Ichnotaxonomy of the Eocene Green River Formation

Total Page:16

File Type:pdf, Size:1020Kb

Ichnotaxonomy of the Eocene Green River Formation Ichnotaxonomy of the Eocene Green River Formation, Soldier Summit and Spanish Fork Canyon, Uinta Basin, Utah: Interpreting behaviors, lifestyles, and erecting the Cochlichnus Ichnofacies By © 2018 Joshua D. Hogue B.S. Old Dominion University, 2013 Submitted to the graduate degree program in Geology and the Graduate Faculty of the University of Kansas in partial fulfillment of the requirements for the degree of Master of Science. Chair: Dr. Stephen T. Hasiotis Dr. Paul Selden Dr. Georgios Tsoflias Date Defended: May 1, 2018 ii The thesis committee for Joshua D. Hogue certifies that this is the approved version of the following thesis: Ichnotaxonomy of the Eocene Green River Formation, Soldier Summit and Spanish Fork Canyon, Uinta Basin, Utah: Interpreting behaviors, lifestyles, and erecting the Cochlichnus Ichnofacies Chair: Dr. Stephen T. Hasiotis Date Approved: May 1, 2018 iii ABSTRACT The Eocene Green River Formation in the Uinta Basin, Utah, has a diverse ichnofauna. Nineteen ichnogenera and 26 ichnospecies were identified: Acanthichnus cursorius, Alaripeda lofgreni, c.f. Aquatilavipes isp., Aulichnites (A. parkerensis and A. tsouloufeidos isp. nov.), Aviadactyla (c.f. Av. isp. and Av. vialovi), Avipeda phoenix, Cochlichnus (C. anguineus and C. plegmaeidos isp. nov.), Conichnus conichnus, Fuscinapeda texana, Glaciichnium liebegastensis, Glaroseidosichnus ign. nov. gierlowskii isp. nov., Gruipeda (G. fuenzalidae and G. gryponyx), Midorikawapeda ign. nov. semipalmatus isp. nov., Planolites montanus, Presbyorniformipes feduccii, Protovirgularia dichotoma, Sagittichnus linki, Treptichnus (T. bifurcus, T. pedum, and T. vagans), and Tsalavoutichnus ign. nov. (Ts. ericksonii isp. nov. and Ts. leptomonopati isp. nov.). Four ichnocoenoses are represented by the ichnofossils—Cochlichnus, Conichnus, Presbyorniformipes, and Treptichnus—representing dwelling, feeding, grazing, locomotion, predation, pupation, and resting behaviors of organisms in environments at and around the sediment-water-air interface. A new Cochlichnus Ichnofacies is established to represent continental assemblages of traces produced in environmental conditions at and around the sediment-water-air interface. The Cochlichnus Ichnofacies can be identified in deposits from as old as the Carboniferous. The Cochlichnus Ichnofacies replaces the Shorebird Ichnofacies and usage of the Mermia Ichnofacies for ephemeral water bodies, and restricts the Mermia Ichnofacies to traces in deeper, perennial water bodies. A new ichnospecies of Aulichnites is proposed, A. tsouloufeidos. Three new ichnogenera with four ichnospecies are established: Glaroseidosichnus gierlowskii, Midorikawapeda semipalmatus, and Tsalavoutichnus (Ts. ericksonii, Ts. leptomonopati). This is the first detailed ichnotaxonomic study of the Soldier Summit and Spanish Fork Canyon localities of the Eocene Green River Formation. iv ACKNOWLEDGMENTS Thank you to the Gunther family for their donation of the slabs used in this study to the University of Kansas (KU), without which this research could not have been conducted. Thank you, also, to Mr. Ronald Voelkel for assistance with the German translation of Walter (1985) for the diagnosis of Glaciichnium liebegastensis. Thanks to KU IchnoBioGeoScience (IBGS) Research Group for their assistance in the early stages of the formulating of this manuscript. v TABLE OF CONTENTS ABSTRACT ...................................................................................................................... iii ACKNOWLEDGEMENTS ............................................................................................ iv TABLE OF CONTENTS ..................................................................................................v INTRODUCTION..............................................................................................................1 GEOLOGIC SETTING.....................................................................................................2 BACKGROUND ................................................................................................................3 MATERIALS AND METHODS ......................................................................................5 SYSTEMATIC ICHNOLOGY .........................................................................................7 PLANTS ............................................................................................................................................. 7 RHIZOLITHS ............................................................................................................................ 7 INVERTEBRATES ........................................................................................................................... 9 Ichnogenus ACANTHICHNUS Hitchcock, 1858 ...................................................................... 9 ACANTHICHNUS CURSORIUS (Hitchcock, 1858) ...........................................................10 Ichnogenus AULICHNITES Fenton & Fenton, 1937a .............................................................11 AULICHNITES PARKERENSIS Fenton & Fenton, 1937a ..................................................12 AULICHNITES TSOULOUFEIDOS new ichnospecies .......................................................13 Ichnogenus COCHLICHNUS Hitchcock, 1858 ........................................................................14 COCHLICHNUS ANGUINEUS (Hitchcock, 1858) .............................................................15 COCHLIHCNUS PLEGMAEIDOS new species ..................................................................18 Ichnogenus CONICHNUS (Männil, 1966) ................................................................................20 CONICHNUS CONICHNUS (Männil, 1966) .......................................................................21 Ichnogenus GLACIICHNIUM Walter, 1985............................................................................22 GLACIICHNIUM LIEBEGASTENSIS Walter, 1985 ...........................................................23 Ichnogenus GLAROSEIDOSICHNUS new genus ...................................................................24 GLAROSEIDOSICHNUS GIERLOWSKII new species ......................................................24 Ichnogenus PLANOLITES Nicholson, 1873 .............................................................................25 PLANOLITES MONTANUS (Richter, 1937).......................................................................26 Ichnogenus PROTOVIRGULARIA (McCoy, 1850) ................................................................28 PROTOVIRGULARIA DICHOTOMA (McCoy, 1850) .......................................................28 vi Ichnogenus SAGITTICHNUS Seilacher, 1953 .........................................................................29 SAGITTICHNUS LINCKI Seilacher, 1953 ..........................................................................30 Ichnogenus TREPTICHNUS (Miller, 1889) .............................................................................31 TREPTICHNUS BIFURCUS (Miller, 1889) ........................................................................33 TREPTICHNUS PEDUM (Seilacher, 1955a) .......................................................................34 TREPTICHNUS VAGANS (Ksiażkiewicz, 1977) ................................................................35 VERTEBRATES ..............................................................................................................................36 Ichnogenus ALARIPEDA Sarjeant & Reynolds, 2001 ............................................................36 ALARIPEDA LOFGRENI Sarjeant & Reynolds, 2001 .........................................................37 Ichnogenus AQUATILAVIPES (Currie, 1981) ........................................................................38 c.f. AQUATILAVIPES isp. ..................................................................................................39 Ichnogenus AVIADACTYLA (Kordos, 1985) ..........................................................................39 c.f. AVIADACTYLA isp. .....................................................................................................41 AVIADACTYLA VIALOVI (Kordos in Kordos & Prakfalvi, 1990) ....................................42 Ichnogenus AVIPEDA (Vyalov, 1965) ......................................................................................43 AVIPEDA PHOENIX (Vyalov, 1966) ..................................................................................44 Ichnogenus FUSCINAPEDA (Sarjeant & Langston, 1994) .....................................................46 FUSCINAPEDA TEXANA Sarjeant & Langston, 1994 .......................................................47 Ichnogenus GRUIPEDA (Panin & Avram, 1962) ....................................................................48 GRUIPEDA FUENZALIDAE Covacevich & Lamperein, 1970 ............................................49 GRUIPEDA GRYPONYX (Sarjeant & Reynolds, 2001) ......................................................50 Ichnogenus MIDORIKAWAPEDA new genus ........................................................................52 MIDORIKAWAPEDA SEMIPALMATUS new species .......................................................53 Ichnogenus PRESBYORNIFORMIPES (Yang & others, 1995) .............................................55 PRESBYORNIFORMIPES FEDUCCII Yang & others, 1995 ..............................................56 Ichnogenus TSALAVOUTICHNUS new genus .......................................................................58
Recommended publications
  • Facies Architecture and Stratigraphy of the Paleogene Huntingdon Formation at Abbotsford, British Columbia
    Facies Architecture and Stratigraphy of the Paleogene Huntingdon Formation at Abbotsford, British Columbia Brett Hohs Tallentire Gilley B.Sc., Simon Fraser University, 1999 A THESIS SUBMInED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE In the DEPARTMENT OF EARTH SCIENCES O Brett Hollis Tallentire Gilley, 2003 SIMON FRASER UNIVERSITY December, 2003 All rights reserved. This work may not be reproduced in whole or part, by photocopy or other means, without the permission of the author. APPROVAL Name: Brett Hollis Tallentire Gilley Degree: Master of Science Title of Thesis: Facies Architecture and Stratigraphy of the Paleogene Huntingdon Formation at Abbotsford, British Columbia Examining Committee: Chair: Dr. Glyn Williams-Jones Assistant Professor Dr. Peter Mustard Senior Supervisor Associate Professor Dr. ames MacEachern SupJ rvisory Associate Profess - Fvpf.Michael ~ilhn Ex rnal Examiner Doua4 as Colleae. De~t.of Geolosv & Anthropology Date Approved: ne 4 , 2 csz aw PARTIAL COPYRIGHT LICENCE I hereby grant to Simon Fraser University the right to lend my thesis, project or extended essay (the title of which is shown below) to users of the Simon Fraser University Library, and to make partial or single copies only for such users or in response to a request from the library of any other university, or other educational institution, on its own behalf or for one of its users. I further agree that permission for multiple copying of this work for scholarly purposes may be granted by me or the Dean of Graduate Studies. It is understood that copying or publication of this work for financial gain shall not be allowed without my written permission.
    [Show full text]
  • Proceedings Op the Twenty-Third Annual Meeting Op the Geological Society Op America, Held at Pittsburgh, Pennsylvania, December 21, 28, and 29, 1910
    BULLETIN OF THE GEOLOGICAL SOCIETY OF AMERICA VOL. 22, PP. 1-84, PLS. 1-6 M/SRCH 31, 1911 PROCEEDINGS OP THE TWENTY-THIRD ANNUAL MEETING OP THE GEOLOGICAL SOCIETY OP AMERICA, HELD AT PITTSBURGH, PENNSYLVANIA, DECEMBER 21, 28, AND 29, 1910. Edmund Otis Hovey, Secretary CONTENTS Page Session of Tuesday, December 27............................................................................. 2 Election of Auditing Committee....................................................................... 2 Election of officers................................................................................................ 2 Election of Fellows................................................................................................ 3 Election of Correspondents................................................................................. 3 Memoir of J. C. Ii. Laflamme (with bibliography) ; by John M. Clarke. 4 Memoir of William Harmon Niles; by George H. Barton....................... 8 Memoir of David Pearce Penhallow (with bibliography) ; by Alfred E. Barlow..................................................................................................................... 15 Memoir of William George Tight (with bibliography) ; by J. A. Bownocker.............................................................................................................. 19 Memoir of Robert Parr Whitfield (with bibliography by L. Hussa- kof) ; by John M. Clarke............................................................................... 22 Memoir of Thomas
    [Show full text]
  • 1 Paleobotanical Proxies for Early Eocene Climates and Ecosystems in Northern North 2 America from Mid to High Latitudes 3 4 Christopher K
    https://doi.org/10.5194/cp-2020-32 Preprint. Discussion started: 24 March 2020 c Author(s) 2020. CC BY 4.0 License. 1 Paleobotanical proxies for early Eocene climates and ecosystems in northern North 2 America from mid to high latitudes 3 4 Christopher K. West1, David R. Greenwood2, Tammo Reichgelt3, Alexander J. Lowe4, Janelle M. 5 Vachon2, and James F. Basinger1. 6 1 Dept. of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, 7 Saskatchewan, S7N 5E2, Canada. 8 2 Dept. of Biology, Brandon University, 270-18th Street, Brandon, Manitoba R7A 6A9, Canada. 9 3 Department of Geosciences, University of Connecticut, Beach Hall, 354 Mansfield Rd #207, 10 Storrs, CT 06269, U.S.A. 11 4 Dept. of Biology, University of Washington, Seattle, WA 98195-1800, U.S.A. 12 13 Correspondence to: C.K West ([email protected]) 14 15 Abstract. Early Eocene climates were globally warm, with ice-free conditions at both poles. Early 16 Eocene polar landmasses supported extensive forest ecosystems of a primarily temperate biota, 17 but also with abundant thermophilic elements such as crocodilians, and mesothermic taxodioid 18 conifers and angiosperms. The globally warm early Eocene was punctuated by geologically brief 19 hyperthermals such as the Paleocene-Eocene Thermal Maximum (PETM), culminating in the 20 Early Eocene Climatic Optimum (EECO), during which the range of thermophilic plants such as 21 palms extended into the Arctic. Climate models have struggled to reproduce early Eocene Arctic 22 warm winters and high precipitation, with models invoking a variety of mechanisms, from 23 atmospheric CO2 levels that are unsupported by proxy evidence, to the role of an enhanced 24 hydrological cycle to reproduce winters that experienced no direct solar energy input yet remained 25 wet and above freezing.
    [Show full text]
  • Download File
    Chronology and Faunal Evolution of the Middle Eocene Bridgerian North American Land Mammal “Age”: Achieving High Precision Geochronology Kaori Tsukui Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Graduate School of Arts and Sciences COLUMBIA UNIVERSITY 2016 © 2015 Kaori Tsukui All rights reserved ABSTRACT Chronology and Faunal Evolution of the Middle Eocene Bridgerian North American Land Mammal “Age”: Achieving High Precision Geochronology Kaori Tsukui The age of the Bridgerian/Uintan boundary has been regarded as one of the most important outstanding problems in North American Land Mammal “Age” (NALMA) biochronology. The Bridger Basin in southwestern Wyoming preserves one of the best stratigraphic records of the faunal boundary as well as the preceding Bridgerian NALMA. In this dissertation, I first developed a chronological framework for the Eocene Bridger Formation including the age of the boundary, based on a combination of magnetostratigraphy and U-Pb ID-TIMS geochronology. Within the temporal framework, I attempted at making a regional correlation of the boundary-bearing strata within the western U.S., and also assessed the body size evolution of three representative taxa from the Bridger Basin within the context of Early Eocene Climatic Optimum. Integrating radioisotopic, magnetostratigraphic and astronomical data from the early to middle Eocene, I reviewed various calibration models for the Geological Time Scale and intercalibration of 40Ar/39Ar data among laboratories and against U-Pb data, toward the community goal of achieving a high precision and well integrated Geological Time Scale. In Chapter 2, I present a magnetostratigraphy and U-Pb zircon geochronology of the Bridger Formation from the Bridger Basin in southwestern Wyoming.
    [Show full text]
  • Flamingo ABOUT the GROUP
    Flamingo ABOUT THE GROUP Bulletin of the IUCN-SSC/Wetlands International The Flamingo Specialist Group (FSG) was established in 1978 at Tour du Valat in France, under the leadership of Dr. Alan Johnson, who coordinated the group until 2004 (see profile at www.wetlands.org/networks/Profiles/January.htm). Currently, the group is FLAMINGO SPECIALIST GROUP coordinated from the Wildfowl & Wetlands Trust at Slimbridge, UK, as part of the IUCN- SSC/Wetlands International Waterbird Network. The FSG is a global network of flamingo specialists (both scientists and non- scientists) concerned with the study, monitoring, management and conservation of the world’s six flamingo species populations. Its role is to actively promote flamingo research and conservation worldwide by encouraging information exchange and cooperation amongst these specialists, and with other relevant organisations, particularly IUCN - SSC, Ramsar, WWF International and BirdLife International. FSG members include experts in both in-situ (wild) and ex-situ (captive) flamingo conservation, as well as in fields ranging from field surveys to breeding biology, diseases, tracking movements and data management. There are currently 165 members around the world, from India to Chile, and from France to South Africa. Further information about the FSG, its membership, the membership list serve, or this bulletin can be obtained from Brooks Childress at the address below. Chair Assistant Chair Dr. Brooks Childress Mr. Nigel Jarrett Wildfowl & Wetlands Trust Wildfowl & Wetlands Trust Slimbridge Slimbridge Glos. GL2 7BT, UK Glos. GL2 7BT, UK Tel: +44 (0)1453 860437 Tel: +44 (0)1453 891177 Fax: +44 (0)1453 860437 Fax: +44 (0)1453 890827 [email protected] [email protected] Eastern Hemisphere Chair Western Hemisphere Chair Dr.
    [Show full text]
  • Description of Bird Tracks from the Kitadani Formation (Aptian), Katsuyama, Fukui, Japan with Three-Dimensional Imaging Techniques
    Memoir of the Fukui Prefectural Dinosaur Museum 17: 1–8 (2018) ARTICLE © by the Fukui Prefectural Dinosaur Museum DESCRIPTION OF BIRD TRACKS FROM THE KITADANI FORMATION (APTIAN), KATSUYAMA, FUKUI, JAPAN WITH THREE-DIMENSIONAL IMAGING TECHNIQUES Takuya IMAI 1, 2, Yuta TSUKIJI 3 and Yoichi AZUMA 1,4 1 Fukui Prefectural Dinosaur Museum, 51-11 Terao, Muroko, Katsuyama, Fukui 911-8601, Japan 2 Graduate School of Natural Science and Technology, Kanazawa University, Kakuma, Kanazawa, Ishikawa 920-1192, Japan 3 Department of Earth and Planetary Systems Science, Graduate School of Science, Hiroshima University, 1-3-1 Kagamiyama, Higashihiroshima, Hiroshima 739-8526, Japan 4 Institute of Dinosaur Reseach, Fukui Prefectural University, 4-1-1 Kenjojima, Matsuoka, Eiheiji, Fukui, 910-1195, Japan ABSTRACT The Early Cretaceous ichnofossils of birds numerously occur in South Korea and China. Together with rich skeletal record from northeastern China, they facilitate our understanding about distribution and diversity of birds during the time. In contrast, in Japan, the fossil record of the Early Cretaceous birds is poorly known. Here, we report two ichnotaxa of the Early Cretaceous birds from the Aptian Kitadani Formation. We employ three-dimensional imaging techniques to objectively document and describe the specimens. Specimens include FPDM-F-74 and FPDM-F-75 recovered from an alternating sequence of fine sandstone and mudstone of the Kitadani Formation cropping out in the Kitadani Dinosaur Quarry, Katsuyama, Fukui, Japan. FPDM-F-74 is large in size, bears slender digits with pointy ends (claw impressions), and lacks hallux and webbing traces. These characters allow assignment of FPDM-F-74 to cf.
    [Show full text]
  • Petroleum Resources Assessment 1
    RN23 KR-95(C)-24 #%#o"#(KIGAM Research Report) 5 # Petroleum Resources Assessment ( I ) fix E 5 Korea Institute of Geology, Mining & Material ilSTfUBUTWH If IMS DOCUMENT IS WIMIS FiHta ms mania V KR-95(C)-24 (KIGAM Research Report) W. ffi % (I ) Petroleum Resources Assessment ( I ) Iff fsef Korea Institute of Geology, Mining & Material DISCLAIMER Portions of this document may be illegible in electronic image products. Images are produced from the best available original document. 4 wmw, m ##% ##&, ^c#, ##c, ggm, ...............................###, *#;#, .......................................... im± &### #SS 23^^) ##K ...............................mmm, Mkm, ncm, ^?n .............. 183 Petroleum Resource's Assessment of the Okinawa Trough -3- i) mwm, ##m, g#&, #jR^, ^c#, g#a, 2) ###, ##&, *m#, #?# Petroleum Resources Assessment of the Okinawa Trough n J.H. Oh, Y.H. Kwak, P.Y. Bong, J.D. Son, T.J. Cheong, H.Y. Lee, B.J. Ryu, B.K. Son, I.G. Hwang, Y.I. Kwon, Y.J. Lee, H.J. Kim, S.S. Yi 2)K.S. Park, K.P. Park, C.S. Shin, D. Sunwoo ABSTRACT The hydrocarbon potential has been evaluated for the Tertiary strata in the northwestern margin of the Okinawa Trough on the basis of the paleontological, petrological, geochemical data from two wells (Nikkan 8-1X and JDZ VII-3), and geophysical data. Abundant marine microfossils such as foraminifers, calcareous z nannofossils and dinocysts were yielded in the sedimentary section of the above wells. Abundant palynomorphs originated from nearby onshore are also encountered. Based on nannofossiles, the biostratigraphic zones from NN12 (Amaurolithus tricorniculatus Zone) to NN19 (P seudoemiliania lacunosa Zone) are established. Four foraminiferal zones and four palynomorph assemblages were identified, which can be corresponded to 2) -Nf- Sb) 34 m -5- calcareous nannofossil zones.
    [Show full text]
  • Constraints on the Timescale of Animal Evolutionary History
    Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J.
    [Show full text]
  • A Review of Vertebrate Track-Bearing Formations
    5 Lockley, M.G. & Lucas, S.G., eds., 2014, Fossil footprints of western North America: NMMNHS Bulletin 62 A REVIEW OF VERTEBRATE TRACK-BEARING FORMATIONS FROM THE MESOZOIC AND EARLIEST CENOZOIC OF WESTERN CANADA WITH A DESCRIPTION OF A NEW THEROPOD ICHNOSPECIES AND REASSIGNMENT OF AN AVIAN ICHNOGENUS RICHARD T. MCCREA1, LISA G. BUCKLEY1, A. GUY PLINT2, PHILIP J. CURRIE3, JAMES W. HAGGART4, CHARLES W. HELM1 AND S. GEORGE PEMBERTON5 1Peace Region Palaeontology Research Centre; Box 1540; Tumbler Ridge, British Columbia; V0C 2W0; CANADA; 2Department of Earth Sciences; University of Western Ontario; London, Ontario; N6A 5B7; CANADA; 3Department of Biological Sciences; University of Alberta, Edmonton, Alberta; T6G 2E9; CANADA; 4Geological Survey of Canada; 1500-605 Robson Street; Vancouver, British Columbia; V6B 5J3; CANADA; 5Department of Earth and Atmospheric Sciences; University of Alberta; Edmonton, Alberta; T6G 2E3; CANADA Abstract—The past quarter century has seen a marked increase in the recognition of fossil vertebrate tracksites in western Canada. Most of these finds were made in Alberta and British Columbia, but the Yukon Territory can lay claim to at least one tracksite and probably has the potential to yield more sites. The record of dinosaur tracks with skin impressions has increased dramatically, and is now represented by specimens of ankylosaurs, large ornithopods, small theropods and tyrannosauroids. Notable new finds include the first record of sauropods in Canada, evidence of herding behavior in ankylosaurs and the first pterosaur tracks in Canada. First discoveries of track specimens from several formations in western Canada include the Mountain Park Member of the Gates Formation in Alberta, and the Boulder Creek, Goodrich, Kaskapau, Cardium and Marshybank formations in northeastern British Columbia.
    [Show full text]
  • The First Record of Anomoepus Tracks from the Middle Jurassic of Henan Province, Central China
    Historical Biology An International Journal of Paleobiology ISSN: 0891-2963 (Print) 1029-2381 (Online) Journal homepage: http://www.tandfonline.com/loi/ghbi20 The first record of Anomoepus tracks from the Middle Jurassic of Henan Province, Central China Lida Xing, Nasrollah Abbassi, Martin G. Lockley, Hendrik Klein, Songhai Jia, Richard T. McCrea & W. Scott Persons IV To cite this article: Lida Xing, Nasrollah Abbassi, Martin G. Lockley, Hendrik Klein, Songhai Jia, Richard T. McCrea & W. Scott Persons IV (2016): The first record of Anomoepus tracks from the Middle Jurassic of Henan Province, Central China, Historical Biology, DOI: 10.1080/08912963.2016.1149480 To link to this article: http://dx.doi.org/10.1080/08912963.2016.1149480 Published online: 22 Feb 2016. Submit your article to this journal View related articles View Crossmark data Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=ghbi20 Download by: [Lida Xing] Date: 22 February 2016, At: 05:53 HISTORICAL BIOLOGY, 2016 http://dx.doi.org/10.1080/08912963.2016.1149480 The first record of Anomoepus tracks from the Middle Jurassic of Henan Province, Central China Lida Xinga, Nasrollah Abbassib, Martin G. Lockleyc, Hendrik Kleind, Songhai Jiae, Richard T. McCreaf and W. Scott PersonsIVg aSchool of the Earth Sciences and Resources, China University of Geosciences, Beijing, China; bFaculty of Sciences, Department of Geology, University of Zanjan, Zanjan, Iran; cDinosaur Tracks Museum, University of Colorado Denver, Denver, CO, USA; dSaurierwelt Paläontologisches Museum, Neumarkt, Germany; eHenan Geological Museum, Henan Province, China; fPeace Region Palaeontology Research Centre, British Columbia, Canada; gDepartment of Biological Sciences, University of Alberta, Edmonton, Canada ABSTRACT ARTICLE HISTORY Small, gracile mostly tridactyl tracks from the Middle Jurassic of Henan Province represent the first example Received 30 December 2015 of the ichnogenus Anomoepus from this region.
    [Show full text]
  • The First Possible Choristoderan Trackway from the Lower
    www.nature.com/scientificreports OPEN The frst possible choristoderan trackway from the Lower Cretaceous Daegu Formation of South Korea and its implications on choristoderan locomotion Yuong‑Nam Lee1*, Dal‑Yong Kong2 & Seung‑Ho Jung2 Here we report a new quadrupedal trackway found in the Lower Cretaceous Daegu Formation (Albian) in the vicinity of Ulsan Metropolitan City, South Korea, in 2018. A total of nine manus‑pes imprints show a strong heteropodous quadrupedal trackway (length ratio is 1:3.36). Both manus and pes tracks are pentadactyl with claw marks. The manus prints rotate distinctly outward while the pes prints are nearly parallel to the direction of travel. The functional axis in manus and pes imprints suggests that the trackmaker moved along the medial side during the stroke progressions (entaxonic), indicating weight support on the inner side of the limbs. There is an indication of webbing between the pedal digits. These new tracks are assigned to Novapes ulsanensis, n. ichnogen., n. ichnosp., which are well‑matched not only with foot skeletons and body size of Monjurosuchus but also the fossil record of choristoderes in East Asia, thereby N. ulsanensis could be made by a monjurosuchid‑like choristoderan and represent the frst possible choristoderan trackway from Asia. N. ulsanensis also suggests that semi‑aquatic choristoderans were capable of walking semi‑erect when moving on the ground with a similar locomotion pattern to that of crocodilians on land. South Korea has become globally famous for various tetrapod footprints from Cretaceous strata1, among which some clades such as frogs2, birds3 and mammals4 have been proved for their existences only with ichnological evidence.
    [Show full text]
  • Pterosaur Distribution in Time and Space: an Atlas 61
    Zitteliana An International Journal of Palaeontology and Geobiology Series B/Reihe B Abhandlungen der Bayerischen Staatssammlung für Pa lä on to lo gie und Geologie B28 DAVID W. E. HONE & ERIC BUFFETAUT (Eds) Flugsaurier: pterosaur papers in honour of Peter Wellnhofer CONTENTS/INHALT Dedication 3 PETER WELLNHOFER A short history of pterosaur research 7 KEVIN PADIAN Were pterosaur ancestors bipedal or quadrupedal?: Morphometric, functional, and phylogenetic considerations 21 DAVID W. E. HONE & MICHAEL J. BENTON Contrasting supertree and total-evidence methods: the origin of the pterosaurs 35 PAUL M. BARRETT, RICHARD J. BUTLER, NICHOLAS P. EDWARDS & ANDREW R. MILNER Pterosaur distribution in time and space: an atlas 61 LORNA STEEL The palaeohistology of pterosaur bone: an overview 109 S. CHRISTOPHER BENNETT Morphological evolution of the wing of pterosaurs: myology and function 127 MARK P. WITTON A new approach to determining pterosaur body mass and its implications for pterosaur fl ight 143 MICHAEL B. HABIB Comparative evidence for quadrupedal launch in pterosaurs 159 ROSS A. ELGIN, CARLOS A. GRAU, COLIN PALMER, DAVID W. E. HONE, DOUGLAS GREENWELL & MICHAEL J. BENTON Aerodynamic characters of the cranial crest in Pteranodon 167 DAVID M. MARTILL & MARK P. WITTON Catastrophic failure in a pterosaur skull from the Cretaceous Santana Formation of Brazil 175 MARTIN LOCKLEY, JERALD D. HARRIS & LAURA MITCHELL A global overview of pterosaur ichnology: tracksite distribution in space and time 185 DAVID M. UNWIN & D. CHARLES DEEMING Pterosaur eggshell structure and its implications for pterosaur reproductive biology 199 DAVID M. MARTILL, MARK P. WITTON & ANDREW GALE Possible azhdarchoid pterosaur remains from the Coniacian (Late Cretaceous) of England 209 TAISSA RODRIGUES & ALEXANDER W.
    [Show full text]