A Comparative Study of the Mechanical Properties of a Dinosaur and Crocodile Fossil Teeth T
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Ontogeny Reveals Function and Evolution of the Hadrosaurid Dinosaur Dental Battery Aaron R
LeBlanc et al. BMC Evolutionary Biology (2016) 16:152 DOI 10.1186/s12862-016-0721-1 RESEARCH ARTICLE Open Access Ontogeny reveals function and evolution of the hadrosaurid dinosaur dental battery Aaron R. H. LeBlanc1*, Robert R. Reisz1,2, David C. Evans3 and Alida M. Bailleul4 Abstract Background: Hadrosaurid dinosaurs, dominant Late Cretaceous herbivores, possessed complex dental batteries with up to 300 teeth in each jaw ramus. Despite extensive interest in the adaptive significance of the dental battery, surprisingly little is known about how the battery evolved from the ancestral dinosaurian dentition, or how it functioned in the living organism. We undertook the first comprehensive, tissue-level study of dental ontogeny in hadrosaurids using several intact maxillary and dentary batteries and compared them to sections of other archosaurs and mammals. We used these comparisons to pinpoint shifts in the ancestral reptilian pattern of tooth ontogeny that allowed hadrosaurids to form complex dental batteries. Results: Comparisons of hadrosaurid dental ontogeny with that of other amniotes reveals that the ability to halt normal tooth replacement and functionalize the tooth root into the occlusal surface was key to the evolution of dental batteries. The retention of older generations of teeth was driven by acceleration in the timing and rate of dental tissue formation. The hadrosaurid dental battery is a highly modified form of the typical dinosaurian gomphosis with a unique tooth-to-tooth attachment that permitted constant and perfectly timed tooth eruption along the whole battery. Conclusions: We demonstrate that each battery was a highly dynamic, integrated matrix of living replacement and, remarkably, dead grinding teeth connected by a network of ligaments that permitted fine scale flexibility within the battery. -
Theropod Teeth from the Upper Maastrichtian Hell Creek Formation “Sue” Quarry: New Morphotypes and Faunal Comparisons
Theropod teeth from the upper Maastrichtian Hell Creek Formation “Sue” Quarry: New morphotypes and faunal comparisons TERRY A. GATES, LINDSAY E. ZANNO, and PETER J. MAKOVICKY Gates, T.A., Zanno, L.E., and Makovicky, P.J. 2015. Theropod teeth from the upper Maastrichtian Hell Creek Formation “Sue” Quarry: New morphotypes and faunal comparisons. Acta Palaeontologica Polonica 60 (1): 131–139. Isolated teeth from vertebrate microfossil localities often provide unique information on the biodiversity of ancient ecosystems that might otherwise remain unrecognized. Microfossil sampling is a particularly valuable tool for doc- umenting taxa that are poorly represented in macrofossil surveys due to small body size, fragile skeletal structure, or relatively low ecosystem abundance. Because biodiversity patterns in the late Maastrichtian of North American are the primary data for a broad array of studies regarding non-avian dinosaur extinction in the terminal Cretaceous, intensive sampling on multiple scales is critical to understanding the nature of this event. We address theropod biodiversity in the Maastrichtian by examining teeth collected from the Hell Creek Formation locality that yielded FMNH PR 2081 (the Tyrannosaurus rex specimen “Sue”). Eight morphotypes (three previously undocumented) are identified in the sample, representing Tyrannosauridae, Dromaeosauridae, Troodontidae, and Avialae. Noticeably absent are teeth attributed to the morphotypes Richardoestesia and Paronychodon. Morphometric comparison to dromaeosaurid teeth from multiple Hell Creek and Lance formations microsites reveals two unique dromaeosaurid morphotypes bearing finer distal denticles than present on teeth of similar size, and also differences in crown shape in at least one of these. These findings suggest more dromaeosaurid taxa, and a higher Maastrichtian biodiversity, than previously appreciated. -
Dinosaur Gallery Explorer’S Notebook
Dinosaur Gallery Explorer’s Notebook Name: Class: Level 3 © Museum of Natural Sciences Education Service 2012 29, Rue Vautier, 1000 Brussels. Tel: +32 (0)2 627 42 52 [email protected] www.sciencesnaturelles.be 1 Dinosaur Gallery - Level 3 Plan of the Gallery Each time you see a number in the margin of this notebook you must move to a new place in the gallery. Find where you are on the plan. entrance via mezzanine (level 0) stairs down to level -2 stairs up to level -1 The numbers on the plan correspond to the different stages on the dinosaur gallery. The numbers start on page 6 of this notebook Make sure you have a sharp pencil and a rubber with you! Make a team of three to answer the questions. 2 Dinosaur Gallery - Level 3 Before your visit... The first pages of this notebook will help you prepare for your visit to the museum! * Words followed by an asterisk are explained in the glossary on the last page. What is a dinosaur? Below are some characteristics of dinosaurs feet underneath their bodies 4 feet terrestrial eggs with shells vertebrate* ATTENTION Dinosaurs were terrestrial animals. At the same time, sea reptiles and flying reptiles lived on the Earth, but these animals were NOT dinosaurs! Herbivore or carnivore? To know whether a dinosaur ate meat or plants, take a look at its teeth herbivore carnivore When a dinosaur was a When a dinosaur was a herbivore, its teeth had flat ends, carnivore, its teeth had pointed like the prongs of a rake or like ends, like knives. -
71St Annual Meeting Society of Vertebrate Paleontology Paris Las Vegas Las Vegas, Nevada, USA November 2 – 5, 2011 SESSION CONCURRENT SESSION CONCURRENT
ISSN 1937-2809 online Journal of Supplement to the November 2011 Vertebrate Paleontology Vertebrate Society of Vertebrate Paleontology Society of Vertebrate 71st Annual Meeting Paleontology Society of Vertebrate Las Vegas Paris Nevada, USA Las Vegas, November 2 – 5, 2011 Program and Abstracts Society of Vertebrate Paleontology 71st Annual Meeting Program and Abstracts COMMITTEE MEETING ROOM POSTER SESSION/ CONCURRENT CONCURRENT SESSION EXHIBITS SESSION COMMITTEE MEETING ROOMS AUCTION EVENT REGISTRATION, CONCURRENT MERCHANDISE SESSION LOUNGE, EDUCATION & OUTREACH SPEAKER READY COMMITTEE MEETING POSTER SESSION ROOM ROOM SOCIETY OF VERTEBRATE PALEONTOLOGY ABSTRACTS OF PAPERS SEVENTY-FIRST ANNUAL MEETING PARIS LAS VEGAS HOTEL LAS VEGAS, NV, USA NOVEMBER 2–5, 2011 HOST COMMITTEE Stephen Rowland, Co-Chair; Aubrey Bonde, Co-Chair; Joshua Bonde; David Elliott; Lee Hall; Jerry Harris; Andrew Milner; Eric Roberts EXECUTIVE COMMITTEE Philip Currie, President; Blaire Van Valkenburgh, Past President; Catherine Forster, Vice President; Christopher Bell, Secretary; Ted Vlamis, Treasurer; Julia Clarke, Member at Large; Kristina Curry Rogers, Member at Large; Lars Werdelin, Member at Large SYMPOSIUM CONVENORS Roger B.J. Benson, Richard J. Butler, Nadia B. Fröbisch, Hans C.E. Larsson, Mark A. Loewen, Philip D. Mannion, Jim I. Mead, Eric M. Roberts, Scott D. Sampson, Eric D. Scott, Kathleen Springer PROGRAM COMMITTEE Jonathan Bloch, Co-Chair; Anjali Goswami, Co-Chair; Jason Anderson; Paul Barrett; Brian Beatty; Kerin Claeson; Kristina Curry Rogers; Ted Daeschler; David Evans; David Fox; Nadia B. Fröbisch; Christian Kammerer; Johannes Müller; Emily Rayfield; William Sanders; Bruce Shockey; Mary Silcox; Michelle Stocker; Rebecca Terry November 2011—PROGRAM AND ABSTRACTS 1 Members and Friends of the Society of Vertebrate Paleontology, The Host Committee cordially welcomes you to the 71st Annual Meeting of the Society of Vertebrate Paleontology in Las Vegas. -
A Troodontid Dinosaur from the Latest Cretaceous of India
ARTICLE Received 14 Dec 2012 | Accepted 7 Mar 2013 | Published 16 Apr 2013 DOI: 10.1038/ncomms2716 A troodontid dinosaur from the latest Cretaceous of India A. Goswami1,2, G.V.R. Prasad3, O. Verma4, J.J. Flynn5 & R.B.J. Benson6 Troodontid dinosaurs share a close ancestry with birds and were distributed widely across Laurasia during the Cretaceous. Hundreds of occurrences of troodontid bones, and their highly distinctive teeth, are known from North America, Europe and Asia. Thus far, however, they remain unknown from Gondwanan landmasses. Here we report the discovery of a troodontid tooth from the uppermost Cretaceous Kallamedu Formation in the Cauvery Basin of South India. This is the first Gondwanan record for troodontids, extending their geographic range by nearly 10,000 km, and representing the first confirmed non-avian tetanuran dinosaur from the Indian subcontinent. This small-bodied maniraptoran dinosaur is an unexpected and distinctly ‘Laurasian’ component of an otherwise typical ‘Gondwanan’ tetrapod assemblage, including notosuchian crocodiles, abelisauroid dinosaurs and gondwanathere mammals. This discovery raises the question of whether troodontids dispersed to India from Laurasia in the Late Cretaceous, or whether a broader Gondwanan distribution of troodontids remains to be discovered. 1 Department of Genetics, Evolution, and Environment, University College London, London WC1E 6BT, UK. 2 Department of Earth Sciences, University College London, London WC1E 6BT, UK. 3 Department of Geology, Centre for Advanced Studies, University of Delhi, New Delhi 110 007, India. 4 Geology Discipline Group, School of Sciences, Indira Gandhi National Open University, New Delhi 110 068, India. 5 Division of Paleontology and Richard Gilder Graduate School, American Museum of Natural History, New York, New York 10024, USA. -
Evidence for a Tyrannosaurus Rex from Southeastern Colorado
Evidence for aTyrannosaurus rex from southeastern Colorado Keith Berry, Platte Valley School District Re-7, Science Department, Kersey, Colorado 80644, and Frontiers of Science Institute, Mathematics and Science Teaching Institute, University of Northern Colorado, Greeley, Colorado 80369, [email protected] Discovery Femur: A limb bone fragment (TSJC racy of ± 0.5 mm along a radial transect, T. 2008.1.2) is also tentatively identified as cf. rex annual growth markers are exception- Dinosaur tooth and bone fragments were T. rex. Theropod bones commonly exhibit ally good predictors for the growth lines recovered from private property at an onion-skin layering in cross section (K. observed in this bone (cχ2 = 1.44, df = 6, undisclosed locality in southeastern Colo- Carpenter, pers. comm. 2007), and this p-value > 0.95). As T. rex is the only animal rado. The site is in an unnamed, transitional bone seems to lack this feature, although known to exhibit this characteristic pattern member of the uppermost Pierre Shale and the bone has distinct, differentiable layers. of growth (Erickson et al. 2004; Chinsamy- is likely within the Baculites eliasi ammonite Whereas the bone itself may not be exclu- Turan 2005), this is believed to be a fairly zone (N. Larson, pers. comm. 2007), mak- sively attributed to a theropod based on its powerful diagnostic test. ing the site early Maastrichtian. This is the gross histological properties alone, there are Significance—Estimated to be about 71 first record of dinosaur fossils from these quantitative reasons supporting this diag- m.y. old based on the age of the Baculites strata. -
Katherine Keenan Bramble
A Histological Analysis of the Hadrosaurid Dental Battery by Katherine Keenan Bramble A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Systematics and Evolution Department of Biological Sciences University of Alberta © Katherine Keenan Bramble, 2017 Abstract The first histological study of an entire hadrosaurid dental battery provides a better understanding of this complex structure. The hadrosaurid dental battery is composed of interlocking, vertically stacked columns of teeth that form a complex grinding surface. The dental battery was previously considered to be a solid, cemented structure based on superficial examination of intact batteries and thin sections of isolated teeth. This first description of the dental battery using thin sections through the entire structure refutes the model of a single, fused mass of teeth. These thin sections confirm the presence of periodontal ligament connections between all teeth, underscoring its dynamic nature. The serial thin sections across an adult dental battery also revealed signs of gradual and possibly ontogenetic tooth migration. These signs include the extensive remodeling of the alveolar septa and the anteroposterior displacement of successive generations of teeth. The four most posterior tooth families migrated posteriorly whereas the remaining tooth families had a progressively more pronounced anterior trajectory. This migration is pronounced enough in some areas to cause extensive resorption of neighbouring teeth. Thin sections through a dental battery of a perinatal specimen reveal that all of the alveolar septa are angled anteriorly, which suggests that extensive and unidirectional tooth migration begins early in ontogeny and that any additional migration happens later in ontogeny. -
The Nonavian Theropod Quadrate II: Systematic Usefulness, Major Trends and Cladistic and Phylogenetic Morphometrics Analyses
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/272162807 The nonavian theropod quadrate II: systematic usefulness, major trends and cladistic and phylogenetic morphometrics analyses Article · January 2014 DOI: 10.7287/peerj.preprints.380v2 CITATION READS 1 90 3 authors: Christophe Hendrickx Ricardo Araujo University of the Witwatersrand Technical University of Lisbon 37 PUBLICATIONS 210 CITATIONS 89 PUBLICATIONS 324 CITATIONS SEE PROFILE SEE PROFILE Octávio Mateus University NOVA of Lisbon 224 PUBLICATIONS 2,205 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Nature and Time on Earth - Project for a course and a book for virtual visits to past environments in learning programmes for university students (coordinators Edoardo Martinetto, Emanuel Tschopp, Robert A. Gastaldo) View project Ten Sleep Wyoming Jurassic dinosaurs View project All content following this page was uploaded by Octávio Mateus on 12 February 2015. The user has requested enhancement of the downloaded file. The nonavian theropod quadrate II: systematic usefulness, major trends and cladistic and phylogenetic morphometrics analyses Christophe Hendrickx1,2 1Universidade Nova de Lisboa, CICEGe, Departamento de Ciências da Terra, Faculdade de Ciências e Tecnologia, Quinta da Torre, 2829-516, Caparica, Portugal. 2 Museu da Lourinhã, 9 Rua João Luis de Moura, 2530-158, Lourinhã, Portugal. s t [email protected] n i r P e 2,3,4,5 r Ricardo Araújo P 2 Museu da Lourinhã, 9 Rua João Luis de Moura, 2530-158, Lourinhã, Portugal. 3 Huffington Department of Earth Sciences, Southern Methodist University, PO Box 750395, 75275-0395, Dallas, Texas, USA. -
A Century of Spinosaurs - a Review and Revision of the Spinosauridae
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Queen Mary Research Online A century of spinosaurs - a review and revision of the Spinosauridae with comments on their ecology HONE David William Elliott1, * HOLTZ Thomas Richard Jnr2 1 School of Biological and Chemical Sciences, Queen Mary University of London, London, E1 4NS, UK 2 Department of Geology, University of Maryland, College Park, MD 20742 USA Abstract: The spinosaurids represent an enigmatic and highly unusual form of large tetanuran theropods that were first identified in 1915. A recent flurry of discoveries and taxonomic revisions of this important and interesting clade had added greatly to our knowledge, however, spinosaur body fossils are generally rare and most species are known from only limited skeletal remains. Their unusual anatomical adaptations to the skull, limbs and axial column all differ from other large theropods and point to an unusual ecological niche and a lifestyle intimately linked to water. Keywords: Theropoda, Megalosauroidea, Baryonychinae, Spinosaurinae, palaeoecology E-mail: [email protected] 1 Introduction The Spinosauridae is an enigmatic clade of large and carnivorous theropods from the Jurassic and Cretaceous that are known from both Gondwana and Laurasia (Holtz et al., 2004). Despite their wide temporal and geographic distribution, the clade is known primarily from teeth and the body fossil record is extremely limited (Bertin, 2010). As such, relatively little is known about this group of animals, although their unusual morphology with regard to skull shape, dentition, dorsal neural spines and other features mark them out as divergent from the essential bauplan of other non-tetanuran theropods (Fig 1). -
Second Discovery of a Spinosaurid Tooth from the Sebayashi Formation (Lower Cretaceous), Kanna Town, Gunma Prefecture, Japan
群馬県立自然史博物館研究報告(21):1-6,2017 1 Bull.Gunma Mus.Natu.Hist(. 21):1-6,2017 Original Article Second discovery of a spinosaurid tooth from the Sebayashi Formation (Lower Cretaceous), Kanna Town, Gunma Prefecture, Japan 1 2 2 KUBOTA Katsuhiro, TAKAKUWA Yuji and HASEGAWA Yoshikazu 1Kanna Dinosaur Center: 51-2, Kagahara, Kanna, Tano, Gunma 370-1602, Japan ([email protected]) 2Gunma Museum of Natural History: 1674-1 Kamikuroiwa, Tomioka, Gunma 370-2345, Japan ([email protected]; [email protected]) Abstract: A fragment of an isolated tooth is described from the Lower Cretaceous Sebayashi Formation of the Sanchu Group. Its crown is almost round in cross section and shows distinctive flutes. Between the flutes, there are longitudinal finely granular structures. The distinctive carinae have poorly defined serrations. It is probably assigned as a spinosaurid theropod dinosaur and is the second report from Japan. This spinosaurid tooth is found from the higher stratigraphic horizon of the same formation than the first. The occurrences of spinosaurids from two horizons suggest that spinosaurids might have habituated this area during the deposit of the Sebayashi Formation. The dental comparison between Asian and other spinosaurids suggests that Asian spinosaurids may have unique dental characteristics and be different from any known spinosaurids, although the phylogenetic relationships between Asian and other spinosaurids (baryonychines and spinosaurines) are unclear. Key words: Dinosaur, Spinosauridae, Sebayashi Formation, Gunma Prefecture, Kanna Town Introduction Macro-sized and longitudinal ornamentation on the crown is characteristic in spinosaurids and had been called as crest, flute, A fragmentary dinosaur tooth was collected in a fossil- ridge, and striation (Fig. -
Mammal-Like Mastication for the Dinosaur Leptoceratops 8 July 2016, by Andrew Farke
Mammal-like mastication for the dinosaur Leptoceratops 8 July 2016, by Andrew Farke in just about every plane of movement imaginable. Different chewing styles characterize different diets as well as different groups of organisms; if you ever get the opportunity, take a look at the fairly simple motions of an iguana chopping up a leaf versus the complex dance of teeth, jaws, and tongue in a cow chewing on grass. More complex motions can allow more thorough processing of food before it enters the stomach, which has all sorts of advantages for digestive efficiency and nutrient extraction. Why do we care about chewing? From a biological perspective, feeding is an incredibly basic yet often poorly understood aspect of an organisms' life. Everything needs to eat, and it's the style of eating that can make it or break it for a species on geological timescales as well as within an individual organism's lifetime. Different styles of chewing can open up different food sources, and is one part of what helps species compete against each other ecologically. If we understand feeding in extinct organisms, we can better understand how they fit within their immediate environment and their world. Tiny scratches on a dinosaur tooth, viewed under a scanning electron microscope. Viewed at actual size, the image would only be a millimeter tall! Credit: Varriale 2016 We all chew, but hardly ever think about it. Even a moment's consideration, though, reveals how complex of a process it actually is. Jaws move, teeth gnash, and food gets broken from big bits into smaller bits. -
The Origin and Evolution of the Dinosaur Infraorder Carnosauria*
PALEONTOLOGICHESKIY ZHURNAL 1989 No. 4 KURZANOV S. M. THE ORIGIN AND EVOLUTION OF THE DINOSAUR INFRAORDER CARNOSAURIA* Paleontological Institute of the Academy of Sciences of the USSR Based on a revision of the systematic composition of the carnosaur families, a new diagram of the phylogenetic relationships within the infraorder is proposed. The question of carnosaurs cannot be considered to be resolved. Excluding the Triassic forms, carnosaurs in the broad or narrow sense have always been considered to be a group of theropods because they are only slightly different from them in fundamental features associated with large body size and a predatory lifestyle. The Late Triassic genera, such as Teratosaurus and Sinosaurus [33], were assigned to these on the basis of extremely meager material and without sufficient justification. This assignment has subsequently been rejected by most authors [13, 16, 17, 24, 25]. Huene [23] suggested that, along with the Sauropoda and Prosauropoda, the carnosaurs form a natural group Pachypodosauria, within which they are thought to be direct descendants of the prosauropods (the carnosaurs proceed directly from Teratosaurus through Magnosaurus). Studies of abundant cranial material (which actually belongs to Sellosaurus gracilis Huene) gave reason to think that the first species had been a prosauropod, whereas typical material (maxilla, ischium) belong to thecodonts from the family Poposauridae [24]. Huene’s diagram, which initially did not receive support, was widely propagated by the discovery of an unusual carnosaur Torvosaurus tanneri Galton et Jensen in the Upper Triassic deposits of Colorado [25]. The exceptionally plesiomorphic nature of some of its features, in the authors’ opinion, gave sufficient justification for removing them from the prosauropods.