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 recognized
1994
Bagnoli, Gabriella
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11568/233569
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