Pleistocene Mammals
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Wild Or Bactrian Camel French: German: Wildkamel Spanish: Russian: Dikiy Verblud Chinese
1 of 4 Proposal I / 7 PROPOSAL FOR INCLUSION OF SPECIES ON THE APPENDICES OF THE CONVENTION ON THE CONSERVATION OF MIGRATORY SPECIES OF WILD ANIMALS A. PROPOSAL: Inclusion of the Wild camel Camelus bactrianus in Appendix I of the Convention on the Conservation of Migratory Species of Wild Animals: B. PROPONENT: Mongolia C. SUPPORTING STATEMENT 1. Taxon 1.1. Classis: Mammalia 1.2. Ordo: Tylopoda 1.3. Familia: Camelidae 1.4. Genus: Camelus 1.5. Species: Camelus bactrianus Linnaeus, 1758 1.6. Common names: English: Wild or Bactrian camel French: German: Wildkamel Spanish: Russian: Dikiy verblud Chinese: 2. Biological data 2.1. Distribution Wild populations are restricted to 3 small, remnant populations in China and Mongolia:in the Taklamakan Desert, the deserts around Lop Nur, and the area in and around region A of Mongolia’s Great Gobi Strict Protected Area (Reading et al 2000). In addition, there is a small semi-captive herd of wild camels being maintained and bred outside of the Park. 2.2. Population Surveys over the past several decades have suggested a marked decline in wild bactrian camel numbers and reproductive success rates (Zhirnov and Ilyinsky 1986, Anonymous 1988, Tolgat and Schaller 1992, Tolgat 1995). Researchers suggest that fewer than 500 camels remain in Mongolia and that their population appears to be declining (Xiaoming and Schaller 1996). Globally, scientists have recently suggested that less than 900 individuals survive in small portions of Mongolia and China (Tolgat and Schaller 1992, Hare 1997, Tolgat 1995, Xiaoming and Schaller 1996). However, most of the population estimates from both China and Mongolia were made using methods which preclude rigorous population estimation. -
1.1 První Chobotnatci 5 1.2 Plesielephantiformes 5 1.3 Elephantiformes 6 1.3.1 Mammutida 6 1.3.2 Elephantida 7 1.3.3 Elephantoidea 7 2
MASARYKOVA UNIVERZITA PŘÍRODOVĚDECKÁ FAKULTA ÚSTAV GEOLOGICKÝCH VĚD Jakub Březina Rešerše k bakalářské práci Využití mikrostruktur klů neogenních chobotnatců na příkladu rodu Zygolophodon Vedoucí práce: doc. Mgr. Martin Ivanov, Dr. Brno 2012 OBSAH 1. Současný pohled na evoluci chobotnatců 3 1.1 První chobotnatci 5 1.2 Plesielephantiformes 5 1.3 Elephantiformes 6 1.3.1 Mammutida 6 1.3.2 Elephantida 7 1.3.3 Elephantoidea 7 2. Kly chobotnatců a jejich mikrostruktura 9 2.1 Přírůstky v klech chobotnatců 11 2.1.1 Využití přírůstků v klech chobotnatců 11 2.2 Schregerův vzor 12 2.2.1 Stavba Schregerova vzoru 12 2.2.2 Využití Schregerova vzoru 12 2.3 Dentinové kanálky 15 3 Sedimenty s nálezy savců v okolí Mikulova 16 3.1 Baden 17 3.2 Pannon a Pont 18 1. Současný pohled na evoluci chobotnatců Současná systematika chobotnatců není kompletně odvozena od jejich fylogeneze, rekonstruované pomocí kladistických metod. Diskutované skupiny tak mnohdy nepředstavují monofyletické skupiny. Přestože jsou taxonomické kategorie matoucí (např. Laurin 2005), jsem do jisté míry nucen je používat. Některým skupinám úrovně stále přiřazeny nebyly a zde této skutečnosti není přisuzován žádný význam. V této rešerši jsem se zaměřil hlavně na poznatky, které následovaly po vydání knihy; The Proboscidea: Evolution and Paleoecology of Elephants and Their Relatives, od Shoshaniho a Tassyho (1996). Chobotnatci jsou součástí skupiny Tethytheria společně s anthracobunidy, sirénami a desmostylidy (Shoshani 1998; Shoshani & Tassy 1996; 2005; Gheerbrant & Tassy 2009). Základní klasifikace sestává ze dvou skupin. Ze skupiny Plesielephantiformes, do které patří čeledě Numidotheriidae, Barytheriidae a Deinotheridae a ze skupiny Elephantiformes, do které patří čeledě Palaeomastodontidae, Phiomiidae, Mammutida, Gomphotheriidae, tetralofodontní gomfotéria, Stegodontidae a Elephantidae (Shoshani & Marchant 2001; Shoshani & Tassy 2005; Gheerbrant & Tassy 2009). -
Robinson, G.S., L.P. Burney, and D.A. Burney, 2005. Landscape
Ecological Monographs, 75(3), 2005, pp. 295±315 q 2005 by the Ecological Society of America LANDSCAPE PALEOECOLOGY AND MEGAFAUNAL EXTINCTION IN SOUTHEASTERN NEW YORK STATE GUY S. ROBINSON,1,4 LIDA PIGOTT BURNEY,2 AND DAVID A. BURNEY3 1Department of Natural Sciences, Fordham College at Lincoln Center, 113 West 60th Street, New York, New York 10023 USA 2The Louis Calder Biological Station, Fordham University, P.O. Box K, Armonk, New York 10504 USA 3Department of Biological Sciences, Fordham University, 441 East Fordham Road, Bronx, New York 10458 USA Abstract. Stratigraphic palynological analyses of four late Quaternary deposits com- prise a landscape-level study of the patterns and processes of megafaunal extinction in southeastern New York State. Distinctive spores of the dung fungus Sporormiella are used as a proxy for megafaunal biomass, and charcoal particle analysis as a proxy for ®re history. A decline in spore values at all sites is closely followed by a stratigraphic charcoal rise. It is inferred that the regional collapse of a megaherbivory regime was followed by landscape transformation by humans. Correlation with the pollen stratigraphy indicates these devel- opments began many centuries in advance of the Younger Dryas climatic reversal at the end of the Pleistocene. However, throughout the region, the latest bone collagen dates for Mammut are considerably later, suggesting that megaherbivores lasted until the beginning of the Younger Dryas, well after initial population collapse. This evidence is consistent with the interpretation that rapid overkill on the part of humans initiated the extinction process. Landscape transformation and climate change then may have contributed to a cascade of effects that culminated in the demise of all the largest members of North America's mammal fauna. -
Bactrian Camel, Two-Humped Camel
Camelus ferus/bactrianus Common name: Bactrian camel, two-humped camel Local name: Havtagai (Mongolian), Wildkamel (German), Jya nishpa yapung (Ladakhi) Classification: Kingdom: Animalia Phylum: Chordata Class: Mammalia Order: Artiodactyla Family: Camelidae Genus: Camelus Species: ferus/bactrianus Profile: The scientific name of the wild Bactrian camel is Camelus ferus, while the domesticated form is called Camelus bactrianus. The distinctive feature of the animal is that it is two-humped whereas the Dromedary camel has a single hump. DNA tests have revealed that there are two or three distinct genetic differences and about 3% base difference between the wild and domestic populations of Bactrian camels. They also differ physically. The wild Bactrian camel is smaller and slender than the domestic breed. The wild camels have a sandy gray- brown coat while the domestic ones have a dark brown coat. The predominant difference between them however is the shape of the humps. While that of the wild camel are small and pyramid-like, those of the domestic ones are large and irregular. The face of a Bactrian camel is long and triangular with a split upper lip. The Bactrian camel is highly adapted to surviving the cold desert climate. Each foot has an undivided sole with two large toes that can spread wide apart for walking on sand. The ears and nose are lined with hair to protect against sand and the muscular nostrils can be closed during sandstorms. The eyes are protected from sand and debris by a double layer of long eyelashes while bushy eyebrows give protection from the sun. It grows a thick shaggy coat during winter, which is shed very rapidly in spring to give the animal a shorn look. -
NENHC 2008 Abstracts
Abstracts APRIL 17 – APRIL 18, 2008 A FORUM FOR CURRENT RESEARCH The Northeastern Naturalist The New York State Museum is a program of The University of the State of New York/The State Education Department APRIL 17 – APRIL 18, 2008 A FORUM FOR CURRENT RESEARCH SUGGESTED FORMAT FOR CITING ABSTRACTS: Abstracts Northeast Natural History Conference X. N.Y. State Mus. Circ. 71: page number(s). 2008. ISBN: 1-55557-246-4 The University of the State of New York THE STATE EDUCATION DEPARTMENT ALBANY, NY 12230 THE UNIVERSITY OF THE STATE OF NEW YORK Regents of The University ROBERT M. BENNETT, Chancellor, B.A., M.S. ................................................................. Tonawanda MERRYL H. TISCH, Vice Chancellor, B.A., M.A., Ed.D. ................................................. New York SAUL B. COHEN, B.A., M.A., Ph.D.................................................................................. New Rochelle JAMES C. DAWSON, A.A., B.A., M.S., Ph.D. .................................................................. Peru ANTHONY S. BOTTAR, B.A., J.D. ..................................................................................... Syracuse GERALDINE D. CHAPEY, B.A., M.A., Ed.D. ................................................................... Belle Harbor ARNOLD B. GARDNER, B.A., LL.B. .................................................................................. Buffalo HARRY PHILLIPS, 3rd, B.A., M.S.F.S. ............................................................................. Hartsdale JOSEPH E. BOWMAN, JR., B.A., -
Redalyc.Study of Cedral Horses and Their Place in the Mexican Quaternary
Revista Mexicana de Ciencias Geológicas ISSN: 1026-8774 [email protected] Universidad Nacional Autónoma de México México Alberdi, María Teresa; Arroyo-Cabrales, Joaquín; Marín-Leyva, Alejandro H.; Polaco, Oscar J. Study of Cedral Horses and their place in the Mexican Quaternary Revista Mexicana de Ciencias Geológicas, vol. 31, núm. 2, 2014, pp. 221-237 Universidad Nacional Autónoma de México Querétaro, México Available in: http://www.redalyc.org/articulo.oa?id=57231524006 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative REVISTA MEXICANA DE CIENCIAS GEOLÓGICAS v. 31, núm. 2, 2014,Cedral p. 221-237horses Study of Cedral Horses and their place in the Mexican Quaternary María Teresa Alberdi1, Joaquín Arroyo-Cabrales2, Alejandro H. Marín-Leyva3, and Oscar J. Polaco2† 1 Departamento de Paleobiología, Museo Nacional de Ciencias Naturales, CSIC, José Gutiérrez Abascal, 2, 28006 Madrid, España. 2 Laboratorio de Arqueozoología “M. en C. Ticul Álvarez Solórzano”, Moneda 16, Col. Centro, 06060 México, D. F., Mexico. 3 Universidad Michoacana de San Nicolás de Hidalgo, Morelia, Michoacán, Mexico. * [email protected] ABSTRACT tral; y un nuevo caballo de pequeño tamaño Equus cedralensis sp. nov., conocido hasta ahora sólo en localidades mexicanas. El conocimiento A detailed study has been undertaken with an unique horse de la presencia conjunta de estas tres especies en el Pleistoceno tardío de bone deposit at Cedral, San Luis Potosí, central Mexico. Morphologi- México (género Equus sp.) es importante para entender los modelos de cal and morphometrical characters are used, as well as bivariate and diversidad y extinción en los primeros tiempos de la presencia humana multivariate statistics for both cranial and postcranial elements, and en el continente. -
Michael O. Woodburne1,* Alberto L. Cione2,**, and Eduardo P. Tonni2,***
Woodburne, M.O.; Cione, A.L.; and Tonni, E.P., 2006, Central American provincialism and the 73 Great American Biotic Interchange, in Carranza-Castañeda, Óscar, and Lindsay, E.H., eds., Ad- vances in late Tertiary vertebrate paleontology in Mexico and the Great American Biotic In- terchange: Universidad Nacional Autónoma de México, Instituto de Geología and Centro de Geociencias, Publicación Especial 4, p. 73–101. CENTRAL AMERICAN PROVINCIALISM AND THE GREAT AMERICAN BIOTIC INTERCHANGE Michael O. Woodburne1,* Alberto L. Cione2,**, and Eduardo P. Tonni2,*** ABSTRACT The age and phyletic context of mammals that dispersed between North and South America during the past 9 m.y. is summarized. The presence of a Central American province of cladogenesis and faunal differentiation is explored. One apparent aspect of such a province is to delay dispersals of some taxa northward from Mexico into the continental United States, largely during the Blancan. Examples are recognized among the various xenar- thrans, and cervid artiodactyls. Whereas the concept of a Central American province has been mentioned in past investigations it is upgraded here. Paratoceras (protoceratid artio- dactyl) and rhynchotheriine proboscideans provide perhaps the most compelling examples of Central American cladogenesis (late Arikareean to early Barstovian and Hemphillian to Rancholabrean, respectively), but this category includes Hemphillian sigmodontine rodents, and perhaps a variety of carnivores and ungulates from Honduras in the medial Miocene, as well as peccaries and equids from Mexico. For South America, Mexican canids and hy- drochoerid rodents may have had an earlier development in Mexico. Remarkably, the first South American immigrants to Mexico (after the Miocene heralds; the xenarthrans Plaina and Glossotherium) apparently dispersed northward at the same time as the first Holarctic taxa dispersed to South America (sigmodontine rodents and the tayassuid artiodactyls). -
Additions to the Late Pleistocene Vertebrate Paleontology of the Las
Additions to the Late Pleistocene Vertebrate Paleontology of ABSTRACT the Las Vegas Formation, Clark County, Nevada DISCUSSION Studies from the 1930s through the 1960s documented one of the most significant late The detailed mapping of over 500 vertebrate paleontologic localities Pleistocene faunas from the Mojave Desert in the Tule Springs area of North Las Vegas. in the upper Las Vegas Wash proved to be an interesting challenge in Recent field investigations in North Las Vegas by the San Bernardino County Museum Kathleen Springer, J. Christopher Sagebiel, Eric Scott, Craig Manker and Chris Austin terms of discerning the stratigraphy. Very little geologic have broadened our knowledge of this fauna across the Las Vegas Wash.Seven units, investigation had been performed in this region since the 1967 work designated A through G, have been defined in the section of the Las Vegas Wash near Division of Geological Sciences, San Bernardino County Museum, Redlands, California of Haynes. That very detailed study was geographically limited to Tule Springs State Park. Units B, D, and E have proven fossiliferous in the area of the the Tule Springs archaeologic investigation and the very near Tule Springs State Park, and date to>40,000 ybp, approximately 25,500 ybp, and about environs at a reconnaissance level. Our study area, falling mostly 14,500 to 9,300 ybp,respectively. Research across the Las Vegas Wash has resulted in within the Gass Peak S.W. 7.5’ U.S.G.S. topographic sheet, had not the discovery of several hundred new fossil localities. In describing the geology at these BACKGROUND been mapped. -
Discovering the Mother of All Bison Researchers Trace Bison to Common Ancestor, Pinpoint Arrival in North America
Discovering the mother of all bison Researchers trace bison to common ancestor, pinpoint arrival in North America. By Katie Willis on March 13, 2017 Unlike other notorious invaders such as zebra mussels, bison were not introduced by humans. But their rapid spread and diversification are hallmarks of an invasive species. Scientists from University of Alberta have pinpointed when bison “The DNA was too degraded, but as techniques have developed, first appeared in North America and learned more about their in particular new ways to 'fish out' bison DNA from the mixture of family tree, thanks to new fossils and genetic tools. bacterial and other DNA in these bones, these have allowed us to piece together these genome sequences,” explains Shapiro. New research by Duane Froese and Alberto Reyes in the Department of Earth and Atmospheric Sciences has identified The group showed that DNA of the earliest Yukon bison was North America’s oldest bison fossils and applied new techniques similar to DNA from a giant long-horned bison, called Bison for ancient DNA extraction to clarify the earliest parts of the bison latifrons, which was excavated in Colorado. family tree. “Bison latifrons is an interesting beast,” says Froese. “Its horns Froese and his colleagues worked with paleogeneticists to measured more than two metres across at the tips and it was sequence the mitochondrial genomes of more than 40 bison, perhaps 25% larger than modern bison.” including the two oldest bison fossils ever recovered: one from Ch’ijee’s Bluff in the Vuntut Gwitchin Territory in northern Yukon, The Colorado fossil was well-dated and only 10,000 to 20,000 and another from Snowmass, Colorado. -
Unraveling the Consequences of the Terminal Pleistocene Megafauna Extinction on Mammal Community Assembly
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Faculty Publications in the Biological Sciences Papers in the Biological Sciences 2016 Unraveling the consequences of the terminal Pleistocene megafauna extinction on mammal community assembly Felisa A. Smith University of New Mexico, Albuquerque, [email protected] Catalina P. Tomé University of Nebraska-Lincoln, [email protected] Emma A. Elliott Smith University of New Mexico, [email protected] S. Kathleen Lyons University of Nebraska - Lincoln, [email protected] Seth D. Newsome University of New Mexico, [email protected] See next page for additional authors Follow this and additional works at: https://digitalcommons.unl.edu/bioscifacpub Part of the Biology Commons, Environmental Monitoring Commons, Paleobiology Commons, and the Paleontology Commons Smith, Felisa A.; Tomé, Catalina P.; Elliott Smith, Emma A.; Lyons, S. Kathleen; Newsome, Seth D.; and Stafford, Thomas W., "Unraveling the consequences of the terminal Pleistocene megafauna extinction on mammal community assembly" (2016). Faculty Publications in the Biological Sciences. 750. https://digitalcommons.unl.edu/bioscifacpub/750 This Article is brought to you for free and open access by the Papers in the Biological Sciences at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Faculty Publications in the Biological Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Authors Felisa A. Smith, Catalina P. Tomé, Emma A. Elliott Smith, S. Kathleen Lyons, Seth D. Newsome, and Thomas W. Stafford This article is available at DigitalCommons@University of Nebraska - Lincoln: https://digitalcommons.unl.edu/ bioscifacpub/750 digitalcommons.unl.edu Unraveling the consequences of the terminal Pleistocene megafauna extinction on mammal community assembly Felisa A. -
Sankey, J.T. 2002. Vertebrate Paleontology And
SANKEY - GLENNS FERRY AND BRUNEAU FORMATIONS. IDAHO Table 2. Stratigraphic level and geologic unit of fossils discussed in this paper. See Systematic Paleontology section (this paper) for referenced specimens and their corresponding IMNH locality. GF, upper Glenns Ferry Formation (normal polarity, upper Olduvai subchron); B, lower Bruneau Formation (lowest Bruneau Formation, normal polarity, uppermost Olduvai subchron; remaining Bruneau Formation, reversed polarity; Fig. 5). IMNH 158 and 159 (collected by the John Tyson family) have imprecise locations, and a wide range of elevations are shown for these two localities. xxxx x x ¥f XX x X XXX a mw Eiychocheilus arcifems Mcheilus --Gila milleri ~u~yes&us -sp. cf. & tierinurn cf. WQsp. &ma SP- d. && sp. cf. *lopolus sp. Colubridae-indeterminate cf. Qm sp. d. sp. d. & sp. sp. cf. M.kptc-stomus param"lodon Taxidea taxus htimiun pid~nrn sp. d. C. &xg&gs Q& sp. cf. c. priscolatrans Felis lacustrjs EAk SP. -v Jhnlwu SP. fdbQmy3Q.1 patus sbdaka- lYlkmV3- I3Ywmu .SP. d-LsEia Leporidae-indeterminate sp. cf. E. sirn~licidm I3aY!ws- cf. Qglntocamelus Sp. '3. QE%!Qps sp. cf. J-Iemiauche0Ul sp. QdQQihsSP. saYs SP. d-- AND WHEREAS.. Honoring John A. White T.3S. Fo Snake River (5 km) Figure 3. Tyson Ranch. Topographic map with locations of the three measured sections (Sinker Butte 7.5' U.S.G.S. Quadrangle). Photograph of TRl (view to Sinker Butte) with arrow pointing to the phreatic tuff near the Glenns Ferry-Bruneau Formational contact. SANKEY - GLENNS FERRY AND BRUNEAU FORMATIONS, IDAHO Figure 4. Three Mile East. Topographic map with locations of measured section (Silver City 4 NE and Sinker Butte 7.5' U.S.G.S. -
Overkill, Glacial History, and the Extinction of North America's Ice Age Megafauna
PERSPECTIVE Overkill, glacial history, and the extinction of North America’s Ice Age megafauna PERSPECTIVE David J. Meltzera,1 Edited by Richard G. Klein, Stanford University, Stanford, CA, and approved September 23, 2020 (received for review July 21, 2020) The end of the Pleistocene in North America saw the extinction of 38 genera of mostly large mammals. As their disappearance seemingly coincided with the arrival of people in the Americas, their extinction is often attributed to human overkill, notwithstanding a dearth of archaeological evidence of human predation. Moreover, this period saw the extinction of other species, along with significant changes in many surviving taxa, suggesting a broader cause, notably, the ecological upheaval that occurred as Earth shifted from a glacial to an interglacial climate. But, overkill advocates ask, if extinctions were due to climate changes, why did these large mammals survive previous glacial−interglacial transitions, only to vanish at the one when human hunters were present? This question rests on two assumptions: that pre- vious glacial−interglacial transitions were similar to the end of the Pleistocene, and that the large mammal genera survived unchanged over multiple such cycles. Neither is demonstrably correct. Resolving the cause of large mammal extinctions requires greater knowledge of individual species’ histories and their adaptive tolerances, a fuller understanding of how past climatic and ecological changes impacted those animals and their biotic communities, and what changes occurred at the Pleistocene−Holocene boundary that might have led to those genera going extinct at that time. Then we will be able to ascertain whether the sole ecologically significant difference between previous glacial−interglacial transitions and the very last one was a human presence.