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1.
1963年在新疆阜康曾经发现过肯氏兽的材料,这批化石中有被称为“九龙壁”的一群个体。这些化石曾被归入副肯氏兽属,命名为短吻副肯氏兽(Parakannemeyeria brevirostris)(孙艾玲,1978)。最近依据这个种建立了一个新属:西域肯氏兽(Xiyukannemeyeria),于是新疆的肯氏兽与华北的肯氏兽就没有相同属了(刘俊、李锦玲,2003)。  相似文献   

2.
记述了新疆吐鲁番中三叠统克拉玛依组肯氏兽类一新材料 ,它与短吻副肯氏兽(Parakannemeyeriabrevirostris)正模特征相似 ,确定二者为同种。将中国已知的中国肯氏兽及副肯氏兽属的所有种进行支序分析 ,发现短吻副肯氏兽与中国肯氏兽及副肯氏兽属的其他种构成姊妹群。在与肯氏兽类其他相关属比较的基础上 ,建议以短吻种为基础建立一新属 :西域肯氏兽 (Xiyukannemeyeria)。  相似文献   

3.
近几十年,华北的二马营组上部地层以产出中国肯氏兽-山西鳄四足动物化石组合而闻名.最近在山西临县白道峪于上覆的铜川组一段发现了中国肯氏兽.本文描述了同一地点同一层位产出的主龙型类化石,包括一具山西鳄的部分骨架以及一些可以归入suchian的主龙类.它们是铜川组一段首次记述的主龙型类.最有鉴定特征的suchian材料包括一个大的髂骨以及一个小的、形状很奇特的、可能是跟骨的骨骼.髂骨可能可以归入一个奇异的波波龙类(poposauroid).因为中国肯氏兽与山西鳄同时出现在白道峪,表明中国肯氏兽-山西鳄组合可以向上延伸到铜川组一段.髂骨与跟骨大小悬殊,可能代表两个从未在中国肯氏兽-山西鳄组合报道过的物种.白道峪发现了特化的波波龙类,支持了波波龙类在中三叠世大量分化的观点.  相似文献   

4.
近几十年,华北的二马营组上部地层以产出中国肯氏兽–山西鳄四足动物化石组合而闻名。最近在山西临县白道峪于上覆的铜川组一段发现了中国肯氏兽。本文描述了同一地点同一层位产出的主龙型类化石,包括一具山西鳄的部分骨架以及一些可以归入suchian的主龙类。它们是铜川组一段首次记述的主龙型类。最有鉴定特征的suchian材料包括一个大的髂骨以及一个小的、形状很奇特的、可能是跟骨的骨骼。髂骨可能可以归入一个奇异的波波龙类(poposauroid)。因为中国肯氏兽与山西鳄同时出现在白道峪,表明中国肯氏兽–山西鳄组合可以向上延伸到铜川组一段。髂骨与跟骨大小悬殊,可能代表两个从未在中国肯氏兽–山西鳄组合报道过的物种。白道峪发现了特化的波波龙类,支持了波波龙类在中三叠世大量分化的观点。  相似文献   

5.
四足动物组合带是全球陆相三叠系对比的有力手段,但是迄今为止中三叠世的四足动物组合尚没有可靠的时间框架。报道了5个采自二马营组和铜川组,与四足动物化石共同产出的火山凝灰岩样品的锆石化学剥蚀-热电离质谱法年龄。结果表明中国肯氏兽动物群时代为安尼期晚期,而永和鳄的时代为拉丁期早期。通过生物地层对比,这一结果还为其他中三叠世的四足动物组合,如南非的犬颌兽带上部、俄罗斯的引鳄动物群以及新疆的克拉玛依组提供了准确的年龄。鄂尔多斯盆地下中三叠统界线应低于二马营组底界。  相似文献   

6.
<正> 肯氏兽类在我国产出相当丰富,过去曾发现于山西二马营组的上部和新疆小泉沟群的下部,化石计有两属六种,时代均为中三迭世。近年,地质科学院程政武在陕西府谷县二马营组底部发现一十分完整的肯氏兽头骨,另立一新属,命名为戏楼沟陕北肯氏兽Shanbeikannemeyeria xilougouensis(尚未发表)。内蒙地区过去从一些破碎的牙齿及骨片上也确定过存在肯氏兽类。我所二、三迭纪组一九七六年野外工作期间在内蒙伊克昭盟准格尔旗布尔洞公社采到一具不完整的肯氏兽骨架(包括头骨),现报道如下。依据化石的  相似文献   

7.
自許耐首次发表了在中国发見的迷齿兽以来(1958),我們陆續累积了一些这一类化石的材料。虽然这些材料也很破碎,但还有必要把它們記述一下,以补足武乡、榆社区的中国肯氏兽动物羣的研究。  相似文献   

8.
Ⅰ.什么是山西武乡中国肯氏兽动物羣 1936年曾在山西武乡县邻境榆社县的銀交附近,发現一批三迭紀的脊椎动物化石,曾鑑定作皮氏中国肯氏兽(Sinokannemeyeria pearsoni Young)。因为这种动物和南非哈鲁系  相似文献   

9.
选择生长健壮的30~60年生成年肯氏南洋杉Araucaria cunninghamii母树进行采种,播种前种子去皮处理,幼苗期加强水肥管理和病虫害防治以提高实生苗苗木质量。以根长、地径和苗高为肯氏南洋杉1、2年生实生苗分级的质量指标,应用快速聚类法K-Means分别进行聚类分析,将苗木分为3级。1年生实生苗苗高(≤12 cm)、地径(≤2.5 cm)过小,不适合出圃造林;2年生实生苗中的Ⅰ级苗和Ⅱ级苗根长、地径、苗高指标均符合出圃造林标准,可以出圃;2年生实生苗中Ⅲ级苗地径、苗高依然未达到出圃标准,不建议出圃。  相似文献   

10.
记述了2012年在山西柳林三交二马营组上部采集的一个兽头类下颌标本,将其命名为幻阔齿兽三交种(Nothogomphodon sanjiaoensis sp.nov.)。新种以下列特征区别于属型种N.danilovi:齿骨下缘起伏,犬齿基部卵圆形,犬齿与第一犬后齿间有显著间隙,犬后齿后缘无辅助齿尖。幻阔齿兽以其特殊的犬后齿形态与具裂齿的基干犬齿兽相似,它也是已知的唯一一类具有这种复杂裂齿齿系的兽头类。将俄罗斯的引鳄动物群与中国的肯氏兽-山西鳄组合带进行比较发现,幻阔齿兽是二者唯一共有的属,而中国的二马营组与克拉玛依组却没有共享的属。  相似文献   

11.
30多年来,中国新近纪堆积物中发现了大量的小哺乳动物化石,但一些种类的材料很少,而且仅在个别地点出现,在动物群中常以未定属、种记述.详细描述了4种罕见的啮齿动物,其中3种,泗洪豪鼠(Sayimys sihongensis)、亚洲别齿始鼠(Apeomys asiaticus)和新来鼠(未定种)(Neocometes sp.)发现于江苏泗洪早中新世下草湾组,一种,细小云南始鼠(Yuneomys pusillus)产自云南禄丰晚中新世石灰坝组.与欧亚或北美有关材料的比较研究表明,江苏泗洪标本无法归入相关属的任何已知种,因此被确定了两个新种(S.sihongensis和A.asiaticus);禄丰原归入Leptodontomys pusillus的标本与该属的特征不符,被指定为新属Ynueomys.泗洪的A.asiaticus和Neocometes sp.分别代表该属在亚洲和中国的首次记录;它们与S.sihongensis在亚洲远东地区的出现,增加了我们对这些稀有动物地理分布和欧亚古生物地理关系的知识.禄丰的新属Yuneomys与共生的Plesieomys和Heteroeomys属同为丘齿型始鼠类,可能都属热带或亚热带森林型动物;在禄丰动物群中缺少脊齿型始鼠类,与华北动物群的组成不同,似乎表明华南和华北始鼠动物群在中新世期间已有明显的分异,进而支持这一时期亚洲出现了不同生态区系的设想.  相似文献   

12.
三叶虫是寒武纪演化动物群中最引人注目的成员之一,其内部解剖结构一直以来受到广泛关注。与其他非生物矿化软体结构相比,三叶虫的消化系统更容易留下化石记录,为探索其内部结构提供了难得的机会。本文描述了来自山东省潍坊市寒武系馒头组的Proasaphiscus, Lioparia, Deiradonyx和Iranoleesia,以及临沂市寒武系张夏组的Maotunia共五个三叶虫属的消化系统。这些保存较好的标本展示了三叶虫的四对头部消化腺,以及可能的头部消化腺与"嗉囊"共存的例子,为了解三叶虫消化系统尤其是头部消化系统的结构提供了新的信息。三叶虫非生物矿化软体结构的保存也显示了这些层位有发现布尔吉斯页岩型特异埋藏化石的潜力。  相似文献   

13.
An early Oligocene (Rupelian) diagnostic larger foraminiferal assemblage is described and illustrated from marls and limestones of the Asmari Formation, at Jabals Hafit and Malaqet in the UAE. An equivalent assemblage is identified in the mudstones of the Tahwah Formation, Wadi Suq, Oman. Although Nummulites intermedius (D'Archiac 1846) and N. fichteli are fully synonymous (e.g. Roveda 1970; Schaub 1981; Sirel 2003), in this study both species are biometrically differentiated, distinct and both names are valid. N. fichteli Michelotti 1841, N. intermedius (D'Archiac 1846) and N. emiratus n. sp., which are index for the early Oligocene (Rupelian), and they are replacing each others competitively and environmentally.

The presence of Blondeauina bouillei n.gen., N. emiratus n.sp., N. intermedius, N. fichteli, Planoperculina complanata (Defrance 1822) and Austrotrillina asmariensis Adams 1968 ascribed the section of the Asmari Formation to the early Oligocene (Rupelian). The studied marls and limestones were deposited in outer and inner shelf environments, respectively. The Asmari Formation in the area studied consists mainly of marl in its lower portion and reefal limestone in its upper part, indicating a major marine regression. The Tahwah Formation in Oman is composed of bioturbated silty and muddy marls and is a facies equivalent to the Asmari Formation marls. The Asmari Formation facies change probably relates to a mid-Oligocene fall in global sea level.

In this study, the Dabaa Formation, a subsurface unit of late Eocene–Oligocene marine shales in the north Western Desert of Egypt, was chosen to correlate with the Oligocene of Emirates and Oman. The Dabaa Formation comprises Spiroclypeus ornatus (Henson 1937) and Eulepidina dilatata (Michelotti 1861). The environment of deposition was inner shelf to littoral, which become estuarine towards the top in many areas. This Oligocene Dabaa sequence is correlatable with Wadi El Arish sequence recently discovered by Kuss and Boukhary (2008) from Risan Aneiza, Northern Sinai, Egypt.  相似文献   

14.
We report the oldest fossil evidence of osteophagia by terrestrial invertebrates on both the Asian and African continents. Bones attributable to the Middle Jurassic dinosaur Chuanjiesaurus (Dinosauria: Sauropoda) were found with post-mortem insect modification in the Chuanjie Formation, Yunnan Province, China. The morphology of the borings closely matches the ichnogenus Cubiculum. Based on the lack of bioglyphs observed in Cubiculum ornatus, a new ichnospecies is proposed here. The new trace fossil, Cubiculum inornatus isp. nov., is interpreted to have been constructed for pupation by an unknown taxon of insect. Additionally, we report even older borings from Early Jurassic dinosaur bones of the Elliott Formation in the Karoo Basin, which represent the second oldest occurrence of insect traces in bone from continental settings. Both trace fossils sites have palaeogeographic implications for the origins and dispersal of osteophagia amongst terrestrial invertebrates during the Mesozoic. These discoveries push back the antiquity of pupation in animal bones by more than 100 million years to the Middle Jurassic, indicating that this behaviour, and osteophagy more generally, originated early in the Mesozoic, roughly comparable with the origination of insect pupation in woody substrates (Late Triassic).  相似文献   

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We report the largest known British specimen of the metriorhynchid crocodylomorph genus Dakosaurus discovered offshore from Chesil Beach, Dorset, England (Kimmeridge Clay Formation). This specimen is large toothed, which has extreme enamel spalling on the labial surface, enlarged carinae (‘carinal flanges’), carinal wear, macroziphodont denticles, and the crown retains much of its labiolingual width along most of its apicobasal length. This suite of morphologies is unique to Dakosaurus. All known Kimmeridge Clay Formation Dakosaurus specimens are isolated tooth crowns. A skull previously referred to Dakosaurus lacks all the cranial apomorphies of D. maximus and D. andiniensis, and cannot be referred to this genus. Furthermore, the vast majority of putative Dakosaurus tooth crowns from the ‘Potton Sands’ ( = Woburn Sands Formation) do indeed represent Dakosaurus (as well as two Plesiosuchus specimens), and they most likely originate from the Kimmeridge Clay Formation.  相似文献   

17.
Only two vertebrate trackways are known from the Paleocene of western Canada and are among the few Paleocene vertebrate trackways known worldwide.

A natural cast trackway consisting of five prints (three pes, two manus) on a fallen block was found along the Red Deer River, near the town of Red Deer, Alberta, in 1927. The discoverers, Ralph Rutherford and Loris Russell, identified the strata the track block had fallen from as belonging to the Paskapoo Formation (upper Paleocene: middle Tiffanian). The trackway was attributed to a mammalian track-maker in two subsequent publications. However, the prints are more characteristic of a reptilian (crocodylian) track-maker.

A natural cast track-bearing block was discovered on Signal Hill in the city of Calgary during the preparation of a new residential subdivision in 1990. The large track-bearing block was found in a rock pile but is suspected to have originated from strata belonging to the Porcupine Hills Formation (Upper Paleocene: late Torrejonian), which was being excavated at the time. This large slab contains twelve prints (six pes, six manus) and is associated with extensive mud cracks. The mammalian affinity of the trackmaker was recognized by researchers from the Royal Tyrrell Museum of Palaeontology.  相似文献   

18.
Abstract:  Three new genera and four new species of the extinct mantidfly subfamily Mesomantispinae (Insecta: Neuroptera: Mantispidae) are described from the Lower Cretaceous Yixian Formation of Liaoning and the Middle Jurassic Jiulongshan Formation of Inner Mongolia: Archaeodrepanicus nuddsi gen. et sp. nov., A. acutus gen. et sp. nov., Sinomesomantispa microdentata gen. et sp. nov., (Yixian Formation) and Clavifemora rotundata gen. et sp. nov. (Jiulongshan Formation). The specimens described herein represent the first Mesozoic mantidfly compression fossils to have body parts preserved, including the specialized raptorial forelegs articulated to the prothorax anteriorly, an autapomorphy of the family. These new taxa further confirm the placement of the subfamily Mesomantispinae within the family Mantispidae; however, the monophyly of Mesomantispinae has not been confirmed, and it is likely that it will prove to be paraphyletic.  相似文献   

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