Zemes un vides zinātnes Earth and Environment Sciences - Latvijas ...

Zemes un vides zinātnes Earth and Environment Sciences - Latvijas ... Zemes un vides zinātnes Earth and Environment Sciences - Latvijas ...

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56 ADVANCES IN PALAEOICHTHYOLOGY References Blom H., Märss T., Miller C.G. 2002 (for 2001). Birkeniid anaspids from the northern hemisphere. Transactions of the Royal Society of Edinburgh: Earth Sciences, 92: 263-323. Gross W. 1958. Anaspiden-Schuppen aus dem Ludlow des Ostseegebiets. Paläontologische Zeitschrift, 32, 1/2: 24-37. Jeppsson L., Anehus R., Fredholm D. 1999. The optimal acetate buffered acetic acid technique for extracting phosphatic fossils. Journal of Paleontology, 73: 964-972. Märss T., Miller C.G. in press. Thelodonts and associated conodonts from the Silurian to lowermost Devonian (Llandovery-Lochkovian) of the Welsh Borderland. Palaeontology. Miller C.G., Blom H., Märss T. in press. Fossils Explained 46 – Anaspids. Geology Today, 19. Traquair R.H. 1898. Report on fossil fishes. Summary of the progress of the Geological Survey of The United Kingdom for 1897, Memoirs: 72-76. Turner S. 1973. Siluro-Devonian thelodonts from the Welsh Borderland. Journal of the Geological Society, London, 129: 557-584. Turner S. 1984. Studies on Palaeozoic Thelodonti (Craniata: Agnatha). Unpublished PhD thesis, University of Newcastle-upon-Tyne, U.K. Vergoossen J.M.J. 1995. Remarks on micro remains of Acanthodians (Gnathostomata) from the Late Pridoli of Manbrook (Upper Silurian, Great Britain). Geobios Special Memoir, 19: 399- 401. Vergoossen J.M.J. 1999. Siluro-Devonian microfossils of Acanthodii and Chondrichthyes (Pisces) from the Welsh Borderland/ South Wales. In: Turner S.T. and Blieck A. (eds) Gross Symposium Volume 3. Modern Geology Special Issue, 24: 23-90. Vergoossen J.M.J. 2000. Acanthodian and chondrichthyan microremains in the Siluro-Devonian of the Welsh Borderland, Great Britain, and their biostratigraphical potential. In: Blieck A. and Turner S. (eds). Palaeozoic vertebrate biochronology and global marine/non-marine correlation. Final Report of IGCP 328 (1991-1996). Courier Forschungsinstitut Senckenberg, 223, pp. 175-199. White E.I. 1946. Jamoytius kerwoodi a new Chordate from the Silurian of Lanarkshire. Geological Magazine, 93: 89-97. Jauns anaspīdu materiāls no Lielbritānijas un Igaunijas vēlā silūra DžAILS MILLERS, TĪJU MJARSS un HENNINGS BLOMS Ir aprakstīts jauns birkenīdu dzimtas anaspīdu taksons Trimpleylepis juncta gen. et sp. nov. no Menbrūkas, Velšborderlanda, augšējā silūra Pršidolas nodaļas. Trimpleylepis concatenata gen. et sp. nov. ir izdalīta no Ohesāres urbuma, Igaunija, silūra Ludlovas nodaļas. Histoloģiskos plānslīpējumos redzams, ka Trimpleylepis ir raksturīgas īpatnības, kas iepriekš atrastas dzimtai Septentrioniidae Blom, Märss et Miller, 2002 piederīgajā materiālā. Tomēr vaskulārie kanāli abu sugu zvīņu plānslīpējumos nav saskatāmi, bet retās kanālu atveres ir novērotas tikai vienā vai divos T. concatenata paraugos, tāpēc šī ģints ievietota dzimtā tikai pagaidām. Taksons Silmalepis cf. erinacea ir atrasts materiālā no Menbrūkas, pagarinot ģints izplatību līdz Pršidolas nodaļai. Jauns anaspīdu materiāls no Gardnera krasta, Velšborderlanda, augšējā silūra, norāda uz to, ka anaspīdu dzimta Rhyncholepididae Kiær, 1924 ir eksistējusi no Venlokas vidus līdz Pršidolas beigām.

ACTA UNIVERSITATIS LATVIENSIS, 2004, Vol. 679, pp. 57-78 Revisiting Lophosteus, a primitive osteichthyan HANS-PETER SCHULTZE and TIIU MÄRSS H.-P. Schultze, Institut für Paläontologie, Museum für Naturkunde, Humboldt Universität, Invalidenstr. 43, D-10115 Berlin, Germany; privat: 2001 Vermont St., Lawrence, Kansas 66046, USA; vrtpaleo@ku.edu T. Märss, Institute of Geology at Tallinn University of Technology, Estonia Ave. 7, Tallinn 10143, Estonia; marss@gi.ee Gross (1968) recognized one species of Lophosteus, L. superbus, from a single locality, Ohesaare Cliff, Saaremaa, and a single time interval, late Pridoli, Late Silurian. Today, six species are recognized and have a worldwide distribution from early Ludlow to early Pragian. We describe three new species from the type locality, the Canadian Arctic and the Urals. The systematic position of the genus is ambiguous. Lophosteus has been placed with sarcopterygians and with actinopterygians, or basal to both osteichthyan groups and in connection to acanthodians. Similarities to placoderms are superficial. We identify Lophosteus as a taxon close to acanthodians. Introduction Pander (1856) described Lophosteus superbus based on a small bone from the Ohesaare cliff, Saaremaa (German: Ösel). Rohon (1893) synonymised the species Pterichthys elegans Pander 1856 with Lophosteus superbus Pander, and treated P. harderi Pander 1856 as a distinct species, L. harderi. He placed Lophosteus in close relationship to sarcopterygians (Holoptychius, Glyptolepis etc.) based on its histology. A second species from the same locality (L. harderi (Pander), 1856) was synonymised with L. superbus by Gross (1969). Gross (1969, 1971) gave the most exhaustive description of the morphology and histology of Lophosteus superbus Pander 1856. Additional material has been described by Märss (1986) who proposed a new species, Lophosteus? connexus, from Vaivere, Saaremaa; Märss (1997) also identified similar Early Devonian scales from the Central Urals as Actinopterygii gen. et sp. A. Burrow (1995a) proposed another species, L. incrementus, from the Lower Devonian of Australia, and Märss (2000) shortly described Lophosteus sp. from Cornwallis Island, Arctic Canada. Here, we synthesise all data on lophosteids, give diagnoses for all species and summarise current knowledge of their relationships. Abbreviations: GIT, Institute of Geology at Tallinn University of Technology, Tallinn, Estonia; IGB, Institute of Geology, Beijing, China; MMM, Mining and Mineralogical Museum, Sydney, Australia; QMF, Queensland Museum fossil collection, S. Brisbane, Queensland, Australia; Tü, Geologisch-Paläontologisches Institut und Museum, Universität Tübingen, Germany; UALVP, Laboratory of Vertebrate Paleontology, University of Alberta, Edmonton, Alberta, Canada; UQY, Geology Department,

ACTA UNIVERSITATIS LATVIENSIS, 2004, Vol. 679, pp. 57-78<br />

Revisiting Lophosteus, a primitive osteichthyan<br />

HANS-PETER SCHULTZE <strong>and</strong> TIIU MÄRSS<br />

H.-P. Schultze, Institut für Paläontologie, Museum für Naturk<strong>un</strong>de, Humboldt Universität,<br />

Invalidenstr. 43, D-10115 Berlin, Germany; privat: 2001 Vermont St., Lawrence, Kansas<br />

66046, USA; vrtpaleo@ku.edu<br />

T. Märss, Institute of Geology at Tallinn University of Technology, Estonia Ave. 7, Tallinn<br />

10143, Estonia; marss@gi.ee<br />

Gross (1968) recognized one species of Lophosteus, L. superbus, from a single locality, Ohesaare<br />

Cliff, Saaremaa, <strong>and</strong> a single time interval, late Pridoli, Late Silurian. Today, six species are<br />

recognized <strong>and</strong> have a worldwide distribution from early Ludlow to early Pragian. We describe<br />

three new species from the type locality, the Canadian Arctic <strong>and</strong> the Urals. The systematic<br />

position of the genus is ambiguous. Lophosteus has been placed with sarcopterygians <strong>and</strong> with<br />

actinopterygians, or basal to both osteichthyan groups <strong>and</strong> in connection to acanthodians.<br />

Similarities to placoderms are superficial. We identify Lophosteus as a taxon close to acanthodians.<br />

Introduction<br />

P<strong>and</strong>er (1856) described Lophosteus superbus based on a small bone from the Ohesaare<br />

cliff, Saaremaa (German: Ösel). Rohon (1893) synonymised the species Pterichthys<br />

elegans P<strong>and</strong>er 1856 with Lophosteus superbus P<strong>and</strong>er, <strong>and</strong> treated P. harderi P<strong>and</strong>er<br />

1856 as a distinct species, L. harderi. He placed Lophosteus in close relationship to<br />

sarcopterygians (Holoptychius, Glyptolepis etc.) based on its histology. A second species<br />

from the same locality (L. harderi (P<strong>and</strong>er), 1856) was synonymised with L. superbus<br />

by Gross (1969). Gross (1969, 1971) gave the most exhaustive description of the<br />

morphology <strong>and</strong> histology of Lophosteus superbus P<strong>and</strong>er 1856. Additional material<br />

has been described by Märss (1986) who proposed a new species, Lophosteus? connexus,<br />

from Vaivere, Saaremaa; Märss (1997) also identified similar Early Devonian scales<br />

from the Central Urals as Actinopterygii gen. et sp. A. Burrow (1995a) proposed another<br />

species, L. incrementus, from the Lower Devonian of Australia, <strong>and</strong> Märss (2000) shortly<br />

described Lophosteus sp. from Cornwallis Isl<strong>and</strong>, Arctic Canada.<br />

Here, we synthesise all data on lophosteids, give diagnoses for all species <strong>and</strong><br />

summarise current knowledge of their relationships.<br />

Abbreviations: GIT, Institute of Geology at Tallinn University of Technology, Tallinn,<br />

Estonia; IGB, Institute of Geology, Beijing, China; MMM, Mining <strong>and</strong> Mineralogical<br />

Museum, Sydney, Australia; QMF, Queensl<strong>and</strong> Museum fossil collection, S. Brisbane,<br />

Queensl<strong>and</strong>, Australia; Tü, Geologisch-Paläontologisches Institut <strong>un</strong>d Museum,<br />

Universität Tübingen, Germany; UALVP, Laboratory of Vertebrate Paleontology,<br />

University of Alberta, Edmonton, Alberta, Canada; UQY, Geology Department,

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