High Rates of Evolution Preceded the Origin of Birds
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The Phylogenetic Position of Ambiortus: Comparison with Other Mesozoic Birds from Asia1 J
ISSN 00310301, Paleontological Journal, 2013, Vol. 47, No. 11, pp. 1270–1281. © Pleiades Publishing, Ltd., 2013. The Phylogenetic Position of Ambiortus: Comparison with Other Mesozoic Birds from Asia1 J. K. O’Connora and N. V. Zelenkovb aKey Laboratory of Evolution and Systematics, Institute of Vertebrate Paleontology and Paleoanthropology, 142 Xizhimenwai Dajie, Beijing China 10044 bBorissiak Paleontological Institute, Russian Academy of Sciences, Profsoyuznaya ul. 123, Moscow, 117997 Russia email: [email protected], [email protected] Received August 6, 2012 Abstract—Since the last description of the ornithurine bird Ambiortus dementjevi from Mongolia, a wealth of Early Cretaceous birds have been discovered in China. Here we provide a detailed comparison of the anatomy of Ambiortus relative to other known Early Cretaceous ornithuromorphs from the Chinese Jehol Group and Xiagou Formation. We include new information on Ambiortus from a previously undescribed slab preserving part of the sternum. Ambiortus is superficially similar to Gansus yumenensis from the Aptian Xiagou Forma tion but shares more morphological features with Yixianornis grabaui (Ornithuromorpha: Songlingorni thidae) from the Jiufotang Formation of the Jehol Group. In general, the mosaic pattern of character distri bution among early ornithuromorph taxa does not reveal obvious relationships between taxa. Ambiortus was placed in a large phylogenetic analysis of Mesozoic birds, which confirms morphological observations and places Ambiortus in a polytomy with Yixianornis and Gansus. Keywords: Ornithuromorpha, Ambiortus, osteology, phylogeny, Early Cretaceous, Mongolia DOI: 10.1134/S0031030113110063 1 INTRODUCTION and articulated partial skeleton, preserving several cervi cal and thoracic vertebrae, and parts of the left thoracic Ambiortus dementjevi Kurochkin, 1982 was one of girdle and wing (specimen PIN, nos. -
LETTER Doi:10.1038/Nature14423
LETTER doi:10.1038/nature14423 A bizarre Jurassic maniraptoran theropod with preserved evidence of membranous wings Xing Xu1,2*, Xiaoting Zheng1,3*, Corwin Sullivan2, Xiaoli Wang1, Lida Xing4, Yan Wang1, Xiaomei Zhang3, Jingmai K. O’Connor2, Fucheng Zhang2 & Yanhong Pan5 The wings of birds and their closest theropod relatives share a ratios are 1.16 and 1.08, respectively, compared to 0.96 and 0.78 in uniform fundamental architecture, with pinnate flight feathers Epidendrosaurus and 0.79 and 0.66 in Epidexipteryx), an extremely as the key component1–3. Here we report a new scansoriopterygid short humeral deltopectoral crest, and a long rod-like bone articu- theropod, Yi qi gen. et sp. nov., based on a new specimen from the lating with the wrist. Middle–Upper Jurassic period Tiaojishan Formation of Hebei Key osteological features are as follows. STM 31-2 (Fig. 1) is inferred Province, China4. Yi is nested phylogenetically among winged ther- to be an adult on the basis of the closed neurocentral sutures of the opods but has large stiff filamentous feathers of an unusual type on visible vertebrae, although this is not a universal criterion for maturity both the forelimb and hindlimb. However, the filamentous feath- across archosaurian taxa12. Its body mass is estimated to be approxi- ers of Yi resemble pinnate feathers in bearing morphologically mately 380 g, using an empirical equation13. diverse melanosomes5. Most surprisingly, Yi has a long rod-like The skull and mandible are similar to those of other scansoriopter- bone extending from each wrist, and patches of membranous tissue ygids, and to a lesser degree to those of oviraptorosaurs and some basal preserved between the rod-like bones and the manual digits. -
A New Raptorial Dinosaur with Exceptionally Long Feathering Provides Insights Into Dromaeosaurid flight Performance
ARTICLE Received 11 Apr 2014 | Accepted 11 Jun 2014 | Published 15 Jul 2014 DOI: 10.1038/ncomms5382 A new raptorial dinosaur with exceptionally long feathering provides insights into dromaeosaurid flight performance Gang Han1, Luis M. Chiappe2, Shu-An Ji1,3, Michael Habib4, Alan H. Turner5, Anusuya Chinsamy6, Xueling Liu1 & Lizhuo Han1 Microraptorines are a group of predatory dromaeosaurid theropod dinosaurs with aero- dynamic capacity. These close relatives of birds are essential for testing hypotheses explaining the origin and early evolution of avian flight. Here we describe a new ‘four-winged’ microraptorine, Changyuraptor yangi, from the Early Cretaceous Jehol Biota of China. With tail feathers that are nearly 30 cm long, roughly 30% the length of the skeleton, the new fossil possesses the longest known feathers for any non-avian dinosaur. Furthermore, it is the largest theropod with long, pennaceous feathers attached to the lower hind limbs (that is, ‘hindwings’). The lengthy feathered tail of the new fossil provides insight into the flight performance of microraptorines and how they may have maintained aerial competency at larger body sizes. We demonstrate how the low-aspect-ratio tail of the new fossil would have acted as a pitch control structure reducing descent speed and thus playing a key role in landing. 1 Paleontological Center, Bohai University, 19 Keji Road, New Shongshan District, Jinzhou, Liaoning Province 121013, China. 2 Dinosaur Institute, Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, California 90007, USA. 3 Institute of Geology, Chinese Academy of Geological Sciences, 26 Baiwanzhuang Road, Beijing 100037, China. 4 University of Southern California, Health Sciences Campus, BMT 403, Mail Code 9112, Los Angeles, California 90089, USA. -
Onetouch 4.0 Scanned Documents
/ Chapter 2 THE FOSSIL RECORD OF BIRDS Storrs L. Olson Department of Vertebrate Zoology National Museum of Natural History Smithsonian Institution Washington, DC. I. Introduction 80 II. Archaeopteryx 85 III. Early Cretaceous Birds 87 IV. Hesperornithiformes 89 V. Ichthyornithiformes 91 VI. Other Mesozojc Birds 92 VII. Paleognathous Birds 96 A. The Problem of the Origins of Paleognathous Birds 96 B. The Fossil Record of Paleognathous Birds 104 VIII. The "Basal" Land Bird Assemblage 107 A. Opisthocomidae 109 B. Musophagidae 109 C. Cuculidae HO D. Falconidae HI E. Sagittariidae 112 F. Accipitridae 112 G. Pandionidae 114 H. Galliformes 114 1. Family Incertae Sedis Turnicidae 119 J. Columbiformes 119 K. Psittaciforines 120 L. Family Incertae Sedis Zygodactylidae 121 IX. The "Higher" Land Bird Assemblage 122 A. Coliiformes 124 B. Coraciiformes (Including Trogonidae and Galbulae) 124 C. Strigiformes 129 D. Caprimulgiformes 132 E. Apodiformes 134 F. Family Incertae Sedis Trochilidae 135 G. Order Incertae Sedis Bucerotiformes (Including Upupae) 136 H. Piciformes 138 I. Passeriformes 139 X. The Water Bird Assemblage 141 A. Gruiformes 142 B. Family Incertae Sedis Ardeidae 165 79 Avian Biology, Vol. Vlll ISBN 0-12-249408-3 80 STORES L. OLSON C. Family Incertae Sedis Podicipedidae 168 D. Charadriiformes 169 E. Anseriformes 186 F. Ciconiiformes 188 G. Pelecaniformes 192 H. Procellariiformes 208 I. Gaviiformes 212 J. Sphenisciformes 217 XI. Conclusion 217 References 218 I. Introduction Avian paleontology has long been a poor stepsister to its mammalian counterpart, a fact that may be attributed in some measure to an insufRcien- cy of qualified workers and to the absence in birds of heterodont teeth, on which the greater proportion of the fossil record of mammals is founded. -
A New Crested Theropod Dinosaur from the Early Jurassic of Yunnan
第55卷 第2期 古 脊 椎 动 物 学 报 pp. 177-186 2017年4月 VERTEBRATA PALASIATICA figs. 1-3 A new crested theropod dinosaur from the Early Jurassic of Yunnan Province, China WANG Guo-Fu1,2 YOU Hai-Lu3,4* PAN Shi-Gang5 WANG Tao5 (1 Fossil Research Center of Chuxiong Prefecture, Yunnan Province Chuxiong, Yunnan 675000) (2 Chuxiong Prefectural Museum Chuxiong, Yunnan 675000) (3 Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences Beijing 100044 * Corresponding author: [email protected]) (4 College of Earth Sciences, University of Chinese Academy of Sciences Beijing 100049) (5 Bureau of Land and Resources of Lufeng County Lufeng, Yunnan 650031) Abstract A new crested theropod, Shuangbaisaurus anlongbaoensis gen. et sp. nov., is reported. The new taxon is recovered from the Lower Jurassic Fengjiahe Formation of Shuangbai County, Chuxiong Yi Autonomous Prefecture, Yunnan Province, and is represented by a partial cranium. Shuangbaisaurus is unique in possessing parasagittal crests along the orbital dorsal rims. It is also distinguishable from the other two lager-bodied parasagittal crested Early Jurassic theropods (Dilophosaurus and Sinosaurus) by a unique combination of features, such as higher than long premaxillary body, elevated ventral edge of the premaxilla, and small upper temporal fenestra. Comparative morphological study indicates that “Dilophosaurus” sinensis could potentially be assigned to Sinosaurus, but probably not to the type species. The discovery of Shuangbaisaurus will help elucidate the evolution of basal theropods, especially the role of various bony cranial ornamentations had played in the differentiation of early theropods. -
The Mesozoic Era Alvarez, W.(1997)
Alles Introductory Biology: Illustrated Lecture Presentations Instructor David L. Alles Western Washington University ----------------------- Part Three: The Integration of Biological Knowledge Vertebrate Evolution in the Late Paleozoic and Mesozoic Eras ----------------------- Vertebrate Evolution in the Late Paleozoic and Mesozoic • Amphibians to Reptiles Internal Fertilization, the Amniotic Egg, and a Water-Tight Skin • The Adaptive Radiation of Reptiles from Scales to Hair and Feathers • Therapsids to Mammals • Dinosaurs to Birds Ectothermy to Endothermy The Evolution of Reptiles The Phanerozoic Eon 444 365 251 Paleozoic Era 542 m.y.a. 488 416 360 299 Camb. Ordov. Sil. Devo. Carbon. Perm. Cambrian Pikaia Fish Fish First First Explosion w/o jaws w/ jaws Amphibians Reptiles 210 65 Mesozoic Era 251 200 180 150 145 Triassic Jurassic Cretaceous First First First T. rex Dinosaurs Mammals Birds Cenozoic Era Last Ice Age 65 56 34 23 5 1.8 0.01 Paleo. Eocene Oligo. Miocene Plio. Ple. Present Early Primate First New First First Modern Cantius World Monkeys Apes Hominins Humans A modern Amphibian—the toad A modern day Reptile—a skink, note the finely outlined scales. A Comparison of Amphibian and Reptile Reproduction The oldest known reptile is Hylonomus lyelli dating to ~ 320 m.y.a.. The earliest or stem reptiles radiated into therapsids leading to mammals, and archosaurs leading to all the other reptile groups including the thecodontians, ancestors of the dinosaurs. Dimetrodon, a Mammal-like Reptile of the Early Permian Dicynodonts were a group of therapsids of the late Permian. Web Reference http://www.museums.org.za/sam/resource/palaeo/cluver/index.html Therapsids experienced an adaptive radiation during the Permian, but suffered heavy extinctions during the end Permian mass extinction. -
Phylogeny of Basal Tetrapoda
Stuart S. Sumida Biology 342 Phylogeny of Basal Tetrapoda The group of bony fishes that gave rise to land-dwelling vertebrates and their descendants (Tetrapoda, or colloquially, “tetrapods”) was the lobe-finned fishes, or Sarcopterygii. Sarcoptrygii includes coelacanths (which retain one living form, Latimeria), lungfish, and crossopterygians. The transition from sarcopterygian fishes to stem tetrapods proceeded through a series of groups – not all of which are included here. There was no sharp and distinct transition, rather it was a continuum from very tetrapod-like fishes to very fish-like tetrapods. SARCOPTERYGII – THE LOBE-FINNED FISHES Includes •Actinista (including Coelacanths) •Dipnoi (lungfishes) •Crossopterygii Crossopterygians include “tetrapods” – 4- legged land-dwelling vertebrates. The Actinista date back to the Devonian. They have very well developed lobed-fins. There remains one livnig representative of the group, the coelacanth, Latimeria chalumnae. A lungfish The Crossopterygii include numerous representatives, the best known of which include Eusthenopteron (pictured here) and Panderichthyes. Panderichthyids were the most tetrapod-like of the sarcopterygian fishes. Panderichthyes – note the lack of dorsal fine, but retention of tail fin. Coelacanths Lungfish Rhizodontids Eusthenopteron Panderichthyes Tiktaalik Ventastega Acanthostega Ichthyostega Tulerpeton Whatcheeria Pederpes More advanced amphibians Tiktaalik roseae – a lobe-finned fish intermediate between typical sarcopterygians and basal tetrapods. Mid to Late Devonian; 375 million years old. The back end of Tiktaalik’s skull is intermediate between fishes and tetrapods. Tiktaalik is a fish with wrist bones, yet still retaining fin rays. The posture of Tiktaalik’s fin/limb is intermediate between that of fishes an tetrapods. Coelacanths Lungfish Rhizodontids Eusthenopteron Panderichthyes Tiktaalik Ventastega Acanthostega Ichthyostega Tulerpeton Whatcheeria Pederpes More advanced amphibians Reconstructions of the basal tetrapod Ventastega. -
Fins, Limbs, and Tails: Outgrowths and Axial Patterning in Vertebrate Evolution Michael I
Review articles Fins, limbs, and tails: outgrowths and axial patterning in vertebrate evolution Michael I. Coates1* and Martin J. Cohn2 Summary Current phylogenies show that paired fins and limbs are unique to jawed verte- brates and their immediate ancestry. Such fins evolved first as a single pair extending from an anterior location, and later stabilized as two pairs at pectoral and pelvic levels. Fin number, identity, and position are therefore key issues in vertebrate developmental evolution. Localization of the AP levels at which develop- mental signals initiate outgrowth from the body wall may be determined by Hox gene expression patterns along the lateral plate mesoderm. This regionalization appears to be regulated independently of that in the paraxial mesoderm and axial skeleton. When combined with current hypotheses of Hox gene phylogenetic and functional diversity, these data suggest a new model of fin/limb developmental evolution. This coordinates body wall regions of outgrowth with primitive bound- aries established in the gut, as well as the fundamental nonequivalence of pectoral and pelvic structures. BioEssays 20:371–381, 1998. 1998 John Wiley & Sons, Inc. Introduction over and again to exemplify fundamental concepts in biological Vertebrate appendages include an amazing diversity of form, theory. The striking uniformity of teleost pectoral fin skeletons from the huge wing-like fins of manta rays or the stumpy limbs of illustrated Geoffroy Saint-Hilair’s discussion of ‘‘special analo- frogfishes, to ichthyosaur paddles, the extraordinary fingers of gies,’’1 while tetrapod limbs exemplified Owen’s2 related concept aye-ayes, and the fin-like wings of penguins. The functional of ‘‘homology’’; Darwin3 then employed precisely the same ex- diversity of these appendages is similarly vast and, in addition to ample as evidence of evolutionary descent from common ances- various modes of locomotion, fins and limbs are also used for try. -
ORIGIN and EVOLUTION of BIRDS Dr. Ramesh Pathak B.Sc. (Hons.) –II
ORIGIN AND EVOLUTION OF BIRDS Dr. Ramesh Pathak B.Sc. (hons.) –II Prof. Parker has shown a number of peculiarities between birds and repiles,so,he said “birds are transformed and glorified reptiles”. Huxley has established a very close relationship by saying birds are “feathered reptiles”. THEORIES OF ORIGIN OF BIRDS A. Cursorial theory : This theory was championed by Baron Nopsa who maintained that the birds evolved from cursorial bipedal dinosaurs. In attempt to move faster during running to pull themselves a bit faster they moved and beat their arms. In such condition, due to continuous use of arms as propellers brought constant increase in the length and breadth of scales present on them. As the scales lengthened ,the pressure against the air caused their edges frayed leading to scales changing into feathers. But this theory was rejected because scales and feathers are fundamentally different structures arising from different layers of skin. B.Tetrapteryx theory :It was proposed by Beebe and Gregorg. According to this theory the ancestors of birds were arboreal reptiles who used to jump from branch to branch and in doing so the scales were transformed into feathers by fraying of the edges. After developing feathers on all the four limbs (Tetrapteryx stage), they used only the anterior wings and the unused posterior wings were lost. This theory was also discarded because there is no evidence that birds had ever four wings. C. Gliding thery : It is based on the idea of Beebe and Georg.It was proposed by Heilmann but does not recognize the tetrapteryx stage. -
Sind Vögel Dinosaurier? Eine Kritische Analyse Fossiler Befunde
W+W Special Paper B-19-4 SIND VÖGEL DINOSAURIER? EINE KRITISCHE ANALYSE FOSSILER BEFUNDE Reinhard Junker August 2019 https://www.wort-und-wissen.de/artikel/sp/b-19-4_dinos-voegel.pdf Bild: Ein rekonstruiertes und künstlerisch dargestelltes Paar von Microraptor gui (Dromaeosauridae , Micro raptorinae). (durbed.deviantart.com, CC BY-SA 3.0) Sind Vögel Dinosaurier? Inhalt 1. Einleitung ...................................................................................... 3. kompakt ..................................................................................................... 4 Methodische Vorbemerkungen ............................................................................... 5 Zitate zu schrittweisem Erwerb von Vogelmerkmalen ...................................................... 6 2. Vogelmerkmale bei Theropoden: Vorläufer oder Konvergenzen ............................................................................... 9 2.1 Federtypen und Flugfähigkeit ..................................................................... 9 2.2 Zähne und Schnabel ................................................................................ 14 Zitate zu Konvergenzen bei Zahnverlust und Ausbildung eines Schnabels ................15 2.3 Gehirn und EQ ........................................................................................ 17 2.4 Furkula ..................................................................................................... 18 2.5 Gastralia, Rippenkorb, Brustbein .............................................................. -
Cranial Osteology of Beipiaosaurus Inexpectus
第57卷 第2期 古 脊 椎 动 物 学 报 pp. 117–132 figs. 1–3 2019年4月 VERTEBRATA PALASIATICA DOI: 10.19615/j.cnki.1000-3118.190115 Cranial osteology of Beipiaosaurus inexpectus (Theropoda: Therizinosauria) LIAO Chun-Chi1,2,3 XU Xing1,2* (1 Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences Beijing 100044 * Corresponding author: [email protected]) (2 CAS Center for Excellence in Life and Paleoenvironment Beijing 100044) (3 University of Chinese Academy of Sciences Beijing 100049) Abstract Beipiaosaurus inexpectus, a key taxon for understanding the early evolution of therizinosaurians, has not been fully described since it was briefly reported on by Xu, Tang and Wang in 1999. Here we present a detailed description of the cranial anatomy of the holotype of this theropod dinosaur. B. inexpectus is unique in some of its cranial features such as the postorbital process of the frontal is large and its abrupt transition from the orbital rim, a long and sharp anterior process of the parietal, the elongate ventral ramus of the squamosal process of parietal, and external mandibular fenestra deep dorsoventrally and extremely posteriorly located. A number of plesiomorphic cranial features (such as relatively large dentary and less downturned degree of dentary symphysis) suggest that B. inexpectus is an early-branching Therizinosaurian, as proposed by previous studies. New information derived from our study is not only important for our understanding of the cranial anatomy of B. inexpectus but also significant to the study of the evolution of Therizinosauria. -
Poultry Through Time
is in a metastable state. The simulations also 3. Brandon, D. G. & Wald, M. Phil. Mag. 6, 1035–1044 Phys. Rev. Lett. 110, 255502 (2013). showed that the metastable domino phase (1961). 9. Kaur, I., Mishin, Y. & Gust, W. Fundamentals of Grain and 4. Sutton, A. P. & Balluffi, R. W. Interfaces in Crystalline Interphase Boundary Diffusion 3rd edn (Wiley, 1995). is stabilized when stress is applied perpen- Materials (Oxford Univ. Press, 1995). 10. Rittner, J. D. & Seidman, D. N. Phys. Rev. B 54, 6999–7015 dicularly to the plane of the simulated grain 5. Rabkin, E. I., Semenov, V. N., Shvindlerman, L. S. & (1996). boundary, so that its energy matches that of Straumal, B. B. Acta Metall. Mater. 39, 627–639 (1991). 11. Han, J., Vitek, V. & Srolovitz, D. J. Acta Mater. 104, 259–273 the stable pearl phase — thereby establishing 6. Cantwell, P. R. et al. Acta Mater. 62, 1–48 (2014). (2016). 7. Maksimova, E. L., Shvindlerman, L. S. & Straumal, B. B. 12. Watanabe, T. & Tsurekawa, S. Acta Mater. 47, 4171–4185 a true thermodynamic equilibrium between Acta Metall. 36, 1573–1583 (1988). (1999). the two phases. 8. Frolov, T., Divinski, S. V., Asta, M. & Mishin, Y. 13. Homer, E. R. Comp. Mater. Sci. 161, 244–254 (2019). Meiners and colleagues’ work clearly proves that phase transformations occur in the grain Palaeontology boundaries of pure metals, and thus opens up fresh opportunities for materials design. The number of possible polymorphs of bulk metals is generally limited, but the variety of Poultry through time grain-boundary structures and their poss- ible metastable polymorphs (sometimes Kevin Padian referred to as complexions6) is essentially boundless10,11.