The Snodgrass Tapes Evolution of the Arthropods Robert Evans Snodgrass Page 1 Figure 1
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Early Fossil Record of Euarthropoda and the Cambrian Explosion
PERSPECTIVE Early fossil record of Euarthropoda and the Cambrian Explosion PERSPECTIVE Allison C. Daleya,b,c,1, Jonathan B. Antcliffea,b,c, Harriet B. Dragea,b,c, and Stephen Patesa,b Edited by Neil H. Shubin, University of Chicago, Chicago, IL, and approved April 6, 2018 (received for review December 20, 2017) Euarthropoda is one of the best-preserved fossil animal groups and has been the most diverse animal phylum for over 500 million years. Fossil Konservat-Lagerstätten, such as Burgess Shale-type deposits (BSTs), show the evolution of the euarthropod stem lineage during the Cambrian from 518 million years ago (Ma). The stem lineage includes nonbiomineralized groups, such as Radiodonta (e.g., Anomalocaris) that provide insight into the step-by-step construction of euarthropod morphology, including the exo- skeleton, biramous limbs, segmentation, and cephalic structures. Trilobites are crown group euarthropods that appear in the fossil record at 521 Ma, before the stem lineage fossils, implying a ghost lineage that needs to be constrained. These constraints come from the trace fossil record, which show the first evi- dence for total group Euarthropoda (e.g., Cruziana, Rusophycus) at around 537 Ma. A deep Precambrian root to the euarthropod evolutionary lineage is disproven by a comparison of Ediacaran and Cambrian lagerstätten. BSTs from the latest Ediacaran Period (e.g., Miaohe biota, 550 Ma) are abundantly fossilif- erous with algae but completely lack animals, which are also missing from other Ediacaran windows, such as phosphate deposits (e.g., Doushantuo, 560 Ma). This constrains the appearance of the euarthropod stem lineage to no older than 550 Ma. -
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. -
Gehling-Ediacaran Publications 2015 Palaeo Down Under2
Gehling-Ediacaran Publications 2015 1. Droser, M.L. and Gehling, J.G. 2015. The advent of animals: the view from the Ediacaran: Proceedings of the National Academy of Sciences 112, 4865-4870. 2. Evans, S.D., Droser, M.L. and Gehling, J.G. 2015. Dickinsonia lift off: Evidence of current derived morphologies. Palaeogeography Palaeoclimatology Palaeoecology ; DOI: 10.1016/j.palaeo.2015.02.006. 3. Hall, C.M.S., Droser, M.L., Gehling, J.G., Dzaugis. M.E. 2015. Paleoecology of the enigmatic Tribrachidium: New data from the Ediacaran of South Australia. Precambrian Research 269:183-194. 4. Gold, D. A., Runnegar, B., Gehling, J.G., and Jacobs, D.K. 2015. Ancestral state reconstruction of ontogeny supports a bilaterian affinity for Dickinsonia. Evolution and Development 17 (6), 315–397. 5. Tarhan, L.G., Droser, M.L. and Gehling, J.G. 2015. Taphonomy and morphology of the Ediacara form genus Aspidella. Precambrian Research 257:124-136. 6. Tarhan, L.G., Droser, M.L. and Gehling, J.G. 2015. Depositional and preservational environments of the Ediacara Member, Rawnsley Quartzite (South Australia): Assessment of paleoenvironmental proxies and the timing of ‘ferruginization’. Palaeogeography, Palaeclimatology, Paleoecology in press. Palaeo Down Under2 — July 2016 Association of Australasian Palaeontologists (AAP) is organizing a Palaeo Down Under 2 conference at the University of Adelaide in South Australia from July 10-15. The conference is preceded by a Field Excursion to key Cambrian localities of Kangaroo Island, the Fleurieu Peninsula and the Cambrian and Ediacaran of the Flinders Ranges from July 3-9. Ediacara Research — South Australia 2015 Ediacara research in South Australia has continued with further excavations at the National Heritage Listed Ediacara Fossil Site at Nilpena, a new site in the northern Flinders Ranges of South Australia, and for the first time, at the historic discovery site in the Ediacara Conservation Park. -
The Origin and Evolution of Arthropods Graham E
INSIGHT REVIEW NATURE|Vol 457|12 February 2009|doi:10.1038/nature07890 The origin and evolution of arthropods Graham E. Budd1 & Maximilian J. Telford2 The past two decades have witnessed profound changes in our understanding of the evolution of arthropods. Many of these insights derive from the adoption of molecular methods by systematists and developmental biologists, prompting a radical reordering of the relationships among extant arthropod classes and their closest non-arthropod relatives, and shedding light on the developmental basis for the origins of key characteristics. A complementary source of data is the discovery of fossils from several spectacular Cambrian faunas. These fossils form well-characterized groupings, making the broad pattern of Cambrian arthropod systematics increasingly consensual. The arthropods are one of the most familiar and ubiquitous of all ani- Arthropods are monophyletic mal groups. They have far more species than any other phylum, yet Arthropods encompass a great diversity of animal taxa known from the living species are merely the surviving branches of a much greater the Cambrian to the present day. The four living groups — myriapods, diversity of extinct forms. One group of crustacean arthropods, the chelicerates, insects and crustaceans — are known collectively as the barnacles, was studied extensively by Charles Darwin. But the origins Euarthropoda. They are united by a set of distinctive features, most and the evolution of arthropods in general, embedded in what is now notably the clear segmentation of their bodies, a sclerotized cuticle and known as the Cambrian explosion, were a source of considerable con- jointed appendages. Even so, their great diversity has led to consider- cern to him, and he devoted a substantial and anxious section of On able debate over whether they had single (monophyletic) or multiple the Origin of Species1 to discussing this subject: “For instance, I cannot (polyphyletic) origins from a soft-bodied, legless ancestor. -
H1.1 Open Water
PAGE .............................................................. 392 ▼ H1.1 OPEN WATER The open-water offshore habitat covers an area of by which solar energy enters the marine ecosystem, Nova Scotia larger than the land mass, and includes similar to the layer of plants on land. The ocean H1.1 Open Water salt water in inlets, bays and estuaries. The water waters are distinctive in having fostered the origins and the organisms it supports are the primary means of life on the planet. Plate H1.1.1: Right Whale, north of Brier Island (Unit 912). Photo: BIOS Habitats Natural History of Nova Scotia, Volume I © Nova Scotia Museum of Natural History .............................................................. PAGE 393 ▼ FORMATION PLANTS Oceans are formed as part of major geological events. The plants of the open ocean are almost entirely Nova Scotia’s open-ocean habitats are part of the microscopic algae, collectively known as phyto- Atlantic Ocean, which opened during the Jurassic plankton. Many different species occur, including Period and has been in continuous existence ever representatives of the prochlorophytes (blue-green since. The quality and depth of the water column algae—evolutionary intermediates between bacteria have fluctuated in relation to post-glacial climatic and algae), diatoms, dinoflagellates, chrysomonads, conditions. cryptomonads, minute flagellates and unicellular reproductive stages of macroscopic algae. Phyto- H1.1 PHYSICAL ASPECTS plankton are often grouped in size classes: Open Water 1. Water conditions, such as salinity, temperature, macroplankton: 200–2000 micrometres, includes ice-formation, turbidity, light penetration, tides larger diatoms. and currents, are extremely variable in the microplankton: 20–200 micrometres, includes waters offshore. most diatoms. 2. Air-water interaction, surface-water turbulence nanoplankton: 2–20 micrometres, includes determines the level of wave and gas exchange. -
Australia's National Heritage
Ediacara Fossils ▲ Date of inscription: 11 January 2007 78 AUSTRALIA’S NATIONAL HERITAGE Ediacara Fossil Site – Nilpena, South Australia Today Australia is a hot, dry continent but hundreds of millions of years ago the landscape was very different – most of eastern Australia lay under shallow, warm seas. Between 570 and 540 million years ago (long before Some scientists believe many of the organisms dinosaurs roamed the Earth) these warm seas were found at Ediacara may represent early algae, lichens inhabited by soft bodied organisms, similar to jellyfi sh. or even multicellular ‘experiments’, which bear little resemblance to organisms existing anywhere Some of these organisms became trapped in fi ne silt in the world today. There are many questions that in tidal fl ats and were fossilised as the silt turned to surrounding these ancient organisms; how they lived, stone. As sea levels changed, the seafl oor become part how they evolved and what creatures alive today are of what we today know as the Flinders Ranges in their descendents. South Australia, and the fossils found there formed part of a period known today as the Ediacaran Period. The fossils of this period resemble the fl atworms, Examples of these unusual and fragile fossils, including soft corals and jellyfi sh we know today and range in Dickinsonia and Spriggina can be seen at the South size from a few centimetres up to a metre long. This Australian Museum. diverse array of fossil specimens includes anemones, annelid worms, crustaceans, echinoderms and possible In 1946, while exploring for minerals, geologist ancestors of trilobites. -
OREGON ESTUARINE INVERTEBRATES an Illustrated Guide to the Common and Important Invertebrate Animals
OREGON ESTUARINE INVERTEBRATES An Illustrated Guide to the Common and Important Invertebrate Animals By Paul Rudy, Jr. Lynn Hay Rudy Oregon Institute of Marine Biology University of Oregon Charleston, Oregon 97420 Contract No. 79-111 Project Officer Jay F. Watson U.S. Fish and Wildlife Service 500 N.E. Multnomah Street Portland, Oregon 97232 Performed for National Coastal Ecosystems Team Office of Biological Services Fish and Wildlife Service U.S. Department of Interior Washington, D.C. 20240 Table of Contents Introduction CNIDARIA Hydrozoa Aequorea aequorea ................................................................ 6 Obelia longissima .................................................................. 8 Polyorchis penicillatus 10 Tubularia crocea ................................................................. 12 Anthozoa Anthopleura artemisia ................................. 14 Anthopleura elegantissima .................................................. 16 Haliplanella luciae .................................................................. 18 Nematostella vectensis ......................................................... 20 Metridium senile .................................................................... 22 NEMERTEA Amphiporus imparispinosus ................................................ 24 Carinoma mutabilis ................................................................ 26 Cerebratulus californiensis .................................................. 28 Lineus ruber ......................................................................... -
What Came Before the Cambrian Explosion
What Came Before the Cambrian? Advanced Reading The Cambrian Explosion was an era of significant evolution of animal life. What came before the Cambrian era that, in a sense, opened the door for the new body forms to evolve? The geologic era before the Cambrian was called the Ediacran, lasting from about 635 to 542 million years ago. Scientists often characterize this era as an “experimental” phase in the evolution of animals. By this time unicellular life had been around for millions of years and a mat of microbes covered parts of the seafloor. The first multicellular animals that evolved could have grazed on those microbes. The fossils from the Ediacran mostly show soft-bodied organisms. Some of these fossils look like fronds, discs and blobs, and aren’t easy to identify. Others seem to be related to Cnidarians or to be soft-bodied relatives of arthropods or perhaps Echinoderms. In addition, there are trace fossils, probably made by worm-like creatures. Many of the fossil animals remain mysterious and may represent lines of animals that no longer exist. But fossils are not the only evidence of animal life in the Ediacran. In fact the first evidence of sponges is not a body fossil but rather a biochemical fossil. When an animal dies, some of its molecules break down into a stable form that can last in rocks for millions of years just like body fossils. These are biochemical fossils. Scientists have found an Ediacran biochemical fossil of a fat molecule found today only in sponges. The name Ediacran comes from the Ediacra Hills of South Australia, the most famous location of these fossils. -
(Polychaeta) Borings in Paraspirifer Bownockeri (Brachiopoda: Devonian)1
114 A. E. ANNALA AND L. A. KAPUSTKA Vol. 83 Copyright © 1983 Ohio Acad. Sci. 003O-O95O/83/0003-O114 $2.00/0 VERMIFORICHNUS (POLYCHAETA) BORINGS IN PARASPIRIFER BOWNOCKERI (BRACHIOPODA: DEVONIAN)1 R. D. HOARE and R. L. WALDEN, Department of Geology, Bowling Green State University, Bowling Green, OH 43403 ABSTRACT. Shells of Paraspirifer bownockeri (Stewart) from the Silica Formation, Middle Devonian of northwestern Ohio, commonly contain numerous borings of a polychaete worm forming the endolithic trace fossil Vermiforichnus clarki Cameron (1969a) which can be exposed by acidizing the specimens. The borings are most abundant on the brachial valve, and their surface openings tend to be concentrated along major growth lines thence extending dominantly in the general direction of the beaks of the valves. In- festations of the polychaete occurred at 2 different time intervals as indicated by the spac- ing of the borings on 2 major growth lines with renewed shell growth between them. Growth of the host was severely reduced immediately following the infestation and in some areas damage to the mantle caused deformation in the shell of the host. OHIO J. SCI. 83 (3): 114-119, 1983 INTRODUCTION (1932) by Hoare and Steller (1967) (fig. 1), Previous interpretations of the larger as boring sponges by Kesling and Chilman borings commonly seen in the brachiopod (1975) and as "Clionoides" sp. by Steller Paraspirifer bownockeri (Stewart) from the (1965), Kesling et al. (1980) and Sparks Silica Formation in northwestern Ohio et al. (1980). These interpretations were have been alluded to as sponge borings, based on the external configuration of the Clionoides thomasi Fenton and Fenton surface opening of the boring only. -
The Presence of Melinna Palmata (Annelida: Polychaeta) and Ensis
Cah. Biol. Mar. (2007) 48 : 391-401 The presence of Melinna palmata (Annelida: Polychaeta) and Ensis directus (Mollusca: Bivalvia) related to sedimentary changes in the Bay of Seine (English Channel, France) Jean-Claude DAUVIN1*, Thierry RUELLET1, Eric THIEBAUT2, Franck GENTIL2, Nicolas DESROY3, Anne-Laure JANSON4, Sylvain DUHAMEL5, Jérôme JOURDE5 and Serge SIMON5 (1) Station Marine de Wimereux, Université des Sciences et Technologies de Lille, FRE CNRS 2816 ELICO, B.P. 80, 62930 Wimereux, France. *Corresponding author: Fax: 33 3 21 99 29 01, E-mail: [email protected] (2) Université Pierre et Marie Curie-Paris 6, Station Biologique de Roscoff, UMR CNRS 7144, B.P. 74, 29682 Roscoff Cedex, France (3) Station IFREMER, 2 bis rue Saint-Georges, B.P. 46, 35042 Saint-Malo Cedex, France (4) Muséum National d’Histoire Naturelle, Département Milieux et Peuplements Aquatiques CNRS UMR 5178 BOME, 61 rue Buffon, 75005 Paris, France (5) Cellule du Suivi du Littoral Normand, 16 quai Casimir Delavigne, 76600 Le Havre, France Abstract: Since late 1990s the annelid polychaete Melinna palmata and the mollusc bivalve Ensis directus have been collected in the eastern part of the Bay of Seine (English Channel), indicating changes in the benthic communities. Melinna palmata was never collected prior to 2002, whereas it was reported in the muddy fine sands of the western part of the Channel, along the French (e.g. Bay of Cherbourg) and southern UK (e.g. Southampton Waters) coasts. Ensis directus was first reported in 1998 and now appears to be well implanted, given the abundant population collected in 2006. -
Identification Guide to the Planktonic Polychaete Larvae Around the Island of Helgoland (German Bight)
HELGOL.~NDER MEERESUNTERSUCHUNGEN Helgol/inder Meeresunters. 48, 1-58 (1994) Identification guide to the planktonic polychaete larvae around the island of Helgoland (German Bight) S. Plate* & E. Husemann* * Biologische Anstalt Helgoland (Meeresstation); D-27483 Helgoland, Federal Republic of Germany ABSTRACT: The purpose of this work is to provide the means of identifying the planktonic larvae of the polychaete species appearing in the plankton around the island of Helgoland (North Sea). During a three-year survey in this area, the larvae of 54 species out of 24 families belonging to the orders Orbiniida, Spionida, Capitelhda, Phyllodocida, Oweniida, Terebelhda, Sabelhda and the former Archiannelida have been recorded. Illustrated keys to the families, genera and species are presented. To facilitate the identification, additional descriptions and information about the seasonal appearance of the species are given. INTRODUCTION More than 13 000 species of polychaetous annelids take part in the marine benthos communities worldwide. Their distribution, species composition and population density are monitored within various benthos surveys. For the North Sea, especially the German Bight and the Wadden Sea, much information about the benthic polychaete fauna is available (Caspers, 1950; Stripp, 1969; DSrjes, 1977; Rachor & Gerlach, 1978; Gillandt, 1979; Salzwedel et al., 1985; Rachor, 1990; Bosselmann, 1991; Kr6ncke, 1991). In contrast, the holoplanktonic polychaete species and the meroplanktonic polychaete larvae, which are only part of the plankton during a more or less expanded phase of their ontogenesis, have never received much attention. Meroplanktonic polychaete larvae are seldomly recorded during studies monitoring the North Sea plankton (Smidt, 1951; Giere, 1968; Fransz, 1981; Bosselmann, 1989; Belgrano et al., 1990). -
Pre-Cambrian Animals
Pre-Canlbrian AniIllals Until recently the fossils of organlsms that lil'ed earlier than the Cambrian period of 500 to 600 million years ago were rare. LVOW a wealth of such fossils has. been found in South Australia by Martin F. Clae;;sner he successive strata of sedimentary forming process affects the entire surface isms may have lived at the surface of the Trock laid down on the earth's crust of the globe. Some Pre-Cambrian forma sea and none on its bottom, or all in the in the course of geologic time pre tions have escaped extreme alteration, deep sea and none on its shores. serve a rich record of the succession of just as the lower Cambrian rocks are al The need for such speculation has at living organisms. Fossils embedded in tered in some places and not in others. last been obviated by the discovery in these rocks set apart the last 60 million The abrupt termination of the fossil the Ediacara Hills in South Australia years as the Cenozoic era-the age of record at the boundary between the of a rich deposit of Pre-Cambrian fos mammals. The next lower strata contain Cambrian and the Pre-Cambrian has ap sils. The first finds at this site were the l50-million-year history of the Meso peared to many observers as a fact or made in 1947 by the Australian geologist zoic-the age of reptiles. Before that paradox of decisive importance. They R. C. Sprigg. In sandstones that were comes the still longer record of the Pale have advanced many different explana thought to belong to the lowest strata ozoic, which leads backward through the tions for the mystery, from cosmic catas of the Cambrian he came upon varieties age of amphibians and the age of fishes trophes to the postulate of an interval of fossil jellyfish.