Maleyev 106 Therizinosaurus Cheloniformis
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The Paleontograph______
__________The Paleontograph________ A newsletter for those interested in all aspects of Paleontology Volume 5 Issue 1 March, 2016 _________________________________________________________________ From Your Editor Welcome to our latest issue. I hope you enjoyed the holidays. If you are anything like me, you are looking forward to Spring. We've had a mild winter here in CO. Weather is different than the east coast. While the nights are colder, the days are warmer. It's a nice change for me. I finally have my fossil lab up and running and I am spending my days, or part thereof, working off my backlog of fossils. It has been a couple of months since our last issue but Bob has kept writing and so we have an interesting issue for you to enjoy. The Paleontograph was created in 2012 to continue what was originally the newsletter of The New Jersey Paleontological Society. The Paleontograph publishes articles, book reviews, personal accounts, and anything else that relates to Paleontology and fossils. Feel free to submit both technical and non-technical work. We try to appeal to a wide range of people interested in fossils. Articles about localities, specific types of fossils, fossil preparation, shows or events, museum displays, field trips, websites are all welcome. This newsletter is meant to be one by and for the readers. Issues will come out when there is enough content to fill an issue. I encourage all to submit contributions. It will be interesting, informative and fun to read. It can become whatever the readers and contributors want it to be, so it will be a work in progress. -
The Endoskeletal Origin of the Turtle Carapace
ARTICLE Received 7 Dec 2012 | Accepted 3 Jun 2013 | Published 9 Jul 2013 DOI: 10.1038/ncomms3107 OPEN The endoskeletal origin of the turtle carapace Tatsuya Hirasawa1, Hiroshi Nagashima2 & Shigeru Kuratani1 The turtle body plan, with its solid shell, deviates radically from those of other tetrapods. The dorsal part of the turtle shell, or the carapace, consists mainly of costal and neural bony plates, which are continuous with the underlying thoracic ribs and vertebrae, respectively. Because of their superficial position, the evolutionary origins of these costo-neural elements have long remained elusive. Here we show, through comparative morphological and embryological analyses, that the major part of the carapace is derived purely from endos- keletal ribs. We examine turtle embryos and find that the costal and neural plates develop not within the dermis, but within deeper connective tissue where the rib and intercostal muscle anlagen develop. We also examine the fossils of an outgroup of turtles to confirm that the structure equivalent to the turtle carapace developed independently of the true osteoderm. Our results highlight the hitherto unravelled evolutionary course of the turtle shell. 1 Laboratory for Evolutionary Morphology, RIKEN Center for Developmental Biology, Kobe 650-0047, Japan. 2 Division of Gross Anatomy and Morphogenesis, Department of Regenerative and Transplant Medicine, Niigata University, Niigata 951-8510, Japan. Correspondence and requests for materials should be addressed to T.H. (email: [email protected]). NATURE COMMUNICATIONS | 4:2107 | DOI: 10.1038/ncomms3107 | www.nature.com/naturecommunications 1 & 2013 Macmillan Publishers Limited. All rights reserved. ARTICLE NATURE COMMUNICATIONS | DOI: 10.1038/ncomms3107 wo types of skeletal systems are recognized in vertebrates, exoskeletal components into the costal and neural plates (Fig. -
Luis V. Rey & Gondwana Studios
EXHIBITION BY LUIS V. REY & GONDWANA STUDIOS HORNS, SPIKES, QUILLS AND FEATHERS. THE SECRET IS IN THE SKIN! Not long ago, our knowledge of dinosaurs was based almost completely on the assumptions we made from their internal body structure. Bones and possible muscle and tendon attachments were what scientists used mostly for reconstructing their anatomy. The rest, including the colours, were left to the imagination… and needless to say the skins were lizard-like and the colours grey, green and brown prevailed. We are breaking the mould with this Dinosaur runners, massive horned faces and Revolution! tank-like monsters had to live with and defend themselves against the teeth and claws of the Thanks to a vast web of new research, that this Feathery Menace... a menace that sometimes time emphasises also skin and ornaments, we reached gigantic proportions in the shape of are now able to get a glimpse of the true, bizarre Tyrannosaurus… or in the shape of outlandish, and complex nature of the evolution of the massive ornithomimids with gigantic claws Dinosauria. like the newly re-discovered Deinocheirus, reconstructed here for the first time in full. We have always known that the Dinosauria was subdivided in two main groups, according All of them are well represented and mostly to their pelvic structure: Saurischia spectacularly mounted in this exhibition. The and Ornithischia. But they had many things exhibits are backed with close-to-life-sized in common, including structures made of a murals of all the protagonist species, fully special family of fibrous proteins called keratin fleshed and feathered and restored in living and that covered their skin in the form of spikes, breathing colours. -
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. -
On Certain Portions of the Skeleton of Protostega Gigas
f %VJ*p^V;^.:H ^^BSdm^% ''Sv ; ^^v;Vv: , ^ ^fc;iS^^ BS^HK9|%^-S-r^ jftaming anb jt'alior. LIBRARY I University "of Illinois. m?; 1&:. mT"-g&K y r r * ^-v^wuiiii uiio w\ji\. mi \ji UCiUl'T^ tile * Latest Date stamped below. A i charge is made on all overdue b kS - U. of I. Library FIELD COLUMBIAN MUSEUM PUBLICATION 7. ZOOLOGICAL SERIES. VOL. i, No. 2. ON CERTAIN PORTIONS OF THE SKELETON OF PROTOSTEGA GIGAS. BY O. P. HAY, PH. D., Assistant Curator of Ichthyology. D. G. ELLIOT, F. R. S. E., Curator of Department. CHICAGO, U. S. A. November 21, 1895, ON CERTAIN PORTIONS OF THE SKELETON OF PROTOS- TEGA GIGAS COPE. O. P. HAY. The Dermochelyoid turtle, Protostega gigas, was first described by Professor E. D. Cope in Proc. Amer. Phil. Soc., 1-871, page 172, and again in the same publication in 1872, page 403. In 1875, m n ^ s ''Cretaceous Vertebrata," pp. 99-113, pis. IX-XIII, the same writer more fully described and illustrated the structure of this remarkable reptile. The materials which were in Professor Cope's hands consisted of a number of vertebrae, ten ribs, some marginal bones, certain por- tions of the skull, some limb bones, and some large plates. Of the lat- ter there were what the describer regarded as two entire and parts of one or two others. These plates he considered as belonging to the carapace, and this was supposed to be free from the ribs, as the pecu- liar carapace otDermochelys is free from the ribs of that turtle. -
Therizinosaurus Cheloniformis
3-EURO-SUPERSAURS THERIZINOSAURUS CHELONIFORMIS Series Supersaurs Appearances can be deceptive. Weighing five tons, up to ten metres tall and boas- ting sharp claws that were longer than those of any other land animal that has ever Face value ¤ 3 existed, the Therizinosaurus was not as dangerous as it looked. The subject of the Date of Issue 17 February 2021 sixth coin in the superlative Supersaurs series was actually a vegetarian and its claws Design K. Kuntner/ H. Andexlinger more suited to detaching vegetation than attacking the other animals that roamed Diameter 34 mm the planet some 70 million years ago. Quality Uncirculated Mintage 65,000 As a theropod, Therizinosaurus cheloniformis was not only distantly related to pre- Alloy Coloured metal dators such as Tyrannosaurus rex but also to present-day birds. Originally carnivor- Total Weight 16.00 g ous, over time the Therizinosaurus changed its diet and became a pure herbivore. Edge Plain During the late Cretaceous period, it lived in areas of the northern continent of Colour application, glow in the dark, Laurasia that now correspond to North America, China and Mongolia. Up to one no packaging. metre in length, flat, curved and pointed at the end, the dinosaur’s claws are re- sponsible for its nickname, ‘scythe lizard’. They were used primarily to reach high Recommended branches in trees as well as perhaps for self-defence. Well preserved remains of one initial issue price: ¤ 12.60 (incl. 20% VAT) of its close relatives have suggested that, rather surprisingly, the Therizinosaurus was also partially feathered. WITH COIN MOTIF COLOURED GLOW-IN-THE-DARK Therizinosaurus features all 12 of the extreme prehistoric animals in the Supersaurs EFFECT series in silhouette on its obverse, while a colour-printed Therizinosaurus is shown in its native prehistoric habitat next to a nest full of eggs on the coin’s glow-in-the- dark reverse. -
ZOOLOGY Exploring the Biodiversity of Colorado and Theworld
CHAPTER 4 — ZOOLOGY Exploring the Biodiversity of Colorado and the World CHAPTER 4 ZOOLOGY Exploring the Biodiversity of Colorado and the World Jeffrey T. Stephenson, Before the Museum Paula E. Cushing, The first collections of specimens that make up what is now the Denver John R. Demboski, and Museum of Nature & Science were actually established well before the Frank-T. Krell founding of the institution in 1900, the selection of a board of trustees, or the construction of a building to house and exhibit the specimens. Edwin Carter (1830–1900) (Fig. 4.1) collected Colorado birds and mammals from the 1860s through the 1890s. Born in New York in 1830, Carter arrived in Colorado in 1859 hoping to make it rich in the goldfields, but he soon became interested in the region’s natural history. He learned hide tanning and, as his prospects for hitting the mother lode faded, he earned his living selling buckskin clothing that he handcrafted. Carter supplemented these earnings by mar- keting foodstuffs and other provisions to the growing population of successful and (mostly) unsuccessful prospectors flooding the region. His interest in nature turned to concern as he observed dwindling numbers of mammals and birds, owing largely to habitat destruction and overhunting. Period photographs of the area’s mining district show a landscape largely denuded of vegetation. By the 1870s, Carter noted that many animal species were becoming scarce. The state’s forests were being devastated, ranches and farms were replacing open prairie, and some species, including the last native bison in Colorado, were on the verge of extirpation or extinction. -
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. -
Comparative Bone Histology of the Turtle Shell (Carapace and Plastron)
Comparative bone histology of the turtle shell (carapace and plastron): implications for turtle systematics, functional morphology and turtle origins Dissertation zur Erlangung des Doktorgrades (Dr. rer. nat.) der Mathematisch-Naturwissenschaftlichen Fakultät der Rheinischen Friedrich-Wilhelms-Universität zu Bonn Vorgelegt von Dipl. Geol. Torsten Michael Scheyer aus Mannheim-Neckarau Bonn, 2007 Angefertigt mit Genehmigung der Mathematisch-Naturwissenschaftlichen Fakultät der Rheinischen Friedrich-Wilhelms-Universität Bonn 1 Referent: PD Dr. P. Martin Sander 2 Referent: Prof. Dr. Thomas Martin Tag der Promotion: 14. August 2007 Diese Dissertation ist 2007 auf dem Hochschulschriftenserver der ULB Bonn http://hss.ulb.uni-bonn.de/diss_online elektronisch publiziert. Rheinische Friedrich-Wilhelms-Universität Bonn, Januar 2007 Institut für Paläontologie Nussallee 8 53115 Bonn Dipl.-Geol. Torsten M. Scheyer Erklärung Hiermit erkläre ich an Eides statt, dass ich für meine Promotion keine anderen als die angegebenen Hilfsmittel benutzt habe, und dass die inhaltlich und wörtlich aus anderen Werken entnommenen Stellen und Zitate als solche gekennzeichnet sind. Torsten Scheyer Zusammenfassung—Die Knochenhistologie von Schildkrötenpanzern liefert wertvolle Ergebnisse zur Osteoderm- und Panzergenese, zur Rekonstruktion von fossilen Weichgeweben, zu phylogenetischen Hypothesen und zu funktionellen Aspekten des Schildkrötenpanzers, wobei Carapax und das Plastron generell ähnliche Ergebnisse zeigen. Neben intrinsischen, physiologischen Faktoren wird die -
(Chelonioidea: Cheloniidae) from the Maastrichtian of the Harrana Fauna–Jordan
Kaddumi, Gigantatypus salahi n.gen., n.sp., from Harrana www.PalArch.nl, vertebrate palaeontology, 3, 1, (2006) A new genus and species of gigantic marine turtles (Chelonioidea: Cheloniidae) from the Maastrichtian of the Harrana Fauna–Jordan H.F. Kaddumi Eternal River Museum of Natural History Amman–Jordan, P.O. Box 11395 [email protected] ISSN 1567–2158 7 figures Abstract Marine turtle fossils are extremely rare in the Muwaqqar Chalk Marl Formation of the Harrana Fauna in comparison to the relatively rich variety of other vertebrate fossils collected from this locality. This paper reports and describes the remains of an extinct marine turtle (Chelonioidea) which will be tentatively assigned to a new genus and species of marine turtles (Cheloniidae Bonaparte, 1835) Gigantatypus salahi n.gen., n.sp.. The new genus represented by a single well–preserved right humerus, reached remarkably large proportions equivalent to that of Archelon Wieland, 1896 and represents the first to be found from this deposit and from the Middle East. The specimen, which exhibits unique combinations of features is characterized by the following morphological features not found in other members of the Cheloniidae: massive species reaching over 12 feet in length; a more prominently enlarged lateral process that is situated more closely to the head; a ventrally situated capitellum; a highly laterally expanded distal margin. The presence of these features may warrant the placement of this new species in a new genus. The specimen also retains some morphological features found in members of advanced protostegids indicating close affinities with the family. Several bite marks on the ventral surface of the fossilized humerus indicate shark–scavenging activities of possibly Squalicorax spp. -
Applications in Paleohistology: Osteohistology of Protostega Gigas
Applications in Paleohistology: Osteohistology of Protostega gigas Laura Wilson, Hannah Hutchinson, Theodore Vlamis, Logan White Department of Geosciences, Fort Hays State University INTRODUCTION RESULTS DISCUSSION Protostega gigas was a large sea turtle (Fig. 1) that lived in the In the femur of VP-17979, the cortical bone is spongiose, with There has been very little previous research on sea turtle bone Late Cretaceous Western Interior Seaway of North America (Fig. 2). large networks of vascular canals and little or no open medullary microstructure, and no other histology study has looked at Protostega fossils are found in the Smoky Hill Member of the cavity at the center of the bone (Fig. 3). The center of the bone has a Protostega, specifically. One study on the long bone histology of the Niobrara Formation in Kansas. Despite their abundance, little is more spongiose texture, there is no obvious decreases in vascular sea turtle Dermochelys (leatherback sea turtle) found spongious bone known about how these turtles grew and aged. Osteohistology is canal size toward the periosteal surface. Vascular canal orientation is through the entire cortex, with concentrically-organized longitudinal the study of bone microstructure, and is used to study bone growth dominated by longitudinal and circumferential canals organized in vascular canals (Houssaye, 2012). The Protostega bone analyzed in rates. Microstructure and growth rates directly relate to phylogeny concentric layers. Vascular canals increase in circumferential this study has a similar microstructure to that described for (evolutionary relationships), ontogeny (growth stage), biomechanics organization towards the outer cortex (Fig. 3). Dermochelys. However, Protostega has more circumferentially (how a bone is used), and environment (Ricqles et al., 1991; Horner Parallel-fibered bone encircled the vascular canals, while woven oriented vascular canals and a slightly less spongiose medullary et al., 2000; Padian and Lamm, 2013). -
An Unusual Basal Therizinosaur Dinosaur with an Ornithischian Dental Arrangement from Northeastern China
An Unusual Basal Therizinosaur Dinosaur with an Ornithischian Dental Arrangement from Northeastern China Hanyong Pu1, Yoshitsugu Kobayashi2*, Junchang Lu¨ 3*,LiXu1, Yanhua Wu1, Huali Chang1, Jiming Zhang1, Songhai Jia1 1 Henan Geological Museum, Zhengzhou, Henan, China, 2 Hokkaido University Museum, Hokkaido University, Sapporo, Japan, 3 Institute of Geology, Chinese Academy of Geological Sciences, Beijing, China Abstract Therizinosauria are an unusual group of theropod dinosaurs, found mostly in the Cretaceous deposits in Mongolia, China and western USA. The basal forms of this group are represented by incomplete or disarticulated material. Here, we report a nearly complete, articulated skeleton of a new basal therizinosaur from the Early Cretaceous Yixian Formation of Jianchang County, western part of Liaoning Province, which sheds light on our understanding of anatomy of basal therizinosaurs. This new dinosaur shows some typical therizinosaur features, such as neural spines of the anterior caudal vertebrae that possess anterior and posterior alae, a rectangular buttress on the ventrolateral side of the proximal end of metacarpal I, and appressed metatarsal shafts. Our phylogenetic analysis suggests that it is a basal therizinosaur (sister taxon to Therizinosauroidea) because it bears many basal therizinosaur characters in the dentition, pelvis and hind limbs. The new therizinosaur described here has unique tooth and jaw characters such as the offsetting of the tooth row by a shelf and dentary teeth with labially concave and lingually convex dentary teeth, similar to ornithopods and ceratopsians. Citation: Pu H, Kobayashi Y, Lu¨ J, Xu L, Wu Y, et al. (2013) An Unusual Basal Therizinosaur Dinosaur with an Ornithischian Dental Arrangement from Northeastern China.