Middle Ordovician Phosphatic Inarticulate Brachiopods from Våstergotland and Dalarna, Sweden
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Middle Ordovician phosphatic inarticulate brachiopods from Våstergotland and Dalarna, Sweden Lars E. Hollller FOSSILS AND STRATA Editor files(t he editorwill provide the necessary information on request) . Stefan Bengtson, Institute of Palaeontology, Box 558, S-751 22 Manuscript processing is designed to ensure rapid and inexpensive Uppsala, Sweden. production without compromising quality. Proofs are produced from the edited text files using desk-top-publishing techniques. Editonal and administrativeboard Galley proofs are sent to the au thors to provide opportunity to Stefan Bengtson (Uppsala) , Fredrik Bockelie (Oslo), Valdemar check the editor's changes and to revise the text if needed. Page Poulsen (Copenhagen) . proofs let the authors check the page layout, cross-references, word-breaks, etc., and to correct any remaining errors in the text. 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[Revised and published version of doetoral thesis pre sented at the Faculty of Science, Uppsala University, 1988.] Phosphatic inarticulate brachiopods are described from Middle Ordovician (Viru Series) strata in Vastergotland and Dalarna, Sweden. The material originates from a series of closely spaced samples through the sequences of the Fj acka and Kårgarde sections, Dalarna, and at Gullhogen quarry, Vastergotland. Fifty-six speeies (34 named, ofwhich 22 are new) are described, assigned to 29 named genera (ofwhich three are new) . The new acrotretacean subfamily Biernatinae is proposed, together with the new acrotretacean genera Cy rtonotreta and Biernatia; the problematical genus Tegulella is erected. For the discinaceans and most of the lingulaceans open nomenclature is applied; the taxonomi cally complicated Family Paterulidae has been excludt;d from systematie treatment alto gether. The lingulaceans and discinaceans share a common type of shell structure which is clearly distinguishable from that of the acrotretaceans. The early on togeny of many speeies is described. In the examined members of the Lingulacea and Discinacea the larval shell is large and smooth, whereas the acrotretaceans have a comparatively small and pitted larval shell. Although the protegular stage as a rule is not observable in fossil material, the cementing ventrai valves of some eoconulids preserve the mould of an organic embryonic (or early larval) shell. The evolution of the phosphatic-shelled inarticulates is diseussed. Within the order Acrotretida (sensu lata) the acquisition ofa ventrai valve with holoperiph eral growth and a pedicle foramen could have taken place convergently severai times from alingulid stock, leading to the acrotretaceans, discinaceans, and siphonotretaceans, respectively; the latter two superfamilies are considered to belong to separate orders, the Discinida and the Siphonotretida. The usefulness of the inarticulates for biostratigraphical correlation is demonstrated. DBrachiopoda, phosphatic inarticulates, Lingulacea, Discinacea, Siphonotretacea, Acrotretacea, new subfamily Biernatinae, new genera Biernatia, Cyrtonotreta, Tegulella, shell structure, ontogeny, evolution, biostratigraphy, palaeoecology, Middle Ordovician, Viistergotland, Dalarna, Sweden, N5815 N6050 E1520 E1337. LarsE. Holmer,Institu te ofPalaeontology, Box 558, S-751 22 Upp sala, Sweden; 1988 12 13, revised 1989 02 28. Contents Introduetion . .. 3 Uhakuan Stage ................................... 20 Historical review . .. 3 Dalby Limestone ..... .. 24 Material and methods .................................. 4 Discussion ....................................... 26 Middle Ordovician stratigraphy in Vastergotland and Life habits ......................................... 26 Dalarna ............................................ 5 Epifauna . .. 29 Localities . .. 6 Endofauna . .. 29 Gullhogen quarry . .. 6 Morphological terms .................................. 30 Kårgarde section . .. 9 Shell structure . .. 30 Fj acka section . .. 12 Lingulacea, Discinacea and Acrothelidae . .. 31 Biostratigraphy and palaeoecology . .. 12 Lingulacea . .. 31 Distribution, abundance and lithofacies ................ 12 Discinacea ....................................... 35 Kundan Stage ............ .. 13 Acrothelidae ..................................... 36 Aserian Stage ...................................