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2007 | 52 | 4 |

Tytuł artykułu

Primary structure of the connecting ring of ammonoids and its preservation

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Warianty tytułu

Języki publikacji

EN

Abstrakty

EN
The most distinctive and important element of the hydrostatic organ of ammonoids and nautiloids is the siphuncular tube. It consists of mineral and organic segments (so−called connecting rings). The connecting ring of ammonites never preserves its original organic matter in the mineralized state, usually having undergone diagenetic phosphatisation, more rarely, calcification, or even complete loss. Our knowledge about its original ultrastructure is based upon comparison with Recent Nautilus and phosphatised or calcified ammonite fossils. We show that depending on the taphonomic history, both calcium phosphate and calcite can participate in the diagenesis of the connecting ring wall. Under standard light microscopy, the phosphatised elements are indistinguishable from the calcified ones. Both are dark brown in colour, due to an excess of carbon. The structure of the phosphatised siphuncle does not closely replicate the structure of its organic elements. This casts doubts on conclusions of other authors who described a complex porous structure in ammonite siphuncles, which is completely dissimilar to the siphuncular structure of Recent Nautilus and suggests that this organ functioned differently in ammonites. SEM observations using a BSE detector on the calcified parts of the walls of connecting rings revealed a multilayered structure with perpendicular elements connecting particular layers, resembling the structure of a stacked nacreous layer.

Wydawca

-

Rocznik

Tom

52

Numer

4

Opis fizyczny

p.823-827,fig.,ref.

Twórcy

autor
  • Institute of Palaeobiology, Polish Academy of Sciences, Twarda 51/55, 00-818 Warsaw, Poland
autor
autor

Bibliografia

  • Andalib, F. 1972. Mineralogy and preservation of siphuncles in Jurassic cephalopods. Neues Jahrbuch fur Geologie und Paläntologie Abhandlungen 140: 33–48.
  • Dzik, J. 1990. The concept of chronospecies in ammonites. In: G. Pallini, F. Cecca, S. Cresta, and M. Santantonio (eds.), Atti del secondo convegno internazionale Fossili, Evoluzione, Ambiente Pergola 25–30 ottobre 1987 estratto, 273–289.
  • Hewitt, R.A. and Westermann, G.E.G. 1983. Mineralogy, structure and homology of ammonoid siphuncles. Neues Jahrbuch fur Geologie und Paläntologie Abhandlungen 165: 378–396.
  • Kulicki, C. 1974. Remarks on the embryogeny and postembryonal development of ammonites. Acta Palaeontologica Polonica 19: 201–224.
  • Kulicki, C. 1979. The ammonite shell: Its structure, development and biological significance. Palaeontologia Polonica 39: 97–142.
  • Kulicki, C. 1994. Septal neck−siphuncular complex in Stolleyites (Ammonoidea), Triassic, Svalbard. Polish Polar Research 15: 37–49.
  • Kulicki, C. and Doguzhaeva, L. 1994. Development and calcification of the ammonitella shell. Acta Palaeontologica Polonica 39: 17–44.
  • Kulicki, C. 1996. Ammonoid shell microstructure. In: N.H. Landman, K. Tanabe, and R.A. Davis (eds.), Ammonoid Paleobiology, 65–101. Topics in Geobiology, Vol. 13. Plenum Press, New York.
  • Kulicki, C. and Mutvei, H. 1982. Ultrastructure of the siphonal tube in Quenstedtoceras (Ammonitina). Stockholm Contributions in Geology 37: 129–138.
  • Makowski, H. 1952. La faune callovienne de Łuków en Pologne. Palaeontologia Polonica 4: 1–64.
  • Makowski, H. 1962. Problem of sexual dimorphism in ammonites. Palaeontologia Polonica 12: 1–92.
  • Mutvei, H. 1972. Ultrastructural studies on cephalopod shells, part I, The septa and siphonal tube in Nautilus. Bulletin of the Geological Institutions of the University of Uppsala, NS 3 (8): 237–261.
  • Mutvei, H., Weitschat. W., Doguzhaeva, L., and Dunca, E. 2004. Connecting ring with pore canals in two genera of Mesozoic ammonoids. Mitteilungen der Geologisch−Palaeontologische Institut der Universitat Hamburg 88: 135–144.
  • Obata, I., Tanabe, K., and Fukuda, Y. 1980. The ammonite siphuncular wall: its microstructure and functional significance. Bulletin of the National Science Museum, Series C (Geology and Paleontology) 8: 59–72.
  • Tanabe, K., Kulicki, C., and Landman, N.H. 2005. Precursory siphuncular membranes in the body chamber of Phylloceras and comparisons with other ammonoids. Acta Palaeontologica Polonica 50: 9–18.
  • Tanabe, K., Mapes, R.H., Sasaki, T., and Landman, N.H. 2000. Soft−part anatomy of the siphuncle in Permian prolecanitid ammonoids Lethaia 33: 83–91.
  • Weitschat, W. and Bandel, K. 1991. Organic components in phragmocones of Boreal Triassic ammonoids: implications for ammonoid biology. Paläontologische Zeitschrift 65: 269–303.

Typ dokumentu

Bibliografia

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Identyfikator YADDA

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