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4. Palaeontology
Zurich Open Repository and Archive University of Zurich Main Library Strickhofstrasse 39 CH-8057 Zurich www.zora.uzh.ch Year: 2015 Palaeontology Klug, Christian ; Scheyer, Torsten M ; Cavin, Lionel Posted at the Zurich Open Repository and Archive, University of Zurich ZORA URL: https://doi.org/10.5167/uzh-113739 Conference or Workshop Item Presentation Originally published at: Klug, Christian; Scheyer, Torsten M; Cavin, Lionel (2015). Palaeontology. In: Swiss Geoscience Meeting, Basel, 20 November 2015 - 21 November 2015. 136 4. Palaeontology Christian Klug, Torsten Scheyer, Lionel Cavin Schweizerische Paläontologische Gesellschaft, Kommission des Schweizerischen Paläontologischen Abhandlungen (KSPA) Symposium 4: Palaeontology TALKS: 4.1 Aguirre-Fernández G., Jost J.: Re-evaluation of the fossil cetaceans from Switzerland 4.2 Costeur L., Mennecart B., Schmutz S., Métais G.: Palaeomeryx (Mammalia, Artiodactyla) and the giraffes, data from the ear region 4.3 Foth C., Hedrick B.P., Ezcurra M.D.: Ontogenetic variation and heterochronic processes in the cranial evolution of early saurischians 4.4 Frey L., Rücklin M., Kindlimann R., Klug C.: Alpha diversity and palaeoecology of a Late Devonian Fossillagerstätte from Morocco and its exceptionally preserved fish fauna 4.5 Joyce W.G., Rabi M.: A Revised Global Biogeography of Turtles 4.6 Klug C., Frey L., Rücklin M.: A Famennian Fossillagerstätte in the eastern Anti-Atlas of Morocco: its fauna and taphonomy 4.7 Leder R.M.: Morphometric analysis of teeth of fossil and recent carcharhinid selachiens -
Reconsideración De La Sistemática De Cervavitus (Cervidae, Artiodactyla, Mammalia) Del Pleistoceno Inferior
e390-11 Dong.qxd 30/1/12 14:36 Página 603 View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Estudios Geológicos (E-Journal) Estudios Geológicos, 67(2) julio-diciembre 2011, 603-611 ISSN: 0367-0449 doi:10.3989/egeol.40534.208 Reconsideration of the systematics of the Early Pleistocene Cervavitus (Cervidae, Artiodactyla, Mammalia) Reconsideración de la sistemática de Cervavitus (Cervidae, Artiodactyla, Mammalia) del Pleistoceno Inferior W. Dong1 ABSTRACT Cervavitus were usually found from the Late Miocene and Pliocene deposits in East Europe, Middle Asia and North China, but they were found recently in many Early Pleistocene localities in southern China. The latter resulted in the discussion of their systematic status between Cervavitus and Cervus. Here we show the Early Pleistocene forms from southern China are morphometrically more similar to northern China Cervavitus species, and the cladistic analysis shows that the southern China forms are closer to classic Cervavitus species than Cervus and that also proves their systematic status in Cervavi- tus rather than in Cervus. Cervavitus originated in Moldovan forests of East Europe in the late Vallesian (MN10) from a brachyodont and holometacarpal ancestor with two/three-tined antlers and Palaeomeryx fold and evolved into C. novorossiae. It dispersed into West Europe forests in the earliest Turolian and further west to France in the Ruscinian. It dispersed into northern China forests in the early Turolian and represented by C. shanxius. The great quantity of C. shanxius specimens with brachyodont teeth and complete lateral metacarpals implies the arid Loess Plateau of today was a humid forested region in the Late Miocene. -
Deer from Late Miocene to Pleistocene of Western Palearctic: Matching Fossil Record and Molecular Phylogeny Data
Zitteliana B 32 (2014) 115 Deer from Late Miocene to Pleistocene of Western Palearctic: matching fossil record and molecular phylogeny data Roman Croitor Zitteliana B 32, 115 – 153 München, 31.12.2014 Institute of Cultural Heritage, Academy of Sciences of Moldova, Bd. Stefan Cel Mare 1, Md-2028, Chisinau, Moldova; Manuscript received 02.06.2014; revision E-mail: [email protected] accepted 11.11.2014 ISSN 1612 - 4138 Abstract This article proposes a brief overview of opinions on cervid systematics and phylogeny, as well as some unresolved taxonomical issues, morphology and systematics of the most important or little known mainland cervid genera and species from Late Miocene and Plio-Pleistocene of Western Eurasia and from Late Pleistocene and Holocene of North Africa. The Late Miocene genera Cervavitus and Pliocervus from Western Eurasia are included in the subfamily Capreolinae. A cervid close to Cervavitus could be a direct forerunner of the modern genus Alces. The matching of results of molecular phylogeny and data from cervid paleontological record revealed the paleozoogeographical context of origin of modern cervid subfamilies. Subfamilies Capreolinae and Cervinae are regarded as two Late Miocene adaptive radiations within the Palearctic zoogeographic province and Eastern part of Oriental province respectively. The modern clade of Eurasian Capreolinae is significantly depleted due to climate shifts that repeatedly changed climate-geographic conditions of Northern Eurasia. The clade of Cervinae that evolved in stable subtropical conditions gave several later radiations (including the latest one with Cervus, Rusa, Panolia, and Hyelaphus) and remains generally intact until present days. During Plio-Pleistocene, cervines repeatedly dispersed in Palearctic part of Eurasia, however many of those lineages have become extinct. -
Aplodontid, Sciurid, Castorid, Zapodid and Geomyoid Rodents of the Rodent Hill Locality, Cypress Hills Formation, Southwest Saskatchewan
APLODONTID, SCIURID, CASTORID, ZAPODID AND GEOMYOID RODENTS OF THE RODENT HILL LOCALITY, CYPRESS HILLS FORMATION, SOUTHWEST SASKATCHEWAN A Thesis Submitted to the College of Graduate Studies and Research in Partial Fulfillment of the Requirements for the Degree of Master of Science in the Department of Geological Sciences University of Saskatchewan Saskatoon By Sean D. Bell © Copyright Sean D. Bell, December 2004. All rights reserved. PERMISSION TO USE In presenting this thesis in partial fulfilment of the requirements for a Master’s degree from the University of Saskatchewan, I agree that the libraries of the University of Saskatchewan may make it freely available for inspection. I further agree that permission for copying of this thesis in any manner, in whole or in part, for scholarly purposes may be granted by the professors who supervised my thesis work or, in their absence, by the Head of the Department of Geological Sciences or the Dean of the College of Graduate Studies and Research. It is understood that any copying or publication or use of this thesis or parts thereof for financial gain shall not be allowed without my written permission. It is also understood that due recognition shall be given to me and to the University of Saskatchewan in any scholarly use which may be made of any material in my thesis. Requests for permission to copy or to make other use of material in this thesis in whole or part should be addressed to: Head of the Department of Geological Sciences 114 Science Place University of Saskatchewan Saskatoon, Saskatchewan S7N 5E2 i ABSTRACT The Rodent Hill Locality is a fossil-bearing site that is part of the Cypress Hills Formation, and is located roughly 15 km northwest of the town of Eastend, Saskatchewan. -
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. -
Reconsideración De La Sistemática De Cervavitus (Cervidae, Artiodactyla, Mammalia) Del Pleistoceno Inferior
e390-11 Dong.qxd 30/1/12 14:36 Página 603 Estudios Geológicos, 67(2) julio-diciembre 2011, 603-611 ISSN: 0367-0449 doi:10.3989/egeol.40534.208 Reconsideration of the systematics of the Early Pleistocene Cervavitus (Cervidae, Artiodactyla, Mammalia) Reconsideración de la sistemática de Cervavitus (Cervidae, Artiodactyla, Mammalia) del Pleistoceno Inferior W. Dong1 ABSTRACT Cervavitus were usually found from the Late Miocene and Pliocene deposits in East Europe, Middle Asia and North China, but they were found recently in many Early Pleistocene localities in southern China. The latter resulted in the discussion of their systematic status between Cervavitus and Cervus. Here we show the Early Pleistocene forms from southern China are morphometrically more similar to northern China Cervavitus species, and the cladistic analysis shows that the southern China forms are closer to classic Cervavitus species than Cervus and that also proves their systematic status in Cervavi- tus rather than in Cervus. Cervavitus originated in Moldovan forests of East Europe in the late Vallesian (MN10) from a brachyodont and holometacarpal ancestor with two/three-tined antlers and Palaeomeryx fold and evolved into C. novorossiae. It dispersed into West Europe forests in the earliest Turolian and further west to France in the Ruscinian. It dispersed into northern China forests in the early Turolian and represented by C. shanxius. The great quantity of C. shanxius specimens with brachyodont teeth and complete lateral metacarpals implies the arid Loess Plateau of today was a humid forested region in the Late Miocene. C. shanxius migrated southwards in the Plio-Pleistocene probably due to the drying envi- ronment in northern China with uplifting of Himalayas and evolved into C. -
Novttates PUBLISHED by the AMERICAN MUSEUM of NATURAL HISTORY CENTRAL PARK WEST at 79TH STREET NEW YORK, N.Y
NAMERICAN MUSEUM Novttates PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET NEW YORK, N.Y. 10024 U.S.A. NUMBER 2596 JUNE 4, 1976 BERYL E. TAYLOR AND S. DAVID WEBB Miocene Leptomerycidae (Artiodactyla, Ruminantia) and Their Relationships 4 AMERICAN MUSEUM Norntates PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK, N.Y. 10024 Number 2596, pp. 1-22, figs. 1-7, tables 1-5 June 4, 1976 Miocene Leptomerycidae (Artiodactyla, Ruminantia) and Their Relationships BERYL E. TAYLOR1 AND S. DAVID WEBB2 ABSTRACT Leptomerycidae, previously thought to have Montana and possibly South Dakota is trans- survived only into the Arikareean, are here recog- ferred to the Leptomerycidae from incertae sedis nized from the medial Miocene (late Hemingford- in the Cervidae. ian into Valentinian) deposits of New Mexico, The relationships between these late Lepto- Texas, and Nebraska. These late-surviving Lepto- merycidae and contemporaneous Blastomery- merycidae belong to the species Pseudoparablas- cinae are shown to be remote despite several tomeryx scotti and P. francescita, previously parallel features in common. Separation of the assigned to the Blastomerycinae. Likewise, Pro- family Leptomerycidae from the family Hyper- nodens silberlingi from Arikareean deposits in tragulidae is advocated. INTRODUCTION The small Oligocene traguloid, Leptomeryx additional evidence to support the Leptomeryci- evansi, is probably the most abundant ungulate dae as.a distinct family and to recognize the sur- in the vast collections of fossil vertebrates from vival of two leptomerycid genera into much the White River Badlands of South Dakota (Clark younger stages of the Miocene. -
Did Impacts, Volcanic Eruptions, Or Climate Change Affect Mammalian Evolution?
Palaeogeography, Palaeoclimatology, Palaeoecology 214 (2004) 283–294 www.elsevier.com/locate/palaeo Did impacts, volcanic eruptions, or climate change affect mammalian evolution? Donald R. Prothero* Department of Geology, Occidental College, Los Angeles, CA 90041, USA Received 30 June 2003; received in revised form 13 April 2004; accepted 20 April 2004 Abstract In recent years, it has become popular to attribute faunal change and mass extinction to impacts, volcanic eruptions, or climatic change. How well do these supposed causes compare to the excellent record of Cenozoic life, especially that of fossil mammals? Two different Cenozoic mammal diversity curves were compared, and important climatic, volcanic, and impact horizons were examined in detail. In no case is there a strong correlation between impacts, eruptions, or climatic events and any episode of mammalian turnover. On the contrary, most of the known impact, eruption, and climatic events of the Cenozoic occurred during intervals of faunal stability. Conversely, episodes of high turnover and faunal change among Cenozoic mammals correlate with no known extrinsic causes. Apparently, extrinsic environmental factors such as impacts, eruptions, and climate change have a minimal effect, and intrinsic biological factors must be more important. D 2004 Elsevier B.V. All rights reserved. Keywords: Cenozoic; Mammals; Evolution 1. Introduction events. Specifically, the impacts of the late Eocene were originally blamed for the Eocene–Oligocene Conventional Neo-Darwinian theory has long extinctions (Alvarez et al., 1982; Asaro et al., 1982), argued that species are well adapted to their environ- although later work has not substantiated this (Pro- ment and should respond with adaptation and evolu- thero, 1994). -
An Analysis of Anchitherine Equids Across the Eocene–Oligocene Boundary in the White River Group of the Western Great Plains
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Dissertations & Theses in Earth and Earth and Atmospheric Sciences, Department Atmospheric Sciences of 2010 An Analysis of Anchitherine Equids Across the Eocene–Oligocene Boundary in the White River Group of the Western Great Plains David M. Masciale University of Nebraska at Lincoln, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/geoscidiss Part of the Geology Commons, Paleobiology Commons, and the Paleontology Commons Masciale, David M., "An Analysis of Anchitherine Equids Across the Eocene–Oligocene Boundary in the White River Group of the Western Great Plains" (2010). Dissertations & Theses in Earth and Atmospheric Sciences. 11. https://digitalcommons.unl.edu/geoscidiss/11 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Dissertations & Theses in Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. AN ANALYSIS OF ANCHITHERINE EQUIDS ACROSS THE EOCENE– OLIGOCENE BOUNDARY IN THE WHITE RIVER GROUP OF THE WESTERN GREAT PLAINS by David M. Masciale A THESIS Presented to the Faculty of The Graduate College at the University of Nebraska In Partial Fulfillment of Requirements For the Degree of Master of Science Major: Geosciences Under the Supervision of Professors Ross Secord and Robert M. Hunt, Jr. Lincoln, NE April, 2010 AN ANALYSIS OF ANCHITHERINE EQUIDS ACROSS THE EOCENE– OLIGOCENE BOUNDARY IN THE WHITE RIVER GROUP OF THE WESTERN GREAT PLAINS David M. Masciale, M.S. University of Nebraska, 2010 Advisers: Ross Secord and Robert M. -
Liebe ID-Freunde
[Back to internetlibrary.html] Wolf-Ekkehard Lönnig 8 May 2007 (last update 16 October 2010), updates 27 Oct. 2007 with Appendix on Cameron & du Toit 2007: "Winning by a Neck…" pp .62-78; 5 Oct. 2008 some language corrections and a brief comment on Brown et al. 2007: "Extensive population genetic structure in the giraffe" on p. 79. The Evolution of the Long-Necked Giraffe (Giraffa camelopardalis L.) What do we really know? (Part 2) As for Part 1, see http://www.weloennig.de/Giraffe.pdf Some Questions, Facts and Quotations to Supplement Part 1 Repetitio est mater studiorum –Repetition is the best teacher (literally: the mother of studies) Summary Introduction: the story which is commonly taught in high schools about the evolution of the long- necked giraffe by natural selection (feeding-competition-hypothesis) fails to explain, among other things, the size differences between males and females. Giraffe cows are up to 1.5 meters shorter than the giraffe bulls, not to mention the offspring. The wide migration range of the giraffe and the low heights of the most common plants in their diet likewise argue against the dominant selection hypothesis. Now to the main points: 1) The fossil „links“, which according to the theory should appear successively and replace each other, usually exist simultaneously for long periods of time. 2) Evolutionary derivations based on similarities rely on circular reasoning (to refer once more to Kuhn's statement) 3) The giraffe has eight cervical vertebrae. Although the 8th vertebra displays almost all the characteristics of a neck vertebra, as an exception to the rule the first rib pair is attached there. -
Postulating Pressures 8Th Grade
Postulating Pressures 8th Grade Duration Concepts Pre-Visit: 30-50 minutes Natural Selection is the mechanism by which evolution occurs. Museum Visit: 60 minutes Genetic variation and environmental pressures are important parts of Post Visit: 50 minutes natural selection, and thus evolution. Location Evidence from geology, fossils and comparative anatomy provide the Age of Mammals Hall bases for the theory of evolution. Supplies Extinction of a species occurs when the environment changes and the characteristics of a species are insufficient for its survival. Worksheet Pencil Objectives Clipboard (optional) Students will formulate hypotheses about selection pressures on an Standards organism based on observations. NGSS MS-LS1-4, MS-LS2-1, MS-LS2 Students will research an organism to find if their hypotheses are -3, MS-LS4-1, MS-LS4-2, MS- supported by evidence. LS4-2, MS-LS4-4, LS4.A, LS4.B, LS4.C Students will choose a project in which they will use present and S+E Practices apply their research. 1, 2, 3, 4, 6, 7, 8 CCSS ELA Outline W.1.2.3.4.7.9, WHST.1.2.7.8.9, L.2 In one classroom session before visiting the Museum, review vocabulary and the concept of evolution by natural selection. Have CA State students select a mammal to focus on for their research paper and Writing Applications begin formulating hypotheses. 2.3.a.b.c.d Investigation and During a trip to the Museum, students will explore the Age of Experimentation 9.a Mammals hall and begin researching their animals natural history. Vocabulary Back in the classroom and or at home, students continue independent Evolution · Climate · research choose one project from the Task Sheet to showcase their Adaptation · Predator · findings. -
Changes in Mammalian Abundance Through the Eocene-Oligocene
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Dissertations & Theses in Earth and Atmospheric Earth and Atmospheric Sciences, Department of Sciences Summer 7-30-2019 Changes in Mammalian Abundance Through the Eocene-Oligocene Climate Transition in the White River Group of Nebraska, USA Robert Gillham University of Nebraska - Lincoln, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/geoscidiss Part of the Oceanography and Atmospheric Sciences and Meteorology Commons, Paleobiology Commons, and the Paleontology Commons Gillham, Robert, "Changes in Mammalian Abundance Through the Eocene-Oligocene Climate Transition in the White River Group of Nebraska, USA" (2019). Dissertations & Theses in Earth and Atmospheric Sciences. 120. https://digitalcommons.unl.edu/geoscidiss/120 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Dissertations & Theses in Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Changes in Mammalian Abundance Through the Eocene- Oligocene Climate Transition in the White River Group of Nebraska, USA By Robert B. Gillham A THESIS Presented to the Faculty of The Graduate College at the University of Nebraska In Partial Fulfillment of Requirements For the Degree of Master of Science Major: Geosciences Under the Supervision of Professor Ross Secord Lincoln, NE August, 2019 Changes in Mammalian Abundance Through the Eocene- Oligocene Climate Transition in the White River Group of Nebraska, USA Robert B. Gillham M.S. University of Nebraska, 2019 Advisor: Ross Secord Marine records show major cooling during the Eocene-Oligocene Climate Transition (EOCT).