Mosaic Evolution in an Asymmetrically Feathered Troodontid Dinosaur with Transitional Features
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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. -
Zheng Et Al. on the Absence of Sternal Elements In
Zheng et al. On the absence of sternal elements in Anchiornis (Paraves: Troodontidae) and Sapeornis (Aves: Pygostylia) and the complex early evolution of the avian sternum Supplementary Information 1. Table S1-S4 2. Histology description 3. Figures S1-11 4. References Tables Table 1. List of Anchiornis specimens from the Shandong Tianyu Museum of Nature as well as published material (n = 229) sorted by size. The number of gastralia is only listed when the preserved basket is relatively complete. Brackets indicate incomplete elements. Parentheses indicate number of preserved pairs of gastralia. Collection No. Complete Articulated Soft-tissue Gastralia (pairs) Femur length (>90%) (mm) STM 0-32 x x x (>10) 40 STM 0-39 x x x x 40 STM 0-132 x x — x (13) 40 STM 0-134 x — x — 40 STM 0-148 x x — x 40 STM 0-5 x x x — 41 STM 0-116 — — — — 41 STM 0-142 x x x x 41 STM 0-56 x x x x 42 STM 0-187 x x x x (>8) 42 STM 0-104 x x x x 43 STM 0-140 x x x x 43 STM 0-182 x x x x 43 STM 0-195 — — — — 43 IVPP V14378 - x - x 43.2 holotype STM 0-1 x x x — 44 STM 0-57 x x x — 44 STM 0-85 x x — x (>7) 44 STM 0-121 x x — x (>11) 44 STM 0-153 — — x x 44 STM 0-189 x x — x (>8) 44 STM 0-38 x x x — 45 STM 0-60 — — x x 45 STM 0-167 x x — x (>5) 45 STM 0-212 x x x x (>5) 45 STM 0-65 x x x x 46 STM 0-186 x x x x 46 STM 0-194 x x x x 46 STM 0-223 — x x x 46 STM 0-10 x x — x 47 STM 0-59 x x x x 47 STM 0-82 x x x x 47 STM 0-136 — x x x 47 STM 0-164 x x x x 47 STM 0-113 — — — x 48 STM 0-120 — x x x (14-15) 48 STM 0-163 — — x — 48 STM 0-58 x x x — 49 STM 0-62 x x x — 49 STM 0-77 -
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. -
Trophic Shift and the Origin of Birds
bioRxiv preprint doi: https://doi.org/10.1101/2020.08.18.256131; this version posted August 18, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC 4.0 International license. Title: Trophic shift and the origin of birds Author: Yonghua Wu Affiliations: 1School of Life Sciences, Northeast Normal University, 5268 Renmin Street, Changchun, 130024, China. 2Jilin Provincial Key Laboratory of Animal Resource Conservation and Utilization, Northeast Normal University, 2555 Jingyue Street, Changchun, 130117, China. * Corresponding author: Yonghua Wu, Ph.D Professor, School of Life Sciences Northeast Normal University 5268 Renmin Street, Changchun, 130024, China Tel: +8613756171649 Email: [email protected] 1 bioRxiv preprint doi: https://doi.org/10.1101/2020.08.18.256131; this version posted August 18, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC 4.0 International license. Abstract Birds are characterized by evolutionary specializations of both locomotion (e.g., flapping flight) and digestive system (toothless, crop, and gizzard), while the potential selection pressures responsible for these evolutionary specializations remain unclear. Here we used a recently developed molecular phyloecological method to reconstruct the diets of the ancestral archosaur and of the common ancestor of living birds (CALB). Our results showed that the ancestral archosaur exhibited a predominant Darwinian selection of protein and fat digestion and absorption, whereas the CALB showed a marked enhanced selection of carbohydrate and fat digestion and absorption, suggesting a trophic shift from carnivory to herbivory (fruit, seed, and/or nut-eater) at the archosaur-to-bird transition. -
A New Understanding of the Lower Cretaceous Jiufotang Formation in Western Liaoning
Open Journal of Geology, 2019, 9, 658-660 https://www.scirp.org/journal/ojg ISSN Online: 2161-7589 ISSN Print: 2161-7570 A New Understanding of the Lower Cretaceous Jiufotang Formation in Western Liaoning Zijie Wu1,2, Longwei Qiu1, Haipeng Wang2 1School of Geosciences, China University of Petroleum, Qingdao, China 2Liaoning Provincial Institute of Geological Exploration Co., Ltd., Dalian, China How to cite this paper: Wu, Z.J., Qiu, Abstract L.W. and Wang, H.P. (2019) A New Un- derstanding of the Lower Cretaceous Jiufo- The Lower Cretaceous Jiufotang Formation in western Liaoning is the most tang Formation in Western Liaoning. Open important fossil production horizon of the Jehol Biota, which is widely dis- Journal of Geology, 9, 658-660. tributed in the Mesozoic basins of western Liaoning. Due to the influence of https://doi.org/10.4236/ojg.2019.910067 historical data, previous scholars believed that there was no volcanic activity Received: August 16, 2019 in the Jiufotang Formation in western Liaoning. In a field investigation in Accepted: September 21, 2019 western Liaoning, the authors discovered basalt and andesite in the Hu- Published: September 24, 2019 jiayingzi bed. In addition, a conformable boundary was found between the Copyright © 2019 by author(s) and Yixian and the Jiufotang formations. It indicates that both the Jiufotang For- Scientific Research Publishing Inc. mation and the Yixian Formation are strata containing volcanic-sedimentary This work is licensed under the Creative rocks, only differing in strength of volcanic activity. Commons Attribution International License (CC BY 4.0). Keywords http://creativecommons.org/licenses/by/4.0/ Open Access Western Liaoning, Lower Cretaceous, Jiufotang Formation, Volcanic Rocks, New Discoveries 1. -
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. -
Zircon U-Pb SHRIMP Dating of the Yixian Formation in Sihetun, Northeast China
Cretaceous Research 28 (2007) 177e182 www.elsevier.com/locate/CretRes New evidence for Cretaceous age of the feathered dinosaurs of Liaoning: zircon U-Pb SHRIMP dating of the Yixian Formation in Sihetun, northeast China Wei Yang a, Shuguang Li a,*, Baoyu Jiang b a Department of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China b Department of Earth Sciences, Nanjing University, Nanjing 210093, China Accepted 30 May 2006 Available online 25 January 2007 Abstract We present the first report of U-Pb SHRIMP dating of zircons from three tuffs interbedded within the ‘‘feathered dinosaur’’-bearing deposits in western Liaoning, China. One is a sample from the Bed 6 tuff (LX-SHT-12) of the Yixian Formation in Sihetun, for which our zircon U-Pb SHRIMP analyses gave a Cretaceous age (124.7 Æ 2.7 Ma), in agreement with a previously published sanidine 40Ar/39Ar age (124.60 Æ 0.25 Ma). The other two are from the Bed 1 tuff (LX-HBJ-1) and Bed 8 tuff (LX-HBJ-6) of the Yixian Formation in Huangbanjigou; the former gave an age of 124.9 Æ 1.7 Ma, the latter an age of 122.8 Æ 1.6 Ma. The three consistent ages indicate that the Yixian Formation was deposited in the Early Cretaceous within a very short time period (ca. 2 Ma). Ó 2006 Published by Elsevier Ltd. Keywords: Zircon U-Pb SHRIMP dating; Yixian Formation; Feathered dinosaurs; Liaoning; Jehol Biota 1. Introduction still the subject of disagreement. Previously K-Ar and Rb-Sr dat- ing results for the volcanic rocks of the formation have yielded Recently, a wide variety of spectacular fossils, including the Jurassic ages of 137 Æ 7 Ma and 142.5 Æ 4Ma(Wang and Diao, ‘‘feathered dinosaurs’’ Sinosauropteryx (Chen et al., 1998), Pro- 1984). -
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. -
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. -
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. -
Molecular Evidence of Keratin and Melanosomes in Feathers of the Early Cretaceous Bird Eoconfuciusornis
Molecular evidence of keratin and melanosomes in feathers of the Early Cretaceous bird Eoconfuciusornis Yanhong Pana,1, Wenxia Zhengb, Alison E. Moyerb,2, Jingmai K. O’Connorc, Min Wangc, Xiaoting Zhengd,e, Xiaoli Wangd, Elena R. Schroeterb, Zhonghe Zhouc,1, and Mary H. Schweitzerb,f,1 aKey Laboratory of Economic Stratigraphy and Palaeogeography of the Chinese Academy of Sciences, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences Nanjing 210008, China; bDepartment of Biological Science, North Carolina State University, Raleigh, NC 27695; cKey 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; dInstitute of Geology and Paleontology, Linyi University, Linyi City, Shandong 276005, China; eShandong Tianyu Museum of Nature, Pingyi, Shandong 273300, China; and fNorth Carolina Museum of Natural Sciences, Raleigh, NC 27601 Contributed by Zhonghe Zhou, October 20, 2016 (sent for review August 10, 2016; reviewed by Dominique G. Homberger and Roger H. Sawyer) Microbodies associated with feathers of both nonavian dinosaurs reported microbodies were embedded. Whether keratinous and early birds were first identified as bacteria but have been proteins were preserved in these feathers, and the potential ex- reinterpreted as melanosomes. Whereas melanosomes in modern tent of this preservation, has not been explored. feathers are always surrounded by and embedded in keratin, Indeed, -
Re-Evaluation of the Haarlem Archaeopteryx and the Radiation of Maniraptoran Theropod Dinosaurs Christian Foth1,3 and Oliver W
Foth and Rauhut BMC Evolutionary Biology (2017) 17:236 DOI 10.1186/s12862-017-1076-y RESEARCH ARTICLE Open Access Re-evaluation of the Haarlem Archaeopteryx and the radiation of maniraptoran theropod dinosaurs Christian Foth1,3 and Oliver W. M. Rauhut2* Abstract Background: Archaeopteryx is an iconic fossil that has long been pivotal for our understanding of the origin of birds. Remains of this important taxon have only been found in the Late Jurassic lithographic limestones of Bavaria, Germany. Twelve skeletal specimens are reported so far. Archaeopteryx was long the only pre-Cretaceous paravian theropod known, but recent discoveries from the Tiaojishan Formation, China, yielded a remarkable diversity of this clade, including the possibly oldest and most basal known clade of avialan, here named Anchiornithidae. However, Archaeopteryx remains the only Jurassic paravian theropod based on diagnostic material reported outside China. Results: Re-examination of the incomplete Haarlem Archaeopteryx specimen did not find any diagnostic features of this genus. In contrast, the specimen markedly differs in proportions from other Archaeopteryx specimens and shares two distinct characters with anchiornithids. Phylogenetic analysis confirms it as the first anchiornithid recorded outside the Tiaojushan Formation of China, for which the new generic name Ostromia is proposed here. Conclusions: In combination with a biogeographic analysis of coelurosaurian theropods and palaeogeographic and stratigraphic data, our results indicate an explosive radiation of maniraptoran coelurosaurs probably in isolation in eastern Asia in the late Middle Jurassic and a rapid, at least Laurasian dispersal of the different subclades in the Late Jurassic. Small body size and, possibly, a multiple origin of flight capabilities enhanced dispersal capabilities of paravian theropods and might thus have been crucial for their evolutionary success.