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Mammal Footprints from the Miocene-Pliocene Ogallala

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Mammalfootprints from the Miocene-Pliocene Ogallala Formation, easternNew Mexico by ThomasE. Williamsonand SpencerG. Lucas, New Mexico Museum of Natural History and Science,1801 Mountain Road NW Albuquerque, New Mexico 87104-7375 Abstract well-develooed mudcracks. The track- ways are diveloped on the mudstone Mammal trackways preserved in the drape but are preserved as infillings at the Miocene-Pliocene Ogallala Formation of base of the overlying conglomerate (Figs. eastern New Mexico represent the first 2-4). Most tracks are preserved on the report of mammal fossils-from this unit in underside of a single, thick conglomerate New Mexico. These trackwavs are Dre- block (Fig. 3). A few isolated mammal served as infillings in a conglomerate near the base of the Ogallala Formation. At least prints were also observed on the under- four mammalian ichnotaxa are represented, side of adjacent blocks.he depth of the including a single trackway of a large camel infillings suggest that tracks were made in (Gambapessp. A), several prints of an uncer- a relatively soft substrate. Some prints are tain family of artiodactyl (Gambapessp B), a accompanied by marks indicating slip- single trackway of a large feloid carnivoran page on a slick, wet substrate (Fig. 5C). (Bestiopeda sp.), and several indistinct im- Infillings of mudcracks and narrow, cylin- pressions, probably representing more than drical burrows and raindrop impressions one trackway of a small canid carnivoran are Dreserved over some areas of the (Chelipus sp ). The footprints are preserved in a channel-margin facies of an Ogallala tracliway slab. Mammal trackways repre- braided stream. sent at least four ichnotaxa. Introduction Description and identif ication In eastern New Mexico, the Ogallala Bestiopeila sp. Formation is composed of alluvial, eolian, 10O km and lacustrine deposits of Miocene to A single trackway referred to Bestiopeda early Pliocene age, about 124Ma (Fig. 1; sp. parallels the trackway of Gambapessp. FIGURE 1-Map showing trackway location Hawley, 1984). In the Texas Panhandle, A described below (Figs. 4,5A). We follow (NMMNH locality L-3096) Tiackway locality is Ogallala Group strata produce the mam- Sarjeant and Langston (1994) rn restricting in the Pliocene Ogallala Formation, San Juan malian fossil assemblages characteristic of Bestiopeda to carnivoran footprints that Mesa, Chavez County, eastern New Mexico. the Clarendonian and Hemphillian land- lack claw impressions. Bestiopedaare gen- Ogallala Formation and correlative deposits mammal "ages" of late Miocene-early erally ascribed to feloids, which normally (Santa Fe Group) are shaded (modified from Hawley, 1984). Pliocene age (Wood el a1.,1941;Tedford et walk with claws retracted or held above a1.,1987).However, no fossil mammals are the ground. These tracks also exhibit other known from the Ogallala Formation in characteristics distinctive of modern cats, New Mexico. Here we report mammal such as plantar pads that have two lobes footprints from the Ogallala Formation, on the front (Halfpenny and Biesiot, 1986) Alsoin this issue the first documentation of fossil mammals and prints that have breadth greater than Ramah Memberof the Crevasse = from the unit in New Mexico. their length (manus length 55 mm; Formation-a new stratigraphic = = breadth 57 mm; digit II length 2l mnl.; unitin theZuni Basin p.6 Locality and stratigraphy III length = 27 mm; IV length = 23 mm;Y length = 22mm). 1996NMGS News p.13 The trackway locality (NMMNH L- OliverLee MemorialState Park p. 14 3096, UTM Zone-13 3756410N 603114E)is Chelipus sp. 1995NM MineralSymposium on the west flank of San Juan Mesa, abstracts p.18 Chavez County, New Mexico. The Several prints possibly representing sev- ServiceiNews p.22 Ogallala Formation consists of 2L m of eral trackways of small, digitigrade foot- conglomerate, sandstone, and caliche (Fig. prints with four digits (II to V) are referred GeographicNames p.23 2). tackways from NMMNH locality L- lo Chelipus sp. (Figs. 4, 58) (overall length = UpcomingMeetings p.23 3095 are found abCve a 3S-cm-thick, lentic- 35 mm; breadth =32mm; digit II length = ular, sandstone and mudstone lens in the 10 mm; III length = 20 mm; IV length = 20 Gomingsoon basal conglomerate of the Ogallala mm; V length = 15 mm). Digital pads are Formation. The lower 25 cm of this lens ovoid and of equal or similar size. Prints Copper in New Mexico consists of a planar-bedded sandstone. are very shallow and indistinct. Manus The upper 10 cm is a mudstone drape with and pes prints probably overlap. No defi- MEASURED STRATIGRAPH IC SECTION LEGEND % s.,,"6" cro*oeire W FIGURE 2-Measured stratigraphic section and lithologic description of Ogallala Formation at trackway locality, sec 22 T4S M9E, San Juan Mesa, coneto New Mexico. ffi "r.r" Effi phn.rb"d" llffiil..*",o* Fl s;6e1on" E_- New Nztexreo localityL-3096 GEOLOGY . Scienceand Service tssN o196-948X Volume 18, No. 1, February 1996 Editor: Carol A Hjellning EDITORIAL BOARD Steve M Cather, NMBMMR, Chairman Thomas Giordano, NMStl Laurel B Goodwin, NMIMT Spencer G Lucas, NM&INHS FrankJ Pazzaglia,UNM Ogaliala Formation Thickness Published quarterly by (m) New Mexico Bureau of Mines and Mineral Resources 5 Caliche; white (N9) weathers pinkish gray a division of New Mexico Institute of Mining and Technology (5 YR 8/1); forms extensive caprock over San Mesa. BOARD OF REGENTS Juan Ex-Officio 4 Conglomerate; Iight brown (5 YR 6/4);poorly Gary Johnsorl Gooernor of New Muico sorted; crudelybedded with some crossbeds; Alan Morgan, Superintendentof Publi Instruction subarkosic; quartzite, sandstone, chert and Appointed Michael Kelly, Pres, 7992-1997,Roswell gneiss clasts; clasts imbricated; J subrounded; Steve S Torres, Secfheas ,\99"1-1997, Albuquerque calcareous. 4.0 Diane D Denish, 7992-7997,Albuquerque 3 Sandstone; light brown (5yR6/4); moderately Delilah A Yega, Studtnt Member , 1995-7997 , Socorro Charles A Zinnerly, 1991-7997, sorted; fine- to coarse-grained; subangular; Socolro calcareous; subarkosic; slope-forming. New Mexico Institute of Mining and Technology President. Daniel H. L6pez 2 Conglomerate; Iight brown (5 YR 6/4); poorly New Mexico Bureau of Mines and Mineral Resources sorted; crudely bedded with some crossbeds; Director 6nd StateGeologist Charles E Chapin subarkosic; quartzite, sandstone, chert and Subscriptions: Issued quarterly, February, gneiss clasts; clasts imbricated; subrounded; May, August, November; subscription price $5 00,/calen- calcareous; fines upward over last 1 m. Track- dar year ways are found abbve 3S-cm-thick, lenticular, Editorial Matter: Articles submitted for publication sandstone and mudstone lens Lower 25 cm should be in the editor's hmds a minimum of five (5) consist of planar-bedded sandstone. Upper 10 months before date of publication (February, May, August, or November) and should be no cm consist of mudstone with well-developed longer than 20 typewdttery double-spaced pages. mudcracks. Trackwavs are developed on All scientific papers will be reviewed by at least two mudstone and preseived as infillings at baseof people in the appropriate field of study. Address inquiries overlying conglomerate. to Carol A Hjellming, Editor of Nm Conglomeratic blocks Mexico Ceology,New Mexico Bureau of Mines and preserving trackways are slumped. 70 Mineral Resources, Socorro, New Mexico 87801- Unconformity 4796 Chinle Group (Upper Triassic) Publishedas public domain, thereforereprorlucible without permission 1 Siltstone and mudstone; light brown (5 YR 5/a); Sourcecredil requested Circulation: "1,000 calcareous. Upper 0 5 m is greenish not measured Printer: Urivercity of New Mexico Printing Services February 1996 New Mexlco Ceology FIGURE 3-Exposures of Ogallala Formation on the west side of San Juan Mesa, eastern New Mexico. Trackways occur in the conglomeratic slump blocks near the base of the Ogallala Formation (see arrow). Note two people to the left of blocks for scale. nite claw impressions are preserved. However, prints have a single lobe on the front of the plantar pad as is seen in mod- ern canid tracks (Halfpenny and Biesiot, 1986) and are longer than wide, indicating that they were not made by a feloid. Gambaltes sp. A A single trackway is referred to Gam- bapessp. A (Figs. 4, 5C). The prints are rel- atively large (overall length = 146 mm; maximum width = 132 mm), didactyl, and symmetrical. The hoofprints of digits III and IV are separated by a continuous interdigital space, and each taper to a pointed apex. At least two of the prints (manus and pes) are followed by marks indicating slippage on the substrate (Fig. 5C). The hoofprints themselves are convex rather than flat, indicating that a fleshy pad was present. Each print is relatively broad with a maximum breadth greater than 35% of its length (Sarjeant and Langston, 1994). They are therefore confi- dently referred to Gambapes. The maxi- FIGURE4-Map of trackway, traced from underside of conglomeraticblock. tacks are preservedas mum breadth of hoofprints of the pes is infillings: l, Gambapessp. A; 2, Bestiopedasp; 3, Gambapessp. B; 4, Chelipussp. Shading indicates area about 50% of its length (medial hoofprint beyond block. length = 146 mm; maximum breadtlt = 72 mm). The prints referred to Gambapessp. A differ from Pecoripeda (sensu Sarjeant The ichnogenus Ceraipedaas emended Gambapessp.Acanconfidentlybereferred and Langston, 1994) in having shorter by Sarjeant and Langston (1994) is intend- to a large camel because of their large size hooves and from Cercipeda (sensu Saqeant ed to embrace didactyl artiodactyl foot- and indications that a fleshy, spreading and Langston, 1994) in lacking dewclaw prints made by cameloids, traguloids, cer- hoof pad similar to that seen in living lmDresslons. voids, and bovoids. The tracks we refer to camels was present. New Mexico Geology February 1996 FIGURE S-Selected prints fromOgallala Formation trackway. A, Left pes (right) and manus (left) prints ol Bestiopedasp. Note mudcrack infillings. Manus length is 55 mm. B, manus? and pes? pfrnts of Chelipus sp. showing-possible overlap of pes on-manus. Note sinuo'us invertebrate trace andraindrop impressions. C, Manus (left) and pes (right) prints of Gambapessp.
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    Origin and Evolution of the Sierra Nevada themed issue Oligocene and Miocene arc volcanism in northeastern California: Evidence for post­Eocene segmentation of the subducting Farallon plate Joseph P. Colgan1,*, Anne E. Egger2, David A. John1, Brian Cousens3, Robert J. Fleck1, and Christopher D. Henry4 1U.S. Geological Survey, 345 Middlefield Road, Mail Stop 973, Menlo Park, California 94025, USA 2Geological and Environmental Sciences, Stanford University, 450 Serra Mall, Stanford, California 94305, USA 3Carleton University, 1125 Colonel By Drive, Ottawa, Ontario, Canada K1S5B6 4Nevada Bureau of Mines and Geology, University of Nevada, Reno, Nevada 89557, USA ABSTRACT sitionally similar to Oligocene rocks in the Unlike the western Cascades, however, vol­ Warner Range. They are distinctly different canic rocks of the ancestral Cascades are a subset The Warner Range in northeastern Cali- from younger (Late Miocene to Pliocene) of a diverse and widespread suite of Cenozoic fornia exposes a section of Tertiary rocks over high-Al, low-K olivine tholeiites, which are volcanic rocks erupted across the Basin and 3 km thick, offering a unique opportunity to more mafic (46%–49% SiO2), did not build Range Province since the Eocene. The ancestral study the long-term history of Cascade arc large edifices, and are thought to be related Cascades samples plotted in Figure 1 are those volcanism in an area otherwise covered by to backarc extension. The Warner Range is considered by du Bray et al. (2009) to be plausi­ younger volcanic rocks. The oldest locally
  • Eocene, Oligocene, and Miocene Rocks and \Fertebrate Fossils at the Emerald Lake Locality, 3 Miles South of Ifellowstone National Park,Wyoming

    Eocene, Oligocene, and Miocene Rocks and \Fertebrate Fossils at the Emerald Lake Locality, 3 Miles South of Ifellowstone National Park,Wyoming

    Eocene, Oligocene, and Miocene Rocks and \fertebrate Fossils at the Emerald Lake Locality, 3 Miles South of Ifellowstone National Park,Wyoming GEOLOGICAL SURVEY PROFESSIONAL PAPER 932-A Prepared in cooperation with the Geological Survey of Wyoming, the Department of Geology of the University of Wyoming, the American Museum of Natural History, and the Carnegie Museum Eocene, Oligocene, and Miocene Rocks and \fertebrate Fossils at the Emerald Lake Locality 3 Miles South of Ifellowstone National Park,Wyoming By J. D. LOVE, MALCOLM C. McKENNA, and MARY R. DAWSON GEOLOGY OF THE TETON-JACKSON HOLE REGION, NORTHWESTERN WYOMING GEOLOGICAL SURVEY PROFESSIONAL PAPER 932-A Prepared in cooperation with the Geological Survey of Wyoming, the Department of Geology of the University of Wyoming, the American Museum of Natural History, and the Carnegie Museum UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1976 UNITED STATES DEPARTMENT OF THE INTERIOR THOMAS S. KLEPPE, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Love, John David, 1913- Eocene, Oligocene, and Miocene rocks and vertebrate fossils at the Emerald Lake locality, 3 miles south of Yellowstone National Park, Wyoming. (Geology of the Teton-Jackson Hole region, northwestern Wyoming) (Geological Survey Professional Paper 932-A) Bibliography: p. Includes index. 1. Geology, Stratigraphic Tertiary. 2. Vertebrates, Fossil. 3. Geology Wyoming Teton Co. I. McKenna, Malcolm C., joint author. II. Dawson, Mary R., joint author. III. Wyoming Geological Survey. IV. Title: Eocene, Oligocene, and Miocene rocks and vertebrate fossils at the Emerald Lake locality ... V. Series. VI. Series: United States Geological Survey Professional Paper 932-A. QE691.L79 551.?'8 76-8159 For sale by the Superintendent of Documents, U.S.