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Jaws, Which Were Obtained by Dr. Hayden in the Bridger Baisin, Wyoming, the Year Previous
Article V.-OSTEOLOGY OF PATRIOFELIS, A MIDDLE EOCENE CREODONT. By J. L. WORTMAN, M. 1). PLATE I. HISTORY AND SYNONOMY. The genus Patriofelis was originally established by Dr. Leidy, in the 'Proceedings' of the Philadelphia Academy, March, I870, p. IO, upon the fragmentary portions of the rami of both lower jaws, which were obtained by Dr. Hayden in the Bridger Baisin, Wyoming, the year previous. In August, I872, Prof. Marsh described (Amer. Jour. Science, Vol. IV, p. io) from the same locality, some remains of a " gigantic Carnivore " which he referred to a new genus and species under the name of Limnofelis ferox. According to Prof. Marsh's statement, his specimen consists of portions of the skull, fragments of the lower jaw, some vertebrae, and other less important parts of the skeleton. In the same paper he describes a second species under the name of Limnofelis latidens, from a last upper premolar, which was obtained in the same horizon. Prof. Cope, in the 'American Naturalist' of i88o (Vol. XIV, p. 745), proposed a third genus from teeth and limb bones, which were collected by the writer in the Wind River Baisin in the summer of I879. To these remains Prof. Cope gave the name Protopsalis tig,-inus. Prof. Scott has described in tle 'Journal of the Philadelphia Academy,' i886 (Vol. IX, p. I74), some remains of a large Creodont from the Bridger formation, which he referred to Prof. Cope's genus Protopsalis. A new species of this genus was proposed by the writer (Bull. Amer. Mus. Nat. Hist., Vol. IV, p. -
Palaeontologia Electronica New Data on the Oxyaenidae from the Early
Palaeontologia Electronica http://palaeo-electronica.org New data on the Oxyaenidae from the Early Eocene of Europe; biostratigraphic, paleobiogeographic and paleoecologic implications Floréal Solé, Emmanuel Gheerbrant and Marc Godinot ABSTRACT The locality of Le Quesnoy (France; MP7) has yielded a diversified mammal fauna including especially large mammals. Oxyaenidae are well documented with two spe- cies identified: Oxyaena woutersi and Palaeonictis gigantea. The Le Quesnoy material illustrates almost the entire dentition of these species. Its study supports the generic attribution of Oxyaena woutersi. Its M2 is more secant than in the primitive Dipsalidictis, but the M1 appears to be slightly less secant than in the earliest species of Oxyaena. Oxyaena woutersi is a morphological intermediate between the Clarkforkian-Wasat- chian Dipsalidictis and the Wasatchian Oxyaena. The M2 of Palaeonictis gigantea is compared to the sole known molar of Dormaalodon woutersi. Dormaalodon is here demonstrated to be a junior synonym of Palaeonictis. Several postcranial elements of Oxyaena woutersi and Palaeonictis gigantea are described: they are the first described for European oxyaenids. The oxyaenid species from Le Quesnoy and Dormaal show a close affinity and support an age very close to MP7 for Le Quesnoy. The Le Quesnoy oxyaenids are morphologically close to the North American species of Wa0, which sup- ports correlation with this level. We revised the European Oxyaenidae previously described from younger localities. Fossils from Meudon, Sinceny and Abbey Wood (MP8+9) are referred to Oxyaena sp. A North American origin of the Oxyaenidae is confirmed. Our study supports a single dispersal event of oxyaenids from North Amer- ica to Europe followed by a short endemic local evolution. -
Hyaenodontidae (Creodonta, Mammalia) and the Position of Systematics in Evolutionary Biology
Hyaenodontidae (Creodonta, Mammalia) and the Position of Systematics in Evolutionary Biology by Paul David Polly B.A. (University of Texas at Austin) 1987 A dissertation submitted in partial satisfaction of the requirements for the degree of Doctor of Philosophy in Paleontology in the GRADUATE DIVISION of the UNIVERSITY of CALIFORNIA at BERKELEY Committee in charge: Professor William A. Clemens, Chair Professor Kevin Padian Professor James L. Patton Professor F. Clark Howell 1993 Hyaenodontidae (Creodonta, Mammalia) and the Position of Systematics in Evolutionary Biology © 1993 by Paul David Polly To P. Reid Hamilton, in memory. iii TABLE OF CONTENTS Introduction ix Acknowledgments xi Chapter One--Revolution and Evolution in Taxonomy: Mammalian Classification Before and After Darwin 1 Introduction 2 The Beginning of Modern Taxonomy: Linnaeus and his Predecessors 5 Cuvier's Classification 10 Owen's Classification 18 Post-Darwinian Taxonomy: Revolution and Evolution in Classification 24 Kovalevskii's Classification 25 Huxley's Classification 28 Cope's Classification 33 Early 20th Century Taxonomy 42 Simpson and the Evolutionary Synthesis 46 A Box Model of Classification 48 The Content of Simpson's 1945 Classification 50 Conclusion 52 Acknowledgments 56 Bibliography 56 Figures 69 Chapter Two: Hyaenodontidae (Creodonta, Mammalia) from the Early Eocene Four Mile Fauna and Their Biostratigraphic Implications 78 Abstract 79 Introduction 79 Materials and Methods 80 iv Systematic Paleontology 80 The Four Mile Fauna and Wasatchian Biostratigraphic Zonation 84 Conclusion 86 Acknowledgments 86 Bibliography 86 Figures 87 Chapter Three: A New Genus Eurotherium (Creodonta, Mammalia) in Reference to Taxonomic Problems with Some Eocene Hyaenodontids from Eurasia (With B. Lange-Badré) 89 Résumé 90 Abstract 90 Version française abrégéé 90 Introduction 93 Acknowledgments 96 Bibliography 96 Table 3.1: Original and Current Usages of Genera and Species 99 Table 3.2: Species Currently Included in Genera Discussed in Text 101 Chapter Four: The skeleton of Gazinocyon vulpeculus n. -
John Day Fossil Beds National Monument
ISSUE VIII JANUARY 2007 NARG Newsletter North America Research Group Northwest Fossil Fest Recap Last August NARG held it's first annual Northwest Fossil Fest held at INSIDE THIS ISSUE the Rice Museum in Hillsboro Oregon. The goal of the Fest was to NW Fossil Fest Recap 1 promote, educate, showcase fossils Radiocarbon Dating Fund 3 from the Pacific NW, and to have John Day Fossil Beds fun, all of which was accomplished. National Monument 3 Taxonomy Report #6 5 The tagline for the Fest is “Inspire, Inquire, Interact” and nothing What is “Fossil Search and Rescue? inspires more than displaying some of the amazing fossils specimens that Oregon Fossils have been found in the Pacific NW. Plants of the Jurassic Period 7 Tami Smith making a batch of Trilobite Cookie Many guests where surprised at the Trilobite Morphology 8 wide range of life forms that once lived where we do today. Inquiry minds want to know and we had a top-notch line up of guest speakers such as Dr. Dr. Ellen Morris Bishop, Dr. Jeffrey A. Myers, and Dr. William. N. Orr. This was a great opportunity for guest not only to learn more about the paleontology and geology of Oregon but also to meet 3 of the leading professionals in these fields. More Trilobite Cookie making There were many ways to interact, from the fossil preparation area where demonstrations took place on tools and techniques used to prepare fossils, to fossil identification, and of course all the kids activities that NARG setup. The Screen for Shark Teeth was probably the biggest hits and over 1000 Bone Valley shark teeth where given away. -
Mammal and Plant Localities of the Fort Union, Willwood, and Iktman Formations, Southern Bighorn Basin* Wyoming
Distribution and Stratigraphip Correlation of Upper:UB_ • Ju Paleocene and Lower Eocene Fossil Mammal and Plant Localities of the Fort Union, Willwood, and Iktman Formations, Southern Bighorn Basin* Wyoming U,S. GEOLOGICAL SURVEY PROFESS IONAL PAPER 1540 Cover. A member of the American Museum of Natural History 1896 expedition enter ing the badlands of the Willwood Formation on Dorsey Creek, Wyoming, near what is now U.S. Geological Survey fossil vertebrate locality D1691 (Wardel Reservoir quadran gle). View to the southwest. Photograph by Walter Granger, courtesy of the Department of Library Services, American Museum of Natural History, New York, negative no. 35957. DISTRIBUTION AND STRATIGRAPHIC CORRELATION OF UPPER PALEOCENE AND LOWER EOCENE FOSSIL MAMMAL AND PLANT LOCALITIES OF THE FORT UNION, WILLWOOD, AND TATMAN FORMATIONS, SOUTHERN BIGHORN BASIN, WYOMING Upper part of the Will wood Formation on East Ridge, Middle Fork of Fifteenmile Creek, southern Bighorn Basin, Wyoming. The Kirwin intrusive complex of the Absaroka Range is in the background. View to the west. Distribution and Stratigraphic Correlation of Upper Paleocene and Lower Eocene Fossil Mammal and Plant Localities of the Fort Union, Willwood, and Tatman Formations, Southern Bighorn Basin, Wyoming By Thomas M. Down, Kenneth D. Rose, Elwyn L. Simons, and Scott L. Wing U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1540 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1994 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Robert M. Hirsch, Acting Director For sale by U.S. Geological Survey, Map Distribution Box 25286, MS 306, Federal Center Denver, CO 80225 Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. -
(Microsyopidae, Primates) from the Paleocene-Eocene Thermal Maximum: One Species Or Two?
Molar Size and Shape Variation in a Large Sample of Niptomomys (Microsyopidae, Primates) from the Paleocene-Eocene Thermal Maximum: One Species or Two? by Rosa S. Felibert Department of Anthropology University of Florida 2017 ABSTRACT The oldest euprimates first appear during a period of rapid, short-term, global warming ~56 mya known as the Paleocene-Eocene Thermal Maximum (PETM). Plesiadapiform primates of similar size and dental morphology to euprimates were present in North America before the PETM, and may have been affected by the arrival of euprimates as ecological competitors. Screenwashing PETM fossil localities in the Bighorn Basin, Wyoming, has yielded many fossils (N≈600) of the microsyopid plesiadapiform Niptomomys. N. doreenae is known from before and after the PETM and may range through it. A second taxon, N. favorum, characterized by its small size and squarer M2 occlusal outline, was described from the large Castle Gardens locality sample. To better characterize PETM primate diversity, we test the validity of N. favorum against a sample of Niptomomys from Castle Gardens, other PETM localities, and published measurements. M2 occlusal outlines (N=62) revealed a continuous range from square to lingually compressed that encompasses the holotype of N. favorum. Linear measurements of M1 (N=127) and M2 (N=163) indicated M1’s from Castle Gardens are larger than those of later PETM localities (p=0.038), but produced no outliers, suggesting the PETM fauna contains one species of Niptomomys. PETM lower molars are smaller than all other measured Niptomomys teeth, paralleling the response to warming effects recorded in larger-bodied mammal lineages. -
A Three-Dimensional Analysis of Morphological Evolution and Locomotor Performance of the Carnivoran Forelimb
A Three-Dimensional Analysis of Morphological Evolution and Locomotor Performance of the Carnivoran Forelimb Alberto Martı´n-Serra*, Borja Figueirido, Paul Palmqvist Departamento de Ecologı´a y Geologı´a, Facultad de Ciencias, Universidad de Ma´laga, Ma´laga, Spain Abstract In this study, three-dimensional landmark-based methods of geometric morphometrics are used for estimating the influence of phylogeny, allometry and locomotor performance on forelimb shape in living and extinct carnivorans (Mammalia, Carnivora). The main objective is to investigate morphological convergences towards similar locomotor strategies in the shape of the major forelimb bones. Results indicate that both size and phylogeny have strong effects on the anatomy of all forelimb bones. In contrast, bone shape does not correlate in the living taxa with maximum running speed or daily movement distance, two proxies closely related to locomotor performance. A phylomorphospace approach showed that shape variation in forelimb bones mainly relates to changes in bone robustness. This indicates the presence of biomechanical constraints resulting from opposite demands for energetic efficiency in locomotion –which would require a slender forelimb– and resistance to stress –which would be satisfied by a robust forelimb–. Thus, we interpret that the need of maintaining a trade-off between both functional demands would limit shape variability in forelimb bones. Given that different situations can lead to one or another morphological solution, depending on the specific ecology of taxa, the evolution of forelimb morphology represents a remarkable ‘‘one-to-many mapping’’ case between anatomy and ecology. Citation: Martı´n-Serra A, Figueirido B, Palmqvist P (2014) A Three-Dimensional Analysis of Morphological Evolution and Locomotor Performance of the Carnivoran Forelimb. -
Genus/Species Skull Ht Lt Wt Stage Range Abacinonyx See Acinonyx Abathomodon See Speothos A
Genus/Species Skull Ht Lt Wt Stage Range Abacinonyx see Acinonyx Abathomodon see Speothos A. fossilis see Icticyon pacivorus? Pleistocene Brazil Abelia U.Miocene Europe Absonodaphoenus see Pseudarctos L.Miocene USA A. bathygenus see Cynelos caroniavorus Acarictis L.Eocene W USA cf. A. ryani Wasatchian Colorado(US) A. ryani Wasatchian Wyoming, Colorado(US) Acinomyx see Acinonyx Acinonyx M.Pliocene-Recent Europe,Asia,Africa,N America A. aicha 2.3 m U.Pliocene Morocco A. brachygnathus Pliocene India A. expectata see Miracinonyx expectatus? Or Felis expectata? A. intermedius M.Pleistocene A. jubatus living Cheetah M.Pliocene-Recent Algeria,Europe,India,China A. pardinensis 91 cm 3 m 60 kg Astian-Biharian Italy,India,China,Germany,France A. sp. L.Pleistocene Tanzania,Ethiopia A. sp. Cf. Inexpectatus Blancan-Irvingtonian California(US) A. studeri see Miracinonyx studeri Blancan Texas(US) A. trumani see Miracinonyx trumani Rancholabrean Wyoming,Nevada(US) Acionyx possibly Acinonyx? A. cf. Crassidens Hadar(Ethiopia) Acrophoca 1.5 m U.Miocene-L.Pliocene Peru,Chile A. longirostris U.Miocene-L.Pliocene Peru A. sp. U.Miocene-L.Pliocene Chile Actiocyon M-U.Miocene W USA A. leardi Clarendonian California(US) A. sp. M.Miocene Oregon(US) Adcrocuta 82 cm 1.5 m U.Miocene Europe,Asia A. advena A. eximia 80 cm 1.5 m Vallesian-Turolian Europe(widespread),Asia(widespread) Adelphailurus U.Miocene-L.Pliocene W USA, Mexico,Europe A. kansensis Hemphillian Arizona,Kansas(US),Chihuahua(Mexico) Adelpharctos M.Oligocene Europe Adilophontes L.Miocene W USA A. brachykolos Arikareean Wyoming(US) Adracodon probably Adracon Eocene France A. quercyi probably Adracon quercyi Eocene France Adracon U.Eocene-L.Oligocene France A. -
~~~~~Present Writer, the Oxyo3na Lutina Skele-
Article XX.-OXYAENA AND PATRIOFELIS RESTUD- IED AS TERRESTRIAL CREODONTS. By HENRY FAIRFIELD OSBORN. PLATES XVIII AND XIX. Comparatively little was known of the skeletal structure of these animals until the American Mus- eum Expeditions of I89I and 1893 secured complete skeletons of each, which Dr. J. L. Wortman carefully described and figured. After a searching comparison with modern land and water Carnivora he con- cluded that Patriofelis was prob- ably aquatic in habit and possibly ancestral to the modern Pinnipedia and that the much older type Fig. I. Dideljhysfvirginiana, left Oxy&ena and the more recent type fore foot. Oxyaznodon, bore similar testimony to affinities with the Seals. In describingPatriofelis he remarked.- "The broad, flat, planti- grade feet with their spreading toes sug- gest at the first glance their use for swim- ming" ('94, p. i6i). -%6 ~~Recently, u n d e r the direction of the ( ~~~~~present writer, the Oxyo3na lutina skele- .............ton has been mounted and the Patriofelis ferox skeleton taken ._...apart and remounted by Mr. Hermann, head preparator. At Fig. 2. Pafriofelisferox, left fore foot, from mounted skeleton. the same time several [269] 270 Bulletin Ame;'ican Museum of Natural History. [Vol. XIII, alterations were made in the restored parts of the skull of Patrio- felis, the teeth were restored, one dorsal vertebra added, and, for reasons stated below, the feet reset in an angulate subdigitigrade instead of a plane plantigrade fashion. A more thorough study of the dentition of this animal was also made from all the mate- rials in the Museum. In this connection a careful restudy of all the evidence led the writer to the opposite conclusion, that these were powerful terres- trial, orpart6y arboreal, animals, analogous to the Cats in habits of feeding, with analogous (not homologous) sectorials, clumsy in limb structure, without prehensile claws, and presenting no evi- dence of successors among the modern Carnivora. -
Mammalia, Carnivora): Appearance of the Eurasian Beardog Ysengrinia in North America Robert M
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Papers in the Earth and Atmospheric Sciences Earth and Atmospheric Sciences, Department of 2002 Intercontinental Migration of Neogene Amphicyonids (Mammalia, Carnivora): Appearance of the Eurasian Beardog Ysengrinia in North America Robert M. Hunt Jr. University of Nebraska-Lincoln, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/geosciencefacpub Part of the Earth Sciences Commons Hunt, Robert M. Jr., "Intercontinental Migration of Neogene Amphicyonids (Mammalia, Carnivora): Appearance of the Eurasian Beardog Ysengrinia in North America" (2002). Papers in the Earth and Atmospheric Sciences. 547. https://digitalcommons.unl.edu/geosciencefacpub/547 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 Papers in the Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK, NY 10024 Number 3384, 53 pp., 24 ®gures, 6 tables December 27, 2002 Intercontinental Migration of Neogene Amphicyonids (Mammalia, Carnivora): Appearance of the Eurasian Beardog Ysengrinia in North America ROBERT M. HUNT, JR.1 CONTENTS Abstract ...................................................................... 2 Introduction .................................................................. -
Newsletter Number 85
The Palaeontology Newsletter Contents 85 Editorial 2 Association Business 3 Association Meetings 16 From our correspondents 28,000 leagues across the sea 20 R for palaeontologists: Introduction 28 Future meetings of other bodies 39 Meeting Reports 46 Obituary Richard Aldridge 66 Sylvester-Bradley reports 69 Publicity Officer: Old Fossils, New Media 82 Book Reviews 85 Books available to review 92 Palaeontology vol 57 parts 1 & 2 93–94 Reminder: The deadline for copy for Issue no 86 is 9th June 2014. On the Web: <http://www.palass.org/> ISSN: 0954-9900 Newsletter 85 2 Editorial The role of Newsletter Reporter is becoming part of the portfolio of responsibilities of the PalAss Publicity Officer, which is Liam Herringshaw’s new post on Council. This reflects a broader re-organization of posts on Council that are aimed at enhancing the efforts of the Association. Council now includes the posts of Education Officer and Outreach Officer, who will, along with the Publicity Officer, develop strategies to engage with different target audiences. The Association has done what it can to stay abreast of developments in social media, through the establishment of the Palass Twitter Feed (@ThePalAss), the development of Palaeontology [online] and the work of Palaeocast, which is a project that has received support from the Association. Progressive Palaeontology has more or less migrated to Facebook. Such methods of delivery have overtaken the Newsletter, the News side-boxes on the Pal Ass website and … However, our real asset in the publicity sphere is you, the members. As palaeontologists, we hold the subject-specific knowledge and the links among the different spheres of knowledge in the other sciences that contribute to our understanding of the history of life. -
How Niche Overlap Between Carnivoramorphans and Creodonts Changed from the Start to the End of the Eocene
Testing the competition hypothesis: How niche overlap between carnivoramorphans and creodonts changed from the start to the end of the Eocene by Brigid Emily Christison A thesis submitted to the Faculty of Graduate and Postdoctoral Affairs in partial fulfillment of the requirements for the degree of Master of Science in Biology Carleton University Ottawa, Ontario 2020 © Brigid Emily Christison Abstract Carnivoramorphans and creodonts are two groups of ancestrally carnivorous mammals that both emerged in the Paleocene (66–56 Ma) of North America. During the Eocene (56–33.9 Ma), carnivoramorphans radiated into some of the taxonomic groups we still see today, while creodont diversity declined until the group went extinct in North America during the Oligocene (33.9–23 Ma) and worldwide during the Miocene (23–5.3 Ma). In this thesis, I test the hypothesis that competition with carnivoramorphans may have led to the extinction of the creodonts in North America by examining changes in niche overlap between the two groups from the start to the end of the Eocene. My results do not support the competition hypothesis, but instead suggest that creodonts were hyperspecialized and un-equipped for the dramatically different environments of the late Eocene and early Oligocene. ii Acknowledgements Land acknowledgement The fossils examined in this study were collected predominantly on Cession 517, 632, and 700 land. These are the territories of the Oglala Sioux Tribe of the Pine Ridge Reservation, Assiniboine and Sioux Tribes of the Fort Peck Indian Reservation,