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Description
Ichnology of the Ediacaran–Cambrian Chapel island formation of Newfoundland, CanadaThe Chapel Island Formation is a 1000+ m thick, mainly siliciclastic succession that is well exposed in coastal cliffs of Burin Peninsula, southeastern Newfoundland, eastern Canada. This unit contains an outstanding record of late Ediacaran early Cambrian trace fossils with some intervals rich in small shelly fossils, and in 1992 the Fortune Head section was ratified as Global Stratotype Section and Point for the Cambrian System. This contribution

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