期刊
GEOLOGICAL MAGAZINE
卷 137, 期 2, 页码 207-209出版社
CAMBRIDGE UNIV PRESS
DOI: 10.1017/S0016756800003800
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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 Pridoli and into the early Devonian, showing some changes during this time.
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