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We Wuz



         What?

















                                                                               Brighton area fossils
                                                                               including clockwise from
                                                                               the top left a cephalopod
                                                                               brachiopod a segment of a
                                                                               gastropod and the shadow
                                                                               of another cephalopod. Left:
                                                                               Brighton area construction
                                                                               site with excavated
                                                                               sedimentary rock pile.








                                                                               A History of Brighton,
                                                                               Part One
                                                                               If you’re in eastern
                                                                               Northumberland, you
                                                                               are over top of some of
                                                                               the oldest rocks in Ontario,
                                                                               barring the Canadian Shield
                                                                               to the North. Brighton’s
                                                                               prehistory is most easily
                                                                               appreciated ‘down’ in Presquile
                                                                               along its rocky southern
                                                                               shoreline, which exposes
                                                                               the sedimentary limestone
                                                                               that was laid down during
                                                                               the Middle Ordovician period,
                                                                               some 460 to 470 million years
                                                                               ago. At that time, Canada, as
                                                                               part of the North American
                                                                               tectonic plate, was roughly
                                                                               situated along the equator
                                                                               and the world was much
                                                                               warmer. The sea level was also
                                                                               much higher and there wasn’t
                                                                               anywhere near enough oxygen
            By Phillip M. Kinzinger                                            for humans to breath.

         22     The Brighton Beacon
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