Determining the Gait of Miocene, Pliocene, and Pleistocene Horses from Fossilized Trackways
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Middle Miocene Paleoenvironmental Reconstruction of the Central Great Plains from Stable Carbon Isotopes in Large Mammals Willow H
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Dissertations & Theses in Earth and Atmospheric Earth and Atmospheric Sciences, Department of Sciences 7-2017 Middle Miocene Paleoenvironmental Reconstruction of the Central Great Plains from Stable Carbon Isotopes in Large Mammals Willow H. Nguy University of Nebraska-Lincoln, [email protected] Follow this and additional works at: http://digitalcommons.unl.edu/geoscidiss Part of the Geology Commons, Paleobiology Commons, and the Paleontology Commons Nguy, Willow H., "Middle Miocene Paleoenvironmental Reconstruction of the Central Great Plains from Stable Carbon Isotopes in Large Mammals" (2017). Dissertations & Theses in Earth and Atmospheric Sciences. 91. http://digitalcommons.unl.edu/geoscidiss/91 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Dissertations & Theses in Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. MIDDLE MIOCENE PALEOENVIRONMENTAL RECONSTRUCTION OF THE CENTRAL GREAT PLAINS FROM STABLE CARBON ISOTOPES IN LARGE MAMMALS by Willow H. Nguy A THESIS Presented to the Faculty of The Graduate College at the University of Nebraska In Partial Fulfillment of Requirements For the Degree of Master of Science Major: Earth and Atmospheric Sciences Under the Supervision of Professor Ross Secord Lincoln, Nebraska July, 2017 MIDDLE MIOCENE PALEOENVIRONMENTAL RECONSTRUCTION OF THE CENTRAL GREAT PLAINS FROM STABLE CARBON ISOTOPES IN LARGE MAMMALS Willow H. Nguy, M.S. University of Nebraska, 2017 Advisor: Ross Secord Middle Miocene (18-12 Mya) mammalian faunas of the North American Great Plains contained a much higher diversity of apparent browsers than any modern biome. -
Southern Exposures
Searching for the Pliocene: Southern Exposures Robert E. Reynolds, editor California State University Desert Studies Center The 2012 Desert Research Symposium April 2012 Table of contents Searching for the Pliocene: Field trip guide to the southern exposures Field trip day 1 ���������������������������������������������������������������������������������������������������������������������������������������������� 5 Robert E. Reynolds, editor Field trip day 2 �������������������������������������������������������������������������������������������������������������������������������������������� 19 George T. Jefferson, David Lynch, L. K. Murray, and R. E. Reynolds Basin thickness variations at the junction of the Eastern California Shear Zone and the San Bernardino Mountains, California: how thick could the Pliocene section be? ��������������������������������������������������������������� 31 Victoria Langenheim, Tammy L. Surko, Phillip A. Armstrong, Jonathan C. Matti The morphology and anatomy of a Miocene long-runout landslide, Old Dad Mountain, California: implications for rock avalanche mechanics �������������������������������������������������������������������������������������������������� 38 Kim M. Bishop The discovery of the California Blue Mine ��������������������������������������������������������������������������������������������������� 44 Rick Kennedy Geomorphic evolution of the Morongo Valley, California ���������������������������������������������������������������������������� 45 Frank Jordan, Jr. New records -
Pleistocene) of California, USA
UC Berkeley PaleoBios Title Taphonomic bias in collections of horse phalanges from the Barstow Formation (Miocene) and Rancho La Brea (Pleistocene) of California, USA Permalink https://escholarship.org/uc/item/3pg5b0ks Journal PaleoBios, 38(1) ISSN 0031-0298 Authors Shi, Yaoran Gu, Victoria W. Farke, Andrew A. Publication Date 2021 DOI 10.5070/P9381052921 Supplemental Material https://escholarship.org/uc/item/3pg5b0ks#supplemental License https://creativecommons.org/licenses/by-nc-sa/4.0/ 4.0 Peer reviewed eScholarship.org Powered by the California Digital Library University of California PaleoBios 38:1–12, April 22, 2021 PaleoBios OFFICIAL PUBLICATION OF THE UNIVERSITY OF CALIFORNIA MUSEUM OF PALEONTOLOGY YAORAN SHI, VICTORIA W. GU, & ANDREW A. FARKE (2021). Tapho- nomic bias in collections of horse phalanges from the Barstow Forma- tion (Miocene) and Rancho La Brea (Pleistocene) of California, USA Cover: Scaphohippus sp. pes in lateral view, showing generalized skeletal anatomy. Illustration by Rob Soto. Citation: Shi, Y., V.W. Gu, and A.A. Farke. 2021. Taphonomic bias in collections of horse phalanges from the Barstow For- mation (Miocene) and Rancho La Brea (Pleistocene) of California, USA. PaleoBios, 38. ucmp_paleobios_52921. Taphonomic bias in collections of horse phalanges from the Barstow Formation (Miocene) and Rancho La Brea (Pleistocene) of California, USA YAORAN SHI¹, VICTORIA W. GU¹, AND ANDREW A. FARKE1–3* ¹The Webb Schools, 1175 West Baseline Road, Claremont, CA 91711 [email protected]; [email protected] ²Raymond M. Alf Museum of Paleontology at The Webb Schools, Claremont, CA 91711 [email protected] ³Dinosaur Institute, Natural History Museum of Los Angeles County, 900 Exposition Blvd., Los Angeles, CA 90007 years ago, southern California), but anecdotal observations suggested that not all positions (proximal, Isolatedmiddle, and equid distal/ungual) phalanges are of relatively the primary common digit (digit finds inIII) the are Barstow recovered Formation with equal (Miocene, frequency. -
Do Trissico Superior Do Rio Grande Do
Ano 23 - Edição especial VI Simpósio Brasileiro de Paleontologia de Vertebrados Ribeirão Preto - Maio/2008 Paleontologia em Destaque. Edição Especial VI Simpósio Brasileiro de Paleontologia de Vertebrados Editores para esta edição especial: Max C. Langer, Jonathas S. Bittencourt e Mariela C. Castro Tiragem: 200 exemplares. Distribuídos em 27 de maio de 2008. Impressão: Gráfica Martingraf Endereço: Laboratório de Paleontologia, FFCLRP-USP. Av. Bandeirantes 3.900. 14040-901, Ribeirão Preto-SP E-mail: [email protected] Web: http://www.sbpbrasil.org/ Paleontologia em Destaque: boletim informativo da Sociedade Brasileira de Paleontologia. -- Vol. 1, no 1 (1984) - ISSN: 1516-1811 1. Geociências. 2. Paleontologia. 3. Sociedade Brasileira de Paleontologia SOCIEDADE BRASILEIRA DE PALEONTOLOGIA (GESTÃO 2007-2009) Presidente: João Carlos Coimbra (UFRGS) Vice-Presidente: Ana Maria Ribeiro (FZB/RS) 1° Secretário: Marina Bento Soares (UFRGS) 2ª Secretária: Soraia Girardi Bauermann (ULBRA) 1ª Tesoureira: Patrícia Hadler Rodrigues (FZB/RS) 2ª Tesoureira: Karin Elise Bohns Meyer (UFMG) Diretora de Publicações: Carla B. Kotzian (UFSM) 2 VI Simpósio Brasileiro de Paleontologia de Vertebrados Boletim de Resumos Editores Max C. Langer Jonathas S. Bittencourt Mariela C. Castro FFCLRP-USP, Ribeirão Preto-SP 2008 3 Logotipo: A concepção tripartida do logotipo do VI Simpósio Brasileiro de Paleontologia de Vertebrados reflete as três eras do Fanerozóico e suas denominações populares: Paleozóico ou “Era dos Peixes” (representado pelo tubarão Tribodus limae, apesar deste ser do Mesozóico), Mesozóico ou “Era dos Répteis” (representado pelo dinossauro Staurikosaurus pricei) e Cenozóico ou “Era dos Mamíferos” (representado pelo tigre dentes-de-sabre Smilodon populator). Ainda, os três táxons escolhidos são representativos dos, talvez, três mais importantes, ou ao menos mais famosos, depósitos fossilíferos contendo vertebrados no Brasil: a Formação Santana, Cretáceo inferior do sul do Ceará (representada por T. -
The Evolution of Occlusal Enamel Complexity in Middle
THE EVOLUTION OF OCCLUSAL ENAMEL COMPLEXITY IN MIDDLE MIOCENE TO RECENT EQUIDS (MAMMALIA: PERISSODACTYLA) OF NORTH AMERICA by NICHOLAS ANTHONY FAMOSO A THESIS Presented to the Department of Geological Sciences and the Graduate School of the University of Oregon in partial fulfillment of the requirements for the degree of Master of Science June 2013 THESIS APPROVAL PAGE Student: Nicholas Anthony Famoso Title: The Evolution of Occlusal Enamel Complexity in Middle Miocene to Recent Equids (Mammalia: Perissodactyla) of North America This thesis has been accepted and approved in partial fulfillment of the requirements for the Master of Science degree in the Department of Geological Sciences by: Dr. Edward Davis Chair Dr. Qusheng Jin Member Dr. Stephen Frost Outside Member and Kimberly Andrews Espy Vice President for Research & Innovation/Dean of the Graduate School Original approval signatures are on file with the University of Oregon Graduate School. Degree awarded June 2013 ii © 2013 Nicholas Anthony Famoso iii THESIS ABSTRACT Nicholas Anthony Famoso Master of Science Department of Geological Sciences June 2013 Title: The Evolution of Occlusal Enamel Complexity in Middle Miocene to Recent Equids (Mammalia: Perissodactyla) of North America Four groups of equids, “Anchitheriinae,” Merychippine-grade Equinae, Hipparionini, and Equini, coexisted in the middle Miocene, and only the Equini remains after 16 million years of evolution and extinction. Each group is distinct in its occlusal enamel pattern. These patterns have been compared qualitatively but rarely quantitatively. The processes controlling the evolution of these occlusal patterns have not been thoroughly investigated with respect to phylogeny, tooth position, and climate through geologic time. I investigated two methods of quantitative analysis, Occlusal Enamel Index for shape and fractal dimensionality for complexity. -
Mojave Miocene Robert E
Mojave Miocene Robert E. Reynolds, editor California State University Desert Studies Center 2015 Desert Symposium April 2015 Front cover: Rainbow Basin syncline, with rendering of saber cat by Katura Reynolds. Back cover: Cajon Pass Title page: Jedediah Smith’s party crossing the burning Mojave Desert during the 1826 trek to California by Frederic Remington Past volumes in the Desert Symposium series may be accessed at <http://nsm.fullerton.edu/dsc/desert-studies-center-additional-information> 2 2015 desert symposium Table of contents Mojave Miocene: the field trip 7 Robert E. Reynolds and David M. Miller Miocene mammal diversity of the Mojave region in the context of Great Basin mammal history 34 Catherine Badgley, Tara M. Smiley, Katherine Loughney Regional and local correlations of feldspar geochemistry of the Peach Spring Tuff, Alvord Mountain, California 44 David C. Buesch Phytoliths of the Barstow Formation through the Middle Miocene Climatic Optimum: preliminary findings 51 Katharine M. Loughney and Selena Y. Smith A fresh look at the Pickhandle Formation: Pyroclastic flows and fossiliferous lacustrine sediments 59 Jennifer Garrison and Robert E. Reynolds Biochronology of Brachycrus (Artiodactyla, Oreodontidae) and downward relocation of the Hemingfordian– Barstovian North American Land Mammal Age boundary in the respective type areas 63 E. Bruce Lander Mediochoerus (Mammalia, Artiodactyla, Oreodontidae, Ticholeptinae) from the Barstow and Hector Formations of the central Mojave Desert Province, southern California, and the Runningwater and Olcott Formations of the northern Nebraska Panhandle—Implications of changes in average adult body size through time and faunal provincialism 83 E. Bruce Lander Review of peccaries from the Barstow Formation of California 108 Donald L. -
The Evolution of Equid Monodactyly: a Review Including a New Hypothesis
Janis, C., & Bernor, R. (2019). The evolution of equid monodactyly: a review including a new hypothesis. Frontiers in Ecology and Evolution, 7, [119]. https://doi.org/10.3389/fevo.2019.00119 Publisher's PDF, also known as Version of record License (if available): CC BY Link to published version (if available): 10.3389/fevo.2019.00119 Link to publication record in Explore Bristol Research PDF-document This is the final published version of the article (version of record). It first appeared online via Frontiers Media at https://www.frontiersin.org/articles/10.3389/fevo.2019.00119/full . Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/pure/about/ebr-terms REVIEW published: 12 April 2019 doi: 10.3389/fevo.2019.00119 The Evolution of Equid Monodactyly: A Review Including a New Hypothesis Christine M. Janis 1,2* and Raymond L. Bernor 3 1 Department of Ecology and Evolutionary Biology, Brown University, Providence, RI, United States, 2 School of Earth Sciences, University of Bristol, Bristol, United Kingdom, 3 Laboratory of Evolutionary Biology, Department of Anatomy, College of Medicine, Howard University, Washington, DC, United States The traditional story of horse evolution is well-known: over time, horses became larger, they attained higher-crowned teeth, and they changed from having three toes (tridactyly) to a single toe (monodactyly). Evolution is often perceived as a progression toward some optimum outcome, in this case the “Noble Steed.” However, the evolutionary advantages of monodactyly are not entirely clear, other than the notion that it must somehow be “more efficient,” especially at the larger body size of the genus Equus. -
In Search of Vanished Ages--Field Trips to Fossil Localities in California, Nevada, and Utah
i In Search Of Vanished Ages Field trips to fossil localities in California, Nevada, and Utah By Inyo A view across the middle Miocene Barstow Formation on California’s Mojave Desert. Here, limestone concretions that occur in rocks deposited in a freshwater lake system approximately 17 million year-ago produce exquisitely preserved, fully three-dimensional insects, spiders, water mites, and fairy shrimp that can be dissolved free of their stone encasings with a diluted acid solution—one of only a handful of localities worldwide where fossil insects can be removed successfully from their matrixes without obliterating the specimens. ii Table of Contents Chapter Page 1—Fossil Plants At Aldrich Hill 1 2—A Visit To Ammonite Canyon, Nevada 6 3—Fossil Insects And Vertebrates On The Mojave Desert, California 15 4—Fossil Plants At Buffalo Canyon, Nevada 45 5--Ordovician Fossils At The Great Beatty Mudmound, Nevada 50 6--Fossil Plants And Insects At Bull Run, Nevada 58 7-- Field Trip To The Copper Basin Fossil Flora, Nevada 65 8--Trilobites In The Nopah Range, Inyo County, California 70 9--Field Trip To A Vertebrate Fossil Locality In The Coso Range, California 76 10--Plant Fossils In The Dead Camel Range, Nevada 83 11-- A Visit To The Early Cambrian Waucoba Spring Geologic Section, California 88 12-- Fossils In Millard County, Utah 95 13--A Visit To Fossil Valley, Great Basin Desert, Nevada 107 14--High Inyo Mountains Fossils, California 119 15--Early Cambrian Fossils In Western Nevada 126 16--Field Trip To The Kettleman Hills Fossil District, -
UC Berkeley Paleobios
UC Berkeley PaleoBios Title New remains of middle Miocene equids from the Cajon Valley Formation, San Bernardino National Forest, San Bernardino County, California, USA Permalink https://escholarship.org/uc/item/6dv597pp Journal PaleoBios, 38(1) ISSN 0031-0298 Authors Stoneburg, Brittney E. McDonald, Andrew T. Dooley, Jr., Alton C. et al. Publication Date 2021 DOI 10.5070/P9381052265 Supplemental Material https://escholarship.org/uc/item/6dv597pp#supplemental License https://creativecommons.org/licenses/by-nc-sa/4.0/ 4.0 Peer reviewed eScholarship.org Powered by the California Digital Library University of California PaleoBios 38:1–10, February 25, 2021 PaleoBios OFFICIAL PUBLICATION OF THE UNIVERSITY OF CALIFORNIA MUSEUM OF PALEONTOLOGY BRITTNEY E. STONEBURG, ANDREW T. MCDONALD, ALTON C. DOOLEY JR., ERIC SCOTT, & CHARLOTTE J. H. HOHMAN (2021). New remains of middle Miocene equids from the Cajon Valley Formation, San Bernardi- no National Forest, San Bernardino County, California, USA. Cover: A. Parahippus brevidens B. Ar- chaeohippus mourningi C. Scaphohippus sumani A selection of Miocene horse teeth figured in this paper. , WSC 8914 upper left M1. Citation: , WS 8826 upper right M3. , WSC 8922 partial right dentary, p4–m3. Scale bars=1 cm. Paleo- Bios Stoneburg, B.E., A.T. McDonald, A.C. Dooley Jr., E. Scott, and C.J.H. Hohman. 2021. New remains of middle Miocene equids from the Cajon Valley Formation, San Bernardino National Forest, San Bernardino County, California, USA. , 38. ucmp_paleobios_52265. New remains of middle Miocene equids from the Cajon Valley Formation, San Bernardino National Forest, San Bernardino County, California, USA * BRITTNEY E. STONEBURG¹ , ANDREW T. MCDONALD¹, ALTON C. -
2010 Overboard in the Mojave
O v e rb o a rd in the Mojave 20 million years of lakes and wetlands edited and compiled by Robert E. Reynolds and David M. Miller and Abstracts of Proceedings: the 2010 Desert Symposium compiled by Robert E. Reynolds Desert Studies Consortium California State University, Fullerton April, 2010 FRONT COVER : The Troy Lake arm of Manix Lake laps against the Newberry Mountains, January 24, 2010. BACK COVER : Above: The Barstow Formation in the Mud Hills is the type locality for the Barstovian land mammal age of the North American continent. Biostratigraphic ranges of taxa are constrained by dated volcanic ashes and magnetostratigraphic polarity. Below: Strata of the Barstow Formation have been folded, faulted, and planed by erosion in the last 10 million years. The colorful Miocene sediments are unconformably overlain by flat-lying tan arkosic sandstone. TITLE PAGE : Rob Fulton kayaked on Silver Lake in 2005. 2 2010 Desert Symposium Table of contents Overboard in the Mojave: the field guide ......................................................................................................................... 7 Robert E. Reynolds and David M. Miller Environments of nearshore lacustrine deposition in the Pleistocene Lake Manix basin, south-central California ............................................................................................................................................................24 Marith C. Reheis and David M. Miller Stratigraphy and paleontology of the middle to late Pleistocene Manix Formation, and paleoenvironments -
Reconciling Taxon Senescence with the Red Queen's
Reconciling taxon senescence with the Red Queen’s Hypothesis Indrė Žliobaitė* (a,b,c), Mikael Fortelius (a,b) and Nils Chr. Stenseth (b) (a) Department of Geosciences and Geography, University of Helsinki, P.O. Box 64, FI-00014 Helsinki, Finland (b) Centre for Ecological and Evolutionary Synthesis (CEES) Dept. of Biosciences, University of Oslo, P.O. Box 1066 Blindern, NO-0316 Oslo, Norway (c) Department of Computer Science, University of Helsinki, P.O. Box 64, FI-00014 Helsinki, Finland *Correspondence: [email protected] October 23, 2017 (preprint) Image credit: Ika Österblad 1 In the fossil record, taxa exhibit a regular pattern of waxing and waning of occupancy, range or diversity between their origin and extinction. This hat-like pattern is well established for species, genera and higher taxa of terrestrial mammals1,2,3, marine invertebrates4,5,6, marine micro-organisms7, and recently living Hawaiian clades of animals and plants8. This pattern appears to contradict the Law of Constant Extinction9, which states that the probability of a taxon’s extinction is independent of its age. Here we show that the apparent contradiction between stochastically constant extinction and the seemingly deterministic “hat” pattern disappears when we consider the peak of taxon’s expansion rather than its final extinction. To a first approximation we find that biotic drivers of evolution pertain mainly to the peak, abiotic drivers mainly to the extinction of taxa. The Red Queen’s Hypothesis9, one of the most influential ideas in evolutionary biology since Darwin, was originally proposed as an explanation of the Law of Constant Extinction. Much effort has since been devoted to the question how this hypothesis, emphasizing biotic interactions, relates to the effects of environmental change. -
Cultural and Paleontological Resources
APPENDIX F (F1 – F4) CULTURAL AND PALEONTOLOGICAL RESOURCES APPENDIX F1 CULTURAL RESOURCES SETTING CULTURAL RESOURCES SETTING Prehistoric Context Archaeological context is presented from various sources in the southwestern portion of the Great Basin, and includes regional data from the Colorado River and Lower Virgin River areas. Cultural resource documents demonstrate that Native Americans have occupied the Three Corners region (western Arizona, southern Nevada, and southeastern California) since the end of the Pleistocene (10,000 Before Christ [BC]), continuing through the initial and middle stages of the Holocene (8000 - 2000 BC) and until the ethnographic present (2000 BC – Present). Archaeologically, cultures are defined by their collective artifact assemblages. Diagnostic artifacts such as projectile points and ceramics are signatures for distinct periods of human occupation. Unfortunately, the open-air context is unsuitable for the preservation of leather, basketry, or wooden objects and many artifacts have been lost to the ravages of time and unfavorable environmental conditions. Objects that persist through time become the contributing elements to the archaeological record (e.g., chipped stone and ceramics) and are responsible for supplying invaluable information about prehistoric cultures and lifeways. Two phases of prehistory are, however, without ceramics and perishable organic artifacts: the Paleoarchaic (9500–5500 BC) and Archaic (5500 BC – Anno Domini [AD] 500). Efforts to refine the cultural chronology of the Mojave Desert and the surrounding environs have recently resulted in a new understanding of the cultural periods and a renewed interest in the archaeology of the Three Corners region (Roberts and Ahlstrom 2000; Ahlstrom et al. 2005; Ahlstrom 2006; Seymour 2006; Lyon and Ahlstrom 2006).