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The Floian corresponds to the lower Arenig; the Arenig continues until the early Darriwilian, subsuming the Dapingian.
The Llanvirn occupies the rest of the Darriwilian, and terminates with it at the base of the Late Ordovician.
The small continent Avalonia separated from Gondwana and began to move north towards Baltica and Laurentia, opening the Rheic Ocean between Gondwana and Avalonia.
The Taconic orogeny, a major mountain-building episode, was well under way in Cambrian times.
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