Using Models to Correct Data: Paleodiversity and the Fossil Record
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Benthic Foraminifera Across the Cretaceous/Paleogene Boundary in the Southern Ocean (ODP Site 690): Diversity, Food and Carbonate Saturation
Marine Micropaleontology 105 (2013) 40–51 Contents lists available at ScienceDirect Marine Micropaleontology journal homepage: www.elsevier.com/locate/marmicro Research paper Benthic foraminifera across the Cretaceous/Paleogene boundary in the Southern Ocean (ODP Site 690): Diversity, food and carbonate saturation Laia Alegret a,⁎, Ellen Thomas b,c a Departamento de Ciencias de la Tierra & Instituto Universitario de Investigación en Ciencias Ambientales de Aragón, Universidad de Zaragoza, Spain b Department of Geology and Geophysics, Yale University, USA c Department of Earth and Environmental Sciences, Wesleyan University, USA article info abstract Article history: The impact of an asteroid at the Cretaceous/Paleogene (K/Pg) boundary triggered dramatic biotic, biogeochem- Received 20 June 2013 ical and sedimentological changes in the oceans that have been intensively studied. Paleo-biogeographical Received in revised form 21 October 2013 differences in the biotic response to the impact and its environmental consequences, however, have been less Accepted 24 October 2013 well documented. We present a high-resolution analysis of benthic foraminiferal assemblages at Southern Ocean ODP Site 690 (Maud Rise, Weddell Sea, Antarctica). Keywords: At this high latitude site, late Maastrichtian environmental variability was high, but benthic foraminiferal assem- Cretaceous/Paleogene boundary fi benthic foraminifera blages were not less diverse than at lower latitudes, in contrast to those of planktic calci ers. Also in contrast to high southern latitudes planktic calcifiers, benthic foraminifera did not suffer significant extinction at the K/Pg boundary, but show export productivity transient assemblage changes and decreased diversity. At Site 690, the extinction rate was even lower (~3%) carbonate saturation than at other sites. -
The MBL Model and Stochastic Paleontology
216 Chapter seven ised exciting new avenues for research, that insights from biology and ecology could more profi tably be applied to paleontology, and that the future lay in assembling large databases as a foundation for analysis of broad-scale patterns of evolution over geological history. But in compar- ison to other expanding young disciplines—like theoretical ecology— paleobiology lacked a cohesive theoretical and methodological agenda. However, over the next ten years this would change dramatically. Chapter Seven One particular ecological/evolutionary issue emerged as the central unifying problem for paleobiology: the study and modeling of the his- “Towards a Nomothetic tory of diversity over time. This, in turn, motivated a methodological question: how reliable is the fossil record, and how can that reliability be Paleontology”: The MBL Model tested? These problems became the core of analytical paleobiology, and and Stochastic Paleontology represented a continuation and a consolidation of the themes we have examined thus far in the history of paleobiology. Ultimately, this focus led paleobiologists to groundbreaking quantitative studies of the inter- The Roots of Nomotheticism play of rates of origination and extinction of taxa through time, the role of background and mass extinctions in the history of life, the survivor- y the early 1970s, the paleobiology movement had begun to acquire ship of individual taxa, and the modeling of historical patterns of diver- Bconsiderable momentum. A number of paleobiologists began ac- sity. These questions became the central components of an emerging pa- tively building programs of paleobiological research and teaching at ma- leobiological theory of macroevolution, and by the mid 1980s formed the jor universities—Stephen Jay Gould at Harvard, Tom Schopf at the Uni- basis for paleobiologists’ claim to a seat at the “high table” of evolution- versity of Chicago, David Raup at the University of Rochester, James ary theory. -
A Framework for Post-Phylogenetic Systematics
A FRAMEWORK FOR POST-PHYLOGENETIC SYSTEMATICS Richard H. Zander Zetetic Publications, St. Louis Richard H. Zander Missouri Botanical Garden P.O. Box 299 St. Louis, MO 63166 [email protected] Zetetic Publications in St. Louis produces but does not sell this book. Any book dealer can obtain a copy for you through the usual channels. Resellers please contact CreateSpace Independent Publishing Platform of Amazon. ISBN-13: 978-1492220404 ISBN-10: 149222040X © Copyright 2013, all rights reserved. The image on the cover and title page is a stylized dendrogram of paraphyly (see Plate 1.1). This is, in macroevolutionary terms, an ancestral taxon of two (or more) species or of molecular strains of one taxon giving rise to a descendant taxon (unconnected comma) from one ancestral branch. The image on the back cover is a stylized dendrogram of two, genus-level speciational bursts or dis- silience. Here, the dissilient genus is the basic evolutionary unit (see Plate 13.1). This evolutionary model is evident in analysis of the moss Didymodon (Chapter 8) through superoptimization. A super- generative core species with a set of radiative, specialized descendant species in the stylized tree com- promises one genus. In this exemplary image; another genus of similar complexity is generated by the core supergenerative species of the first. TABLE OF CONTENTS Preface..................................................................................................................................................... 1 Acknowledgments.................................................................................................................................. -
What Really Happened in the Late Triassic?
Historical Biology, 1991, Vol. 5, pp. 263-278 © 1991 Harwood Academic Publishers, GmbH Reprints available directly from the publisher Printed in the United Kingdom Photocopying permitted by license only WHAT REALLY HAPPENED IN THE LATE TRIASSIC? MICHAEL J. BENTON Department of Geology, University of Bristol, Bristol, BS8 1RJ, U.K. (Received January 7, 1991) Major extinctions occurred both in the sea and on land during the Late Triassic in two major phases, in the middle to late Carnian and, 12-17 Myr later, at the Triassic-Jurassic boundary. Many recent reports have discounted the role of the earlier event, suggesting that it is (1) an artefact of a subsequent gap in the record, (2) a complex turnover phenomenon, or (3) local to Europe. These three views are disputed, with evidence from both the marine and terrestrial realms. New data on terrestrial tetrapods suggests that the late Carnian event was more important than the end-Triassic event. For tetrapods, the end-Triassic extinction was a whimper that was followed by the radiation of five families of dinosaurs and mammal- like reptiles, while the late Carnian event saw the disappearance of nine diverse families, and subsequent radiation of 13 families of turtles, crocodilomorphs, pterosaurs, dinosaurs, lepidosaurs and mammals. Also, for many groups of marine animals, the Carnian event marked a more significant turning point in diversification than did the end-Triassic event. KEY WORDS: Triassic, mass extinction, tetrapod, dinosaur, macroevolution, fauna. INTRODUCTION Most studies of mass extinction identify a major event in the Late Triassic, usually placed at the Triassic-Jurassic boundary. -
Low-Latitude Origins of the Four Phanerozoic Evolutionary Faunas
bioRxiv preprint doi: https://doi.org/10.1101/866186; this version posted December 6, 2019. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. Low-Latitude Origins of the Four Phanerozoic Evolutionary Faunas A. Rojas1*, J. Calatayud1, M. Kowalewski2, M. Neuman1, and M. Rosvall1 1Integrated Science Lab, Department of Physics, Umeå University, SE-901 87 Umeå, Sweden 5 2Florida Museum of Natural History, Division of Invertebrate Paleontology, University of Florida, Gainesville, FL 32611, USA *Correspondence to: [email protected] Abstract: Sepkoski’s hypothesis of Three Great Evolutionary Faunas that dominated 10 Phanerozoic oceans represents a foundational concept of macroevolutionary research. However, the hypothesis lacks spatial information and fails to recognize ecosystem changes in Mesozoic oceans. Using a multilayer network representation of fossil occurrences, we demonstrate that Phanerozoic oceans sequentially harbored four evolutionary faunas: Cambrian, Paleozoic, Mesozoic, and Cenozoic. These mega-assemblages all emerged at low latitudes and dispersed 15 out of the tropics. The Paleozoic–Mesozoic transition was abrupt, coincident with the Permian mass extinction, whereas the Mesozoic–Cenozoic transition was protracted, concurrent with gradual ecological shifts posited by the Mesozoic Marine Revolution. These findings support the notion that long-term ecological changes, historical contingencies, and major geological events all have played crucial roles in shaping the evolutionary history of marine animals. 20 One Sentence Summary: Network analysis reveals that Phanerozoic oceans harbored four evolutionary faunas with variable tempo and underlying causes. -
David M. Raup 1933–2015
David M. Raup 1933–2015 A Biographical Memoir by Michael Foote and Arnold I. Miller ©2017 National Academy of Sciences. Any opinions expressed in this memoir are those of the authors and do not necessarily reflect the views of the National Academy of Sciences. DAVID MALCOLM RAUP April 24, 1933–July 9, 2015 Elected to the NAS, 1979 David M. Raup, one of the most influential paleontolo- gists of the second half of the 20th century, infused the field with concepts from modern biology and established several major lines of research that continue today: Theoretical morphology. Why, despite eons of evolution, is the spectrum of realized biological forms such a tiny fraction of those that are theoretically possible? First-order patterns in the geologic history of biodiversity. Has biodiversity increased steadily over time? What does the answer imply about the biosphere and the nature of the fossil record? Mathematical modeling of evolution. What By Michael Foote patterns result, for example, from the structure of evolu- and Arnold I. Miller tionary trees? And what is the apparent order that emerges from stochastic processes? Biological extinction. What temporal patterns are evident in the history of life and what are their implications for the drivers of extinction and for Earth’s place in the cosmos? The pilot and the paleontologist In The Right Stuff(1979), author Tom Wolfe observed that the calm West Virginia drawl of the renowned test pilot and World War II ace Chuck Yeager could still be heard in the voices of virtually all commercial pilots, decades after Yeager became the first to break the sound barrier. -
World Atlas of Biodiversity
WORLD ATLAS OF BIODIVERSITY EARTH'S LIVING RESOURCES IN THE 21st CENTURY ^ > (\ X >r BRIAN GROOMBRIDGE and MARTIN D. JENKINS UNEP WCMC World Atlas of Biodiversity addresses the remark- ible growth in concern at all levels for living things and the environment and the increased appreciation ' the links between the state of ecosystems and the state of humankind. Building on a wealth of re- search and analysis by the conservation community worldwide, this book provides a comprehensive and accessible view of key global issues in biodiver- sity. It outlines some of the broad ecological relationships between humans and the rest of the iterial world and summarizes information on the health of the planet. Opening with an outline of some fundamental aspects of material cycles and energy flow in the biosphere, the book goes on to discuss the expansion of this diversity through geo- logical time and the pattern of its distribution over the surface of the Earth, and analyzes trends in the condition of the main ecosystem types and the species integral to them. Digitized by tine Internet Arciiive in 2010 witii funding from UNEP-WCIVIC, Cambridge Iittp://www.arcliive.org/details/worldatlasofbiod02groo World Atlas of Biodiversity Published in association witli Ihe contents of this volume do not UNEP-WCMC by the University of necessarily reflect the views or policies of California Press UNEP-WCfvIC, contributory organizations, University of California Press editors or publishers. The designations Berl<eley and Los Angeles, California employed and the presentations do not imply University of California Press, Ltd. the expression of any opinion whatsoever on London, England the part of UNEP-WCIvIC or contributory organizations, editors or publishers © 2002 UNEP World Conservation concerning the legal status of any country, Monitoring Centre territory, city or area or its authority, or UNEP-WCMC concerning the delimitation of its frontiers or 219 Huntingdon Road boundaries or the designation of its name or Cambridge CB3 DDL, UK allegiances. -
THE LAZARUS AMMONOID FAMILY GONIATITIDAE, the TETRANGULARLY COILED ENTOGONITIDAE, and MISSISSIPPIAN BIOGEOGRAPHY Author(S): DIETER KORN, CHRISTIAN KLUG, ROYAL H
THE LAZARUS AMMONOID FAMILY GONIATITIDAE, THE TETRANGULARLY COILED ENTOGONITIDAE, AND MISSISSIPPIAN BIOGEOGRAPHY Author(s): DIETER KORN, CHRISTIAN KLUG, ROYAL H. MAPES Source: Journal of Paleontology, 79(2):356-365. Published By: The Paleontological Society DOI: http://dx.doi.org/10.1666/0022-3360(2005)079<0356:TLAFGT>2.0.CO;2 URL: http://www.bioone.org/doi/full/10.1666/0022-3360%282005%29079%3C0356%3ATLAFGT %3E2.0.CO%3B2 BioOne (www.bioone.org) is a nonprofit, online aggregation of core research in the biological, ecological, and environmental sciences. BioOne provides a sustainable online platform for over 170 journals and books published by nonprofit societies, associations, museums, institutions, and presses. Your use of this PDF, the BioOne Web site, and all posted and associated content indicates your acceptance of BioOne’s Terms of Use, available at www.bioone.org/page/terms_of_use. Usage of BioOne content is strictly limited to personal, educational, and non-commercial use. Commercial inquiries or rights and permissions requests should be directed to the individual publisher as copyright holder. BioOne sees sustainable scholarly publishing as an inherently collaborative enterprise connecting authors, nonprofit publishers, academic institutions, research libraries, and research funders in the common goal of maximizing access to critical research. J. Paleont., 79(2), 2005, pp. 356±365 Copyright q 2005, The Paleontological Society 0022-3360/05/0079-356$03.00 THE LAZARUS AMMONOID FAMILY GONIATITIDAE, THE TETRANGULARLY COILED ENTOGONITIDAE, AND MISSISSIPPIAN BIOGEOGRAPHY DIETER KORN,1 CHRISTIAN KLUG,2 AND ROYAL H. MAPES3 1Museum fuÈr Naturkunde der Humboldt-UniversitaÈt zu Berlin, Invalidenstraûe 43, D-10115 Berlin, Germany, ,[email protected]., 2PalaÈontologisches Institut und Museum, UniversitaÈt ZuÈrich, Karl-Schmid-Str. -
Late Ludfordian and Early Pridoli Monograptids from the Polish Lowland
LATE LUDFORDIAN AND EARLY PRIDOLI MONOGRAPTIDS FROM THE POLISH LOWLAND ADAM URBANEK Urbanek, A. 1997. Late Ludfordian and early Pfidoli monograptids from the Polish Low land. In: A. Urbanek and L. Teller (eds), Silur ian Graptolite Faunas in the East European Platform: Stratigraphy and Evolution. - Palaeontologia Polonica 56, 87-23 1. Graptolites etched from the Mielnik-I wellcore (EPoland) reveal the main features of the development of monograptid faunas within the late Ludfordian-early Pi'idoli interval. Fifteen species and subspecies are described and Monog raptus (Slovinog raptus) subgen. n. as well as Neocolonograptu s gen. n. are erected. Morphology of many species has been described adequately for the first time and their systematic position corrected. Four grap tolite zones of the late Ludfordian are distinguished. The late Ludfordian fauna, which appears after the kozlowskii Event, is composed mainly of immigrants dominated by hooded monograptids. They reappear as a result of the Lazarus effect. Some of them initiated the lobate-spinose phyletic line terminating with Mon ograptus (Uncinatograptus) spineus, a highly characteristic index species. The lobate and the lobate-spinose types are accompanied by bilobate forms (Pse udomonoclimac is latilobu s). The graptolite sequence indicates that the appeara nce of the early Pfidoli fauna was preceded by a biotic crisis, namely the spineus Event. Therefore this fauna is made up of a few holdovers and some new elements which developed from Pristiograptus dubiu s stem lineage (Neocolonograptus gen. n., Istrograpt us Tsegelnjuk). This early assemblage, com posed of bilobate forms, was later enriched by hooded monograptid s, reappearing after the spineus Event. -
Current Status of Philippine Mollusk Museum Collections and Research, and Their Implications on Biodiversity Science and Conservation
Philippine Journal of Science 147 (1): 123-163, March 2018 ISSN 0031 - 7683 Date Received: 28 Feb 2017 Current Status of Philippine Mollusk Museum Collections and Research, and their Implications on Biodiversity Science and Conservation Dino Angelo E. Ramos2*, Gizelle A. Batomalaque1,3, and Jonathan A. Anticamara1,2 1Ecology and Taxonomy Academic Group (ETAG), Institute of Biology, University of the Philippines, Diliman, Quezon City 1101 Philippines 2UP Biology Invertebrate Museum, Institute of Biology, University of the Philippines, Diliman, Quezon City 1101 Philippines 3Department of Biodiversity, Earth, and Environmental Science, Drexel University, Philadelphia, Pennsylvania 19104 USA Mollusks are an invaluable resource in the Philippines, but recent reviews on the status of museum collections of mollusks or research trends in the country are lacking. Such assessments can contribute to a more comprehensive evaluation of natural history museums in the Philippines, as well as biodiversity management. This review showed that local museums in the Philippines have much to improve in terms of their accessibility and geographic coverage in order to effectively cater to research and conservation needs of the country. Online access to databases was lacking for local museums, making it cumbersome to retrieve collection information. The UST museum held the most species and subspecies across all museums (4899), comparable to the national museums of countries such as the USA and France. In terms of size, there were larger Philippine mollusk collections in museums abroad. Majority of mollusk specimens come from Regions 4 and 7, while the CAR and Region 12 were least sampled. Publications on Philippine mollusks are dominated by taxonomic and biodiversity research. -
A New Picture of Life's History on Earth
Commentary A new picture of life’s history on Earth Mark Newman* Santa Fe Institute, 1399 Hyde Park Road, Santa Fe, NM 87501 hen most people think of paleon- his primary source (2, 3). Other compila- database is as exhaustive as possible, sub- Wtology, they picture the field pale- tions also have been published (4, 5), but stantial biases are introduced. For exam- ontologist digging up fossils with a tooth- Sepkoski’s database has received more ple, it is quite feasible that the increase in brush and publishing descriptions of the attention by far than any other. Sepkoski’s diversity toward recent times seen in Fig. anatomies of uncovered specimens in the database was simple in structure: it re- 1 is a result primarily of the greater vol- trade literature. New discoveries of dino- corded the first and last known occur- ume of rock available from recent times, saurs even make the national headlines. rences in the fossil record of more than and the greater amount of effort that has For many decades the discovery and de- 30,000 marine invertebrate genera in been put into studying these rocks. A scription of a previously unknown fossil about 4,000 families. Marine invertebrates number of studies over the years have species was the calling card that gained have been the focus of most statistical presented evidence showing that apparent would-be paleontologists professional ac- studies, because preservation is much diversity is closely correlated with the ceptance. However, in the last quarter of more reliable in marine environments and intensity with which different periods of a century or so, many of the most intrigu- invertebrates are much more numerous geologic time have been sampled (6, 7). -
Palaeontologia Electronica the Paleobiological Revolution
Palaeontologia Electronica http://palaeo-electronica.org The Paleobiological Revolution: Essays on the Growth of Modern Paleontology Reviewed by Brian Switek David Sepkoski and Michael Ruse (editors) belief that paleon- University of Chicago Press, 2009 tology was more 584 pp., $65.00 (hardcover) closely related to ISBN 978-0-226-74861-0 geology rein- By the middle of the 20th century a great forced the idea divide had opened within evolutionary biology. As that it had little to summarized by paleontologist George Gaylord contribute to the Simpson, many geneticists “said that paleontology life sciences. had no further contributions to make to biology”, Despite this wide- while paleontologists believed that the emerging spread reticence science of genetics “had no significance for the to treat paleontol- true biologist.” (Simpson, 1944). Simpson, for his ogy as an evolu- own part, attempted to bring the disciplines into tionary discipline, accord in his classic Tempo and Mode in Evolution, however, paleon- but despite his efforts genetics eventually out- tologists such as stripped paleontology as the evolutionary science G.G. Simpson and du jour. Paleontology, some evolutionary theorists Norman Newell believed, could only testify to the fact of evolution fostered paleobiological research through the while telling us nothing of how such changes actu- 1950’s and 1960’s, setting a long fuse that finally ally occurred. Fortunately, however, some paleon- exploded in the 1970’s. Thomas Schopf, Niles tologists were not satisfied with this blinkered view Eldredge, Stephen Jay Gould, Elisabeth Vrba, of their discipline, and they began what historians David Raup, James Valentine, Jack Sepkoski, and David Sepkoski and Michael Ruse have called The many others transformed paleontology from a rela- Paleobiological Revolution.