Using the Price Equation to Quantify Species Selection and Other Macroevolutionary Forces in Cretaceous Molluscs

Total Page:16

File Type:pdf, Size:1020Kb

Using the Price Equation to Quantify Species Selection and Other Macroevolutionary Forces in Cretaceous Molluscs University of Calgary PRISM: University of Calgary's Digital Repository Graduate Studies The Vault: Electronic Theses and Dissertations 2019-08-12 Using the Price Equation to Quantify Species Selection and Other Macroevolutionary Forces in Cretaceous Molluscs Jordan, Katherine J. Jordan, K. J. (2019). Using the Price Equation to Quantify Species Selection and Other Macroevolutionary Forces in Cretaceous Molluscs (Unpublished master's thesis). University of Calgary, Calgary, AB. http://hdl.handle.net/1880/110722 master thesis University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Downloaded from PRISM: https://prism.ucalgary.ca UNIVERSITY OF CALGARY Using the Price Equation to Quantify Species Selection and Other Macroevolutionary Forces in Cretaceous Molluscs by Katherine J. Jordan A THESIS SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE GRADUATE PROGRAM IN BIOLOGICAL SCIENCES CALGARY, ALBERTA AUGUST, 2019 © Katherine J. Jordan 2019 Abstract Species selection and other macroevolutionary forces are challenging processes to study and quantify when using fossil data. Here, I used the Price equation to analyze changes in geographic range sizes prior to and during a mass extinction event to estimate the relative contribution of three macroevolutionary processes (species selection, anagenesis, and immigration). I also tested the hypothesis that larger geographic range size increases a group’s survivability during mass extinctions. I applied a similar method to Rankin et al. (2015) to study marine gastropods and bivalves of the Gulf and Atlantic Coastal Plain (originally studied by Jablonski (1987)) over the last 16 million years of the Cretaceous Period. I found three major changes in mean geographic range size shared by both gastropods and bivalves during the end- Cretaceous: an increase in mean range size during the late Campanian, a decrease in the mid- Maastrichtian, and an increase near the end of the Cretaceous Period (late Maastrichtian). The Price Equation indicates that the late Campanian increase in geographic range size was attributable primarily to immigration, the mid-Maastrichtian decrease was due to different combinations of the three processes (species selection, anagenetic change, and immigration) in gastropods and bivalves, and the late Maastrichtian increase was attributable to species selection. These changes in geographic range size coincide with a marine transgression event, a period of global climate change, and a marine regression event, respectively. A statistically significant correlation between larger geographic range size and increased survivability was found for one time increment (approximately four million years before the KPg boundary). This study shows that the relative contribution of interacting macroevolutionary processes fluctuated over the end- Cretaceous extinction event and suggests that large geographic range size can increase survivability under certain conditions leading up to a mass extinction. ii Keywords: species selection, anagenetic change, immigration, the Price equation, macroevolution, mass extinction. iii Acknowledgements I would like to start with an acknowledgement to those who have helped me in my professional development. A heartfelt thank you is much overdue to my advisor Dr. Jeremy Fox whose patience and kindness have gotten me to this point. I am appreciative of every bit of advice, cooking, and funding I have received as member of his lab. I hope that my hard work and future success will be the biggest demonstration of my thanks, Jeremy. I would also like to thank Dr. Jessica Theodor for being the role model I needed. Her strength and passion are inspiring. I am grateful for all the work she has done to help me become the paleontologist I dreamed I could be. A thank you to Dr. Mindi Summers and Dr. Charles Henderson, as well, for enhancing my invertebrate knowledge to make this thesis possible. To my twin sister, Rebecca: Her wisdom and love have helped me immensely. I am so glad you are my sister. To my undergraduate professor Dr. Brian Penney: It was Dr. Penney who found out about the graduate opportunity here in Calgary. In a way, I hope I have carried on his legacy by attending graduate school in Alberta as he did. Thank you so much, Dr. Penney. My friends here in Canada Selina, Colby, Rachel, and all the rest (from campus and Telus Spark): you all got me through and were more kind than I deserved at times. I appreciate you more than you will ever know. I would also like to extend my gratitude to my mother, Vicki, my partner, Aaron, my dearest friends, Caitlyn, Jess, and Matt. I am the best person I can be because of you all. Thank you for all your support in the last two years. I hope to make you all proud. iv Dedication This thesis is dedicated to my grandparents, Leroy and Dorothy Weed of Stonington, ME. Thank you for giving me a love of the ocean that has stayed with me and brought me, ironically, to the prairies of Alberta. v Table of Contents Abstract .............................................................................................................................. ii Acknowledgements .......................................................................................................... iv Dedication ...........................................................................................................................v Table of Contents ............................................................................................................. vi List of Tables and Equations ........................................................................................ viii List of Figures and Illustrations ..................................................................................... ix Epigraph .............................................................................................................................x CHAPTER ONE: INTRODUCTION ..............................................................................1 1.1: Macroevolution and the Price Equation………………………………………1 1.2: The Cretaceous Mass Extinction and Cretaceous Molluscs…………………10 CHAPTER TWO: METHODS ......................................................................................13 2.1: The Price Equation…………………………………………………………. 13 2.2: Dataset Selection and Preparation for Analysis……………………………. 16 CHAPTER THREE: RESULTS ....................................................................................22 3.1: The Price Equation Results………………………………………………….22 3.2: Statistical Analysis of Datasets……………………………………………. 26 3.3: Further Analysis of Datasets………………………………………………...27 CHAPTER FOUR: DISCUSSION .................................................................................29 4.1: Macroevolutionary Change Within Time Increment T2-T3………………...29 4.2: Macroevolutionary Change Within Time Increment T6-T7………………...30 4.3: Macroevolutionary Change Within Time Increment T7-T8………………...32 4.4: Periods of Macroevolutionary Stasis in the Data……………………………33 4.5: Differential Survivorship Among Cretaceous Molluscs…………………….35 4.6: Limitations of the Study……………………………………………….….... 38 CHAPTER FIVE: CONCLUSION ................................................................................41 REFERENCES .................................................................................................................43 APPENDIX 1: Table of gastropod ancestor-descendant pairs of the Gulf and Atlantic Coastal Plain. Species names and ranges from Hunt et al. (2005) Appendix B………………….51 APPENDIX 2: Table of bivalve ancestor-descendant pairs of the Gulf and Atlantic Coastal Plain. Species names and ranges from Hunt et al. (2005) Appendix B………………….57 APPENDIX 3: Species used in PAST biostratigraphy analysis. Species were used based on their occurrence and presence in the formations used in the study. Data collected from the Paleobiology Database (PBDB)………………………………………………………….62 APPENDIX 4: Results of the PAST unitary association analysis. Maximal cliques presented from the unitary associated output……………………………………………………….66 vi APPENDIX 5: Gastropod dataset arranged in time bin for Price equation analysis…….67 APPENDIX 6: Bivalve dataset arranged in time bin for Price equation analysis……….77 APPENDIX 7: Gastropod Price equation analysis by time increment. The title “n/a” is indicative of those descendants without ancestors (i.e. immigrants) ……………………………….84 APPENDIX 8: Bivalve Price equation analysis by time increment. The title “n/a” is indicative of those descendants without ancestors (i.e. immigrants) ……………………………….109 vii List of Tables and Equations Table 1: Results of Permutation Test for Each Time Increment. P values are reported. Null hypothesis: geographic range size and number of descendants left per time bin are independent of each other……………………………………………………………………………………25 Equation 1: Modified from Rankin et al. (2015) ………………………………………….... 13 Equation 2: The extended Price equation modified from Rankin et al. (2015), eq. 2.1………14 viii List of Figures and Illustrations Figure 1: Total mean geographic range size change (blue line) gives the Price Equation answer for the gastropod analysis. In comparison, the three separate
Recommended publications
  • 12/04 CURRICULUM VITAE Karl W
    12/04 CURRICULUM VITAE Karl W. Flessa Department of Geosciences University of Arizona Tucson, Arizona 85721 (520) 621-7336 FAX (520) 621-2672 [email protected] Personal Data Birth Date: August 3, 1946 Place of Birth: Nürnberg, Germany Citizenship: U.S.A. (since 1950) Education and Degrees Ph.D., Geological Sciences, 1973. Brown University, Providence, Rhode Island A.B., Geology, 1968. Lafayette College, Easton, Pennsylvania Principal Administrative Appointments Head, Department of Ecology and Evolutionary Biology, University of Arizona, 1997-1999 Project Director, Research Training Group: Analysis of Biological Diversification, 1992-1994 Program Director, National Science Foundation, 1988-1990 Director, University of Arizona Geology Field Camp; 1983, 1985-1988 Academic Appointments Fellow, Udall Center for Studies in Public Policy, 2002-2003 Professor of Geosciences, University of Arizona, 1987-present Professor of Ecology & Evolutionary Biology, University of Arizona, 1997-present Visiting Professor, Facultad de Ciencias Marinas, Universidad Autónoma de Baja California, Ensenada, México, 1999 Research Associate, Smithsonian Institution, 1988-1991 Associate Professor, University of Arizona; 1981-1987 Humboldt Fellow, Universität Tübingen, Germany, and University of Birmingham, U.K.; 1983- 1984 Research Associate, Arizona-Sonora Desert Museum; 1978-present Assistant Professor, University of Arizona; 1977-1981 Assistant Professor, State University of New York at Stony Brook; 1972-1977 Senior Assistant, Marine Biological Laboratory; 6/72-8/72 Lecturer, Case Western Reserve University; 1/71-6/71 Research Interests Current research interests focus on 1) the environmental history and conservation biology of the Colorado River Delta, 2) the taphonomy and paleoecology of Recent and Pleistocene invertebrates in the Gulf of California, 3) the quality of the fossil record, and 4) the biogeography of Recent bivalve mollusks.
    [Show full text]
  • Paleoecology of Late Cretaceous Methane Cold-Seeps of the Pierre Shale, South Dakota
    City University of New York (CUNY) CUNY Academic Works All Dissertations, Theses, and Capstone Projects Dissertations, Theses, and Capstone Projects 10-2014 Paleoecology of Late Cretaceous methane cold-seeps of the Pierre Shale, South Dakota Kimberly Cynthia Handle Graduate Center, City University of New York How does access to this work benefit ou?y Let us know! More information about this work at: https://academicworks.cuny.edu/gc_etds/355 Discover additional works at: https://academicworks.cuny.edu This work is made publicly available by the City University of New York (CUNY). Contact: [email protected] Paleoecology of Late Cretaceous methane cold-seeps of the Pierre Shale, South Dakota by Kimberly Cynthia Handle A dissertation submitted to the Graduate Faculty in Earth and Environmental Sciences in partial fulfillment of the requirements for the degree of Doctor of Philosophy, The City University of New York 2014 i © 2014 Kimberly Cynthia Handle All Rights Reserved ii This manuscript has been read and accepted for the Graduate Faculty in Earth and Environmental Sciences in satisfaction of the dissertation requirement for the degree of Doctor of Philosophy. Neil H. Landman____________________________ __________________ __________________________________________ Date Chair of Examining Committee Harold C. Connolly, Jr.___ ____________________ __________________ __________________________________________ Date Deputy - Executive Officer Supervising Committee Harold C. Connolly, Jr John A. Chamberlain Robert F. Rockwell The City University of New York iii ABSTRACT The Paleoecology of Late Cretaceous methane cold-seeps of the Pierre Shale, South Dakota By Kimberly Cynthia Handle Adviser: Neil H. Landman Most investigations of ancient methane seeps focus on either the geologic or paleontological aspects of these extreme environments.
    [Show full text]
  • PRISCUM the Newsletter of the Paleontological Society Volume 13, Number 2, Fall 2004
    PRISCUM The Newsletter of the Paleontological Society Volume 13, Number 2, Fall 2004 Paleontological PRESIDENT’S Society Officers COLUMN: Inside... President Treasurer’s Report 2 William I. Ausich WE NEED YOU! GSA Information 2 President-Elect by William I. Ausich Reviews of PS- David Bottjer Sponsored Sessions 3 Past-President Why are you a member of The Paleontology Portal 5 Patricia H. Kelley The Paleontological Society? In PS Lecture Program 6 Secretary the not too distance past, the Books for Review 9 Roger D. K. Thomas only way to receive a copy of the Journal of Book Reviews 9 Treasurer Paleontology and Paleobiology was to pay your dues Conference Announce- and belong to the Society. I suppose one could Mark E. Patzkowsky have borrowed a copy from a friend or wander over ments 14 JP Managing Editors to the library. However, this was probably done Ann (Nancy) F. Budd with a heavy burden of guilt. Now, as we move Christopher A. Brochu into the digital age of scientific journal publishing, Jonathan Adrain one can have copies of the Journal of Paleontology and Paleobiology transmitted right to your Paleobiology Editors computer. It actually may arrive faster than the Tomasz Baumiller U.S. mail, you do not have to pay anything, and Robyn Burnham you do not even have to walk over to the library. Philip Gingerich No need for shelf space, no hassle, no dues, no Program Coordinator guilt – isn’t the Web great? The Web is great, but the Society needs dues-paying members in order Mark A. Wilson to continue to publish in paper, digitally, or both.
    [Show full text]
  • Similarity of Mammalian Body Size Across the Taxonomic Hierarchy and Across Space and Time Felisa A
    University of New Mexico UNM Digital Repository Biology Faculty & Staff ubP lications Scholarly Communication - Departments 5-1-2004 Similarity of Mammalian Body Size across the Taxonomic Hierarchy and across Space and Time Felisa A. Smith James H. Brown John P. Haskell S. Kathleen Lyons John Alroy See next page for additional authors Follow this and additional works at: http://digitalrepository.unm.edu/biol_fsp Part of the Biology Commons Recommended Citation Smith, Felisa A.; James H. Brown; John P. Haskell; S. Kathleen Lyons; John Alroy; Eric L. Charnov; Tamar Dayan; Brian J. Enquist; S.K. Morgan Ernest; Elizabeth A. Hadly; David Jablonski; Kate E. Jones; Dawn M. Kaufman; Pablo A. Marquet; Brian A. Maurer; Karl J. Niklas; Warren P. Porter; Kaustuv Roy; Bruce Tiffney; and Michael R. Willig. "Similarity of Mammalian Body Size across the Taxonomic Hierarchy and across Space and Time." 163, 5 (2004). http://digitalrepository.unm.edu/biol_fsp/82 This Article is brought to you for free and open access by the Scholarly Communication - Departments at UNM Digital Repository. It has been accepted for inclusion in Biology Faculty & Staff ubP lications by an authorized administrator of UNM Digital Repository. For more information, please contact [email protected]. Authors Felisa A. Smith, James H. Brown, John P. Haskell, S. Kathleen Lyons, John Alroy, Eric L. Charnov, Tamar Dayan, Brian J. Enquist, S.K. Morgan Ernest, Elizabeth A. Hadly, David Jablonski, Kate E. Jones, Dawn M. Kaufman, Pablo A. Marquet, Brian A. Maurer, Karl J. Niklas, Warren P. Porter, Kaustuv Roy, Bruce Tiffney, and Michael R. Willig This article is available at UNM Digital Repository: http://digitalrepository.unm.edu/biol_fsp/82 vol.
    [Show full text]
  • The First Record of Agerostrea Ungulata (Von Schlotheim, 1813) (Bivalvia: Ostreoidea) from the Upper Maastrichtian of Kwazulu, S
    The first record of Agerostrea ungulata (von Schlotheim, 1813) (Bivalvia: Ostreoidea) from the Upper Maastrichtian of KwaZulu, South Africa, with a discussion of its distribution in southeast Africa and Madagascar Herbert Christian Klinger Natural History Collections Department, Iziko South African Museum, P.O. Box 61, Cape Town, 8000 South Africa E-mail: [email protected] & Department of Geological Sciences, University of Cape Town, Private Bag, Rondebosch, 7701 South Africa & Nikolaus Malchus Dept. de Geologia/Unitat Paleontologia, Universitat Autònoma de Barcelona, 08193 Bellaterra (Cerdanyola del Vallès), Catalonia, Spain E-mail: [email protected] (with 2 figures) Received 2 July 2007. Accepted 14 December 2007 Recent (2005) excavations for expansions to the harbour at Richards Bay, KwaZulu-Natal, South Africa, yielded a single specimen of the ostreid Agerostrea ungulata (von Schlotheim, 1813). This is the first, and thus far only, record of this species from the Upper Maastrichtian of South Africa. Its distribution in southeast Africa and Madagascar is discussed Key words: Cretaceous, Maastrichtian, Ostreoidea, South Africa. CONTENTS Abstract · · · · · · · · · · · · · · · · · · 11 Genus Agerostrea · · · · · · · · · · 11 and southeast Africa · · · · · · · 12 Introduction · · · · · · · · · · · · · · · 11 Agerostrea ungulata · · · · · · · · 11 Acknowledgements · · · · · · · · 15 Systematic palaeontology · · · 11 Distribution in Madagascar References· · · · · · · · · · · · · · · · 15 INTRODUCTION Genus Agerostrea Vyalov, 1936 Recent (2005) submarine excavations for expansion to the (Vyalov 1936, p. 20; Stenzel 1971, p. N1158; Malchus 1990, harbour at Richards Bay, KwaZulu-Natal, South Africa, p. 160). yielded new and additional invertebrate faunas that had not been found during previous excavations in 1997. The cepha- Type species lopods and nannofossils from the latter works were described Ostracites ungulatus von Schlotheim, 1813, p.
    [Show full text]
  • Bedrock Geology of Round Rock and Surrounding Areas, Williamson and Travis Counties, Texas
    Bedrock Geology of Round Rock and Surrounding Areas, Williamson and Travis Counties, Texas Todd B. Housh Bedrock Geology of Round Rock and Surrounding Areas, Williamson and Travis Counties, Texas Todd B. Housh Copyright 2007 Todd B Housh, PhD, PG Round Rock, TX 78664 Cover photograph: The “Round Rock,” an erosional pedestal of Edward’s limestone that marked the low‐water crossing of Brushy Creek by the Chisholm Trail. 2 Table of Contents Introduction 5 Tectonic History 6 Previous Studies 8 Other Geologic Constraints 9 Stratigraphy 9 Comanche Series Fredericksburg Group Walnut Formation 10 Comanche Peak 10 Edwards 12 Kiamichi 13 Washita Group Georgetown 14 Del Rio 15 Buda 16 Gulf Series Woodbine Group Pepper 16 Eagle Ford Group 17 Austin Group 19 Taylor Group 21 Tertiary and Quaternary Systems Plio‐Pleistocene to Recent 22 Structure 23 Acknowledgements 27 Bibliography 28 Appendix 1. Compilation of sources of other geologic information. 34 Appendix 2. Localities of note to observe important geologic 40 features in the Round Rock Area. Appendix 3. Checklist of Cretaceous and Pleistocene fossils 45 3 4 Bedrock Geology of Round Rock and Surrounding Areas, Williamson and Travis Counties, Texas Todd B. Housh Introduction The purpose of this study was to produce a map of the bedrock geology of the city of Round Rock, Texas and its environs and to evaluate the geologic structure of the area. Most of the City of Round Rock lies within the Round Rock 7.5 minute quadrangle, Williamson County, Texas1, although parts of the city also lie within the Pflugerville West 7.5 minute quadrangle, Travis County, Texas2 and the Hutto 7.5 minute quadrangle, Williamson County, Texas3.
    [Show full text]
  • Oyster Life Positions and Shell Beds from the Upper Jurassic of Poland
    Oyster life positions and shell beds from the Upper Jurassic of Poland MARCINMACHALSKI Machalski, M. 1998. Oyster life positions and shell beds from the Upper Jurassic of Poland. - Acta P alae ontologic a P olonica 43, 4, 609-634. Life positions of three oyster species, Actinostreon gregareun (J. Sowerby, 1816), Deltoideum delta (Smith,1817), and Nanogyra virgula (Defrance, 1820) from the Polish Upper Jurassic (Kimmeńdgian and Volgian) sequences' mainly from the parautochthon- ous shell beds, are reconstructed. The oysters reveal variation in morphology and/or settling behaviouą which is interpreted in terms of ecophenotypic response to the fluctuations in sedimentation rate and the softness of substrate.Both A. gregareum and 'choose' D. delta could between a mud-sticking and reclining mode of life. The latter sfrategy is manifested e.g., by a cup-shaped, Gryphaea-|kemorphoĘpe documented for the first time n D. delta. N. virgula was previously regarded as a cup-shaped recliner, but the collected material suggests that many specimens could live in a lateral position or form clusters composed of mutually attached specimens. Sedimentation rates during the oyster life cycles can be inferred from the reconstructed oyster life positions and ranged from approximately 7-I3 cmin the case of largest mud-sticking specimens to nil in flaq fan-shaped recliners. The oyster life habits can thus provide valuable insights into sedimentary and ecologic dynamics of oyster shell beds. T"heActinostreon beds origin- ated under dynamic bypassing conditions, whereas Deltoideum beds in a regime of starvation or total bypassing of sediment. In the case of the Nanogyra virgula beds, the evidence is ambiguous due to difficulties in reconsfructing the life attitude of many specimens of this species.
    [Show full text]
  • "Diversity of Life Through Time"
    Diversity of Life through Introductory article Time Article Contents . Diversification of Life Carl Simpson, Museum fu¨rNaturkunde,Berlin,Germany . Calibrating Global Diversity Trends . Patterns – Marine and Terrestrial Wolfgang Kiessling, Museum fu¨rNaturkunde,Berlin,Germany . What Causes Global-Scale Biotic Transitions? Based in part on the previous version of this Encyclopedia of Life Sciences . Limits to Diversity – Equilibrium and Expansion Models (ELS) article, Diversity of Life through Time by Arnold I Miller. Local and Regional Patterns . Sources of Biodiversity . Radiations Online posting date: 15th November 2010 Global diversity is the total number of taxa living in the biodiversity changes in the past will help us to understand present day or at any time in the geological past. Recon- fate of biodiversity in the face of human-induced changes structing the trajectory of global diversity by compiling to the planet. Many human-induced changes to the Earth data from the fossil record has been a major research have natural analogues in the geological past (e.g. intervals of global warming or ocean acidification); analyses of past agenda for palaeontologists for decades. The goal is to biodiversity during times of known environmental change produce an accurate reconstruction of the pattern of can help us predict how diversity will be affected by current global diversity that will ultimately allow us to under- environmental changes. Researchers seeking to determine stand the causes of diversity increases, decreases and whether the Earth is currently experiencing a mass extinc- transitions in the composition of the biota. The Paleo- tion of species have looked at the history of biodiversity biology Database, a new large-scale database based on for insights into levels of diversification and extinction individual collections of fossil taxa, allows palaeontolo- expected ‘naturally’, in a world not influenced unduly by gists to standardise sampling, thereby controlling for Homo sapiens.
    [Show full text]
  • Biostratigraphy, Paleogeography, and Paleoenvironments
    BIOSTRATIGRAPHY, PALEOGEOGRAPHY, AND PALEOENVIRONMENTS OF THE UPPER CRETACEOUS (CAMPANIAN) NORTHERN MISSISSIPPI EMBAYMENT by SANDY M. EBERSOLE A DISSERTATION Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Department of Geological Sciences in the Graduate School of The University of Alabama TUSCALOOSA, ALABAMA 2009 Copyright Sandy M. Ebersole 2009 ALL RIGHTS RESERVED ABSTRACT Most paleogeographic and paleoenvironmental reconstructions of the northern Mississippi Embayment during the Late Campanian (Late Cretaceous) illustrate a generalized gulf between central Mississippi and Arkansas stretching northward into southern Illinois. The most detailed reconstruction shows a large river flowing from the Appalachians to the northeastern edge of the gulf with a river delta covering most of the northern embayment and stretching from southern Illinois to west-central Alabama. Lack of age constraints, incorrect stratigraphic correlations, paucity of detailed geologic maps and subsurface data, and misunderstanding of the basin geometry have led to inaccurate or vague paleogeographic interpretations of the Upper Cretaceous northern Mississippi Embayment. This project correlates the marine and nonmarine biostratigraphy, identifies the upper Campanian lithofacies, interprets the paleoenvironment of each lithofacies, and maps these interpretations to create a paleogeographic model of the northern Mississippi Embayment during the Late Campanian. Biostratigraphic indicators used in this project include
    [Show full text]
  • UTILIZING the PALEOBIOLOGY DATABASE to PROVIDE EDUCATIONAL OPPORTUNITIES for UNDERGRADUATES Rowan Lockwood William and Mary Phoebe A
    Downloaded from https://www.cambridge.org/core. Williams College Library, on 01 Mar 2019 at 18:07:48, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/9781108681667 Downloaded from https://www.cambridge.org/core. Williams College Library, on 01 Mar 2019 at 18:07:48, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/9781108681667 Elements of Paleontology UTILIZING THE PALEOBIOLOGY DATABASE TO PROVIDE EDUCATIONAL OPPORTUNITIES FOR UNDERGRADUATES Rowan Lockwood William and Mary Phoebe A. Cohen Williams College Mark D. Uhen George Mason University Katherine Ryker University of South Carolina Downloaded from https://www.cambridge.org/core. Williams College Library, on 01 Mar 2019 at 18:07:48, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/9781108681667 University Printing House, Cambridge CB2 8BS, United Kingdom One Liberty Plaza, 20th Floor, New York, NY 10006, USA 477 Williamstown Road, Port Melbourne, VIC 3207, Australia 314–321, 3rd Floor, Plot 3, Splendor Forum, Jasola District Centre, New Delhi – 110025, India 79 Anson Road, #06–04/06, Singapore 079906 Cambridge University Press is part of the University of Cambridge. It furthers the University’s mission by disseminating knowledge in the pursuit of education, learning, and research at the highest international levels of excellence. www.cambridge.org Information on this title: www.cambridge.org/9781108717908 DOI: 10.1017/9781108681667 © The Paleontological Society 2018 This publication is in copyright.
    [Show full text]
  • Morphogenesis and Ecogenesis of Bivalves in the Phanerozoic
    Morphogenesis and Ecogenesis of Bivalves in the Phanerozoic L. A. Nevesskaja Paleontological Institute, Russian Academy of Sciences, Profsoyuznaya ul. 123, Moscow, 117997 Russia e-mail: [email protected] Received March 18, 2002 Contents Vol. 37, Suppl. 6, 2003 The supplement is published only in English by MAIK "Nauka/lnlerperiodica" (Russia). I’uleonlologicul Journal ISSN 003 I -0301. INTRODUCTION S59I CHAPTER I. MORPHOLOGY OF BIVALVES S593 (1) S true lure of the Soil Body S593 (2) Development of the Shell (by S.V. Popov) S597 (3) Shell Mierosluelure (by S.V. Popov) S598 (4) Shell Morphology S600 (5) Reproduetion and Ontogenelie Changes of the Soft Body and the Shell S606 CHAPTER II. SYSTEM OF BIVALVES S609 CHAPTER III. CHANGES IN THE TAXONOMIC COMPOSITION OF BIVALVES IN THE PHANEROZOIC S627 CHAPTER IV. DYNAMICS OF THE TAXONOMIC DIVERSITY OF BIVALVES IN THE PHANEROZOIC S631 CHAPTER V. MORPHOGENESIS OF BIVALVE SHELLS IN THE PHANEROZOIC S635 CHAPTER VI. ECOLOGY OF BIVALVES S644 (1) Faelors Responsible lor the Distribution of Bivalves S644 (a) Abiotic Factors S644 (b) Biotic Factors S645 (c) Environment and Composition of Benthos in Different Zones of the Sea S646 (2) Elhologieal-Trophie Groups of Bivalves and Their Distribution in the Phanerozoic S646 (a) Ethological-Trophic Groups S646 (b) Distribution of Ethological-Trophic Groups in Time S649 CHAPTER VII. RELATIONSHIPS BETWEEN THE SHELL MORPHOLOGY OF BIVALVES AND THEIR MODE OF LIFE S652 (1) Morphological Characters of the Shell Indicative of the Mode of Life, Their Appearance and Evolution S652 (2) Homeomorphy in Bivalves S654 CHAPTER VIII. MORPHOLOGICAL CHARACTERIZATION OF THE ETHOLOGICAL-TROPHIC GROUPS AND CHANGES IN THEIR TAXONOMIC COMPOSITION OVER TIME S654 (1) Morphological Characterization of Major Ethological-Trophic Groups S654 (2) Changes in the Taxonomic Composition of the Ethological-Trophic Groups in Time S657 CHAPTER IX.
    [Show full text]
  • Curriculum Vitae
    Carl Simpson 1 CU Museum of Natural History Phone (USA): +1 303-735-5323 University of Colorado, 265 UCB [email protected] Boulder, CO, 8039-0265 http://simpson-carl.github.io @simpson carl Current Position Assistant Professor, Department of Geological Sciences, University of Colorado, Boulder. Curator of Invertebrate Paleontology, CU Museum, University of Colorado, Boulder. Education Ph.D. Department of Geophysical Sciences, 2006 University of Chicago, Chicago, IL, USA B.A. College of Creative Studies (Biology), June 2000 University of California, Santa Barbara, CA, USA Professional Experience 2015 - 2016 Springer Fellow, Department of Paleobiology, National Museum of Natural History, Smithsonian Institution 2012-2015 Abbott Fellow, Department of Paleobiology, National Museum of Natural His- tory, Smithsonian Institution. 2012 Visiting Scholar, Cooperation and Evolution of Multicellularity program. Kavli In- stitute for Theoretical Physics. 2011 Visiting Scholar Fellowship, National Evolutionary Synthesis Center. 2008-2012 Postdoctoral Researcher, Museum f¨ur Naturkunde, Leibniz Institute for Evo- lution and Biodiversity at the Humbolt University, Berlin. 2006-2008 Research Associate, Department of Biology, Duke University. 2004 Research assistant for John Alroy, the Paleobiology Database, National Center for Ecological Analysis and Synthesis. 2001 Santa Fe Institute Complex Systems Summer School; Budapest, Hungary. 2001 Comparative Invertebrate Embryology. Friday Harbor Marine Laboratories. Fellowships & Grants • Springer Fellowship, \Quantifying the stochastic and deterministic aspects of macroevo- lution" Smithsonian Institution, National Museum of Natural History 2015-2016. • NSF ELT Collaborative Research: \Investigating the Biotic and Paleoclimatic Con- sequences of Dust in the Late Paleozoic." 2013-2017. with Gerilyn Soreghan, Linda Hinnov, Sarah Aciego, and Nicholas Heavens. • Abbott Postdoctoral Fellowship, \The Macroevolution of Bryozoan Polymorphism" Smithsonian Institution, National Museum of Natural History.
    [Show full text]