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The World at the Time of Messel: Conference Volume
T. Lehmann & S.F.K. Schaal (eds) The World at the Time of Messel - Conference Volume Time at the The World The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment and the History of Early Primates 22nd International Senckenberg Conference 2011 Frankfurt am Main, 15th - 19th November 2011 ISBN 978-3-929907-86-5 Conference Volume SENCKENBERG Gesellschaft für Naturforschung THOMAS LEHMANN & STEPHAN F.K. SCHAAL (eds) The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference Frankfurt am Main, 15th – 19th November 2011 Conference Volume Senckenberg Gesellschaft für Naturforschung IMPRINT The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference 15th – 19th November 2011, Frankfurt am Main, Germany Conference Volume Publisher PROF. DR. DR. H.C. VOLKER MOSBRUGGER Senckenberg Gesellschaft für Naturforschung Senckenberganlage 25, 60325 Frankfurt am Main, Germany Editors DR. THOMAS LEHMANN & DR. STEPHAN F.K. SCHAAL Senckenberg Research Institute and Natural History Museum Frankfurt Senckenberganlage 25, 60325 Frankfurt am Main, Germany [email protected]; [email protected] Language editors JOSEPH E.B. HOGAN & DR. KRISTER T. SMITH Layout JULIANE EBERHARDT & ANIKA VOGEL Cover Illustration EVELINE JUNQUEIRA Print Rhein-Main-Geschäftsdrucke, Hofheim-Wallau, Germany Citation LEHMANN, T. & SCHAAL, S.F.K. (eds) (2011). The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates. 22nd International Senckenberg Conference. 15th – 19th November 2011, Frankfurt am Main. Conference Volume. Senckenberg Gesellschaft für Naturforschung, Frankfurt am Main. pp. 203. -
Updated Aragonian Biostratigraphy: Small Mammal Distribution and Its Implications for the Miocene European Chronology
Geologica Acta, Vol.10, Nº 2, June 2012, 159-179 DOI: 10.1344/105.000001710 Available online at www.geologica-acta.com Updated Aragonian biostratigraphy: Small Mammal distribution and its implications for the Miocene European Chronology 1 2 3 4 3 1 A.J. VAN DER MEULEN I. GARCÍA-PAREDES M.A. ÁLVAREZ-SIERRA L.W. VAN DEN HOEK OSTENDE K. HORDIJK 2 2 A. OLIVER P. PELÁEZ-CAMPOMANES * 1 Faculty of Earth Sciences, Utrecht University Budapestlaan 4, 3584 CD Utrecht, The Netherlands. Van der Meulen E-mail: [email protected] Hordijk E-mail: [email protected] 2 Departamento de Paleobiología, Museo Nacional de Ciencias Naturales MNCN-CSIC C/ José Gutiérrez Abascal 2, 28006 Madrid, Spain. García-Paredes E-mail: [email protected] Oliver E-mail: [email protected] Peláez-Campomanes E-mail: [email protected] 3 Netherlands Centre for Biodiversity-Naturalis Darwinweg 2, 2333 CR Leiden, The Netherlands. Van den Hoek Ostende E-mail: [email protected] 4 Departamento de Paleontología, Facultad de Ciencias Geológicas, Universidad Complutense de Madrid. IGEO-CSIC C/ José Antonio Novais 2, 28040 Madrid, Spain. Álvarez-Sierra E-mail: [email protected] * Corresponding author ABSTRACT This paper contains formal definitions of the Early to Middle Aragonian (Late Early–Middle Miocene) small- mammal biozones from the Aragonian type area in North Central Spain. The stratigraphical schemes of two of the best studied areas for the Lower and Middle Miocene, the Aragonian type area in Spain and the Upper Freshwater Molasse from the North Alpine Foreland Basin in Switzerland, have been compared. -
Paleoenvironment of the Late Eocene Chadronian-Age Whitehead Creek Locality (Northwestern Nebraska)
St. Cloud State University theRepository at St. Cloud State Culminating Projects in Cultural Resource Management Department of Anthropology 10-2019 Paleoenvironment of the Late Eocene Chadronian-Age Whitehead Creek Locality (Northwestern Nebraska) Samantha Mills Follow this and additional works at: https://repository.stcloudstate.edu/crm_etds Part of the Archaeological Anthropology Commons Recommended Citation Mills, Samantha, "Paleoenvironment of the Late Eocene Chadronian-Age Whitehead Creek Locality (Northwestern Nebraska)" (2019). Culminating Projects in Cultural Resource Management. 28. https://repository.stcloudstate.edu/crm_etds/28 This Thesis is brought to you for free and open access by the Department of Anthropology at theRepository at St. Cloud State. It has been accepted for inclusion in Culminating Projects in Cultural Resource Management by an authorized administrator of theRepository at St. Cloud State. For more information, please contact [email protected]. Paleoenvironment of the Late Eocene Chadronian-Age Whitehead Creek Locality (Northwestern Nebraska) by Samantha M. Mills A Thesis Submitted to the Graduate Faculty of St. Cloud State University in Partial Fulfillment of the Requirements for the Degree of Master of Science in Functional Morphology October, 2019 Thesis Committee: Matthew Tornow, Chairperson Mark Muñiz Bill Cook Tafline Arbor 2 Abstract Toward the end of the Middle Eocene (40-37mya), the environment started to decline on a global scale. It was becoming more arid, the tropical forests were disappearing from the northern latitudes, and there was an increase in seasonality. Research of the Chadronian (37- 33.7mya) in the Great Plains region of North America has documented the persistence of several mammalian taxa (e.g. primates) that are extinct in other parts of North America. -
Paleogene and Neogene Time Scale of GTS 2012 Paleogene Neogene N
Paleogene and Neogene Time Scale of GTS 2012 Paleogene Neogene N. Vandenberghe 1, F.J. Hilgen 2 and R.P. Speijer 3 F.J. Hilgen 1, L.J. Lourens 2 and J.A. Van Dam 3 1. Department of Earth and Environmental Sciences, K. U. Leuven, Celestijnenlaan 200E, B - 3001 Leuven, Belgium, [email protected] 1. Department of Earth Sciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, The Netherlands, [email protected] 2. Department of Earth Sciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, The Netherlands, [email protected] 2. Department of Earth Sciences, Utrecht University, Budapestlaan 4, 3508 TA Utrecht, The Netherlands, [email protected] 3. Department of Earth and Environmental Sciences, K. U. Leuven, Celestijnenlaal 200E, B - 3001 Leuven, Belgium, [email protected] 3. Institut Català de Paleontologia Miquel Crusafont (ICP), Campus de la UAB, Mòdul ICP, E-08193 cerdanyola del Vallès, Spain, [email protected] Of the 9 Paleogene stages, only 3 remain to be formally defined: the Bartonian and Priabonian stages of upper Paleogene Time Scale Eocene and the Chattian (base of upper Oligocene). Larger 18 13 AGE Epoch/Age Polarity Mega- Dinoflagellate Cysts North American O C AGE -1.0 -0.5 -0.5 Of the 8 Neogene stages, only 2 remain to be formally defined: the Burdigalian and Langhian stages of lower and middle Mio- (Ma) Chron Cycles Planktonic Foraminifera Benthic Calcareous Nannofossils Radiolarians NALMA MP European Mammals ALMA SALMA 0.0 0.5 1.0 1.5 2.0 0.0 0.5 1.0 1.5 2.0 2.5 Age (Stage) (Ma) During the Paleogene, the global climate, being warm (Stage) Northwestern Europe Mammals other zones Foraminifera ELMA R T low latitude southern high latitude until the late Eocene, shows a significant cooling trend cene. -
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. -
Problems of Classification As Applied to the Rodentia
263 PROBLEMS OF CLASSIFICATION AS APPLIED TO THE RODENTIA by Albert E. WOOD* ABSTRACT A classification should be both usable and useful, not too complex either in the amount of splitting or in the number of hierarchies involved, and not so simple as to give a false assurance of knowledge of relationships. Classifi cations are only possible because we do not have complete knowledge of the evolution of the organisms concerned, because gaps in the record are necessary to allow the separation of the various taxa. Rodent classification is compli cated by the large number of organisms involved and by the great amount of parallelism that has taken place In the evolution of any and all features. If several independent features are characteristic of a certain taxon, should an effort be made to define the group on the basis of all the features, or should only one be selected as the determi nant ? Unless the evolution of the several features was closely linked, the former solution will sooner or later lead to insurmountable problems. A classification is a formal arrangement that expresses the author's opinion of the relationships of the organisms concerned. It should be an attempt to approximate the actual genetic relationships existing, or that formerly existed, among the pertinent organisms. During the course of organizing a classification of the mammalian Order Rodentia, I encountered a number of problems of a general nature, some of which are discussed below. Usually, there are extensive gaps in our knowledge of organisms, particularly of fossil ones. These are useful in classification, because we use the gaps to delimit the various units being classified. -
Chinaxiv:202107.00041V1 Chronostratigraphy, Biostratigraphy, Magnetostratigraphy
ChinaXiv合作期刊 Stratigraphical significance of Ulantatal sequence (Nei Mongol, China) in refining the latest Eocene and Oligocene terrestrial regional stages Joonas WASILJEFF1* ZHANG Zhao-Qun2,3,4* (1 Department of Geosciences and Geography, University of Helsinki P.O. Box 64, Helsinki 00014, Finland) (2 Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences Beijing 100044, China) (3 CAS Center for Excellence in Life and Paleoenvironment Beijing 100044, China) (4 College of Earth and Planetary Sciences, University of Chinese Academy of Sciences Beijing 100049, China) * Corresponding authors: [email protected]; [email protected] Abstract Robust regional chronostratigraphic framework is the basis of understanding climatic and faunal events in the geologic history. One of the most dramatic faunal turnovers of the past 50 million years in Asia is linked to the Eocene–Oligocene Transition (EOT) at about 34 Ma. However, the chronostratigraphic relationships between faunal modulation and geologic events associated with the EOT in China have remained uncertain before and after the epoch boundaries, mainly due to the scarcity of continuous records and problems in correlating and subdividing the classic areas containing abundant mammalian fossils. Past decades have seen developments in establishing Chinese regional Paleogene Land Mammal Ages, and albeit many ages are well constrained, some, such as those of the latest Eocene and the Oligocene, have remained unsettled. In this paper, we present how recent evidence from the fossiliferous Ulantatal sequence, Nei Mongol, China, provides better constraints to the latest Eocene and Oligocene Chinese Land Mammal ages (Baiyinian, Ulantatalian, and Tabenbulukian). -
Novitatesamerican MUSEUM PUBLISHED by the AMERICAN MUSEUM of NATURAL HISTORY CENTRAL PARK WEST at 79TH STREET NEW YORK, N.Y
NovitatesAMERICAN MUSEUM PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET NEW YORK, N.Y. 10024 U.S.A. NUMBER 2626 JUNE 30, 1977 JOHN H. WAHLERT Cranial Foramina and Relationships of Eutypomys (Rodentia, Eutypomyidae) AMERICAN MUSEUM Novitates PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK, N.Y. 10024 Number 2626, pp. 1-8, figs. 1-3, table 1 June 30, 1977 Cranial Foramina and Relationships of Eutypomys (Rodentia, Eutypomyidae) JOHN H. WAHLERT1 ABSTRACT Derived characters of the sphenopalatine, lies had common ancestry in a stem species from interorbital, and dorsal palatine foramina are which no other rodent groups are descended. The shared by the Eutypomyidae and Castoridae. two families may be included in a monophyletic These support the hypothesis that the two fami- superfamily, Castoroidea. INTRODUCTION Eutypomys is an extinct sciuromorphous gave more characters shared with castorids; he, rodent known in North America from strata that too, found many features in common with the range in age from latest Eocene to early Miocene. ischyromyoids. Wood noted the similarity of The genus was named by Matthew (1905) based molar crown pattern to that of Paramys and ex- on the species Eutypomys thomsoni. "Progres- plained it as a parallelism that possibly indicates sive" characters of the teeth and hind feet led relationship. Wilson (1949b) pointed out that the Matthew to ally it with the beaver family, Cas- dental pattern of Eutypomys is more like that of toridae. He pointed out that it retains many sciuravids than that of paramyids. -
New Paroxyclaenid Mammals from the Early Eocene of the Paris Basin
Published in "Journal of Systematic Palaeontology 17(20): 1711–1743, 2019" which should be cited to refer to this work. New paroxyclaenid mammals from the early Eocene of the Paris Basin (France) shed light on the origin and evolution of these endemic European cimolestans aà b c d Floreal Sole , Olivia Plateau ,Kevin Le Verger and Alain Phelizon aDirectorate Earth and History of Life, Palaeobiosphere Evolution Research Unit, Royal Belgian Institute of Natural Sciences, Rue Vautier 29, B–1000 Brussels, Belgium; bUniversite de Fribourg, Faculte des sciences, Departement de geosciences, Chemin du musee 6, Fribourg 1700, Switzerland; cCR2P–MNHN, UPMC-Paris 6 (Sorbonne Universites)–Museum National d’Histoire Naturelle, CP 38, 8 rue Buffon, 75005, Paris, France; dSocieted’Etude des Sciences Naturelles de Reims, 122 bis, rue du Barbatre,^ 51100 Reims, France We present new species of an enigmatic family of mammals, which is endemic to Europe, the Paroxyclaenidae: Merialus bruneti sp. nov., Fratrodon tresvauxi gen. et sp. nov., Paraspaniella gunnelli gen. et sp. nov., and Sororodon tresvauxae gen. et sp. nov. The fossils described come from six localities of the Ypresian of the Paris Basin (France): Pourcy (MP7), Mutigny, Avenay, Conde-en-Brie (MP8 þ 9), Grauves and Premontre (MP10). They allow the description of three new genera and four new species belonging to the subfamilies Merialinae and Paroxyclaeninae. Two of these new species represent the earliest occurrence of each subfamily. Fossils from Mutigny, Avenay and Conde-en- Brie indicate that merialines were more abundant than paroxyclaenines during the Ypresian. Surprisingly, merialines disappeared from the fossil record at the end of the Ypresian – the youngest records are close to MP10 – while the paroxyclaenines were present in Europe until the end of the middle Eocene. -
Advanced Online Publication
ChinaXiv合作期刊 古 脊 椎 动 物 学 报 VERTEBRATA PALASIATICA A new species of Brontotheriidae from the Middle Eocene of Junggar Basin, Xinjiang, China Li Shuo1,2 (1 Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences Beijing 100044 [email protected]) (2 University of Chinese Academy of Sciences Beijing 100049) Abstract A new species of large Irdinmanhan brontothere, Epimanteoceras mae sp. nov., is described based on an incomplete skull which was collected from the Üqbulak Formation of Sangequan site, Junggar Basin of Xinjiang Uygur Autonomous Region. The new specimen can Advancedbe assigned to the genus Epimanteocerasonline by the large superorbital publication processes, the broad frontal bone, the shallow central fossae on the molars, and the absence of the anterolingual cingular cusp on molars and the hypocone on M3. E. mae is characterized by the slightly laterally bowed zygomatic arches, the medially arched parasagittal ridges, the posteromedially angled external auditory pseudomeatus, and the prominent occipital pillar processes. E. mae and E. formosus are closely related. It is uncertain whether E. mae or E. formosus forms the sister group to Brontotheriina, but both of them are the basal group of the latter in the phylogenetic analysis. They are both closed to the Irdinmanhan brontothere Protitan grangeri from Nei Mongol but much primitive than Aktautitan hippopotamopus from Kazakhstan. The discovery of E. mae in Sangequan indicates that the age of Üqbulak Formation is Middle Eocene, and earlier than that of Kyzylbulak Formation bearing A. hippopotamopus in Kazakhstan. Moreover, the discovery of E. -
New Cricetid Rodents from Strata Near the Eocene-Oligocene Boundary in Erden Obo Section (Nei Mongol, China)
RESEARCH ARTICLE New Cricetid Rodents from Strata near the Eocene-Oligocene Boundary in Erden Obo Section (Nei Mongol, China) Qian Li1*, Jin Meng2,1, Yuanqing Wang1 1 Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, China, 2 Division of Paleontology, American Museum of Natural History, New York, New York, United States of America a11111 * [email protected] Abstract New cricetids (Eucricetodon wangae sp. nov., Eucricetodon sp. and Pappocricetodon sizi- wangqiensis sp. nov.) are reported from the lower and middle parts of the “Upper Red” beds OPEN ACCESS of the Erden Obo section in Nei Mongol, China. Eucricetodon wangae is more primitive than Citation: Li Q, Meng J, Wang Y (2016) New Cricetid other known species of the genus from lower Oligocene of Asia and Europe in having a sin- Rodents from Strata near the Eocene-Oligocene gle anterocone on M1, a single connection between the protocone and the paracone, the Boundary in Erden Obo Section (Nei Mongol, China). PLoS ONE 11(5): e0156233. doi:10.1371/journal. anterior metalophule connection in M1-2 and weaker anteroconid and ectomesolophid in pone.0156233 lower molars. Pappocricetodon siziwangqiensis is more advanced than other species of the Editor: Karen E. Samonds, Northern Illinois genus in permanently missing P4 and having posterior protolophule connection. These fos- University, UNITED STATES sils suggest that the age of the “Upper Red” of the Erden Obo section is younger than the Received: January 23, 2016 age of the Upper Eocene Houldjin and Caijiachong formations, but older than those contain- ing the Shandgolian faunas; the “Upper Red” is most closely correlative to the Ergilian beds Accepted: May 11, 2016 in age, and probably close to the Eocene/Oligocene boundary. -
2014BOYDANDWELSH.Pdf
Proceedings of the 10th Conference on Fossil Resources Rapid City, SD May 2014 Dakoterra Vol. 6:124–147 ARTICLE DESCRIPTION OF AN EARLIEST ORELLAN FAUNA FROM BADLANDS NATIONAL PARK, INTERIOR, SOUTH DAKOTA AND IMPLICATIONS FOR THE STRATIGRAPHIC POSITION OF THE BLOOM BASIN LIMESTONE BED CLINT A. BOYD1 AND ED WELSH2 1Department of Geology and Geologic Engineering, South Dakota School of Mines and Technology, Rapid City, South Dakota 57701 U.S.A., [email protected]; 2Division of Resource Management, Badlands National Park, Interior, South Dakota 57750 U.S.A., [email protected] ABSTRACT—Three new vertebrate localities are reported from within the Bloom Basin of the North Unit of Badlands National Park, Interior, South Dakota. These sites were discovered during paleontological surveys and monitoring of the park’s boundary fence construction activities. This report focuses on a new fauna recovered from one of these localities (BADL-LOC-0293) that is designated the Bloom Basin local fauna. This locality is situated approximately three meters below the Bloom Basin limestone bed, a geographically restricted strati- graphic unit only present within the Bloom Basin. Previous researchers have placed the Bloom Basin limestone bed at the contact between the Chadron and Brule formations. Given the unconformity known to occur between these formations in South Dakota, the recovery of a Chadronian (Late Eocene) fauna was expected from this locality. However, detailed collection and examination of fossils from BADL-LOC-0293 reveals an abundance of specimens referable to the characteristic Orellan taxa Hypertragulus calcaratus and Leptomeryx evansi. This fauna also includes new records for the taxa Adjidaumo lophatus and Brachygaulus, a biostratigraphic verifica- tion for the biochronologically ambiguous taxon Megaleptictis, and the possible presence of new leporid and hypertragulid taxa.