Abstract
It was with great interest that I read the recent article by Westgate, Chen, and Delorme reporting on the discovery of ostracode fossils in the Sunnybrook diamicton in the MetroToronto region of southern Ontario. I have followed the ongoing controversy surrounding the interpretations of the depositional origin of the sediments in the Metro-Toronto area, as I think most Canadian Quaternary geologists have. I therefore wish to comment on a number of points brought out in the article.
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