Mammuthus Exilis from the California Channel Islands: Height, Mass, and Geologic Age
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New Data on the Diversity of Elephants (Mammalia, Proboscidea) in the Early and Early Middle Pleistocene of France
New data on the diversity of Elephants (Mammalia, Proboscidea) in the Early and early Middle Pleistocene of France N. Aouadi Laboratory of Prehistory, Aix en Provence, France - [email protected] SUMMARY: The remains of elephants are relatively scarce in Western Europe especially during the Early Pleistocene. The excavations of Ceyssaguet and Soleilhac (Haute-Loire, France) yielded a set of elephant teeth and bones, which belong to Mammuthus and Palaeoloxodon group. The majority of bones from Ceyssaguet (dated at 1.2 Ma.) are those of Mammuthus meridionalis but a very few bone legs belong proba- bly to the Palaeoloxodon group. On the other hand the majority of elephant finds from Soleilhac belong to Palaeoloxodon antiquus. Nevertheless some teeth could be assigned to Mammuthus meridionalis. 1. INTRODUCTION postcranials bones of elephants. The age of the site (by K/A) is estimated at 1.2 Ma. The most 1.1 Review of Pleistocene Elephant species part of fossils provides from legs either found from Western Europe connected or partly dissociated. Our study of those fossils showed the possible presence of Two groups of elephants are known from two elephants species: Mammuthus meridionalis Western Europe: the Mammuthus group and in level 2 (the majority of bones) and probably Palaeoloxodon group. The first one contains Palaeoloxodon antiquus in level 3. three subgroups: Mammuthus meridionalis The humerus from level 2 are flattened (with three subspecies: Mammuthus meridion- transversely and present a triangular section, alis gromovi, Mammuthus meridionalis merid- which characterised those of Mammuthus. On ionalis and Mammuthus meridionalis vestinus); the fourth carpal bone the higher facet for Mammuthus trogontherii (which appears at pyramidal and the lower one for metacarpal the beginning of Galerian) and the later is bone V touched together along the external Mammuthus primigenius (Palombo 1995). -
Late Quaternary Extinctions on California's
Flightless ducks, giant mice and pygmy mammoths: Late Quaternary extinctions on California’s Channel Islands Torben C. Rick, Courtney A. Hofman, Todd J. Braje, Jesu´ s E. Maldonado, T. Scott Sillett, Kevin Danchisko and Jon M. Erlandson Abstract Explanations for the extinction of Late Quaternary megafauna are heavily debated, ranging from human overkill to climate change, disease and extraterrestrial impacts. Synthesis and analysis of Late Quaternary animal extinctions on California’s Channel Islands suggest that, despite supporting Native American populations for some 13,000 years, few mammal, bird or other species are known to have gone extinct during the prehistoric human era, and most of these coexisted with humans for several millennia. Our analysis provides insight into the nature and variability of Quaternary extinctions on islands and a broader context for understanding ancient extinctions in North America. Keywords Megafauna; island ecology; human-environmental interactions; overkill; climate change. Downloaded by [Torben C. Rick] at 03:56 22 February 2012 Introduction In earth’s history there have been five mass extinctions – the Ordovician, Devonian, Permian, Triassic and Cretaceous events – characterized by a loss of over 75 per cent of species in a short geological time period (e.g. 2 million years or less: Barnosky et al. 2011). Although not a mass extinction, one of the most heavily debated extinction events is the Late Quaternary extinction of megafauna, when some two-thirds of large terrestrial mammalian genera (444kg) worldwide went extinct (Barnosky et al. 2004). Explanations for this event include climate change, as the planet went from a glacial to interglacial World Archaeology Vol. -
Tooth Morphology of Mammuthus Meridionalis from the Southern Bight of the North Sea and from Several Localities in the Netherlands
Hans van Essen Dieren Tooth morphology of Mammuthus meridionalis from the southern bight of the North Sea and from several localities in the Netherlands Van Essen, H., 2003 - Tooth morphology of Mammuthus meridionalis from the southern bight of the North Sea and from several localities in the Netherlands - 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: 453-511 [ISSN 0923-9308] Published 24 May 2003 Dental remains of M. meridionalis (NESTI, 1825) from the southern bight of the North Sea and from the continental part of The Netherlands are morphologically compared with a sample from the fluvio-lacustrine beds of the Valdarno Superiore (Italy), from which the lectotype of the spe- cies was collected. In part, the samples from Italy and northwestern Europe have different ages, yet there is a large amount of morphological overlap. This leads to the conclusion that M. meri- dionalis was conservative in its dental evolution. The reliability of dating based on morphological characteristics of smaller samples is therefore reduced. Bavelian in situ material from Oosterhout and Dorst shows typical morphological characteristics in the ontogenetically earlier teeth (M1/m1), and somewhat advanced traits in the later teeth (M2-M3/m3). With reference to similar material from Germany and Italy this is interpreted as indicative of a minor shift in mean dental morphology. Correspondence: Hans van Essen, Burg. Bloemersstraat 62, 6952 BB Dieren, The Netherlands Keywords: Early Pleistocene, North Sea, The Netherlands, Mammuthus meridionalis, morphology, evolution INTRODUCTION bed Formations are adjacent to the western This paper deals with the largely unstratified limit of the study area and in part have lateral dental remains of Plio-Pleistocene to late equivalents among the now submarine strata Early Pleistocene mammoths (M. -
Educator Guide Presented by the Field Museum
at the San Diego Natural History Museum July 4-November 11, 2013 Educator Guide Presented by The Field Museum INSIDE: Exhibition Introduction • Planning Your Visit Gallery Overviews and Guiding Questions • Focused Field Trip Activities Correlations to California State Content Standards • Additional Resources Mammoths and Mastodons: Titans of the Ice Age at the San Diego Natural History Museum is supported by: City of San Diego Commission for Arts and Culture County of San Diego Board of Supervisors, Community Enhancement Program Walter J. and Betty C. Zable Foundation Qualcomm Foundation The Kenneth T. and Eileen L. Norris Foundation VWR Charitable Foundation Education Sponsor: The Field Museum gratefully acknowledges the collaboration and assistance of the Shemanovskii Regional Museum and Exhibition Complex and the International Mammoth Committee. Walking Map The Field Museum • Mammoths and Mastodons Educator Guide • fieldmuseum.org/mammoths Page 2 www.sdnhm.org/mammoths-mastodons Exhibition Introduction Mammoths and Mastodons: Titans of the Ice Age July 4–November 11, 2013 Millions of years ago, colossal mammals roamed Europe, Asia, and North America. From the gigantic mammoth to the massive mastodon, these creatures have captured the world’s fascination. Meet “Lyuba,” the best-preserved baby mammoth in the world, and discover all that we’ve learned from her. Journey back to the Ice Age through monumental video installations, roam among saber-toothed cats and giant bears, and wonder over some of the oldest human artifacts in existence. Hands-on exciting interactive displays reveal the difference between a mammoth and a mastodon, This sketch shows a Columbian mammoth, an offer what may have caused their extinction, and show African elephant, and an American mastodon how today’s scientists excavate, analyze, and learn more (from back to front). -
Mammoths and Mastodons Teachable Moments
Teachable Moments Guide: Mammoths & Mastodons Grades K - 12 Section 1 | Stomping Grounds: Mammoths and Mastodons Duration Highlight Pieces: American Mastodon & Columbian Mammoth Articulated Skeletons 30-45 minutes Field Journal Activity: Next to the life-sized model of the Columbian Mammoth is a mural depicting life in North America during the last Ice Age. Allow students time to observe the mural and then NGSS Alignment guide your students’ observations with the following questions: What do you see in this DCIs environment? What is happening in this mural? Is there anything here that surprises you? Do you think anything is missing from this image? 3-LS4-1, 3, 4 MS/HS Extension: How does this mural demonstrate the biodiversity of Ice Age Los Angeles? Ask MS-LS4-1,2 your students to look for other murals in the museum that also depict Ice Age biodiversity and have HS-LS4-1 them compare these images. S+E Practices Section 2 | Pushed to Their Limits: Mammoths in Miniature 1,3, 4 Highlight Pieces: Pygmy Mammoth Model & Lower Jaw How were pygmy mammoths better adapted to changing climate than larger mammoth species? Crosscutting Concepts Field Journal Activity: Invite your students to examine the lower jaws of the Columbian mammoth and the 1, 2, 7 pygmy mammoth on display. Using their Paleontology Field Journals, have students compare the similarities CA EP&Cs and differences or draw some of their reflections. III.a MS/HS Extension: Are there other examples of animals adapting to their environment by adapting their size? How would this help -
Pakefield to Easton Bavents County: Suffolk District
Site Name: Pakefield to Easton Bavents County: Suffolk District: Waveney District Council Status: Site of Special Scientific Interest (SSSI) notified under Section 28 of the Wildlife and Countryside Act 1981 substituted by Schedule 9 to the Countryside & Rights of Way Act 2000. Local Planning Authority: Waveney District Council National Grid reference: TM 521828 Area: 735.33ha Ordnance Survey Sheet: 156 1:10,000: TM57 NW, TM 58NW, TM 58 SW Previous Notification Date: 7 September Notification Date: 8 December (under 1981 Act) 1989 2005 Reasons for Notification: Pakefield to Easton Bavents is nationally important for the geological exposures of the Lower Pleistocene Norwich Crag Formations and associated Pleistocene vertebrate assemblages, and the coastal geomorphology of Benacre Ness. The site is also nationally important for its vegetated shingle features, saline lagoons, flood-plain fens, an assemblage of nationally rare and nationally scarce vascular plants, scarce breeding birds, four breeding bird assemblages in four different habitats and wintering bitterns Botaurus stellaris. General description: Geology The two low cliffs between Easton Broad and Southwold provide excellent exposures of the three major elements of the Norwich Crag Formation; the Crag itself (Chillesford Church Member), the Baventian Clay (Easton Bavents Member) and the Westleton Beds (Westleton Member). This is the type locality for the Baventian Cold Stage. The stratigraphical relationship of the Antian to the Bramertonian stage and of the Baventian to the Pre-Pastonian -
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. -
Morphological Differences in Mammuthus Meridionalis and Palaeoloxodon Antiquus Carpal Bones
Morphological differences in Mammuthus meridionalis and Palaeoloxodon antiquus carpal bones P. Reggiani Paleontological Museum of Possagno, Piove di Sacco, Padova, Italy [email protected] SUMMARY: Mammuthus meridionalis and Palaeloxodon antiquus carpal bones are described. The exami- nation of some carpals and comparisons with material found in Italy has made it possible to highlight some of the typical characteristics of these two species. 1. INTRODUCTION been taken into consideration. Since the carpal bones are little described in the literatura, we Excavations carried out in 1992 and 1993 found it appropriate to introduce some charac- gave some fundamental answers to enquiries teristic for distinguishing these two species of posed after the discovery of the Paleontological elephants. remains in the Steggio zone (Possagno, Treviso, north-east Italy). It was possible to fill 2. ANATOMICAL DESCRIPTION a stratographic time gap consisting of the apparent absence of evidence of a Quaternary In the distal articular surface of all the unci- era in a formation geologically defined Tertiary forms we have studied, three facets of articula- (Paronuzzi & Tonon 1992). In the Quaternary tion for the third, quarter and fifth metacarpal lacustrine site at Steggio many fossil bones are present. were recovered, among which were various In M. meridionalis the unciforms (n = 7) are carpal bones of Mammuthus (Archidiskodon) proportionally tall and narrow, while in P. meridionalis (Nesti 1825). antiquus they are low and wide (n = 6), as can The topic of this study is an analysis of some be seen in the figure 1. This difference is high- carpal bones of pleistocene elephants. The lighted in figure 2, and in fact the values of the examinations of the remains of Steggio DT/H – DT/DAP relationship (Fig. -
The Pattern and Process of Mammoth Evolution in Eurasia Adrian M
ARTICLE IN PRESS Quaternary International 126–128 (2005) 49–64 The pattern and process of mammoth evolution in Eurasia Adrian M. Listera,*, Andrei V. Sherb, Hans van Essenc, Guangbiao Weid a Department of Biology, University College London, London WC1E 6BT, UK b Severtsov Institute of Ecology and Evolution, Russian Academy of Sciences, Moscow 119071, Russia c Faculty of Archaeology, Leiden University, P.O. Box 9515, 2300 RA Leiden, The Netherlands d Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, P.O. Box 643, Beijing 100044, China Available online 17 July 2004 Abstract Mammoth evolution in Eurasia represents one of the best-studied examples of evolutionary pattern and process in the terrestrial fossil record. A pervasive belief in the gradual transformation of chronospecies in Europe is giving way to a more complex model incorporating geographical variation across the whole of northern Eurasia. This in turn casts doubt on biostratigraphic deductions which assume gradual transformation of molar morphology, simultaneous across the species’ range. The earliest European elephantids, Mammuthus rumanus, occur in the interval 3.5–2.5 Ma, and are distinctly more primitive than the better-known M. meridionalis. The species ‘M. gromovi’, identified in the interval c. 2.6–2.2 Ma, appears to be a junior synonym of M. meridionalis. M. meridionalis dispersed widely and, in the interval 2.0–1.5 Ma, gave rise to M. trogontherii in eastern Asia, probably in China, spreading to NE Siberia by 1.2 Ma. Between that date and c. 600 ka, flow of genes and/or individuals westwards produced an interaction with European M. -
Mammuthus Meridionalis from Apollonia-1 (Mygdonia Basin, Northern Greece) and Its Importance Within the Early Pleistocene Mammoth Evolution in Europe G.E
15th International Congress of the Geological Society of Greece Athens, 22-24 May, 2019 | Harokopio University of Athens, Greece Bulletin of the Geological Society of Greece, Sp. Pub. 7 Ext. Abs. GSG2019-022 Mammuthus meridionalis from Apollonia-1 (Mygdonia Basin, Northern Greece) and its Importance within the Early Pleistocene Mammoth Evolution in Europe G.E. Konidaris1, D.S. Kostopoulos2, G.D. Koufos2 (1) Palaeoanthopology, Senckenberg Centre for Human Evolution and Palaeoenvironment, Eberhard Karls University of Tübingen, Rümelinstr. 23, 72070 Tübingen Germany, [email protected] (2) Laboratory of Geology and Palaeontology, Department of Geology, Aristotle University of Thessaloniki, 54124 Thessaloniki, Greece Introduction-Fossiliferous locality Mammoths originated in Africa at the end of the Miocene and during the late Pliocene migrated through the Levant to Eurasia, where they thrived until the Late Pleistocene. Eurasian mammoths show significant morphological adaptations through time, related to the general dietary trend from browse-dominated mixed feeding towards grazing, as a response to the changing environments of the Pleistocene (Lister & Sher, 2001). These adaptations are related to biomechanical advantages for grazing and increased resistance to abrasion, and are evident in skull and dental morphology: shortening and heightening of the cranium and mandible, enamel thinning, and increase in the height of the molar crown (hypsodonty) and the number of enamel plates in the molars (Lister, 1996). Μammoths (Mammuthus) are distinguished in Europe into four species: 1) a primitive morph, commonly, but tentatively, attributed to M. rumanus (early Villafranchian, late Pliocene); 2) the southern mammoth M. meridionalis (middle Villafranchian–Epivillafranchian, Early Pleistocene); 3) the steppe mammoth M. trogontherii (Middle Pleistocene); and 4) the wooly mammoth M. -
Mammoths Fact Sheet
Geology fact sheet: MAMMOTHS The three species of elephant alive today (the African Bush, African Forest and the Asian elephant) are all that remain of a very diverse group of ‘elephantids’. Elephantids evolved and diversified during the last five million years. The earliest species lived in the tropical woodlands of Africa, but later species migrated into Europe, Asia and even North America. The mammoths were a group of elephantids which specialised in eating grasses and shrubs of the cooler areas of northern Europe. When the Ice Age brought freezing temperatures to most of Europe, mammoths were well adapted to survive. Norfolk is one of the best places in the world to find mammoth fossils because much of the county has sediments of the right age (from the last 3 million years). A diverse group of animals – just a few extinct and extant proboscidean (including the elephantids). Mammuthus meridionalis, the ‘Southern Mammoth’, is the ancestor of the two later species found in Norfolk. It lived between about 3 million and 750,000 years ago in Europe. It lived on a varied diet of grasses, shrubs and trees. A Southern Mammoth, with an average-height human silhouette for scale Mammuthus trogontherii, the ‘Steppe Mammoth’, replaced its ancestor species Mammuthus meridionalis about 750,000 years ago. These large mammoths ate grasses, but also trees and shrubs. It was probably the largest species of elephantid ever to have lived. It weighed at least ten tonnes and stood four metres high at the shoulder. The famous West Runton Mammoth skeleton is from this species. The largest living elephants today weigh only about five tonnes and are three to three and a half metres high. -
Quaternary Vertebrates of New Mexico
Vertebrate Paleontology in New Mexico. New Mexico Museum of Natural History and Science, Bulletin 2, 1993 179 QUATERNARY VERTEBRATES OF NEW MEXICO ARTHUR H. HARRIS Laboratory for Environmental Biology, University of Texas at El Paso. El Paso, TX 79968—0519 Abstract—Approximately 346 species of vertebrates are represented in the Quaternary fossil record of New Mexico. These include 4 fishes, I salamander, 13 anurans, 5 turtles, 19 lizards, 23 snakes, 119 birds, and 162 mammals. Some 22 taxa are from the vicinity of the Blancan/Irvingtonian transition, 12 most likely are Irvingtonian, and 4 are possibly Illinoian in age. Although many sites are undated with precision, most remaining sites probably are Wisconsinan, with well over 300 taxa. INTRODUCTION omitted, particularly those from the archaeological literature, this list Although Quaternary vertebrate fossils have long been known from provides a starting point. Documentation of occurrence necessarily is New Mexico, there never has been a comprehensive list for the state. limited because of the immense number of taxa represented from the Existence of such a database would greatly simplify research in paleo- state coupled with space limitations for publication. Work in progress biology and add depth to studies of modern biogeography and syste- eventually should alleviate this situation. matics. This paper attempts to establish such a database by bringing The references include a large proportion of the primary and important together published records for the state and adding unpublished records secondary literature, but the aim has been to allow entry into the lit- represented in the collections of the Laboratory for Environmental Bi- erature rather than to provide an exhaustive bibliography.