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Geckos from the Middle Miocene of Devı´Nska Nova´ Ves (Slovakia): New Material and a Review of the Previous Record
Swiss Journal of Geosciences (2018) 111:183–190 https://doi.org/10.1007/s00015-017-0292-1 (0123456789().,-volV)(0123456789().,-volV) Geckos from the middle Miocene of Devı´nska Nova´ Ves (Slovakia): new material and a review of the previous record 1 2 3 Andrej Cˇ ernˇ ansky´ • Juan D. Daza • Aaron M. Bauer Received: 16 May 2017 / Accepted: 17 July 2017 / Published online: 16 January 2018 Ó Swiss Geological Society 2017 Abstract New species of a gecko of the genus Euleptes is described here—E. klembarai. The material comes from the middle Miocene (Astaracian, MN 6) of Slovakia, more precisely from the well-known locality called Zapfe‘s fissure fillings (Devı´nska Nova´ Ves, Bratislava). The fossil material consists of isolated left maxilla, right dentary, right pterygoid and cervical and dorsal vertebrae. The currently known fossil record suggests that isolation of environment of the Zapfe‘s fissure site, created a refugium for the genus Euleptes in Central Europe (today, this taxon still inhabits southern part of Europe and North Africa—E. europea), probably resulting from the island geography of this area during the middle Miocene. The isolation of this territory might have facilitated allopatric speciation. Keywords Gekkota Á Euleptes Á Neogene Á Zapfe’s fissure 1 Introduction superb preservation of skeletal and soft tissue (Bo¨hme 1984; Daza and Bauer 2012; Daza et al. 2013b, 2016). Gekkota (geckos and pygopods) is a speciose clade of Very important and superbly preserved find in Baltic amber lepidosaurs, comprising more than 1600 extant species is represented by Yantarogecko balticus from the Early (Bauer 2013; Uetz and Freed 2017). -
11 Sualdea Et Al.Indd
SPANISH J OURNAL OF P ALAEONTOLOGY 20 years at campus: heritage assessment update for Somosaguas fossil geosite (Pozuelo de Alarcón, Madrid) Lucía R. SUALDEA 1* , Adriana OLIVER 2, Fernando BLANCO 3, Iris MENÉNDEZ 1,4 , Manuel HERNÁNDEZ FERNÁNDEZ1,4, Laura DOMINGO 1,5 & Ana Rosa GÓMEZ CANO 6,7 1 Departamento de Geodinámica, Estratigrafía y Paleontología, Facultad de Ciencias Geológicas, Universidad Complutense de Madrid, C/ José Antonio Novais 12, 28040, Madrid; [email protected], [email protected], [email protected], [email protected]. 2 Geosfera, C/ Madres de la Plaza de Mayo, 2, 28523, Rivas-Vaciamadrid, Madrid; [email protected] 3 Museum für Naturkunde, Leibniz-Institut für Evolutions und Biodiversitätsforschung, Invalidenstraße 43, 10115, Berlin, Germany; [email protected] 4 Departamento de Geología Sedimentaria y Cambio Medioambiental, Instituto de Geociencias IGEO (CSIC, UCM), C/ Dr. Severo Ochoa, 7, 28040, Madrid 5 Earth and Planetary Sciences Department. University of California Santa Cruz, 1156 High Street, 95064, Santa Cruz, USA 6 Transmitting Science, C/ Gardenia 2, Piera, 08784, Barcelona. 7 Institut Català de Paleontologia Miquel Crusafont, Edifi ci ICP, Campus de la UAB s/n, 08193, Cerdanyola del Vallès; [email protected] * Corresponding author Sualdea, L.R., Oliver, A., Blanco, F., Menéndez, I., Hernández Fernández, M., Domingo, L. & Gómez Cano, A.R. 2019. 20 years at campus: heritage assessment update for Somosaguas fossil geosite (Pozuelo de Alarcón, Madrid). [20 años en el campus: actualización de la valoración -
Carnivora from the Late Miocene Love Bone Bed of Florida
Bull. Fla. Mus. Nat. Hist. (2005) 45(4): 413-434 413 CARNIVORA FROM THE LATE MIOCENE LOVE BONE BED OF FLORIDA Jon A. Baskin1 Eleven genera and twelve species of Carnivora are known from the late Miocene Love Bone Bed Local Fauna, Alachua County, Florida. Taxa from there described in detail for the first time include the canid cf. Urocyon sp., the hemicyonine ursid cf. Plithocyon sp., and the mustelids Leptarctus webbi n. sp., Hoplictis sp., and ?Sthenictis near ?S. lacota. Postcrania of the nimravid Barbourofelis indicate that it had a subdigitigrade posture and most likely stalked and ambushed its prey in dense cover. The postcranial morphology of Nimravides (Felidae) is most similar to the jaguar, Panthera onca. The carnivorans strongly support a latest Clarendonian age assignment for the Love Bone Bed. Although the Love Bone Bed local fauna does show some evidence of endemism at the species level, it demonstrates that by the late Clarendonian, Florida had become part of the Clarendonian chronofauna of the midcontinent, in contrast to the higher endemism present in the early Miocene and in the later Miocene and Pliocene of Florida. Key Words: Carnivora; Miocene; Clarendonian; Florida; Love Bone Bed; Leptarctus webbi n. sp. INTRODUCTION can Museum of Natural History, New York; F:AM, Frick The Love Bone Bed Local Fauna, Alachua County, fossil mammal collection, part of the AMNH; UF, Florida Florida, has produced the largest and most diverse late Museum of Natural History, University of Florida. Miocene vertebrate fauna known from eastern North All measurements are in millimeters. The follow- America, including 43 species of mammals (Webb et al. -
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). -
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A new marine vertebrate assemblage from the Late Neogene Purisima Formation in Central California, part II: Pinnipeds and Cetaceans Robert W. BOESSENECKER Department of Geology, University of Otago, 360 Leith Walk, P.O. Box 56, Dunedin, 9054 (New Zealand) and Department of Earth Sciences, Montana State University 200 Traphagen Hall, Bozeman, MT, 59715 (USA) and University of California Museum of Paleontology 1101 Valley Life Sciences Building, Berkeley, CA, 94720 (USA) [email protected] Boessenecker R. W. 2013. — A new marine vertebrate assemblage from the Late Neogene Purisima Formation in Central California, part II: Pinnipeds and Cetaceans. Geodiversitas 35 (4): 815-940. http://dx.doi.org/g2013n4a5 ABSTRACT e newly discovered Upper Miocene to Upper Pliocene San Gregorio assem- blage of the Purisima Formation in Central California has yielded a diverse collection of 34 marine vertebrate taxa, including eight sharks, two bony fish, three marine birds (described in a previous study), and 21 marine mammals. Pinnipeds include the walrus Dusignathus sp., cf. D. seftoni, the fur seal Cal- lorhinus sp., cf. C. gilmorei, and indeterminate otariid bones. Baleen whales include dwarf mysticetes (Herpetocetus bramblei Whitmore & Barnes, 2008, Herpetocetus sp.), two right whales (cf. Eubalaena sp. 1, cf. Eubalaena sp. 2), at least three balaenopterids (“Balaenoptera” cortesi “var.” portisi Sacco, 1890, cf. Balaenoptera, Balaenopteridae gen. et sp. indet.) and a new species of rorqual (Balaenoptera bertae n. sp.) that exhibits a number of derived features that place it within the genus Balaenoptera. is new species of Balaenoptera is relatively small (estimated 61 cm bizygomatic width) and exhibits a comparatively nar- row vertex, an obliquely (but precipitously) sloping frontal adjacent to vertex, anteriorly directed and short zygomatic processes, and squamosal creases. -
Reef-Coral Fauna of Carrizo Creek, Imperial County, California, and Its Significance
THE REEF-CORAL FAUNA OF CARRIZO CREEK, IMPERIAL COUNTY, CALIFORNIA, AND ITS SIGNIFICANCE . .By THOMAS WAYLAND VAUGHAN . INTRODUCTION. occur has been determined by Drs . Arnold and Dall to be lower Miocene . The following conclusions seem warranted : Knowledge of the existence of the unusually (1) There was water connection between the Atlantic and interesting coral fauna here discussed dates Pacific across Central America not much previous to the from the exploration of Coyote Mountain (also upper Oligocene or lower Miocene-that is, during the known as Carrizo Mountain) by H . W. Fair- upper Eocene or lower Oligocene . This conclusion is the same as that reached by Messrs. Hill and Dall, theirs, how- banks in the early nineties.' Dr. Fairbanks ever, being based upon a study of the fossil mollusks . (2) sent the specimens of corals he collected to During lower Miocene time the West Indian type of coral Prof. John C. Merriam, at the University of fauna extended westward into the Pacific, and it was sub- California, who in turn sent them to me . sequent to that time that the Pacific and Atlantic faunas There were in the collection representatives of have become so markedly differentiated . two species and one variety, which I described As it will be made evident on subsequent under the names Favia merriami, 2 Stephano- pages that this fauna is much younger than ctenia fairbanksi,3 and Stephanoccenia fair- lower Miocene, the inference as to the date of banksi var. columnaris .4 As the geologic hori- the interoceanic connection given in the fore- zon was not even approximately known at that going quotation must be modified . -
Cozzette Sandstone, Book Cliffs, Colorado, U.S.A
Journal of Sedimentary Research, 2015, v. 85, 459–488 Research Article DOI: http://dx.doi.org/10.2110/jsr.2015.26 TECTONICALLY CONTROLLED NEARSHORE DEPOSITION: COZZETTE SANDSTONE, BOOK CLIFFS, COLORADO, U.S.A. 1 2 2 ANDREW S. MADOF, NICHOLAS CHRISTIE-BLICK, AND MARK H. ANDERS 1Chevron Energy Technology Company, Houston, Texas 77002-7308, U.S.A. 2Department of Earth and Environmental Sciences and Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964-8000, U.S.A. e-mail: [email protected] ABSTRACT: The Book Cliffs of eastern Utah and western Colorado have been pivotal in the development of outcrop-based sequence stratigraphic concepts for nonmarine to shallow marine siliciclastic depositional settings. Prior studies in this area, and more generally in the Cretaceous western interior foreland basin of North America, have concluded that nearshore accumulation is controlled for the most part by the interaction between oscillatory eustatic change and longer-term regional patterns of flexural subsidence. New outcrop and subsurface evidence reported here from the eastern Book Cliffs suggests that three-dimensional tectonic tilting at length scales of up to , 50 km (31 mi) and timescales of less than , 200 kyr also strongly influenced sedimentation. Continental ice sheets are thought to have been small at the time. Documented patterns of accumulation are inconsistent with those expected from interactions of eustasy and regional flexure alone. The upper Campanian Cozzette Sandstone Member of the Mount Garfield Formation consists of twelve lithofacies arranged into six lithofacies assemblages, inferred to have been deposited in shallow marine, marginal marine, and nonmarine depositional environments. -
Maquetación 1
ISSN (print): 1698-6180. ISSN (online): 1886-7995 www.ucm.es /info/estratig/journal.htm Journal of Iberian Geology 33 (2) 2007: 261-282 Callovian and the Callovian - Oxfordian transition sedimentary record in NE Iberian Chain: Taphonomic analysis and palaeogeography El Calloviense y el registro sedimentario del tránsito Calloviense-Oxfordiense en la Cordillera Ibérica nororiental: Análisis tafonómico y paleogeografía G. Meléndez1, J. Ramajo2, J. Bello1, K.N. Page3 1Departamento de Geología (Paleontología). Universidad de Zaragoza. C./ Pedro Cerbuna 12; 50009- Zaragoza (España). [email protected], [email protected] 2Departamento de Geología (Estratigrafía). Universidad de Zaragoza. C./ Pedro Cerbuna 12; 50009- Zaragoza (España). [email protected] 3School of Earth, Ocean & Environmental Sciences, University of Plymouth, Drake Circus, Plymouth PL4 8AA, UK. [email protected] Received: 07/10/06 / Accepted: 30/11/06 Abstract A comparative study is made on Callovian to middle Oxfordian sequences along the Northeastern Iberian Chain (E. Spain). In the NW areas, from Veruela-Ricla to Tosos (SW-S of Zaragoza), Callovian deposits are represented by expanded carbonate sequences (mudstone and marls with a variable content in clastics) ranging from early Bullatus to Athleta Biozone. Farther East in the near area of Moneva-Ariño (Sierra de Arcos) and in the area of Calanda (SE of Zaragoza), this stratigraphic interval is represented by a strongly condensed, 2-4 m thick, highly incomplete sequence. Bullatus to early Anceps biozones are partly represented under bioclastic or oolitic packstone facies. The Callovian-Oxfordian transition interval deposits are represented by a decimeter-thick iron- ooid fossiliferous limestone condensed sequence (low values of sedimentation rate) formed by expanded sediments (high values of instant rate of sediment accumulation). -
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. -
First Record of Non-Mineralized Cephalopod Jaws and Arm Hooks
Klug et al. Swiss J Palaeontol (2020) 139:9 https://doi.org/10.1186/s13358-020-00210-y Swiss Journal of Palaeontology RESEARCH ARTICLE Open Access First record of non-mineralized cephalopod jaws and arm hooks from the latest Cretaceous of Eurytania, Greece Christian Klug1* , Donald Davesne2,3, Dirk Fuchs4 and Thodoris Argyriou5 Abstract Due to the lower fossilization potential of chitin, non-mineralized cephalopod jaws and arm hooks are much more rarely preserved as fossils than the calcitic lower jaws of ammonites or the calcitized jaw apparatuses of nautilids. Here, we report such non-mineralized fossil jaws and arm hooks from pelagic marly limestones of continental Greece. Two of the specimens lie on the same slab and are assigned to the Ammonitina; they represent upper jaws of the aptychus type, which is corroborated by fnds of aptychi. Additionally, one intermediate type and one anaptychus type are documented here. The morphology of all ammonite jaws suggest a desmoceratoid afnity. The other jaws are identifed as coleoid jaws. They share the overall U-shape and proportions of the outer and inner lamellae with Jurassic lower jaws of Trachyteuthis (Teudopseina). We also document the frst belemnoid arm hooks from the Tethyan Maastrichtian. The fossils described here document the presence of a typical Mesozoic cephalopod assemblage until the end of the Cretaceous in the eastern Tethys. Keywords: Cephalopoda, Ammonoidea, Desmoceratoidea, Coleoidea, Maastrichtian, Taphonomy Introduction as jaws, arm hooks, and radulae are occasionally found Fossil cephalopods are mainly known from preserved (Matern 1931; Mapes 1987; Fuchs 2006a; Landman et al. mineralized parts such as aragonitic phragmocones 2010; Kruta et al. -
Issn: 2250-0588 Fossil Mammals
IJREISS Volume 2, Issue 8 (August 2012) ISSN: 2250-0588 FOSSIL MAMMALS (RHINOCEROTIDS, GIRAFFIDS, BOVIDS) FROM THE MIOCENE ROCKS OF DHOK BUN AMEER KHATOON, DISTRICT CHAKWAL, PUNJAB, PAKISTAN 1Khizar Samiullah* 1Muhammad Akhtar, 2Muhammad A. Khan and 3Abdul Ghaffar 1Zoology department, Quaid-e-Azam campus, Punjab University, Lahore, Punjab, Pakistan 2Zoology Department, GC University, Faisalabad, Punjab, Pakistan 3Department of Meteorology, COMSATS Institute of Information Technology (CIIT), Islamabad ABSTRACT Fossil site Dhok Bun Ameer Khatoon (32o 47' 26.4" N, 72° 55' 35.7" E) yielded a significant amount of mammalian assemblage including two families of even-toed fossil mammal (Giraffidae, and Bovidae) and one family of odd-toed (Rhinocerotidae) of the Late Miocene (Samiullah, 2011). This newly discovered site has well exposed Chinji and Nagri formation and has dated approximately 14.2-9.5 Ma. This age agrees with the divergence of different mammalian genera. Sedimentological evidence of the site supports that this is deposited in locustrine or fluvial environment, as Chinji formation is composed primarily of mud-stone while the Nagri formation is sand dominated. Palaeoenvironmental data indicates that Miocene climate of Pakistan was probably be monsoonal as there is now a days. Mostly the genera recovered from this site resemble with the overlying younger Dhok Pathan formation of the Siwaliks while the size variation in dentition is taxonomically important for vertebrate evolutionary point of view and this is the main reason to conduct this study at this specific site to add additional information in the field of Palaeontology. A detailed study of fossils mammals found in Miocene rocks exposed at Dhok Bun Ameer Khatoon was carried out. -
The Planktonic Foraminifera of the Jurassic. Part III: Annotated Historical Review and References
Swiss J Palaeontol (2017) 136:273–285 DOI 10.1007/s13358-017-0130-0 The planktonic foraminifera of the Jurassic. Part III: annotated historical review and references Felix M. Gradstein1,2 Received: 21 February 2017 / Accepted: 3 April 2017 / Published online: 7 July 2017 Ó Akademie der Naturwissenschaften Schweiz (SCNAT) 2017 Abstract Over 70 publications on Jurassic planktonic With few exceptions, Jurassic planktonic foraminifera foraminifera, particularly by East and West European and publications based on thin-sections are not covered in this Canadian micropalaeontologists, are summarized and review. Emphasis is only on thin-section studies that had briefly annotated. It provides an annotated historic over- impact on our understanding of Jurassic planktonic for- view for this poorly understood group of microfossils, aminifera. By the same token, microfossil casts do not going back to 1881 when Haeusler described Globigerina allow study of the taxonomically important wall structure helvetojurassica from the Birmenstorfer Schichten of and sculpture; reference to such studies is limited to few of Oxfordian age in Canton Aargau, Switzerland. historic interest. The first four, presumably planktonic foraminiferal spe- Keywords Jurassic Á Planktonic foraminifera Á Annotated cies from Jurassic strata, were described in the second half of historical review 1881–2015 the nineteenth century: Globigerina liasina from the Middle Lias of France (Terquem and Berthelin 1875), G. helveto- jurassica from the Early Oxfordian of Switzerland (Haeusler Annotated historical overview 1881, 1890) and G. oolithica and G. lobata from the Bajocian of France (Terquem 1883). Some descriptions were from Jurassic planktonic foraminifera have been studied since the internal moulds. It was not until 1958 (see below) that more second half of the nineteen’s century, but it was not until after attention was focused on the occurrences of early planktonic the Second World War that micropalaeontological studies foraminifera, with emphasis on free specimens.