ICE AGE MAMMALS of YUKON an X-Ray Image of a Complete Arctic Ground Squirrel Mummy Found Preserved in Its Burrow
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Lucy in the Sky with Diamonds and Butterflies
Home / Life / Specials Lucy in the sky with diamonds and butterflies A butterfly flapping its wings in Brazil can produce a tornado in Texas. The author of this poetic image was Edward Lorenz, a meteorologist who in 1972 explained how small changes in a system as complex as the atmosphere can generate large effects. This expression was a huge success and since then has often been used. Two million years ago, in the middle of the Pleistocene, a population of African apes lived astride the border between two worlds: the old world of the forest and the new world of the grasslands. They were Australopithechi, “southern apes”, which had recently climbed down from the trees but were already able to walk as bipeds, just in a way that was a little more ungainly than we do. They had their feet on the ground but their paws still on branches because trees remained a safe refuge into which they could climb to rest and to escape the large felines of the time, huge and ferocious beasts like the sabre-toothed cat ( Homotherium crenatidens ), the Megantereon, cousin of the sabre-toothed tiger and the worst of all of them: the Dinofelis, literally meaning “terrible cat”. It seems that the incisions found on the fossilised bones of some Australopitechi were the result of attacks by that prehistoric leopard. The most famous Australopitecus is Lucy, a young female who lived just over three million years ago, discovered in Ethiopia in November 1974. Reconstruction of Lucy, the female Australopithecus afarensis found in Hadar, Ethiopia. Credits: discovermagazine.com, copyright John Gurche / Courtesy Yale University Press Lucy who walked in the sky with diamonds in reality is called “A.L. -
Ancient Mitogenomes Shed Light on the Evolutionary History And
Ancient Mitogenomes Shed Light on the Evolutionary History and Biogeography of Sloths Frédéric Delsuc, Melanie Kuch, Gillian Gibb, Emil Karpinski, Dirk Hackenberger, Paul Szpak, Jorge Martinez, Jim Mead, H. Gregory Mcdonald, Ross Macphee, et al. To cite this version: Frédéric Delsuc, Melanie Kuch, Gillian Gibb, Emil Karpinski, Dirk Hackenberger, et al.. Ancient Mitogenomes Shed Light on the Evolutionary History and Biogeography of Sloths. Current Biology - CB, Elsevier, 2019. hal-02326384 HAL Id: hal-02326384 https://hal.archives-ouvertes.fr/hal-02326384 Submitted on 22 Oct 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. 1 Ancient Mitogenomes Shed Light on the Evolutionary 2 History and Biogeography of Sloths 3 Frédéric Delsuc,1,13,*, Melanie Kuch,2 Gillian C. Gibb,1,3, Emil Karpinski,2,4 Dirk 4 Hackenberger,2 Paul Szpak,5 Jorge G. Martínez,6 Jim I. Mead,7,8 H. Gregory 5 McDonald,9 Ross D. E. MacPhee,10 Guillaume Billet,11 Lionel Hautier,1,12 and 6 Hendrik N. Poinar2,* 7 Author list footnotes 8 1Institut des Sciences de l’Evolution de Montpellier -
Extinction of Harrington's Mountain Goat (Vertebrate Paleontology/Radiocarbon/Grand Canyon) JIM I
Proc. Nati. Acad. Sci. USA Vol. 83, pp. 836-839, February 1986 Geology Extinction of Harrington's mountain goat (vertebrate paleontology/radiocarbon/Grand Canyon) JIM I. MEAD*, PAUL S. MARTINt, ROBERT C. EULERt, AUSTIN LONGt, A. J. T. JULL§, LAURENCE J. TOOLIN§, DOUGLAS J. DONAHUE§, AND T. W. LINICK§ *Department of Geology, Northern Arizona University, and Museum of Northern Arizona, Flagstaff, AZ 86011; tDepartment of Geosciences and tArizona State Museum and Department of Geosciences, University of Arizona, Tucson, AZ 85721; §National Science Foundation Accelerator Facility for Radioisotope Analysis, University of Arizona, Tucson, AZ 85721 Communicated by Edward S. Deevey, Jr., October 7, 1985 ABSTRACT Keratinous horn sheaths of the extinct Har- rington's mountain goat, Oreamnos harringtoni, were recov- ered at or near the surface of dry caves of the Grand Canyon, Arizona. Twenty-three separate specimens from two caves were dated nondestructively by the tandem accelerator mass spectrometer (TAMS). Both the TAMS and the conventional dates indicate that Harrington's mountain goat occupied the Grand Canyon for at least 19,000 years prior to becoming extinct by 11,160 + 125 radiocarbon years before present. The youngest average radiocarbon dates on Shasta ground sloths, Nothrotheriops shastensis, from the region are not significantly younger than those on extinct mountain goats. Rather than sequential extinction with Harrington's mountain goat disap- pearing from the Grand Canyon before the ground sloths, as one might predict in view ofevidence ofclimatic warming at the time, the losses were concurrent. Both extinctions coincide with the regional arrival of Clovis hunters. Certain dry caves of arid America have yielded unusual perishable remains of extinct Pleistocene animals, such as hair, dung, and soft tissue of extinct ground sloths (1) and, recently, ofmammoths (2). -
O Ssakach Drapieżnych – Część 2 - Kotokształtne
PAN Muzeum Ziemi – O ssakach drapieżnych – część 2 - kotokształtne O ssakach drapieżnych - część 2 - kotokształtne W niniejszym artykule przyjrzymy się ewolucji i zróżnicowaniu zwierząt reprezentujących jedną z dwóch głównych gałęzi ewolucyjnych w obrębie drapieżnych (Carnivora). Na wczesnym etapie ewolucji, drapieżne podzieliły się (ryc. 1) na psokształtne (Caniformia) oraz kotokształtne (Feliformia). Paradoksalnie, w obydwu grupach występują (bądź występowały w przeszłości) formy, które bardziej przypominają psy, bądź bardziej przypominają koty. Ryc. 1. Uproszczone drzewo pokrewieństw ewolucyjnych współczesnych grup drapieżnych (Carnivora). Ryc. Michał Loba, na podstawie Nyakatura i Bininda-Emonds, 2012. Tym, co w rzeczywistości dzieli te dwie grupy na poziomie anatomicznym jest budowa komory ucha środkowego (bulla tympanica, łac.; ryc. 2). U drapieżnych komora ta jest budowa przede wszystkim przez dwie kości – tylną kaudalną kość entotympaniczną i kość ektotympaniczną. U kotokształtnych, w miejscu ich spotkania się ze sobą powstaje ciągła przegroda. Obydwie części komory kontaktują się ze sobą tylko za pośrednictwem małego okienka. U psokształtnych 1 PAN Muzeum Ziemi – O ssakach drapieżnych – część 2 - kotokształtne Ryc. 2. Widziane od spodu czaszki: A. baribala (Ursus americanus, Ursidae, Caniformia), B. żenety zwyczajnej (Genetta genetta, Viverridae, Feliformia). Strzałkami zaznaczono komorę ucha środkowego u niedźwiedzia i miejsce występowania przegrody w komorze żenety. Zdj. (A, B) Phil Myers, Animal Diversity Web (CC BY-NC-SA -
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). -
A Middle Holocene Steppe Bison and Paleoenvironments from the Versleuce Meadows, Whitehorse, Yukon, Canada Grant D
1138 ARTICLE A middle Holocene steppe bison and paleoenvironments from the Versleuce Meadows, Whitehorse, Yukon, Canada Grant D. Zazula, Elizabeth Hall, P. Gregory Hare, Christian Thomas, Rolf Mathewes, Catherine La Farge, André L. Martel, Peter D. Heintzman, and Beth Shapiro Abstract: A partial skeleton of a bison was recovered during residential house construction in Whitehorse, Yukon, Canada. The specimen represents a young (estimated 6 year old) bison individual that died, was partially scavenged by carnivores, and subsequently buried by calcareous silt sediment in a pond or small lake during the middle Holocene, ϳ5400 years ago. Palaeoenvironmental data, including molluscs, pollen, vascular plant, and bryophyte macrofossils demonstrate that the small waterbody was surrounded by white spruce dominated boreal forest. Morphometric analysis of the skeleton reveals that its taxonomic affinity is ambiguous, likely owing to it representing an ontogenetically young individual, though it does share some cranial and horn core characteristics of named species such as Bison occidentalis or Bison priscus. Mitochondrial genomic data confirm that this bison belongs to Clade 2A (northern clade), which represents Pleistocene steppe bison (B. cf. priscus) in Beringia through the Holocene and is not represented in living bison species. These data further demonstrate that northern steppe bison population survived the late Pleistocene extinction event, persisted locally in southern Yukon into the Holocene, and are best characterized as a species with a high degree of morphological variability and ecological flexibility. Résumé : Le squelette partiel d’un bison a été récupéré durant la construction d’immeubles résidentiels a` Whitehorse (Yukon, Canada). Le spécimen représente un unique jeune bison (d’âge estimé a` 6 ans) qui est mort, a été partiellement dévoré par des carnivores pour ensuite être enseveli sous du silt calcareux dans un étang ou un petit lac durant l’Holocène moyen, il y a ϳ5400 ans. -
Variable Impact of Late-Quaternary Megafaunal Extinction in Causing
Variable impact of late-Quaternary megafaunal SPECIAL FEATURE extinction in causing ecological state shifts in North and South America Anthony D. Barnoskya,b,c,1, Emily L. Lindseya,b, Natalia A. Villavicencioa,b, Enrique Bostelmannd,2, Elizabeth A. Hadlye, James Wanketf, and Charles R. Marshalla,b aDepartment of Integrative Biology, University of California, Berkeley, CA 94720; bMuseum of Paleontology, University of California, Berkeley, CA 94720; cMuseum of Vertebrate Zoology, University of California, Berkeley, CA 94720; dRed Paleontológica U-Chile, Laboratoria de Ontogenia, Departamento de Biología, Facultad de Ciencias, Universidad de Chile, Chile; eDepartment of Biology, Stanford University, Stanford, CA 94305; and fDepartment of Geography, California State University, Sacramento, CA 95819 Edited by John W. Terborgh, Duke University, Durham, NC, and approved August 5, 2015 (received for review March 16, 2015) Loss of megafauna, an aspect of defaunation, can precipitate many megafauna loss, and if so, what does this loss imply for the future ecological changes over short time scales. We examine whether of ecosystems at risk for losing their megafauna today? megafauna loss can also explain features of lasting ecological state shifts that occurred as the Pleistocene gave way to the Holocene. We Approach compare ecological impacts of late-Quaternary megafauna extinction The late-Quaternary impact of losing 70–80% of the megafauna in five American regions: southwestern Patagonia, the Pampas, genera in the Americas (19) would be expected to trigger biotic northeastern United States, northwestern United States, and Berin- transitions that would be recognizable in the fossil record in at gia. We find that major ecological state shifts were consistent with least two respects. -
Quaternary Records of the Dire Wolf, Canis Dirus, in North and South America
Quaternary records of the dire wolf, Canis dirus, in North and South America ROBERT G. DUNDAS Dundas, R. G. 1999 (September): Quaternary records of the dire wolf, Canis dirus, in North and South Ameri- ca. Boreas, Vol. 28, pp. 375–385. Oslo. ISSN 0300-9483. The dire wolf was an important large, late Pleistocene predator in North and South America, well adapted to preying on megaherbivores. Geographically widespread, Canis dirus is reported from 136 localities in North America from Alberta, Canada, southward and from three localities in South America (Muaco, Venezuela; Ta- lara, Peru; and Tarija, Bolivia). The species lived in a variety of environments, from forested mountains to open grasslands and plains ranging in elevation from sea level to 2255 m (7400 feet). Canis dirus is assigned to the Rancholabrean land mammal age of North America and the Lujanian land mammal age of South Amer- ica and was among the many large carnivores and megaherbivores that became extinct in North and South America near the end of the Pleistocene Epoch. Robert G. Dundas, Department of Geology, California State University, Fresno, California 93740-8031, USA. E-mail: [email protected]; received 20th May 1998, accepted 23rd March 1999 Because of the large number of Canis dirus localities Rancho La Brea, comparing them with Canis lupus and and individuals recovered from the fossil record, the dire wolf specimens from other localities. Although dire wolf is the most commonly occurring large knowledge of the animal’s biology had greatly predator in the Pleistocene of North America. By increased by 1912, little was known about its strati- contrast, the species is rare in South America. -
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. -
A Contextual Review of the Carnivora of Kanapoi
A contextual review of the Carnivora of Kanapoi Lars Werdelin1* and Margaret E. Lewis2 1Department of Palaeobiology, Swedish Museum of Natural History, Box 50007, S-10405 Stockholm, Swe- den; [email protected] 2Biology Program, School of Natural Sciences and Mathematics, Stockton University, 101 Vera King Farris Drive, Galloway, NJ 08205, USA; [email protected] *Corresponding author Abstract The Early Pliocene is a crucial time period in carnivoran evolution. Holarctic carnivoran faunas suffered a turnover event at the Miocene-Pliocene boundary. This event is also observed in Africa but its onset is later and the process more drawn-out. Kanapoi is one of the earliest faunas in Africa to show evidence of a fauna that is more typical Pliocene than Miocene in character. The taxa recovered from Kanapoi are: Torolutra sp., Enhydriodon (2 species), Genetta sp., Helogale sp., Homotherium sp., Dinofelis petteri, Felis sp., and Par- ahyaena howelli. Analysis of the broader carnivoran context of which Kanapoi is an example shows that all these taxa are characteristic of Plio-Pleistocene African faunas, rather than Miocene ones. While some are still extant and some went extinct in the Early Pleistocene, Parahyaena howelli is unique in both originating and going extinct in the Early Pliocene. Keywords: Africa, Kenya, Miocene, Pliocene, Pleistocene, Carnivora Introduction Dehghani, 2011; Werdelin and Lewis, 2013a, b). In Kanapoi stands at a crossroads of carnivoran this contribution we will investigate this pattern and evolution. The Miocene –Pliocene boundary (5.33 its significance in detail. Ma: base of the Zanclean Stage; Gradstein et al., 2012) saw a global turnover among carnivores (e.g., Material and methods Werdelin and Turner, 1996). -
LOCOMOTOR ADAPTATIONS and ECOMORPHOLOGY of SHORT-FACED BEARS (Arctodus Simus) in EASTERN BERINGIA
Palaeontology Program Government of the Yukon Occasional Papers in Earth Sciences No. 7 LOCOMOTOR ADAPTATIONS AND ECOMORPHOLOGY OF SHORT-FACED BEARS (Arctodus simus) IN EASTERN BERINGIA Paul E. Matheus The Alaska Quaternary Center, Department of Geology and Geophysics and The Institute of Arctic Biology University of Alaska Fairbanks YUKON Palaeontology Program Department of Tourism and Culture Elaine Taylor, Minister 2003 Publication Note: This monograph was originally written as as Matheus 1995 and 2001. The dissertation also Chapters 2, 3, and 4 of the Ph.D. dissertation contained an appendix with stable isotope data on entitled, “Paleoecology and Ecomorphology of the modern and Pleistocene carnivores along with a Giant Short-Faced Bear in Eastern Beringia,” manual for extracting and purifying collagen from completed by the author in 1997 at The University bone. The present monograph may be cited of Alaska Fairbanks. The content is essentially directly, but if the citation is used to establish unchanged, except for minor editing, typographic when the ideas herein were established or data corrections, and re-formatting. The complete herein made public, then the dissertation or dissertation contained two additional papers Matheus (1995) take precedence. (Chapters 1 and 5) that are cited in this monograph YUKON Palaeontology Program Department of Tourism and Culture Elaine Taylor, Minister 2003 LOCOMOTOR ADAPTATIONS AND ECOMORPHOLOGY OF SHORT-FACED BEARS (Arctodus simus) IN EASTERN BERINGIA Paul E. Matheus TABLE OF CONTENTS Frontispiece -
Article XXIV.-List of the Pleistocene Fauna from Hay Springs, Nebraska
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Mammalogy Papers: University of Nebraska State Museum Museum, University of Nebraska State 1902 Article XXIV.-List of the Pleistocene Fauna from Hay Springs, Nebraska W. D. Matthew Follow this and additional works at: https://digitalcommons.unl.edu/museummammalogy Matthew, W. D., "Article XXIV.-List of the Pleistocene Fauna from Hay Springs, Nebraska" (1902). Mammalogy Papers: University of Nebraska State Museum. 284. https://digitalcommons.unl.edu/museummammalogy/284 This Article is brought to you for free and open access by the Museum, University of Nebraska State at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Mammalogy Papers: University of Nebraska State Museum by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Article XXIV.-LIST OF THE PLEISTOCENE FAUNA FROM HAY SPRINGS, NEBRASKA. By W. D. MATTHEW. In I893 and I897 field-parties from the American Museum were sent out by Professor Osborn to collect in the Pleistocene at this locality, a bone-bed near the Niobrara River, not far from Hay Springs. A large collection of horse and camel re- mains was obtained, and a few specimens of other animals. The horses have been carefully studied by Mr. Gidley, the camels by Dr. Wortman; the remainder of the fauna has been revised and partially studied by the writer, but no results have hitherto been published. A list of the fauna may be of some interest to compare with that found in the Sheridan or Equus Beds at other localities. The appended lists, when based on materials in the Cope Collection, are from deter- minations by Professor Cope, revised in a few cases by the writer.