Linking Top-Down Forces to the Pleistocene Megafaunal Extinctions
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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. -
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 -
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). -
La Brea and Beyond: the Paleontology of Asphalt-Preserved Biotas
La Brea and Beyond: The Paleontology of Asphalt-Preserved Biotas Edited by John M. Harris Natural History Museum of Los Angeles County Science Series 42 September 15, 2015 Cover Illustration: Pit 91 in 1915 An asphaltic bone mass in Pit 91 was discovered and exposed by the Los Angeles County Museum of History, Science and Art in the summer of 1915. The Los Angeles County Museum of Natural History resumed excavation at this site in 1969. Retrieval of the “microfossils” from the asphaltic matrix has yielded a wealth of insect, mollusk, and plant remains, more than doubling the number of species recovered by earlier excavations. Today, the current excavation site is 900 square feet in extent, yielding fossils that range in age from about 15,000 to about 42,000 radiocarbon years. Natural History Museum of Los Angeles County Archives, RLB 347. LA BREA AND BEYOND: THE PALEONTOLOGY OF ASPHALT-PRESERVED BIOTAS Edited By John M. Harris NO. 42 SCIENCE SERIES NATURAL HISTORY MUSEUM OF LOS ANGELES COUNTY SCIENTIFIC PUBLICATIONS COMMITTEE Luis M. Chiappe, Vice President for Research and Collections John M. Harris, Committee Chairman Joel W. Martin Gregory Pauly Christine Thacker Xiaoming Wang K. Victoria Brown, Managing Editor Go Online to www.nhm.org/scholarlypublications for open access to volumes of Science Series and Contributions in Science. Natural History Museum of Los Angeles County Los Angeles, California 90007 ISSN 1-891276-27-1 Published on September 15, 2015 Printed at Allen Press, Inc., Lawrence, Kansas PREFACE Rancho La Brea was a Mexican land grant Basin during the Late Pleistocene—sagebrush located to the west of El Pueblo de Nuestra scrub dotted with groves of oak and juniper with Sen˜ora la Reina de los A´ ngeles del Rı´ode riparian woodland along the major stream courses Porciu´ncula, now better known as downtown and with chaparral vegetation on the surrounding Los Angeles. -
Dinner in a Dinosaur
Benchmarks DECEMBER 31, 1853: DINNER IN A DINOSAUR he weather in London on Saturday, Dec. 31, 1853, could On New Year’s Eve, 1853, Benjamin Waterhouse Hawkins hosted not have pleased Benjamin Waterhouse Hawkins. a formal dinner in the mold of an Iguanodon. After a relatively warm Friday, the temperature had plummeted, snow had begun to fall, and for the first to celebrate the “triumphs of industry and art,” and hired Ttime in more than a decade, masses of ice floated down the Hawkins to direct the “Fossil Department.” They tasked him Thames River. The snow made the streets so slippery that with populating a vast geologic display with giant monsters injured pedestrians filled the hospitals. of the ancient world, including the first three dinosaurs ever For New Year’s Eve, Hawkins was hosting an elaborate feast described: Megalosaurus, Iguanodon and Hylaeosaurus. at his sculpting studio in Sydenham, 11 kilometers south of Hawkins was uniquely qualified to bring these great ani- London. Would his guests be able to find transportation out to mals to life. He had initially achieved fame for his detailed Sydenham and then across the pastures of muddy swamp that illustrations of animals collected by British explorers, includ- surrounded the wooden building where the dinner would be ing the still relatively obscure naturalist Charles Darwin. held? Hawkins hoped so; he had been planning the meal for Subsequently, Hawkins started to sculpt, and to write and more than a month. It would be the first time that most of his illustrate books on animal anatomy. For his efforts in taking dinner-mates had seen the incredible life-sized dinosaurs that new scientific findings and translating them into words and he was building for the Crystal Palace Exhibition, which Queen images accessible to the general public, Hawkins earned Victoria and Prince Albert would open to the public in June. -
Genomic Adaptations and Evolutionary History of the Extinct Scimitar-Toothed Cat, Homotherium Latidens
Report Genomic Adaptations and Evolutionary History of the Extinct Scimitar-Toothed Cat, Homotherium latidens Graphical Abstract Authors Ross Barnett, Michael V. Westbury, Marcela Sandoval-Velasco, ..., Jong Bhak, Nobuyuki Yamaguchi, M. Thomas P. Gilbert Correspondence [email protected] (M.V.W.), [email protected] (M.T.P.G.) In Brief Here, Barnett et al. sequence the nuclear genome of Homotherium latidens through a combination of shotgun and target-capture approaches. Analyses confirm Homotherium to be a highly divergent lineage from all living cat species (22.5 Ma) and reveal genes under selection putatively related to a cursorial and diurnal hunting behavior. Highlights d Nuclear genome and exome analyses of extinct scimitar- toothed cat, Homotherium latidens d Homotherium was a highly divergent lineage from all living cat species (22.5 Ma) d Genetic adaptations to cursorial and diurnal hunting behaviors d Relatively high levels of genetic diversity in this individual Barnett et al., 2020, Current Biology 30, 1–8 December 21, 2020 ª 2020 The Authors. Published by Elsevier Inc. https://doi.org/10.1016/j.cub.2020.09.051 ll Please cite this article in press as: Barnett et al., Genomic Adaptations and Evolutionary History of the Extinct Scimitar-Toothed Cat, Homotherium latidens, Current Biology (2020), https://doi.org/10.1016/j.cub.2020.09.051 ll OPEN ACCESS Report Genomic Adaptations and Evolutionary History of the Extinct Scimitar-Toothed Cat, Homotherium latidens Ross Barnett,1,35 Michael V. Westbury,1,35,36,* Marcela Sandoval-Velasco,1,35 Filipe Garrett Vieira,1 Sungwon Jeon,2,3 Grant Zazula,4 Michael D. -
Megaloceros Giganteus) from the Pleistocene in Poland
Palaeontologia Electronica palaeo-electronica.org Healed antler fracture from a giant deer (Megaloceros giganteus) from the Pleistocene in Poland Kamilla Pawłowska, Krzysztof Stefaniak, and Dariusz Nowakowski ABSTRACT We evaluated the skull of an ancient giant deer with a deformity of one antler. The skull was found in the 1930s in the San River near Barycz, in southeastern Poland. Its dating (39,800±1000 yr BP) corresponds to MIS-3, when the giant deer was wide- spread in Europe. Our diagnostics for the antler included gross morphology, radiogra- phy, computed tomography, and histopathology. We noted signs of fracture healing of the affected antler, including disordered arrangement of lamellae, absence of osteons, and numerous Volkmann’s canals remaining after blood vessel loss. The antler defor- mity appears to be of traumatic origin, with a healing component. No similar evaluation process has been described previously for this species. Kamilla Pawłowska. corresponding author, Institute of Geology, Adam Mickiewicz University, Maków Polnych 16, Poznań 61-606, Poland, [email protected] Krzysztof Stefaniak. Division of Palaeozoology, Department of Evolutionary Biology and Ecology, Faculty of Biological Sciences, University of Wrocław, Sienkiewicza 21, Wrocław 50-335, Poland, [email protected] Dariusz Nowakowski. Department of Anthropology, Wroclaw University of Environmental and Life Sciences, Kożuchowska 6/7, Wrocław 51-631, Poland, [email protected] Keywords: giant deer; Megaloceros giganteus; paleopathology; Pleistocene; Poland INTRODUCTION -
New Record of Terminal Pleistocene Elk/Wapiti (Cervus Canadensis) from Ohio, USA
2 TERMINAL PLEISTOCENE ELK FROM OHIO VOL. 121(2) New Record of Terminal Pleistocene Elk/Wapiti (Cervus canadensis) from Ohio, USA BRIAN G. REDMOND1, Department of Archaeology, Cleveland Museum of Natural History, Cleveland, OH, USA; DAVID L. DYER, Ohio History Connection, Columbus, OH, USA; and CHARLES STEPHENS, Sugar Creek Chapter, Archaeological Society of Ohio, Massillon, OH, USA. ABSTRACT. The earliest appearance of elk/wapiti (Cervus canadensis) in eastern North America is not thoroughly documented due to the small number of directly dated remains. Until recently, no absolute dates on elk bone older than 10,000 14C yr BP (11,621 to 11,306 calibrated years (cal yr) BP) were known from this region. The partial skeleton of the Tope Elk was discovered in 2017 during commercial excavation of peat deposits from a small bog in southeastern Medina County, Ohio, United States. Subsequent examination of the remains revealed the individual to be a robust male approximately 8.5 years old at death. The large size of this individual is compared with late Holocene specimens and suggests diminution of elk since the late Pleistocene. Two accelerator mass spectrometry (AMS) radiocarbon assays on bone collagen samples taken from the scapula and metacarpal of this individual returned ages of 10,270 ± 30 14C yr BP (Beta-477478) (12,154 to 11,835 cal yr BP) and 10,260 ± 30 14C yr BP (Beta-521748) (12,144 to 11,830 cal yr BP), respectively. These results place Cervus canadensis in the terminal Pleistocene of the eastern woodlands and near the establishment of the mixed deciduous forest biome over much of the region. -
How the 'Seven Deadly Agents Of
Paper presented at the How the ‘Seven Deadly Agents of Destruction’ conference can help preserve the Crystal Palace Dinosaurs Liesa Brierley, Ellinor Michel, Anthony Lewis, Chris Aldhous and Lois Olmstead Introduction Compared to collections kept safe inside museums, outdoor sculpture is affected by additional risk factors. Sculpture in the public realm is exposed to the elements, pollution and direct sunshine. It is more vulnerable to vandalism and the proximity to nature can also take its toll. At the same time, the condition of outdoor sculpture is often not monitored as rigorously as that of museum collections. However, damage doesn’t go unnoticed by the public and, channelled in the right way, the public’s critical eye can be turned to positive pressure, increasing support for conservation work and helping to improve conditions for the displays. To conservation professionals, the Canadian Conservation Institute’s framework of Ten Agents of Deterioration is a familiar and well-established way of describing risk factors to cultural heritage. This paper describes an attempt to translate this framework into a short animated film about risks to outdoor sculpture, using the Crystal Palace Dinosaurs, a renowned Victorian sculpture park in south London, as the stage for the message. The film is aimed at a broad audience of non-professionals of all ages and it is hoped that it will deliver an increased sense of both understanding and ownership of the sculpture park. The Crystal Palace Dinosaurs The Crystal Palace Dinosaurs are the first life-sized sculptural reconstructions of extinct animals, built to engage and enlighten the public on the paradigm- shifting advances in science in the mid-19th century (Owen 1854, McCarthy and Gilbert 1994, Pigott 2004, Bramwell and Peck 2008). -
'Felis' Pamiri Ozansoy, 1959 (Carnivora, Felidae) from the Upper Miocene Of
1 Re-appraisal of 'Felis' pamiri Ozansoy, 1959 (Carnivora, Felidae) from the upper Miocene of 2 Turkey: the earliest pantherin cat? 3 4 Denis GERAADS and Stéphane PEIGNE 5 Centre de Recherche sur la Paléobiodiversité et les Paléoenvironnements (UMR 7207), Sorbonne 6 Universités, MNHN, CNRS, UPMC, CP 38, 8 rue Buffon, 75231 PARIS Cedex 05, France 7 8 Running head: 'Felis' pamiri from Turkey 9 10 Abstract 11 Although the divergence of the Panthera clade from other Felidae might be as old as the 12 earliest middle Miocene, its fossil record before the Pliocene is virtually non-existent. Here we 13 reassess the affinities of a felid from the early upper Miocene of Turkey, known by well-preserved 14 associated upper and lower dentitions. We conclude that it belongs to the same genus 15 (Miopanthera Kretzoi, 1938) as the middle Miocene 'Styriofelis' lorteti (Gaillard, 1899), and that 16 this genus is close to, if not part of, the Panthera clade. 17 18 Keywords: Carnivora – Felidae – Pantherini – Phylogeny – Upper Miocene – Turkey 19 20 Introduction 21 The Felidae can be divided in two subfamilies (Johnson et al. 2006; Werdelin et al. 2010) 22 Felinae (= Pantherinae, or big cats, plus Felinae, or smaller cats, in e.g., Wilson and Mittermeier 23 2009) and Machairodontinae, although their monophyly is hard to demonstrate, the second one 24 being extinct. The Neogene fossil record of the Machairodontinae, or saber-toothed felids, is 25 satisfactory, but that of other members of the family, conveniently called conical-toothed felids 26 (although several of them have compressed, flattened canines) is much more patchy. -
Patterns of Late Quaternary Megafaunal Extinctions in Europe and Northern Asia
Cour. Forsch.-Inst. Senckenberg | 259 | 287 – 297 | 2 Figs | Frankfurt a. M., 13. 12. 2007 Patterns of Late Quaternary megafaunal extinctions in Europe and northern Asia With 2 figs Anthony J. STUART & Adrian M. LISTER A b s t r a c t This paper summarizes the results so far of our ‘Late Quaternary Megafaunal Extinctions’ project, focussing on an assessment of latest available dates for selected target species from Europe and northern Asia. Our approach is to directly radiocarbon-date material of extinct megafauna to construct their spatio-temporal histories, and to seek correlations with the environmental and archaeological records with the aim of estab- lishing the cause or causes of extinction. So far we have focussed on Mammuthus primigenius, Coelodonta antiquitatis, and Megaloceros giganteus, and are accumulating data on Panthera leo/spelaea, Crocuta crocuta and Ursus spelaeus. Attempts to date Palaeoloxodon antiquus and Stephanorhinus hemitoechus (from southern Europe) were largely unsuccessful. The pattern of inferred terminal dates is staggered, with extinctions occurring over ca. 30 millennia, with some species previously thought extinct in the Late Pleistocene – M. primigenius and M. giganteus – surviving well into the Holocene. All species show dramatic range shifts in response to climatic/vegeta- tional changes, especially the beginning of the Last Glacial Maximum, Late Glacial Interstadial, Allerød, Younger Dryas and Holocene, and there was a general trend of progressive range reduction and fragmenta- tion prior to final extinction. With the possible exceptions of P. antiquus, S. hemitoechus and Homo nean- derthalensis, extinctions do not correlate with the appearance of modern humans. However, although most of the observed patterns can be attributed to environmental changes, some features – especially failures to recolonize – suggest human involvement.