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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. -
Colonial Tunicates: Species Guide
SPECIES IN DEPTH Colonial Tunicates Colonial Tunicates Tunicates are small marine filter feeder animals that have an inhalant siphon, which takes in water, and an exhalant siphon that expels water once it has trapped food particles. Tunicates get their name from the tough, nonliving tunic formed from a cellulose-like material of carbohydrates and proteins that surrounds their bodies. Their other name, sea squirts, comes from the fact that many species will shoot LambertGretchen water out of their bodies when disturbed. Massively lobate colony of Didemnum sp. A growing on a rope in Sausalito, in San Francisco Bay. A colony of tunicates is comprised of many tiny sea squirts called zooids. These INVASIVE SEA SQUIRTS individuals are arranged in groups called systems, which form interconnected Star sea squirts (Botryllus schlosseri) are so named because colonies. Systems of these filter feeders the systems arrange themselves in a star. Zooids are shaped share a common area for expelling water like ovals or teardrops and then group together in small instead of having individual excurrent circles of about 20 individuals. This species occurs in a wide siphons. Individuals and systems are all variety of colors: orange, yellow, red, white, purple, grayish encased in a matrix that is often clear and green, or black. The larvae each have eight papillae, or fleshy full of blood vessels. All ascidian tunicates projections that help them attach to a substrate. have a tadpole-like larva that swims for Chain sea squirts (Botryloides violaceus) have elongated, less than a day before attaching itself to circular systems. Each system can have dozens of zooids. -
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. -
Extent and Duration of Marine Anoxia During the Frasnian– Famennian (Late Devonian) Mass Extinction in Poland, Germany, Austria and France
This is a repository copy of Extent and duration of marine anoxia during the Frasnian– Famennian (Late Devonian) mass extinction in Poland, Germany, Austria and France. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/297/ Article: Bond, D.P.G., Wignall, P.B. and Racki, G. (2004) Extent and duration of marine anoxia during the Frasnian– Famennian (Late Devonian) mass extinction in Poland, Germany, Austria and France. Geological Magazine, 141 (2). pp. 173-193. ISSN 0016-7568 https://doi.org/10.1017/S0016756804008866 Reuse See Attached Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ Geol. Mag. 141 (2), 2004, pp. 173–193. c 2004 Cambridge University Press 173 DOI: 10.1017/S0016756804008866 Printed in the United Kingdom Extent and duration of marine anoxia during the Frasnian– Famennian (Late Devonian) mass extinction in Poland, Germany, Austria and France DAVID BOND*, PAUL B. WIGNALL*† & GRZEGORZ RACKI‡ *School of Earth Sciences, University of Leeds, Leeds LS2 9JT, UK ‡Department of Palaeontology and Stratigraphy, University of Silesia, ul. Bedzinska 60, PL-41-200 Sosnowiec, Poland (Received 25 March 2003; accepted 10 November 2003) Abstract – The intensity and extent of anoxia during the two Kellwasser anoxic events has been investigated in a range of European localities using a multidisciplinary approach (pyrite framboid assay, gamma-ray spectrometry and sediment fabric analysis). -
SILURIAN TIMES NEWSLETTER of the INTERNATIONAL SUBCOMMISSION on SILURIAN STRATIGRAPHY (ISSS) (INTERNATIONAL COMMISSION on STRATIGRAPHY, ICS) No
SILURIAN TIMES NEWSLETTER OF THE INTERNATIONAL SUBCOMMISSION ON SILURIAN STRATIGRAPHY (ISSS) (INTERNATIONAL COMMISSION ON STRATIGRAPHY, ICS) No. 27 (for 2019) Edited by ZHAN Renbin INTERNATIONAL UNION OF GEOLOGICAL SCIENCES President: CHENG Qiuming (Canada) Vice-Presidents: Kristine ASCH (Germany) William CAVAZZA (Italy) Secretary General: Stanley C. FINNEY (USA) Treasurer: Hiroshi KITAZATO (Japan) INTERNATIONAL COMMISSION ON STRATIGRAPHY Chairman: David A.T. HARPER (UK) Vice-Chairman: Brian T. HUBER (USA) Secretary General: Philip GIBBARD (UK) SUBCOMMISSION ON SILURIAN STRATIGRAPHY Chairman: Petr ŠTORCH (Czech Republic) Vice-Chairman: Carlo CORRADINI (Italy) Secretary: ZHAN Renbin (China) Other titular members: Anna ANTOSHKINA (Russia) Carlton E. BRETT (USA) Bradley CRAMER (USA) David HOLLOWAY (Australia) Jisuo JIN (Canada) Anna KOZŁOWSKA (Poland) Jiří KŘÍŽ (Czech Republic) David K. LOYDELL (UK) Peep MÄNNIK (Estonia) Michael J. MELCHIN (Canada) Axel MUNNECKE (Germany) Silvio PERALTA (Argentina) Thijs VANDENBROUCKE (Belgium) WANG Yi (China) Živilė ŽIGAITĖ (Lithuania) Silurian Subcommission website: http://silurian.stratigraphy.org 1 CONTENTS CHAIRMAN’S CORNER 3 ANNUAL REPORT OF SILURIAN SUBCOMMISSION FOR 2019 7 INTERNATIONAL COMMISSION ON STRATGRAPHY STATUTES 15 REPORTS OF ACTIVITIES IN 2019 25 1. Report on the ISSS business meeting 2019 25 2. Report on the 15th International Symposium on Early/Lower Vertebrates 28 3. Report on the 13th International Symposium on the Ordovician System in conjunction with the 3rd Annual Meeting of IGCP 653 32 GUIDELINES FOR THE ISSS AWARD: KOREN' AWARD 33 ANNOUNCEMENTS OF MEETINGS and ACTIVITIES 34 1. Lithological Meeting: GEOLOGY OF REEFS 34 SILURIAN RESEARCH 2019: NEWS FROM THE MEMBERS 36 RECENT PUBLICATIONS ON THE SILURIAN RESEARCH 67 MEMBERSHIP NEWS 77 1. List of all Silurian workers and interested colleagues 77 2. -
Middle East Journal of Science (2018) 4(1):45-51
Middle East Journal of Science (2018) 4(1):45-51 INTERNATIONAL Middle East Journal of Science ENGINEERING, (2018) 4(1): 45 - 51 SCIENCE AND EDUCATION Published online JUNE, 2018 (http://dergipark.gov.tr/mejs) GROUP doi: 10.23884/mejs.2018.4.1.06 ISSN:2536-5312 Received: January 16, 2018 Accepted: May 03, 2018 MOLLUSCS: THEIR USAGE AS NUTRITION, MEDICINE, APHRODISIAC, COSMETIC, JEWELRY, COWRY, PEARL, ACCESSORY AND SO ON FROM THE HISTORY TO TODAY İhsan EKİN1*, Rıdvan ŞEŞEN2 1Department of Energy Systems Engineering, Faculty of Engineering, Şırnak University, Şırnak, Turkey 2Department of Biology, Faculty of Science, Dicle University, Diyarbakır, Turkey *Correspondence: e-mail: [email protected] Abstract:The present study has evaluated the usage and properties of the mollusca phylum from the history to today. Many types of molluscs are eaten worldwide, either cooked or raw due to their rich nutritional value. Furthermore, they are used as pearl, cowry and accessory materials, for tools like household dishes, cooking pots and utensils such as a spoon, cutlery, scoops, spatulas, etc. Some of them are destructive and caused ecological damage, some serve as intermediate hosts for human parasites; some can cause damage to crops. Mollusc meat is known to be highly nutritious and salutary owing to its high content of essential amino acids, proteins, fatty acids, vitamins, and minerals. In addition, some of the bioactive compounds including antiviral, antimicrobial, antiprotozoal, antifungal, antihelminthic and anticancer products are producing by molluscs as medicines. The largest edible snail is African land snail Achatina achatina mostly consumed by African people. Molluscs were very prominent dishes during the Roman Empire due to their aphrodisiac effect. -
Early Cretaceous) Wessex Formation of the Isle of Wight, Southern England
A new albanerpetontid amphibian from the Barremian (Early Cretaceous) Wessex Formation of the Isle of Wight, southern England STEVEN C. SWEETMAN and JAMES D. GARDNER Sweetman, S.C. and Gardner, J.D. 2013. A new albanerpetontid amphibian from the Barremian (Early Cretaceous) Wes− sex Formation of the Isle of Wight, southern England. Acta Palaeontologica Polonica 58 (2): 295–324. A new albanerpetontid, Wesserpeton evansae gen. et sp. nov., from the Early Cretaceous (Barremian) Wessex Formation of the Isle of Wight, southern England, is described. Wesserpeton is established on the basis of a unique combination of primitive and derived characters relating to the frontals and jaws which render it distinct from currently recognized albanerpetontid genera: Albanerpeton (Late Cretaceous to Pliocene of Europe, Early Cretaceous to Paleocene of North America and Late Cretaceous of Asia); Celtedens (Late Jurassic to Early Cretaceous of Europe); and Anoualerpeton (Middle Jurassic of Europe and Early Cretaceous of North Africa). Although Wesserpeton exhibits considerable intraspecific variation in characters pertaining to the jaws and, to a lesser extent, frontals, the new taxon differs from Celtedens in the shape of the internasal process and gross morphology of the frontals in dorsal or ventral view. It differs from Anoualerpeton in the lack of pronounced heterodonty of dentary and maxillary teeth; and in the more medial loca− tion and direction of opening of the suprapalatal pit. The new taxon cannot be referred to Albanerpeton on the basis of the morphology of the frontals. Wesserpeton currently represents the youngest record of Albanerpetontidae in Britain. Key words: Lissamphibia, Albanerpetontidae, microvertebrates, Cretaceous, Britain. Steven C. -
The Pax Gene Family: Highlights from Cephalopods Sandra Navet, Auxane Buresi, Sébastien Baratte, Aude Andouche, Laure Bonnaud-Ponticelli, Yann Bassaglia
The Pax gene family: Highlights from cephalopods Sandra Navet, Auxane Buresi, Sébastien Baratte, Aude Andouche, Laure Bonnaud-Ponticelli, Yann Bassaglia To cite this version: Sandra Navet, Auxane Buresi, Sébastien Baratte, Aude Andouche, Laure Bonnaud-Ponticelli, et al.. The Pax gene family: Highlights from cephalopods. PLoS ONE, Public Library of Science, 2017, 12 (3), pp.e0172719. 10.1371/journal.pone.0172719. hal-01921138 HAL Id: hal-01921138 https://hal.archives-ouvertes.fr/hal-01921138 Submitted on 13 Nov 2018 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Distributed under a Creative Commons Attribution| 4.0 International License RESEARCH ARTICLE The Pax gene family: Highlights from cephalopods Sandra Navet1☯, Auxane Buresi1☯, SeÂbastien Baratte1,2, Aude Andouche1, Laure Bonnaud-Ponticelli1, Yann Bassaglia1,3* 1 UMR BOREA MNHN/CNRS7208/IRD207/UPMC/UCN/UA, MuseÂum National d'Histoire Naturelle, Sorbonne UniversiteÂs, Paris, France, 2 Univ. Paris Sorbonne-ESPE, Sorbonne UniversiteÂs, Paris, France, 3 Univ. Paris Est CreÂteil-Val de Marne, CreÂteil, France ☯ These authors contributed equally to this work. * [email protected] a1111111111 a1111111111 a1111111111 a1111111111 Abstract a1111111111 Pax genes play important roles in Metazoan development. Their evolution has been exten- sively studied but Lophotrochozoa are usually omitted. -
Yaksha Perettii
Yaksha perettii Yaksha perettii is an extinct species of albanerpetontid amphibian, and the only species in the genus Yaksha. It is known from three Yaksha perettii specimens found in Cenomanian aged Burmese amber from Temporal range: Early Cenomanian Myanmar. The remains of Yaksha perettii are the best preserved of 99 Ma all albanerpetontids, which usually consist of isolated fragments or ↓ crushed flat, and have provided significant insights in the PreꞒ Ꞓ O S D C P T J K PgN morphology and lifestyle of the group. Contents Etymology Discovery Description Phylogeny Holotype skull of Yaksha perettii, dark References grey represents preserved soft tissue Scientific classification Etymology Kingdom: Animalia Phylum: Chordata The generic epithet is named after the Yaksha, a class of nature Class: Amphibia and guardian spirits in Indian religions, while the specific epithet honors Dr. Adolf Peretti, who provided some of the specimens, Order: †Allocaudata including the holotype.[1] Family: †Albanerpetontidae Discovery Genus: †Yaksha Daza et al, 2020 The paratype specimen was originally described in 2016 amongst Species: †Y. perettii a collection of fossil lizard species from Burmese amber, and was initially identified as a stem-chameleon.[2] However Professor Binomial name Susan E. Evans, a researcher who has extensively worked on †Yaksha perettii albanerpetontids, recognised the specimen as belonging to the Daza et al, 2020 group.[3] Subsequently, another specimen was discovered in the collection of gemologist Dr. Adolf Peretti, which would later become the holotype specimen.[4] The paper describing Yaksha perettii was published in November 2020 in the journal Science.[1] Description The species is known from three specimens, the small juvenile skeleton described in the 2016 paper (JZC Bu154), a complete adult skull and lower jaws (GRS-Ref-060829), and a partial adult postcranium (GRSRef- 27746). -
The Cambrian Explosion: a Big Bang in the Evolution of Animals
The Cambrian Explosion A Big Bang in the Evolution of Animals Very suddenly, and at about the same horizon the world over, life showed up in the rocks with a bang. For most of Earth’s early history, there simply was no fossil record. Only recently have we come to discover otherwise: Life is virtually as old as the planet itself, and even the most ancient sedimentary rocks have yielded fossilized remains of primitive forms of life. NILES ELDREDGE, LIFE PULSE, EPISODES FROM THE STORY OF THE FOSSIL RECORD The Cambrian Explosion: A Big Bang in the Evolution of Animals Our home planet coalesced into a sphere about four-and-a-half-billion years ago, acquired water and carbon about four billion years ago, and less than a billion years later, according to microscopic fossils, organic cells began to show up in that inert matter. Single-celled life had begun. Single cells dominated life on the planet for billions of years before multicellular animals appeared. Fossils from 635,000 million years ago reveal fats that today are only produced by sponges. These biomarkers may be the earliest evidence of multi-cellular animals. Soon after we can see the shadowy impressions of more complex fans and jellies and things with no names that show that animal life was in an experimental phase (called the Ediacran period). Then suddenly, in the relatively short span of about twenty million years (given the usual pace of geologic time), life exploded in a radiation of abundance and diversity that contained the body plans of almost all the animals we know today. -
Biology Chapter 19 Kingdom Protista Domain Eukarya Description Kingdom Protista Is the Most Diverse of All the Kingdoms
Biology Chapter 19 Kingdom Protista Domain Eukarya Description Kingdom Protista is the most diverse of all the kingdoms. Protists are eukaryotes that are not animals, plants, or fungi. Some unicellular, some multicellular. Some autotrophs, some heterotrophs. Some with cell walls, some without. Didinium protist devouring a Paramecium protist that is longer than it is! Read about it on p. 573! Where Do They Live? • Because of their diversity, we find protists in almost every habitat where there is water or at least moisture! Common Examples • Ameba • Algae • Paramecia • Water molds • Slime molds • Kelp (Sea weed) Classified By: (DON’T WRITE THIS DOWN YET!!! • Mode of nutrition • Cell walls present or not • Unicellular or multicellular Protists can be placed in 3 groups: animal-like, plantlike, or funguslike. Didinium, is a specialist, only feeding on Paramecia. They roll into a ball and form cysts when there is are no Paramecia to eat. Paramecia, on the other hand are generalists in their feeding habits. Mode of Nutrition Depends on type of protist (see Groups) Main Groups How they Help man How they Hurt man Ecosystem Roles KEY CONCEPT Animal-like protists = PROTOZOA, are single- celled heterotrophs that can move. Oxytricha Reproduce How? • Animal like • Unicellular – by asexual reproduction – Paramecium – does conjugation to exchange genetic material Animal-like protists Classified by how they move. macronucleus contractile vacuole food vacuole oral groove micronucleus cilia • Protozoa with flagella are zooflagellates. – flagella help zooflagellates swim – more than 2000 zooflagellates • Some protists move with pseudopods = “false feet”. – change shape as they move –Ex. amoebas • Some protists move with pseudopods.