Axial nature of the cupule‐bearing organ in Caytoniales

Abstract Caytoniales are an important group of seed plants, and the nature of their female reproductive organ may influence interpretations of the seed plant phylogeny and the origin of angiosperms. Although not convincingly demonstrated by clear evidence, cupules on previously described specimens were interpreted as being distichously arranged, implying that the cupule‐bearing organ in Caytoniales was a pinnate megasporophyll. Here a female reproductive organ of Paracaytonia hongtaoi gen. et sp. nov. (Caytoniales) is reported from Liaoning, China. The well preserved specimen clearly shows a spiral arrangement of cupules along the reproductive axis, suggesting that the cupule‐bearing organ in Caytoniales is not a megasporophyll but a branch. This new information on the axial nature of the cupule‐bearing organ in Caytoniales has significant implications on the placement of Caytoniales in the seed plant phylogeny and interpretation of the relationship between Caytoniales and angiosperms.     

A revision of Aceratherium blanfordi Lydekker, 1884 (Mammalia: Rhinocerotidae) from the Early Miocene of Pakistan: postcranials as a key

Rhinocerotids are particularly abundant and diversified in Neogene deposits of the Indian subcontinent, but their systematics is far from being well defined. Based on the revision of old collections and new findings from the Early Miocene of the Bugti Hills and Zinda Pir, Pakistan, ‘Aceratherium blanfordi Lydekker, 1884’ is a chimera, consisting of two dentally convergent but postcranially distinct rhinocerotid taxa: Pleuroceros blanfordi and Mesaceratherium welcommi sp. nov. Postcranial features appear to be much more diagnostic than craniodental morphology in this case. A phylogenetic analysis based on 282 morphological characters scored for 28 taxa (four outgroups and ingroup including both taxa of interest and a ‘branching group’) strengthens this statement and supports Pleuroceros and Mesaceratherium as monophyletic genera within Rhinocerotinae. Both genera are recognized for the first time outside Europe. In the Bugti Hills, P. blanfordi and M. welcommi are part of an exceptionally diversified rhinocerotid fauna, with up to nine species associated in the same locality (Kumbi 4f). This rhinocerotid assemblage confirms the earliest Miocene age (Agenian/Aquitanian) of the upper member of the Chitarwata Formation as a whole. Coeval homotaxic rhinocerotid faunas from Europe (France, Czech Republic) and East Africa (Uganda, Kenya) support broad and sustainable rhinocerotid interchanges amongst South Asia, Europe, and Africa under compatible environmental conditions throughout earliest Miocene times. © 2010 The Linnean Society of London, Zoological Journal of the Linnean Society, 2010, 160 , 139–194.     

内蒙古宝格达乌拉晚中新世副竹鼠化石(英文)

描述了1996-2007年间在内蒙古阿巴嘎旗晚中新世宝格达乌拉组采集的副竹鼠化石。材料包括下颌骨1件、牙齿14枚和肢骨4件,分别采自该组的2个地点。根据标本较大的尺寸、形态特征,以及颊齿的釉质曲线高度,宝格达乌拉材料被归入三趾马层副竹鼠Pararhizomys hipparionum Teilhard de Chardin Young,1931。Pararhizomys是一类具高冠、脊形和冠面构造简单颊齿的啮齿动物。该属目前发现的化石地点少,材料也不多,主要集中于中国北方和蒙古高原周缘,其地史分布为晚中新世早期至上新世中期。与鼢鼠类(siphneids)和鼠平类(arvicolids)一样,Pararhizomys属的颊齿有由低冠到高冠发展的趋势,具体表现为牙齿侧面釉质曲线(dentine tract)由平直、远离内外两侧谷底到起伏、接近甚至超过内外两侧谷底。为方便比较,本文为釉质曲线的高度设立"H"指数,即从每侧最深谷的谷底和釉质曲线的最高处取平行于冠面的平行线,此两平行线之间的垂直距离为"H"。H值越大,表明齿冠越低,反之则齿冠越高。尽管目前发现的副竹鼠标本不多,但似乎可以看到从早期到晚期,其颊齿的个体有从小变大,釉质曲线高度H值逐渐减小,即齿冠逐渐增高的趋势。由于Pararhizomys的牙齿形态多少与竹鼠类的低冠竹鼠Brachyrhizomys和竹鼠属Rhizo-mys及拟速掘鼠属Tachyoryctoides有相似之处,故常被与Brachyrhizomys和Rhizomys一起归入竹鼠科(Rhizom yidae),但该属的牙齿不具中脊和下中脊,褶沟少,一般为2-3个,与上述三属有明显的不同。本文对下门齿所作的切片观察也表明,Pararhizomys的釉质层结构与Brachyrhizomys,Rhizomys和Tachyoryctoides者相差甚远,其内层(PI)明显增厚,釉柱和釉柱间质(IPM)的排列方式存在明显差别。颊齿的冠高、冠面形态,以及下门齿的釉质层结构,似乎都表明了Pararhizomys属不大可能归入竹鼠科或速掘鼠科(Tachyorictoididae)。而下门齿釉质层切片显示了Brachyrhizomys与Rhizomys有着高度相似的釉质结构,进一步证明了两者有较接近的亲缘关系。地理分布上,Pararhizomys与Tachyoryctoides属只发现于古北区,伴生的哺乳动物显示了其可能适应偏冷、干旱的草原环境,而Brachyrhizomys和Rhizomys主要局限于东洋区,共生的哺乳动物多能适应温暖、湿润的树林环境。     

山西垣曲原蹄犀(犀科,奇蹄目,哺乳纲)化石

火石坡是垣曲盆地近年来新发现的化石点,产有丰富的哺乳动物化石,多数已被报道(黄学诗等,1999;Zhang et al.,2001;刘丽萍、黄学诗,2002;黄学诗、王景文,2002;Dawson et al.,2003;黄学诗,2004),本文仅对其中的奇蹄目原蹄犀类化石予以简单记述,它的发现为垣曲盆地始新世动物群增加了新成员.     

SOCIAL BEHAVIOUR AND MASS MORTALITY IN THE BASAL CERATOPSIAN DINOSAUR PSITTACOSAURUS (EARLY CRETACEOUS, PEOPLE'S REPUBLIC OF CHINA)

Abstract:  An exceptionally preserved herd of the ceratopsian dinosaur Psittacosaurus was recovered from the Lujiatun Beds of the Lower Cretaceous Yixian Formation, Liaoning Province, north-east China. This specimen provides the earliest direct evidence of post-nestling gregarious behaviour in this important dinosaur clade. The sediment in which the skeletons occur represents a lahar (volcanic mudflow), indicating that the six individuals present were entombed simultaneously during a catastrophic mass mortality event. Reconstruction of the herd age profile shows it was composed of offspring from at least two clutches, revealing that group fidelity in these dinosaurs extended beyond time spent together in the nest. This demonstrates that sociality appeared much earlier in ceratopsian evolution than is generally acknowledged and that such behaviour preceded the evolution of the elaborate horns and frills seen in derived ceratopsids.     

侏罗纪的施迈斯内果(Schmeissneria)是不是被子植物?

中华施迈斯内果在辽西的发现为被子植物的历史添上了重要的一笔。施迈斯内果是一个具有近170年研究历史的植物化石属。新近发现的中华施迈斯内果中发现了以前没被认识到的新特征(未成熟的雌性器官的中央结构有一个纵向的隔壁和封闭的顶端)。新的特征促使人们重新审视该化石的系统位置。王鑫等人通过仔细分析被子植物的定义、结合新的化石特征认为施迈斯内果代表了一个具有被子植物特征的新类群。按照现有的被子植物定义,施迈斯内果可以归入被子植物。这样一来,被子植物的历史就会被前推到早侏罗世。当然也不排除未来被子植物的定义改变后为施迈斯内果建立一个与被子植物平行的种子植物新类群的可能性。文章简要地介绍了施迈斯内果的由来、特征以及王鑫等人如何判定其为被子植物的逻辑思维过程,以便大家论评。     

海南蕨类植物自然分布及区系组成

海南岛现有蕨类植物种数约400种,分布基本上呈现西南部丰富,东北部贫乏的趋势,临高-琼中-万宁一线是其物种多寡的分界线,土壤、地形、地质多方面的共同作用形成这条分界线。海南岛蕨类区系组成复杂,且外来植物成分占据多数,马来西亚、印度、中南半岛和东亚植物区系成分在海南岛蕨类区系中占有较大比重。海南岛是现代蕨类发育的一个中心,多样的环境条件促成了蕨类植物的演化。     

云南早泥盆世西山村组华南鱼类的首次发现

记述了云南曲靖地区早泥盆世洛霍考夫期华南鱼类一新属———王冠鱼(Stephaspis gen.nov.)。新属发现于西山村组下部致密坚硬的石英砂岩中,其主要特征是:个体较大的华南鱼类,头甲呈长盾形,后缘向后凸出;角发育,侧向延伸,末端向头甲后侧方自然倾斜,内角不发育;具吻突,但不甚发育;中背孔较大,呈纵向椭圆形,前端稍尖,后端圆钝;眶孔较小,圆形,背位;头甲背面具一对背窗,呈狭长椭圆形,靠近头甲侧缘;感觉管系统不甚发育,仅见后眶上管、侧背管、侧横管及背联络管,后眶上管呈V字形;纹饰为细小的粒状瘤点。新属不仅是华南鱼类在西山村组的首次发现,也指示了目前华南鱼类出现的最低层位,为探讨华南鱼类的起源与早期辐射提供了重要资料。     

A primitive ornithischian dinosaur from the Late Triassic of South Africa, and the early evolution and diversification of Ornithischia

Although the group played an important role in the evolution of Late Mesozoic terrestrial ecosystems, the early evolutionary history of the ornithischian dinosaurs remains poorly understood. Here, we report on a new primitive ornithischian, Eocursor parvus gen. et sp. nov., from the Late Triassic (?Norian) Lower Elliot Formation of South Africa. Eocursor is known from a single specimen comprising substantial cranial and postcranial material and represents the most complete Triassic member of Ornithischia, providing the earliest evidence for the acquisition of many key ornithischian postcranial characters, including an opisthopubic pelvis. A new phylogenetic analysis positions this taxon near the base of Ornithischia, as the sister taxon to the important and diverse clade Genasauria. The problematic clade Heterodontosauridae is also positioned basal to Genasauria, suggesting that an enlarged grasping manus may represent a plesiomorphic ornithischian condition. This analysis provides additional phylogenetic support for limited ornithischian diversity during the Late Triassic, and suggests that several major ornithischian clades may have originated later than generally believed. There are few morphological differences between Late Triassic and Early Jurassic ornithischians, supporting previous suggestions that the Early Jurassic ornithischian radiation may simply represent the filling of vacant ecological space following Late Triassic terrestrial extinctions.