Selected palynomorphs from the Morgan Creek locality in southern Saskatchewan, Canada, indicate that the basin of deposition was an inland fresh-water pond or lake environment. The region of the basin experienced warm air and ocean surface temperatures (20-25C), low pH values (3.5-4.0), and moderate to high rainfall.The presence of Pandanus, Livistona, and other angiosperm taxa strongly suggests that the Morgan Creek locality has its modern analogue in areas within Southeast Asia -Indomalaysia.