High Ecological Complexity in Benthic Ediacaran Communities
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The Ediacaran Frondose Fossil Arborea from the Shibantan Limestone of South China
Journal of Paleontology, 94(6), 2020, p. 1034–1050 Copyright © 2020, The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/ licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/20/1937-2337 doi: 10.1017/jpa.2020.43 The Ediacaran frondose fossil Arborea from the Shibantan limestone of South China Xiaopeng Wang,1,3 Ke Pang,1,4* Zhe Chen,1,4* Bin Wan,1,4 Shuhai Xiao,2 Chuanming Zhou,1,4 and Xunlai Yuan1,4,5 1State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Palaeoenvironment, Chinese Academy of Sciences, Nanjing 210008, China <[email protected]><[email protected]> <[email protected]><[email protected]><[email protected]><[email protected]> 2Department of Geosciences, Virginia Tech, Blacksburg, Virginia 24061, USA <[email protected]> 3University of Science and Technology of China, Hefei 230026, China 4University of Chinese Academy of Sciences, Beijing 100049, China 5Center for Research and Education on Biological Evolution and Environment, Nanjing University, Nanjing 210023, China Abstract.—Bituminous limestone of the Ediacaran Shibantan Member of the Dengying Formation (551–539 Ma) in the Yangtze Gorges area contains a rare carbonate-hosted Ediacara-type macrofossil assemblage. This assemblage is domi- nated by the tubular fossil Wutubus Chen et al., 2014 and discoidal fossils, e.g., Hiemalora Fedonkin, 1982 and Aspidella Billings, 1872, but frondose organisms such as Charnia Ford, 1958, Rangea Gürich, 1929, and Arborea Glaessner and Wade, 1966 are also present. -
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. -
Exceptionally Preserved Jellyfishes from the Middle Cambrian Paulyn Cartwright1, Susan L
Exceptionally Preserved Jellyfishes from the Middle Cambrian Paulyn Cartwright1, Susan L. Halgedahl2, Jonathan R. Hendricks3, Richard D. Jarrard2, Antonio C. Marques4, Allen G. Collins5, Bruce S. Lieberman3* 1 Department of Ecology and Evolutionary Biology, University of Kansas, Lawrence, Kansas, United States of America, 2 Department of Geology and Geophysics, University of Utah, Salt Lake City, Utah, United States of America, 3 Department of Geology, and Division of Invertebrate Paleontology, Natural History Museum, University of Kansas, Lawrence, Kansas, United States of America, 4 Departamento de Zoologia, Instituto de Biocieˆncias, Universidade de Sa˜o Paulo, Sa˜o Paulo, Sa˜o Paulo, Brazil, 5 National Systematics Laboratory of NOAA Fisheries Service, National Museum of Natural History, Smithsonian Institution, Washington, D. C., United States of America Cnidarians represent an early diverging animal group and thus insight into their origin and diversification is key to understanding metazoan evolution. Further, cnidarian jellyfish comprise an important component of modern marine planktonic ecosystems. Here we report on exceptionally preserved cnidarian jellyfish fossils from the Middle Cambrian (,505 million years old) Marjum Formation of Utah. These are the first described Cambrian jellyfish fossils to display exquisite preservation of soft part anatomy including detailed features of structures interpreted as trailing tentacles and subumbrellar and exumbrellar surfaces. If the interpretation of these preserved characters is correct, their presence is diagnostic of modern jellyfish taxa. These new discoveries may provide insight into the scope of cnidarian diversity shortly after the Cambrian radiation, and would reinforce the notion that important taxonomic components of the modern planktonic realm were in place by the Cambrian period. -
The Cambrian Explosion: How Much Bang for the Buck?
Essay Book Review The Cambrian Explosion: How Much Bang for the Buck? Ralph Stearley Ralph Stearley THE RISE OF ANIMALS: Evolution and Diversification of the Kingdom Animalia by Mikhail A. Fedonkin, James G. Gehling, Kathleen Grey, Guy M. Narbonne, and Patricia Vickers-Rich. Baltimore, MD: Johns Hopkins University Press, 2007. 327 pages; includes an atlas of Precambrian Metazoans, bibliography, index. Hardcover; $79.00. ISBN: 9780801886799. THE CAMBRIAN EXPLOSION: The Construction of Animal Bio- diversity by Douglas H. Erwin and James W. Valentine. Greenwood Village, CO: Roberts and Company, 2013. 406 pages; includes one appendix, references, index. Hardcover; $60.00. ISBN: 9781936221035. DARWIN’S DOUBT: The Explosive Origin of Animal Life and the Case for Intelligent Design by Stephen C. Meyer. New York: HarperCollins, 2013. 498 pages; includes bibliography and index. Hardcover; $28.99. ISBN: 9780062071477. y the time that Darwin published Later on, this dramatic appearance of B On the Origin of Species in 1859, complicated macroscopic fossils would the principle of biotic succession become known by the shorthand expres- had been well established and proven to sion “Cambrian explosion.” Because the be a powerful aid to correlating strata dispute between Sedgwick and Roderick and deciphering the history of Earth, to Murchisonontheboundarybetweenthe which the rock layers testified. However, Cambrian and Silurian systems had not for Darwin, there remained a major been fully resolved by 1859, Darwin con- issue regarding fossils for his compre- sidered these fossils “Silurian” (and thus hensive explanation for the history of for him, the issue would have been life. The problem was this: the base of labeled the “Silurian explosion”!). -
The Influence of Environmental Setting on the Community Ecology of Ediacaran Organisms
bioRxiv preprint doi: https://doi.org/10.1101/861906; this version posted December 2, 2019. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. 1 The influence of environmental setting on the community ecology of Ediacaran organisms 2 3 Emily G. Mitchell1, Nikolai Bobkov2,3, Natalia Bykova2,4, Alavya Dhungana,5, Anton 4 Kolesnikov2,6, 7, Ian R. P. Hogarth8,9 Alexander G. Liu10, Tom M.R. Mustill10,11, Nikita 5 Sozonov2,3, Shuhai Xiao4 and Dmitriy V. Grazhdankin2,3 . 6 7 [email protected] 8 9 1Department of Zoology, University of Cambridge, UK. 10 2Institute of Petroleum Geology and Geophysics, Novosibirsk, Russian Federation. 11 3Novosibirsk State University, Russian Federation. 12 4Department of Geosciences, Virginia Tech, Blacksburg, VA 24061, United States. 13 5 Department of Earth Sciences, Durham University, UK. 14 6Geological Institute, Russian Academy of Sciences, Moscow, Russian Federation. 15 7Department of Geography, Moscow Pedagogical State University, Moscow, Russian 16 Federation. 17 8Department of Chemical Engineering, University of Cambridge, UK. 18 9Current address: University College London, UCL Institute for Innovation and Public 19 Purpose, UK. 20 10Department of Earth Sciences, University of Cambridge, UK. 21 11Current address: Gripping Films, St. John's Church Road, London, England, E9 6EJ. 22 23 24 1 bioRxiv preprint doi: https://doi.org/10.1101/861906; this version posted December 2, 2019. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. -
Taphonomy of the Ediacaran Fossil Pteridinium Simplex Preserved Three
Taphonomy of the Ediacaran Fossil Pteridinium Simplex Preserved Three- Dimensionally in Mass Flow Deposits, Nama Group, Namibia Author(s): Mike Meyer , David Elliott , James D. Schiffbauer , Michael Hall , Karl H. Hoffman , Gabi Schneider , Patricia Vickers-Rich , and Shuhai Xiao Source: Journal of Paleontology, 88(2):240-252. 2014. Published By: The Paleontological Society DOI: http://dx.doi.org/10.1666/13-047 URL: http://www.bioone.org/doi/full/10.1666/13-047 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. Journal of Paleontology, 88(2), 2014, p. 240–252 Copyright Ó 2014, The Paleontological Society 0022-3360/14/0088-0240$03.00 DOI: 10.1666/13-047 TAPHONOMY OF THE EDIACARAN FOSSIL PTERIDINIUM SIMPLEX PRESERVED THREE-DIMENSIONALLY IN MASS FLOW DEPOSITS, NAMA GROUP, NAMIBIA MIKE MEYER,1,5 DAVID ELLIOTT,2 JAMES D. SCHIFFBAUER,3 MICHAEL HALL,2 KARL H. -
The Advent of Animals: the View from the Ediacaran SPECIAL FEATURE
The advent of animals: The view from the Ediacaran SPECIAL FEATURE Mary L. Drosera,1 and James G. Gehlingb,c aDepartment of Earth Sciences, University of California, Riverside, CA 92521; bSouth Australia Museum, Adelaide, SA 5000, Australia; and cUniversity of Adelaide, Adelaide, SA 5000, Australia Edited by Neil H. Shubin, The University of Chicago, Chicago, IL, and approved December 9, 2014 (received for review April 15, 2014) Patterns of origination and evolution of early complex life on this relationships within the Ediacara Biota and, importantly, reveals the planet are largely interpreted from the fossils of the Precam- morphologic disparity of these taxa. brian soft-bodied Ediacara Biota. These fossils occur globally and However, although fossils of the Ediacara Biota are not easily represent a diverse suite of organisms living in marine environments. classified with modern taxa, they nonetheless provide the record Although these exceptionally preserved fossil assemblages are typi- of early animals. One of the primary issues is that they are soft- cally difficult to reconcile with modern phyla, examination of the bodied and preserved in a manner that is, in many cases, unique to morphology, ecology, and taphonomy of these taxa provides keys to the Ediacaran. An alternative venue for providing insight into these their relationships with modern taxa. Within the more than 30 million organisms and the manner in which they fit into early animal evo- y range of the Ediacara Biota, fossils of these multicellular organisms lution is offered by examination of the paleoecology, morphology, demonstrate the advent of mobility, heterotrophy by multicellular and taphonomy of fossils of the Ediacara Biota. -
The Proterozoic Fossil Record of Heterotrophic Eukaryotes
Chapter 1 The Proterozoic Fossil Record of Heterotrophic Eukaryotes SUSANNAH M. PORTER Department of Earth Science, University of California, Santa Barbara, CA 93106, USA. 1. Introduction .................................................... 1 2. Eukaryotic Tree................................................. 2 3. Fossil Evidence for Proterozoic Heterotrophs ........................... 4 3.1. Opisthokonts ............................................... 4 3.2. Amoebozoa................................................ 5 3.3. Chromalveolates............................................ 7 3.4. Rhizaria................................................... 9 3.5. Excavates.................................................. 10 3.6. Summary.................................................. 10 4. Why Are Heterotrophs Rare in Proterozoic Rocks?........................ 12 5. Conclusions.................................................... 14 Acknowledgments.................................................. 15 References....................................................... 15 1. INTRODUCTION Nutritional modes of eukaryotes can be divided into two types: autotrophy, where the organism makes its own food via photosynthesis; and heterotrophy, where the organism gets its food from the environment, either by taking up dissolved organics (osmotrophy), or by ingesting particulate organic matter (phagotrophy). Heterotrophs dominate modern eukaryotic Neoproterozoic Geobiology and Paleobiology, edited by Shuhai Xiao and Alan Jay Kaufman, © 2006 Springer. Printed -
Mistaken Point, with Insets Showing Some of the Diverse Ediacaran Macrofossils Present at Mistake Point (Photo: A
Open File NFLD/3320 GEOLOGICAL ASSOCIATION OF CANADA Newfoundland and Labrador Section 2015 FALL FIELD TRIP The Ediacaran fossils of the Avalon Peninsula Alex G. Liu and James Conliffe with contributions from Liam Herringshaw, Jack Matthews, and Duncan McIlroy September 18–20th, 2015 Cover photo: Overview of the fossil bearing bedding planes at Mistaken Point, with insets showing some of the diverse Ediacaran macrofossils present at Mistake Point (photo: A. Liu) GAC Newfoundland and Labrador Section – 2015 Fall Field Trip Ediacaran macrofossils from the Mistaken Point ‘E’ Surface. 2 GAC Newfoundland and Labrador Section – 2015 Fall Field Trip TABLE OF CONTENTS INTRODUCTION AND OVERVIEW 4 ACKNOWLEDGEMENTS 4 SAFETY INFORMATION 5 MISTAKEN POINT ECOLOGICAL RESERVE (MPER) 7 PART 1: BACKGROUND MATERIAL 9 INTRODUCTION 9 Introduction to the Neoproterozoic‒Phanerozoic Transition 9 Stratigraphy, Structural Geology, and Depositional Environment of the Avalon Peninsula 13 EDICARAN PALEONTOLOGY OF THE AVALON PENINSULA 16 Preservation of Ediacaran macrofossils 16 The Avalon Assemblage 18 Current research into the Mistaken Point Ediacaran Fossils 21 PART 2: FIELD TRIP ITINERARY 24 Day One – Harbour Main and Spaniard’s Bay 25 Day Two – Mistaken Point Ecological Reserve 31 Day Three – Mistaken Point Ecological Reserve and Ferryland 46 INVENTORY OF TAXA IN MISTAKEN POINT ECOLOGICAL RESERVE 53 REFERENCES 54 3 GAC Newfoundland and Labrador Section – 2015 Fall Field Trip INTRODUCTION AND OVERVIEW The Mistaken Point Ecological Reserve (Fig. 1) is home to the some of the world’s most impressive Ediacaran fossil assemblages. Large bedding planes covered in thousands of exceptionally preserved specimens can be found in situ throughout a continuous ~2 km succession of sedimentary strata. -
1 New Occurrences of Palaeopascichnus from The
New occurrences of Palaeopascichnus from the Stáhpogieddi Formation, Arctic Norway, and their bearing on the age of the Varanger Ice Age Sören Jensen1, Anette E.S. Högström2, Magne Høyberget3, Guido Meinhold4,5, Duncan McIlroy6, Jan Ove R. Ebbestad7, Wendy L. Taylor8, Heda Agić9, and Teodoro Palacios1 1Área de Paleontología, University of Extremadura, E-06006 Badajoz, Spain. 2Tromsø University Museum, UiT the Arctic University of Norway, N-9037 Tromsø, Norway. 3Rennesveien 14, N-4513 Mandal, Norway. 4Geoscience Center, University of Göttingen, Goldschmidtstr. 3, 37077 Göttingen, Germany. 5School of Geography, Geology and the Environment, Keele University, Keele, Staffordshire, ST5 5BG, UK. 6Department of Earth Sciences, Memorial University of Newfoundland, St. John’s, NL, A1B 3X5, Canada. 7Museum of Evolution, Uppsala University, Norbyvägen 16, SE-752 36 Uppsala, Sweden. 8Department of Geological Sciences, University of Cape Town, Rondebosch 7701, Cape Town, South Africa. 9Department of Earth Science, University of California at Santa Barbara, 1006 Webb Hall, CA 93106 Santa Barbara, USA. Corresponding author: Sören Jensen (email: [email protected]) 1 Abstract: We report on new occurrences of the late Ediacaran problematicum Palaeopascichnus (Protista?) from the Stáhpogieddi Formation, Arctic Norway. The stratigraphically lowest occurrences are in beds transitional between the Lillevannet and Indreelva members: the highest in the second cycle of the Manndrapselva Member, stratigraphically close to the lowest occurrences of Cambrian-type trace fossils. This establishes a long stratigraphical range of Palaeopascichnus on the Digermulen Peninsula, as has been previously documented from Newfoundland, South Australia and elsewhere in Baltica. The age range of Palaeopascichnus in Avalonia and Baltica is ~565 to 541 Ma. -
Multicellular Life and Changes to Ecosystems
Evidence for Multicellular Life and Changes to Ecosystems 1 Microbial ecosystems • Microbialites are well known from 3.5 Ga to the present • >2000 fossil locations in WA • Photosynthesis at 2.4 Ga caused the Great Oxidation Event • Distribution now limited by grazers Stromatolite from Bitter Springs Formation (850 Ma), Amadeus Basin, Australia (J St John 2015, Creative Commons) Microbialites are deposits that have resulted from microbes trapping and binding sediment and/or precipitating minerals. These are possibly the first ecosystems on Earth. They include stromatolites, thrombolites, dendrolites and MISS (microbially induced sedimentary structures). The oldest microbialite fossils are from the Dresser Formation in the Pilbara, 3.5 billion years ago. Microbial mats were the dominant form of life for 3 billion years until the evolution of grazers severely limited their distribution. Microbialites are also a disaster fauna that moves into ecological sites during and after extinctions, but are normally limited by grazers. Although microbialite fossils are the result of many cells living together, they are not evidence of multicellular life. Microbial mats exhibit some specialisation, but not true multicellularity. 2 Early multicellular life • 2.1 Ga colonial organism, Gabon, Africa − Time of Great Oxidation Event 10 cm diameter fossil from − Trace fossils indicate possible Gabon. movement B Potin 2015, Creative Commons • 1.56 Ga seaweed (?), North China − Up to 30 cm long, 8 cm wide − Probably photosynthetic Linear (1) and tongue-shaped (2) fossils from Gauyuzhuang Formation. Coates et al 2015 https://doi.org/10.3389/fpls.2014.00737 Open Access Multicellular organisms have arisen independently in a variety of plant lineages, but probably only once in the animals.* The colonial organisms found in 2.1-billion-year-old Franceville deposits in Gabon appeared during the Great Oxidation Event. -
The Cambrian Evidence That Darwin Failed to Comprehend Years? Evolutionists Cannot Offer Any Logical Scenario to Answer That Question
First English Edition in November 2007 Translated by Carl Nino Rossini Edited by Tam Mossman Published by: GLOBAL PUBLISHING Talatpasa Mah. Emirgazi Caddesi Ibrahim Elmas ‹fl Merkezi A Blok Kat 4 Okmeydani - Istanbul / Turkey Phone: (+90 212) 222 00 88 Printed and bound by Secil Ofset in Istanbul 100 Yil Mah. MAS-SIT Matbaacilar Sitesi 4. Cadde No: 77 Bagcilar-Istanbul/Turkey Phone: (+90 212) 629 06 15 All translations from the Qur'an are from The Noble Qur'an: a New Rendering of its Meaning in English by Hajj Abdalhaqq and Aisha Bewley, published by Bookwork, Norwich, UK. 1420 CE/1999 AH. www.harunyahya.com - www.harunyahya.net 2 “The fossil record had caused Darwin more grief than joy. Nothing distressed him more than the Cambrian explosion, the coincident appearance of almost all complex organic designs.” (Stephen J. Gould) 3 About the Author Now writing under the pen-name of HARUN YAHYA, Adnan Oktar was born in Ankara in 1956. Having completed his primary and secondary educa- tion in Ankara, he studied arts at Istanbul's Mimar Si- nan University and philosophy at Istanbul University. Since the 1980s, he has published many books on po- litical, scientific, and faith-related issues. Harun Yahya is well-known as the author of important works dis- closing the imposture of evolutionists, their invalid claims, and the dark liaisons between Darwinism and such bloody ideologies as fascism and communism. Harun Yahya's works, translated into 57 different languages, constitute a collection for a total of more than 45,000 pages with 30,000 illustrations.