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This page is a summary of: Ammonoid-calibrated sporomorph assemblages reflect a shift from hygrophytic to xerophytic elements in the late Anisian (Middle Triassic) of the Southern Alps (Italy), Review of Palaeobotany and Palynology, July 2015, Elsevier,
DOI: 10.1016/j.revpalbo.2014.02.010.
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