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1978 | 23 | 4 |

Tytuł artykułu

Discoveries on graptolites by X-Ray studies

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Języki publikacji

EN

Abstrakty

EN
The X-ray method has been used for analysing pyritized graptolites with the purpose of finding traces of the unknown soft parts. The investigated material comprises mainly Llandoverian graptolites from Bornholm, Denmark, which occur in dark grey shales and frequently are pyritized. The graptolites are generally uniformly filled with pyrite throughout the rhabdosomes. However, at a few horizons from the cyphus Zone, pyrite is observed specially concentrated in the distal part of the thecal tubes, both in diplograptids and monograptids. In other specimens from the same horizon pyrite is found in rounded concentrations just outside the thecal apertures. Continuous extraskeletal pyrite is rare, but is nevertheless found (preferably around the distal parts of some Retiolites rhabdosomes). The pyrite replacements within the thecae and outside the thecal mouths have almost equal form and size throughout each rhabdosome, and may have replaced decaying soft parts. Howeyer, with the present material it has not been possible to clarify any exact structures.

Wydawca

-

Rocznik

Tom

23

Numer

4

Opis fizyczny

p.463-471,ref.

Twórcy

  • Institute of Historical Geology and Palaentology, University of Copenhagen, Oster Volgade 10, DK-1350 Copenhagen K, Denmark

Bibliografia

  • BJERRESKOV, M. 1975. Llandoverian and Wenlockian graptolites from Bornholm. - Fossils and Strata, 8, 94 pp.
  • BLIND, W. and STURMER, W. 1977. Viriatellina fuchsi Kutscher (Tentaculoidea) mit Sipho und Fangarmen. - Neues Jahrb. Geol. Paläont., 513-522.
  • BRÜHL, 1896. Ueber die Verwendung von Röntgenschen X-Strahlen zu palaeontologisch- diagnostischen Zwecken. - Verhandlungen d. Berliner Physiologischen Gesellschaft im Arch. Anat. Physiol., Physiologischer Teil., 547-550.
  • BULMAN, O.M.B. 1970. Graptolithina, with sections on Enteropneusta and Pterobranchia. In: Teichert, C. (ed.), Treatise on Invertebrate Paleontology, V (2nd edition), XXXii +163, Geol. Soc. Amer. & Univ. Kansas Press.
  • EMERY, K.O. and RITTENBERG, S.C. 1952. Early diagenesis of California basin sediments in relation to origin of oil. - Bull. Amer. Assoc, Petrol. Geol., 36, 736-806.
  • KIRK, N.H. 1972. Some thoughts on the construction of the rhabdosome in the Graptolithina with special reference to extrathecal tissue and its bearing on the theory of automobility. - Univ. Coll. Wales, Aberystwyth, Dept. Geol. Publ., 1, 1-21.
  • KOZŁOWSKI, R. 1949. Les Graptolithes et quelques nouveaux groupes d'animaux du Tremadoc de la Pologne. - Palaeont. Pol., 3, 1-235.
  • - 1966. On the structure and relationships of graptolites. - J. Paleont., 40, 489-501.
  • LEMOINE, M. 1896. De l'application des rayons de Röntgen à la paléontologie. - C. R. Acad. Sci., 123, 764-765.
  • RICKARDS, R.B. 1975. Palaeoecology of the Graptolithina, an extinct class of the phylum Hemichordata. - Biol. Rev., 50, 397-436.
  • STÜRMER, W. 1969. Pyrit-Erhaltung von Weichteilen bei devonischen Cephalopoden. - Paläont. Z. 43, 10-12.
  • - 1970. Soft parts of cephalopods and trilobites: some surprising results of X-ray examinations of Devonian slates. - Science, 170, 1300-1302.
  • - and BERGSTRÖM, J. 1973. New discoveries on trilobites by X-rays. - Paläont. Z., 47, 104-141.
  • - and - 1976. The arthropods Mimetaster and Vachonisia from the Devonian Hunsrück Shale. - Ibidem, 50, 78-111.
  • URBANEK, A. 1976. The problem of Graptolite affinities in the light of ultrastructural studies on peridermal derivatives in pterobranchs. - Acta Palaeont. Pol., 21, 3-36.

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Bibliografia

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