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2005 | 50 | 3 |

Tytuł artykułu

Ontogeny of a new cyrtosymboline trilobite from the Famennian of Morocco

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Warianty tytułu

Języki publikacji

EN

Abstrakty

EN
Abundant trilobite remains were recovered from late mid−Famennian marlstones from various sites in Eastern Tafilalet, southeast Morocco. All belong to a single taxon previously identified as Cyrtosymbole (Waribole) prima. This taxon is designated the type species of Osmolskabole gen. nov. A redefinition of this species, including the description of newly discovered, disarticulated exuviae both in limestone and silicified state of preservation, is given. In particular, silicified sclerites of various sizes allow the first complete growth series of a cyrtosymboline proetid to be presented. The close morphological resemblance of its protaspid stages to known proetoid larvae emphasizes the homogeneity of the early ontogeny in this superfamily. The Famennian proetoid anaprotaspis is also of comparable size to that of other Devonian proetoid larvae. However, their size−range is much less than that observed in Carboniferous larvae. This suggests that the survival of proetoid trilobites at the Frasnian−Famennian Kellwasser crisis did not result from a modification of the developmental strategy, as it might have been the case at the terminal Devonian extinction event. Moreover, O. prima possesses a plectrum from the metaprotaspid to the mid meraspid periods. This implies that the natant hypostomal condition is not steadily acquired early in the ontogeny of the Proetida. Thus we preclude the use of this character in the diagnosis of this order.

Wydawca

-

Rocznik

Tom

50

Numer

3

Opis fizyczny

p.449-464,fig.,ref.

Twórcy

  • Universite Montpellier II, 34095 Motpellier Cedex 05, France
autor

Bibliografia

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  • Alberti, H. 1975b. Neue Trilobiten (Waribole) aus dem Ober−Devon IV–V (Nord−Afrika und Mittel−Europa) – Beitrag 4 – Revision einiger Typus−Spezies der Proetidae Salter, 1864, aus dem Ober−Devon II–V. Neues Jahrbuch für Geologie und Paläontologie Abhandlungen 150: 207–226.
  • Alberti, H. 1976. Neue Trilobiten (Cyrtosymbole) aus dem Ober−Devon II (Nord−Afrika und Mittel−Europa) – Beitrag 5. Neues Jahrbuch für Geologie und Paläontologie Abhandlungen 152: 19–50.
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  • Chatterton, B.D.E., Edgecombe, G.D., Vaccari, N.E., and Waisfeld, B.G. 1999. Ontogenies of some Ordovician Telephinidae from Argentina, and larval patterns in the Proetida (Trilobita). Journal of Paleontology 73: 219–239.
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  • Chlupáč, I. 1966. The Upper Devonian and Lower Carboniferous trilobites of the Moravian karst. Sborník Geologických Věd – Paleontologie 7: 1–143.
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  • Crônier, C. and Clarkson, E.N.K. 2001. Variation of eye−lens distribution in a new late Devonian phacopid trilobite. Transactions of the Royal Society of Edinburgh 92: 103–113.
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  • Fortey, R.A. and Clarkson, E.N.K. 1976. The function of the glabellar “tubercule” in Nileus and other trilobites. Lethaia 9: 101–106.
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  • Hawle, I. and Corda, A.J.C. 1847. Prodrom einer Monographie der böhmischen Trilobiten. Abhandlungen Koeniglichen Boehmischen Gesellschaft der Wissenschaften 5: 1–176.
  • Hupé, P. 1953. Classe des trilobites. In: J. Piveteau (ed.), Traité de Paléontologie. Vol. 3, Les formes ultimes d’Invertébrés: Morphologie et évolution: Onychophores–Arthropodes–Echinodermes–Stomocordés, 44–246. Masson, Paris.
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  • Wilmot, N.V. 1991. Sensory field maps of proetide trilobites. Transactions of the Royal Society of Edinburgh, Earth Sciences 82: 183–193.

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Bibliografia

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