The Middle Ordovician of the Oslo Region, Norway
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Paleozoic Gastropoda from the Moose River Synclinorium, Northern Maine
Paleozoic Gastropoda from the Moose River Synclinorium, Northern Maine GEOLOGICAL SURVEY PROFESSIONAL PAPER 503-A Paleozoic Gastropoda from the Moose River Synclinorium, Northern Maine By ARTJiUR J. BOUCOT and ELLIS L. YOCHELSON CONTRIBUTIONS TO PALEONTOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 503-A An investigation of fossils primarily of Devonian age UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1966 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402- Price 30 cents (paper cover) CONTENTS Page Page Abstract __________________________________________ _ A1 Register of localities ___________________________ -- __ _ A15 Introduction ______________________________________ _ 1 References cited __________________ ---- __ ------------ 17 Occurrence and distribution of the gastropods _________ _ 3 Index ____________________________________________ _ 19 Systematic paleontology ____________________________ _ 3 ILLUSTRATIONS [Plates follow index] PLATE 1. Gastropoda and miscellaneous fossils 2-3. Gastropoda Page FIGURE 1. Correlation table______________________ A2 2. Sketch of "Euomphalopterus" __ _ _ _ _ _ _ _ _ _ _ 17 TABLE Page TABLE 1. Distribution of gastropods in Paleozoic rocks of the Moose River synclinorium ________________ - ____ -- __ ------ A4 III CONTRIBUTIONS TO PALEONTOLOGY PALEOZOIC GASTROPODA FROM THE MOOSE RIVER SYNCLINORIUM, NORTHERN MAINE By ARTHUR J. BoucoT and ELLIS L. Y OCHELSON .ABSTRACT units which has been determined from study of other Large-scale collecting in the middle Paleozoic strata of the fossil groups (chiefly brachipods and corals). Moose River synclinorium has yielded a few gastropods-one Except where indicated, the taxonomic classification Ordovician species, six species from the Silurian, and two from follows that published by Knight, Batten, and Y ochel rocks of Silurian or Devonian age, one of these also oceurring son (1960). -
Type and Figured Fossils in the Worthen Collection at the Illinois
s Cq&JI ^XXKUJtJLI 14oGS: CIR 524 c, 2 TYPE AND FIGURED FOSSILS IN THE WORTHEN COLLECTION AT THE ILLINOIS STATE GEOLOGICAL SURVEY Lois S. Kent GEOLOGICAL ILLINOIS Illinois Department of Energy and Natural Resources, STATE GEOLOGICAL SURVEY DIVISION CIRCULAR 524 1982 COVER: This portrait of Amos Henry Worthen is from a print presented to me by Worthen's great-grandson, Arthur C. Brookley, Jr., at the time he visited the Illinois State Geological Survey in the late 1950s or early 1960s. The picture is the same as that published in connection with the memorial to Worthen in the appendix to Vol. 8 of the Geological Survey of Illinois, 1890. -LSK Kent, Lois S., Type and figured fossils in the Worthen Collection at the Illinois State Geological Survey. — Champaign, III. : Illinois State Geological Survey, 1982. - 65 p. ; 28 cm. (Circular / Illinois State Geological Survey ; 524) 1. Paleontology. 2. Catalogs and collections. 3. Worthen Collection. I. Title. II. Series. Editor: Mary Clockner Cover: Sandra Stecyk Printed by the authority of the State of Illinois/1982/2500 II I IHOI'.MAII '.I 'II Of.ir.AI MIHVI y '> 300 1 00003 5216 TYPE AND FIGURED FOSSILS IN THE WORTHEN COLLECTION AT THE ILLINOIS STATE GEOLOGICAL SURVEY Lois S. Kent | CIRCULAR 524 1982 ILLINOIS STATE GEOLOGICAL SURVEY Robert E. Bergstrom, Acting Chief Natural Resources Building, 615 East Peabody Drive, Champaign, IL 61820 TYPE AND FIGURED FOSSILS IN THE WORTHEN COLLECTION AT THE ILLINOIS STATE GEOLOGICAL SURVEY CONTENTS Acknowledgments 2 Introduction 2 Organization of the catalog 7 Notes 8 References 8 Fossil catalog 13 ABSTRACT This catalog lists all type and figured specimens of fossils in the part of the "Worthen Collection" now housed at the Illinois State Geological Survey in Champaign, Illinois. -
Lexique Stratigraphique Canadien - Volume V-B - Region Des Appalaches, Des Basses-Terres Du Saint-Laurent Et Des Iles De La Madeleine Lexique Stratigraphique
DV 91-23 LEXIQUE STRATIGRAPHIQUE CANADIEN - VOLUME V-B - REGION DES APPALACHES, DES BASSES-TERRES DU SAINT-LAURENT ET DES ILES DE LA MADELEINE LEXIQUE STRATIGRAPHIQUE CANADIEN Volume Fa Région des Appalaches, des Basses-Terres du Saint-Laurent et des îles de la Madeleine par Yvon Globensky et collaborateurs 1993 Québec ©© LEXIQUE STRATIGRAPHIQUE CANADIEN Volume r-8 Région des Appalaches, des Basses-Terres du Saint-Laurent et des Îles de la Madeleine par Yvon Globensky et collaborateurs DV 91-23 1993 Quebec ®® DIRECTION GÉNÉRALE DE L'EXPLORATION GÉOLOGIQUE ET MINÉRALE Sous-ministre adjoint: R.Y. Lamarche DIRECTION DE LA RECHERCHE GÉOLOGIQUE Directeur: A. Simard, par intérim SERVICE GÉOLOGIQUE DE QUÉBEC Chef: J.-M. Charbonneau Manuscrit soumis le: 30-01-91 Accepté pour publication le: 14-06-91 Lecteur critique J. Béland Édition Géomines / F. Dompierre Préparé par la Division de l'édition (Service de la géoinformation, DGEGM) Couvert 1: 1) Paucicrura rogata et Platystrophia amoena. Membre de Rosemont. Au SW de Saint-Jean-sur-Richelieu. Photo: tirée de Globensky, 1981b, page 39 2) Formation de Solomon's Corner. Saint-Armand-Station. Photo: tirée de Globensky, 1981b, page 126 3) Faciès de Terrebonne, formation de Tétreauville. Rivière L'Assomption. Photo: Y. Globensky 4) Formation de Covey Hill. Coupe à l'extrémité NW du lac Gulf, à l'ouest de Covey Hill. Photo: tirée de Globensky, 1986, page 9 Couvert 4: 1) Formation d'Indian Point. Péninsule de Forillon. Photo: D. Brisebois 2) Coupe type de la Formation de Wallace Creek. Étang Streit, près de Philipsburg. Photo: tirée de Globensky, 1981b, page 101 3) Euomphalopsis sp. -
Guide to Fossil C911ecting
Educational Series - 1 ISSN 0544-3083 Guide to Fossil C911ecting ~~1. I ~l in/~~;/~_ Minnesota Minnesota Geological Survey Guide To FossIl Collecting In Minnesota R. K. Hogberg, R. E. Sloan and Sarah Tufford First edition 1965: revised edition 1967: reprinted 1979: reprinted 1985 ISSN 0544-3083 Geologic Time Chart_Minnesota Time Era Period Events in Minnesota Characteristic Life Quaternary 20 ENO· .ofMommals ZOIC 40 Tertiary No record in Minnesota ~ 60 M Sea enters Minnesota from E Cretaceous 100 S West. Deposition of sediments. 0 Z A~ of R.ptil.s 0 Jurassic I No record in Minnesota C Triassic k 200 Permian Ag.of Pennsylvanian No record in Minnesota Amphibians ..~ Mississippian ~ ~ ~ P Sea enters Minnesota from 300 Devonian "-() South. Deposition of sediments. .. A .~ L ~ . Silurian No record in Minnesota Ag. of Corals E 0 • of Straight 400 Ordovician Seas cover Minnesota at intervals. Z c_~ 0 I C Cambrian Deposition of sediments. A~ of Trilobit.s ~ Lava flows and deposition of sediments. PRECAMBRIAN Deposition of iron-rich sediments. First r.cord oIl,f. 4 \12 billion years lang Formation of mountains and igneous intrusions. Guide To FOSJt'l Colletting In Minnesota FoSSILS tell us what life was like on earth in ancient geologic time. A fossil clam, for example, lived on a sea bottom much as its modern relatives do. By finding many fossil clams, we can deter mine the extent of a prehistoric sea. Fossils also indicate the climates of the geologic past. Fossils show us that life on earth has not always been the same. In fact primitive algae and bacteria have given rise to reptile s, mammals, and finally to man. -
CINCINNATIAN GASTROPOD PRIMER by Ron Fine HOW DO SCIENTISTS CLASSIFY GASTROPODS?
CINCINNATIAN GASTROPOD PRIMER By Ron Fine HOW DO SCIENTISTS CLASSIFY GASTROPODS? KINGDOM: Animalia (Animals) Mammals Birds Fish Amphibians Molluscs Insects PHYLUM: Mollusca (Molluscs) Cephalopods Gastropods Bivalves Monoplacophorans Scaphopods Aplacophorans Polyplacophorans CLASS: Gastropoda (Gastropods or Snails) Gastropods 2 HOW MANY KINDS OF GASTROPODS ARE THERE? There are 611 Families of gastropods, but 202 are now extinct Whelk Slug Limpet Land Snail Conch Periwinkle Cowrie Sea Butterfly Nudibranch Oyster Borer 3 THERE ARE 60,000 TO 80,000 SPECIES! IN ENDLESS SHAPES AND PATTERNS! 4 HABITAT-WHERE DO GASTROPODS LIVE? Gardens Deserts Ocean Depths Mountains Ditches Rivers Lakes Estuaries Mud Flats Tropical Rain Forests Rocky Intertidal Woodlands Subtidal Zones Hydrothermal Vents Sub-Arctic/Antarctic Zones 5 HABITAT-WHAT WAS IT LIKE IN THE ORDOVICIAN? Gastropods in the Ordovician of Cincinnati lived in a tropical ocean, much like the Caribbean of today 6 DIET-WHAT DO GASTROPODS EAT? Herbivores Detritus Parasites Plant Eaters Mud Eaters Living on other animals Scavengers Ciliary Carnivores Eat dead animals Filter feeding in the water Meat Eaters 7 ANATOMY-HOW DO YOU IDENTIFY A GASTROPOD? Gastropod is Greek, from “gaster” meaning ‘stomach’ and “poda” meaning ‘foot’ They are characterized by a head with antennae, a large foot, coiled shell, a radula and operculum Torsion: all of a gastropod’s anatomy is twisted, not just the shell They are the largest group of molluscs, only insects are more diverse Most are hermaphrodites 8 GASTROPOD ANATOMY-FOOT Gastropods have a large “foot”, used for locomotion. Undulating bands of muscles propel the gastropod forward, even on vertical surfaces. SLIME! Gastropods excrete slime to help their foot glide over almost any surface. -
Euconospira with Color Marking from the Permian of Japan
Title Euconospira with Color Marking from the Permian of Japan Author(s) Hayasaka, Ichirô Citation Journal of the Faculty of Science, Hokkaido University. Series 4, Geology and mineralogy, 8(4), 349-360 Issue Date 1954-03 Doc URL http://hdl.handle.net/2115/35869 Type bulletin (article) File Information 8(4)_349-360.pdf Instructions for use Hokkaido University Collection of Scholarly and Academic Papers : HUSCAP EacewOStwre,4 WX[rcH COMOR MARKXNG FROM Tew PERMIAN ew JAPAN ' ' By Ichir6 HAYASAI<A (With 2 Plates) Contyibution from the Department of Geology and Mineralogy, Faculty of Seience, Hokkaid6 University, Sappero; No. 521 I. Xntrodtictoi'y. Whi}e examinlng iate Paleozoie maeyo-fossils of Japan in 'the eab- inet of the Department o£ Geology and Mineralogy, Hok}{aid6 Univeysity, the writey recently happened to eome aeross with a troehiform gas- tropod with an almost fiat base. It originated in the Pe]rmian liiiries'u'one oE Central Japan, Althottgh the speeiinen is slight}y deformeel and partlY damaged, most of the more important diagnostie charaeters aye xeeogitized quite cieayly. A narrow selenizone buried between periphe- rai fia'nges is reeogni.zed though the latter are mostly broken off. These featuifes, although apertural part is }ost, show that the fossil belongs to tlte genus EzLconospi7'a IJi,mcii and ScoFiET,i} whieh is vLTidely distri.buted in North America ranging fyom Caybonifexous to Permian. The original work of UT,Jucff and ScoFiEr.D i.n whleh .the genus was first introdueed to seiej)ce- is beyond the reach of the present vLiri£er. However, it is bniefiy but exhaust・ively diagnosed by J. -
Bedrock Geology of Franklin Grove Quadrangle
STATEMAP Franklin Grove-BG Bedrock Geology of Franklin Grove Quadrangle Lee County, Illinois Franck Delpomdor and Joseph Devera 2020 615 East Peabody Drive Champaign, Illinois 61820-6918 (217) 244-2414 http://www.isgs.illinois.edu © 2020 University of Illinois Board of Trustees. All rights reserved. For permission information, contact the Illinois State Geological Survey. Introduction Previous work The first geological features of Lee County were illustrated Geographic location and geomorphological framework very generally on early statewide geologic maps at scale The Franklin Grove 7.5-minute Quadrangle is located in 1/500,000 (Worthen 1875; Weller 1906). Stratigraphy and north-central Illinois in the north-central part of Lee County, structural geology investigations in the Franklin Grove area Illinois, about 32 miles southwest of Rockford (Winnebago include those by Cady (1920), Leighton (1922), Templeton County), 45 miles east of Illinois-Iowa border, 50 miles and Saxby (1947), Templeton and Willman (1952, 1963), south of the Illinois-Wisconsin border, and 90 miles west Kolata and Buschbach (1976), Willman and Kolata (1978), of Chicago (Cook and DuPage Counties). Map coverage and Kolata et al. (1978). In addition, a map showing the bed- extends to the east from the Dixon East Quadrangle and rock geology of Lee County, including the Franklin Grove south of the Daysville Quadrangle. The quadrangle cov- Quadrangle, was published by McGarry (1999). Geologic ers approximately a 55 square mile area that is bounded by features were generalized in the Geologic Map of Illinois 41°45’00” and 41°52’30” North latitude and 89°15’00” and at scale 1/500,000 (Kolata 2005). -
Comparative Taxonomic Richness and Abundance of Late Ordovician Gastropods and Bivalves in Mollusc-Rich Strata of the Cincinnati Arch
RESEARCH REPORTS 559 Comparative Taxonomic Richness and Abundance of Late Ordovician Gastropods and Bivalves in Mollusc-rich Strata of the Cincinnati Arch PHILIP M. NOVACK-GOTTSHALL Department of Biology, Box 90338, Duke University, Durham, NC 27708-0338, E-Mail: [email protected] ARNOLD I. MILLER Department of Geology, PO Box 210013, University of Cincinnati, Cincinnati, OH 45221-0013 PALAIOS, 2003, V. 18, p. 559±571 roevolutionary rates (Sepkoski, 1978; Stanley, 1979; Raup and Sepkoski, 1984; Gilinsky, 1994; Foote, 2000). Howev- Using a ®eld analysis of Upper Ordovician mollusc-rich er, while such studies are essential for understanding the faunas of the Cincinnati Arch, this study tests whether the ecological underpinnings of evolution, they are limited by large-scale patterns of Ordovician gastropods and bivalves their large-scale observational framework. In other words, observed in a companion study are maintained at the ®ner they cannot be used to test ecological causes of these pat- scales of individual strata and localities, and when utiliz- terns without using ®ner-scale data, particularly without ing abundance data in addition to taxonomic richness. using abundance data (see also Lidgard, 2002). Non-metric multidimensional scaling and several statisti- With the exception of terrestrial plant paleoecology cal analyses show that the taxonomic richness and abun- where the use of abundance data is commonplace (Pfeffer- dance of these classes within samples were signi®cantly korn and Thomson, 1982; DiMichele et al., 1985; Di- negatively correlated, such that bivalve-rich settings were Michele and Wing, 1988; Lupia et al., 1999), use of abun- only sparsely inhabited by gastropods and vice versa. -
Novttatesamerican MUSEUM PUBLISHED by the AMERICAN MUSEUM of NATURAL HISTORY CENTRAL PARK WEST at 79TH STREET NEW YORK, N.Y
NovttatesAMERICAN MUSEUM PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET NEW YORK, N.Y. 10024 U.S.A. NUMBER 2579 MAY 29, 1975 HAROLD B. ROLLINS Gastropods from the Lower Mississippian Wassonville Limestone in Southeastern Iowa & AMERICAN MUSEUM Novitates PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK, N.Y. 10024 Number 2579, pp. 1-35, figs. 1-11, tables 1-26 May 29, 1975 Gastropods from the Lower Mississippian Wassonville Limestone in Southeastern Iowa' HAROLD B. ROLLINS2 ABSTRACT A Lower Mississippian (Kinderhookian) gas- An unexpected aspect of the Wassonville gas- tropod fauna is described from the Wassonville tropod fauna is that it shows greater taxonomic Formation in southeastern Iowa. This represents affinity with the European Carboniferous than one of the few well-preserved Lower Mississip- with other North American Carboniferous pian gastropod faunas known from North faunas. This probably reflects the paucity of de- America and, as such, contributes to our under- scribed North American Mississippian gastropod standing of a rather critical time in the evolution faunas and the increased understanding, through of Paleozoic gastropods. recent study (notably Batten, 1966), of British Twenty-eight species are described, eight of and Belgium Tournaisian and Visean gastro- which are new. The new taxa are: Sinuitina nudi- pods. dorsa, Platyschisma laudoni, Trepospira (An- The genus Cerithiodes, long known from gyomphalus) penelenticulata, Baylea angulosa, the Upper Paleozoic of Europe, is recognized Glabrocingulum (Glabrocingulum) minutum, for the first time in the Carboniferous of North Glyptotomaria (Dictyotomaria) quasicapillaria, America. Cerithioides judiae, and Baylea trifibra. -
The Middle Ordovician Section in East Central Missouri
Scholars' Mine Masters Theses Student Theses and Dissertations 1922 The Middle Ordovician section in east central Missouri Morris James Ingerson Josiah Bridge Follow this and additional works at: https://scholarsmine.mst.edu/masters_theses Part of the Geology Commons Department: Recommended Citation Ingerson, Morris James and Bridge, Josiah, "The Middle Ordovician section in east central Missouri" (1922). Masters Theses. 7088. https://scholarsmine.mst.edu/masters_theses/7088 This thesis is brought to you by Scholars' Mine, a service of the Missouri S&T Library and Learning Resources. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. TRE ]HDDLE ORDOVICIAN SECTION IK EAST CEH'l'RAL MISSOURI BY Josiah Bridge , M. s. Assistant Professor of Geology and M. J. Ingerson Graduate Assistant in Geology A T HE S I S submitted to the Faculty of the SCHOOL OF MINES AND METALLURGY OF THE UNIVERSITY OF MISSOURI in partial fulfil~ent of the work required for the Degree of M&Bter or Science :M . J. Ingerson Rolla., Mo . 1 9 2 2 Approved by c. i . Clj-CJ-i/u:__ -----------------~ ------------ Profess~r of Geology LIST OF ILLUSTRATIONS Page Section of the Joachim at Pacific, Mo. in pocket Section of Joachim at Tavern Rock, Mo. in pocket Ledge of Plattin at Joa.chim-Plattin facing page contact near Pacific, Mo. 16 "Chimneys" of Plattin Limestone near facing page Port Royal, Mo. 1'7 Section of the Plattin at Hirnms Station, in pocket Mo. -
Stratigraphy, Structure and Early Paleozoic Gastropoda of the Callahan Area, Klameth Mountains, California
AN ABSTRACT OF THE THESIS OF David Malcolm Rohr for the degree of Doctor of Philosophy in Geology presented on 15 June 1977 Title:STRATIGRAPHY, STRUCTURE, AND EARLY PALEOZOIC GASTROPODA OF THE CALLAHAN AREA, KLAMATH MOUNTAINS, CALIFORNIA Redacted for Privacy Abstract approved: A. IV Boucot The sedimentary, metamorphic, and igneous rocks of the Callahan, California area formed on, or adjacent to, a Lower Paleo- zoic island arc complex which has since been tectonically disrupted. Sandstone, shale, lithic wacke, chert, banded quartzite, siliceous mudstone, conglomerate, and limestone of the eastern Klamath belt were deposited from the Middle Ordovician through the Early Devonian on top of the peridotite of the Early? Ordovician Trinity ophiolitic complex.Shallow water deposition began in the Middle Ordovician with the Facey Rock Limestone.Sandstone, siltstone, and shale of the Moffett Creek Formation probably formed as turbidity flows adjacent to the arc and were later disrupted, possibly at shallow depths in a subduction zone.Other units in the Callahan area (Calla- han Chert, Gazelle Formation, quartzite of Squaw Gulch, siliceous mudstone of Thompson Gulch) may have formed in basins on the Moffett Creek Formation. The Moffett Creek Formation was derived from a primarily plutonic-metamorphic terrane, possibly a deeply eroded arc complex, while the overlying Gazelle Formation was derived from a primarily calc-alkaline volcanic source. Amphibolite and impure marbles of the Grouse Ridge Formation, which have an Early or Middle Devonian age -
Ordovician News
ORDOVICIAN NEWS SUBCOMMISSION ON ORDOVICIAN STRATIGRAPHY INTERNATIONAL COMMISSION ON STRATIGRAPHY Number 38 (for 2020) Edited by Bertrand Lefebvre INTERNATIONAL UNION OF GEOLOGICAL SCIENCES President: John LUDDEN (United Kingdom) Vice-Presidents: Daekyo CHEONG (Korea) Hassina MOURI (South Africa) Secretary General: Stanley C. FINNEY (USA) Treasurer: Hiroshi KITAZATO (Japan) INTERNATIONAL COMMISSION ON STRATIGRAPHY Chairman: David A.T. HARPER (United Kingdom) Vice-Chairman: Shuzhong SHEN (China) Secretary General: Philip GIBBARD (United Kingdom) SUBCOMMISSION ON ORDOVICIAN STRATIGRAPHY Chairman: Thomas SERVAIS (France) Vice-Chairman: ZHAN Renbin (China) Secretary: Bertrand LEFEBVRE (France) Sachiko AGEMATSU-WATANABE (Japan) Matilde BERESI (Argentina) André DESROCHERS (Canada) Mansoureh GHOBADI POUR (Iran) Daniel GOLDMAN (USA) Lars HOLMER (Sweden) Petr KRAFT (Czech Republic) Patrick I. McLAUGHLIN (USA) Tõnu MEIDLA (Estonia) Leon NORMORE (Australia) Elena RAEVSKAYA (Russia) Alycia STIGALL (USA) Tatiana TOLMACHEVA (Russia) WANG Wenhui (China) Charles WELLMAN (United Kingdom) Seth YOUNG (USA) Yong Yi ZHEN (Australia) Ordovician Subcommission website : http://ordovician.stratigraphy.org CONTENTS Page CHAIRMAN'S MESSAGE 2 SECRETARY’S MESSAGE 5 ANNUAL REPORT OF ORDOVICIAN SUBCOMMISSION FOR 2020 6 ONLINE MEETING OF THE VOTING MEMBERS OF THE SUBCOMMISSION 15 BOOK REVIEW • The Ordovician Period – a new contribution chapter to Geologic Time Scale 2020 (Gradstein et al., eds.: Elsevier, 2020) 17 REPORTS OF RECENT CONFERENCES • IGCP 653 virtual Annual Meeting, Copenhagen, September 2020 19 CONFERENCE ANNOUNCEMENTS • IGCP 668 virtual Annual Meeting, Tsukuba, July 2021 21 • IGCP 653/735 virtual Annual Meeting, Lille, September 2021 24 • International Conference on Palaeobiology, High Resolution Stratigraphy and Fossil Energy, Nanjing, November 2021 26 • IGCP 735 – SOS Regional Meeting, Lille, May–June 2022 30 • 14th International Symposium on the Ordovician System, Estonia, 2023 38 NEW IGCP PROJECT • IGCP 735: Rocks and the Rise of Ordovician Life (Rocks n'ROL).