Lower Aptian charophytes are first reported from the Central Tunisian Atlas.
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A new stratigraphic framework the non-marine Kebar Formation is provided.
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Biostratigraphic dating by charophytes supports previous dating with ostracods.
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Clavatoraceans of European affinity are first reported in North Africa.
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The Tethyan Archipelago was an effective Laurasian-Gondwanan biogeographic bridge.
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