolia, China. The present discovery demonstrates that present knowledge of the Jurassic Neuropetra fauna remains very poor. The fossil specimens are deposited in Yizhou Fossil Museum and Department of Biology, Capital Normal University, respectively.     

竹节虫化石在中国的首次发现及其生物学特征 (竹节虫目:神科,新科)(英文)

本文建立竹节虫目昆虫化石1新科,即Haginhasmatidae,包括3新属,3新种和一个本命名种：Hagiphasmaparadoxagen．etsp．nov,Aethephasmamegistagen．etsp．nov．和Orephasmaeummphagen．etsp.nov,并给出新科内属的检索表。对消化道痕迹和保存完好的亚生殖板进行了分析,并与现代类群作了比较。竹节虫化石在我国是首次报道,所有化石材料均采自河北省和辽宁省晚珠罗世义县组地层中,保存在中国地质博物馆。     

美蝎蛉化石在中国首次发现(昆虫纲,长翅目)

描述了美蝎蛉化石2新属2新种:Tsuchingothaumashihi gen.et sp.nov.,Typhothauma yixianensis gen. et sp.nov..化石采自于中国东北侏罗纪非海相地层中.这是美蝎蛉化石在中国的首次发现.新的化石表明美蝎蛉的早期分异在中侏罗世就已存在.     

A review of fossil cycad megasporophylls, with new evidence of Crossozamia pomel and its associated leaves from the lower permian of Taiyuan, China

Four species of cycad megasporophyll from the Lower Permian of Taiyuan, China, are described as Crossozamia chinensis (Zhu and Du) comb. nov., C. minor sp. nov., C. spadicia sp. nov. and C. cucullata comb. nov. together with the associated leaves Tianbaolinia circinalis gen. et sp. nov., Yuania chinensis Zhu and Du and Taeniopteris taiyuanensis Halle. An axis bearing megasporophylls in organic connection is described for the first time. Two possible evolutionary pathways from this structure to those of the female reproductive organs of extant cycads are proposed, involving either the reduction of the megasporophylls and their compaction on the axis, or the reduction of the “strobilus” axis. It is suggested that migration of cycads from North China to Europe might have occurred through transportation of their buoyant seeds by the palaeoceanic currents of the Tethys sea.     

A New Genus (Protosciadopityoxylon gen. nov.) of Early Cretaceous Fossil Wood from Liaoning,China

A new genus ( Protosciadopityoxylon gen nov. ) of Early Cretaceous fossil wood reported in the present paper was discovered from Liaoning Province, China, and is named as a new species:Protosciadopityoxylon liaoningense gen. et sp. nov. It is described here and this generic name, adopted by the authors, is employed for fossil wood that is believed to be nearly related to the recent genus Sciadopitys and the fossil genus Sciadopityoxylon. The new genus bears some similarities to Protophyllocladoxylon,Protocircoporoxylon and Xenoxylon in different geological ages, but it differs from them in the types of cross-field pitting.     

陕西中三叠世中蝎蛉科两新属和新种(昆虫纲,长翅目)

记述中蝎蛉科Mesopanorpodidae 2新属、新种：Triassochoristites jinsuoguanensis gen．et sp．nov．,Forcinerva tongchuanensis gen．et sp．nov．化石标本采自陕西铜川中三叠世铜川组下段上部的灰绿色泥岩和页岩。这些新属、种系陕西昆虫群(陕西生物群的一个类别)铜川昆虫组合的新成员。铜川组的时代相当于欧洲拉丁尼期(Ladinian Stagc)。     

中国东北晚侏罗世虻类化石(昆虫纲:双翅目)

本文论述了辽宁西部上侏罗统虻类６个科的化石,包括１新科,１０个新属和１５个新种。其中Ｐａｌａｅｐａｎｇｏｎｉｕｓ ｅｕｐｔｅｒｕｓ ｇｅｎ．ｅｔ ｓｐ．ｎｏｖ．,Ｅｌｐａｎｇｏｎｉｕｓ ｐｌｅｔｕｓ ｇｅｎ,ｅｔ ｓｐ．ｎｏｖ．和Ａｌｌｏｍｙｉａ ｒｕｄｅｒａｌｉｓ ｇｅｎ．ｅｔ ｓｐ．ｎｏｖ．均属于虻科（Ｔａｂａｎｉｄａｅ）;Ｏｒｓｏｂｒａｃｈｙｃｅｒｏｎ ｃｈｉｎｅｎｓｉｓ ｇｅｎ．ｅｔ ｓｐ     

The earliest Timematids in Burmese amber reveal diverse tarsal pads of stick insects in the mid‐Cretaceous

Many extant insects have developed pad structures, euplantulae or arolia on their tarsi to increase friction or enhance adhesion for better mobility. Many polyneopteran insects with euplantulae, for example, Grylloblattodea, Mantophasmatodea and Orthoptera, have been described from the Mesozoic. However, the origin and evolution of stick insects' euplantulae are poorly understood due to rare fossil records. Here, we report the earliest fossil records of Timematodea hitherto, Tumefactipes prolongates gen. et sp. nov. and Granosicorpes Urates gen. et sp. nov., based on three specimens from mid-Cretaceous Burmese amber. Specimens of Tumefactipes prolongates gen. et sp. nov. have extremely specialized and expanded euplantulae on their tarsomere II. These new findings are the first known and the earliest fossil records about euplantula structure within Phasmatodea, demonstrating the diversity of euplantulae in Polyneoptera during the Mesozoic. Such tarsal pads might have increased friction and helped these mid-Cretaceous stick insects to climb more firmly on various surfaces, such as broad leaves, wetted tree branches or ground. These specimens provide more morphological data for us to understand the relationships of Timematodea, Euphasmatodea, Orthoptera and Embioptera, suggesting that Timematodea might be monophyletic with Euphasmatodea rather than Embioptera and Phasmatodea should have a closer relationship with Orthoptera rather than Embioptera.