陕西蓝田灞河组陕西转角羚一新种(英文)

1997～ 2 0 0 1年 ,中科院古脊椎动物与古人类研究所与芬兰赫尔辛基大学合作 ,于灞河组地层中发现哺乳动物化石计 45种。其中牛科化石种类与蓬蒂期典型三趾马动物群中的种类不同 ,至少存在分别归属于Shaanxispira、Protoryx、Dorcadoryx和Gazella的 4个新的种类。本文仅记述其中陕西转角羚羊一新种 :灞河陕西转角羚 (Shaanxispirabaheensissp .nov .)。该种主要鉴定特征 :角心长而直 ,粗壮 ,横断面呈圆形 ,具一条发育的棱 ,起始于前内侧 ,右角上呈顺时针方向旋转一周至一周半 (从角基部视 ) ,角心前视向两侧中等程度散开 ,侧视中等后倾 ,起始于眼眶之后 ,角柄短。鼻骨窄 ,向上隆起 ,其后缘延伸至眼眶前棱之后的位置 ;眶前窝较宽浅 ,面部长而窄 ;角前额顶宽、稍隆起 ,眶上孔成椭圆形 ,眶上窝发育 ,向前的沟槽可延伸至泪骨 ;额骨在角前轻微隆起 ;角后颅顶宽、短 ,颅轴与面轴交角约为 90°。枕面宽、平 ,面向后下方。牙齿齿冠中等高度。臼齿上底柱与肋皆不发育。p4的下后尖位于下原尖之后 ,在老年个体上与下内尖连接 ,封闭后内谷。与已知大型转角羚羊相比较 ,灞河组新发现的种类与周氏陕西转角羚最为接近。不同的是该新种角心只发育一条棱 ,而不是两条 ,角心横断面呈圆形 ;顶骨较短 ;臼齿列相对较短 ,下臼?     

岩羊和矮岩羊头骨形态特征比较

本文报道了岩羊和矮岩羊的头骨形态学资料,涉及头骨特征描述和一些形态学指标测定,被测定的指标主要有上颊齿列基长、眼窝长、乳突间距、眶间距、颧宽、枕颅高、枕髁宽、脑颅最大宽、眶下孔距、上颌臼齿外宽、角基最窄、最小角尖距、角尖距、最大角间距、角基周长、角基长径、角基短径、角外侧长,应用判别分析和单变量分析对岩羊和矮岩羊头骨的测量值进行统计与分析,以探讨这两个种头骨之间的形态差异。结果表明：（1）岩羊和矮岩羊头骨在形态上十分相似,但矮岩羊的头骨细长,脑颅狭窄,角直且朝上翘,角内侧具一明显角棱,亦较直,角基部狭窄,老年个体角基部愈合;岩羊的脑颅宽大,角粗大而长,向两侧分开,弯曲度较大,内侧角棱弯曲呈长S型,角尖朝向后方,角基部较宽,不愈合在一起。（2）岩羊和矮岩羊头骨的18项形态测量指标中乳突间距、眶间距、颧宽、脑颅最大宽、上颌臼齿外宽、角基周长、角基长径差异极显著（P〈0.01）,枕颅高、枕髁宽、眶下孔距、角尖距、最大角间距、角基短径、角外侧长差异显著（P〈0.05）;典型判别的正确率：岩羊为100%,矮岩羊为83.3%,交互验证法检验的结果,判别正确率：岩羊100%,矮岩羊为83.3%。这两个判别函数可以从角上区别岩羊和矮岩羊。     

陕西蓝田灞河组的小羚羊(Dorcadoryx Teilhard et Trassaert, 1938, Bovidae)

描述了牛科小羚羊(Dorcadorys Teilhard et Trassaert,1938)一新种:D.orientalis sp. nov.。材料发现于陕西蓝田Loc.6,晚中新世灞河组中部。它和属型种Dorcadoryx triquetricor- nis的主要不同在于它的角心长,向上分散度大,角后窝深而狭长,眼眶向头骨两侧突出不明显,下颌骨水平支低而纤细,颊齿窄和前臼齿列相对长等。Dorcadoryx是中国北方和蒙古地区晚中新世至早上新世的特有类型之一。我国山西晚中新世的?Tragoreas(Bohlin,1935)、蒙古新近纪晚期的Tragoreas sp.2和sp.3以及Olonbulukia(?)sp.(Dmitrieva,1977)可能是它的成员。经修订,属的主要特征是个体小至中等大小,头骨狭长,角基之间的额面不向上隆起,头骨弯曲发生在额顶骨之间,眶上孔小,眶前窝大,颅顶部狭长,基枕部具中沟,前结节不明显,角心位于眼眶之上、不旋转,内外侧扁,分散度不大,稍向后弯曲,角柄长,角后窝存在, 前臼齿列退化以及p4的下后尖和下前尖相连等。它可能属于山羊亚科,包含4—5种。新种可能是其中的一个早期类型。     

山西静乐贺丰上新世的步氏羚羊（Gazella balcki Teilhard and Young,…

重新厘定后,步氏羚羊（Ｇａｚｅｌｌａｂｌａｃｋｉ）的主要特征是个体中等大小,脑颅部宽而短,枕面向后突出不明显,枕髁与枕面处的一同一平面中,基枕面平,呈方形,具宽浅而长的中纵沟;角心纤细,短而直,从角基向角顶方向迅速变尖,基部横切面为次圆形,颊齿高冠,前臼齿列短和ｐ４有封闭的前内谷等,它出现在我国山西上上新统的地层中,依据头骨和颊齿的性状,它可有是现生种Ｇ．ｐｉｃｔｉｃａｕｄａｔａ和Ｇ．ｇｕｔｈｕｒ     

山西静乐贺丰上新世的步氏羚羊

重新厘定后,步氏羚羊（Gazellablacki）的主要特征是个体中等大小,脑颅部宽而短,枕面向后突出不明显,枕髁与枕面处在同一平面中,基枕面平,呈方形,具宽浅而长的中纵沟;角心纤细,短而直,从角基向角项方向迅速变尖,基部横切面为次圆形;颊齿高冠,前臼齿列短和p4有封闭的前内谷等。它出现在我国山西上上新统的地层中。依据头骨和颊齿的性状,它可能是现生种G．picticaudata和G．gutturosa的祖先类型。     

南京1号直立人头骨与肯尼亚KNM-ER 3733人类头骨化石的形态比较

KNM-ER 3733人类头骨化石的年代为距今1.78百万年,1975年发现于肯尼亚。Walker和Leakey注意到这具头骨与周口店直立人的在脑颅形态上很相近,但二者在年代上相差大约1百万年,故认为直立人形态在这1百万年期间是稳定的。长期来此观点缺乏更多的人类化石证据来支持。1993年在中国发现了南京1号人类头骨化石。该头骨与KNM-ER 3733头骨一样兼具脑颅和面颅,且都属于成年女性个体,但南京1号人类头骨化石的年代比KNM-ER 3733人类头骨化石的要晚大约1百万年。因此,南京1号人类头骨是目前所知的可用来验证直立人头骨形态是否在1百万年期间保持稳定的唯一合适的人类头骨化石材料。形态比较表明,这两个人类头骨化石的脑颅虽然在眶上圆枕上沟的发育程度、眶后收缩的程度、额骨横向隆起的程度、角圆枕和乳后突的发育与否、顶骨形状以及骨壁厚度的表现上有所差异,但有更多的形态性状显示出相近。这些相近表现在脑颅的长、宽、高值上;颅容量上;脑颅的低矮性上;脑颅最大宽之位置上;额骨、顶骨、枕骨之矢弧值的比例上;眶上圆枕的纤细上;顶骨的大小和矢向扁平性上;颞线位置和颞鳞顶缘的形状上;枕鳞的低宽形状上;上枕鳞与下枕鳞之间的转折形状和比例上;枕骨圆枕和枕骨圆枕上沟的发育程度上等。这两具头骨的面颅虽然有同属突颌型的面角、皆发育有鼻骨间嵴、两鼻骨组成的上部宽度与下部宽度皆差别很大,但有更多的形态性状显示出差别。这些差别表现在面型上、颜面上部扁平度上、眶形和眶型上、上颌额突外侧面的朝向上、鼻骨横向隆起程度上、鼻梁外突程度上、鼻型上、颧骨下缘外展程度上、颊高上、颧上颌下缘的形状上、上颌颧突基部的位置上以及颧结节的位置上等。因此,南京1号头骨与KNM-ER 3733头骨之间在脑颅上显示出较多的相近性状,在面颅上则显示出较多的相异性状。脑颅方面的相近性状大多具有分类上的鉴别价值。这两个头骨脑颅形态的相近支持把KNM-ER 3733头骨鉴定为"直立人"的观点;也提示了南京1号头骨的脑颅似乎保持着1百多万年前的"祖先"形态。如果直立人的某些成员在至少1百万年期间保持着形态稳定的话,则这种形态上的稳定主要是表现在脑颅形态上。这两具头骨的面颅形态上较大差异的意义,目前尚不清楚。     

南京直立人与印尼、周口店直立人的面颅形态比较

本文对南京直立人1号头骨与印尼Sangiran17头骨和周口店11号头骨作面颅形态上的比较。结果表明,南京1号头骨的面颅与周口店11号头骨的有许多共同的形态:较小的面颅尺寸、眶下区呈扁平状、较扁平的上部颜面、眶上圆枕较纤细、中眶型的眼眶、发育有颧切迹、上颌骨颧突基部位置较高等。南京1号头骨的面颅在另外一些方面显示出与Sangiran17头骨的形态上相近:阔上面型的面型、眶上圆枕内侧部比外侧部稍靠前、眶上圆枕下缘略呈平直状、鼻梁发育有中矢锐嵴、鼻梁横向呈峰状拱起、颧骨下缘外展、颧结节相对位置稍偏外侧、颧骨较高等。南京直立人面颅兼具周口店直立人11号头骨的和印尼直立人Sangiran17头骨的形态。从南京直立人的面颅形态可以推测我国南方的与北方的直立人群之间在体质形态上已经出现一定程度的地理变异。南京1号头骨面颅上的某些形态特征,如颧骨下缘外展等,可能反映了特征的梯度变异现象。这些特征的梯度变异的成因目前还很难确定。     

内蒙古中部新发现的始施氏貘(哺乳纲,奇蹄目)头骨材料(英文)

记述了产自内蒙古呼和勃尔和剖面阿山头组的始施氏貘(Schlosseria magister)幼年头骨、头骨碎片及产自额尔登敖包底白层的S.magister成年头骨。幼年头骨在脊齿貘科属首次描述,成年头骨材料也是目前S.magister中首次描述。幼年头骨主要特征如下:头骨细长,脑颅部略有扩张,有眶后突,眶后收缩明显,矢状脊轻微发育;鼻切迹浅,位于前臼齿列之前,由前颌骨和鼻骨构成;眼眶大,眶前缘位于M1后部上方,眶下孔位于DP3-4之上;基蝶骨向后向中央逐渐加厚,末端隆起;翼蝶骨很大,从腹面看向后向背侧扩展,末端形成三角形的翼蝶骨突,覆盖在卵圆孔上;岩骨岬部表面有内颈动脉及其分支留下的3条沟痕;最内侧的为内颈动脉内侧沟,沿着岬部弯曲前行至最前部;镫骨动脉沟短小,横跨在圆窗前腹侧;岬动脉沟最长,起始于卵圆窗前内侧,沿岬部向前延伸;弓形下窝所在位置平滑,无凹陷。S.magister乳颊齿主要特征如下:DP2冠面大致呈三角形,前窄后宽,前缘较尖,长明显大于宽;外脊上仅有一个中央主尖前尖,一个非常不明显的小棱(可能为雏形的原脊)紧贴在前尖后舌侧壁上;前、后附尖不明显。DP3冠面呈梯形,与DP2相比明显增大,亚臼齿化,前附尖和后附尖略大,原、后脊明显。前尖大,后尖尚未分离;原尖很弱,几乎无法辨认,原脊低且不发育;次尖大而钝,比原尖更靠舌侧,后脊比原脊略发育,中部具小的后小尖;后脊在次尖处拐向后唇侧,使得磨蚀面呈V形。DP4冠面近方形,完全臼齿化,后尖已从外脊上分化出来,比前尖稍小,向舌侧倾斜,后尖肋明显;舌侧尖、脊发育完好,原尖和次尖大而钝,原脊、后脊近乎平行,比DP3的更高更长;两条脊分别在原尖和后尖处拐向后唇侧方,形成V形的磨蚀面。S.magister在由幼年向成年转变的过程中,主要变化趋势如下:1)吻部特征不同,主要表现为鼻切迹的位置、形态以及与之相关的前颌骨、上颌骨形态的差异。幼年头骨的鼻切迹位于前臼齿列之前,由前颌骨和鼻骨组成;成年头骨的鼻切迹后缩至M1-2之上,由鼻骨和上颌骨组成,并且因鼻切迹后缩造成鼻骨不与前颌骨接触。幼年和成年个体上颌骨的整体形态,眶前窝、眶下孔的位置和形态都差异显著。2)与咀嚼功能相关的结构改变。幼年个体的矢状脊微弱,而成年个体的则高且突起,暗示了后者具有相对强大的颞肌,以适应咀嚼功能。对比发现,S.magister与Lophialetes expeditus成年头骨在大小、整体形态和一些具有分类意义的特征上(如鼻骨和泪骨、前颌骨的接触方式,眶后突、关节后突、下颌关节窝的形状,矢状脊的高度等)非常接近。参照童永生、雷奕振(1984)对脊齿貘类头骨的划分方法,将Schlosseria magister的头骨与L.expeditus的划为一组,同时纠正了原有划分方案中存在的问题。     

中国三节叶蜂属一新种(膜翅目,三节叶蜂科)

记述中国三节叶蜂科三节叶蜂属1新种,长颊黑毛三节叶蜂Arge dolichogenata Wei et Nie,sp.nov..新种与Arge gracilicornis(Klug,1814)近似,但体型显著较大,体长9～10 mm;触角明显粗壮,短于中胸;颜面和内眶刻点粗密,侧脊弧形弯曲,额窝深,额脊显著;前翅2Rs室几乎等长于1Rs室,Rs脉第3段2倍于Rs第4段长,前后翅Cu<,2脉桩显著;雌虫锯腹片锯刃强烈突出;雄虫下生殖板端部宽截形,阳茎瓣头叶较宽,尾突窄长,腹侧中钩长且向上勾曲.新种模式标本保存于中南林业科技大学昆虫模式标本室.?＃     

吉林乾安大布苏发现完整原始牛骨架化石

１９９８年７月长春科技大学（原长春地质学院）退休教师刘翰先生在赴吉林省乾安大布苏泡子一带进行地质旅游考察过程中，在大布苏泡子东北命字井村牛道沟口（东经１２３°４１＇４６＂，北纬４４°４３＇４５＂）发现并抢救性挖掘到一具比较完整的牛科骨架化石。该化石角心粗大，弯曲，横断面近圆形，基部侧伸且较直，并逐渐向前转向，角面上具有明显的纵沟。额部与枕部夹角小于９０°，枕孔近圆形。牙齿粗壮，上臼齿近方形，磨蚀的上、下臼齿的原尖、次尖呈扁圆形或圆形，齿柱较发育。另外，经过对修复后的左侧盆骨观察，发现其髂骨颈较细…     

滇东中泥盆统的节甲鱼类化石

本文记述了节甲鱼类中称为北极鱼类的三个新属种:Exutaspis megista,Kunmingolepislucaowanensis,Yangaspis jinningensis,化石分别采自武定海口组(广义),海口和晋宁的海口组。代表我国中泥盆世该类化石鱼类的首次记述。     

A new fossil from the Jurassic of Patagonia reveals the early basicranial evolution and the origins of Crocodyliformes

Extant crocodylians have a limited taxonomic and ecological diversity but they belong to a lineage (Crocodylomorpha) that includes basal and rather generalized species and a highly diverse clade, Crocodyliformes. The latter was among the most successful groups of Mesozoic tetrapods, both in terms of taxonomic and ecological diversity. Crocodyliforms thrived in terrestrial, semiaquatic, and marine environments, and their fossil diversity includes carnivorous, piscivorous, insectivorous, and herbivorous species. This remarkable ecological and trophic diversity is thought only to occur in forms with a completely akinetic skull, characterized by a functionally integrated and tightly sutured braincase‐quadrate‐palate complex. However, the patterns of evolutionary change that led to the highly modified skull of crocodyliforms and that likely enabled their diversification remain poorly understood. Herein, a new basal crocodylomorph from the Late Jurassic of Patagonia is described, Almadasuchus figarii gen. et sp. nov. The new taxon is known from a well‐preserved posterior region of the skull as well as other craniomandibular and postcranial remains. Almadasuchus figarii differs from all other crocodylomorphs in the presence of six autapomorphic features, including the presence of a large lateral notch on the upper temporal bar, an otic shelf of the squamosal that is wider than long, a deep subtriangular concavity on the posterolateral surface of the squamosal, and an elongated pneumatopore on the ventral surface of the quadrate. Phylogenetic analysis focused on the origin of Crocodyliformes places Almadasuchus as the sister group of Crocodyliformes, supported by synapomorphic features of the skull (e.g. subtriangular basisphenoid, absence of basipterygoid process, absence of a sagittal ridge on the frontal, and a flat anterior skull roof with an ornamented dorsal surface). New braincase information provided by Almadasuchus and other crocodylomorphs indicates that most of the modifications on the posterior region of the skull of crocodyliforms, including the strongly sutured braincase, quadrate, and the extensive secondary palate appeared in a stepwise manner, and pre‐dated the evolutionary changes in the snout, jaws, and dentition. This indicates that the progressively increased rigidity of the skull provided the structural framework that allowed the great ecological diversification of crocodyliforms during the course of the Mesozoic. The phylogenetic pattern of character acquisition inferred for the strongly sutured (akinetic) skull and the appearance of more diverse feeding behaviours that create high mechanical loads on the skull provides another interesting parallel between the evolution of Mesozoic crocodyliforms and the evolutionary origins of mammals.     

A comparative study of stereolithographically modelled skulls of Petralona and Broken Hill: implications for future studies of middle Pleistocene hominid evolution

Computer generated three-dimensional stereolithographic models of middle Pleistocene skulls from Petralona and Broken Hill are described and compared. The anterior cranial fossae of these models are also compared with that of another middle Pleistocene skull, Arago 21. Stereolithographic modelling reproduces not only the outer surfaces of skulls, but also features within the substance of the bones, and details of the internal braincase. The skulls of Petralona and, to a somewhat lesser degree, Broken Hill are extremely pneumatized. Previously undescribed features associated with pneumatization are detailed, along with their possible functional significance, polarity, and potential for understanding hominid cranial variation. Petralona and Broken Hill also exhibit a dramatic suite of cerebral features that is probably related to extensive pneumatization of the skull, namely frontal lobes that are tilted and located behind rather than over the orbits, laterally flared temporal lobes, marked occipital projection, and basal location of the cerebellum. Comparison of the anterior cranial fossae of Petralona, Broken Hill, and Arago 21 suggests that external resemblance of skulls may not always correlate with endocranial similarity. We believe that stereolithographic reconstructions have the potential for helping to resolve difficult questions about the origins of Neanderthal and anatomically modern people.     

New data on the braincase of the aetosaurian archosaur (Reptilia: Diapsida) Stagonolepis robertsoni Agassiz

New data on the braincase of the aetosaurian archosaur Stagonolepis robertsoni Agassiz are presented, based on new preparation, synthetic casting, and interpretation of fossil material from the Triassic Elgin Sandstones, Scotland. The metotic fissure is not divided by bone. The perilymphatic foramen is completely bound by bone, and faces away from the otic capsule in a posterolateral direction. A prominent subvertical ridge on the anterolateral edge of the exoccipital and upper part of the basioccipital cannot be directly associated with the subcapsular process of the chondrocranium of extant crocodilians. This ridge projects laterally beyond the ventral ramus of the opisthotic, and lies anterior to the external foramina for the hypoglossal nerve. The overall structure of the braincases (especially the otic region) of S. robertsoni and other aetosaurians, where known, is more similar (in terms of derived archosaurian characters) to those of crocodylomorphs than are the braincases of other major suchian groups. This provides evidence for the currently unorthodox hypothesis that, among major suchian clades, Aetosauria and Crocodylomorpha are each others' closest relatives. Support for this hypothesis is found in features of the palatine and prefrontal that have not been considered in recent studies of suchian phylogeny. This alternative phylogenetic hypothesis demands further investigation but, combined with the new morphological data that it explains, it provides a framework for the understanding of the evolution of the derived and distinctive braincase structure of extant crocodilians.  © 2002 The Linnean Society of London, Zoological Journal of the Linnean Society, 2002, 136 , 7−23.     

Cranial Morphology of the Brachystelechid ‘Microsaur’ Quasicaecilia texana Carroll Provides New Insights into the Diversity and Evolution of Braincase Morphology in Recumbirostran ‘Microsaurs’

Recumbirostran ‘microsaurs,’ a group of early tetrapods from the Late Carboniferous and Early Permian, are the earliest known example of adaptation to head-first burrowing in the tetrapod fossil record. However, understanding of the diversity of fossorial adaptation within the Recumbirostra has been hindered by poor anatomical knowledge of the more divergent forms within the group. Here we report the results of μCT study of Quasicaecilia texana, a poorly-known recumbirostran with a unique, broad, shovel-like snout. The organization of the skull roof and braincase of Quasicaecilia is found to be more in line with that of other recumbirostrans than previously described, despite differences in overall shape. The braincase is found to be broadly comparable to Carrolla craddocki, with a large presphenoid that encompasses much of the interorbital septum and the columella ethmoidalis, and a single compound ossification encompassing the sphenoid, otic, and occipital regions. The recumbirostran braincase conserves general structure and topology of braincase regions and cranial nerve foramina, but it is highly variable in the number of ossifications and their extent, likely associated with the reliance on braincase ossifications to resist compression during sediment compaction and mechanical manipulation by epaxial and hypaxial musculature. Expansion of the deep ventral neck musculature in Quasicaecilia, autapomorphic among recumbirostrans, may reflect unique biomechanical function, and underscores the importance of future attention to the role of the cervical musculature in contextualizing the origin and evolution of fossoriality in recumbirostrans.     

黑犀(奇蹄目,犀科)化石在中国的首次发现

黑犀(Diceros属)的惟一现生代表D.bicornis生活在非洲。该属在新近纪时期曾广泛分布于希腊、土耳其和伊朗等地区,但从未在东亚地区发现过。新种甘肃黑犀(Diceros gan- suensis sp.nov.)是该属在中国和东亚的首次发现。化石采自甘肃临夏盆地晚中新世柳树组中部。新种以尺寸较小、头型短、枕顶高耸、枕面窄而高、枕嵴无中沟、副枕突短小、下颌上升支距m3较近、前臼齿较小、DP1无后脊、P2原脊孤立、P2和P3后脊细窄而区别于东地中海地区的Diceros neumayri。D.neumayri的分类位置一直是一个争论的焦点,曾在黑犀(Diceros属)和白犀(Ceratotherium属)之间反复变更。研究显示,甘肃黑犀和D.neumayri的一系列共同的原始特征表明它们与更进步的白犀有明显的区别,应该归入黑犀属。