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Department of Geology, University College of Wales, Aberystwyth, Dyfed SY23 3DB, U.K.
The construction of graptolite periderm is discussed with particular reference to the rival extra-thecal tissue (secretion) and pterobranch (mortaring) models, and it is concluded that only the former model fits the observed structures. Evidence from a number of retiolite graptoloids demonstrates that they also have a continuous periderm, and were constructed in a similar manner.
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D. K. Loydell Worldwide correlation of Telychian (Upper Llandovery) strata using graptolites Geological Society, London, Special Publications, 1993; 70: 323 - 340. [Abstract] [PDF] |
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