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Bryozoan Studies 2019
BRYOZOAN STUDIES 2019 Edited by Patrick Wyse Jackson & Kamil Zágoršek Czech Geological Survey 1 BRYOZOAN STUDIES 2019 2 Dedication This volume is dedicated with deep gratitude to Paul Taylor. Throughout his career Paul has worked at the Natural History Museum, London which he joined soon after completing post-doctoral studies in Swansea which in turn followed his completion of a PhD in Durham. Paul’s research interests are polymatic within the sphere of bryozoology – he has studied fossil bryozoans from all of the geological periods, and modern bryozoans from all oceanic basins. His interests include taxonomy, biodiversity, skeletal structure, ecology, evolution, history to name a few subject areas; in fact there are probably none in bryozoology that have not been the subject of his many publications. His office in the Natural History Museum quickly became a magnet for visiting bryozoological colleagues whom he always welcomed: he has always been highly encouraging of the research efforts of others, quick to collaborate, and generous with advice and information. A long-standing member of the International Bryozoology Association, Paul presided over the conference held in Boone in 2007. 3 BRYOZOAN STUDIES 2019 Contents Kamil Zágoršek and Patrick N. Wyse Jackson Foreword ...................................................................................................................................................... 6 Caroline J. Buttler and Paul D. Taylor Review of symbioses between bryozoans and primary and secondary occupants of gastropod -
Mammal Footprints from the Miocene-Pliocene Ogallala
Mammalfootprints from the Miocene-Pliocene Ogallala Formation, easternNew Mexico by ThomasE. Williamsonand SpencerG. Lucas, New Mexico Museum of Natural History and Science,1801 Mountain Road NW Albuquerque, New Mexico 87104-7375 Abstract well-develooed mudcracks. The track- ways are diveloped on the mudstone Mammal trackways preserved in the drape but are preserved as infillings at the Miocene-Pliocene Ogallala Formation of base of the overlying conglomerate (Figs. eastern New Mexico represent the first 2-4). Most tracks are preserved on the report of mammal fossils-from this unit in underside of a single, thick conglomerate New Mexico. These trackwavs are Dre- block (Fig. 3). A few isolated mammal served as infillings in a conglomerate near the base of the Ogallala Formation. At least prints were also observed on the under- four mammalian ichnotaxa are represented, side of adjacent blocks.he depth of the including a single trackway of a large camel infillings suggest that tracks were made in (Gambapessp. A), several prints of an uncer- a relatively soft substrate. Some prints are tain family of artiodactyl (Gambapessp B), a accompanied by marks indicating slip- single trackway of a large feloid carnivoran page on a slick, wet substrate (Fig. 5C). (Bestiopeda sp.), and several indistinct im- Infillings of mudcracks and narrow, cylin- pressions, probably representing more than drical burrows and raindrop impressions one trackway of a small canid carnivoran are Dreserved over some areas of the (Chelipus sp ). The footprints are preserved in a channel-margin facies of an Ogallala tracliway slab. Mammal trackways repre- braided stream. sent at least four ichnotaxa. -
71St Annual Meeting Society of Vertebrate Paleontology Paris Las Vegas Las Vegas, Nevada, USA November 2 – 5, 2011 SESSION CONCURRENT SESSION CONCURRENT
ISSN 1937-2809 online Journal of Supplement to the November 2011 Vertebrate Paleontology Vertebrate Society of Vertebrate Paleontology Society of Vertebrate 71st Annual Meeting Paleontology Society of Vertebrate Las Vegas Paris Nevada, USA Las Vegas, November 2 – 5, 2011 Program and Abstracts Society of Vertebrate Paleontology 71st Annual Meeting Program and Abstracts COMMITTEE MEETING ROOM POSTER SESSION/ CONCURRENT CONCURRENT SESSION EXHIBITS SESSION COMMITTEE MEETING ROOMS AUCTION EVENT REGISTRATION, CONCURRENT MERCHANDISE SESSION LOUNGE, EDUCATION & OUTREACH SPEAKER READY COMMITTEE MEETING POSTER SESSION ROOM ROOM SOCIETY OF VERTEBRATE PALEONTOLOGY ABSTRACTS OF PAPERS SEVENTY-FIRST ANNUAL MEETING PARIS LAS VEGAS HOTEL LAS VEGAS, NV, USA NOVEMBER 2–5, 2011 HOST COMMITTEE Stephen Rowland, Co-Chair; Aubrey Bonde, Co-Chair; Joshua Bonde; David Elliott; Lee Hall; Jerry Harris; Andrew Milner; Eric Roberts EXECUTIVE COMMITTEE Philip Currie, President; Blaire Van Valkenburgh, Past President; Catherine Forster, Vice President; Christopher Bell, Secretary; Ted Vlamis, Treasurer; Julia Clarke, Member at Large; Kristina Curry Rogers, Member at Large; Lars Werdelin, Member at Large SYMPOSIUM CONVENORS Roger B.J. Benson, Richard J. Butler, Nadia B. Fröbisch, Hans C.E. Larsson, Mark A. Loewen, Philip D. Mannion, Jim I. Mead, Eric M. Roberts, Scott D. Sampson, Eric D. Scott, Kathleen Springer PROGRAM COMMITTEE Jonathan Bloch, Co-Chair; Anjali Goswami, Co-Chair; Jason Anderson; Paul Barrett; Brian Beatty; Kerin Claeson; Kristina Curry Rogers; Ted Daeschler; David Evans; David Fox; Nadia B. Fröbisch; Christian Kammerer; Johannes Müller; Emily Rayfield; William Sanders; Bruce Shockey; Mary Silcox; Michelle Stocker; Rebecca Terry November 2011—PROGRAM AND ABSTRACTS 1 Members and Friends of the Society of Vertebrate Paleontology, The Host Committee cordially welcomes you to the 71st Annual Meeting of the Society of Vertebrate Paleontology in Las Vegas. -
Growth Geometry and Measurement of Growth Rates in Marine Bryozoans: a Review
BRYOZOAN STUDIES 2019 Growth geometry and measurement of growth rates in marine bryozoans: a review Abigail M. Smith1* and Marcus M. Key, Jr.2 1 Department of Marine Science, University of Otago, P.O. Box 56, Dunedin 9054, New Zealand [*corresponding author: email: [email protected]] 2 Department of Earth Sciences, Dickinson College, P.O. Box 1773, Carlisle, PA 17013-2896, USA ABSTRACT measuring and reporting growth rate in bryozoans The relationship between age and size in colonial will ensure they are robust and comparable. marine organisms is problematic. While growth of individual units may be measured fairly easily, the growth of colonies can be variable, complex, and INTRODUCTION difficult to measure. We need this information in Bryozoans are lophophorate aquatic invertebrates order to manage and protect ecosystems, acquire which typically form colonies by iterative addition bioactive compounds, and understand the history of of modular clones (zooids). Freshwater species environmental change. Bryozoan colonial growth are uncalcified; the majority of marine species are forms, determined by the pattern of sequential calcified, so that there is an extensive fossil record of addition of zooids or modules, enhance feeding, marine bryozoan colonies. When calcified colonies colony integration, strength, and/or gamete/larval grow large, they can provide benthic structures dispersal. Colony age varies from three months to which enhance biodiversity by provision of sheltered 86 years. Growth and development, including both habitat. Agencies who wish to manage or protect addition of zooids and extrazooidal calcification, these productive habitats need to understand the can be linear, two-dimensional across an area, or longevity and stability of these structures. -
Phytoliths of the Barstow Formation Through the Middle Miocene Climatic Optimum: Preliminary Findings Katharine M
Phytoliths of the Barstow Formation through the Middle Miocene Climatic Optimum: preliminary findings Katharine M. Loughney 1,2 and Selena Y. Smith 1, 1 Museum of Paleontology, University of Michigan, 1109 Geddes Ave., Ann Arbor, MI 48109 2 Department of Earth & Environmental Sciences, University of Michigan, 1100 North University Ave., Ann Arbor, MI 48109 abstract—The Middle Miocene Climatic Optimum (MMCO) was an interval of signif- icant warming between 17.0 – 14.0 Ma, and a record of the interval is preserved in its entirety in the type Barstow Formation (19.3 – 13.3 Ma) of southern California. In order to understand the biotic impacts of the MMCO, it is necessary to understand vegetation; however, macrofloral records from the middle Miocene in this region are rare and do not span the MMCO. Phytoliths (plant silica) can be preserved in continental sediments even when macrofossil or pollen remains are not, and they can be diagnostic of specific plant clades and/or functional groups, some of which are useful environmental indica- tors. Sixty-eight sediment samples were collected from 12 stratigraphic sections measured within the Barstow Formation in the Mud Hills, Calico Mountains, and Daggett Ridge, and 39 samples were processed for phytoliths. Ten samples yielded phytoliths, although phytoliths were rare in most of these samples. Paleosols from the uppermost part of the Barstow Formation yielded the most abundant and most diverse phytolith assemblages, including grass bilobates and echinate spheres of palms; grass phytoliths were also identi- fied in samples from the Owl Conglomerate and Middle members but were rare. These phytolith data provide evidence that grasses were present throughout deposition of the Barstow Formation, and that they coexisted with palms in mixed-vegetation habitats. -
Geologic Mapping, Rainbow Basin Field Trip Information
FIELD TRIP 1 Geologic Mapping, Rainbow Basin (Vicinity Barstow, California) Ge 101 Fall Quarter 2013 General Information: We will be departing at 8:00 a.m. on Friday, November 1 from the parking area in front of Arms ("Arms Circle"). Please arrive by 7:45 so there is time to get the trucks packed etc. Attached is a map of how to get to the field area. We will be staying in a motel in Barstow on Friday and Saturday nights (California Inn). We will depart from the motel parking lot for the field area at 8 a.m. on Saturday and Sunday mornings. We will leave the field area at 4 p.m. Sunday, and arrive back at Caltech by 7 p.m. Meals: Rainbow basin is remote and there are no options to purchase food there. We will make a brief stop at a supermarket in Barstow Friday morning to purchase lunch food, snacks and drinks. You may however opt to bring your own food and pack it in ice chests before we leave, up to and including three lunches, two breakfasts and two dinners. Prof. and TAs usually opt for breakfast at Carrows (a short drive from the motel) at 7 a.m., but the California Inn has a free breakfast. There are lots of restaurant options for dinner, from McDonalds up to various moderately priced restaurants. If you opt to purchase lunch food Friday morning in Barstow and otherwise eat in restaurants, you should budget about $80-100. Report: The field report will be an inked and colored geologic map with a map legend and cross section, plus a short description of the geologic history of the map area, listing events depicted on the geologic map, plus additional information compiled in Lab. -
Marine Bryozoans (Ectoprocta) of the Indian River Area (Florida)
MARINE BRYOZOANS (ECTOPROCTA) OF THE INDIAN RIVER AREA (FLORIDA) JUDITH E. WINSTON BULLETIN OF THE AMERICAN MUSEUM OF NATURAL HISTORY VOLUME 173 : ARTICLE 2 NEW YORK : 1982 MARINE BRYOZOANS (ECTOPROCTA) OF THE INDIAN RIVER AREA (FLORIDA) JUDITH E. WINSTON Assistant Curator, Department of Invertebrates American Museum of Natural History BULLETIN OF THE AMERICAN MUSEUM OF NATURAL HISTORY Volume 173, article 2, pages 99-176, figures 1-94, tables 1-10 Issued June 28, 1982 Price: $5.30 a copy Copyright © American Museum of Natural History 1982 ISSN 0003-0090 CONTENTS Abstract 102 Introduction 102 Materials and Methods 103 Systematic Accounts 106 Ctenostomata 106 Alcyonidium polyoum (Hassall), 1841 106 Alcyonidium polypylum Marcus, 1941 106 Nolella stipata Gosse, 1855 106 Anguinella palmata van Beneden, 1845 108 Victorella pavida Saville Kent, 1870 108 Sundanella sibogae (Harmer), 1915 108 Amathia alternata Lamouroux, 1816 108 Amathia distans Busk, 1886 110 Amathia vidovici (Heller), 1867 110 Bowerbankia gracilis Leidy, 1855 110 Bowerbankia imbricata (Adams), 1798 Ill Bowerbankia maxima, New Species Ill Zoobotryon verticillatum (Delle Chiaje), 1828 113 Valkeria atlantica (Busk), 1886 114 Aeverrillia armata (Verrill), 1873 114 Cheilostomata 114 Aetea truncata (Landsborough), 1852 114 Aetea sica (Couch), 1844 116 Conopeum tenuissimum (Canu), 1908 116 IConopeum seurati (Canu), 1908 117 Membranipora arborescens (Canu and Bassler), 1928 117 Membranipora savartii (Audouin), 1926 119 Membranipora tuberculata (Bosc), 1802 119 Membranipora tenella Hincks, -
Structural and Stratigraphic Evolution of the Calico Mountains
Structural and stratigraphic evolution of the Calico Mountains: Implications for early Miocene extension and Neogene transpression in the central Mojave Desert, California John S. Singleton* Phillip B. Gans Department of Earth Science, University of California, Santa Barbara, California 93106, USA ABSTRACT rapid unroofi ng of the central Mojave meta- (the Waterman Hills detachment fault) that morphic core complex, yet extension in the juxtaposes tilted early Miocene volcanic and New geologic mapping, structural data, Calico Mountains is minor and is overprinted sedimentary rocks in the hanging wall against and 40Ar/39Ar geochronology document early by dextral faulting and transpression. variably mylonitized basement rocks in the Miocene sedimentation and volcanism and Calico Member beds north of the Calico footwall. Based on apparent offsets of pre-Ter- Neogene deformation in the Calico Moun- fault are intensely folded into numerous tiary markers, several workers (Glazner et al., tains, located in a complexly deformed region east-west–trending, upright anticlines and 1989; Walker et al., 1990; Martin et al., 1993) of California’s central Mojave Desert. Across synclines that represent 25%–33% (up to proposed that 40–60 km of northeast-directed most of the Calico Mountains, volcaniclastic ~0.5 km) north-south shortening. Folds are normal slip occurred along the Waterman Hills sediments and dacitic rocks of the Pickhan- detached along the base of the Calico Mem- detachment fault. The distribution of exten- dle Formation accumulated rapidly between ber and thrust over the Pickhandle Forma- sion is controversial. Dokka (1989) argued that ca. 19.4 and 19 Ma. Overlying fi ne-grained tion, which dips homoclinally ~15–30°S to regional extension occurred within an east- lacustrine beds (here referred to as the Cal- SE. -
Synoptic Taxonomy of Major Fossil Groups
APPENDIX Synoptic Taxonomy of Major Fossil Groups Important fossil taxa are listed down to the lowest practical taxonomic level; in most cases, this will be the ordinal or subordinallevel. Abbreviated stratigraphic units in parentheses (e.g., UCamb-Ree) indicate maximum range known for the group; units followed by question marks are isolated occurrences followed generally by an interval with no known representatives. Taxa with ranges to "Ree" are extant. Data are extracted principally from Harland et al. (1967), Moore et al. (1956 et seq.), Sepkoski (1982), Romer (1966), Colbert (1980), Moy-Thomas and Miles (1971), Taylor (1981), and Brasier (1980). KINGDOM MONERA Class Ciliata (cont.) Order Spirotrichia (Tintinnida) (UOrd-Rec) DIVISION CYANOPHYTA ?Class [mertae sedis Order Chitinozoa (Proterozoic?, LOrd-UDev) Class Cyanophyceae Class Actinopoda Order Chroococcales (Archean-Rec) Subclass Radiolaria Order Nostocales (Archean-Ree) Order Polycystina Order Spongiostromales (Archean-Ree) Suborder Spumellaria (MCamb-Rec) Order Stigonematales (LDev-Rec) Suborder Nasselaria (Dev-Ree) Three minor orders KINGDOM ANIMALIA KINGDOM PROTISTA PHYLUM PORIFERA PHYLUM PROTOZOA Class Hexactinellida Order Amphidiscophora (Miss-Ree) Class Rhizopodea Order Hexactinosida (MTrias-Rec) Order Foraminiferida* Order Lyssacinosida (LCamb-Rec) Suborder Allogromiina (UCamb-Ree) Order Lychniscosida (UTrias-Rec) Suborder Textulariina (LCamb-Ree) Class Demospongia Suborder Fusulinina (Ord-Perm) Order Monaxonida (MCamb-Ree) Suborder Miliolina (Sil-Ree) Order Lithistida -
Tr-98-04 30-26
SE9900227 Technical Report TR-98-04 Volume I MAQARIN natural analogue study: Phase III Edited by J A T Smellie December 1998 Svensk Karnbranslehantering AB Swedish Nuclear Fuel and Waste Management Co Box 5864 SE-102 40 Stockholm Sweden Tel 08-459 84 00 +46 8 459 84 00 Fax 08-661 57 19 +46 8 661 57 19 30-26 MAQARIN natural analogue study: Phase III Edited by J.A.T. Smellie December 1998 VOLUME!: Chapters 1-13 VOLUME II: Appendices A-R This report concerns a study which was conducted for SKB. The conclusions and viewpoints presented in the report are those of the author(s) and do not necessarily coincide with those of the client. Information on SKB technical reports from 1977-1978 (TR 121), 1979 (TR 79-28), 1980 (TR 80-26), 1981 (TR 81-17), 1982 (TR 82-28), 1983 (TR 83-77), 1984 (TR 85-01), 1985 (TR 85-20), 1986 (TR 86-31), 1987 (TR 87-33), 1988 (TR 88-32), 1989 (TR 89-40), 1990 (TR 90-46), 1991 (TR 91-64), 1992 (TR 92-46), 1993 (TR 93-34), 1994 (TR 94-33), 1995 (TR 95-37) and 1996 (TR 96-25) is available through SKB. m^ffm?^ AKE TIBERIAS Qarfah , . /olbta' ? / .-V- ) had Set L^ Shafeni ," • '., Haiyan' /""•' ,. ^_ .I-...-- oel. MuiSti £1 Husetntya /..'" oHaiyan '• o £1 Jazza umman ,.-;p"i>EI Majarra A^ Ucn Pd Oananir t-^jAb'u Nuseir ,•"' ' ftaiib ..;•-•—.. | Jcbel el Adorn ; ,.-",' -•\' °Hawwara"-. / \ Bartholomew 1995 \ Reproduced with kind permission \ . , .,„ , . ''..\A::;..._ \ ««* '''a, •' / ACKNOWLEDGEMENTS his study has been funded by Nagra (Switzerland), Nirex (U.K.), SKB (Sweden) Tand the Environment Agency (U.K.); their active support is gratefully acknowledged. -
New Records of the Bryozoan Metrarabdotos from the Pirabas Formation (Lower Miocene), Pará State, Brazil
Palaeontologia Electronica palaeo-electronica.org New records of the bryozoan Metrarabdotos from the Pirabas Formation (Lower Miocene), Pará State, Brazil Laís V. Ramalho, Vladimir A. Távora, and Kamil Zagorsek ABSTRACT The Pirabas Formation in Pará State, Brazil, contains a very rich and diverse fauna of Early Miocene age, including several groups of invertebrates and vertebrates. Previous studies of bryozoans from Brazil included two species of Metrarabdotos ones, but these need revision. The present study describes three new species of Metrarab- dotos (M. aquaeguttum sp. nov., M. elongatum sp. nov., M. capanemensis sp. nov.) collected from two outcrops: Atalaia Beach at Salinópolis city and B-17 Mine at Capa- nema city. Laís V. Ramalho. Instituto Español de Oceanografia – IEO, Puerto Pesquero, s/n, Fuengirola. 29640; and Universidad de Málaga, Málaga – España. [email protected] Vladimir A. Távora. Laboratório de Paleontologia, Faculdade de Geologia, Instituto de Geociências, Universidade Federal do Pará, Caixa Postal 1611, Belém, Pará, Brazil. [email protected] Kamil Zagorsek. Department of Geography, Technical University of Liberec, Studentská 2, CZ-461 17 Liberec, Czech Republic. [email protected] Keywords: new species; Lower Miocene; Brazil; Caribbean Biogeographic Province; Bryozoans Submission: 20 July 2016 Acceptance: 12 June 2017 INTRODUCTION The cheilostome bryozoan genus Metrarabdo- tos Canu, 1914 comprises 38 fossil and six living Bryozoans are important fossils for geological species (Bock, 2014). These species, including reconstructions. They have broad stratigraphical both fossil and living representatives, are exclu- distributions and provide evidence for biogeo- sively tropical and northern subtropical (Rosso, graphic, phylogenetic, and environmental interpre- 2005; Cheetham et al., 2007). Cheetham (1967) tations. -
Mojave Miocene Robert E
Mojave Miocene Robert E. Reynolds, editor California State University Desert Studies Center 2015 Desert Symposium April 2015 Front cover: Rainbow Basin syncline, with rendering of saber cat by Katura Reynolds. Back cover: Cajon Pass Title page: Jedediah Smith’s party crossing the burning Mojave Desert during the 1826 trek to California by Frederic Remington Past volumes in the Desert Symposium series may be accessed at <http://nsm.fullerton.edu/dsc/desert-studies-center-additional-information> 2 2015 desert symposium Table of contents Mojave Miocene: the field trip 7 Robert E. Reynolds and David M. Miller Miocene mammal diversity of the Mojave region in the context of Great Basin mammal history 34 Catherine Badgley, Tara M. Smiley, Katherine Loughney Regional and local correlations of feldspar geochemistry of the Peach Spring Tuff, Alvord Mountain, California 44 David C. Buesch Phytoliths of the Barstow Formation through the Middle Miocene Climatic Optimum: preliminary findings 51 Katharine M. Loughney and Selena Y. Smith A fresh look at the Pickhandle Formation: Pyroclastic flows and fossiliferous lacustrine sediments 59 Jennifer Garrison and Robert E. Reynolds Biochronology of Brachycrus (Artiodactyla, Oreodontidae) and downward relocation of the Hemingfordian– Barstovian North American Land Mammal Age boundary in the respective type areas 63 E. Bruce Lander Mediochoerus (Mammalia, Artiodactyla, Oreodontidae, Ticholeptinae) from the Barstow and Hector Formations of the central Mojave Desert Province, southern California, and the Runningwater and Olcott Formations of the northern Nebraska Panhandle—Implications of changes in average adult body size through time and faunal provincialism 83 E. Bruce Lander Review of peccaries from the Barstow Formation of California 108 Donald L.