Evidence for Serialia (Mollusca, Monoplacophora + Polyplacophora)
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Shell Microstructures in Early Cambrian Molluscs
Shell microstructures in Early Cambrian molluscs ARTEM KOUCHINSKY Kouchinsky, A. 2000. Shell microstructures in Early Cambrian molluscs. - Acta Palaeontologica Polonica 45,2, 119-150. The affinities of a considerable part of the earliest skeletal fossils are problematical, but investigation of their microstructures may be useful for understanding biomineralization mechanisms in early metazoans and helpful for their taxonomy. The skeletons of Early Cambrian mollusc-like organisms increased by marginal secretion of new growth lamel- lae or sclerites, the recognized basal elements of which were fibers of apparently aragon- ite. The juvenile part of some composite shells consisted of needle-like sclerites; the adult part was built of hollow leaf-like sclerites. A layer of mineralized prism-like units (low aragonitic prisms or flattened spherulites) surrounded by an organic matrix possibly existed in most of the shells with continuous walls. The distribution of initial points of the prism-like units on a periostracurn-like sheet and their growth rate were mostly regular. The units may be replicated on the surface of internal molds as shallow concave poly- gons, which may contain a more or less well-expressed tubercle in their center. Tubercles are often not enclosed in concave polygons and may co-occur with other types of tex- tures. Convex polygons seem to have resulted from decalcification of prism-like units. They do not co-occur with tubercles. The latter are interpreted as casts of pore channels in the wall possibly playing a role in biomineralization or pits serving as attachment sites of groups of mantle cells. Casts of fibers and/or lamellar units may overlap a polygonal tex- ture or occur without it. -
Atkins Peel.Vp
Yochelcionella (Mollusca, Helcionelloida) from the lower Cambrian of North America CHRISTIAN J. ATKINS & JOHN S. PEEL Five named species of the helcionelloid mollusc genus Yochelcionella Runnegar & Pojeta, 1974 are recognized from the lower Cambrian (Cambrian Series 2) of North America: Yochelcionella erecta (Walcott, 1891), Y. americana Runnegar & Pojeta, 1980, Y. chinensis Pei, 1985, Y. greenlandica Atkins & Peel, 2004 and Y. gracilis Atkins & Peel, 2004, linking lower Cambrian outcrops along the present north-eastern seaboard. Yochelcionella erecta, an Avalonian species, is de- scribed for the first time; other species are derived from Laurentia. A revised concept of the Chinese species, Y. chinensis, is based mainly on a large sample from the Forteau Formation of western Newfoundland and the species may have stratigraphic utility between Cambrian palaeocontinents. • Key words: Yochelcionella, Helcionelloida, Mollusca, lower Cambrian (Cambrian Series 2), North America. ATKINS,C.J.&PEEL, J.S. 2008. Yochelcionella (Mollusca, Helcionelloida) from the lower Cambrian of North America. Bulletin of Geosciences 83(1), 23–38 (8 figures). Czech Geological Survey, Prague. ISSN 1214-1119. Manuscript re- ceived September 26, 2007; accepted in revised form January, 10, 2008; issued March 31, 2008. Christian J. Atkins, Department of Earth Sciences (Palaeobiology), Uppsala University, Villavägen 16, SE-752 36 Uppsala, Sweden; [email protected] • John S. Peel, Department of Earth Sciences (Palaeobiology) and Mu- seum of Evolution, Uppsala University, Villavägen 16, SE-752 36 Uppsala, Sweden; [email protected] A fossil referable to the helcionelloid mollusc Yochelcio- there is debate about its precise function and the orienta- nella Runnegar & Pojeta, 1974 was illustrated by Walcott tion of the shell. -
The Functional Morphology of the Cambrian Univalved Mollusks— Helcionellids
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/236216830 The Functional Morphology of the Cambrian Univalved Mollusks— Helcionellids. 1 Article in Paleontological Journal · July 2000 CITATIONS READS 29 411 1 author: Pavel Parkhaev Russian Academy of Sciences 85 PUBLICATIONS 1,150 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Worldwide Cambrian molluscan fauna View project All content following this page was uploaded by Pavel Parkhaev on 29 May 2014. The user has requested enhancement of the downloaded file. Paleontological Journal, Vol. 34, No. 4, 2000, pp. 392–399. Translated from Paleontologicheskii Zhurnal, No. 4, 2000, pp. 32–39. Original Russian Text Copyright © 2000 by Parkhaev. English Translation Copyright © 2000 by åÄIä “Nauka /Interperiodica” (Russia). The Functional Morphology of the Cambrian Univalved Mollusks—Helcionellids. 1 P. Yu. Parkhaev Paleontological Institute, Russian Academy of Sciences, ul. Profsoyuznaya 123, Moscow, 117868 Russia Received October 21, 1998 Abstract—The soft-body anatomy of helcionellids is reconstructed on the basis of a morphofunctional analy- ses of their shells. Evidently, two systems for the internal organization of helcionellids are possible: the first corresponds to that of the gastropodian class; the second, to that of the monoplacophorian. INTRODUCTION maximum number of analogies and the least number of contradictions with recent animals. Intensive study of the Cambrian fauna and stratigra- phy during recent decades shows us a diverse biota of Helcionellids were common elements of the mala- this geological period. Mollusks are well represented cofauna in the Early–Middle Cambrian and achieved a among the numerous newly described taxa in a variety rather high taxonomic diversity in comparison with of groups. -
Adulthood and Phylogenetic Analysis in Gastropods: Character Recognition and Coding in Shells of Lavigeria (Cerithioidea, Thiaridae) from Lake Tanganyika
Blackwell Science, LtdOxford, UKZOJZoological Journal of the Linnean Society0024-4082The Lin- nean Society of London, 2004? 2004 140? 223240 Original Article L. N. PAPADOPOULOS ET AL .ADULTHOOD AND PHYLOGENETIC CODING IN GASTROPOD SHELLS Zoological Journal of the Linnean Society, 2004, 140, 223–240. With 7 figures Adulthood and phylogenetic analysis in gastropods: character recognition and coding in shells of Lavigeria (Cerithioidea, Thiaridae) from Lake Tanganyika LEONARD N. PAPADOPOULOS1*, JONATHAN A. TODD2 and ELLINOR MICHEL1† 1Institute for Biodiversity & Ecosystem Dynamics/Zoological Museum, University of Amsterdam, PO Box 94766, 1090 GT Amsterdam, the Netherlands 2Department of Palaeontology, The Natural History Museum, London SW7 5BD, UK Received February 2003; accepted for publication July 2003 In the study of gastropod shell morphology, determination of comparable ontogenetic stages is crucial, because all the states that various shell features go through during ontogeny are preserved on the shell. The protoconch/teleoconch transition and marks of episodic growth are among the few ways of defining discrete, comparable, growth stages. In gastropods with determinate growth the attainment of adulthood may provide additional shell markers permitting comparison among individuals and taxa. Adulthood is reflected in shell morphology in ways as diverse as shell dep- osition covering all the previous whorls and radically changing the shape of the shell through to slight changes in the trajectory of the suture. While the very prominent adulthood-related changes of shell morphology have been used as systematic characters, the more moderate changes have not been studied in detail and their potential systematic value has been ignored. In this paper we give a detailed account of adult modifications of the shell appearing with cessation of growth. -
Caenogastropoda
13 Caenogastropoda Winston F. Ponder, Donald J. Colgan, John M. Healy, Alexander Nützel, Luiz R. L. Simone, and Ellen E. Strong Caenogastropods comprise about 60% of living Many caenogastropods are well-known gastropod species and include a large number marine snails and include the Littorinidae (peri- of ecologically and commercially important winkles), Cypraeidae (cowries), Cerithiidae (creep- marine families. They have undergone an ers), Calyptraeidae (slipper limpets), Tonnidae extraordinary adaptive radiation, resulting in (tuns), Cassidae (helmet shells), Ranellidae (tri- considerable morphological, ecological, physi- tons), Strombidae (strombs), Naticidae (moon ological, and behavioral diversity. There is a snails), Muricidae (rock shells, oyster drills, etc.), wide array of often convergent shell morpholo- Volutidae (balers, etc.), Mitridae (miters), Buccin- gies (Figure 13.1), with the typically coiled shell idae (whelks), Terebridae (augers), and Conidae being tall-spired to globose or fl attened, with (cones). There are also well-known freshwater some uncoiled or limpet-like and others with families such as the Viviparidae, Thiaridae, and the shells reduced or, rarely, lost. There are Hydrobiidae and a few terrestrial groups, nota- also considerable modifi cations to the head- bly the Cyclophoroidea. foot and mantle through the group (Figure 13.2) Although there are no reliable estimates and major dietary specializations. It is our aim of named species, living caenogastropods are in this chapter to review the phylogeny of this one of the most diverse metazoan clades. Most group, with emphasis on the areas of expertise families are marine, and many (e.g., Strombidae, of the authors. Cypraeidae, Ovulidae, Cerithiopsidae, Triphori- The fi rst records of undisputed caenogastro- dae, Olividae, Mitridae, Costellariidae, Tereb- pods are from the middle and upper Paleozoic, ridae, Turridae, Conidae) have large numbers and there were signifi cant radiations during the of tropical taxa. -
Deep-Sea Video Technology Tracks a Monoplacophoran to the End of Its Trail (Mollusca, Tryblidia)
Deep-sea video technology tracks a monoplacophoran to the end of its trail (Mollusca, Tryblidia) Sigwart, J. D., Wicksten, M. K., Jackson, M. G., & Herrera, S. (2018). Deep-sea video technology tracks a monoplacophoran to the end of its trail (Mollusca, Tryblidia). Marine Biodiversity, 1-8. https://doi.org/10.1007/s12526-018-0860-2 Published in: Marine Biodiversity Document Version: Publisher's PDF, also known as Version of record Queen's University Belfast - Research Portal: Link to publication record in Queen's University Belfast Research Portal Publisher rights Copyright 2018 the authors. This is an open access article published under a Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium, provided the author and source are cited. General rights Copyright for the publications made accessible via the Queen's University Belfast Research Portal is retained by the author(s) and / or other copyright owners and it is a condition of accessing these publications that users recognise and abide by the legal requirements associated with these rights. Take down policy The Research Portal is Queen's institutional repository that provides access to Queen's research output. Every effort has been made to ensure that content in the Research Portal does not infringe any person's rights, or applicable UK laws. If you discover content in the Research Portal that you believe breaches copyright or violates any law, please contact [email protected]. Download date:06. Oct. 2021 Deep-sea video technology tracks a monoplacophoran to the end of its trail (Mollusca, Tryblidia) Sigwart, J. -
The Continuing Debate on Deep Molluscan Phylogeny: Evidence for Serialia (Mollusca, Monoplacophora + Polyplacophora)
Hindawi Publishing Corporation BioMed Research International Volume 2013, Article ID 407072, 18 pages http://dx.doi.org/10.1155/2013/407072 Research Article The Continuing Debate on Deep Molluscan Phylogeny: Evidence for Serialia (Mollusca, Monoplacophora + Polyplacophora) I. Stöger,1,2 J. D. Sigwart,3 Y. Kano,4 T. Knebelsberger,5 B. A. Marshall,6 E. Schwabe,1,2 and M. Schrödl1,2 1 SNSB-Bavarian State Collection of Zoology, Munchhausenstraße¨ 21, 81247 Munich, Germany 2 Faculty of Biology, Department II, Ludwig-Maximilians-Universitat¨ Munchen,¨ Großhaderner Straße 2-4, 82152 Planegg-Martinsried, Germany 3 Queen’s University Belfast, School of Biological Sciences, Marine Laboratory, 12-13 The Strand, Portaferry BT22 1PF, UK 4 Department of Marine Ecosystems Dynamics, Atmosphere and Ocean Research Institute, University of Tokyo, 5-1-5 Kashiwanoha, Kashiwa, Chiba 277-8564, Japan 5 Senckenberg Research Institute, German Centre for Marine Biodiversity Research (DZMB), Sudstrand¨ 44, 26382 Wilhelmshaven, Germany 6 Museum of New Zealand Te Papa Tongarewa, P.O. Box 467, Wellington, New Zealand Correspondence should be addressed to M. Schrodl;¨ [email protected] Received 1 March 2013; Revised 8 August 2013; Accepted 23 August 2013 Academic Editor: Dietmar Quandt Copyright © 2013 I. Stoger¨ et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Molluscs are a diverse animal phylum with a formidable fossil record. Although there is little doubt about the monophyly of the eight extant classes, relationships between these groups are controversial. We analysed a comprehensive multilocus molecular data set for molluscs, the first to include multiple species from all classes, including five monoplacophorans in both extant families. -
Research Article the Continuing Debate on Deep Molluscan Phylogeny: Evidence for Serialia (Mollusca, Monoplacophora + Polyplacophora)
Hindawi Publishing Corporation BioMed Research International Volume 2013, Article ID 407072, 18 pages http://dx.doi.org/10.1155/2013/407072 Research Article The Continuing Debate on Deep Molluscan Phylogeny: Evidence for Serialia (Mollusca, Monoplacophora + Polyplacophora) I. Stöger,1,2 J. D. Sigwart,3 Y. Kano,4 T. Knebelsberger,5 B. A. Marshall,6 E. Schwabe,1,2 and M. Schrödl1,2 1 SNSB-Bavarian State Collection of Zoology, Munchhausenstraße¨ 21, 81247 Munich, Germany 2 Faculty of Biology, Department II, Ludwig-Maximilians-Universitat¨ Munchen,¨ Großhaderner Straße 2-4, 82152 Planegg-Martinsried, Germany 3 Queen’s University Belfast, School of Biological Sciences, Marine Laboratory, 12-13 The Strand, Portaferry BT22 1PF, UK 4 Department of Marine Ecosystems Dynamics, Atmosphere and Ocean Research Institute, University of Tokyo, 5-1-5 Kashiwanoha, Kashiwa, Chiba 277-8564, Japan 5 Senckenberg Research Institute, German Centre for Marine Biodiversity Research (DZMB), Sudstrand¨ 44, 26382 Wilhelmshaven, Germany 6 Museum of New Zealand Te Papa Tongarewa, P.O. Box 467, Wellington, New Zealand Correspondence should be addressed to M. Schrodl;¨ [email protected] Received 1 March 2013; Revised 8 August 2013; Accepted 23 August 2013 Academic Editor: Dietmar Quandt Copyright © 2013 I. Stoger¨ et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Molluscs are a diverse animal phylum with a formidable fossil record. Although there is little doubt about the monophyly of the eight extant classes, relationships between these groups are controversial. We analysed a comprehensive multilocus molecular data set for molluscs, the first to include multiple species from all classes, including five monoplacophorans in both extant families. -
Caenogastropoda During Mesozoic Times
Caenogastropoda during Mesozoic times Klaus Bandel Bandel, K. Caenogastropoda during Mesozoic times. — Scripta Geol., Spec. Issue 2: 7-56, 15 pls. Lei• den, December 1993. Klaus Bandel, Institut für Paläontologie und Geologie, Universität Hamburg, Bundesstraße 55, D 20146 Hamburg 13, Germany. Key words: evolution, Mollusca, Gastropoda, Mesozoicum. The following groups of Mesozoic Caenogastropoda are discussed here: Cerithioidea and Littorinoi- dea-Rissooidea seemingly merging with each other during Triassic times; the fresh water and land snails of the Viviparoidea and Cyclophoroidea with unknown marine relatives but a Mesozoic histo• ry; the Vermetoidea, Turritelloidea and Campaniloidea with a late appearance in the Mesozoic; the Ctenoglossa with a continuous history from the Middle Palaeozoic to modern times; the Subulitoidea, Murchisonioidea and Loxonematoidea with Palaeozoic ancestors but unclear Middle Mesozoic rela• tions; the Purpurinoidea as potential ancestors and relatives of the Stromboidea, the latter suddenly appearing in the Jurassic; the Heteropoda and Vanikoroidea with possible relation to each other but very uncertain relations to the others; and the Neomesogastropoda and Neogastropoda which begin their history in the Mid Cretaceous with still rather uncertain precursors. Contents Introduction 7 Taxonomie discussion 8 Palaeo-Caenogastropoda 8 Meta-Mesogastropoda 24 Neomesogastropoda 30 Neogastropoda 39 Conclusions 44 Acknowledgements 46 References 51 Introduction The history of most groups of Caenogastropoda during Palaeozoic times is still uncertain. Only the Subulitoidea, Murchisonioidea, Loxonematoidea and Zygopleur- oidea, and questionable Cerithioidea of the Stegocoelia type, can be traced through much of the Palaeozoic (Knight, 1931; Wenz, 1938-1944; Knight et al., 1960; Hoare & Sturgeon, 1978, 1980a, 1980b, 1981, 1985; Yoo, 1988, 1989; Bandel, 1991a; own data). -
The Continuing Debate on Deep Molluscan Phylogeny: Evidence for Serialia (Mollusca, Monoplacophora + Polyplacophora)
The Continuing Debate on Deep Molluscan Phylogeny: Evidence for Serialia (Mollusca, Monoplacophora + Polyplacophora) Stöger, I., Sigwart, J. D., Kano, Y., Marshall, B. A., Schwabe, E., & Schrödl, M. (2013). The Continuing Debate on Deep Molluscan Phylogeny: Evidence for Serialia (Mollusca, Monoplacophora + Polyplacophora). BioMed Research International, 2013, [407072]. https://doi.org/10.1155/2013/407072 Published in: BioMed Research International Document Version: Early version, also known as pre-print Queen's University Belfast - Research Portal: Link to publication record in Queen's University Belfast Research Portal Publisher rights Copyright 2013 The authors General rights Copyright for the publications made accessible via the Queen's University Belfast Research Portal is retained by the author(s) and / or other copyright owners and it is a condition of accessing these publications that users recognise and abide by the legal requirements associated with these rights. Take down policy The Research Portal is Queen's institutional repository that provides access to Queen's research output. Every effort has been made to ensure that content in the Research Portal does not infringe any person's rights, or applicable UK laws. If you discover content in the Research Portal that you believe breaches copyright or violates any law, please contact [email protected]. Download date:11. Jan. 2021 The continuing debate on deep molluscan phylogeny: Evidence for Serialia (Mollusca, Monoplacophora + Polyplacophora) I. Stöger1, J. D. Sigwart2, Y. Kano3, T. Knebelsberger4, B. A. Marshall5, E. Schwabe1, M. Schrödl1§ 1Bavarian State Collection of Zoology, Münchhausenstr. 21, 81247 Munich, Germany. GeoBioCenterLMU and Department II, Faculty of Biology, Ludwig Maximilians-Universität München, Germany. -
Shell Microstructures in Early Mollusks
Vol. XLII(4): 2010 THE FESTIVUS Page 43 SHELL MICROSTRUCTURES IN EARLY MOLLUSKS MICHAEL J. VENDRASCO1*, SUSANNAH M. PORTER1, ARTEM V. KOUCHINSKY2, GUOXIANG LI3, and CHRISTINE Z. FERNANDEZ4 1Institute for Crustal Studies, University of California, Santa Barbara, CA, 93106, USA 2Department of Palaeozoology, Swedish Museum of Natural History, Box 50007, SE-104 05 Stockholm, Sweden 3LPS, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing 210008, P.R. China, 414601 Madris Ave., Norwalk, CA 90650, USA Abstract: Shell microstructures in some of the oldest known mollusk fossils (from the early to middle Cambrian Period; 542 to 510 million years ago) are diverse, strong, and in some cases unusual. We herein review our recent work focused on different aspects of shell microstructures in Cambrian mollusks, briefly summarizing some of the major conclusions from a few of our recent publications and adding some new analysis. Overall, the data suggest that: (1) mollusks rapidly evolved disparate shell microstructures; (2) early mollusks had a complex shell with a different type of shell microstructure in the outer layer than in the inner one; (3) the modern molluscan biomineralization system, with precise control over crystal shapes and arrangements in a mantle cavity bounded by periostracum, was already in place during the Cambrian; (4) shell microstructure data provide a suite of characters useful in phylogenetic analyses of mollusks and mollusk-like Problematica, allowing better determination -
Chapter 5. Paleozoic Invertebrate Paleontology of Grand Canyon National Park
Chapter 5. Paleozoic Invertebrate Paleontology of Grand Canyon National Park By Linda Sue Lassiter1, Justin S. Tweet2, Frederick A. Sundberg3, John R. Foster4, and P. J. Bergman5 1Northern Arizona University Department of Biological Sciences Flagstaff, Arizona 2National Park Service 9149 79th Street S. Cottage Grove, Minnesota 55016 3Museum of Northern Arizona Research Associate Flagstaff, Arizona 4Utah Field House of Natural History State Park Museum Vernal, Utah 5Northern Arizona University Flagstaff, Arizona Introduction As impressive as the Grand Canyon is to any observer from the rim, the river, or even from space, these cliffs and slopes are much more than an array of colors above the serpentine majesty of the Colorado River. The erosive forces of the Colorado River and feeder streams took millions of years to carve more than 290 million years of Paleozoic Era rocks. These exposures of Paleozoic Era sediments constitute 85% of the almost 5,000 km2 (1,903 mi2) of the Grand Canyon National Park (GRCA) and reveal important chronologic information on marine paleoecologies of the past. This expanse of both spatial and temporal coverage is unrivaled anywhere else on our planet. While many visitors stand on the rim and peer down into the abyss of the carved canyon depths, few realize that they are also staring at the history of life from almost 520 million years ago (Ma) where the Paleozoic rocks cover the great unconformity (Karlstrom et al. 2018) to 270 Ma at the top (Sorauf and Billingsley 1991). The Paleozoic rocks visible from the South Rim Visitors Center, are mostly from marine and some fluvial sediment deposits (Figure 5-1).