Hyoid Apparatus: a Little Known Complex of Bones and Its “Contribution” to Proboscidean Evolution
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Open Thesis Final V2.Pdf
The Pennsylvania State University The Graduate School Department of the Geosciences TAXONOMIC AND ECOLOGIC IMPLICATIONS OF MAMMOTH MOLAR MORPHOLOGY AS MEASURED VIA COMPUTED TOMOGRAPHY A Thesis in Geosciences by Gregory J Smith 2015 Gregory J Smith Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science August 2015 ii The thesis of Gregory J Smith was reviewed and approved* by the following: Russell W. Graham EMS Museum Director and Professor of the Geosciences Thesis Advisor Mark Patzkowsky Professor of the Geosciences Eric Post Director of the Polar Center and Professor of Biology Timothy Ryan Associate Professor of Anthropology and Information Sciences and Technology Michael Arthur Professor of the Geosciences Interim Associate Head for Graduate Programs and Research *Signatures are on file in the Graduate School iii ABSTRACT Two Late Pleistocene species of Mammuthus, M. columbi and M. primigenius, prove difficult to identify on the basis of their third molar (M3) morphology alone due to the effects of dental wear. A newly-erupted, relatively unworn M3 exhibits drastically different characters than that tooth would after a lifetime of wear. On a highly-worn molar, the lophs that comprise the occlusal surface are more broadly spaced and the enamel ridges thicken in comparison to these respective characters on an unworn molar. Since Mammuthus taxonomy depends on the lamellar frequency (# of lophs/decimeter of occlusal surface) and enamel thickness of the third molar, given the effects of wear it becomes apparent that these taxonomic characters are variable throughout the tooth’s life. Therefore, employing static taxonomic identifications that are based on dynamic attributes is a fundamentally flawed practice. -
Paleobiogeography of Trilophodont Gomphotheres (Mammalia: Proboscidea)
Revista Mexicana deTrilophodont Ciencias Geológicas, gomphotheres. v. 28, Anúm. reconstruction 2, 2011, p. applying235-244 DIVA (Dispersion-Vicariance Analysis) 235 Paleobiogeography of trilophodont gomphotheres (Mammalia: Proboscidea). A reconstruction applying DIVA (Dispersion-Vicariance Analysis) María Teresa Alberdi1,*, José Luis Prado2, Edgardo Ortiz-Jaureguizar3, Paula Posadas3, and Mariano Donato1 1 Departamento de Paleobiología, Museo Nacional de Ciencias Naturales, CSIC, José Gutiérrez Abascal 2, 28006, Madrid, España. 2 INCUAPA, Departamento de Arqueología, Universidad Nacional del Centro, Del Valle 5737, B7400JWI Olavarría, Argentina. 3 LASBE, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, Paseo del Bosque S/Nº, B1900FWA La Plata, Argentina. * [email protected] ABSTRACT The objective of our paper was to analyze the distributional patterns of trilophodont gomphotheres, applying an event-based biogeographic method. We have attempted to interpret the biogeographical history of trilophodont gomphotheres in the context of the geological evolution of the continents they inhabited during the Cenozoic. To reconstruct this biogeographic history we used DIVA 1.1. This application resulted in an exact solution requiring three vicariant events, and 15 dispersal events, most of them (i.e., 14) occurring at terminal taxa. The single dispersal event at an internal node affected the common ancestor to Sinomastodon plus the clade Cuvieronius – Stegomastodon. A vicariant event took place which resulted in two isolated groups: (1) Amebelodontinae (Africa – Europe – Asia) and (2) Gomphotheriinae (North America). The Amebelodontinae clade was split by a second vicariant event into Archaeobelodon (Africa and Europe), and the ancestors of the remaining genera of the clade (Asia). In contrast, the Gomphotheriinae clade evolved mainly in North America. -
Foraging Ecology and Conservation Biology of African Elephants: Ecological and Evolutionary Perspectives on Elephant-Woody Plant Interactions in African Landscapes
Foraging ecology and conservation biology of African elephants: Ecological and evolutionary perspectives on elephant-woody plant interactions in African landscapes Item Type Thesis Authors Dudley, Joseph Paine Download date 27/09/2021 15:01:40 Link to Item http://hdl.handle.net/11122/9523 INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter free, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand comer and continuing from left to right in equal sections with small overlaps. Each original is also photographed in one exposure and is included in reduced form at the back o f the book. Photographs included in the original manuscript have been reproduced xerographically in this copy. Higher quality 6” x 9” black and white photographic prints are available for any photographs or illustrations appearing in this copy for an additional charge. Contact UMI directly to order. UMI A Bell & Howell Information Company 300 North Zed) Road, Ann Arbor MI 48106-1346 USA 313/761-4700 800/521-0600 Reproduced with permission of the copyright owner. -
Enamel Prism Patterns in Proboscidean Molar Teeth F
Elephant Volume 2 | Issue 2 Article 11 9-6-1986 Enamel Prism Patterns in Proboscidean Molar Teeth F. Daniel Cring Department of Anthropology, University of Florida Follow this and additional works at: https://digitalcommons.wayne.edu/elephant Recommended Citation Cring, F. D. (1986). Enamel Prism Patterns in Proboscidean Molar Teeth. Elephant, 2(2), 72-79. Doi: 10.22237/elephant/ 1521732011 This Article is brought to you for free and open access by the Open Access Journals at DigitalCommons@WayneState. It has been accepted for inclusion in Elephant by an authorized editor of DigitalCommons@WayneState. Enamel Prism Patterns in Proboscidean Molar Teeth Cover Page Footnote This study was made possible by a research grant from Sigma Xi, the Scientific Research Society, and by the help of two friends, J. Shoshani and C. T. Madden. This article is available in Elephant: https://digitalcommons.wayne.edu/elephant/vol2/iss2/11 72 ELEPHANT Vol. 2, No. 2 ENAMEL PRISM PATTERNS IN PROBOSCIDEAN MOLAR TEETH by F. Daniel Cring Department of Anthropology, University of Florida Gainesville, Florida 32611 USA ABSTRACT: Molar fragments of five proboscidean taxa, representing three families, were examined under the scanning electron microscope for their enamel prism patterns. (Three of the five examined are extinct.) Results show that enamel prisms of Deinotherium are the least dense, whereas the prisms of the Elephantidae genera (Loxodonta, Elephas and Mammuthus) are the most dense, with the enamel prisms of Gomphotherium being intermediate in their density. No significant variations were found among Elephantidae genera. These observations correlate with those of earlier workers (e.g., Osborn, 1942) in that many of the morphological changes used to separate elephants (sensu stricto) from other proboscideans are the result of an evolutionary trend in diet, from the predominately browsing animals (having brachyodont thick-enamel molar teeth) to the predominately grazing animals (having hypsodont thin-enamel molar teeth). -
A Grazing Gomphotherium in Middle Miocene Central Asia, 10
www.nature.com/scientificreports OPEN A grazing Gomphotherium in Middle Miocene Central Asia, 10 million years prior to the origin of the Received: 16 November 2017 Accepted: 29 March 2018 Elephantidae Published: xx xx xxxx Yan Wu1,2, Tao Deng1,2,3, Yaowu Hu1,7, Jiao Ma1,7, Xinying Zhou1,2, Limi Mao4, Hanwen Zhang 5,6, Jie Ye1 & Shi-Qi Wang1,2,3 Feeding preference of fossil herbivorous mammals, concerning the coevolution of mammalian and foral ecosystems, has become of key research interest. In this paper, phytoliths in dental calculus from two gomphotheriid proboscideans of the middle Miocene Junggar Basin, Central Asia, have been identifed, suggesting that Gomphotherium connexum was a mixed feeder, while the phytoliths from G. steinheimense indicates grazing preference. This is the earliest-known proboscidean with a predominantly grazing habit. These results are further confrmed by microwear and isotope analyses. Pollen record reveals an open steppic environment with few trees, indicating an early aridity phase in the Asian interior during the Mid-Miocene Climate Optimum, which might urge a diet remodeling of G. steinheimense. Morphological and cladistic analyses show that G. steinheimense comprises the sister taxon of tetralophodont gomphotheres, which were believed to be the general ancestral stock of derived “true elephantids”; whereas G. connexum represents a more conservative lineage in both feeding behavior and tooth morphology, which subsequently became completely extinct. Therefore, grazing by G. steinheimense may have acted as a behavior preadaptive for aridity, and allowing its lineage evolving new morphological features for surviving later in time. This study displays an interesting example of behavioral adaptation prior to morphological modifcation. -
Redalyc.FOSSIL PROBOSCIDEA from the UPPER CENOZOIC OF
Revista Geológica de América Central ISSN: 0256-7024 [email protected] Universidad de Costa Rica Costa Rica Lucas, Spencer G.; Alvarado, Guillermo E. FOSSIL PROBOSCIDEA FROM THE UPPER CENOZOIC OF CENTRAL AMERICA: TAXONOMY, EVOLUTIONARY AND PALEOBIOGEOGRAPHIC SIGNIFICANCE Revista Geológica de América Central, núm. 42, 2010, pp. 9-42 Universidad de Costa Rica San José, Costa Rica Disponible en: http://www.redalyc.org/articulo.oa?id=45437349001 Cómo citar el artículo Número completo Sistema de Información Científica Más información del artículo Red de Revistas Científicas de América Latina, el Caribe, España y Portugal Página de la revista en redalyc.org Proyecto académico sin fines de lucro, desarrollado bajo la iniciativa de acceso abierto Revista Geológica de América Central, 42: 9-42, 2010 ISSN: 0256-7024 FOSSIL PROBOSCIDEA FROM THE UPPER CENOZOIC OF CENTRAL AMERICA: TAXONOMY, EVOLUTIONARY AND PALEOBIOGEOGRAPHIC SIGNIFICANCE Proboscideos FÓsiles del Cenozoico Superior de AMÉrica Central: TaxonomÍA, evoluciÓN Y significado paleogeogrÁfico Spencer G. Lucas1* & Guillermo E. Alvarado2 1New Mexico Museum of Natural History and Science, 1801 Mountain Road N.W., Albuquerque, New Mexico 87104 USA 2Escuela Centroamericana de Geología, Universidad de Costa Rica, Apdo. 214, 2060, San José, Costa Rica *Autor para contacto: [email protected] (Recibido: 03/02/2010; aceptado: 22/06/2010) ABSTRACT: Fossils of proboscideans from Central America are assigned to four genera: Gomphotherium, Cuvieronius, Mammut and Mammuthus. Previous reports of Stegomastodon, Rhynchotherium and Haplomastodon from Central Amer- ica are based on incorrect taxonomic identifications or on fossils not definitely diagnostic of these genera. The oldest proboscidean records from Central America (Guatemala, El Salvador, Honduras, and Costa Rica) are Late Miocene (early Hemphillian, ~ 7 Ma) records of Gomphotherium, and this suggests that gomphotheres dispersed from North America to Central America about nine million years after they dispersed from Asia to North America. -
Mammalia: Proboscidea: Gomphotheriidae) from the Continental Shelf, Pearl Islands, Panama
Quaternary International xxx (2015) 1e14 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint Forum communication Quaternary gomphotheres (Mammalia: Proboscidea: Gomphotheriidae) from the continental shelf, Pearl Islands, Panama * Gary S. Morgan a, , Bruce J. MacFadden b, Martín Martínez c a New Mexico Museum of Natural History, Albuquerque, NM 87104, USA b Florida Museum of Natural History, University of Florida, Gainesville, FL 32611, USA c Museo de Ciencias Naturales de Panama, Panama City, Panama article info abstract Article history: Fishermen have recovered four Quaternary proboscidean teeth from the continental shelf in the vicinity Available online xxx of the Pearl Islands, about 50e80 km offshore from the southern coast of Panama. Two upper third molars (M3) and one lower third molar (m3) are similar to comparable teeth of the Pleistocene gom- Keywords: phothere Cuvieronius based on the presence of 4½ to 5½ lophs/lophids that are either horizontal or Pearl Islands slightly inclined to long axis of the tooth and rather complicated enamel with single trefoils, incipient Panama double trefoils, and numerous small accessory cusps. Cuvieronius is also known from the Pleistocene El Pleistocene Hatillo and La Trinidaíta sites from the Azuero Peninsula in Panama. The teeth of Cuvieronius from the Gomphothere Cuvieronius Pearl Islands are referred to C. hyodon following recent taxonomic revisions indicating a single pan- American species of this genus was present in both North America and South America. The oldest re- cords of Cuvieronius are from early Pleistocene (early Irvingtonian) faunas in El Salvador, Florida, and New Mexico. Cuvieronius dispersed to South America in the early Pleistocene during the Great American Biotic Interchange, with the earliest record of C. -
Proboscidea (Mammalia) from the Upper Miocene of Crevillente (Alicante, Spain)
SG126 079-110 mazo 16-01-2007 09:03 Pagina 79 Proboscidea (Mammalia) from the Upper Miocene of Crevillente (Alicante, Spain) A.V. Mazo & P. Montoya Mazo, A.V. & Montoya, P. Proboscidea (Mammalia) from the Upper Miocene of Crevillente (Alicante, Spain). Scripta Geologica, 126: 79-109, 8 figs., 8 pls, 7 tables, Leiden, November 2003. A.V. Mazo, Museo Nacional de Ciencias Naturales (CSIC), José Gutiérrez Abascal 2, 28006 Madrid, Spain; P. Montoya, Departament de Geologia, Àrea de Paleontologia, Universitat de València, Dr. Moliner 50, 46100 Burjassot, Spain ([email protected]). Key words — Proboscidea, Tetralophodon, Deinotherium, Miocene, Spain. The fossil Proboscidea from the Spanish Turolian (Upper Miocene) sites of Crevillente 2 (MN11) and Crevillente 15 and 16 (MN12) are described. The mastodont from Crevillente 2 is assigned to Tetralo- phodon cf. longirostris ‘grandincisivoid form’, recognised for the first time in the Iberian Peninsula, and that from Crevillente 16 to Tetralophodon longirostris. The Deinotheriidae from Crevillente 2 and Crevillente 15 are identified as Deinotherium giganteum and Deinotherium sp., respectively. The status of ‘Mastodon’ grandincisivus and the ‘grandincisivoid forms’ of Gomphotherium and Tetralophodon are discussed. Contents Introduction ..................................................................................................................................................... 79 Systematic palaeontology ........................................................................................................................ -
Table of Contents
Educator Guide TABLE OF CONTENTS Unit LESSON PLANS Page Unit 1: ABOUT THIS GUIDE Grades 1-8: Elephant Education Chart 3 Unit 2: MOTHER KNOWS BEST! Grades 1-3: Elephant Family Playground Game 4 Grades 4-8: Elephant Diary or Elephant Interview 5 Unit 3: HOW TO BUILD AN ELEPHANT Grades 1-3: Class Discussion 6 Grades 4-8: Elephant Parts Posters 7 Unit 4: ALL IN THE FAMILY Grades 1-3: Class Discussion 8 Grades 4 -8: Venn Diagram 8 Unit 5: LOCAL & LONG - DISTANCE CALLS Grades 1-8: Elephant Puppets 10 Unit 6: ELEPHANTS AND PEOPLE Grades 4 -8: Human/Elephant Relationship Presentation 12 Unit 7: FAMILY TREE Grades 3 -8: Elephant Ancestor Family Tree 14 Unit 8: STRANGE COUSINS Grades 1-8: True or False Guessing Game 18 Unit 9: WHAT'S FOR DINNER ON THE SAVANNA? Grades 4 -8: Ecology Pyramid 20 Unit 10: WHITE GOLD Grades 5 -8: Soap Carvings 22 Unit 11: A PLACE TO LIVE Grades 1-3: Color the Map 24 Grades 4 -8: Graph the Populations 25 Unit 12: GETTING THE WORD OUT Grades 1-8: Conservation Poster 26 Unit 13: CAMERAS GREAT AND SMALL Grades l-8: Make a Pinhole Camera 27 Unit 14: JUST FOR FUN Crossword Puzzle 29 Wordsearch & Maze 30 Puzzle Solutions 31 BIBLIOGRAPHY AND RELATED SOURCES 32 CREDITS AND ADDITIONAL RESOURCES 33 2 DISCOVERY COMMUNICATIONS, INC. ABOUT THIS GUIDE This Educator's Guide has been designed to enrich your students' LESSON PLAN experience in viewing Discovery's IMAX' feature, Africa's Elephant Grades 1 - 8: Kingdom. -
Diversity of the Pleistocene Gomphotheres (Gomphotheriidae, Proboscidea) from South America
José Luis Prado 1, María Teresa Alberdi 2, Begoña Sánchez 2 & Beatriz Azanza 2 1 Universidad Nacional del Centro UNC, Olavarría 2 Museo Nacional de Ciencias Naturales, Madrid Diversity of the Pleistocene Gomphotheres (Gomphotheriidae, Proboscidea) from South America Prado, J.L., Alberdi, M.T. , Sánchez, B. & Azanza, B., 2003 - Diversity of the Pleistocene Gomphotheres (Gomphotheriidae, Proboscidea) from South America - in: Reumer, J.W.F., De Vos, J. & Mol, D. (eds.) - ADVANCES IN MAMMOTH RESEARCH (Proceedings of the Second International Mammoth Conference, Rotterdam, May 16-20 1999) - DEINSEA 9: 347-363 [ISSN 0923-9308] Published 24 May 2003 The gomphotheres were recorded in South America from the early Middle Pleistocene (Ensenadan Land-mammal Age) to the latest Pleistocene (Lujanian Land-mammal Age). They were descen- dants of the gomphothere stock that originated in North America and arrived to South America during the ‘Great American Biotic Interchange’. Only two genera are recognised: Cuvieronius with only one species (Cuvieronius hyodon), and Stegomastodon with two species (Stegomastodon waringi and Stegomastodon platensis). Two corridors would have developed during the Pleistocene in South America. These two corridors have conditioned the paleobiogeographic his- tory of most North American mammals in South America. In fact, different models can be postu- lated for different groups depending on their capacity to produce distinct adaptive types throug- hout the duration of their dispersion process. In the case of South American gomphotheres, the small Cuvieronius utilised the Andean corridor, whereas the larger Stegomastodon dispersed through the eastern route. Cuvieronius hyodon is geographically restricted to the Andean Region in Ecuador, Peru, Bolivia, Chile and Northwestern Argentina, it inhabited an arid landscape. -
Cenozoic Cooling and Grassland Expansion in Oregon and Washington
PaleoBios 28(3):89–113, January 22, 2009 © 2009 University of California Museum of Paleontology Cenozoic cooling and grassland expansion in Oregon and Washington GREGORY J. RETALLACK Department of Geological Sciences, University of Oregon, Eugene, OR 97403; [email protected] Many different kinds of paleosols are common in Cenozoic badlands of the high deserts of eastern Oregon and Washington. Pedotypes, taxonomic orders, and climofunctions are three distinct approaches that use paleosol data to reconstruct past climate, ecosystems, topography, parent materials, and landscape stability. Because the back-arc paleotopographic setting, rhyolitic parent material, and rate of subsidence changed little for paleosols of eastern Oregon and Washington over the past 45 million years, these paleosols record primarily changing climate and vegeta- tion. Paleosols of Oregon and Washington are evidence of the transition from a late Eocene (35 Ma) peak of warm, humid forests to cool, desert shrublands in the Oligocene. The reversion to warm-wet forests in the middle Miocene (16 Ma) was followed by general cooling and spread of sod grasslands that culminated in the last ice age (>1.8 Ma). These records are compatible with a greenhouse model for climate change of cooling induced by coevolutionary advances in carbon sequestration and consumption by grassland soils and sediments, punctuated by warming from volcano-tectonic and extraterrestrial perturbations. The abundant Cenozoic paleosols in the Pacific Northwest are multifaceted guides to past global change. INTRODUCTION soil structures (angular blocky peds and sesqui-argillans), soil Oregon’s Painted Hills of red-streaked badlands are the microfabrics (porphyroskelic skelmasepic), grain-size distri- best known of colorful badlands scattered throughout the bution (subsurface clay enrichment) and chemical composi- high desert of eastern Oregon and Washington (Figs. -
Gomphothere Proboscidean (Gomphotherium) from the Late Neogene of Panama
Journal of Paleontology, 89(2), 2015, p. 360–365 Copyright © 2015, The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/ by/3.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/15/0088-0906 doi: 10.1017/jpa.2014.31 Gomphothere proboscidean (Gomphotherium) from the late Neogene of Panama Bruce J. MacFadden,1 Gary S. Morgan,2 Douglas S. Jones,1 and Aldo F. Rincon1 1Florida Museum of Natural History, University of Florida, Gainesville FL 32611, USA, 〈bmacfadd@flmnh.ufl.edu〉; 〈dsjones@flmnh.ufl.edu〉; 〈arincon@ufl.edu〉 2New Mexico Museum of Natural History and Science, Albuquerque, NM 87104, USA, 〈[email protected]〉 Abstract.—The proboscidean Gomphotherium is reported here from the Alajuela Formation of Panama. Gomphotherium was widespread throughout Holarctica during the Miocene, and the Panama fossil represents the extreme southernmost occurrence of this genus in the New World. Allocation of the Panama Gomphotherium to a valid species is impossible given both the fragmentary material represented and the taxonomic complexity of species assigned to this genus. In North America, Gomphotherium has a relatively long biochronological range from the middle Miocene (~15 Ma) to early Pliocene (~5 Ma). Based on morphological comparisons, the Panama Gomphotherium is either middle Miocene, thus representing the earliest-known entry of this genus into Central America, or late Miocene/early Pliocene, which challenges the currently accepted middle Miocene age of the Alajuela Formation as it has been previously reported from Panama.