Mcmenamin FM

Total Page:16

File Type:pdf, Size:1020Kb

Mcmenamin FM The Garden of Ediacara • Frontispiece: The Nama Group, Aus, Namibia, August 9, 1993. From left to right, A. Seilacher, E. Seilacher, P. Seilacher, M. McMenamin, H. Luginsland, and F. Pflüger. Photograph by C. K. Brain. The Garden of Ediacara • Discovering the First Complex Life Mark A. S. McMenamin C Columbia University Press New York C Columbia University Press Publishers Since 1893 New York Chichester, West Sussex Copyright © 1998 Columbia University Press All rights reserved Library of Congress Cataloging-in-Publication Data McMenamin, Mark A. The garden of Ediacara : discovering the first complex life / Mark A. S. McMenamin. p. cm. Includes bibliographical references and index. ISBN 0-231-10558-4 (cloth) — ISBN 0–231–10559–2 (pbk.) 1. Paleontology—Precambrian. 2. Fossils. I. Title. QE724.M364 1998 560'.171—dc21 97-38073 Casebound editions of Columbia University Press books are printed on permanent and durable acid-free paper. Printed in the United States of America c 10 9 8 7 6 5 4 3 2 1 p 10 9 8 7 6 5 4 3 2 1 For Gene Foley Desert Rat par excellence and to the memory of Professor Gonzalo Vidal This page intentionally left blank Contents Foreword • ix Preface • xiii Acknowledgments • xv 1. Mystery Fossil 1 2. The Sand Menagerie 11 3. Vermiforma 47 4. The Nama Group 61 5. Back to the Garden 121 6. Cloudina 157 7. Ophrydium 167 8. Reunite Rodinia! 173 9. The Mexican Find: Sonora 1995 189 10. The Lost World 213 11. A Family Tree 225 12. Awareness of Ediacara 239 13. Revenge of the Mole Rats 255 Epilogue: Parallel Evolution • 279 Appendix • 283 Index • 285 This page intentionally left blank Foreword Dorion Sagan Virtually as soon as earth’s crust cools enough to be hospitable to life, we find evidence of life on its surface. But we are latecomers, and just as we must be familiar with the beginning of a mystery novel to understand its end, we must scrutinize the often ignored early phase of evolution. Mark McMenamin’s allusively named Garden of Ediacara hones in on some of the key events and players in life’s early phase—a time for the biosphere that, like the first three years of a human life, is not only for- mative and revealing but essential to understanding the full sweep of a living existence. Da Vinci found shells on mountains that suggested a long geological past. Hutton and, later, Darwin extended such thinking, drawing forth a temporal expanse wide enough to explain modern anomalies and complexities. But when early commentators surveyed the fossil history of life on earth, they were not overly impressed with life’s earliest phase. It almost seemed as if nothing was going on. Until the “Cambrian explosion”—the widespread appearance of fossil forms, including the famous horseshoe-crab-like trilobites, during the Cambrian geological period—it seemed as if life had barely started. Now you don’t see them, now you do: Like the goddess Minerva bursting forth fully formed from the head of Zeus, the sudden appearance of hard-backed animals in the fossil record had about it the lingering aura of myth or celestial-fostered miracle. Whence come animals from evolutionary chaos? For geologist Preston Cloud, one of the first of the modern paleobiol- ogists, the appearance of animal life corresponded to a global atmospheric increase in free oxygen. This theory, repeated in textbooks, may be an anthropomorphic fairy tale, a kind of industrial fiction. Fire-starting oxy- gen, the gas of choice, spurs the biosphere to produce complex life forms, paving the way for air-breathing mammals. But there is probably no x • Foreword causal relationship between oxygen increase and animal life. The Cambrian explosion was 540 million years ago, whereas according to the rock record of oxygen-rich uranium and iron ores, atmospheric oxygen began to build up far earlier, some 1800 million years ago. Nothing is so destructive of a beautiful theory as an ugly fact. Although classical evolutionists pictured a gradual evolution of animal life from soft-bodied to hard-bodied forms, the shelled creatures of the Cambrian stick out like a sore thumb. There does seem to be a sudden- ness about them, one not explicable on the basis of gradual evolution. Today we understand that the Cambrian fauna were preceded by a strange and motley collection of often symmetrical soft-bodied forms. These are the Ediacarans, eponymous subheroes of the Australian outcrop where the first such fossils were found. The Ediacarans’ global “garden,” more than a cryptic play on Eden’s idyllic and instantaneous fertility, refers to their largely vegetative existence. With the playful attitude of a true sci- entific explorer, Mark McMenamin treks the planet and mines the litera- ture, some of it itself almost fossiliferous, in an exposition of medusoids, ring stones, concentrically fretted, radially flaring, and other enigmatic trace and body fossils left by the soft-bodied pre-Cambrian forms. Who were these beings? Were they animals? Our ancestors? More likely, we find, they were our cousins. Although superficially similar to jellyfish, the Ediacaran medusoids probably never swam: They are preserved concave side up, like bowls rather than like swim- mers. They may have been so quickly replaced all over the world not as a result of evolution-igniting oxygen, but because evolution had gotten to the point where predators with eyes and a murderous appetite for Ediacaran sushi had come into their own. In McMenamin’s persuasive reading, the earliest animals (or animal-like life, for they may have been blastula-less colonial microbes called protoctists—predating predation) were languid, limpid vegetarians. Harmless antecedents to Tennyson’s bloody nature tooth and claw, they were eyeless representatives of a vic- timless Edenlike world. This was a green and serene world where there was no reason for calcified coverings, for carapaces or spiky armor because the victimizing element of Animalia had not yet evolved. The Ediacarans, on this view, were translucent beings with photo- synthetic inclusions, soaking up the sun and living off the excess of their living internal gardens. Today creatures such as the snail Placobranchus, the giant clam Tridacna, and the seaweed-looking worm Convoluta roscoffensis, whose mouth is closed throughout its adult life, have gone back to the simpler “Edenic” lifestyle of autotrophic sunbathing. Ryan Foreword • xi Drum has even made the semiserious suggestion that this would be a good thing for junkies: Inject them with algae, select for ever more pal- lid and translucent demeanor, and in time we might have societally harmless anthropoids nutrifying themselves in languor at a delicious if safe remove from the normal frenetic hustle of urban animal life. The photosynthetic cells might even migrate to the germ cells of these veg- etablarians, permitting true speciation of Homo photosyntheticus from Homo sapiens ancestors. It would be a mistake to think such “planimals” only freaks of sym- biosis or figments of science fiction. All plants and algae on the planet are composed of eukaryotic cells whose existence has been brought to us by primeval mergers with cyanobacteria, green prokaryotes that were eaten (living salad) by larger cells. Blessed with a permanent case of indi- gestion, these larger cells benefitted from the metabolic independence of the preplants now dwelling Jonah-like inside them. McMenamin’s Garden of Ediacara hypothesis explains the widespread soft-bodied beings, many flat and fronded, as early testimony to the power of pho- tosymbiosis. By turns starfishy and Star Treky, branched and sand dol- laresque—switching, like some fossil equivalent to a Necker cube, from twisting worm to growing stem in the paleontologist’s imagination— these creatures may well have been neither plant nor animal. On the television program The X Files, FBI agents Sculley and Mulder find “a cell that is not a plant cell or an animal cell. And it’s dividing mitoti- cally.” How creepy! How strange! The only problem with this would-be biological bizarrerie is that such uncanny cells are more prevalent on the surface of earth than either plant or animal cells. They’re in your house right now, and they live in your body. Bacteria, although they do not divide mitotically, are neither animals nor plants. And their symbio- genetic offspring, the protoctists, which do divide mitotically (and which are on your skin right now), were certainly among the ancestors to the Ediacarans. But the “metacellularity” of the Ediacaran organisms may not have led to any large extant forms of life familiar to us today. They were jellyfish-like and starfish-like, but neither truly medusoids nor echinoderms. Some secreted copious mucous layers as a means of gliding locomotion. True aliens from our own past, some of these fabu- lously real beings lost their innocence and symmetry. Concentrating sense organs at one end, some may have been, before animals proper, the first organisms to evolve heads. Which, as in the knowledge gained from the Tree of Good and Evil in the redolent Garden of Eden, may have spelled the beginning of the end. xii • Foreword For despite the scene drawn by some evolutionists of a planet of pure con- tingency, devoid of direction, certain patterns do have a way of cropping up again and again in evolution. Eusocial animals, for example, come not only in bee and ant but in naked mole rat flavors. Humans too, losing the inevitable link between sex and reproduction, may be moving toward eusociality. Like a tale told by a stutterer, evolution doubtless is circuitous and may well contain only the raw material, rather than the denouement, of meaning. But there are these patterns. Not just hominids but many species of mammal, for example, show an increase in body and brain size over evolutionary time.
Recommended publications
  • Αξιολόγηση Διαφορετικών Υποστρωμάτων Στην in Vitro Ριζοβολία Εκφύτων Αλόης (Aloe Vera L.) Για Επιχειρηματική Παραγωγή Υγιούς Πολλαπλασιαστικού Υλικού
    ΤΕΧΝΟΛΟΓΙΚΟ ΕΚΠΑΙΔΕΥΤΙΚΟ ΙΔΡΥΜΑ ΚΡΗΤΗΣ ΣΧΟΛΗ ΤΕΧΝΟΛΟΓΙΑΣ ΓΕΩΠΟΝΙΑΣ & ΤΕΧΝΟΛΟΓΙΑΣ ΤΡΟΦΙΜΩΝ ΤΜΗΜΑ ΤΕΧΝΟΛΟΓΩΝ ΓΕΩΠΟΝΩΝ Αξιολόγηση διαφορετικών υποστρωμάτων στην in vitro ριζοβολία εκφύτων αλόης (Aloe vera L.) για επιχειρηματική παραγωγή υγιούς πολλαπλασιαστικού υλικού Πτυχιακή Εργασία ΣΠΟΥΔΑΣΤΡΙΑ ΧΡΟΝΑΚΗ ΑΓΑΠΗ ΗΡΑΚΛΕΙΟ, ΑΠΡΙΛΙΟΣ 2018 ΚΑΘΗΓΗΤΕΣ ΤΡΙΜΕΛΟΥΣ ΕΞΕΤΑΣΤΙΚΗ ΕΠΙΤΡΟΠΗΣ Ομότ. Kαθ. κ. Γραμματικάκη Γαρυφαλλιά Επίκ. Καθ. κ. Δραγασάκη Μαγδαληνή Επίκ. Καθ. κ. Πασχαλίδης Κωνσταντίνος ΤΟ ΕΡΓΟ ΑΥΤΟ ΥΛΟΠΟΙΗΘΗΚΕ ΣΤΟ ΕΡΓΑΣΤΗΡΙΟ ΓΕΩΡΓΙΑΣ ΚΑΙ ΠΑΡΑΓΩΓΗΣ ΠΟΛΛΑΠΛΑΣΙΑΣΤΙΚΟΥ ΥΛΙΚΟΥ ΤΟΥ ΤΜΗΜΑΤΟΣ ΤΕΧΝΟΛΟΓΩΝ ΓΕΩΠΟΝΩΝ,ΤΗΣ ΣΧΟΛΗΣ ΤΕΧΝΟΛΟΓΙΑΣ ΓΕΩΠΟΝΙΑΣ ΤΟΥ ΤΕΙ ΚΡΗΤΗΣ 2 Πρόλογος Η παρούσα διατριβή ξεκίνησε και ολοκληρώθηκε στο Εργαστήριο Γεωργίας και Παραγωγής Πολλαπλασιαστικού Υλικού, του Τμήματος Τεχνολόγων Γεωπόνων της Σχολής Τεχνολογίας Γεωπονίας & Τεχνολογίας Τροφίμων, του ΤΕΙ Κρήτης. Με την ολοκλήρωση της συγκεκριμένης ερευνητικής εργασίας, θα ήθελα να ευχαριστήσω την Καθηγήτρια κ. Γραμματικάκη Γαρυφαλλιά, τόσο για την εμπιστοσύνη που μου έδειξε, αναθέτοντάς μου το θέμα της παρούσας μελέτης, όσο και για την βοήθεια που μου προσέφερε σε όλα τα στάδια της εκτέλεσής της. Επιπλέον, θεωρώ υποχρέωση μου να ευχαριστήσω το προσωπικό του Εργαστηρίου, κ. Κωνσταντίνα Αργυροπούλου για τη συμπαράσταση και τη φιλική της συμπεριφορά. Ευχαριστώ θερμά τον κ. Παπαδημητρίου Μιχάλη, Καθηγητή του ΤΕΙ Κρήτης, για τη χορήγηση του γενετικού υλικού έναρξης που χρησιμοποιήθηκε στην μελέτη, καθώς και τον κύριο Αλεξόπουλο Παναγιώτη, υπάλληλο της εταιρίας Hellenic Aloe, για την ευγενική
    [Show full text]
  • Motorcycle Tour South Africa and Namibia, from Cape Town to Windhoek Motorcycle Tour South Africa and Namibia, from Cape Town to Windhoek
    Motorcycle tour South Africa and Namibia, from Cape Town to Windhoek Motorcycle tour South Africa and Namibia, from Cape Town to Windhoek Duração Dificuldade Veículo de apoio 14 días Normal-Hard Sim Language Guia en,de Sim Namibia, a vast 830 thousand square kilometre expense of desert flanked by the icy Atlantic Ocean, is home to slightly less than 1.7 million citizens. That’s less than half the number of Cape Town residents. Unending roads stretch out as far as the eye can see under a sky that’s so big it can only be described as heavenly with space enough to truly breathe. The two-week trip starts in Cape Town and winds its way up our west coast to culminate in Namibia’s capital, Windhoek. With both on and off-road riding, the 2,100 miles city to city tour is an epic tribute to solitude and uninterrupted riding with out-of-this world scenery. Your on-road riding experience will be punctuated by some gravel road riding exploring such places as the mountainous Cedarberg region, the Northern Cape, one of the world’s oldest deserts as well as the Fish River Canon, the world’s second largest canyon. Approximately 50% of this tour is on dirt roads, some basic off-road riding skills are required. Itinerário 1 - - Cidade do Cabo - 0 Welcome. Almost all international flights arrive in Cape Town before midday. Our tour guide will meet you at the airport and taxi you directly to your hotel where you can freshen-up and perhaps have a light bite to eat.
    [Show full text]
  • Ediacaran) of Earth – Nature’S Experiments
    The Early Animals (Ediacaran) of Earth – Nature’s Experiments Donald Baumgartner Medical Entomologist, Biologist, and Fossil Enthusiast Presentation before Chicago Rocks and Mineral Society May 10, 2014 Illinois Famous for Pennsylvanian Fossils 3 In the Beginning: The Big Bang . Earth formed 4.6 billion years ago Fossil Record Order 95% of higher taxa: Random plant divisions domains & kingdoms Cambrian Atdabanian Fauna Vendian Tommotian Fauna Ediacaran Fauna protists Proterozoic algae McConnell (Baptist)College Pre C - Fossil Order Archaean bacteria Source: Truett Kurt Wise The First Cells . 3.8 billion years ago, oxygen levels in atmosphere and seas were low • Early prokaryotic cells probably were anaerobic • Stromatolites . Divergence separated bacteria from ancestors of archaeans and eukaryotes Stromatolites Dominated the Earth Stromatolites of cyanobacteria ruled the Earth from 3.8 b.y. to 600 m. [2.5 b.y.]. Believed that Earth glaciations are correlated with great demise of stromatolites world-wide. 8 The Oxygen Atmosphere . Cyanobacteria evolved an oxygen-releasing, noncyclic pathway of photosynthesis • Changed Earth’s atmosphere . Increased oxygen favored aerobic respiration Early Multi-Cellular Life Was Born Eosphaera & Kakabekia at 2 b.y in Canada Gunflint Chert 11 Earliest Multi-Cellular Metazoan Life (1) Alga Eukaryote Grypania of MI at 1.85 b.y. MI fossil outcrop 12 Earliest Multi-Cellular Metazoan Life (2) Beads Horodyskia of MT and Aust. at 1.5 b.y. thought to be algae 13 Source: Fedonkin et al. 2007 Rise of Animals Tappania Fungus at 1.5 b.y Described now from China, Russia, Canada, India, & Australia 14 Earliest Multi-Cellular Metazoan Animals (3) Worm-like Parmia of N.E.
    [Show full text]
  • NAMIBIA Angola, Zambia,Namibia,Botswana,Zimbabweandsouthafrica
    © Lonely Planet Publications 304 lonelyplanet.com NAMIBIA •• Highlights 305 extreme sports in Swakopmund ( p360 ), N a m i b i a HOW MUCH? take a safari through Etosha ( p332 ), hike Dune surfing US$25 the Fish River Canyon ( p385 ) and go on an exped ition through the northwest and Foreign newspaper US$1.70 along the Skele ton Coast ( p354 ). Night in a budget hotel US$12.50 Package of kudu biltong US$1 CLIMATE & WHEN TO GO Traditional German dinner US$6 Namibia’s climatic variations correspond Wedged between the Kalahari and the South Atlantic, Namibia enjoys both vast potential roughly to its geographical subdivisions. In and promise as one of the youngest countries in Africa. In addition to a striking diversity LONELY PLANET INDEX the arid Central Namib, summer daytime of cultures and national origins, Namibia is also a photographer’s dream – it boasts wild temperatures may climb to over 40°C, but seascapes, rugged mountains, lonely deserts, stunning wildlife, colonial cities and nearly 1L of petrol US$0.75 can fall to below freezing during the night. Rainfall is heaviest in the northeast, which unlimited elbow room. 1L of bottled water US$0.50-1 enjoys a subtropical climate, and along the Bottle of beer US$1 A predominantly arid country, Namibia can be divided into four main topographical re- Okavango River, rainfall reaches over 600mm Souvenir T-shirt US$5-10 annually. The northern and interior regions gions: the Namib Desert and coastal plains in the west, the eastward-sloping Central Plateau, Snack US$1-2 experience the ‘little rains’ between October the Kalahari along the borders with South Africa and Botswana, and the densely wooded and December, while the main stormy period bushveld of the Kavango and Caprivi regions.
    [Show full text]
  • Plant Rescue Management Plan
    Plant Rescue Management Plan 86 MW Oya Wind Energy Facility (WEF) and associated David Hoare Consulting infrastructure between Sutherland and Matjiesfontein, Western and Northern Cape Provinces Plant Rescue Management Plan for the proposed 86 David Hoare MW Oya Wind Energy Consulting (Pty) Ltd Facility between Sutherland and Matjiesfontein in the Address: Western and Northern Cape Postnet Suite #116 Private Bag X025 Lynnwood Ridge Provinces. 0040 41 Soetdoring Avenue Lynnwood Manor Pretoria Telephone: 087 701 7629 Location: Cell: 083 284 5111 Witzenberg Local Municipality within the Cape Winelands District Fax: 086 550 2053 Municipality Email: [email protected] Prepared for Oya Energy (Pty) Ltd 5th Floor, 125 Buitengracht Street Cape Town 8001 Report author: Dr D.B. Hoare (Pr.Sci.Nat.) 13 November 2020 Report version: 1st draft i Details of specialist consultant Company name David Hoare Consulting (Pty) Ltd Registration no.: CK2017/308639/07 Address Postnet Suite #116 Private Bag X025 Lynnwood Ridge 0040 Contact person Dr David Hoare Contact details Cell: 083 284 5111 Email: [email protected] Qualifications PhD Botany (Nelson Mandela Metropolitan University) MSc Botany (University of Pretoria) BSc (Hons) Botany (Rhodes University) BSc Botany, Zoology (Rhodes University) 2 TABLE OF CONTENTS DETAILS OF SPECIALIST CONSULTANT ........................................................................................................................ 2 TABLE OF CONTENTS .................................................................................................................................................
    [Show full text]
  • Contributions to the Neoproterozoic Geobiology
    Contributions to the Neoproterozoic Geobiology Bing Shen Dissertation submitted to the faculty of the Virginia Polytechnic Institute and State University in partial fulfillment of the requirements for the degree of Doctor of Philosophy In Department of Geosciences Shuhai Xiao (Chair) Robert Bodnar Michal Kowalewski J. Fred Read November 29, 2007 Blacksburg, Virginia Key words: Neoproterozoic, Ediacaran, Ediacara fossils, China, Disparity, Sulfur isotope, Carbon isotope Copyright 2007, Bing Shen Contributions to the Neoproterozoic Geobiology Bing Shen Abstract This thesis makes several contributions to improve our understanding of the Neoproterozoic Paleobiology. In chapter 1, a comprehensive quantitative analysis of the Ediacara fossils indicates that the oldest Ediacara assemblage—the Avalon assemblage— already encompassed the full range of Ediacara morphospace. A comparable morphospace range was occupied by the subsequent White Sea and Nama assemblages, although it was populated differently. In contrast, taxonomic richness increased in the White Sea assemblage and declined in the Nama assemblage. The Avalon morphospace expansion mirrors the Cambrian explosion, and both may reflect similar underlying mechanisms. Chapter 2 describes problematic macrofossils collected from the Neoproterozoic slate of the upper Zhengmuguan Formation in North China and sandstone of the Zhoujieshan Formation in Chaidam. Some of these fossils were previously interpreted as animal traces. Our study of these fossils recognizes four genera and five species. None of these taxa can be interpreted as animal traces. Instead, they are problematic body fossils of unresolved phylogenetic affinities. Chapter 3 reports stable isotopes of the Zhamoketi cap dolostone atop the Tereeken diamictite in the Quruqtagh area, eastern Chinese Tianshan. Our new data indicate that carbonate associated sulfate (CAS) abundance decreases rapidly in the basal 34 cap dolostone and δ SCAS composition varies between +9‰ and +15‰ in the lower 2.5 34 m.
    [Show full text]
  • Durham Research Online
    Durham Research Online Deposited in DRO: 23 May 2017 Version of attached le: Accepted Version Peer-review status of attached le: Peer-reviewed Citation for published item: Betts, Marissa J. and Paterson, John R. and Jago, James B. and Jacquet, Sarah M. and Skovsted, Christian B. and Topper, Timothy P. and Brock, Glenn A. (2017) 'Global correlation of the early Cambrian of South Australia : shelly fauna of the Dailyatia odyssei Zone.', Gondwana research., 46 . pp. 240-279. Further information on publisher's website: https://doi.org/10.1016/j.gr.2017.02.007 Publisher's copyright statement: c 2017 This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/ Additional information: Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full DRO policy for further details. Durham University Library, Stockton Road, Durham DH1 3LY, United Kingdom Tel : +44 (0)191 334 3042 | Fax : +44 (0)191 334 2971 https://dro.dur.ac.uk Accepted Manuscript Global correlation of the early Cambrian of South Australia: Shelly fauna of the Dailyatia odyssei Zone Marissa J.
    [Show full text]
  • Aloe Scientific Primer International Aloe Science Council
    The International Aloe Science Council Presents an Aloe Scientific Primer International Aloe Science Council Commonly Traded Aloe Species The plant Aloe spp. has long been utilized in a variety of ways throughout history, which has been well documented elsewhere and need not be recounted in detail here, particularly as the purpose of this document is to discuss current and commonly traded aloe species. Aloe, in its various species, can presently and in the recent past be found in use as a decorative element in homes and gardens, in the creation of pharmaceuticals, in wound care products such as burn ointment, sunburn protectant and similar applications, in cosmetics, and as a food, dietary supplements and other health and nutrition related items. Recently, various species of the plant have even been used to weave into clothing and in mattresses. Those species of Aloe commonly used in commerce today can be divided into three primary categories: those used primarily in the production of crude drugs, those used primarily for decorative purposes, and those used in health, nutritional and related products. For reference purposes, this paper will outline the primary species and their uses, but will focus on the species most widely used in commerce for health, nutritional, cosmetic and supplement products, such as aloe vera. Components of aloe vera currently used in commerce The Aloe plant, and in particular aloe vera, has three distinct raw material components that are processed and found in manufactured goods: leaf juice; inner leaf juice; and aloe latex. A great deal of confusion regarding the terminology of this botanical and its components has been identified, mostly because of a lack of clear definitions, marketing, and other factors.
    [Show full text]
  • New High‐Resolution Age Data from the Ediacaran–Cambrian Boundary Indicate Rapid, Ecologically Driven Onset of the Cambrian Explosion
    Received: 14 June 2018 | Revised: 6 October 2018 | Accepted: 19 October 2018 DOI: 10.1111/ter.12368 PAPER New high‐resolution age data from the Ediacaran–Cambrian boundary indicate rapid, ecologically driven onset of the Cambrian explosion Ulf Linnemann1 | Maria Ovtcharova2 | Urs Schaltegger2 | Andreas Gärtner1 | Michael Hautmann3 | Gerd Geyer4 | Patricia Vickers-Rich5,6,7 | Tom Rich6 | Birgit Plessen8 | Mandy Hofmann1 | Johannes Zieger1 | Rita Krause1 | Les Kriesfeld7 | Jeff Smith7 1Senckenberg Collections of Natural History Dresden, Museum of Mineralogy Abstract and Geology, Dresden, Germany The replacement of the late Precambrian Ediacaran biota by morphologically disparate 2Département des Sciences de la Terre, animals at the beginning of the Phanerozoic was a key event in the history of life on University of Geneva, Genève, Switzerland ‐ 3Paläontologisches Institut und Museum, Earth, the mechanisms and the time scales of which are not entirely understood. A Zürich, Switzerland composite section in Namibia providing biostratigraphic and chemostratigraphic data 4 Bayerische Julius-Maximilians-Universität, bracketed by radiometric dating constrains the Ediacaran–Cambrian boundary to Lehrstuhl für Geodynamik und Geomaterialforschung, Würzburg, Germany 538.6–538.8 Ma, more than 2 Ma younger than previously assumed. The U–Pb‐CA‐ID 5Department of Chemistry and TIMS zircon ages demonstrate an ultrashort time frame for the LAD of the Ediacaran Biotechnology, Swinburne University of Technology, Melbourne (Hawthorne), biota to the FAD of a complex, burrowing Phanerozoic biota represented by trace fos- Victoria, Australia sils to a 410 ka time window of 538.99 ± 0.21 Ma to 538.58 ± 0.19 Ma. The extre- 6 Museums Victoria, Melbourne, Victoria, mely short duration of the faunal transition from Ediacaran to Cambrian biota within Australia less than 410 ka supports models of ecological cascades that followed the evolution- 7School of Earth, Atmosphere and Environment, Monash University, ary breakthrough of increased mobility at the beginning of the Phanerozoic.
    [Show full text]
  • Unusual Arrangement of Bones at Ichthyosaur State Park in Nevada by Mark A
    GEOLOGY EVIDENCE FOR A TRIASSIC KRAKEN Unusual Arrangement of Bones at Ichthyosaur State Park in Nevada by Mark A. S. McMenamin Did a giant kraken drag nine huge ichthyosaurs back to its lair in the Triassic era, where their fossil remains are found today? The author of this hypothesis tells why he thinks so. he Triassic Kraken hypothesis, pre- Tsented to the Geological Society of America at its October annual meeting in Minneapolis (McMenamin and McMe- namin 2011), generated an enormous amount of attention on Internet media, immediately after the Society’s press re- lease announcing the discovery. Nine gigantic ichthyosaurs are pre- served in a rock layer belonging to the Shaly Limestone Member of the Luning Formation at the Ichthyosaur State Park in Courtesy of Mark McMenamin Nevada. Geological analysis of this fossil Shonisaurus ichthyosaur vertebral disks at the Berlin-Ichthyosaur State Park in Ne- site had shown it to be a deep water de- vada, arranged in curious linear patterns with almost geometric regularity. The ar- posit (Holger 1992), thus invalidating ranged vertebrae in this Specimen-U resemble the pattern of sucker discs on a cepha- Camp’s (1980) original hypothesis that lopod tentacle, with each vertebra strongly resembling a coleoid sucker. the fossil bed represented an ichthyosaur mass-stranding event. Holger’s (1992) metric patterns, some of which resem- bone arrangement has indeed “never study left unexplained, however, how it ble the sucker arrays on cephalopod been observed at other localities.” came to be that nine giant Shonisaurus tentacles. Seilacher remarked that Jurassic ich- ichthyosaurs sequentially accumulated A YouTube video from the Seattle thyosaur skeletons in Germany, which at virtually the same spot on the Triassic Aquarium, showing a Pacific Octopus may provide analogous examples, occur sea floor.
    [Show full text]
  • Back Matter (PDF)
    Index Acraman impact ejecta layer 53–4, 117, 123, 126–9, Aspidella 130–2, 425–7 controversy 300, 301–3, 305 acritarchs ecology 303 Amadeus and Officer Basins 119 synonyms 302 biostratigraphy 115–25, 130–2 Australia Australian correlations 130–2 Acraman impact ejecta layer 53–4, 117, 123, 126–9, composite zonation scheme 119, 131, 132 130–2, 425–7 India 318–20 carbon isotope chemostratigraphy 126–9 Ireland 289 correlations of Ediacaran System and Period 18, Spain 232 115–35 sphaeromorphid 324 Marinoan glaciation 53–4, 126 Adelaide, Hallett Cove 68 Australia, Ediacaran System and Period Adelaide Rift Complex 115–22, 425 Bunyeroo–Wonoka Formation transition correlations with Officer Basin 127 137–9, 426 dating (Sr–Rb) 140 Centralian Superbasin 118, 125 generalized time–space diagram, correlations composite zonation scheme 131 between tectonic units 120 correlation methods and results 125–32 location maps 116, 118 time–space diagram 120 SE sector cumulative strata thickness 139 Vendian climatic indicators 17 stratigraphic correlation with Officer Basin 127 See also Adelaide Rift Complex; Flinders Ranges Stuart Shelf drill holes, correlations 117 Avalonian assemblages, Newfoundland 237–57, Sturtian (Umberatana) Group 116, 138 303–7, 427 Umberatana Group 116, 138 Africa backarc spreading, Altenfeld Formation 44–5, 47–8 Vendian climatic indicators 17 Baliana–Krol Group, NW Himalaya 319 see also Namibia Barut Formation, Iran 434 Aldanellidae 418 Bayesian analysis algal metaphyta, White Sea Region 271–4 eumetazoans 357–9 algal microfossils, White
    [Show full text]
  • 8D7N Best of Nambia
    0 Windhoeekk –– SossusvleiSossusvlei –– Walvisalvis BayBay –– SwakopmundSwakopmund –– Windhoekk Namib Desert, Sossuslei MINIMUM 4 ADULTS Season Twin Share Single Room Supplement January - June 11,950 1,820 July – November 12,260 1,890 December 12,510 1,960 PRICE INCLUSIONS Return airport-hotel-airport transfer Day City Hotel/Lodge (or similar class) 07 Nights hotel accommodation with 01 Windhoek Avani Windhoek Hotel & Casino daily breakfast 02 Kalahari Desert Lapa Lange Lodge Service of an English speaking driver cum 03 & 04 Sossuslei Area Le Mirage Resort & Spa guide 05 & 06 Walvis Bay Lagoon Flamingo Villas Boutique Hotel Lunch and dinner as specified in the 07 Windhoe Avani Windhoek Hotel & Casino itinerary Bottled mineral water daily DAY ITINERARY Med Emergency Rescue and Evacuation 01 WINDHOEK – ARRIVAL (D) within Namibia Arrived at Windhoek Airport, meet and greet by local representative and transfer to Value Added Tax Tourism Levy hotel for check in. PRICE EXCLUSIONS 02 WINDHOEK – MARIENTAL (B/L/D) International airfare Morning depart south to Kalahari Desert. Afternoon nature Sundowner Drive. After Applicable airport taxes dinner enjoy the clear night skies with star gazing (subject to weather condition). Personal Incidental Expenses Travel Insurance 03 MARIENTAL – SOSSUSVLEI (B/L/D) Gratuities to guide & driver : Morning walk with SAN Bushman family. Later depart to Namib Desert en-route visit US$20 per person per day – pay direct the Duwisib Castle. Arrive at Sossusvlei and check in hotel. Evening Sunset Quad REMARKS Bike Trip. Tour prices quoted are subject to change 04 SOSSUSVLEI (B/L/D) with or without prior notice Visit Dunes at Sossusvlei, Dead Vlei, Dune45 & Sesriem Canyon Subject to availability upon making reservation 05 SOSSUSVLEI – WALVIS BAY (B/L/D) No refund for un-utilized tours or services Cross the Tropic of Capricorn through the Kuiseb Pass , Kuiseb Canyon, the Moon Terms & Conditions Apply Landscape and the Welwitschia Plains.
    [Show full text]