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  Estonian Journal of Earth Sciences

ISSN 1736-7557 (electronic)  ISSN 1736-4728 (print)
An international scientific journal

Formerly: Proceedings of the Estonian Academy of Sciences, Geology
Published since 1952

Estonian Journal of Earth Sciences

ISSN 1736-7557 (electronic)  ISSN 1736-4728 (print)
An international scientific journal

Formerly: Proceedings of the Estonian Academy of Sciences, Geology
Published since 1952

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First record of Telephina (Trilobita) from the Ordovician of northeastern Estonia and its stratigraphical implications; pp. 83–90

(Full article in PDF format) doi: 10.3176/earth.2011.2.02


Authors

Helje Pärnaste, Adrian Popp

Abstract

For the first time a telephinid trilobite was recorded from the shallow-water rocks of the North Estonian Confacies Belt in the oil-shale mining area of northeast Estonia. A cranidium of Telephina (Telephops) biseriata (Asklund) was collected from a loose boulder of the kerogenous limestone of the Viivikonna Formation, Kukruse Stage, together with a rich assemblage of other trilobites, bryozoans, ostracods and rare graptolites. In its type area Jämtland, Sweden, T. biseriata occurs together with Pygodus anserinus and Hustedograptus teretiusculus in the Ståltorp Limestone Member of the Andersö Shale Formation, marking the latest Darriwilian. The occurrence in the North Estonian Confacies Belt of Telephina, known as a pelagic trilobite inhabiting deeper-water areas, probably reflects a transgression event at this time. Together with T. biseriata, other trilobite taxa such as Remopleurides and Lonchodomas, common in the Hustedograptus teretiusculus Biozone in deeper-water areas, arrive in the North Estonian Confacies Belt. Graptolites from the other loose boulders at the same locality have been identified as Hustedograptus cf. uplandicus, which occur together with a few dendroids.

Keywords

Ordovician, Baltoscandia, Viivikonna Formation, Kukruse Stage, trilobites, Telephina.

References

Ahlberg , P. 1995a. Telephinid trilobites from the Ordovician of Sweden. Palaeontology , 38 , 259–285.

Ahlberg , P. 1995b. Telephinid trilobites from the Ordovician of the East Baltic. GFF , 117 , 49–52.
doi:10.1080/11035899509546196

Angelin , N. P. 1854. Palaeontologia Scandinavica I. Crustacea formationis transitionis , Fasc. 2. Sansom and Wallin , Lund , pp. 21–92.

Asklund , B. 1936. Zur Kenntnis der jämtländischen Ogygiocaris-fauna. Sveriges Geologiska Undersökning , Series C , 395 , 1–12 , pls 1 , 2.

Barrande , J. 1852. Système Silurien du centre de la Bohême. 1ère Partie: Recherches paléontologiques , I Crustacés: Trilobites. Prague and Paris , 935 pp. , 50 pls.

Bruton , D. L. & Høyberget , M. 2006. A reconstruction of Telephina bicuspis , a pelagic trilobite from the Middle Ordovician of the Oslo Region , Norway. Lethaia , 39 , 359–364.
doi:10.1080/00241160600989041

Bergström , S. M. 1973. Correlation of the late Lasnamägian Stage (Middle Ordovician) with the graptolite succession. Geologiska Föreningens i Stockholm Förhandlingar , 95 , 9–18.

Bulman , O. M. B. 1936. On the graptolites prepared by Holm , Pt. VII. The graptolite fauna of the Lower Orthoceras limestone Hälluden , Öland , and its bearing on the evolution of the lower Ordovician graptolites. Arkiv för Zoologi , 28A , 17 , 1–107.

Chatterton , B. D. E. , Edgecombe , G. D. , Vaccari , N. E. & Waisfeld , B. G. 1999. Ontogenies of some Ordovician Telephinidae from Argentina , and larval patterns in the Proetida (Trilobita). Journal of Paleontology , 73 , 219–239.

Eisenack , A. 1937. Neue Mikrofossilien des baltischen Silurs IV. Palaeontologische Zeitschrift , 19 , 217–243.

Fortey , R. A. 1975. Early Ordovician trilobite communities. Fossils and Strata , 4 , 331–352.

Fortey , R. A. & Owens , R. M. 1975. Proetida: a new order of trilobites. Fossils and Strata , 4 , 227–239.

Hadding , A. 1913a. Släktet Telephus Barr. Geologiska Föreningens i Stockholm Förhandlingar , 35 , 25–50.

Hadding , A. 1913b. Undre Dicellograptusskiffern i Skåne jämte några därmed ekvivalenta bildningar. Lunds Universitets Årsskrift , N.F. 2 , 9(15) , 1–91 , pls 18.

Hall , J. 1847. Natural History of New-York , Part VI: Paleontology of New-York , Vol. 1. Albany , New York , 338 pp.

Hansen , T. 2009. Trilobites from the Middle Ordovician Elnes Formation of the Oslo Region , Norway. Fossils and Strata , 56 , 1–215.

Haq , B. U. & Schutter , S. T. 2008. A chronology of Paleozoic sea-level changes. Science , 322 , 64–68.
doi:10.1126/science.1161648

Hints , O. , Nõlvak , J. & Viira , V. 2007. Age of Estonian kuker­site oil shale – Middle or Late Ordovician? Oil Shale , 24 , 527–533.

Karis , L. 1982. The sequence in the Lower Allochthon of Jämtland. In IV International Symposium on the Ordovician System , Field Excursion Guide (Bruton , D. L & Williams , S. J. , eds) , Palaeontological Contributions from the University of Oslo , 279 , 55–63.

Maletz , J. & Egenhoff , S. O. 2004. Dendroid graptolites in the Elnes Formation (Middle Ordovician) , Oslo Region , Norway. Norwegian Journal of Geology , 85 , 217–221.

Männil , R. 1963. Biostratigraficheskoe obosnovanie raschleneniya ordovikskikh otlozhenij zapadnoj Latvii [The biostratigraphic subdivision of the Ordovician strata in Latvia]. Eesti NSV Teaduste Akadeemia Uurimused , 13 , 41–74 [in Russian].

Männil , R. 1976. Distribution of graptoloids in the Ordovician carbonate rocks of the East Baltic area. In Graptolity i stratigrafiya [Graptolites and Stratigraphy] (Kaljo , D. & Koren¢ , T. , eds) , pp. 105–118. Academy of Sciences of the Estonian SSR , Tallinn [in Russian , with English summary].

Månsson , K. 1995. Trilobites and stratigraphy of the Middle Ordovician Killeröd Formation , Scania , Sweden. GFF , 117 , 97–106.
doi:10.1080/11035899509546206

Marek , L. 1952. Contribution to the stratigraphy and fauna of the uppermost part of the Králův Dvůr Shales (Ashgillian). Sbornik Ústředního Ústavu Geologického , 19 , 429–455 (in Czeck , with English summary].

Nikolaisen , F. 1963. The Middle Ordovician of the Oslo Region , Norway. 14. The trilobite family Telephinidae. Norsk Geologisk Tidsskrift , 43 , 345–399.

Nõlvak , J. 2008. Distribution of Ordovician chitinozoans. In Männamaa (F-367) drill core (Põldvere , A. , ed.) , Estonian Geological Sections , 9 , 13–18.

Nõlvak , J. & Goldman , D. 2004. Distribution of Nemagraptus in the East Baltic Ordovician. In WOGOGOB-2004: Conference Materials. Abstracts and Field Guide Book (Hints , O. & Ainsaar , L. , eds) , pp. 75–76. Tartu University Press , Tartu.

Nõlvak , J. & Goldman , D. 2007. Biostratigraphy and taxo­nomy of three-dimensionally preserved nemagraptids from the Middle and Upper Ordovician of Baltoscandia. Journal of Paleontology , 81 , 254–260.
doi:10.1666/0022-3360(2007)81[254:BATOTP]2.0.CO;2

Pålsson , C. , Månsson , K. & Bergström , S. M. 2002. Bio­strati­graphic and palaeoecologic significance of graptolites , trilobites , and conodonts in the Middle–Upper Ordo­vician Andersö Shale: an unusual “mixed facies” deposit in Jämtland , central Sweden. Transactions of the Royal Society of Edinburgh: Earth Sciences , 93 , 35–57.

Pärnaste , H. , Popp , A. & Owens , R. M. 2009. Distribution of the Proetida (Trilobita) in Baltoscandian Ordovician strata. Estonian Journal of Earth Sciences , 58 , 10–23.
doi:10.3176/earth.2009.1.02

Portlock , J. E. 1843. Report on Geology of the County of Londonderry , and Parts of Tyrone and Fermanagh. Dublin and London , 784 pp.

Romano , M. & Owen , A. W. 1993. Early Caradoc trilobites of eastern Ireland and their palaeogeographical significance. Palaeontology , 36 , 681–720.

Thorslund , P. 1960. Notes on the Cambro-Silurian of Jämtland and Road-log. In The Cambrian , Ordovician , and Silurian in Västergötland , Närke , Dalarna , and Jämtland , Central Sweden. 21st International Geological Congress , Guide to Excursions Nos A 23 and C 18 (Thorslund , P. & Jaanusson , V. , eds) , pp. 35–51. Geological Survey of Sweden.

Thorslund , P. & Asklund , B. 1935. Stratigrafiska och tektoniska studier inom Föllingeområdet i Jämtland. Sveriges Geologiska Undersökning , Serie C , 388 , 1–61.

Tripp , R. P. 1976. Trilobites from the basal superstes Mud­stones (Ordovician) at Aldons Quarry , near Girvan , Ayrshire. Transactions of the Royal Society of Edinburgh , 69 , 369–423.

Ulrich , E. O. 1930. Ordovician trilobites of the family Telephidae and concerned stratigraphic correlations. Proceedings of the United States National Museum , 76 , 1–101.

Viira , V. 2008. Conodont biostratigraphy in the Middle–Upper Ordovician boundary beds of Estonia. Estonian Journal of Earth Sciences , 57 , 23–38.
doi:10.3176/earth.2008.1.03

Viira , V. , Aldridge , R. J. & Curtis , S. 2006. Conodonts of the Kiviõli Member , Viivikonna Formation (Upper Ordovician) in the Kohtla section , Estonia. Proceedings of the Estonian Academy of Sciences , Geology , 55 , 213–240.

Wandås , B. T. G. 1984. The Middle Ordovician of the Oslo Region , Norway. 33. Trilobites from the lowermost part of the Ogygiocaris Series. Norsk Geologisk Tidsskrift , 63 (for 1983) , 211–267.

Whittington , H. B. & Kelly , S. R. A. 1997. Morphological term applied to trilobites. In Treatise on Invertebrate Paleontology , Part O. Arthropoda 1. Trilobita , revised volume 1: Introduction (Kaesler , R. I. , ed.) , pp. 313–329. Geological Society of America , Boulder , and University of Kansas Press , Lawrence.

Wiman , C. 1895. Ueber die Graptolithen. Bulletin of the Geological Institutions of the University of Uppsala , 2 , 239–316.
 
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