In the Lower Ordovician platform and slope deposits of western Newfoundland and in platform deposits of Oeland (Sweden) transgressive-regressive cycles of the third order, superimposed to the global Cambro-Ordovician sea level rise have been recognized. Conodont faunas from the Newfoundland slope deposits allow correlation between Laurentia and Baltica across the Iapetus Ocean. Four transgressive-regressive cycles have been recognized
Sea level changes and conodont correlation across the Iapetus Ocean during the Late Tremadocian - Early Arenigian.
BAGNOLI, GABRIELLA
1994-01-01
Abstract
In the Lower Ordovician platform and slope deposits of western Newfoundland and in platform deposits of Oeland (Sweden) transgressive-regressive cycles of the third order, superimposed to the global Cambro-Ordovician sea level rise have been recognized. Conodont faunas from the Newfoundland slope deposits allow correlation between Laurentia and Baltica across the Iapetus Ocean. Four transgressive-regressive cycles have been recognizedFile in questo prodotto:
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