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Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK
* E-mail: rbr1000{at}esc.cam.ac.uk
It is argued that there is overwhelming evidence from a good graptolite record that the earliest club mosses on Earth were of Gorstian (Ludlow, Silurian) age, and that Baragwanathia longifolia Lang & Cookson and its associated flora persisted through the P
ídolí and into the early Devonian, showing some changes during this time.
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