An Analysis of Fossil Identification Guides to Improve Data Reporting in Citizen Science Programs
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Phylogenetic Relationships of Serpulidae (Annelida: Polychaeta) Based on 18S Rdna Sequence Data, and Implications for Opercular Evolution Janina Lehrkea,Ã, Harry A
ARTICLE IN PRESS Organisms, Diversity & Evolution 7 (2007) 195–206 www.elsevier.de/ode Phylogenetic relationships of Serpulidae (Annelida: Polychaeta) based on 18S rDNA sequence data, and implications for opercular evolution Janina Lehrkea,Ã, Harry A. ten Hoveb, Tara A. Macdonaldc, Thomas Bartolomaeusa, Christoph Bleidorna,1 aInstitute for Zoology, Animal Systematics and Evolution, Freie Universitaet Berlin, Koenigin-Luise-Street 1-3, 14195 Berlin, Germany bZoological Museum, University of Amsterdam, P.O. Box 94766, 1090 GT Amsterdam, The Netherlands cBamfield Marine Sciences Centre, Bamfield, British Columbia, Canada, V0R 1B0 Received 19 December 2005; accepted 2 June 2006 Abstract Phylogenetic relationships of (19) serpulid taxa (including Spirorbinae) were reconstructed based on 18S rRNA gene sequence data. Maximum likelihood, Bayesian inference, and maximum parsimony methods were used in phylogenetic reconstruction. Regardless of the method used, monophyly of Serpulidae is confirmed and four monophyletic, well- supported major clades are recovered: the Spirorbinae and three groups hitherto referred to as the Protula-, Serpula-, and Pomatoceros-group. Contrary to the taxonomic literature and the hypothesis of opercular evolution, the Protula- clade contains non-operculate (Protula, Salmacina) and operculate taxa both with pinnulate and non-pinnulate peduncle (Filograna vs. Vermiliopsis), and most likely is the sister group to Spirorbinae. Operculate Serpulinae and poorly or non-operculate Filograninae are paraphyletic. It is likely that lack of opercula in some serpulid genera is not a plesiomorphic character state, but reflects a special adaptation. r 2007 Gesellschaft fu¨r Biologische Systematik. Published by Elsevier GmbH. All rights reserved. Keywords: Serpulidae; Phylogeny; Operculum; 18S rRNA gene; Annelida; Polychaeta Introduction distinctive calcareous tubes and bilobed tentacular crowns, each with numerous radioles that bear shorter Serpulids are common members of marine hard- secondary branches (pinnules) on the inner side. -
Biomineralization of Polychaete Annelids in the Fossil Record
minerals Review Biomineralization of Polychaete Annelids in the Fossil Record Olev Vinn Department of Geology, University of Tartu, Ravila 14A, 50411 Tartu, Estonia; [email protected]; Tel.: +372-5067728 Received: 31 August 2020; Accepted: 25 September 2020; Published: 29 September 2020 Abstract: Ten distinct microstructures occur in fossil serpulids and serpulid tubes can contain several layers with different microstructures. Diversity and complexity of serpulid skeletal structures has greatly increased throughout their evolution. In general, Cenozoic serpulid skeletal structures are better preserved than Mesozoic ones. The first complex serpulid microstructures comparable to those of complex structures of molluscs appeared in the Eocene. The evolution of serpulid tube microstructures can be explained by the importance of calcareous tubes for serpulids as protection against predators and environmental disturbances. Both fossil cirratulids and sabellids are single layered and have only spherulitic prismatic tube microstructures. Microstructures of sabellids and cirratulids have not evolved since the appearance of calcareous species in the Jurassic and Oligocene, respectively. The lack of evolution in sabellids and cirratulids may result from the unimportance of biomineralization for these groups as only few species of sabellids and cirratulids have ever built calcareous tubes. Keywords: biominerals; calcite; aragonite; skeletal structures; serpulids; sabellids; cirratulids; evolution 1. Introduction Among polychaete annelids, calcareous tubes are known in serpulids, cirratulids and sabellids [1–3]. The earliest serpulids and sabellids are known from the Permian [4], and cirratulids from the Oligocene [5]. Only serpulids dwell exclusively within calcareous tubes. Polychaete annelids build their tubes from calcite, aragonite or a mixture of both polymorphs. Calcareous polychaete tubes possess a variety of ultrastructural fabrics, from simple to complex, some being unique to annelids [1]. -
The Marine Fauna of New Zealand : Spirorbinae (Polychaeta : Serpulidae)
ISSN 0083-7903, 68 (Print) ISSN 2538-1016; 68 (Online) The Marine Fauna of New Zealand : Spirorbinae (Polychaeta : Serpulidae) by PETER J. VINE ANOGlf -1,. �" ii 'i ,;.1, J . --=--� • ��b, S�• 1 • New Zealand Oceanographic Institute Memoir No. 68 1977 The Marine Fauna of New Zealand: Spirorbinae (Polychaeta: Serpulidae) This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/ Frontispiece Spirorbinae on a piece of alga washed up on the New Zealand seashore. This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/ NEW ZEALAND DEPARTMENT OF SCIENTIFIC AND INDUSTRIAL RESEARCH The Marine Fauna of New Zealand: Spirorbinae (Polychaeta: Serpulidae) by PETER J. VINE Department of Zoology, University College, Singleton Park, Swansea, Wales, UK and School of Biological Sciences, James Cook University of North Queensland, Townsville, Australia PERMANENT ADDRESS "Coe! na Mara", Faul, c/- Dr Casey, Clifden, County Galway, Ireland New Zealand Oceanographic Institute Memoir No. 68 1977 This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/ Citation according to World list of Scientific Periodicals (4th edition: Mem. N.Z. oceanogr. Inst. 68 ISSN 0083-7903 Received for publication at NZOI January 1973 Edited by T. K. Crosby, Science InformationDivision, DSIR and R. -
Filogranula Cincta (Goldfuss, 1831), a Serpulid Worm (Polychaeta, Sedentaria, Serpulidae) from the Bohemian Cretaceous Basin
SBORNÍK NÁRODNÍHO MUZEA V PRAZE ACTA MUSEI NATIONALIS PRAGAE Řada B – Přírodní vědy • sv. 71 • 2015 • čís. 3–4 • s. 293–300 Series B – Historia Naturalis • vol. 71 • 2015 • no. 3–4 • pp. 293–300 FILOGRANULA CINCTA (GOLDFUSS, 1831), A SERPULID WORM (POLYCHAETA, SEDENTARIA, SERPULIDAE) FROM THE BOHEMIAN CRETACEOUS BASIN TOMÁŠ KOČÍ Department of Palaeontology, Natural History Museum, National Museum, Václavské náměstí 68, 115 79 Praha 1, the Czech Republic; Ivančická 581, Praha 9 – Letňany 199 00, the Czech Republic; e-mail: [email protected] MANFRED JÄGER Lindenstrasse 53, D-72348 Rosenfeld, Germany; e-mail: [email protected] Kočí, T., Jäger, M. (2015): Filogranula cincta (GOLDFUSS, 1831), a serpulid worm (Polychaeta, Sedentaria, Serpulidae) from the Bohemian Cretaceous Basin. – Acta Mus. Nat. Pragae, Ser. B Hist. Nat., 71(3-4): 293–300, Praha. ISSN 1804-6479. Abstract. Tubes of the serpulid worm Filogranula cincta (GOLDFUSS, 1831) were found in several rocky coast facies and other nearshore / shallow water localities in the Bohemian Cretaceous Basin ranging in geological age from the Late Cenomanian to the Late Turonian. A mor - phological description, discussion regarding systematics and taxonomy and notes on palaeoecology and stratigraphy are presented. ■ Late Cretaceous, Polychaeta, Filogranula, Serpulidae, Palaeoecology Received April 24, 2015 Issued December, 2015 Introduction any Filogranula cincta specimen. It seems that, apart from the vague mention from Strehlen by Wegner (1913), for more Filogranula cincta (GOLDFUSS, 1831) is a small and than a hundred years no additional finds of Filogranula inconspicuous but nevertheless common serpulid species in cincta from the BCB had been published until the present the Bohemian Cretaceous Basin (BCB). -
Smithsonian Contributions to Paleobiology • Number 90
SMITHSONIAN CONTRIBUTIONS TO PALEOBIOLOGY • NUMBER 90 Geology and Paleontology of the Lee Creek Mine, North Carolina, III Clayton E. Ray and David J. Bohaska EDITORS ISSUED MAY 112001 SMITHSONIAN INSTITUTION Smithsonian Institution Press Washington, D.C. 2001 ABSTRACT Ray, Clayton E., and David J. Bohaska, editors. Geology and Paleontology of the Lee Creek Mine, North Carolina, III. Smithsonian Contributions to Paleobiology, number 90, 365 pages, 127 figures, 45 plates, 32 tables, 2001.—This volume on the geology and paleontology of the Lee Creek Mine is the third of four to be dedicated to the late Remington Kellogg. It includes a prodromus and six papers on nonmammalian vertebrate paleontology. The prodromus con tinues the historical theme of the introductions to volumes I and II, reviewing and resuscitat ing additional early reports of Atlantic Coastal Plain fossils. Harry L. Fierstine identifies five species of the billfish family Istiophoridae from some 500 bones collected in the Yorktown Formation. These include the only record of Makairapurdyi Fierstine, the first fossil record of the genus Tetrapturus, specifically T. albidus Poey, the second fossil record of Istiophorus platypterus (Shaw and Nodder) and Makaira indica (Cuvier), and the first fossil record of/. platypterus, M. indica, M. nigricans Lacepede, and T. albidus from fossil deposits bordering the Atlantic Ocean. Robert W. Purdy and five coauthors identify 104 taxa from 52 families of cartilaginous and bony fishes from the Pungo River and Yorktown formations. The 10 teleosts and 44 selachians from the Pungo River Formation indicate correlation with the Burdigalian and Langhian stages. The 37 cartilaginous and 40 bony fishes, mostly from the Sunken Meadow member of the Yorktown Formation, are compatible with assignment to the early Pliocene planktonic foraminiferal zones N18 or N19. -
Geology Final.Indb
Paleontology of the Neoproterozoic Uinta Mountain Group Robin M. Nagy* and Susannah M. Porter* ABSTRACT Sedimentary rocks of the Uinta Mountain Group (northeastern Utah) preserve fossils deposited in a marine setting during middle Neoproterozoic time. Although well preserved, species diversity is much lower than many other midddle Neoproterozoic siliciclastic deposits. Microfossil assemblages are mostly limited to Leiosphaeridia sp., Bavlinella faveolata, and fi laments. Diverse ornamented acritarchs, vase- shaped microfossils, and the macroscopic compression fossil Chuaria circularis, also occur, but are much more rare. Although the Uinta Mountain Group does not preserve as wide a range of facies as other middle Neoproterozoic units – the unit is carbonate-free – it is unlikely that preservation alone can account for its relatively limited fossil diversity. Rather, the Uinta Mountain Group likely records deposition in an environment that was inimical to most eukaryotes. INTRODUCTION own (see table 2). We find that although the UMG is fossiliferous throughout its stratigraphic and The Uinta Mountain Group (UMG) is one geographic range, (appendix A) fossil assemblages of several western North American successions are, for the most part, taxonomically depauperate, that provide a glimpse of middle Neoproterozoic limited to just one or a few morphologically simple life (Link and others, 1993). Other successions species. This probably reflects, at least in part, the from this region have yielded important insight limited range of taphonomic windows preserved into this critical interval, including the earliest in the UMG, but also suggests that much of the evidence for eukaryotic biomineralization UMG was deposited in an environment inimical to (Horodyski and Mankiewicz, 1990; Porter and high species diversity. -
Polychaeta, Serpulidae) from the Hawaiian Islands1 JULIE H
Deepwater Tube Worms (Polychaeta, Serpulidae) from the Hawaiian Islands1 JULIE H. BAILEy-BROCK2 THREE SERPULID TUBE WORMS have been dis (1906), but no serpulids were found. Hart covered on shells and coral fragments taken in man (1966a) reviewed the literature in an dredges from around the Hawaiian Islands. The extensive analysis of the Hawaiian polychaete two serpulines Spirobranchus latiscapus Maren fauna. Straughan (1969), presented a more zeller and Vermiliopsis infundibulum Philippi recent survey of the littoral and upper sublit are new records for the islands. However, the toral Serpulidae. Other works by Vine (1972) small spirorbid Pileolaria (Duplicaria) dales and Vine, Bailey-Brock, and Straughan (1972) traughanae Vine has been described previously include ecological data collected from settle from within diving depths (Vine, 1972), but ment plates and by diving, but no records ex it is absent from shoal waters and intertidal re tend below 28 meters. Serpulids have been gions. 3 The occurrence of this species in the described from deepwater collections in other dredged collections indicates an extensive depth parts of the world. Southward (1963) found range in the Hawaiian Islands. 14 species of calcareous tube worms on hard The tube worms were obtained from col substrata dredged from depths as great as 1,755 lections taken during two separate oceano meters along the continental shelf off south graphic investigations in Hawaiian waters. western Britain. Antarctic collections yielded 14 Material consisting mostly of the pink serpuline genera and more than 23 species from depths Spirobranchus latiscapus was loaned by Dr. E. C. ranging from the littoral zone down to 4,930 Jones of the National Marine Fisheries Service 4,963 meters in the South Sandwich Trench (N.M.F.S.) and was taken from an average (Hartman, 1966b, 1967). -
Tayside, Central and Fife Tayside, Central and Fife
Detail of the Lower Devonian jawless, armoured fish Cephalaspis from Balruddery Den. © Perth Museum & Art Gallery, Perth & Kinross Council Review of Fossil Collections in Scotland Tayside, Central and Fife Tayside, Central and Fife Stirling Smith Art Gallery and Museum Perth Museum and Art Gallery (Culture Perth and Kinross) The McManus: Dundee’s Art Gallery and Museum (Leisure and Culture Dundee) Broughty Castle (Leisure and Culture Dundee) D’Arcy Thompson Zoology Museum and University Herbarium (University of Dundee Museum Collections) Montrose Museum (Angus Alive) Museums of the University of St Andrews Fife Collections Centre (Fife Cultural Trust) St Andrews Museum (Fife Cultural Trust) Kirkcaldy Galleries (Fife Cultural Trust) Falkirk Collections Centre (Falkirk Community Trust) 1 Stirling Smith Art Gallery and Museum Collection type: Independent Accreditation: 2016 Dumbarton Road, Stirling, FK8 2KR Contact: [email protected] Location of collections The Smith Art Gallery and Museum, formerly known as the Smith Institute, was established at the bequest of artist Thomas Stuart Smith (1815-1869) on land supplied by the Burgh of Stirling. The Institute opened in 1874. Fossils are housed onsite in one of several storerooms. Size of collections 700 fossils. Onsite records The CMS has recently been updated to Adlib (Axiel Collection); all fossils have a basic entry with additional details on MDA cards. Collection highlights 1. Fossils linked to Robert Kidston (1852-1924). 2. Silurian graptolite fossils linked to Professor Henry Alleyne Nicholson (1844-1899). 3. Dura Den fossils linked to Reverend John Anderson (1796-1864). Published information Traquair, R.H. (1900). XXXII.—Report on Fossil Fishes collected by the Geological Survey of Scotland in the Silurian Rocks of the South of Scotland. -
Database of Bibliography of Living/Fossil
www.shark-references.com Version 16.01.2018 Bibliography database of living/fossil sharks, rays and chimaeras (Chondrichthyes: Elasmobranchii, Holocephali) Papers of the year 2017 published by Jürgen Pollerspöck, Benediktinerring 34, 94569 Stephansposching, Germany and Nicolas Straube, Munich, Germany ISSN: 2195-6499 DOI: 10.13140/RG.2.2.32409.72801 copyright by the authors 1 please inform us about missing papers: [email protected] www.shark-references.com Version 16.01.2018 Abstract: This paper contains a collection of 817 citations (no conference abstracts) on topics related to extant and extinct Chondrichthyes (sharks, rays, and chimaeras) as well as a list of Chondrichthyan species and hosted parasites newly described in 2017. The list is the result of regular queries in numerous journals, books and online publications. It provides a complete list of publication citations as well as a database report containing rearranged subsets of the list sorted by the keyword statistics, extant and extinct genera and species descriptions from the years 2000 to 2017, list of descriptions of extinct and extant species from 2017, parasitology, reproduction, distribution, diet, conservation, and taxonomy. The paper is intended to be consulted for information. In addition, we provide data information on the geographic and depth distribution of newly described species, i.e. the type specimens from the years 1990 to 2017 in a hot spot analysis. New in this year's POTY is the subheader "biodiversity" comprising a complete list of all valid chimaeriform, selachian and batoid species, as well as a list of the top 20 most researched chondrichthyan species. Please note that the content of this paper has been compiled to the best of our abilities based on current knowledge and practice, however, possible errors cannot entirely be excluded. -
From the Late Miocene Gatun Formation of Panama Catalina Pimiento,1,2,3 Gerardo Gonza´ Lez-Barba,4 Dana J
Journal of Paleontology, 87(5), 2013, p. 755–774 Copyright Ó 2013, The Paleontological Society 0022-3360/13/0087-755$03.00 DOI: 10.1666/12-117 SHARKS AND RAYS (CHONDRICHTHYES, ELASMOBRANCHII) FROM THE LATE MIOCENE GATUN FORMATION OF PANAMA CATALINA PIMIENTO,1,2,3 GERARDO GONZA´ LEZ-BARBA,4 DANA J. EHRET,5 AUSTIN J. W. HENDY,1,2 1 2 BRUCE J. MACFADDEN, AND CARLOS JARAMILLO 1Florida Museum of Natural History, University of Florida, Gainesville, FL 32611, USA, ,[email protected].; ,[email protected].; ,[email protected].; 2Smithsonian Tropical Research Institute, Center for Tropical Paleoecology and Archaeology, Box 2072, Panama, Republic of Panama, ,[email protected].; 3Department of Biology, University of Florida, Gainesville, FL 32611, USA; 4Museo de Historia Natural, Area de Ciencias del Mar, La Paz, Universidad Autonoma de Baja California Sur, AP 23080, Mexico, ,[email protected].; and 5Alabama Museum of Natural History, University of Alabama, Tuscaloosa, Alabama, 35487, USA, ,[email protected]. ABSTRACT—The late Miocene Gatun Formation of northern Panama contains a highly diverse and well sampled fossil marine assemblage that occupied a shallow-water embayment close to a purported connection between the Pacific and Atlantic (Caribbean) oceans. However, the diverse chondrichthyan fauna has been poorly documented. Based on recent field discoveries and further analysis of existing collections, the chondrichthyan fauna from this unit comprises at least 26 taxa, of which four species are extinct today. The remaining portion of the total chondrichthyan biodiversity has affinities with modern taxa and is therefore comprised of long-lived species. Based on known records of the modern geographic distribution range of the Gatun chondrichthyans, the fauna has mixed biogeographic affinities suggesting that around 10 million yr ago, a connection likely occurred between the Pacific Ocean and the Caribbean Sea. -
Arbeitskreis Paläontologie Hannover
HEFT 3 75–107 ARBEITSKREIS PALÄONTOLOGIE HANNOVER 45. JAHRGANG 2017 45. Jahrgang 2017 ARBEITSKREIS Heft 3 PALÄONTOLOGIE HANNOVER Zeitschrift für Amateur-Paläontologen Herausgeber: INHALT: Arbeitskreis Paläontologie Hannover http://www.ap-h.de 75 Joachim Ladwig, Ein Zahn des lamniformen Haies Carcharomodus escheri (AGASSIZ, 1843) aus dem miozänen Glimmerton von Groß Geschäftsstelle: Pampau (Schleswig-Holstein) Eckhardt Krause Plutoweg 6 31275 Lehrte-Ahlten 78 Anne Jäger, Mein erster Fund eines Rudisten aus dem Untercampan von Höver Schriftleitung: Christian Schneider Heidekrugstraße 50 82 Anne Jäger & Peter Girod, Funde unserer 12555 Berlin Mitglieder Dr. Peter Girod Holteistraße 2 10245 Berlin 87 Christian Schneider, Neufund eines Hemiaster aquisgranensis SCHLÜTER 1899 in den ober- Lektorat: Katrin Glenk campanen Ablagerungen von Misburg Alle Autoren sind für ihre Beiträge selbst verantwortlich. 90 Christian Langhoff, Ein artikulierter Cirripedia- Druck: Fund aus dem Obercampan von Lägerdorf in Druckhaus Köhler Schleswig-Holstein Siemensstraße 1-3 31177 Harsum 91 Christian Schneider, Die Echinidenfauna des Cenomans von Wunstorf Die Zeitschrift erscheint in vierteljährlicher Folge. Der Abonnementspreis ist im Mitgliedsbeitrag von 30,- € enthalten. Ein Abonnement ohne Mitgliedschaft ist nicht möglich. Zahlungen auf das Konto: Kontoinhaber: APH - ARBEITSKREIS PALÄONTOLOGIE HANNOVER Sparkasse Hannover Umschlagseite 1: BIC: SPKHDE2H Cameroptychium scharnhorsti, senonensis-Zone IBAN: DE57 2505 0180 0901 0290 68 (Untercampan), Grube Alemannia -
Shark–Cetacean Trophic Interaction, Duinefontein, AUTHOR: Koeberg, (5 Ma), South Africa Romala Govender1
Research Article Sharks vs cetaceans, Duinefontein (Koeberg), South Africa Page 1 of 7 Shark–Cetacean trophic interaction, Duinefontein, AUTHOR: Koeberg, (5 Ma), South Africa Romala Govender1 AFFILIATION: This study forms part of a larger project to reconstruct the Mio-Pliocene marine palaeoenvironment along 1Natural History Department, South Africa’s west coast. It documents the shark–cetacean trophic interaction during the Zanclean (5 Ma) Iziko Museums of South Africa, at Duinefontein (Koeberg). The damage described on the fragmentary cetacean bones was compared Cape Town, South Africa with similar damage observed on fossils from Langebaanweg, a Mio-Pliocene site on the west coast of South Africa, and data present in the literature. This comparison showed that the damage was the result of CORRESPONDENCE TO: Romala Govender shark bites. The state of preservation makes it difficult to determine if the shark bite marks were the cause of death or as a result of scavenging. The presence of the bite marks on the bone would, however, indicate some EMAIL: degree of skeletonisation. Bite marks on some cranial fragments would suggest that the cetacean’s body [email protected] was in an inverted position typical of a floating carcass. The preservation of the material suggests that the bones were exposed to wave action resulting in their fragmentation as well as abrasion, polishing and rolling. POSTAL ADDRESS: It also suggests that the cetacean skeletons were exposed for a long time prior to burial. The morphology of Natural History Department, Iziko Museums of South Africa, the bites suggests that the damage was inflicted by sharks with serrated and unserrated teeth.