Highly Specialized Suspension-Feeding Bony Fish
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Stratigraphy and Paleontology of Mid-Cretaceous Rocks in Minnesota and Contiguous Areas
Stratigraphy and Paleontology of Mid-Cretaceous Rocks in Minnesota and Contiguous Areas GEOLOGICAL SURVEY PROFESSIONAL PAPER 1253 Stratigraphy and Paleontology of Mid-Cretaceous Rocks in Minnesota and Contiguous Areas By WILLIAM A. COBBAN and E. A. MEREWETHER Molluscan Fossil Record from the Northeastern Part of the Upper Cretaceous Seaway, Western Interior By WILLIAM A. COBBAN Lower Upper Cretaceous Strata in Minnesota and Adjacent Areas-Time-Stratigraphic Correlations. and Structural Attitudes By E. A. M EREWETHER GEOLOGICAL SURVEY PROFESSIONAL PAPER 1 2 53 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1983 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Cobban, William Aubrey, 1916 Stratigraphy and paleontology of mid-Cretaceous rocks in Minnesota and contiguous areas. (Geological Survey Professional Paper 1253) Bibliography: 52 p. Supt. of Docs. no.: I 19.16 A. Molluscan fossil record from the northeastern part of the Upper Cretaceous seaway, Western Interior by William A. Cobban. B. Lower Upper Cretaceous strata in Minnesota and adjacent areas-time-stratigraphic correlations and structural attitudes by E. A. Merewether. I. Mollusks, Fossil-Middle West. 2. Geology, Stratigraphic-Cretaceous. 3. Geology-Middle West. 4. Paleontology-Cretaceous. 5. Paleontology-Middle West. I. Merewether, E. A. (Edward Allen), 1930. II. Title. III. Series. QE687.C6 551.7'7'09776 81--607803 AACR2 For sale by the Distribution Branch, U.S. -
High-Resolution Correlation of the Upper Cretaceous Stratigraphy Between the Book Cliffs and the Western Henry Mountains Syncline, Utah, U.S.A
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Dissertations & Theses in Earth and Atmospheric Earth and Atmospheric Sciences, Department of Sciences 5-2012 HIGH-RESOLUTION CORRELATION OF THE UPPER CRETACEOUS STRATIGRAPHY BETWEEN THE BOOK CLIFFS AND THE WESTERN HENRY MOUNTAINS SYNCLINE, UTAH, U.S.A. Drew L. Seymour University of Nebraska, [email protected] Follow this and additional works at: http://digitalcommons.unl.edu/geoscidiss Part of the Geology Commons, Sedimentology Commons, and the Stratigraphy Commons Seymour, Drew L., "HIGH-RESOLUTION CORRELATION OF THE UPPER CRETACEOUS STRATIGRAPHY BETWEEN THE BOOK CLIFFS AND THE WESTERN HENRY MOUNTAINS SYNCLINE, UTAH, U.S.A." (2012). Dissertations & Theses in Earth and Atmospheric Sciences. 88. http://digitalcommons.unl.edu/geoscidiss/88 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. HIGH-RESOLUTION CORRELATION OF THE UPPER CRETACEOUS STRATIGRAPHY BETWEEN THE BOOK CLIFFS AND THE WESTERN HENRY MOUNTAINS SYNCLINE, UTAH, U.S.A. By Drew L. Seymour A THESIS Presented to the Faculty of The Graduate College at the University of Nebraska In Partial Fulfillment of Requirements For Degree of Master of Science Major: Earth and Atmospheric Sciences Under the Supervision of Professor Christopher R. Fielding Lincoln, NE May, 2012 HIGH-RESOLUTION CORRELATION OF THE UPPER CRETACEOUS STRATIGRAPHY BETWEEN THE BOOK CLIFFS AND THE WESTERN HENRY MOUNTAINS SYNCLINE, UTAH. U.S.A. Drew L. Seymour, M.S. -
Annotated Checklist of Fossil Fishes from the Smoky Hill Chalk of the Niobrara Chalk (Upper Cretaceous) in Kansas
Lucas, S. G. and Sullivan, R.M., eds., 2006, Late Cretaceous vertebrates from the Western Interior. New Mexico Museum of Natural History and Science Bulletin 35. 193 ANNOTATED CHECKLIST OF FOSSIL FISHES FROM THE SMOKY HILL CHALK OF THE NIOBRARA CHALK (UPPER CRETACEOUS) IN KANSAS KENSHU SHIMADA1 AND CHRISTOPHER FIELITZ2 1Environmental Science Program and Department of Biological Sciences, DePaul University,2325 North Clifton Avenue, Chicago, Illinois 60614; and Sternberg Museum of Natural History, Fort Hays State University, 3000 Sternberg Drive, Hays, Kansas 67601;2Department of Biology, Emory & Henry College, P.O. Box 947, Emory, Virginia 24327 Abstract—The Smoky Hill Chalk Member of the Niobrara Chalk is an Upper Cretaceous marine deposit found in Kansas and adjacent states in North America. The rock, which was formed under the Western Interior Sea, has a long history of yielding spectacular fossil marine vertebrates, including fishes. Here, we present an annotated taxo- nomic list of fossil fishes (= non-tetrapod vertebrates) described from the Smoky Hill Chalk based on published records. Our study shows that there are a total of 643 referable paleoichthyological specimens from the Smoky Hill Chalk documented in literature of which 133 belong to chondrichthyans and 510 to osteichthyans. These 643 specimens support the occurrence of a minimum of 70 species, comprising at least 16 chondrichthyans and 54 osteichthyans. Of these 70 species, 44 are represented by type specimens from the Smoky Hill Chalk. However, it must be noted that the fossil record of Niobrara fishes shows evidence of preservation, collecting, and research biases, and that the paleofauna is a time-averaged assemblage over five million years of chalk deposition. -
Cryptoclidid Plesiosaurs (Sauropterygia, Plesiosauria) from the Upper Jurassic of the Atacama Desert
Journal of Vertebrate Paleontology ISSN: (Print) (Online) Journal homepage: https://www.tandfonline.com/loi/ujvp20 Cryptoclidid plesiosaurs (Sauropterygia, Plesiosauria) from the Upper Jurassic of the Atacama Desert Rodrigo A. Otero , Jhonatan Alarcón-Muñoz , Sergio Soto-Acuña , Jennyfer Rojas , Osvaldo Rojas & Héctor Ortíz To cite this article: Rodrigo A. Otero , Jhonatan Alarcón-Muñoz , Sergio Soto-Acuña , Jennyfer Rojas , Osvaldo Rojas & Héctor Ortíz (2020): Cryptoclidid plesiosaurs (Sauropterygia, Plesiosauria) from the Upper Jurassic of the Atacama Desert, Journal of Vertebrate Paleontology, DOI: 10.1080/02724634.2020.1764573 To link to this article: https://doi.org/10.1080/02724634.2020.1764573 View supplementary material Published online: 17 Jul 2020. Submit your article to this journal Article views: 153 View related articles View Crossmark data Full Terms & Conditions of access and use can be found at https://www.tandfonline.com/action/journalInformation?journalCode=ujvp20 Journal of Vertebrate Paleontology e1764573 (14 pages) © by the Society of Vertebrate Paleontology DOI: 10.1080/02724634.2020.1764573 ARTICLE CRYPTOCLIDID PLESIOSAURS (SAUROPTERYGIA, PLESIOSAURIA) FROM THE UPPER JURASSIC OF THE ATACAMA DESERT RODRIGO A. OTERO,*,1,2,3 JHONATAN ALARCÓN-MUÑOZ,1 SERGIO SOTO-ACUÑA,1 JENNYFER ROJAS,3 OSVALDO ROJAS,3 and HÉCTOR ORTÍZ4 1Red Paleontológica Universidad de Chile, Laboratorio de Ontogenia y Filogenia, Departamento de Biología, Facultad de Ciencias, Universidad de Chile, Las Palmeras 3425, Santiago, Chile, [email protected]; 2Consultora Paleosuchus Ltda., Huelén 165, Oficina C, Providencia, Santiago, Chile; 3Museo de Historia Natural y Cultural del Desierto de Atacama. Interior Parque El Loa s/n, Calama, Región de Antofagasta, Chile; 4Facultad de Ciencias Naturales y Oceanográficas, Universidad de Concepción, Barrio Universitario, Concepción, Región del Bío Bío, Chile ABSTRACT—This study presents the first plesiosaurs recovered from the Jurassic of the Atacama Desert that are informative at the genus level. -
Memorial to W.A. “Bill” Cobban (1916–2015) NEAL L
Memorial to W.A. “Bill” Cobban (1916–2015) NEAL L. LARSON Larson Paleontology Unlimited, LLC, Keystone, South Dakota 57745, USA; [email protected] NEIL H. LANDMAN American Museum of Natural History, Division of Paleontology (Invertebrates), New York, New York 10024, USA; [email protected] STEPHEN C. HOOK Atarque Geologic Consulting, LLC, Socorro, New Mexico 87810, USA; [email protected] Dr. W.A. “Bill” Cobban, one of the most highly re- spected, honored and published geologist-paleontologists of all time, passed away peacefully in his sleep in the morning of 21 April 2015 at the age of 98 in Lakewood, Colorado. Bill was an extraordinary field collector, geologist, stratigrapher, biostratigrapher, paleontologist, and mapmaker who spent nearly his entire life working for the U.S. Geo- logical Survey (USGS). In a career that spanned almost 75 years, he fundamentally changed our understanding of the Upper Cretaceous Western Interior through its fossils, making it known throughout the world. William Aubrey “Bill” Cobban was born in 1916 near Great Falls, Montana. As a teenager, he discovered a dinosaur in the Kootenai Formation catching the attention of Barnum Brown, premier dinosaur collector at the American Museum of Natural History, where the dinosaur now resides. A few years later, as Bill told, he read about the discovery of fossil bones in Shelby, Montana, during excavation of the Toole County Courthouse. The bones turned out to actually be baculites and other iridescent ammonites. These ammonites made such an impression on Bill they would change his life forever. He attended Montana State University in 1936, where he met a geology professor who encouraged an already developing love for geology and paleontology and received his B.S. -
Phylogeny, Diversity, and Ecology of the Ammonoid Superfamily Acanthoceratoidea Through the Cenomanian and Turonian
PHYLOGENY, DIVERSITY, AND ECOLOGY OF THE AMMONOID SUPERFAMILY ACANTHOCERATOIDEA THROUGH THE CENOMANIAN AND TURONIAN DAVID A.A. MERTZ A Thesis Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE August 2017 Committee: Margaret Yacobucci, Advisor Andrew Gregory Keith Mann © 2017 David Mertz All Rights Reserved iii ABSTRACT Margaret Yacobucci Both increased extinction and decreased origination, caused by rising oceanic anoxia and decreased provincialism, respectively, have been proposed as the cause of the Cenomanian Turonian (C/T) extinction event for ammonoids. Conflicting evidence exists for whether diversity actually dropped across the C/T. This study used the ammonoid superfamily Acanthoceratoidea as a proxy for ammonoids as a whole, particularly focusing on genera found in the Western Interior Seaway (WIS) of North America, including Texas. Ultimately, this study set out to determine 1) whether standing diversity decreased across the C/T boundary in the WIS, 2) whether decreased speciation or increased extinction in ammonoids led to a drop in diversity in the C/T extinction event, 3) how ecology of acanthoceratoid genera changed in relation to the C/T extinction event, and 4) whether these ecological changes indicate rising anoxia as the cause of the extinction. In answering these questions, three phylogenetic analyses were run that recovered the families Acanthoceratidae, Collignoniceratidae, and Vascoceratidae. Pseudotissotiidae was not recovered at all, while Coilopoceratidae was recovered but reclassified as a subfamily of Vascoceratidae. Seven genera were reclassified into new families and one genus into a new subfamily. After calibrating the trees with stratigraphy, I was able to determine that standing diversity dropped modestly across the C/T boundary and the Early/Middle Turonian boundary. -
Supporting Information
Supporting Information Clarke et al. 10.1073/pnas.1607237113 Major Axes of Shape Variation and Their Anatomical a comparison: the crown teleost vs. stem teleost comparison on Correlates molecular timescales. Here, the larger SL dataset delivers a All relative warp axes that individually account for >5% of the majority of trees where crown teleosts possess significantly variation across the species sampled are displayed in Table S3. higher rates than stem teleosts, whereas the CS and pruned SL Morphospaces derived from the first three axes, containing all datasets find this result in a large minority (Fig. S3). 398 Mesozoic neopterygian species in our shape dataset, are Overall, these results suggest that choice of size metric is presented in Fig. S1. Images of sampled fossil specimens are also relatively unimportant for our dataset, and that the overall size included in Fig. S1 to illustrate the anatomical correlates of and taxonomic samplings of the dataset are more likely to in- shape axes. The positions of major neopterygian clades in mor- fluence subsequent results, despite those factors having a rela- phospace are indicated by different colors in Fig. S2. Major tively small influence here. Nevertheless, choice of metric may be teleost clades are presented in Fig. S2A and major holostean important for other datasets (e.g., different groups of organisms clades in Fig. S2B. or datasets of other biological/nonbiological structures), because RW1 captures 42.53% of the variance, reflecting changes from it is possible to envisage scenarios where the choice of size metric slender-bodied taxa to deep-bodied taxa (Fig. S1 and Table S3). -
Large-Bodied Suspension Feeders, Which Include the Most
Friedman, M., Shimada, K., Martin, L.D., Everhart, M.J., Liston, J.J., Maltese, A. and Triebold, M. (2010) 100-million-year dynasty of giant planktivorous bony fishes in the Mesozoic seas. Science, 327 (5968). pp. 990-993. ISSN 0036-8075 http://eprints.gla.ac.uk/55074/ Deposited on: 7 December 2011 Enlighten – Research publications by members of the University of Glasgow http://eprints.gla.ac.uk 100-million-year dynasty of giant suspension-feeding bony fishes in the Mesozoic seas Matt Friedman1, Kenshu Shimada2,3, Larry D. Martin4, Michael J. Everhart3, Jeff Liston5, Anthony Maltese6, Michael Triebold6 1Department of Earth Sciences, University of Oxford, Parks Road, Oxford OX1 3PR, UK. 2Environmental Science Program and Department of Biological Sciences, DePaul University, 2325 North Clifton Avenue, Chicago, Illinois 60614, USA. 3Sternberg Museum of Natural History, Fort Hays State University, 3000 Sternberg Drive, Hays, Kansas 67601, USA. 4Natural History Museum and Biodiversity Research Center, University of Kansas, 1345 Jayhawk Boulevard, Lawrence, Kansas 66045, USA. 5Division of Ecology and Evolutionary Biology, Faculty of Biomedical and Life Sciences, University of Glasgow, University Avenue, Glasgow G12 8QQ, UK. 6Triebold Paleontology, Inc., and Rocky Mountain Dinosaur Resource Center, 201 South Fairview Street, Woodland Park, Colorado 80863, USA. Large-bodied suspension feeders (planktivores), which include the most massive animals to have ever lived, are conspicuously absent from Mesozoic marine environments. The only clear representatives of this trophic guild in the Mesozoic are an enigmatic and apparently short-lived (ca. 20 Ma) radiation of bony fishes assigned to †Pachycormidae, a stem teleost clade. Here we report several new discoveries of these giant fishes from Asia, Europe and North America, which not only deliver the first detailed anatomical information on this poorly understood group, but also extend its range deeper into the Jurassic and to the very end of the Cretaceous. -
Belemnites of the Bohemian Cretaceous Basin in a Global Context
Acta Geologica Polonica, Vol. 54 (2004), No.4, pp. 511-533 Belemnites of the Bohemian Cretaceous Basin in a global context MARTIN KOStAKl, STANISLAV CECH2, BORIS EKRT3, MARTIN MAZUCHl, FRANK WIESE4, SILKE VOIGTs, CHRISTOPHER J. WOOD6 lInstitute of Geology and Palaeontology, Charles University, Albertov 6, Prague 2, 12843, Czech Republic, E-mail: kostak@natw:[email protected] 2Czech Geological Swvey, Kldrov 3, 11821, Czech Republic, E-mail: [email protected] 3National Museum, Vdclavske namest! 68, Prague 1,11579, Czech Republic, E-mail: [email protected] 4Fachlichtung Palaontologie, FU Berlin, Malteserstl: 74-100, D-12249 Berlin, GClmany, E-mail: [email protected] 5 Geological Institute, University of Cologne, Zulpicher StI: 49a, D-50764 Cologne, Gelmany, E-mail: [email protected] 631 Periton Lane, Minehead, Somerset, TA24 SAQ, UK, [email protected] ABSTRACT: KostAK, M., QCH, S., EKRT, E., MAzUCH, M., WIESE, F., VOIGT, S. & WOOD, C.l 2004. Belemnites of the Bohemian Cretaceous Basin in a global context. Acta Geologica Polonica, 54 (4), 511-533. Warszawa. Belemnites occur infrequently from the Upper Cenomanian through the Middle/Upper Coniacian in the Bohemian Cretaceous. Four species of the family Belemnitellidae PAVLOW, 1914 have been described so far. A typical boreal fau nal incursion, represented by belemnites, happened five to six times in the Bohemian Cretaceous Basin (BCB). Praeactinocamax plenus immigrated during the Late Cenomanian Metoicoceras geslinianum ammonite Zone (plenus Event); there were two short-term incursions of P. bohemicus in the Late Turonian (Subplionocyclus neptuni to Plionocyclus gelmali ammonite zones) and an incursion of Goniocamax lundgreni in the late Early Coniacian (below and intra-Cremnoceramus crassus inoceramid Zone). -
Re-Evaluation of Pachycormid Fishes from the Late Jurassic of Southwestern Germany
Editors' choice Re-evaluation of pachycormid fishes from the Late Jurassic of Southwestern Germany ERIN E. MAXWELL, PAUL H. LAMBERS, ADRIANA LÓPEZ-ARBARELLO, and GÜNTER SCHWEIGERT Maxwell, E.E., Lambers, P.H., López-Arbarello, A., and Schweigert G. 2020. Re-evaluation of pachycormid fishes from the Late Jurassic of Southwestern Germany. Acta Palaeontologica Polonica 65 (3): 429–453. Pachycormidae is an extinct group of Mesozoic fishes that exhibits extensive body size and shape disparity. The Late Jurassic record of the group is dominated by fossils from the lithographic limestone of Bavaria, Germany that, although complete and articulated, are not well characterized anatomically. In addition, stratigraphic and geographical provenance are often only approximately known, making these taxa difficult to place in a global biogeographical context. In contrast, the late Kimmeridgian Nusplingen Plattenkalk of Baden-Württemberg is a well-constrained locality yielding hundreds of exceptionally preserved and prepared vertebrate fossils. Pachycormid fishes are rare, but these finds have the potential to broaden our understanding of anatomical variation within this group, as well as provide new information regarding the trophic complexity of the Nusplingen lagoonal ecosystem. Here, we review the fossil record of Pachycormidae from Nusplingen, including one fragmentary and two relatively complete skulls, a largely complete fish, and a fragment of a caudal fin. These finds can be referred to three taxa: Orthocormus sp., Hypsocormus posterodorsalis sp. nov., and Simocormus macrolepidotus gen. et sp. nov. The latter taxon was erected to replace “Hypsocormus” macrodon, here considered to be a nomen dubium. Hypsocormus posterodorsalis is known only from Nusplingen, and is characterized by teeth lacking apicobasal ridging at the bases, a dorsal fin positioned opposite the anterior edge of the anal fin, and a hypural plate consisting of a fused parhypural and hypurals. -
Fossil Fish Fauna from the Uppermost Graneros Shale (Upper Cretaceous) in Southeastern Nebraska
DePaul Discoveries Volume 1 Issue 1 Article 7 2012 Fossil Fish Fauna from the Uppermost Graneros Shale (Upper Cretaceous) in Southeastern Nebraska Kevin R. Jansen DePaul University, [email protected] Follow this and additional works at: https://via.library.depaul.edu/depaul-disc Part of the Life Sciences Commons, and the Physical Sciences and Mathematics Commons Recommended Citation Jansen, Kevin R. (2012) "Fossil Fish Fauna from the Uppermost Graneros Shale (Upper Cretaceous) in Southeastern Nebraska," DePaul Discoveries: Vol. 1 : Iss. 1 , Article 7. Available at: https://via.library.depaul.edu/depaul-disc/vol1/iss1/7 This Article is brought to you for free and open access by the College of Science and Health at Via Sapientiae. It has been accepted for inclusion in DePaul Discoveries by an authorized editor of Via Sapientiae. For more information, please contact [email protected]. Fossil Fish Fauna from the Uppermost Graneros Shale (Upper Cretaceous) in Southeastern Nebraska Acknowledgements Faculty Advisor: Dr. Kenshu Shimada, Department of Environmental Science and Studies & Department of Biological Sciences This article is available in DePaul Discoveries: https://via.library.depaul.edu/depaul-disc/vol1/iss1/7 Jansen: Fossil Fish Fauna from the Uppermost Graneros Shale (Upper Cretaceous) in Southeastern Nebraska DEPAUL DISCOVERIES (2O12) Fossil Fish Fauna from the Uppermost Graneros Shale (Upper Cretaceous) in Southeastern Nebraska Kevin R. Jansen* Department of Environmental Science and Studies ABSTRACT The Graneros Shale is a rock deposited in the Late Cretaceous Western Interior Seaway of North America about 95 million years ago. Many fossil fish remains were collected from the uppermost portion of the Graneros Shale in southeastern Nebraska and were analyzed for their unique characteristics. -
A Synoptic Review of the Vertebrate Fauna from the “Green Series
A synoptic review of the vertebrate fauna from the “Green Series” (Toarcian) of northeastern Germany with descriptions of new taxa: A contribution to the knowledge of Early Jurassic vertebrate palaeobiodiversity patterns I n a u g u r a l d i s s e r t a t i o n zur Erlangung des akademischen Grades eines Doktors der Naturwissenschaften (Dr. rer. nat.) der Mathematisch-Naturwissenschaftlichen Fakultät der Ernst-Moritz-Arndt-Universität Greifswald vorgelegt von Sebastian Stumpf geboren am 9. Oktober 1986 in Berlin-Hellersdorf Greifswald, Februar 2017 Dekan: Prof. Dr. Werner Weitschies 1. Gutachter: Prof. Dr. Ingelore Hinz-Schallreuter 2. Gutachter: Prof. Dr. Paul Martin Sander Tag des Promotionskolloquiums: 22. Juni 2017 2 Content 1. Introduction .................................................................................................................................. 4 2. Geological and Stratigraphic Framework .................................................................................... 5 3. Material and Methods ................................................................................................................... 8 4. Results and Conclusions ............................................................................................................... 9 4.1 Dinosaurs .................................................................................................................................. 10 4.2 Marine Reptiles .......................................................................................................................