Abstract

Tracheids of Psilophyton dawsonii Banks, Leclercq, and Hueber 1975 from calcareous pebbles of late Early Devonian age on the Gaspé Peninsula, eastern Canada, are shown to have scalariform bordered and circular bordered pits. Macerated tracheids embedded in Spurr epoxy resin and sectioned at 2 μm; peels, ground sections, SEM and petrographic observations all indicate that interconnections between the scalariform bars are composed of secondary wall material and that the patterns produced are not artifacts of preservation. The interconnections produce a wide range of patterns from simple vertical strands, to reticula, to more extensive interconnections that outline circular openings. The circular openings result in scalariform bordered pits that are considered to be multiaperturate. P. dawsonii is believed to illustrate the most complex pitting yet demonstrated conclusively in Early Devonian time. Among trimerophytes P. forbesii, tracheids of P. charientos, and Hostinella from Röragen, Norway lack only the circular bordered pits.

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