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EAA Meeting 2016 Vilnius
www.eaavilnius2016.lt PROGRAMME www.eaavilnius2016.lt PROGRAMME Organisers CONTENTS President Words .................................................................................... 5 Welcome Message ................................................................................ 9 Symbol of the Annual Meeting .............................................................. 13 Commitees of EAA Vilnius 2016 ............................................................ 14 Sponsors and Partners European Association of Archaeologists................................................ 15 GENERAL PROGRAMME Opening Ceremony and Welcome Reception ................................. 27 General Programme for the EAA Vilnius 2016 Meeting.................... 30 Annual Membership Business Meeting Agenda ............................. 33 Opening Ceremony of the Archaelogical Exhibition ....................... 35 Special Offers ............................................................................... 36 Excursions Programme ................................................................. 43 Visiting Vilnius ............................................................................... 57 Venue Maps .................................................................................. 64 Exhibition ...................................................................................... 80 Exhibitors ...................................................................................... 82 Poster Presentations and Programme ........................................... -
Dino Hunt Checklist Card Name Type Rarity Acanthopholis
Dino Hunt Checklist Card Name Type Rarity Acanthopholis Dinosaur Common Acrocanthosaurus Dinosaur Rare Albertosaurus Dinosaur Rare Albertosaurus Dinosaur Ultra Rare Alioramus Dinosaur Rare Allosaurus Dinosaur Rare* Altispinax Dinosaur Rare* Amargasaurus Dinosaur Uncommon* Ammosaurus Dinosaur Uncommon* Anatotitan Dinosaur Common Anchiceratops Dinosaur Common Anchisaurus Dinosaur Common* Ankylosaurus Dinosaur Uncommon* Antarctosaurus Dinosaur Common Apatosaurus Dinosaur Uncommon* Archaeopteryx Dinosaur Rare* Archelon Dinosaur Rare Arrhinoceratops Dinosaur Common Avimimus Dinosaur Common Baby Ankylosaur Dinosaur Common Baby Ceratopsian Dinosaur Common Baby Hadrosaur Dinosaur Common Baby Raptor Dinosaur Rare Baby Sauropod Dinosaur Common Baby Theropod Dinosaur Rare Barosaurus Dinosaur Uncommon Baryonyx Dinosaur Rare* Bellusaurus Dinosaur Common Brachiosaurus Dinosaur Rare* Brachyceratops Dinosaur Uncommon Camarasaurus Dinosaur Common Camarasaurus Dinosaur Ultra Rare Camptosaurus Dinosaur Common Carnotaurus Dinosaur Rare Centrosaurus Dinosaur Common Ceratosaurus Dinosaur Rare* Cetiosaurus Dinosaur Common* Changdusaurus Dinosaur Common Chasmosaurus Dinosaur Common Chilantaisaurus Dinosaur Rare Coelophysis Dinosaur Uncommon* Coloradisaurus Dinosaur Common* Compsognathus Dinosaur Rare* Corythosaurus Dinosaur Common* Cryolophosaurus Dinosaur Rare Cynognathus Dinosaur Rare Dacentrurus Dinosaur Common* Daspletosaurus Dinosaur Rare Datousaurus Dinosaur Common Deinocheirus Dinosaur Rare* Deinonychus Dinosaur Uncommon* Deinosuchus Dinosaur Rare* Diceratops -
The Paleoecology and Biogeography of Ordovician Edrioasteroids
University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Doctoral Dissertations Graduate School 8-2011 The Paleoecology and Biogeography of Ordovician Edrioasteroids Rene Anne Lewis University of Tennessee - Knoxville, [email protected] Follow this and additional works at: https://trace.tennessee.edu/utk_graddiss Part of the Paleontology Commons Recommended Citation Lewis, Rene Anne, "The Paleoecology and Biogeography of Ordovician Edrioasteroids. " PhD diss., University of Tennessee, 2011. https://trace.tennessee.edu/utk_graddiss/1094 This Dissertation is brought to you for free and open access by the Graduate School at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Doctoral Dissertations by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. To the Graduate Council: I am submitting herewith a dissertation written by Rene Anne Lewis entitled "The Paleoecology and Biogeography of Ordovician Edrioasteroids." I have examined the final electronic copy of this dissertation for form and content and recommend that it be accepted in partial fulfillment of the requirements for the degree of Doctor of Philosophy, with a major in Geology. Michael L. McKinney, Major Professor We have read this dissertation and recommend its acceptance: Colin D. Sumrall, Linda C. Kah, Arthur C. Echternacht Accepted for the Council: Carolyn R. Hodges Vice Provost and Dean of the Graduate School (Original signatures are on file with official studentecor r ds.) THE PALEOECOLOGY AND BIOGEOGRAPHY OF ORDOVICIAN EDRIOASTEROIDS A Dissertation Presented for the Doctor of Philosophy Degree The University of Tennessee, Knoxville René Anne Lewis August 2011 Copyright © 2011 by René Anne Lewis All rights reserved. -
Early Cretaceous) Wessex Formation of the Isle of Wight, Southern England
A new albanerpetontid amphibian from the Barremian (Early Cretaceous) Wessex Formation of the Isle of Wight, southern England STEVEN C. SWEETMAN and JAMES D. GARDNER Sweetman, S.C. and Gardner, J.D. 2013. A new albanerpetontid amphibian from the Barremian (Early Cretaceous) Wes− sex Formation of the Isle of Wight, southern England. Acta Palaeontologica Polonica 58 (2): 295–324. A new albanerpetontid, Wesserpeton evansae gen. et sp. nov., from the Early Cretaceous (Barremian) Wessex Formation of the Isle of Wight, southern England, is described. Wesserpeton is established on the basis of a unique combination of primitive and derived characters relating to the frontals and jaws which render it distinct from currently recognized albanerpetontid genera: Albanerpeton (Late Cretaceous to Pliocene of Europe, Early Cretaceous to Paleocene of North America and Late Cretaceous of Asia); Celtedens (Late Jurassic to Early Cretaceous of Europe); and Anoualerpeton (Middle Jurassic of Europe and Early Cretaceous of North Africa). Although Wesserpeton exhibits considerable intraspecific variation in characters pertaining to the jaws and, to a lesser extent, frontals, the new taxon differs from Celtedens in the shape of the internasal process and gross morphology of the frontals in dorsal or ventral view. It differs from Anoualerpeton in the lack of pronounced heterodonty of dentary and maxillary teeth; and in the more medial loca− tion and direction of opening of the suprapalatal pit. The new taxon cannot be referred to Albanerpeton on the basis of the morphology of the frontals. Wesserpeton currently represents the youngest record of Albanerpetontidae in Britain. Key words: Lissamphibia, Albanerpetontidae, microvertebrates, Cretaceous, Britain. Steven C. -
Chitinozoan Dynamics and Biostratigraphy in the Väo Formation (Darriwilian) of the Uuga Cliff, Pakri Peninsula, NW Estonia
Estonian Journal of Earth Sciences, 2010, 59, 1, 25–36 doi: 10.3176/earth.2010.1.02 Chitinozoan dynamics and biostratigraphy in the Väo Formation (Darriwilian) of the Uuga Cliff, Pakri Peninsula, NW Estonia Mairy Tammekänd, Olle Hints, and Jaak Nõlvak Institute of Geology at Tallinn University of Technology, Ehitajate tee 5, 19086 Tallinn, Estonia; [email protected], [email protected], [email protected] Received 3 August 2009, accepted 27 October 2009 Abstract. The distribution of chitinozoans in the Väo Formation (Lasnamägi and Uhaku regional stages, Darriwilian) of the Uuga Cliff, Pakri Peninsula, NW Estonia, was investigated from 62 samples. Chitinozoans are very common and assemblages are diverse, with a total of 36 species and up to 170 specimens per gram of rock. The assemblage is dominated by Belonechitina, Desmochitina, Cyathochitina, and Euconochitina. The relative and absolute frequency of particular taxa displays regular and possibly cyclic patterns, which are not directly reflected in lithology or geochemistry. Abrupt changes in chitinozoan abundance, coinciding with some of the discontinuity surfaces, suggest the presence of stratigraphical gaps. The diversity of chitinozoans is the highest in the lower part of the Väo Formation (Rebala Member), where up to 20 species were identified in one sample and the standing species diversity exceeded 25. Within the studied interval at least 11 biostratigraphical horizons can be distinguished, including the subzonal boundaries within the Laufeldochitina striata Zone. The disappearance of abundant Belonechitina pellifera can be used for tracing the lower boundary of the Uhaku Stage. Key words: chitinozoans, frequency patterns, diversity, biostratigraphy, Ordovician, Estonia. INTRODUCTION Although the largest chitinozoan collections in the world come from the Baltic area (Paris et al. -
Brains and Intelligence
BRAINS AND INTELLIGENCE The EQ or Encephalization Quotient is a simple way of measuring an animal's intelligence. EQ is the ratio of the brain weight of the animal to the brain weight of a "typical" animal of the same body weight. Assuming that smarter animals have larger brains to body ratios than less intelligent ones, this helps determine the relative intelligence of extinct animals. In general, warm-blooded animals (like mammals) have a higher EQ than cold-blooded ones (like reptiles and fish). Birds and mammals have brains that are about 10 times bigger than those of bony fish, amphibians, and reptiles of the same body size. The Least Intelligent Dinosaurs: The primitive dinosaurs belonging to the group sauropodomorpha (which included Massospondylus, Riojasaurus, and others) were among the least intelligent of the dinosaurs, with an EQ of about 0.05 (Hopson, 1980). Smartest Dinosaurs: The Troodontids (like Troödon) were probably the smartest dinosaurs, followed by the dromaeosaurid dinosaurs (the "raptors," which included Dromeosaurus, Velociraptor, Deinonychus, and others) had the highest EQ among the dinosaurs, about 5.8 (Hopson, 1980). The Encephalization Quotient was developed by the psychologist Harry J. Jerison in the 1970's. J. A. Hopson (a paleontologist from the University of Chicago) did further development of the EQ concept using brain casts of many dinosaurs. Hopson found that theropods (especially Troodontids) had higher EQ's than plant-eating dinosaurs. The lowest EQ's belonged to sauropods, ankylosaurs, and stegosaurids. A SECOND BRAIN? It used to be thought that the large sauropods (like Brachiosaurus and Apatosaurus) and the ornithischian Stegosaurus had a second brain. -
Titanosauriform Teeth from the Cretaceous of Japan
“main” — 2011/2/10 — 15:59 — page 247 — #1 Anais da Academia Brasileira de Ciências (2011) 83(1): 247-265 (Annals of the Brazilian Academy of Sciences) Printed version ISSN 0001-3765 / Online version ISSN 1678-2690 www.scielo.br/aabc Titanosauriform teeth from the Cretaceous of Japan HARUO SAEGUSA1 and YUKIMITSU TOMIDA2 1Museum of Nature and Human Activities, Hyogo, Yayoigaoka 6, Sanda, 669-1546, Japan 2National Museum of Nature and Science, 3-23-1 Hyakunin-cho, Shinjuku-ku, Tokyo 169-0073, Japan Manuscript received on October 25, 2010; accepted for publication on January 7, 2011 ABSTRACT Sauropod teeth from six localities in Japan were reexamined. Basal titanosauriforms were present in Japan during the Early Cretaceous before Aptian, and there is the possibility that the Brachiosauridae may have been included. Basal titanosauriforms with peg-like teeth were present during the “mid” Cretaceous, while the Titanosauria with peg-like teeth was present during the middle of Late Cretaceous. Recent excavations of Cretaceous sauropods in Asia showed that multiple lineages of sauropods lived throughout the Cretaceous in Asia. Japanese fossil records of sauropods are conformable with this hypothesis. Key words: Sauropod, Titanosauriforms, tooth, Cretaceous, Japan. INTRODUCTION humerus from the Upper Cretaceous Miyako Group at Moshi, Iwaizumi Town, Iwate Pref. (Hasegawa et al. Although more than twenty four dinosaur fossil local- 1991), all other localities provided fossil teeth (Tomida ities have been known in Japan (Azuma and Tomida et al. 2001, Tomida and Tsumura 2006, Saegusa et al. 1998, Kobayashi et al. 2006, Saegusa et al. 2008, Ohara 2008, Azuma and Shibata 2010). -
Dinosaurs British Isles
DINOSAURS of the BRITISH ISLES Dean R. Lomax & Nobumichi Tamura Foreword by Dr Paul M. Barrett (Natural History Museum, London) Skeletal reconstructions by Scott Hartman, Jaime A. Headden & Gregory S. Paul Life and scene reconstructions by Nobumichi Tamura & James McKay CONTENTS Foreword by Dr Paul M. Barrett.............................................................................10 Foreword by the authors........................................................................................11 Acknowledgements................................................................................................12 Museum and institutional abbreviations...............................................................13 Introduction: An age-old interest..........................................................................16 What is a dinosaur?................................................................................................18 The question of birds and the ‘extinction’ of the dinosaurs..................................25 The age of dinosaurs..............................................................................................30 Taxonomy: The naming of species.......................................................................34 Dinosaur classification...........................................................................................37 Saurischian dinosaurs............................................................................................39 Theropoda............................................................................................................39 -
Palynology of the Middle Ordovician Hawaz Formation in the Murzuq Basin, South-West Libya
This is a repository copy of Palynology of the Middle Ordovician Hawaz Formation in the Murzuq Basin, south-west Libya. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/125997/ Version: Accepted Version Article: Abuhmida, F.H. and Wellman, C.H. (2017) Palynology of the Middle Ordovician Hawaz Formation in the Murzuq Basin, south-west Libya. Palynology, 41. pp. 31-56. ISSN 0191-6122 https://doi.org/10.1080/01916122.2017.1356393 Reuse Items deposited in White Rose Research Online are protected by copyright, with all rights reserved unless indicated otherwise. They may be downloaded and/or printed for private study, or other acts as permitted by national copyright laws. The publisher or other rights holders may allow further reproduction and re-use of the full text version. This is indicated by the licence information on the White Rose Research Online record for the item. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ Palynology of the Middle Ordovician Hawaz Formation in the Murzuq Basin, southwest Libya Faisal H. Abuhmidaa*, Charles H. Wellmanb aLibyan Petroleum Institute, Tripoli, Libya P.O. Box 6431, bUniversity of Sheffield, Department of Animal and Plant Sciences, Alfred Denny Building, Western Bank, Sheffield, S10 2TN, UK Twenty nine core and seven cuttings samples were collected from two boreholes penetrating the Middle Ordovician Hawaz Formation in the Murzuq Basin, southwest Libya. -
The Dinosaurs Transylvanian Province in Hungary
COMMUNICATIONS OF THE YEARBOOK OF THE ROYAL HUNGARIAN GEOLOGICAL IMPERIAL INSTITUTE ================================================================== VOL. XXIII, NUMBER 1. ================================================================== THE DINOSAURS OF THE TRANSYLVANIAN PROVINCE IN HUNGARY. BY Dr. FRANZ BARON NOPCSA. WITH PLATES I-IV AND 3 FIGURES IN THE TEXT. Published by The Royal Hungarian Geological Imperial Institute which is subject to The Royal Hungarian Agricultural Ministry BUDAPEST. BOOK-PUBLISHER OF THE FRANKLIN ASSOCIATION. 1915. THE DINOSAURS OF THE TRANSYLVANIAN PROVINCE IN HUNGARY. BY Dr. FRANZ BARON NOPCSA. WITH PLATES I-IV AND 3 FIGURES IN THE TEXT. Mit. a. d. Jahrb. d. kgl. ungar. Geolog. Reichsanst. XXIII. Bd. 1 heft I. Introduction. Since it appears doubtful when my monographic description of the dinosaurs of Transylvania1 that formed my so-to-speak preparatory works to my current dinosaur studies can be completed, due on one hand to outside circumstances, but on the other hand to the new arrangement of the vertebrate material in the kgl. ungar. geologischen Reichsanstalt accomplished by Dr. KORMOS, the necessity emerged of also exhibiting some of the dinosaur material located here, so that L. v. LÓCZY left the revision to me; I view the occasion, already briefly anticipating my final work at this point, to give diagnoses of the dinosaurs from the Transylvanian Cretaceous known up to now made possible from a systematic division of the current material, as well as to discuss their biology. The reptile remains known from the Danian of Transylvania will be mentioned only incidentally. Concerning the literature, I believe in refraining from more exact citations, since this work presents only a preliminary note. -
Crustaceans Topics in Biodiversity
Topics in Biodiversity The Encyclopedia of Life is an unprecedented effort to gather scientific knowledge about all life on earth- multimedia, information, facts, and more. Learn more at eol.org. Crustaceans Authors: Simone Nunes Brandão, Zoologisches Museum Hamburg Jen Hammock, National Museum of Natural History, Smithsonian Institution Frank Ferrari, National Museum of Natural History, Smithsonian Institution Photo credit: Blue Crab (Callinectes sapidus) by Jeremy Thorpe, Flickr: EOL Images. CC BY-NC-SA Defining the crustacean The Latin root, crustaceus, "having a crust or shell," really doesn’t entirely narrow it down to crustaceans. They belong to the phylum Arthropoda, as do insects, arachnids, and many other groups; all arthropods have hard exoskeletons or shells, segmented bodies, and jointed limbs. Crustaceans are usually distinguishable from the other arthropods in several important ways, chiefly: Biramous appendages. Most crustaceans have appendages or limbs that are split into two, usually segmented, branches. Both branches originate on the same proximal segment. Larvae. Early in development, most crustaceans go through a series of larval stages, the first being the nauplius larva, in which only a few limbs are present, near the front on the body; crustaceans add their more posterior limbs as they grow and develop further. The nauplius larva is unique to Crustacea. Eyes. The early larval stages of crustaceans have a single, simple, median eye composed of three similar, closely opposed parts. This larval eye, or “naupliar eye,” often disappears later in development, but on some crustaceans (e.g., the branchiopod Triops) it is retained even after the adult compound eyes have developed. In all copepod crustaceans, this larval eye is retained throughout their development as the 1 only eye, although the three similar parts may separate and each become associated with their own cuticular lens. -
Virginia Tidwell, Kenneth Carpenter & Williams Brooks, New
ORYCTOS, V ol . 2 : 21 - 37, Décembre 1999 NEW SAUROPOD FROM THE LOWER CRETACEOUS OF UTAH, USA Virginia TIDWELL, Kenneth CARPENTER and William BROOKS Department of Earth and Space Sciences, Denver Museum of Natural History, 2001 Colorado Blvd., Denver, CO 80205, USA. Abstract : The sauropod record for the Lower Cretaceous is poor in North America and consists mostly of iso - lated bones. Recently, however, a partial semiarticulated skeleton of a brachiosaurid, Cedarosaurus weiskopfae n.g., n.sp, was recovered from the Yellow Cat Member of the Cedar Mountain Formation, Utah, USA. The humeral leng - th is almost the same as the femur, while the dorsal and caudal vertebrae, and the metacarpal all display characters that identify the specimen as brachiosaurid. The forelimb and caudal vertebrae distinctly set it apart from all cur - rently described genera in that family. A brief review of Early to Middle Cretaceous brachiosaurs sorts through the confusing jumble of taxa that has developed over the years. In North America, most brachiosaurids found in Lower or Middle Cretaceous strata have historically been referred to the genus Pleurocoelus. The review illustrates the need for a reexamination of Pleurocoelus type material, as well as several specimens referred to that genus. Other material previously assigned to Pleurocoelus may yet prove to be the same as Cedarosaurus weiskopfae . Key words: Lower Cretaceous, brachiosaurid, new taxon, South-central United States. INTRODUCTION and several manus and pes elements. Only the proxi - mal end of the femur was recovered from the left side Until recently remains of Cretaceous sauropods and it is likely that all other elements were eroded in North America have been limited to the advanced away.