Century Dinosaur Research at IVPP
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Anchiornis and Scansoriopterygidae
SpringerBriefs in Earth System Sciences SpringerBriefs South America and the Southern Hemisphere Series Editors Gerrit Lohmann Lawrence A. Mysak Justus Notholt Jorge Rabassa Vikram Unnithan For further volumes: http://www.springer.com/series/10032 Federico L. Agnolín · Fernando E. Novas Avian Ancestors A Review of the Phylogenetic Relationships of the Theropods Unenlagiidae, Microraptoria, Anchiornis and Scansoriopterygidae 1 3 Federico L. Agnolín “Félix de Azara”, Departamento de Ciencias Naturales Fundación de Historia Natural, CEBBAD, Universidad Maimónides Buenos Aires Argentina Fernando E. Novas CONICET, Museo Argentino de Ciencias Naturales “Bernardino Rivadavia” Buenos Aires Argentina ISSN 2191-589X ISSN 2191-5903 (electronic) ISBN 978-94-007-5636-6 ISBN 978-94-007-5637-3 (eBook) DOI 10.1007/978-94-007-5637-3 Springer Dordrecht Heidelberg New York London Library of Congress Control Number: 2012953463 © The Author(s) 2013 This work is subject to copyright. All rights are reserved by the Publisher, whether the whole or part of the material is concerned, specifically the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfilms or in any other physical way, and transmission or information storage and retrieval, electronic adaptation, computer software, or by similar or dissimilar methodology now known or hereafter developed. Exempted from this legal reservation are brief excerpts in connection with reviews or scholarly analysis or material supplied specifically for the purpose of being entered and executed on a computer system, for exclusive use by the purchaser of the work. Duplication of this publication or parts thereof is permitted only under the provisions of the Copyright Law of the Publisher’s location, in its current version, and permission for use must always be obtained from Springer. -
A New Troodontid Theropod, Talos Sampsoni Gen. Et Sp. Nov., from the Upper Cretaceous Western Interior Basin of North America
A New Troodontid Theropod, Talos sampsoni gen. et sp. nov., from the Upper Cretaceous Western Interior Basin of North America Lindsay E. Zanno1,2*, David J. Varricchio3, Patrick M. O’Connor4,5, Alan L. Titus6, Michael J. Knell3 1 Field Museum of Natural History, Chicago, Illinois, United States of America, 2 Biological Sciences Department, University of Wisconsin-Parkside, Kenosha, Wisconsin, United States of America, 3 Department of Earth Sciences, Montana State University, Bozeman, Montana, United States of America, 4 Department of Biomedical Sciences, Ohio University College of Osteopathic Medicine, Athens, Ohio, United States of America, 5 Ohio Center for Ecology and Evolutionary Studies, Ohio University, Athens, Ohio, United States of America, 6 Grand Staircase-Escalante National Monument, Bureau of Land Management, Kanab, Utah, United States of America Abstract Background: Troodontids are a predominantly small-bodied group of feathered theropod dinosaurs notable for their close evolutionary relationship with Avialae. Despite a diverse Asian representation with remarkable growth in recent years, the North American record of the clade remains poor, with only one controversial species—Troodon formosus—presently known from substantial skeletal remains. Methodology/Principal Findings: Here we report a gracile new troodontid theropod—Talos sampsoni gen. et sp. nov.— from the Upper Cretaceous Kaiparowits Formation, Utah, USA, representing one of the most complete troodontid skeletons described from North America to date. Histological assessment of the holotype specimen indicates that the adult body size of Talos was notably smaller than that of the contemporary genus Troodon. Phylogenetic analysis recovers Talos as a member of a derived, latest Cretaceous subclade, minimally containing Troodon, Saurornithoides, and Zanabazar. -
The Dashanpu Dinosaur Fauna of Zigong Sichuan Short Report V - Labyrinthodont Amphibia
The Dashanpu Dinosaur Fauna of Zigong Sichuan Short Report V - Labyrinthodont Amphibia Zhiming Dong (Institute of Vertebrate Paleontology, Paleoanthropology, Academia Sinica) Vertebrata PalAsiatica Volume XXIII, No. 4 October, 1985 pp. 301-305 Translated by Will Downs Department of Geology Bilby Research Center Northern Arizona University December, 1990 Abstract A brief discussion is presented on the morphological characteristics and phylogenetic position of Sinobrachyops placenticephalus (gen. et sp. nov.). The specimen is derived from the well-known Middle Jurassic Dashanpu dinosaur quarries of Zigong County, Sichaun Province. Sinobrachyops is the youngest geological occurrence of a labyrinthodont amphibian known to date. Its discovery extends the upper geochronological limit for the Labyrinthodontia into the Middle Jurassic. Introduction The first fossils collected from Dashanpu, Zigong, in 1979, were a pair of rhachitomous vertebrae. This discovery created a sense of perplexity among the workers, for the morphology of these pleurocentra and intercentra suggested an assignment to the Labyrinthodontia. This group of amphibians, however, was traditionally believed to have become extinct in the Late Triassic, a traditional concept that must be abandoned if scientific investigation is to be advanced and left unfettered. In 1983 the Institute of Vertebrate Paleontology, Paleoanthropology Academia Sinica launched a paleontological expedition in the Shishugou Formation (Middle-Late Jurassic) from the Kelameili region, northeast Jungar Basin, Xinjiang Autonomous Region, where several rhachitomous vertebrae were discovered. Later, a fragmentary skull of a labyrinthodont amphibian was collected, confirming that this group extended into the Middle Jurassic. The discovery from the Shishugou Formation convinced the workers that the rhachitomous vertebrae at Dashanpu belonged to the Labyrinthodontia. -
First Turtle Remains from the Middle-Late Jurassic Yanliao Biota, NE China
Vol.7, No.1 pages 1-11 Science Technology and Engineering Journal (STEJ) Research Article First Turtle Remains from the Middle-Late Jurassic Yanliao Biota, NE China Lu Li1,2,3, Jialiang Zhang4, Xiaolin Wang1,2,3, Yuan Wang1,2,3 and Haiyan Tong1,5* 1 Laboratory of Vertebrate Evolution and Human Origins of the Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China 2 CAS Center for Excellence in Life and Paleoenvironment, Beijing 100044, China 3 College of Earth and Planetary Sciences, University of China Academy of Sciences, Beijing 100044, China 4 State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Beijing 100083, China 5 Palaeontological Research and Education Centre, Mahasarakham University, Kantarawichai, Maha Sarakham 44150, Thailand * Corresponding author: [email protected] (Received: 14th August 2020, Revised: 11th January 2021, Accepted: 9th March 2021) Abstract - The Middle-Late Jurassic Yanliao Biota, preceding the Early Cretaceous Jehol Biota in NE China has yielded a rich collection of plant, invertebrate and vertebrate fossils. But contrary to the Jehol Biota which is rich in freshwater vertebrates, in the Yanliao Biota the aquatic reptiles are absent, and turtles have not been reported so far. In this paper, we report on the first turtle remains from the Yanliao Biota. The material consists of a partial skeleton from the Upper Jurassic Tiaojishan Formation of Bawanggou site (Qinglong, Hebei Province, China). Characterized by a broad skull with a pair of sulci carotici and a remnant of an interpterygoid vacuity, a well-developed anterior lobe of the plastron with mesiolaterally elongated epiplastra and a relatively large oval entoplastron; it is assigned to Annemys sp. -
Evidence of a New Carcharodontosaurid from the Upper Cretaceous of Morocco
http://app.pan.pl/SOM/app57-Cau_etal_SOM.pdf SUPPLEMENTARY ONLINE MATERIAL FOR Evidence of a new carcharodontosaurid from the Upper Cretaceous of Morocco Andrea Cau, Fabio Marco Dalla Vecchia, and Matteo Fabbri Published in Acta Palaeontologica Polonica 2012 57 (3): 661-665. http://dx.doi.org/10.4202/app.2011.0043 SOM1. PHYLOGENETIC ANALYSIS Material and Methods The data set of the phylogenetic analysis includes 37 Operational Taxonomic Units (OTUs) (35 ingroup neotheropod taxa, including one based on MPM 2594; and two basal theropod outgroups, Herrerasaurus and Tawa), and 808 character statements (see S2 and S3, below). The phylogenetic analyses were conducted through PAUP* vers. 4.010b (Swofford 2002). In the analysis, Herrerasaurus was used as root of the tree. The tree search strategy follows Benson (2009). The analysis initially performed a preliminary search using PAUPRat (Sikes and Lewis 2001). The unique topologies among the most parsimonious trees (MPTs) resulted after the preliminary search were used as a starting point for 1000 tree-bisection-reconnection branch swapping heuristic searches using PAUP*. Included taxa (and source for codings) Outgroup Herrerasaurus (Sereno 1993; Sereno and Novas 1993; Novas 1994; Sereno 2007) Tawa (Nesbitt et al. 2009) Ingroup Abelisaurus (Bonaparte and Novas 1985; Carrano and Sampson 2008) Acrocanthosaurus (Stoval and Landston 1950; Harris 1998; Currie and Carpenter 2000; Eddy and Clarke 2011) Allosaurus (Gilmore 1920; Madsen 1976) Baryonyx (Charig and Milner 1997; Mateus et al. 2010) Carcharodontosaurus (Stromer 1931; Sereno et al. 1996; Brusatte and Sereno 2007) Carnotaurus (Bonaparte et al. 1990) Ceratosaurus (Gilmore 1920; Madsen and Welles 2000). Compsognathus (Peyer 2006) Cryolophosaurus (Smith et al. -
A New Xinjiangchelyid Turtle from the Middle Jurassic of Xinjiang, China and the Evolution of the Basipterygoid Process in Mesozoic Turtles Rabi Et Al
A new xinjiangchelyid turtle from the Middle Jurassic of Xinjiang, China and the evolution of the basipterygoid process in Mesozoic turtles Rabi et al. Rabi et al. BMC Evolutionary Biology 2013, 13:203 http://www.biomedcentral.com/1471-2148/13/203 Rabi et al. BMC Evolutionary Biology 2013, 13:203 http://www.biomedcentral.com/1471-2148/13/203 RESEARCH ARTICLE Open Access A new xinjiangchelyid turtle from the Middle Jurassic of Xinjiang, China and the evolution of the basipterygoid process in Mesozoic turtles Márton Rabi1,2*, Chang-Fu Zhou3, Oliver Wings4, Sun Ge3 and Walter G Joyce1,5 Abstract Background: Most turtles from the Middle and Late Jurassic of Asia are referred to the newly defined clade Xinjiangchelyidae, a group of mostly shell-based, generalized, small to mid-sized aquatic froms that are widely considered to represent the stem lineage of Cryptodira. Xinjiangchelyids provide us with great insights into the plesiomorphic anatomy of crown-cryptodires, the most diverse group of living turtles, and they are particularly relevant for understanding the origin and early divergence of the primary clades of extant turtles. Results: Exceptionally complete new xinjiangchelyid material from the ?Qigu Formation of the Turpan Basin (Xinjiang Autonomous Province, China) provides new insights into the anatomy of this group and is assigned to Xinjiangchelys wusu n. sp. A phylogenetic analysis places Xinjiangchelys wusu n. sp. in a monophyletic polytomy with other xinjiangchelyids, including Xinjiangchelys junggarensis, X. radiplicatoides, X. levensis and X. latiens. However, the analysis supports the unorthodox, though tentative placement of xinjiangchelyids and sinemydids outside of crown-group Testudines. A particularly interesting new observation is that the skull of this xinjiangchelyid retains such primitive features as a reduced interpterygoid vacuity and basipterygoid processes. -
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. -
New Tyrannosaur from the Mid-Cretaceous of Uzbekistan Clarifies Evolution of Giant Body Sizes and Advanced Senses in Tyrant Dinosaurs
New tyrannosaur from the mid-Cretaceous of Uzbekistan clarifies evolution of giant body sizes and advanced senses in tyrant dinosaurs Stephen L. Brusattea,1, Alexander Averianovb,c, Hans-Dieter Suesd, Amy Muira, and Ian B. Butlera aSchool of GeoSciences, University of Edinburgh, Edinburgh EH9 3FE, United Kingdom; bZoological Institute, Russian Academy of Sciences, St. Petersburg 199034, Russia; cDepartment of Sedimentary Geology, Saint Petersburg State University, St. Petersburg 199178, Russia; and dDepartment of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington, DC 20560 Edited by Neil H. Shubin, The University of Chicago, Chicago, IL, and approved January 29, 2016 (received for review January 5, 2016) Tyrannosaurids—the familiar group of carnivorous dinosaurs in- We here report the first diagnostic tyrannosauroid from the mid- cluding Tyrannosaurus and Albertosaurus—were the apex predators Cretaceous, a new species from the Turonian (ca. 90–92 million in continental ecosystems in Asia and North America during the years ago) Bissekty Formation of Uzbekistan. This formation has latest Cretaceous (ca. 80–66 million years ago). Their colossal sizes recently emerged as one of the most important records of mid- and keen senses are considered key to their evolutionary and eco- Cretaceous dinosaurs globally (9–11). Possible tyrannosauroid logical success, but little is known about how these features devel- specimens from the Bissekty Formation were reported more than oped as tyrannosaurids evolved from smaller basal tyrannosauroids a half century ago (12), and, more recently, several isolated fossils that first appeared in the fossil record in the Middle Jurassic (ca. 170 were assigned to the group (9, 13), but none of these has been 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. -
Late Jurassic Theropod Dinosaur Bones from the Langenberg Quarry
Late Jurassic theropod dinosaur bones from the Langenberg Quarry (Lower Saxony, Germany) provide evidence for several theropod lineages in the central European archipelago Serjoscha W. Evers1 and Oliver Wings2 1 Department of Geosciences, University of Fribourg, Fribourg, Switzerland 2 Zentralmagazin Naturwissenschaftlicher Sammlungen, Martin-Luther-Universität Halle-Wittenberg, Halle (Saale), Germany ABSTRACT Marine limestones and marls in the Langenberg Quarry provide unique insights into a Late Jurassic island ecosystem in central Europe. The beds yield a varied assemblage of terrestrial vertebrates including extremely rare bones of theropod from theropod dinosaurs, which we describe here for the first time. All of the theropod bones belong to relatively small individuals but represent a wide taxonomic range. The material comprises an allosauroid small pedal ungual and pedal phalanx, a ceratosaurian anterior chevron, a left fibula of a megalosauroid, and a distal caudal vertebra of a tetanuran. Additionally, a small pedal phalanx III-1 and the proximal part of a small right fibula can be assigned to indeterminate theropods. The ontogenetic stages of the material are currently unknown, although the assignment of some of the bones to juvenile individuals is plausible. The finds confirm the presence of several taxa of theropod dinosaurs in the archipelago and add to our growing understanding of theropod diversity and evolution during the Late Jurassic of Europe. Submitted 13 November 2019 Accepted 19 December 2019 Subjects Paleontology, -
The Princeton Field Guide to Dinosaurs, Second Edition
MASS ESTIMATES - DINOSAURS ETC (largely based on models) taxon k model femur length* model volume ml x specific gravity = model mass g specimen (modeled 1st):kilograms:femur(or other long bone length)usually in decameters kg = femur(or other long bone)length(usually in decameters)3 x k k = model volume in ml x specific gravity(usually for whole model) then divided/model femur(or other long bone)length3 (in most models femur in decameters is 0.5253 = 0.145) In sauropods the neck is assigned a distinct specific gravity; in dinosaurs with large feathers their mass is added separately; in dinosaurs with flight ablity the mass of the fight muscles is calculated separately as a range of possiblities SAUROPODS k femur trunk neck tail total neck x 0.6 rest x0.9 & legs & head super titanosaur femur:~55000-60000:~25:00 Argentinosaurus ~4 PVPH-1:~55000:~24.00 Futalognkosaurus ~3.5-4 MUCPv-323:~25000:19.80 (note:downsize correction since 2nd edition) Dreadnoughtus ~3.8 “ ~520 ~75 50 ~645 0.45+.513=.558 MPM-PV 1156:~26000:19.10 Giraffatitan 3.45 .525 480 75 25 580 .045+.455=.500 HMN MB.R.2181:31500(neck 2800):~20.90 “XV2”:~45000:~23.50 Brachiosaurus ~4.15 " ~590 ~75 ~25 ~700 " +.554=~.600 FMNH P25107:~35000:20.30 Europasaurus ~3.2 “ ~465 ~39 ~23 ~527 .023+.440=~.463 composite:~760:~6.20 Camarasaurus 4.0 " 542 51 55 648 .041+.537=.578 CMNH 11393:14200(neck 1000):15.25 AMNH 5761:~23000:18.00 juv 3.5 " 486 40 55 581 .024+.487=.511 CMNH 11338:640:5.67 Chuanjiesaurus ~4.1 “ ~550 ~105 ~38 ~693 .063+.530=.593 Lfch 1001:~10700:13.75 2 M. -
New Tyrannosaur from the Mid-Cretaceous of Uzbekistan Clarifies Evolution of Giant Body Sizes and Advanced Senses in Tyrant Dinosaurs
Edinburgh Research Explorer New tyrannosaur from the mid-Cretaceous of Uzbekistan clarifies evolution of giant body sizes and advanced senses in tyrant dinosaurs Citation for published version: Brusatte, SL, Averianov, A, Sues, H, Muir, A & Butler, IB 2016, 'New tyrannosaur from the mid-Cretaceous of Uzbekistan clarifies evolution of giant body sizes and advanced senses in tyrant dinosaurs', Proceedings of the National Academy of Sciences, pp. 201600140. https://doi.org/10.1073/pnas.1600140113 Digital Object Identifier (DOI): 10.1073/pnas.1600140113 Link: Link to publication record in Edinburgh Research Explorer Document Version: Peer reviewed version Published In: Proceedings of the National Academy of Sciences General rights Copyright for the publications made accessible via the Edinburgh Research Explorer is retained by the author(s) and / or other copyright owners and it is a condition of accessing these publications that users recognise and abide by the legal requirements associated with these rights. Take down policy The University of Edinburgh has made every reasonable effort to ensure that Edinburgh Research Explorer content complies with UK legislation. If you believe that the public display of this file breaches copyright please contact [email protected] providing details, and we will remove access to the work immediately and investigate your claim. Download date: 04. Oct. 2021 Classification: Physical Sciences: Earth, Atmospheric, and Planetary Sciences; Biological Sciences: Evolution New tyrannosaur from the mid-Cretaceous of Uzbekistan clarifies evolution of giant body sizes and advanced senses in tyrant dinosaurs Stephen L. Brusattea,1, Alexander Averianovb,c, Hans-Dieter Suesd, Amy Muir1, Ian B. Butler1 aSchool of GeoSciences, University of Edinburgh, Edinburgh EH9 3FE, UK bZoological Institute, Russian Academy of Sciences, St.