Fossil Birds: Contributions to the Understanding of Avian Evolution
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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. -
Tiny Fossil Sheds Light on Miniaturization of Birds
Retraction Tiny fossil sheds light on miniaturization of birds Roger B. J. Benson Nature 579, 199–200 (2020) In view of the fact that the authors of ‘Hummingbird-sized dinosaur from the Cretaceous period of Myanmar‘ (L. Xing et al. Nature 579, 245–249; 2020) are retracting their report, I wish to retract this News & Views article, which dealt with this study and was based on the accuracy and reproducibility of their data. Nature | 22 July 2020 ©2020 Spri nger Nature Li mited. All rights reserved. drives the assembly of DNA-PK and stimulates regulation of protein synthesis. And, although 3. Dragon, F. et al. Nature 417, 967–970 (2002). its catalytic activity in vitro, although does so further studies are required, we might have 4. Adelmant, G. et al. Mol. Cell. Proteom. 11, 411–421 (2012). much less efficiently than can DNA. taken a step closer to deciphering the 5. Britton, S., Coates, J. & Jackson, S. P. J. Cell Biol. 202, Taken together, these observations suggest mysterious ribosomopathies. 579–595 (2013). a model in which KU recruits DNA-PKcs to the 6. Barandun, J. et al. Nature Struct. Mol. Biol. 24, 944–953 (2017). small-subunit processome. In the case of Alan J. Warren is at the Cambridge Institute 7. Ma, Y. et al. Cell 108, 781–794 (2002). kinase-defective DNA-PK, the mutant enzyme’s for Medical Research, Hills Road, Cambridge 8. Yin, X. et al. Cell Res. 27, 1341–1350 (2017). inability to regulate its own activity gives the CB2 OXY, UK. 9. Sharif, H. et al. -
Mini Page 1.28.15.Indd
© 2015 Universal Uclick Roaming North America from The Mini Page © 2015 Universal Uclick Land of Dinosaurs Gigantic dinosaurs such as It wasn’t snowing then Tyrannosaurus rex (ty-RAN- Right now, in the middle of the oh-SORE-rus RECKS) and winter, if you look at the states where Triceratops (tri-SER-uh-tops) the Hell Creek Formation is, it is hard ruled western North America 66 to imagine that in the time of the million years ago. dinosaurs it was a rainy, subtropical Dinosaurs had been roaming forest. There were no cold winters. It the Earth for about 165 million would have been much like southern years. And then, in just a few Florida today. years, all dinosaurs but birds The Earth was much warmer 66 were wiped from the planet. million to 68 million years ago, at the Much of what we know end of the Cretaceous (kruh-TAY-shus) about these awesome animals Period. There were no polar ice caps. and the land they ruled comes The planet’s sea levels were much from fossil discoveries in one higher than today. The oceans had set of rocks, the Hell Creek flooded parts of North America, Formation. This layer of rocks creating a huge inland sea. Dinosaurs covers parts of Montana, North lived to the east and west of the sea. Dakota, South Dakota and Wyoming. (It is called the Lance At the top of the Formation in Wyoming.) art, Anzu In November 2014, the (the pink art by Mary Parrish, courtesy Smithsonian National Museum of Natural History Smithsonian’s National dinosaurs) Museum of Natural History in In the background, an Edmontosaurus (ed-MON- roam toh-SAW-rus) travels through a swamp in the through Washington, D.C., opened a new Hell Creek Formation area 66 million years ago. -
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 Caenagnathid Dinosaur from the Upper Cretaceous Wangshi
www.nature.com/scientificreports OPEN A new caenagnathid dinosaur from the Upper Cretaceous Wangshi Group of Shandong, China, with Received: 12 October 2017 Accepted: 7 March 2018 comments on size variation among Published: xx xx xxxx oviraptorosaurs Yilun Yu1, Kebai Wang2, Shuqing Chen2, Corwin Sullivan3,4, Shuo Wang 5,6, Peiye Wang2 & Xing Xu7 The bone-beds of the Upper Cretaceous Wangshi Group in Zhucheng, Shandong, China are rich in fossil remains of the gigantic hadrosaurid Shantungosaurus. Here we report a new oviraptorosaur, Anomalipes zhaoi gen. et sp. nov., based on a recently collected specimen comprising a partial left hindlimb from the Kugou Locality in Zhucheng. This specimen’s systematic position was assessed by three numerical cladistic analyses based on recently published theropod phylogenetic datasets, with the inclusion of several new characters. Anomalipes zhaoi difers from other known caenagnathids in having a unique combination of features: femoral head anteroposteriorly narrow and with signifcant posterior orientation; accessory trochanter low and confuent with lesser trochanter; lateral ridge present on femoral lateral surface; weak fourth trochanter present; metatarsal III with triangular proximal articular surface, prominent anterior fange near proximal end, highly asymmetrical hemicondyles, and longitudinal groove on distal articular surface; and ungual of pedal digit II with lateral collateral groove deeper and more dorsally located than medial groove. The holotype of Anomalipes zhaoi is smaller than is typical for Caenagnathidae but larger than is typical for the other major oviraptorosaurian subclade, Oviraptoridae. Size comparisons among oviraptorisaurians show that the Caenagnathidae vary much more widely in size than the Oviraptoridae. Oviraptorosauria is a clade of maniraptoran theropod dinosaurs characterized by a short, high skull, long neck and short tail. -
New Oviraptorid Dinosaur (Dinosauria: Oviraptorosauria) from the Nemegt Formation of Southwestern Mongolia
Bull. Natn. Sci. Mus., Tokyo, Ser. C, 30, pp. 95–130, December 22, 2004 New Oviraptorid Dinosaur (Dinosauria: Oviraptorosauria) from the Nemegt Formation of Southwestern Mongolia Junchang Lü1, Yukimitsu Tomida2, Yoichi Azuma3, Zhiming Dong4 and Yuong-Nam Lee5 1 Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China 2 National Science Museum, 3–23–1 Hyakunincho, Shinjukuku, Tokyo 169–0073, Japan 3 Fukui Prefectural Dinosaur Museum, 51–11 Terao, Muroko, Katsuyama 911–8601, Japan 4 Institute of Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China 5 Korea Institute of Geoscience and Mineral Resources, Geology & Geoinformation Division, 30 Gajeong-dong, Yuseong-gu, Daejeon 305–350, South Korea Abstract Nemegtia barsboldi gen. et sp. nov. here described is a new oviraptorid dinosaur from the Late Cretaceous (mid-Maastrichtian) Nemegt Formation of southwestern Mongolia. It differs from other oviraptorids in the skull having a well-developed crest, the anterior margin of which is nearly vertical, and the dorsal margin of the skull and the anterior margin of the crest form nearly 90°; the nasal process of the premaxilla being less exposed on the dorsal surface of the skull than those in other known oviraptorids; the length of the frontal being approximately one fourth that of the parietal along the midline of the skull. Phylogenetic analysis shows that Nemegtia barsboldi is more closely related to Citipati osmolskae than to any other oviraptorosaurs. Key words : Nemegt Basin, Mongolia, Nemegt Formation, Late Cretaceous, Oviraptorosauria, Nemegtia. dae, and Caudipterygidae (Barsbold, 1976; Stern- Introduction berg, 1940; Currie, 2000; Clark et al., 2001; Ji et Oviraptorosaurs are generally regarded as non- al., 1998; Zhou and Wang, 2000; Zhou et al., avian theropod dinosaurs (Osborn, 1924; Bars- 2000). -
Appendix A. Supplementary Material
Appendix A. Supplementary material Comprehensive taxon sampling and vetted fossils help clarify the time tree of shorebirds (Aves, Charadriiformes) David Cernˇ y´ 1,* & Rossy Natale2 1Department of the Geophysical Sciences, University of Chicago, Chicago 60637, USA 2Department of Organismal Biology & Anatomy, University of Chicago, Chicago 60637, USA *Corresponding Author. Email: [email protected] Contents 1 Fossil Calibrations 2 1.1 Calibrations used . .2 1.2 Rejected calibrations . 22 2 Outgroup sequences 30 2.1 Neornithine outgroups . 33 2.2 Non-neornithine outgroups . 39 3 Supplementary Methods 72 4 Supplementary Figures and Tables 74 5 Image Credits 91 References 99 1 1 Fossil Calibrations 1.1 Calibrations used Calibration 1 Node calibrated. MRCA of Uria aalge and Uria lomvia. Fossil taxon. Uria lomvia (Linnaeus, 1758). Specimen. CASG 71892 (referred specimen; Olson, 2013), California Academy of Sciences, San Francisco, CA, USA. Lower bound. 2.58 Ma. Phylogenetic justification. As in Smith (2015). Age justification. The status of CASG 71892 as the oldest known record of either of the two spp. of Uria was recently confirmed by the review of Watanabe et al. (2016). The younger of the two marine transgressions at the Tolstoi Point corresponds to the Bigbendian transgression (Olson, 2013), which contains the Gauss-Matuyama magnetostratigraphic boundary (Kaufman and Brigham-Grette, 1993). Attempts to date this reversal have been recently reviewed by Ohno et al. (2012); Singer (2014), and Head (2019). In particular, Deino et al. (2006) were able to tightly bracket the age of the reversal using high-precision 40Ar/39Ar dating of two tuffs in normally and reversely magnetized lacustrine sediments from Kenya, obtaining a value of 2.589 ± 0.003 Ma. -
Insight Into the Evolution of Avian Flight from a New Clade of Early
J. Anat. (2006) 208, pp287–308 IBlackwnell Publishing sLtd ight into the evolution of avian flight from a new clade of Early Cretaceous ornithurines from China and the morphology of Yixianornis grabaui Julia A. Clarke,1 Zhonghe Zhou2 and Fucheng Zhang2 1Department of Marine, Earth and Atmospheric Sciences, North Carolina State University, Raleigh, NC, USA 2Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, China Abstract In studies of the evolution of avian flight there has been a singular preoccupation with unravelling its origin. By con- trast, the complex changes in morphology that occurred between the earliest form of avian flapping flight and the emergence of the flight capabilities of extant birds remain comparatively little explored. Any such work has been limited by a comparative paucity of fossils illuminating bird evolution near the origin of the clade of extant (i.e. ‘modern’) birds (Aves). Here we recognize three species from the Early Cretaceous of China as comprising a new lineage of basal ornithurine birds. Ornithurae is a clade that includes, approximately, comparatively close relatives of crown clade Aves (extant birds) and that crown clade. The morphology of the best-preserved specimen from this newly recognized Asian diversity, the holotype specimen of Yixianornis grabaui Zhou and Zhang 2001, complete with finely preserved wing and tail feather impressions, is used to illustrate the new insights offered by recognition of this lineage. Hypotheses of avian morphological evolution and specifically proposed patterns of change in different avian locomotor modules after the origin of flight are impacted by recognition of the new lineage. -
1 JOURNAL of VERTEBRATE PALEONTOLOGY a New
JOURNAL OF VERTEBRATE PALEONTOLOGY A new caenagnathid (Dinosauria: Oviraptorosauria) from the Horseshoe Canyon Formation of Alberta, Canada, and a reevaluation of the relationships of Caenagnathidae GREGORY F. FUNSTON*,,PHILIP J. CURRIE Department of Biological Sciences, CW 405, Biological Sciences Building, University of Alberta,Edmonton, Alberta, Canada T6G 2E9 [email protected]; [email protected] SUPPLEMENTARY DATA 1 1 CHARACTERS MODIFIED FROM LAMANNA ET AL. (2014) 78. Dentary: (0) elongate; (1) proportionally short and deep, with maximum depth of dentary between 25% and 50% of dentary length (with length measured from the tip of the jaw to the end of the posterodorsal process); (2) extremely short and deep, with maximum depth 50% or more of dentary length. [ORDERED] Modification—Removed [ORDERED] Justification—Mandibular variation through ontogeny in has not been qualified in oviraptorosaurs, nor has the degree of intraspecific variation. This character in particular is correlated with size in caenagnathids, such that larger specimens tend show state 0, and smaller specimens tend to show state 2, with a smooth gradient between. 84. Anterodorsal margin of dentary in lateral view: (0) straight; (1) concave; (2) broadly concave. [ORDERED] Modification—Removed [ORDERED] Justification—As above, though the opposite correlation to size is shown: large specimens tend to show state 2, and small specimens tend to show state 0. 176. Manual phalanx II-2: (0) longer than II-1; (1) subequal to or slightly shorter than II- 1; (2) distinctly shorter than II-1. [ORDERED] Modification—Removed [ORDERED] Justification—Caenagnathid manual proportions are highly variable, with a number of apparent reversals within clades. For example, Hagryphus giganteus, scored as character state 1 for this character, is consistently recovered as a basal caenagnathid, but within more derived caenagnathids, all three character states for this character are present, indicating that the character state can move both directions. -
Ciconiiformes, Charadriiformes, Coraciiformes, and Passeriformes.]
Die Vogelwarte 39, 1997: 131-140 Clues to the Migratory Routes of the Eastern Fly way of the Western Palearctics - Ringing Recoveries at Eilat, Israel [I - Ciconiiformes, Charadriiformes, Coraciiformes, and Passeriformes.] By Reuven Yosef Abstract: R euven , Y. (1997): Clues to the Migratory Routes of the Eastern Fly way of the Western Palearctics - Ringing Recoveries at Eilat, Israel [I - Ciconiiformes, Charadriiformes, Coraciiformes, and Passeriformes.] Vogelwarte 39: 131-140. Eilat, located in front of (in autumn) or behind (in spring) the Sinai and Sahara desert crossings, is central to the biannual migration of Eurasian birds. A total of 113 birds of 21 species ringed in Europe were recovered either at Eilat (44 birds of 12 species) or were ringed in Eilat and recovered outside Israel (69 birds of 16 spe cies). The most common species recovered are Lesser Whitethroat {Sylvia curruca), White Stork (Ciconia cico- nia), Chiffchaff (Phylloscopus collybita), Swallow {Hirundo rustica) Blackcap (S. atricapilla), Pied Wagtail {Motacilla alba) and Sand Martin {Riparia riparia). The importance of Eilat as a central point on the migratory route is substantiated by the fact that although the number of ringing stations in eastern Europe and Africa are limited, and non-existent in Asia, several tens of birds have been recovered in the past four decades. This also stresses the importance of taking a continental perspective to future conservation efforts. Key words: ringing, recoveries, Eilat, Eurasia, Africa. Address: International Bird Center, P. O. Box 774, Eilat 88106, Israel. 1. Introduction Israel is the only land brigde between three continents and a junction for birds migrating south be tween Europe and Asia to Africa in autumn and north to their breeding grounds in spring (Yom-Tov 1988). -
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.