DOCSLIB.ORG

UTRECHT MICROPALEONTOLOGICAL Bulletins

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
UTRECHT MICROPALEONTOLOGICAL Bulletins UTRECHT MICROPALEONTOLOGICAL BUllETINS SPECIAL PUBLICATION RODENTS FROM THE MIDDLE OLIGOCENE OF TURKISH 5 THRACE Editor C. W. Drooger Department of Stratigraphy and Paleontology State University of Utrecht Budapestlaan 4, Postbus 80.021 3508 TA Utrecht, Netherlands Sales office U.M.B.: Budapestlaan 4, 3584 CD Utrecht, Netherlands Postal account: 30 28 890, T. van Schaik, Leusden Bank account: 55 89 855, Algemene Bank Nederland, T. van Schaik, Leusden > After prepayment to the sales office on one of the above accounts, the books will be sent by surface mail without further charges. Orders for these books not directly from the purchaser to the sales office may cause much higher costs to the purchaser. Bull. 1. T. FREUDENTHAL - Stratigraphy of Neogene deposits in the Khania Pro- vince, Crete, with special reference to foraminifera of the family Planor- bulinidae and the genus Heterostegina. 208 p., 15 pI., 33 figs. (1969) f 32,- Bull. 2. J.E. MEULENKAMP - Stratigraphy of Neogene deposits in the Rethymnon Province, Crete, with special reference to the phylogeny of uniserial Uvigerina from the Mediterranean region. 172 p., 6 pI., 53 figs. (1969) f 29,- Bull. 3. J. G. VERDENIUS - Neogene stratigraphy of the Western Guadalquivir basin, S. Spain. 109 p., 9 pI., 12 figs. (1970) f 28,- Bull. 4. R. C. TJALSMA - Stratigraphy and foraminifera of the Neogene of the Eastern Guadalquivir basin, S. Spain. 161 p., 16 pI., 28 figs. (1971) f 44,- Bull. 5. C. W. DROOGER, P. MARKS, A. PAPP et al. - Smaller radiate Nummulites of northwestern Europe. 137 p., 5 pI., 50 figs. (1971) f 37,- Bull. 6. W. SISSINGH - Late Cenozoic Ostracoda of the South Aegan Island arc. 187 p., 12 pI., 44 figs. (1972) f 57,- Bull. 7. author's edition. F. M. GRAD STEIN - Mediterranean Pliocene Globorotalia, a biometrical approach. 128 p., 8 pI., 44 figs. (1974) f 39,- Bull. 8. J. A. BROEKMAN - Sedimentation and paleoecology of Pliocene lagoonal- shallow marine deposits on the island of Rhodos (Greece). 148 p., 7 pI., 9 figs. (1974) f 47,- Bull. 9. D. S. N. RAJU - Study of Indian Miogypsinidae. 148 p., 8 pI., 39 figs. (1974) f 38,- Bull. 10. W. A. VAN WAMEL - Conodont biostratigraphy of the Upper Cambrian and Lower Ordovician of north-western (Hand, south-eastern Sweden. 128 p., 8 pI., 25 figs. (1974) f 40,- Bull. 11.W. J. ZACHARIASSE - Planktonic foraminiferal biostratigraphy of the Late Neogene of Crete (Greece). 171 p., 17 pI., 23 figs. (1975) f 52,- Bull. 12. J. T. VAN GORSEL-Evolutionary trends and stratigraphic significance of the Late Cretaceous Helicorbitoides-Lepidorbitoideslineage. 100p., 15pI., 14 figs. (1975) f 37,- Bull. 13. E. F. J. DE MULDER - Microfauna and sedimentary-tectonic history of the Oligo-Miocene of the Ionian Islands and western Epirus (Greece). 140 p., 4 pI., 47 figs. (1975) f 45,- Bull. 14. R. T. E. SCHUTTENHELM - History and modes of Miocene carbonate deposition in the interior of the Piedmont Basin, NW Italy. 208 p., 5 pI., 54 figs. (1976) f 56,- RODENTS FROM THE MIDDLE OLIGOCENE OF TURKISH THRACE ENGIN UNAY-BAYRAKTAR 'As elsewhere. extreme splitters and specialists without a broad vista of classification raise each of the sub­ families and many of the tribes or smaller groups of this classification (of the Cricetidae) to family rank, a procedure that is not necessarily wrong but is disproportionate and is not generally adopted' G.G. Simpson, 1945 The principles of classification and a classification of mammals. p. 206 To Tuncer Printed in the Netherlands by Loonzetterij Abe. Hoogeveen and OMI-GB, Utrecht April 20, 1989 CONTENTS page Abstract 5 Chapter 1 Introduction 7 General introductory remarks 7 Geological setting 9 Review of literature on fossil mammals from the Lignite-Sandstone Formation 10 Rodent localities in the Lignite-Sandstone Formation 13 Absolute age determinations 14 Acknowledgements 14 Chapter 2 Taxonomy 17 Muroidea 17 Remarks on the classification of the European Paleogene Muroidea 17 Melissiodontidae Schaub, 1925 19 Paracricetodontinae Mein and Freudenthal, 1971 19 Paracricetodon Schaub, 1925 19 Trakymys n. gen. 29 Melissiodontinae Schaub, 1925 33 Edirnella n. gen. 34 Pseudocricetodontidae Engesser, 1987 38 Pseudocricetodontinae Engesser, 1987 38 Pseudocricetodon Thaler, 1969 39 Lignitella n. subgen. 47 Adelomyarioninae n. subfam. 48 Kerosinia n. gen. 49 Eucricetodontidae n. fam. 56 Eucricetodontinae Mein and Freudenthal, 1971 56 Eucricetodon Thaler, 1966 57 Heterocricetodontidae n. fam. 60 Heterocricetodon Schaub, 1925 60 Geomyoidea 61 Eomyidae Deperet and Douxami, 1902 61 Eomys Schlosser, 1884 61 Gliroidea 70 Gliridae Thomas, 1897 70 Bransatoglis Hugueney, 1967 71 Glis Brisson, 1762 76 3 Theridomyoidea 82 Pseudosciuridae Zittel, 1893 82 Suevosciurus Dehm, 1937 82 Castoroidea 84 Castoridae Gray, 1821 84 Steneofiber Geoffrey, 1833 84 Sciuroidea 85 Petauristidae Miller, 1912 85 Ctenodactyloidea 86 Ctenodactyloidea indet. 86 Chapter 3 Biostratigraphy, chronostratigraphy and paleoecology 89 References 95 4 ABSTRACT Associations of Middle Oligocene rodent teeth are described from five localities in the Lignite-Sandstone Formation of the Ergene basin. The Muroidea are the most abundant as well as the most diverse group in these associations. In rodent faunas of Western Europe the Theridomyoidea dominate. So far representatives of the Theridomyidae have not been found in Thrace and do not seem to have reached Turkey. In addition to seven new (sub)species four new (sub)genera of the Muroidea are defined: Trakymys, Edirnella, Lignite!!a and Kerosinia. The classification of the European Paleogene representatives of this superfamily is discussed and revised. It is concluded that raising a number of taxonomic entities within the Muroidea to a higher rank in the hierachy is in better accordance with our pre­ sent knowledge of the group than the widely followed classification of Mein and Freudenthal (1971), who include all Tertiary hamsters in one family: the Cricetidae. In addition to Muroidea the rodent associations from Thrace contain teeth of members of the families Eomyidae, Gliridae, Pseudosciuridae, Castoridae and Petauristidae in limited numbers. New species of each of the genera Eomys, Bransatoglis and Glis are described. The faunal details suggest that the five localities correspond to successive levels during an Oligocene time span of approximately one My. Two major zones are apparent but there seem to be possibilities to make a further (sub)zonal subdivision. Our faunas are correlated with part of the MP 23-27 in­ terval of the European standard zonation. The large numbers of Melissiodon­ tidae and Anthracotheriidae suggest vegetated wetland biotopes throughout the investigated interval. 5 N t MOUNTAIN RANCE ROAD RIVER "'­ BORDER NORTH ANATOLIA I I 8 16 24 km Fig. J. Map of western Turkey showing the position of the area studied and of geographical names men­ tioned in the text. Chapter 1 INTRODUCTION GENERAL INTRODUCTORY REMARKS In the course of the 'Tertiary of Southern Thrace' project of the scientific research department of the Mineral Research and Exploration Institute of Turkey (M.T.A.) (1978-1981) the Oligocene deposits in the Karasati syncline in the southern part of the Ergene basin (fig. 2) were prospected for vertebrate re­ mains. Although the Ergene basin was outside the actual study area of the pro­ ject, and therefore not mapped in detail, it seemed of interest to try and establish a more detailed biozonation for the economically important Lignite­ Sandstone Formation (Perejas, 1939) than had been done so far (Ozansoy, 1962, 1964, 1966, Lebkiichner, 1974). A.J. van der Meulen and H. de Bruijn (pers. comm.) had recently found small mammals in the dump from a closed lignite quarry in the same formation near Kyprinos (Greece, fig. 1). This study aims at filling a gap in our knowledge of the Oligocene rodents of southeastern Europe. The insectivores which occur associated with the rodents will not be dealt with in this paper. Information about the geology of the area (e.g. fig. 2) is derived almost ex­ clusively from the literature (Kopp et al. 1969; Lebkiichner, 1974; ~enol, 1980 and others), and is reproduced without criticism. The rodent teeth described below were collected by wet-screening material from the five fossiliferous localities. The mesh of the finest sieve used is 0.5 mm. Because of induration of the claystone it was necessary in some cases to soak the sediment in kerosine prior to washing. The approximate weight of the matrix washed from the various localities was: 2200 kg for Kocayarma, 1900 kg for Kavakdere, 1000 kg for Karacali, 900 kg for Haskoy, and 900 kg for Papkoy. The residues obtained after washing were sorted using a Leitz microscope. The measurements of the rodent cheek teeth are maximum lengths measured in the direction of the tooth row and maximum widths at right angles to the length. All measurements were taken using an ocular micrometer (50 micron units). All values are given in 0.1 mm units. Estimates of the relative abundance of the various taxa in each association are based on the number of complete, or almost complete, Mlml and M/m2. We used a Student's t-test to evaluate differences between the calculated means of length andlor width of a particular tooth when comparing the material from different localities. A five per cent level of significance was 7 00 LEGEND --_/.~:::_---:_-_. 'vtu hacp Format 101" Lignite Seams (Interpretedl Lignite Sana stone Formation Kocayarma Conglomerate Alluvial Depos,ls ~L Roaos o Mammal Localities '0 Fig. 2. Geological map of the Karasati syncline (after Lebkiichner (1974)). The lignite seams [-VI of Lebkiicher are indicated by a-f. chosen and confidence intervals of ninety five per cent are given in the tables. The terminology used for parts of cheek teeth is essentially after Mein and Freudenthal (1971) for the Muroidea, after Fahlbusch (1970) for the Eomyidae and after de Bruijn (1967) for the Gliridae.
Load more

Recommended publications
  • Biostratigraphy and Paleoecology of Continental Tertiary Vertebrate Faunas in the Lower Rhine Embayment (NW-Germany)
    Netherlands Journal of Geosciences / Geologie en Mijnbouw 81 (2): 177-183 (2002) Biostratigraphy and paleoecology of continental Tertiary vertebrate faunas in the Lower Rhine Embayment (NW-Germany) Th. Mors Naturhistoriska Riksmuseet/Swedish Museum of Natural History, Department of Palaeozoology, P.O. Box 50007, SE-104 05 Stockholm, Sweden; e-mail: [email protected] Manuscript received: October 2000; accepted: January 2002 ^ Abstract This paper discusses the faunal content, the mammal biostratigraphy, and the environmental ecology of three important con­ tinental Tertiary vertebrate faunas from the Lower Rhine Embayment. The sites investigated are Rott (MP 30, Late Oligocene), Hambach 6C (MN 5, Middle Miocene), Frechen and Hambach 11 (both MN 16, Late Pliocene). Comparative analysis of the entire faunas shows the assemblages to exhibit many conformities in their general composition, presumably re­ sulting from their preference for wet lowlands. It appears that very similar environmental conditions for vertebrates reoc- curred during at least 20 Ma although the sites are located in a tectonically active region with high subsidence rates. Differ­ ences in the faunal composition are partly due to local differences in the depositional environment of the sites: lake deposits at the margin of the embayment (Rott), coal swamp and estuarine conditions in the centre of the embayment (Hambach 6C), and flood plain environments with small rivulets (Frechen and Hambach 1 l).The composition of the faunal assemblages (di­ versity and taxonomy) also documents faunal turnovers with extinctions and immigrations (Oligocene/Miocene and post- Middle Miocene), as a result of changing climate conditions. Additional vertebrate faunal data were retrieved from two new assemblages collected from younger strata at the Hambach mine (Hambach 11C and 14).
    [Show full text]
  • Rodents of Middle Miocene Localities of Lazarevac Village and Bele Vode (Central Serbia)
    Bulletin of the Natural History Museum, 2008, 1. 79 Bulletin of the Natural History Museum, 2008, 1: 79-98. uDc: 569.32:551.782.1(497.11) RODENTS OF MIDDLE MIOCENE LOCALITIES OF LAZAREVAC VILLAGE AND BELE VODE (CENTRAL SERBIA) Zo r a n Ma r k o v i ć Natural History Museum, Njegoševa 51, 11000 Belgrade, Serbia E-mail: [email protected] The dental remains of rodents from two localities - Lazarevac village and Bele Vode in Central Serbia - are used to determine the age of the sediments and to reconstruct the paleoecology of the habitat. The species recorded at Lazarevac village are Spermophilinus bredai, Miopetaurista dehmi, Cricetodon meini, Megacricetodon minor, Democricetodon mutilus and Miodyromys aegercii; species from Bele Vode are Cricetodon meini, Democricetodon mutilus and Miodyromys aegercii. The rodents’ assemblages can be placed in MN6. Key words: Rodentia, MN6, Central Serbia INTRODUCTION Early in the year 2001, the Natural History Museum in Belgrade was notified of the discovery of fossil bones of a large mammal within the area of Lazarevac village, situated northeast of Trstenik. The team of geologists from the Museum immediately visited the site where the owner of the plot had discovered the remains while he was excavating sand needed for the cultivation of fruit tree saplings. After a preliminary 80 Ma r k o v i ć , Z. – Rodents of middle miocene from Central Serbia check it was obvious that the bones are from a proboscidean mammal. The complete identification was performed after the animal was excavated by Marković et al. (2004a) and it showed that this specimen belonged to Deinotherium giganteum.
    [Show full text]
  • ABSTRACTS BOOK Proof 03
    1st – 15th December ! 1st International Meeting of Early-stage Researchers in Paleontology / XIV Encuentro de Jóvenes Investigadores en Paleontología st (1December IMERP 1-stXIV-15th EJIP), 2018 BOOK OF ABSTRACTS Palaeontology in the virtual era 4 1st – 15th December ! Ist Palaeontological Virtual Congress. Book of abstracts. Palaeontology in a virtual era. From an original idea of Vicente D. Crespo. Published by Vicente D. Crespo, Esther Manzanares, Rafael Marquina-Blasco, Maite Suñer, José Luis Herráiz, Arturo Gamonal, Fernando Antonio M. Arnal, Humberto G. Ferrón, Francesc Gascó and Carlos Martínez-Pérez. Layout: Maite Suñer. Conference logo: Hugo Salais. ISBN: 978-84-09-07386-3 5 1st – 15th December ! Palaeontology in the virtual era BOOK OF ABSTRACTS 6 4 PRESENTATION The 1st Palaeontological Virtual Congress (1st PVC) is just the natural consequence of the evolution of our surrounding world, with the emergence of new technologies that allow a wide range of communication possibilities. Within this context, the 1st PVC represents the frst attempt in palaeontology to take advantage of these new possibilites being the frst international palaeontology congress developed in a virtual environment. This online congress is pioneer in palaeontology, offering an exclusively virtual-developed environment to researchers all around the globe. The simplicity of this new format, giving international projection to the palaeontological research carried out by groups with limited economic resources (expensive registration fees, travel, accomodation and maintenance expenses), is one of our main achievements. This new format combines the benefts of traditional meetings (i.e., providing a forum for discussion, including guest lectures, feld trips or the production of an abstract book) with the advantages of the online platforms, which allow to reach a high number of researchers along the world, promoting the participation of palaeontologists from developing countries.
    [Show full text]
  • The Small Mammals from Gratkorn: an Overview
    Palaeobio Palaeoenv (2014) 94:135–162 DOI 10.1007/s12549-013-0147-3 ORIGINAL PAPER The small mammals from Gratkorn: an overview Jérôme Prieto & Chiara Angelone & Isaac Casanovas-Vilar & Martin Gross & Janós Hír & Lars W.van den Hoek Ostende & Lutz Christian Maul & Davit Vasilyan Received: 14 November 2013 /Revised: 10 December 2013 /Accepted: 16 December 2013 /Published online: 26 February 2014 # Senckenberg Gesellschaft für Naturforschung and Springer-Verlag Berlin Heidelberg 2014 Abstract The rich and diverse fossil mammalian assemblage accumulation by nocturnal raptors. In addition to the informa- from Gratkorn (Middle Miocene, Austria) is of primary im- tion provided by the lower vertebrates and the molluscs, portance for the understanding of the faunal evolution in which occur in abundance in the same thin fossil-enriched Central Europe. Besides large mammals, the fauna comprises: layer, the mammal fauna gives a mixed picture of the envi- Schizogalerix voesendorfensis, Galericinae gen. et sp. indet., ronment (basically forested vs. open landscape). This could Desmanodon fluegeli, Dinosorex sp., cf. Myotis sp., indicate the presence of different microhabitats around the “Cricetodon” fandli, Megacricetodon minutus, Eumyarion excavation place, but may also be a taphonomical artefact sp., Spermophilinus bredai, Blackia sp., Forsythia gaudryi, based on various different agents of accumulation contribut- Albanensia albanensis, Muscardinus aff. sansaniensis, ing to the thanatocoenosis. Nevertheless, the extreme quick Miodyromys sp., Keramidomys sp., Euroxenomys minutus accumulation of the fossils provides an exceptional windows minutus, Prolagus oeningensis, cf. Eurolagus fontannesi and in the late Sarmatian s. str. ecosystems. Ochotonidae indet. Based on the degree of corrosion on the dental elements and the presence of pellets, most, but not all, Keywords Miocene .
    [Show full text]
  • Towards Computational Techniques for Identifying Candidate Chronofaunas
    Ann. Zool. Fennici 51: 43–48 ISSN 0003-455X (print), ISSN 1797-2450 (online) Helsinki 7 April 2014 © Finnish Zoological and Botanical Publishing Board 2014 Towards computational techniques for identifying candidate chronofaunas Ella Bingham1 & Heikki Mannila2 1) Helsinki Institute for Information Technology HIIT, Aalto University, P.O. Box 15600, FI-00076 Aalto, Finland (corresponding author’s e-mail: [email protected]) 2) Department of Computer and Information Science, Aalto University, P.O. Box 15400, FI-00076 Aalto, Finland Received 2 Oct. 2013, final version received 4 Dec. 2013, accepted 9 Dec. 2013 Bingham, E. & Mannila, H. 2014: Towards computational techniques for identifying candidate chronofaunas. — Ann. Zool. Fennici 51: 43–48. A chronofauna is a geographically restricted collection of interacting animal popula- tions that maintains its base structure over a long period of time. We describe a simple computational method that can identify candidate chronofaunas on the basis of pres- ence-absence matrices only: A candidate chronofauna is a collection of sites that share an exceptionally large number of taxa with the defining site of the chronofauna. We show examples of candidate chronofaunas in the NOW data (see http://www.helsinki. fi/science/now). Introduction populations. These characteristics are not directly observable from the basis of presence-absence The concept of chronofauna was defined by data only. Olson (1952) as “a geographically restricted, However, some aspects of the concept are natural assemblage of interacting animal popu- computational and can be identified on the basis lations that has maintained its base structure of presence-absence matrices. In this paper, we over a geologically significant period of time”.
    [Show full text]
  • 6 Workshop on the Neogene
    NEOGENE OF THE PARATETHYAN REGION 6TH WORKSHOP ON THE NEOGENE OF CENTRAL AND SOUTH-EASTERN EUROPE AN RCMNS INTERIM COLLOQUIUM PROGRAMME page 45. ABSTRACTS page 10101. FIELD TRIP GUIDEBOOK page 102124. 31 MAY - 3 JUNE 2015, ORFŰ, HUNGARY Fig. 0.1 Simplified geological map with field stops (map modified from Gyalog (2013)) NEOGENE OF THE PARATETHYAN REGION 6TH WORKSHOP ON THE NEOGENE OF CENTRAL AND SOUTH-EASTERN EUROPE an RCMNS Interim Colloquium Programme Abstracts Field Trip Guidebook 31 May - 3 June 2015, Orfű, Hungary NEOGENE OF THE PARATETHYAN REGION 6 W N C S‐E E an RCMNS Interim Colloquium 31 May ‐ 3 June 2015, Orfű, Hungary PROGRAMME, ABSTRACTS AND FIELD TRIP GUIDEBOOK Organizing Commiee Imre M (MOL Hungarian Oil and Gas Plc. / MTA‐MTM‐ELTE Research Group for Paleontology, Budapest) Ágnes K (Hungarian Geological Society) Orsolya S (Eötvös Loránd University, Budapest) Kriszna S (University of Pécs) Gábor C (Geological and Geophysical Instute of Hungary, Budapest) Alfréd D (Hungarian Natural History Museum, Budapest) György L (University of Miskolc) Ildikó S (Geological and Geophysical Instute of Hungary, Budapest) Emőke T (Eötvös Loránd University, Budapest) Klára P (Geological and Geophysical Instute of Hungary, Budapest) Katalin B (Eötvös Loránd University, Budapest) Lilla T (Eötvös Loránd University, Budapest) Editors István‐Róbert B Ágnes K Imre M Kriszna S Published by Hungarian Geological Society H‐1015 Budapest, Csalogány u. 12. [email protected]‐online.hu www.foldtan.hu Budapest 2015 ISBN 978‐963‐8221‐57‐5 Cover photo: Uppermost part of the Pannonian calcareous marls and their transion to the overlying –sll Pannonian–coarse sands at Pécs‐Danitzpuszta.
    [Show full text]
  • New Data on the Miocene Stem Lagomorph Eurolagus Fontannesi, and Its Northernmost Record
    New data on the Miocene stem lagomorph Eurolagus fontannesi, and its northernmost record ŁUCJA FOSTOWICZ−FRELIK, ADAM NADACHOWSKI, and MAGDALENA KOWALEWSKA−GROSZKOWSKA Fostowicz−Frelik, Ł., Nadachowski, A., and Kowalewska−Groszkowska, M. 2012. New data on the Miocene stem lagomorph Eurolagus fontannesi, and its northernmost record. Acta Palaeontologica Polonica 57 (1): 1–20. We describe new dental material of Eurolagus fontannesi from the Late Miocene (Early Vallesian, MN 9) lignite beds of Bełchatów A (central Poland), which is the northernmost occurrence of this lagomorph. This material considerably in− creases the sample size of this rare genus and species. We review the systematic position of Eurolagus and argue that it is not an ochotonid, but represents a terminal taxon of an independently evolved stem lineage of Lagomorpha. The enamel of the molars, here studied for the first time, exhibits a relatively thin decussating external and a radial internal layer, and in general resembles the palaeolagine lagomorphs (Palaeolagus) rather than the archaeolagine leporids (Hypolagus)or advanced ochotonids (Ochotona). The dental wear features of Eurolagus fontannesi indicate that the species was a sylvan mixed−feeder. This agrees with the Bełchatów A paleoenvironment, which is best approximated as the kind of mixed mesophytic forest now encountered in the Caucasus, Iran, and India. The extinction of Eurolagus was probably related to the noticeable faunal change following the increased cooling of the European climate during the Late Miocene. The first indicator of this event can be observed in Bełchatów A, marked by the immigration of Microtocricetus and the absence of Neocometes. Key words: Lagomorpha, Eurolagus, microwear, paleoecology, semihypsodonty, Vallesian, Bełchatów, Poland.
    [Show full text]
  • Download Vol. 20, No. 3
    BULLETIN of the FLORIDA STATE MUSEUM Biological Sciences Volume 20 1976 Number 3 LATEST PLIOCENE MAMMALS FROM HAILE XV A, ALACHUA COUNTY, FLORIDA JESSE S. ROBERTSON 0 e UNIVERSITY OF FLORIDA GAINESVILLE Numbers of the BULLETIN OF THE FLORIDA STATE MUSEUM, BIOLOGICAL SCIENCES, are published at irregular intervals. Volumes contain about 300 pages and are not necessarily completed in any one calendar year. CARTER R, GEBERT, Editor RHODA J. RYBAK, Managing Editor Consultants for this issue: CLAYTON E. RAY S. DAVID WEBB Communications concerning purchase or exchange of the publications and all manu- scripts should be addressed to the Managing Editor of the Bulletin, Florida State Museum, Museum Road, University of Florida, Gainesville, Florida 32611. This public document was promulgated at an annual cost of $2824.29 or $2.824 per copy. It makes available to libraries, scholars, and all interested persons the results of researches in the natural sciences, emphasizing the Circum-Caribbean region. Publication date: July 7, 1976 Price: $2.85 LATEST PLIOCENE MAMMALS FROM HAILE XV A, ALACHUA COUNTY, FLORIDA JESSE S. ROBERTSON, JR.1 SYNOPSIS: The mammalian fauna of Haile XV A is the first known from the Gulf Coastal Plain during Blancan ( Latest Pliocene) time. The mammals are repre- sented by 8 orders, 17 families, and 18 genera, of which two are new species and three are new to North America. Kraglievichia, a giant, extinct armadillo previously known only from Late Miocene and Pliocene deposits of South America, is reported for the first time in North America and a new species is described. A brief review of the subfamily Chlamytheriinae suggests that Plaina Castellanos is a synonym of Krag- lievichia Castellanos and that Holistetteria Castellanos is a synonym of Pampatherium Ameghino.
    [Show full text]
  • The Squirrels from the Ribesalbes-Alcora Basin (East of Spain)
    Diggers, gliders and runners: The squirrels from the Ribesalbes-Alcora Basin (East of Spain) Vicente D. crespo, AnA FAgoAgA, FrAncisco J. ruiz-sánchez & plini MontoyA The Campisano Ravine in the Ribesalbes­Alcora Basin (Spain, early Miocene, biozone C, MN 4) yielded a relatively diverse assemblage of squirrels, composed by the ground squirrels Heteroxerus rubricati, Atlantoxerus blacki and Aragoxerus sp. the marmotines Palaeosciurus cf. sutteri, Spermophilinus sp., Marmotini indet. and the flying squirrel Aliveria cf. luteyni. Heteroxerus rubricati, Atlantoxerus blacki and Spermophilinus are typical early Miocene species from the Iberian Peninsula, and in this work we increase the knowledge of the variability of them. In MN4, the genus Aragoxerus is reported for the first time in the Iberian Peninsula, and, apart from France, it is its only record in Europe. We report here the first record of the species Palaeosciurus cf. sutteri in the Iberian Peninsula, and one of the oldest in Europe. The occurrence of Aliveria cf. luteyni marks the first record of the genus Aliveria in Western Europe. Additionally, the palaeoecological significance of this assemblage is discussed. • Key words: Sciuridae, Miocene, Aragonian, Iberian Peninsula, paleoecology, biostratigraphy. CRESPO, V.D., FAGOAGA, A., RUIZ-SÁNCHEZ, F.J. & MONTOYA, P. 2021. Diggers, gliders and runners: The squirrels from the Ribesalbes­Alcora Basin (East of Spain). Bulletin of Geosciences 96(1), 83–97 (3 figures, 2 tables). Czech Geological Survey, Prague. ISSN 1214­1119. Manuscript received June 7, 2020; accepted in revised form November 16, 2020; published online December 6, 2020; issued January 10, 2021. Vicente D. Crespo, Consejo Nacional de Investigaciones Científicas y Técnicas, División de Paleontología de Vertebrados, Museo de La Plata (UNLP), Paseo del Bosque s/n, B1900FWA La Plata, Argentina & Museo Paleontológico de Alpuente, Av.
    [Show full text]
  • Oldest Skeleton of a Fossil Flying Squirrel Casts New Light on The
    RESEARCH ARTICLE Oldest skeleton of a fossil flying squirrel casts new light on the phylogeny of the group Isaac Casanovas-Vilar1*, Joan Garcia-Porta2, Josep Fortuny1,3,O´ scar Sanisidro4, Je´ roˆ me Prieto5,6, Marina Querejeta7, Sergio Lla´ cer1, Josep M Robles1, Federico Bernardini8,9, David M Alba1 1Institut Catala` de Paleontologia Miquel Crusafont, Universitat Auto`noma de Barcelona, Barcelona, Spain; 2Centre de Recerca Ecolo`gica i Aplicacions Forestals, Universitat Auto`noma de Barcelona, Barcelona, Spain; 3Centre de Recherches sur les Pale´oenvironnements et la Pale´obiodiversite´, Muse´um national d’Histoire naturelle, Paris, France; 4Biodiversity Institute, University of Kansas, Lawrence, United States; 5Department fu¨ r Geo- und Umweltwissenschaften, Pala¨ ontologie, Ludwig-Maximilians-Universita¨ t Mu¨ nchen, Munich, Germany; 6Bayerische Staatssammlung fu¨ r Pala¨ ontologie und Geologie, Munich, Germany; 7Bavarian State Collection of Zoology, Munich, Germany; 8Centro Fermi, Museo Storico della Fisica e Centro Studi e Ricerche Enrico Fermi, Roma, Italy; 9Multidisciplinary Laboratory, The ‘Abdus Salam’ International Centre for Theoretical Physics, Trieste, Italy Abstract Flying squirrels are the only group of gliding mammals with a remarkable diversity and wide geographical range. However, their evolutionary story is not well known. Thus far, identification of extinct flying squirrels has been exclusively based on dental features, which, contrary to certain postcranial characters, are not unique to them. Therefore, fossils attributed to this clade may indeed belong to other squirrel groups. Here we report the oldest fossil skeleton of a flying squirrel (11.6 Ma) that displays the gliding-related diagnostic features shared by extant forms and allows for a recalibration of the divergence time between tree and flying squirrels.
    [Show full text]
  • The Great American Biotic Interchange in Florida
    Bull. Fla. Mus. Nat. Hist. (2005) 45(4): 271-311 271 THE GREAT AMERICAN BIOTIC INTERCHANGE IN FLORIDA Gary S. Morgan1 Late Neogene vertebrate faunas from Florida provide the most complete record of South American mammals and birds that arrived in temperate North America during the Great American Biotic Interchange (GABI). The first major pulse of the GABI began in the early Hemphillian (late Miocene, ~9 Ma), defined in part on the first appearance of two sloths of South American origin, the megalonychid Pliometanastes and the mylodontid Thinobadistes. The type localities of Pliometanastes protistus (McGehee Farm) and Thinobadistes segnis (Mixson’s Bone Bed) are both earliest Hemphillian (8-9 Ma) sites from northern Florida. Pliometanastes evidently gave rise to Megalonyx in the late Hemphillian. The latest Hemphillian (~5 Ma) Palmetto Fauna documents the earliest occurrence of Megalonyx in Florida. The second major pulse of the GABI occurred during the late Pliocene and early Pleistocene, from 2.7 to1.5 Ma. The late Blancan is defined by the first appearance in temperate North America of a diverse assemblage of vertebrates from South America, including ten genera, all of which occur in Florida during the late Blancan: the giant flightless bird Titanis, the glyptodont Glyptotherium, the armadillos Dasypus and Pachyarmatherium, the pampathere Holmesina, the mylodontid Glossotherium, the megatheriid Eremotherium, the porcupine Erethizon, and the capy- baras Hydrochaeris and Neochoerus. During the late Blancan, Titanis, Dasypus, Pachyarmatherium, Holmesina, Eremotherium, and Hydrochaeris are primarily restricted to Florida, whereas Glyptotherium, Glossotherium, Erethizon, and Neochoerus are more widespread, occurring in Florida as well as the western United States.
    [Show full text]
  • Rodentia: Mammalia) of Cave
    THE SCIURIDAE (RODENTIA: MAMMALIA) OF CAVE BASIN (OREGON), A NEW MIDDLE MIOCENE MICROFOSSIL LOCALITY by EVA MARIE BIEDRON A THESIS Presented to the Department of Geological Sciences and the Robert D. Clark Honors College in partial fulfillment of the requirements for the degree of Bachelor of Science July 2016 An Abstract of the Thesis of Eva Marie Biedron for the degree of Bachelor of Sciences in the Department of Geological Sciences to be taken July 2016 Title: The Sciuridae (Rodentia: Mammalia) of Cave Basin (Oregon), a new Middle Miocene microfossil locality Approv004;-~ Dr. Samantha S. B. Hopkins Cave Basin is a Mid-Miocene vertebrate fossil site located on the South Fork of the Crooked River, near Paulina in Central Oregon. In this basin, the Mascall Formation is composed of tuffs, paleosols, diatomites, fluvial and lacustrine sediments, producing floral, macrofaunal, and microfaunal vertebrate fossils. I describe seven genera of squirrels from the Cave Basin fauna, including a new latest Hemingfordian boundary species of Miospermophilus and the first record of Miopetaurista in the Miocene of North America. The sediments and diverse community of terrestrial, arboreal, and semi­ fossorial squirrels found at Cave Basin indicate an environment supporting woodland, marginal forest, and non-forest environments around a body/bodies of water with non­ permanent boundaries. The Cave Basin assemblage provides a window into the diversity of local environments and mammalian communities present during the Mid­ Miocene Climatic Optimum. Additionally, the Cave Basin sciurid assemblage is one of the most diverse in Oregon and highlights the range of micromammal niches available in mixed environments.
    [Show full text]