The paleoenvironments that resulted in the Ottawa area varied with time. At some points in history it was dry land inhabited by land organisms. At other times, it was covered with Epeiric seas and only marine organisms could survive. Then there was the glacial period in which most of Canada was covered with glaciers and few organisms survived.
The organisms at the time of the Cambrian/Ordovician transgressions had several life modes. There were infauna and epifauna; which are terms for organisms living in the sea floor or on the sea floor respectively. Within the epifauna there were vagile or moving creatures and sessile or motionless creatures. There were benthic organisms or bottom dwellers, planktic organisms or floaters, and nectic organisms or swimmers.
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Painting by Michael Léveiller
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