A Tribute to Burkart Engesser
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The Record of Deinotheriidae from the Miocene of the Swiss Jura Mountains (Jura Canton, Switzerland)
bioRxiv preprint doi: https://doi.org/10.1101/2020.08.10.244061. this version posted August 10, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. It is made available under a CC-BY 4.0 International license. The record of Deinotheriidae from the Miocene of the Swiss Jura Mountains (Jura Canton, Switzerland) 1 Gagliardi Fanny, 2, 3 Maridet Olivier & 2, 3 Becker Damien 1 Biology, University of Neuchâtel, CH-2000 Neuchâtel, Switzerland; [email protected] 2 Jurassica Museum, Route de Fontenais 21, CH-2900 Porrentruy, Switzerland; [email protected], [email protected] [corresponding authors] 3 Earth Sciences, University of Fribourg, Chemin du Musée 6, CH-1900 Fribourg, Switzerland Abstract: The Miocene sands of the Swiss Jura Mountains, long exploited in quarries for the construction industry, have yielded abundant fossil remains of large mammals. Among Deinotheriidae (Proboscidea), two species, Prodeinotherium bavaricum and Deinotherium giganteum, had previously been identified in the Delémont valley, but never described. A third species, Deinotherium levius, from the locality of Charmoille in Ajoie, is reported herein for the first time in Switzerland. These occurrences are dated from the late early to the early late Miocene, correlating to the European Mammal biozones MN4 to MN9. The study is completed by a discussion on the palaeobiogeography of dinotheres at European scale. Key words: Prodeinotherium, Deinotherium, Bois de Raube formation, Miocene, Jura, Switzerland. Introduction The order of Proboscidea currently regroups large mammals whose common characteristic is the possession of a trunk and tusks. Within the Afrotherians superorder, it has for sister group the Sirenia order (dugongs and manatees). -
LETTER Doi:10.1038/Nature14423
LETTER doi:10.1038/nature14423 A bizarre Jurassic maniraptoran theropod with preserved evidence of membranous wings Xing Xu1,2*, Xiaoting Zheng1,3*, Corwin Sullivan2, Xiaoli Wang1, Lida Xing4, Yan Wang1, Xiaomei Zhang3, Jingmai K. O’Connor2, Fucheng Zhang2 & Yanhong Pan5 The wings of birds and their closest theropod relatives share a ratios are 1.16 and 1.08, respectively, compared to 0.96 and 0.78 in uniform fundamental architecture, with pinnate flight feathers Epidendrosaurus and 0.79 and 0.66 in Epidexipteryx), an extremely as the key component1–3. Here we report a new scansoriopterygid short humeral deltopectoral crest, and a long rod-like bone articu- theropod, Yi qi gen. et sp. nov., based on a new specimen from the lating with the wrist. Middle–Upper Jurassic period Tiaojishan Formation of Hebei Key osteological features are as follows. STM 31-2 (Fig. 1) is inferred Province, China4. Yi is nested phylogenetically among winged ther- to be an adult on the basis of the closed neurocentral sutures of the opods but has large stiff filamentous feathers of an unusual type on visible vertebrae, although this is not a universal criterion for maturity both the forelimb and hindlimb. However, the filamentous feath- across archosaurian taxa12. Its body mass is estimated to be approxi- ers of Yi resemble pinnate feathers in bearing morphologically mately 380 g, using an empirical equation13. diverse melanosomes5. Most surprisingly, Yi has a long rod-like The skull and mandible are similar to those of other scansoriopter- bone extending from each wrist, and patches of membranous tissue ygids, and to a lesser degree to those of oviraptorosaurs and some basal preserved between the rod-like bones and the manual digits. -
Oligocene and Early Miocene Mammal Biostratigraphy of the Valley of Lakes in Mongolia
Palaeobio Palaeoenv (2017) 97:219–231 DOI 10.1007/s12549-016-0264-x ORIGINAL PAPER Oligocene and early Miocene mammal biostratigraphy of the Valley of Lakes in Mongolia Mathias Harzhauser1 & Gudrun Daxner-Höck1 & Margarita A. Erbajeva2 & Paloma López-Guerrero1,3 & Olivier Maridet4,5 & Adriana Oliver 1,6 & Werner E. Piller7 & Ursula B. Göhlich1 & Reinhard Ziegler8 Received: 13 July 2016 /Revised: 28 October 2016 /Accepted: 10 November 2016 /Published online: 15 December 2016 # The Author(s) 2017. This article is published with open access at Springerlink.com Abstract The Taatsiin Gol Basin in Mongolia is a key area for data. Therefore, we test and evaluate the informal biozonation understanding the evolution and dispersal of Central Asian scheme that has been traditionally used for biostratigraphic mammal faunas during the Oligocene and early Miocene. correlations within the basin. Based on the analysis of the huge After two decades of intense fieldwork, the area is extraordi- dataset, a formalised biostratigraphic scheme is proposed. It narily well sampled and taxonomically well studied, yielding a comprises the Cricetops dormitor Taxon Range Zone large dataset of 19,042 specimens from 60 samples. The spec- (Rupelian), subdivided into the Allosminthus khandae Taxon imens represent 176 species-level and 99 genus-level taxa com- Range Subzone and the Huangomys frequens Abundance prising 135 small mammal species and 47 large mammals. A Subzone, the Amphechinus taatsiingolensis Abundance Zone detailed lithostratigraphy and new magnetostratigraphic and (early Chattian), the Amphechinus major Taxon Range Zone radiometric datings provide an excellent frame for these biotic (late Chattian), subdivided into the Yindirtemys deflexus This article is a contribution to the special issue BThe Valley of Lakes in Mongolia, a key area of Cenozoic mammal evolution and stratigraphy^. -
Geodiversitas 2019 ● 41 ● 9 Directeur De La Publication : Bruno David, Président Du Muséum National D’Histoire Naturelle
geodiversitas 2019 ● 41 ● 9 DIRECTEUR DE LA PUBLICATION : Bruno David, Président du Muséum national d’Histoire naturelle RÉDACTEUR EN CHEF / EDITOR-IN-CHIEF : Didier Merle ASSISTANTS DE RÉDACTION / ASSISTANT EDITORS : Emmanuel Côtez ([email protected]) MISE EN PAGE / PAGE LAYOUT : Emmanuel Côtez COMITÉ SCIENTIFIQUE / SCIENTIFIC BOARD : Christine Argot (MNHN, Paris) Beatrix Azanza (Museo Nacional de Ciencias Naturales, Madrid) Raymond L. Bernor (Howard University, Washington DC) Alain Blieck (chercheur CNRS retraité, Haubourdin) Henning Blom (Uppsala University) Jean Broutin (UPMC, Paris) Gaël Clément (MNHN, Paris) Ted Daeschler (Academy of Natural Sciences, Philadelphie) Bruno David (MNHN, Paris) Gregory D. Edgecombe (The Natural History Museum, Londres) Ursula Göhlich (Natural History Museum Vienna) Jin Meng (American Museum of Natural History, New York) Brigitte Meyer-Berthaud (CIRAD, Montpellier) Zhu Min (Chinese Academy of Sciences, Pékin) Isabelle Rouget (UPMC, Paris) Sevket Sen (MNHN, Paris) Stanislav Štamberg (Museum of Eastern Bohemia, Hradec Králové) Paul Taylor (The Natural History Museum, Londres) COUVERTURE / COVER : Left specimen: Hebertides jurassica Guinot, De Angeli & Garassino, 2007, in dorsal view; Right specimen: Xantho cf. moldavicus (Yanakevich, 1977), in outer lateral view; Background: Panoramic view of the Museum quarry ‘la carrière-musée’ (Channay-sur-Lathan). Geodiversitas est indexé dans / Geodiversitas is indexed in: – Science Citation Index Expanded (SciSearch®) – ISI Alerting Services® – Current Contents® / Physical, -
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 . -
Up-To-Date Spanish Continental Neogene Synthesis and Paleoclimatic Interpretation
Up-to-date Spanish continental Neogene synthesis and paleoclimatic interpretation 1 2 2 4 J. P. CALV0 , R. DAAMS , J. MORALES , N. LOPEZ-MARTINEZ3, 1. AGUSTI , 6 6 6 P. ANADONS, 1. ARMENTEROS , L. CABRERN, J. CIVIS , A. CORROCHAN0 , 2 IO M. DIAZ- MOLINN, E. ELIZAGN, M. HOYOS , E. MARTIN-SUAREZ , J. MARTINEZ", I2 13 13 E. MOISSENET , A. MUNOZ , A. PEREZ-GARCIA , A. PEREZ-GONZALEZ'\ I6 I6 J. M. PORTER01S, F.ROBLES , C. SANTISTEBAN , 17 IO I9 T. TORRES , A. J. VAN DER MEULEN 18, J. A. VERA AND P. MEIN I Dpto Petrolog{a, Fac.GeoI6gicas, Univ.Complutense. 28040 MADRID. 2 Museo Nacional Ciencias Naturales, CSIC. Jose Gutierrez Abascal, 2. 28006 MADRID. 3Dpto Paleontolog{a, Fac.GeoI6gicas, Univ.Complutense. 28040 MADRID. 4Institut Paleontologia "M. Crusafont". 08201 Sabadell, BARCELONA. 5Inst. "Jaume Almera ", CSIC. Mart{ i Franques sin. 08028 BARCELONA. 6Dpto Geolog{a, Fac.Ciencias, Univ.Salamanca. 37008 SALAMANCA. 7 Dpto Geolog{a Dindmica, Fac.Geolog{a, Univ.Barcelona. 08028 BARCELONA. 8 Dpto Estratigrafla, Fac.GeoI6gicas, Univ.Complutense. 28040 MADRID. 9ITGE. Plaza del Temple, 1. 46003 VALENCIA. 10 Dpto Geolog{a, Fac.Ciencias, Univ.Granada. 18071 GRANADA. 11 EGEO. Gaztambide, 61. 28015 MADRID. 12 1 rue Voltaire. 75011 PARIS. 13 Dpto Geolog{a, Fac.Ciencias, Univ.Zaragoza. 50009 ZARAGOZA. 14 Centro de Ciencias Medioambientales, CSIC. Serrano, 115. 28006 MADRID. 15 Compaii{a General de Sondeos (CGS). San Roque, 3. Majadahonda, MADRID. 16 Dpto Geolog{a, Fac.BioI6gicas, Univ. Valencia. Dr.Moliner sin, Burjassot, VALENCIA. 17 Esc.Tecn.Sup.Ingenieros de Minas. R{os Rosas, 21. 28003 MADRID. 18 Inst. v.Aarwetenschappen. -
The Eomyidae in Asia: Biogeography, Diversity and Dispersals
FOSSIL IMPRINT • vol. 76 • 2020 • no. 1 • pp. 181–200 (formerly ACTA MUSEI NATIONALIS PRAGAE, Series B – Historia Naturalis) THE EOMYIDAE IN ASIA: BIOGEOGRAPHY, DIVERSITY AND DISPERSALS YURI KIMURA1,2,*, ISAAC CASANOVAS-VILAR2, OLIVIER MARIDET3,4, DANIELA C. KALTHOFF5, THOMAS MÖRS6, YUKIMITSU TOMIDA1 1 Department of Geology and Paleontology, National Museum of Nature and Science, 4-1-1 Amakubo, Tsukuba, Ibaraki, 305-0005, Japan; e-mail: [email protected]. 2 Institut Català de Paleontologia Miquel Crusafont, ICTA-ICP. Edifici Z. Carrer de les Columnes, s/n., Campus de la Universitat Autònoma de Barcelona, E-08193 Cerdanyola del Vallès, Barcelona, Spain. 3 JURASSICA Museum, Route de Fontenais 21, CH-2900 Porrentruy, Switzerland. 4 Département des Géosciences, Université de Fribourg, Chemin du Musée 6, CH-1700 Fribourg, Switzerland. 5 Department of Zoology, Swedish Museum of Natural History, P.O. Box 50007, SE-104 05 Stockholm, Sweden. 6 Department of Palaeobiology, Swedish Museum of Natural History, P.O. Box 50007, SE-104 05 Stockholm, Sweden. * corresponding author Kimura, Y., Casanovas-Vilar, I., Maridet, O., Kalthoff, D. C., Mörs, T., Tomida, Y. (2019): The Eomyidae in Asia: Biogeography, diversity and dispersals. – Fossil Imprint, 76(1): 181–200, Praha. ISSN 2533-4050 (print), ISSN 2533-4069 (on-line). Abstract: In Asia, the first find of an eomyid rodent was reported almost one century after the first studies of the family Eomyidae in North America and Europe. Since then, eomyid rodents have been increasingly found in Asia particularly over the past two decades. Here, we review the Asian record of this family at the genus level. -
The Mammalian Assemblage of Mazan (Vaucluse, France) and Its Position in the Early Oligocene European Palaeobiogeography
Swiss J Geosci (2013) 106:231–252 DOI 10.1007/s00015-013-0145-5 The mammalian assemblage of Mazan (Vaucluse, France) and its position in the Early Oligocene European palaeobiogeography Olivier Maridet • Marguerite Hugueney • Loı¨c Costeur Received: 4 December 2012 / Accepted: 12 August 2013 / Published online: 16 November 2013 Ó Swiss Geological Society 2013 Abstract The locality of Mazan (Provence, South-Eastern other Early Oligocene localities allows deciphering the France) yielded numerous remains of vertebrates, including European mammalian palaeobiogeography at the beginning numerous isolated teeth and a few bone fragments of of the Oligocene. The mammalian assemblage of Mazan mammals. A preliminary faunal list was published by Triat shows significant affinities with other localities from Wes- et al; the present systematic revision of the mammalian tern Europe (especially French and Spanish localities), remains and the description of new specimens reveal that while localities from the eastern part of Europe (Anatolian, the assemblage comprises 18 taxa belonging to 7 orders and Bavarian and Bohemian localities) are noticeably different, 10 families. Among the mammalian remains, the therid- even though these were not subjected to strong palaeobio- omyids and cricetids are the two most abundant groups. geographic differentiation nor endemism. The locality of This revision confirms the ascription of the locality to the Paguera 1 (Majorca)–possibly already insular in the Early biochronological unit MP21, which corresponds to the very Oligocene–shows peculiar affinities with Anatolian and beginning of the Oligocene. As this locality overlies the Bavarian localities rather than with those in Western Late Eocene faunas of Mormoiron, it clearly illustrates the European. -
Oligocene and Early Miocene Mammal Biostratigraphy of the Valley of Lakes in Mongolia
Published in "Palaeobiodiversity and Palaeoenvironments 97(1): 219–231, 2017" which should be cited to refer to this work. Oligocene and early Miocene mammal biostratigraphy of the Valley of Lakes in Mongolia Mathias Harzhauser1 & Gudrun Daxner-Höck1 & Margarita A. Erbajeva2 & Paloma López-Guerrero1,3 & Olivier Maridet4,5 & Adriana Oliver 1,6 & Werner E. Piller7 & Ursula B. Göhlich1 & Reinhard Ziegler8 Abstract The Taatsiin Gol Basin in Mongolia is a key area for data. Therefore, we test and evaluate the informal biozonation understanding the evolution and dispersal of Central Asian scheme that has been traditionally used for biostratigraphic mammal faunas during the Oligocene and early Miocene. correlations within the basin. Based on the analysis of the huge After two decades of intense fieldwork, the area is extraordi- dataset, a formalised biostratigraphic scheme is proposed. It narily well sampled and taxonomically well studied, yielding a comprises the Cricetops dormitor Taxon Range Zone large dataset of 19,042 specimens from 60 samples. The spec- (Rupelian), subdivided into the Allosminthus khandae Taxon imens represent 176 species-level and 99 genus-level taxa com- Range Subzone and the Huangomys frequens Abundance prising 135 small mammal species and 47 large mammals. A Subzone, the Amphechinus taatsiingolensis Abundance Zone detailed lithostratigraphy and new magnetostratigraphic and (early Chattian), the Amphechinus major Taxon Range Zone radiometric datings provide an excellent frame for these biotic (late Chattian), subdivided -
Teruel, Spain)
Freudenthal… 26/7/07 19:05 Página 97 Treb. Mus. Geol. Barcelona, 12: 97 -173 (2004) Gliridae (Rodentia, Mammalia) from the Eocene and Oligocene of the Sierra Palomera (Teruel, Spain) Matthijs FREUDENTHAL* RESUMEN FREUDENTAL, M. Gliridae (Rodentia, Mammalia) del Eoceno y Oligoceno en la Sierra Palomera (Teruel, Spain). En este trabajo se hace una revisión taxonómica de los Gliridae pertenecientes a los géneros Glamys y Gliravus a partir de material obtenido en la Sierra Palomera y en el área de Montalbán (Teruel, España). Esta revisión lleva a una definición más precisa del género Glamys; a una limitación del género Gliravus, que incluye la especie-tipo y algunas especies estrechamente relacionadas; y a la definición de un género nuevo, Schizogliravus. Con esta nueva clasificación se soluciona el problema del género Gliravus, que se había convertido en un refugio en donde meter todas las especies que no cabían en otro género. Se proponen términos adicionales en la nomenclatura de los dientes de los Gliridae. Se describen dos especies nuevas: Glamys umbriae y Schizogliravus montisal- bani, la especie-tipo del nuevo género Schizogliravus. Dentro del género Glamys se pueden reconocer al menos tres líneas, supuesta- mente adaptadas a condiciones ambientales diferentes. Palabras clave: Gliridae, Mammalia, Eoceno, Oligoceno, España. * Departamento de Estratigrafía y Paleontología, Fac. de Ciencias, Universidad de Granada, Campus Fuente Nueva, E-18002, Granada, Spain. Email: [email protected] Freudenthal… 26/7/07 19:05 Página 98 98 ABSTRACT On the basis of material from the Sierra Palomera and the area of Montalbán (Teruel, Spain) the glirid genera Glamys and Gliravus are revised. -
Palaeontologia Electronica Microtoid Cricetids and the Early History Of
Palaeontologia Electronica http://palaeo-electronica.org Microtoid cricetids and the early history of arvicolids (Mammalia, Rodentia) Oldrich Fejfar, Wolf-Dieter Heinrich, Laszlo Kordos, and Lutz Christian Maul ABSTRACT In response to environmental changes in the Northern hemisphere, several lines of brachyodont-bunodont cricetid rodents evolved during the Late Miocene as “micro- toid cricetids.” Major evolutionary trends include increase in the height of cheek tooth crowns and development of prismatic molars. Derived from a possible Megacricetodon or Democricetodon ancestry, highly specialised microtoid cricetids first appeared with Microtocricetus in the Early Vallesian (MN 9) of Eurasia. Because of the morphological diversity and degree of parallelism, phylogenetic relationships are difficult to detect. The Trilophomyinae, a more aberrant cricetid side branch, apparently became extinct without descendants. Two branches of microtoid cricetids can be recognized that evolved into “true” arvicolids: (1) Pannonicola (= Ischymomys) from the Late Vallesian (MN 10) to Middle Turolian (MN 12) of Eurasia most probably gave rise to the ondatrine lineage (Dolomys and Propliomys) and possibly to Dicrostonyx, whereas (2) Microt- odon known from the Late Turolian (MN 13) and Early Ruscinian (MN 14) of Eurasia and possibly parts of North America evolved through Promimomys and Mimomys eventually to Microtus, Arvicola and other genera. The Ruscinian genus Tobienia is presumably the root of Lemmini. Under this hypothesis, in contrast to earlier views, two evolutionary sources of arvicolids would be taken into consideration. The ancestors of Pannonicola and Microtodon remain unknown, but the forerunner of Microtodon must have had a brachyodont-lophodont tooth crown pattern similar to that of Rotundomys bressanus from the Late Vallesian (MN 10) of Western Europe. -
Tertiary Anuran Assemblages of Europe
1 Tertiary anuran assemblages of Europe Localities are listed according to their geological age; those of the same age are ordered according to their geographic position (from the west to the east). Abbreviations of taxa: Alb – Albionbatrachus sp., Albionbatrachus wightensis, Eo wa – Eopelobates wagneri Pel cul – Pelobates cultripes, Pelobates cf. cultripes Albionbatrachus cf. wightensis Hyl arb – Hyla arborea, Hyla (arborea) sp. Pel de – Pelobates decheni Alyt sp. – Alytes sp., cf. Alytes Hyl sp. – Hyla sp., cf. Hyla Pel fus – Pelobates fuscus, Pelobates cf. fuscus Bo sp. – Bombina sp. Lat sp. – Latonia sp., cf. Latonia Pel syr – Pelobates cf. syriacus Bo bo – Bombina bombina, Bombina (bombina) sp. Lat gig – Latonia gigantea, Latonia cf. gigantea Pld are –Pelodytes cf. arevacus Bo va – Bombina variegata Lat rag – Latonia ragei, Latonia cf. ragei Pld pu – Pelodytes punctatus, Pelodytes cf. punctatus B ? – Bufonidae indet. Lat sey – Latonia seyfriedi Pld sp. – Pelodytes sp., cf. Pelodytes Buf sp. – Bufo sp. Lat ver – Latonia vertaizoni, Latonia aff. L. vertaizoni Pli sp. – Pliobatrachus sp., Pliobatrachus langhae, Buf buf – Bufo bufo, Bufo cf. B. bufo Lut – Lutetiobatrachus gracilis (Anura inc. sedis) Pliobatrachus cf. langhae Buf cal – Bufo calamita, Bufo aff. B. calamita M? – Microhylidae indet. R? – Ranidae indet., Buf ges – Bufo (= Palaeophrynus) gessneri Me tob – Messelobatrachus tobieni Ra arv – Rana arvalis, Rana cf. arvalis Buf pri – Bufo priscus, Bufo cf. B. priscus Opi hes – Opisthocoellelus hessi Ra sp. – Rana sp., Ranomorphus similis* Buf rad – Bufo raddei Opi wei – Opisthocoellelus weigelti Ra da – Rana dalmatina Buf viri – Bufo viridis, Bufo cf. B. viridis, Bufo aff. B. P? – Pelobatidae indet. Ra esc – Rana esculenta viridis, Bufo (viridis) sp.