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The Origin and Early Evolution of Dinosaurs
Biol. Rev. (2010), 85, pp. 55–110. 55 doi:10.1111/j.1469-185X.2009.00094.x The origin and early evolution of dinosaurs Max C. Langer1∗,MartinD.Ezcurra2, Jonathas S. Bittencourt1 and Fernando E. Novas2,3 1Departamento de Biologia, FFCLRP, Universidade de S˜ao Paulo; Av. Bandeirantes 3900, Ribeir˜ao Preto-SP, Brazil 2Laboratorio de Anatomia Comparada y Evoluci´on de los Vertebrados, Museo Argentino de Ciencias Naturales ‘‘Bernardino Rivadavia’’, Avda. Angel Gallardo 470, Cdad. de Buenos Aires, Argentina 3CONICET (Consejo Nacional de Investigaciones Cient´ıficas y T´ecnicas); Avda. Rivadavia 1917 - Cdad. de Buenos Aires, Argentina (Received 28 November 2008; revised 09 July 2009; accepted 14 July 2009) ABSTRACT The oldest unequivocal records of Dinosauria were unearthed from Late Triassic rocks (approximately 230 Ma) accumulated over extensional rift basins in southwestern Pangea. The better known of these are Herrerasaurus ischigualastensis, Pisanosaurus mertii, Eoraptor lunensis,andPanphagia protos from the Ischigualasto Formation, Argentina, and Staurikosaurus pricei and Saturnalia tupiniquim from the Santa Maria Formation, Brazil. No uncontroversial dinosaur body fossils are known from older strata, but the Middle Triassic origin of the lineage may be inferred from both the footprint record and its sister-group relation to Ladinian basal dinosauromorphs. These include the typical Marasuchus lilloensis, more basal forms such as Lagerpeton and Dromomeron, as well as silesaurids: a possibly monophyletic group composed of Mid-Late Triassic forms that may represent immediate sister taxa to dinosaurs. The first phylogenetic definition to fit the current understanding of Dinosauria as a node-based taxon solely composed of mutually exclusive Saurischia and Ornithischia was given as ‘‘all descendants of the most recent common ancestor of birds and Triceratops’’. -
A Re-Evaluation of the Enigmatic Dinosauriform Caseosaurus Crosbyensis from the Late Triassic of Texas, USA and Its Implications for Early Dinosaur Evolution
A re-evaluation of the enigmatic dinosauriform Caseosaurus crosbyensis from the Late Triassic of Texas, USA and its implications for early dinosaur evolution MATTHEW G. BARON and MEGAN E. WILLIAMS Baron, M.G. and Williams, M.E. 2018. A re-evaluation of the enigmatic dinosauriform Caseosaurus crosbyensis from the Late Triassic of Texas, USA and its implications for early dinosaur evolution. Acta Palaeontologica Polonica 63 (1): 129–145. The holotype specimen of the Late Triassic dinosauriform Caseosaurus crosbyensis is redescribed and evaluated phylogenetically for the first time, providing new anatomical information and data on the earliest dinosaurs and their evolution within the dinosauromorph lineage. Historically, Caseosaurus crosbyensis has been considered to represent an early saurischian dinosaur, and often a herrerasaur. More recent work on Triassic dinosaurs has cast doubt over its supposed dinosaurian affinities and uncertainty about particular features in the holotype and only known specimen has led to the species being regarded as a dinosauriform of indeterminate position. Here, we present a new diagnosis for Caseosaurus crosbyensis and refer additional material to the taxon—a partial right ilium from Snyder Quarry. Our com- parisons and phylogenetic analyses suggest that Caseosaurus crosbyensis belongs in a clade with herrerasaurs and that this clade is the sister taxon of Dinosauria, rather than positioned within it. This result, along with other recent analyses of early dinosaurs, pulls apart what remains of the “traditional” group of dinosaurs collectively termed saurischians into a polyphyletic assemblage and implies that Dinosauria should be regarded as composed exclusively of Ornithoscelida (Ornithischia + Theropoda) and Sauropodomorpha. In addition, our analysis recovers the enigmatic European taxon Saltopus elginensis among herrerasaurs for the first time. -
Attachment J Assessment of Existing Paleontologic Data Along with Field Survey Results for the Jonah Field
Attachment J Assessment of Existing Paleontologic Data Along with Field Survey Results for the Jonah Field June 12, 2007 ABSTRACT This is compilation of a technical analysis of existing paleontological data and a limited, selective paleontological field survey of the geologic bedrock formations that will be impacted on Federal lands by construction associated with energy development in the Jonah Field, Sublette County, Wyoming. The field survey was done on approximately 20% of the field, primarily where good bedrock was exposed or where there were existing, debris piles from recent construction. Some potentially rich areas were inaccessible due to biological restrictions. Heavily vegetated areas were not examined. All locality data are compiled in the separate confidential appendix D. Uinta Paleontological Associates Inc. was contracted to do this work through EnCana Oil & Gas Inc. In addition BP and Ultra Resources are partners in this project as they also have holdings in the Jonah Field. For this project, we reviewed a variety of geologic maps for the area (approximately 47 sections); none of maps have a scale better than 1:100,000. The Wyoming 1:500,000 geology map (Love and Christiansen, 1985) reveals two Eocene geologic formations with four members mapped within or near the Jonah Field (Wasatch – Alkali Creek and Main Body; Green River – Laney and Wilkins Peak members). In addition, Winterfeld’s 1997 paleontology report for the proposed Jonah Field II Project was reviewed carefully. After considerable review of the literature and museum data, it became obvious that the portion of the mapped Alkali Creek Member in the Jonah Field is probably misinterpreted. -
The Origin and Biogeographic Diversification of Fishes in the Family Poeciliidae
RESEARCH ARTICLE The origin and biogeographic diversification of fishes in the family Poeciliidae David N. Reznick1*, Andrew I. Furness2, Robert W. Meredith3, Mark S. Springer1 1 Department of Biology, University of California Riverside, Riverside, California, United States of America, 2 Department of Ecology and Evolutionary Biology, University of California Irvine, Irvine, California, United States of America, 3 Department of Biology and Molecular Biology, Montclair State University, Montclair, New Jersey, United States of America * [email protected] a1111111111 a1111111111 a1111111111 Abstract a1111111111 a1111111111 The fish subfamily Poeciliinae (sensu Parenti, 1981) is widely distributed across the West- ern Hemisphere and a dominant component of the fish communities of Central America. Poeciliids have figured prominently in previous studies on the roles of dispersal and vicari- ance in shaping current geographic distributions. Most recently, Hrbek et al. combined a OPEN ACCESS DNA-based phylogeny of the family with geological models to provide a biogeographic per- spective that emphasized the role of both vicariance and dispersal. Here we expand on that Citation: Reznick DN, Furness AI, Meredith RW, Springer MS (2017) The origin and biogeographic effort with a database enlarged in the quantity of sequence represented per species, in the diversification of fishes in the family Poeciliidae. number of species included, and in an enlarged and more balanced representation of the PLoS ONE 12(3): e0172546. doi:10.1371/journal. order Cyprinodontiformes. We combine a robust timetree based upon multiple fossil calibra- pone.0172546 tions with enhanced biogeographic analyses that include ancestral area reconstructions to Editor: Axel Meyer, University of Konstanz, provide a detailed biogeographic history of this clade. -
The Origin of Birds
The Origin of Birds Birds have many unusual synapomorphies among modern animals: [ Synapomorphies (shared derived characters), representing new specializations evolved in the most recent common ancestor of the ingroup] • Feathers • Warm-blooded (also in mammals) • Specialized lungs & air-sacs • Hollow bones • Toothless beaks • Large brain Technical name for birds is Aves, and “avian” means “of or concerning birds”. • Cervicals very different from dorsals, allowing neck to fold into “S”-shape • Backwards-pointing pubis • Synsacrum (sacrum fused to pelves; pelvic bones • Fibula reduced to proximal splint fused together) • Astragalus & calcaneum fused to tibia • Proximal caudals very mobile • Hinge-like ankle joint • Pygostyle (distal caudals all fused together) • Furcula - (the wishbone) • Tarsometatarsus (distal tarsals fused to • Forelimb very long, has become wing metatarsals; all metatarsals fused together) • Carpometacarpus (semilunate carpal block fused • Main pedal digits II-IV to metacarpals; all metacarpals fused together) • Pedal digit I reversed, placed at bottom of • Three fingers, but digits all reduced so no unguals tarsometatarsus 1 Compare modern birds to their closest relatives, crocodilians • Difficult to find relatives using only modern animals (turtles have modified necks and toothless beaks, but otherwise very • different; bats fly and are warm-blooded, but are clearly mammals; etc.) • With discovery of fossils, other potential relations: pterosaurs had big brains, “S”- shaped neck, hinge-like foot, but wings are VERY different. • In 1859, Darwin published the Origin; some used birds as a counter-example against evolution, as there were apparently known transitional forms between birds and other vertebrates. In 1860, a feather (identical to modern birds' feathers) was found in the Solnhofen Lithographic Limestone of Bavaria, Germany: a Late Jurassic formation. -
The Lost World of Fossil Lake
Snapshots from Deep Time THE LOST WORLD of FOSSIL LAKE lance grande With photography by Lance Grande and John Weinstein The University of Chicago Press | Chicago and London Ray-Finned Fishes ( Superclass Actinopterygii) The vast majority of fossils that have been mined from the FBM over the last century and a half have been fossil ray-finned fishes, or actinopterygians. Literally millions of complete fossil ray-finned fish skeletons have been excavated from the FBM, the majority of which have been recovered in the last 30 years because of a post- 1970s boom in the number of commercial fossil operations. Almost all vertebrate fossils in the FBM are actinopterygian fishes, with perhaps 1 out of 2,500 being a stingray and 1 out of every 5,000 to 10,000 being a tetrapod. Some actinopterygian groups are still poorly understood be- cause of their great diversity. One such group is the spiny-rayed suborder Percoidei with over 3,200 living species (including perch, bass, sunfishes, and thousands of other species with pointed spines in their fins). Until the living percoid species are better known, ac- curate classification of the FBM percoids (†Mioplosus, †Priscacara, †Hypsiprisca, and undescribed percoid genera) will be unsatisfac- tory. 107 Length measurements given here for actinopterygians were made from the tip of the snout to the very end of the tail fin (= total length). The FBM actinop- terygian fishes presented below are as follows: Paddlefishes (Order Acipenseriformes, Family Polyodontidae) Paddlefishes are relatively rare in the FBM, represented by the species †Cros- sopholis magnicaudatus (fig. 48). †Crossopholis has a very long snout region, or “paddle.” Living paddlefishes are sometimes called “spoonbills,” “spoonies,” or even “spoonbill catfish.” The last of those common names is misleading because paddlefishes are not closely related to catfishes and are instead close relatives of sturgeons. -
Name-Bearing Fossil Type Specimens and Taxa Named from National Park Service Areas
Sullivan, R.M. and Lucas, S.G., eds., 2016, Fossil Record 5. New Mexico Museum of Natural History and Science Bulletin 73. 277 NAME-BEARING FOSSIL TYPE SPECIMENS AND TAXA NAMED FROM NATIONAL PARK SERVICE AREAS JUSTIN S. TWEET1, VINCENT L. SANTUCCI2 and H. GREGORY MCDONALD3 1Tweet Paleo-Consulting, 9149 79th Street S., Cottage Grove, MN 55016, -email: [email protected]; 2National Park Service, Geologic Resources Division, 1201 Eye Street, NW, Washington, D.C. 20005, -email: [email protected]; 3Bureau of Land Management, Utah State Office, 440 West 200 South, Suite 500, Salt Lake City, UT 84101: -email: [email protected] Abstract—More than 4850 species, subspecies, and varieties of fossil organisms have been named from specimens found within or potentially within National Park System area boundaries as of the date of this publication. These plants, invertebrates, vertebrates, ichnotaxa, and microfossils represent a diverse collection of organisms in terms of taxonomy, geologic time, and geographic distribution. In terms of the history of American paleontology, the type specimens found within NPS-managed lands, both historically and contemporary, reflect the birth and growth of the science of paleontology in the United States, with many eminent paleontologists among the contributors. Name-bearing type specimens, whether recovered before or after the establishment of a given park, are a notable component of paleontological resources and their documentation is a critical part of the NPS strategy for their management. In this article, name-bearing type specimens of fossil taxa are documented in association with at least 71 NPS administered areas and one former monument, now abolished. -
Curriculum Vitae
1 CURRICULUM VITAE NAME: SANKAR CHATTERJEE ADDRESS: Department of Geosciences Museum of Texas Tech University, MS/Box 43191 Lubbock, TX 79409-3191, USA. Phone: (806) 742-1986 Fax: (806) 742-1136 E-mail: [email protected] Website: http://www.gesc.ttu.edu/Fac_pages/chatterjee/ PERSONAL INFORMATION: Born: May 28, 1943, Calcutta, India. U. S. Citizen Married, two boys. PRESENT POSITION: Paul Whitfield Horn Professor of Geosciences and Museum Science; Curator of Paleontology and Director, Antarctic Research Center, Museum of Texas Tech University. EDUCATION: • B. S. in Geology Honors, First in First Class, Jadavpur University, 1962. • M. S. in Applied Geology, First in First Class, Jadavpur University, 1964. • Predoctoral Fellow, London University, 1967-68. • Ph. D. in Geology, Calcutta University, Calcutta, India, 1970. • Postdoctoral Fellow, Smithsonian Institution, 1977-78. ACADEMIC POSITIONS: • Honorary Professor, Indian Institute of Science Education and Research, Calcutta, India, 2010 – Present. • Visiting Professor, Indian Statistical Institute, Calcutta, India, 1996 - Present. • Paul Whitfield Horn Professor & Curator of Paleontology, Texas Tech University, 1994 - Present. • Visiting Professor, Tübingen University, Germany, summer, 1992. • Visiting Professor, Tübingen University, Germany, summer, 1991. • Professor & Curator of Paleontology, Texas Tech University, 1987-1994. • Associate Professor & Curator, Texas Tech University, 1984-87. • Assistant Professor & Curator of Paleontology, Texas Tech University, 1979-84. • Assistant -
Skeletal Completeness of the Non‐Avian Theropod Dinosaur Fossil
University of Birmingham Skeletal completeness of the non-avian theropod dinosaur fossil record Cashmore, Daniel; Butler, Richard DOI: 10.1111/pala.12436 License: Creative Commons: Attribution (CC BY) Document Version Publisher's PDF, also known as Version of record Citation for published version (Harvard): Cashmore, D & Butler, R 2019, 'Skeletal completeness of the non-avian theropod dinosaur fossil record', Palaeontology, vol. 62, no. 6, pp. 951-981. https://doi.org/10.1111/pala.12436 Link to publication on Research at Birmingham portal Publisher Rights Statement: Cashmore, D & Butler, R (2019), 'Skeletal completeness of the non-avian theropod dinosaur fossil record', Palaeontology, vol. 62, no. 6, pp. 951-981. © 2019 The Authors 2019. https://doi.org/10.1111/pala.12436 General rights Unless a licence is specified above, all rights (including copyright and moral rights) in this document are retained by the authors and/or the copyright holders. The express permission of the copyright holder must be obtained for any use of this material other than for purposes permitted by law. •Users may freely distribute the URL that is used to identify this publication. •Users may download and/or print one copy of the publication from the University of Birmingham research portal for the purpose of private study or non-commercial research. •User may use extracts from the document in line with the concept of ‘fair dealing’ under the Copyright, Designs and Patents Act 1988 (?) •Users may not further distribute the material nor use it for the purposes of commercial gain. Where a licence is displayed above, please note the terms and conditions of the licence govern your use of this document. -
Late Cretaceous Stratigraphy and Vertebrate Faunas of the Markagunt, Paunsaugunt, and Kaiparowits Plateaus, Southern Utah
GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association Volume 3 2016 LATE CRETACEOUS STRATIGRAPHY AND VERTEBRATE FAUNAS OF THE MARKAGUNT, PAUNSAUGUNT, AND KAIPAROWITS PLATEAUS, SOUTHERN UTAH Alan L. Titus, Jeffrey G. Eaton, and Joseph Sertich A Field Guide Prepared For SOCIETY OF VERTEBRATE PALEONTOLOGY Annual Meeting, October 26 – 29, 2016 Grand America Hotel Salt Lake City, Utah, USA Post-Meeting Field Trip October 30–November 1, 2016 © 2016 Utah Geological Association. All rights reserved. For permission to copy and distribute, see the following page or visit the UGA website at www.utahgeology.org for information. Email inquiries to [email protected]. GEOLOGY OF THE INTERMOUNTAIN WEST an open-access journal of the Utah Geological Association Volume 3 2016 Editors UGA Board Douglas A. Sprinkel Thomas C. Chidsey, Jr. 2016 President Bill Loughlin [email protected] 435.649.4005 Utah Geological Survey Utah Geological Survey 2016 President-Elect Paul Inkenbrandt [email protected] 801.537.3361 801.391.1977 801.537.3364 2016 Program Chair Andrew Rupke [email protected] 801.537.3366 [email protected] [email protected] 2016 Treasurer Robert Ressetar [email protected] 801.949.3312 2016 Secretary Tom Nicolaysen [email protected] 801.538.5360 Bart J. Kowallis Steven Schamel 2016 Past-President Jason Blake [email protected] 435.658.3423 Brigham Young University GeoX Consulting, Inc. 801.422.2467 801.583-1146 UGA Committees [email protected] [email protected] Education/Scholarship -
The Green River Formation of the West- Central United States: Flood Or Post- Flood? Michael J
Forum The Green River Formation of the west- central United States: Flood or post- Flood? Michael J. Oard and John H. Whitmore Many creationists believe the Genesis Flood was responsible for the bulk of sedimentary rocks and fossils. However, disagreements often arise in trying to determine where the Flood/post-Flood boundary should be placed in the stratigraphic record. This forum is a friendly exchange between two young-earth creationists who hold differing views on the origin of the Green River Formation (GRF). The authors have examined the rocks in the field together. Mike Oard will defend the thesis that the GRF was deposited in the Flood and John Whitmore will defend the thesis that it is a post-Flood lacustrine (lake) deposit. This paper outlines the geological setting of the GRF. he Green River Formation (GRF) outcrops local units, often confined to sub-basins. There are three Textensively in basins within the central Rocky main formations in the basin. The lowest is the Wasatch Mountains, west-central United States. It is not a continuous Formation, which is coarser grained and considered fluvial. formation, but consists of lithologically similar strata that In the Greater Green River Basin, the Wasatch underlies the occupy four major, separate basins exposed in south-west GRF, but it also occurs around the edges of the basin, where Wyoming and adjacent areas of north-east Utah and north- it laterally intertongues with the GRF. Overlying the GRF west Colorado (figure 1*). These basins, and their adjacent are the Bridger and Washakie Formations. They consist mountain ranges, formed (along with many other basins) mostly of volcanoclastic sediments and are thought to have during the Laramide orogeny in the late Cretaceous and early been deposited in fluvial and lacustrine settings. -
Synoptic Taxonomy of Major Fossil Groups
APPENDIX Synoptic Taxonomy of Major Fossil Groups Important fossil taxa are listed down to the lowest practical taxonomic level; in most cases, this will be the ordinal or subordinallevel. Abbreviated stratigraphic units in parentheses (e.g., UCamb-Ree) indicate maximum range known for the group; units followed by question marks are isolated occurrences followed generally by an interval with no known representatives. Taxa with ranges to "Ree" are extant. Data are extracted principally from Harland et al. (1967), Moore et al. (1956 et seq.), Sepkoski (1982), Romer (1966), Colbert (1980), Moy-Thomas and Miles (1971), Taylor (1981), and Brasier (1980). KINGDOM MONERA Class Ciliata (cont.) Order Spirotrichia (Tintinnida) (UOrd-Rec) DIVISION CYANOPHYTA ?Class [mertae sedis Order Chitinozoa (Proterozoic?, LOrd-UDev) Class Cyanophyceae Class Actinopoda Order Chroococcales (Archean-Rec) Subclass Radiolaria Order Nostocales (Archean-Ree) Order Polycystina Order Spongiostromales (Archean-Ree) Suborder Spumellaria (MCamb-Rec) Order Stigonematales (LDev-Rec) Suborder Nasselaria (Dev-Ree) Three minor orders KINGDOM ANIMALIA KINGDOM PROTISTA PHYLUM PORIFERA PHYLUM PROTOZOA Class Hexactinellida Order Amphidiscophora (Miss-Ree) Class Rhizopodea Order Hexactinosida (MTrias-Rec) Order Foraminiferida* Order Lyssacinosida (LCamb-Rec) Suborder Allogromiina (UCamb-Ree) Order Lychniscosida (UTrias-Rec) Suborder Textulariina (LCamb-Ree) Class Demospongia Suborder Fusulinina (Ord-Perm) Order Monaxonida (MCamb-Ree) Suborder Miliolina (Sil-Ree) Order Lithistida