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Limb ossification patterns for the Lower Jurassic (Toarcian) ichthyosaur, Stenopterygius , are described. It is found that limb ossification follows a continuous proximal to distal sequence from the propodial elements through to the terminal elements of 1st to 4th digit in the manus and the 1st to 3rd digit in the pes. The 5th manal and 4th pedal digit begin ossification later than more preaxial digits and also show evidence of proximal addition of elements near the distal mesopodial row in a manner consistent with delayed ossification of the 5th distal mesopodial in other diapsids. Ossification of manal elements in the Supernumerary 3–4 (S3-4) digit and the 5th digit appear interdependent; if one or the other is highly ossified, ossification of the other is retarded. The 1st pedal digit is considered to be lost in Stenopterygius and the 4th pedal digit is identified as the 5th digit. Delayed ossification of the mesopodium is not observed. The most preaxial proximal tarsal is identified as the centralc; the remaining proximal tarsals are the astragalus and calcaneum, and it is inferred that the astragalus and calcaneum ossified from within a single proximal cartilage.  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.
Current phylogenics of mosasauroid reptiles are reviewed and a new phylogeny examining aigialosaur interrelationships presented. Patterns of mesopodial ossification and overall limb morphology are described for adult mosasauroids. Ossification sequences are mapped onto a phylogeny in order to assess the distribution of ontogenetic characters. Consistent and ordered distributions are found. Based on the phylogenetic distribution of ossification patterns, an overall mesopodial ossification sequence for mosasaurs is proposed. Carpal sequence: ulnare—distal carpal four (dc4)—intermedium—dc3—radiale or dc2—de1 or pisiform and dc5. Tarsal sequence: astragalus—distal tarsal four or calcaneum. Skeletal paedomorphosis is recognized as a dominant pattern in the evolution of mosasauroid limbs. Apomorphic characters of skeletal paedomorphosis, apparent in most taxa, reach extremes in tylosaurs. Arguments for the presence of a single proximal cartilage in the tarsus of mosasaurs are made. This cartilage is presumed to include ossification centres from which both the astragalus and calcaneum will ossify.  相似文献   

5.
Theropod dinosaurs and birds share a specialized ankle joint in which the proximal tarsal series. the astragalus and calcaneum is braced against the tibia by an ascending process. This feature has been used since T. H. Huxley's time (1870) to support the proposal that birds evolved from dinosaurs. However, according to Martin, Stewart & Whetstone (1980), the avian tarsus is not homologous with that of theropods. They argue that while the ascending process in theropods is continuous with the astragalus in Archaeopteryx and all later birds, it is an independent ossification associated primarily with the calcaneum. A preliminary study of tarsal ontogeny in birds (McGowan, 1984), undertaken to resolve this problem, revealed two developmental pathways, one exemplified in ratites and the other in carinates. The ratite condition corresponded to that of theropods, the bony ascending process being part of the astragalus, while in carinates the corresponding process was part of the calcaneum. The present study, based on more extensive material, reveals that, although the carinate process becomes associated with the calcaneum during later development, there is evidence that it originates as a cartilaginous process from the astragalus and is therefore homologous with the ratite condition. As the avian tarsus is homologous with that of theropods, and of Archaeopteryx , it may be used to support a close phylogenetic relationship among them.  相似文献   

6.
The oldest talpid, Eotalpa, was previously known only from isolated cheek teeth from the European late Middle Eocene to earliest Oligocene. Screenwashing of Late Eocene sediments of the Hampshire Basin, UK, has yielded cranial and postcranial elements: maxilla, dentary, ulna, metacarpals, distal tibia, astragalus, calcaneum, metatarsals and phalanges. In addition to M1–2 myotodonty, typical talpid features are as follows: ulna with long medially curved olecranon and deep abductor fossa and astragalar body with lateral process. However, Eotalpa retains certain soricid‐like primitive states (M1 preparacrista, P4 with prominent mesiolingual protocone lobe, strongly angled astragalar neck and calcaneum with no space for a cuboid medial process) not found in modern talpids. Eotalpa is more derived than the most primitive living talpid Uropsilus in having lost the M1–2 talon shelf, developed a convex radial facet on the ulna, an incipient proximal olecranon crest, relatively shorter metapodials and depressed manual unguals. Its astragalus with medial trochlear ridge taller than the lateral one and massive medial plantar process is typical of the Lipotyphla. Eotalpa lacks synostosis of tibia and fibula, found in other Talpidae, Soricidae and Erinaceidae, suggesting that synostosis in these groups has been independently acquired. Cladistic analysis places Eotalpa as stem member of the Talpidae and shows that much homoplasy arose during the early evolution of the family. Ground dwelling in Eotalpa is indicated by the following: astragalus with a medially dipping head, curved in a single plane; calcaneum with distal peroneal process and strongly overlapping ectal and sustentacular facets; and matching sized ectal and sustentacular facets on calcaneum and astragalus. These features would have restricted ankle mobility. Ungual and metatarsal shape and ulnar structure suggest a primitive stage in fossorial evolution and argue against a semiaquatic precursor stage in talpid fossoriality. Shrew‐moles may represent a reversal to surface foraging rather than an intermediate stage in fossoriality.  相似文献   

7.
The homology of the fifth metatarsal in turtles and in diapsid reptiles is reassessed in the light of new phylogenetic studies. The two nearest outgroups to turtles — pareiasaurs and procolophonoids — both lack a fifth distal tarsal but retain a normal fifth metatarsal. The fifth distal tarsal was therefore lost at the base of the clade that contains turtles. Thus, the hooked fifth metatarsal in turtles must consist entirely of a modified fifth metatarsal: it does not include contributions from the fifth distal tarsal, as commonly supposed. In diapsids, loss of the fifth distal tarsal appears to have occurred at the base of crown-clade diapsids, hooking of the fifth metatarsal subsequently occurring within lepidosauromorphs, and in archosauromorphs. If so, the hooked fifth metatarsal in archosauromorphs, and some lepidosauromorphs, consists entirely of a modified fifth metatarsal. In both turtles and diapsids, integration of the elements distal to the mesotarsal joint precedes evolution of the hooked fifth metatarsal, supporting the view that the latter element evolved to perform a lever function (analogous to the “heel bone” of mammals).  相似文献   

8.
本文详细记述了陕西府谷下三叠统上部二马营组底部的一古鳄类化石.据其骨骼形态特征拟订为古鳄亚目(Proterosuchia)、引鳄科(Erythrosuchidae)的一新属种:石拐古城鳄(Guchengosuchus shiguaiensis gen. et sp. nov.),同引鳄科内已知属的对比,表明新属古城鳄与武氏鳄 Vjushkovia 的关系最为接近.  相似文献   

9.
Carpal and tarsal anatomy was documented based on the observation of dry skeletons of adult specimens representing 25 species in 15 genera and on data taken from the literature. In addition, histological sections and cleared and double‐stained autopodia of recently hatched and juvenile specimens representing seven chelid and pelomedusoid species were studied. There is much more morphological diversity in the manus than in the pes. Variation in autopodial skeletons includes: the astragalus and calcaneum are either separated or fused; fusion of distal carpals 3–4−5 or just 4–5; number of centralia in the carpus; and presence/absence of a pisiform and of an accessory radial element. The widespread and probably basal phalangeal formula for Pleurodira is 2.3.3.3.3. Deviations are Pelomedusa subrufa, exhibiting a reduction to 2.2.2.2.2, Pelusios spp. with one phalanx less in digit I and for one species in digit V as well, and Acanthochelys pallidipectoris with an additional phalanx in the fourth finger. Six discrete characters itemizing some of the morphological variation observed were plotted on a composite pleurodire phylogeny, revealing not only homoplastic patterns but also the utility of some characters in supporting the monophyly of several clades. The pisiform is the last carpal element to ossify in Chelus fimbriatus. We hypothesize that the so‐called fifth hooked metatarsal represents the fusion of distal tarsal 5 with metatarsal V. The accessory radial element that was occasionally present in the turtles examined may represent an atavism of the otherwise lost radiale of turtles.  相似文献   

10.
B. Hughes 《Journal of Zoology》1968,156(4):457-481
A new reconstruction of the tarsus of Stenaulorhynchus stockleyi differs from that previously offered by von Huene (1938) and Schaeffer (1941), and leads to a revaluation of the tarsi of other rhynchosaurs and rhynchocephalians. The tarsi of the rhynchosaurs Stenaulorhynchus, Scaphonyx, Cephalonia, Rhynchosaurus, Hyperodapedon, Howesia and Mesosuchus appear to comprise a proximal row of three bones (tibiale, intermedium, and fibulare) and a distal row of three bones associated with metatarsals–4. The metatarsals increase in length but decrease in thickness from the first to fourth, and the fifth is "hooked". The first metatarsal of Stenaulorhynchus, Scaphonyx , and Rhynchosaurus is unusually short. Among the remaining rhynchocephalians, the tarsi of claraziids and pleurosaurids are simplified in accord with aquatic habits involving the use of the limbs as paddles, and those of sphenodontids and Sapheosaurus are alike in the following respects. An astragalus (intermedium+tibiale+ centrale) and calcaneum (fibulare), or a single conjoined bone, occupy the proximal row of the tarsus and the distal row comprises four (first to fourth), three (second to fourth), or but two (third and fourth) bones; the fourth is the largest. The metatarsals increase in length from first to fourth but do not decrease in thickness. In both rhynchosaurian and spheno-dontid types tarsal movement is largely mesotarsal, a condition derived from their eosuchian ancestors and not independently developed as Schaeffer (1941) has thought. The specialization of the sphenodontid tarsus parallels that seen in lizards which have the same eosuchian ancestry.  相似文献   

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