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2006 | 51 | 2 |

Tytuł artykułu

Apparatus of the conodont Scolopodus striatus Pander, 1856 and re-evaluation of Pander's species of Scolopodus

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Języki publikacji

EN

Abstrakty

EN
The Lower Ordovician conodont Scolopodus striatus Pander, 1856 (= Scolopodus rex Lindström, 1955) has an apparatus composed of five element morphotypes: acontiodiform, subrounded, compressed paltodiform, paltodiform, and scandodiform. The identification of the morphotypes is based on the general asymmetry of elements and shape of their bases. The elements are variable within each morphological group and form a continuous transition series generally reflected in differences in the depth of the basal cavity, height and degree of lateral compression of the base. The new collection from the localities near St. Petersburg, the type area of the first investigations on conodonts by Christian Pander in 1856, was examined and species of Scolopodus named by him are revised. All Pander’s species with the exception of the type species Scolopodus sublaevis are identified as a single species of Scolopodus that was named 99 years later as Scolopodus rex. The S. sublaevis sensu formae was not recognised in collections studied and its validity is questionable. S. striatus is the most easily recognisable among Pander’s species of Scolopodus and is here proposed to be a senior synonym of S. rex.

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-

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Tom

51

Numer

2

Opis fizyczny

p.247-260,fig.,ref.

Twórcy

  • All Russian Scientific Research Geological Institute, Sredny 74, 199106 St.Petersburg, Russia

Bibliografia

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  • Fåhræus, L.E. 1982. Recognition and redescription of Pander’s (1856) Scolopodus (form−) species—constituents of multi−element taxa (Conodontophorida, Ordovician). Geologica et Palaeontologica 16: 19–28.
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  • Lindström, M. 1964. Conodonts. 196 pp. Elsevier, Amsterdam.
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  • Löfgren, A. 1978. Arenigian and Llanvirnian conodonts from Jämtland, northern Sweden. Fossils and Strata 13: 1–129.
  • Löfgren, A. 1994. Arenig (Lower Ordovician) conodonts and biozonation in the eastern Siljan district, Central Sweden. Journal of Paleontology 68: 1350–1368.
  • Löfgren, A. 1995. The middle Lanna/Volkhov Stage (middle Arenig) in Sweden and its conodont fauna. Geological Magazine 132: 693–711.
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  • Löfgren, A. 1999. The Ordovician conodont Semiacontiodus cornuformis (Sergeeva, 1963) and related species in Baltoscandia. Geologica et Palaeontologica 33: 71–91.
  • Nicoll, R.S. 1994. Seximembrate apparatus structure of the Late Cambrian coniform conodont Teridontus nakamurai from the Chatsworth Limestone, Georgina Basin, Queensland. Bureau of Mineral Resources. Journal of Australian Geology and Geophysics 15: 367–379.
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  • Seo, K.−S., Lee, H.−Y., and Ethington, R.E. 1994. Early Ordovician conodonts from the Dugumol Formation in the Baegunsan Syncline, eastern Yeongweol and Samcheog areas, Kangweon−Do, Korea. Journal of Paleontology 68: 599–616.
  • Sergeeva, S.P. 1974. Some mew conodonts from the Ordovician deposits of Leningrad region [in Russian]. Paleontologičeskij sbornik 2: 79–84.
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  • Tolmacheva, T.Ju., Koren’, T.N., Holmer, L.E., Popov, L.E., and Raevskaya, E. 2001. The Hunneberg Stage (Ordovician) in the area east of St. Petersburg, north−western Russia. Paläontologische Zeitschrift 74: 543–561.
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Bibliografia

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