Affiliation:
1. Department of Earth Sciences University of Bristol Bristol BS8 1RL United Kingdom
2. Biological Sciences University of Aberystwyth Penglais Aberystwyth Ceredigion SY23 1NL United Kingdom
Abstract
AbstractMost remains of Carboniferous lyginopteridalean seed‐plant fronds used to be classified in a single fossil‐genus (Sphenopteris) based mainly on pinnule morphology. By incorporating additional characters linked to frond architecture and rachial features a more natural taxonomy has now been achieved. Eight fossil‐genera of lyginopteridalean fronds are now recognised (Sphenopteris,Calymmotheca,Eusphenopteris,Karinopteris,Mariopteris,Palmatopteris,Spathulopteris,Sphenopteridium) for which the diagnostic descriptions, nomenclatural types and stratigraphical/chronological distribution are clarified. This provides a more natural and therefore robust means of recording these fossils, which will help improve studies on past plant diversity and floristics. A by‐product of this revision is that some fossil‐species of fern fronds previously placed inSphenopteriswill need to be reclassified into fossil‐genera that are defined on reproductive structures.
Subject
Plant Science,Ecology, Evolution, Behavior and Systematics
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