Chapter 15 Biogeography of Ordovician and Silurian gastropods, monoplacophorans and mimospirids

Author:

Ebbestad Jan Ove R.1,Frýda Jiří2,Wagner Peter J.3,Horný Radvan J.4,Isakar Mare5,Stewart Sarah6,Percival Ian G.7,Bertero Verònica8,Rohr David M.9,Peel John S.10,Blodgett Robert B.11,Högström Anette E. S.12

Affiliation:

1. Museum of Evolution, Uppsala University, Norbyvägen 16, SE–752 36 Uppsala, Sweden

2. Czech Geological Survey, Geologicka 6, 150 00 Prague, Czech Republic

3. Department of Paleobiology, Smithsonian Institution, PO Box 37012, Washington, DC 20013-7012, USA

4. Department of Palaeontology, National Museum, Václavské náměstí 68, 115 79 Prague 1, Czech Republic

5. The Museum of Geology of the University of Tartu, Vanemuise 46, 51014 Tartu, Estonia

6. National Museum of Scotland, Chambers Street, Edinburgh EH1 1JF, UK

7. Geological Survey of New South Wales, WB Clarke Geoscience Centre, 947–953 Londonderry Road, Londonderry, NSW 2753, Australia

8. CICTERRA-CONICET, Centro de Investigaciones Paleobiológicas, Facultad de Ciencias Exactas, Físicas y Naturales, Universidad Nacional de Córdoba, Av. Velez Sarsfield 299, X5000JJC Córdoba, Argentina

9. Department of Earth and Physical Sciences, Sul Ross State University, Alpine, TX 79832, USA

10. Department of Earth Sciences (Palaeobiology), Uppsala University, Villavägen 16, SE–752 36 Uppsala, Sweden

11. 2821 Kingfisher Drive, Anchorage, AK 99502, USA

12. Tromsø University Museum, Natural Sciences, N-9037 Tromsø, Norway

Abstract

AbstractThe biogeographical distribution of Ordovician and Silurian gastropods, monoplacophorans and mimospirids has been analysed on a generic level. The dataset contains 334 genera and 2769 species, yielding 1231 records of genera with 2274 occurrences worldwide. There is a bias towards eastern Laurentia, Baltica and Perunica records. Some 53.1% of the records are Ordovician. The study demonstrates that these molluscs are well suited to being used to improve understanding of Ordovician and Silurian biogeographical provinciality. Specific points are that: a Lower Ordovician assemblage is evident in Laurentia; the fauna of the Argentinean Precordillera is Laurentian until the Darriwilian, when taxa are shared with North China; Late Silurian gastropods from the Alexander terrane (SE Alaska) are unknown in Laurentia, but support a rift origin of this terrane from NE Siberia; Perunica, Ibero-Armorica and Morocco cluster together throughout the Ordovician but Perunica and Morocco are closer; Darriwilian–Sandbian deep-water Bohemian taxa occur in Baltica; a Laurentian–Baltica proximity is unsupported until the Silurian; Siberia clusters with North China and eastern Laurentia during the Tremadocian–Darriwilian; during the Gorstian–Pridoli Siberia clusters with the Farewell and Alexander terranes; North China may have been close to Laurentia and the Argentinean margin of Gondwana; and the affinity of Tarim taxa is problematic.

Publisher

Geological Society of London

Subject

Geology

Reference107 articles.

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4. First record of Malayaspira Kobayashi, 1958 (Mollusca, Gastropoda) in the Lower–Middle Ordovician San Juan Formation, Argentine Precordillera;Bertero;Ameghiniana,2009

5. Ceratopea (Gastropoda) from Lower Ordovician of south Spitsbergen;Birkenmajer;Bulletin of the Polish Academy of Sciences. Earth Sciences,1998

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