Clarkson, Euan N. K., Taylor, Cecilia M. (1995) Ontogeny of the trilobite Olenus wahlenbergi Westergård, 1922 from the upper Cambrian Alum Shales of Andrarum, Skåne, Sweden. Transactions of the Royal Society of Edinburgh: Earth Sciences, 86 (1) 13-34 doi:10.1017/s0263593300002133
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Ontogeny of the trilobite Olenus wahlenbergi Westergård, 1922 from the upper Cambrian Alum Shales of Andrarum, Skåne, Sweden | ||
| Journal | Transactions of the Royal Society of Edinburgh: Earth Sciences | ||
| Authors | Clarkson, Euan N. K. | Author | |
| Taylor, Cecilia M. | Author | ||
| Year | 1995 | Volume | 86 |
| Issue | 1 | ||
| Publisher | Cambridge University Press (CUP) | ||
| DOI | doi:10.1017/s0263593300002133Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 494448 | Long-form Identifier | mindat:1:5:494448:9 |
| GUID | 0 | ||
| Full Reference | Clarkson, Euan N. K., Taylor, Cecilia M. (1995) Ontogeny of the trilobite Olenus wahlenbergi Westergård, 1922 from the upper Cambrian Alum Shales of Andrarum, Skåne, Sweden. Transactions of the Royal Society of Edinburgh: Earth Sciences, 86 (1) 13-34 doi:10.1017/s0263593300002133 | ||
| Plain Text | Clarkson, Euan N. K., Taylor, Cecilia M. (1995) Ontogeny of the trilobite Olenus wahlenbergi Westergård, 1922 from the upper Cambrian Alum Shales of Andrarum, Skåne, Sweden. Transactions of the Royal Society of Edinburgh: Earth Sciences, 86 (1) 13-34 doi:10.1017/s0263593300002133 | ||
| In | (1995) Transactions of the Royal Society of Edinburgh: Earth Sciences Vol. 86 (1) Cambridge University Press (CUP) | ||
| Abstract/Notes | AbstractThe upper Cambrian trilobite Olenus wahlenbergi Westergård, 1922 occurs abun- dantly in stinkstone concretions in the Alum Shales at Andrarum, in Skåne, southern Sweden (Olenus/Homagnostus obesus Zone). All growth stages from anaprotaspis onwards are represented, though the early stages are comparatively uncommon and complete specimens are rare. Fine details of structure are preserved, suitable for scanning electron microscopic study.The protaspis has five axial rings, which in the adult become divided transversely and reduced to three, and the preglabellar field expands markedly in the holaspis. The librigena broadens during development and the eye, with its widely separated lenses is retained on the librigena throughout meraspid development. The visual surface dehisces during ecdysis from the early holaspid onwards, due to emplacement of the ocular suture. The hypostome apparently changes from a conterminant to a natant condition in the early holaspis, which is consistent with the growth of the preglabellar field at this stage. The transitory pygidium has a slightly serrated margin throughout development, but becomes entire when all thoracic segments have been liberated.Cuticular sculpture changes dramatically throughout ontogeny. Large (Type A) tubercles appear on the fixigena in early meraspides; these become prominent and coalesce by the end of meraspid development. They are abruptly replaced by smaller (Type B) tubercles in the early holaspid, which link to form a rough network in mature specimens. Comparable Type A tubercles in early meraspid librigenae give rise to a strong polygonal caecal sculpture in holaspids, while a radial sculpture on the broadening anterior border develops independently. The significance of these cuticular changes remains obscure. A median occipital organ is described for the first time in the Olenidae. | ||
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