Late Ordovician carbonate mounds from North Greenland: a peri-Laurentian dimension to the Boda Event?
Late Katian (Late Ordovician) carbonate mudmounds in the TuresO Formation, Peary Land, North Greenland, succeed normal marine faunas dominated by brachiopods, bryozoans, cephalopod and gastropod molluscs, aulaceratid stromatoporoids, corals and receptaculitid algae, in the BOrglum River Formation, and are themselves succeeded by organic-rich, largely barren limestones. This peri-Laurentian success