Palynostratigraphic investigation of upper maastrichtlan and paleocene strata near Tate Lake, N.W.T. ...
Sedimentary strata near Tate Lake, south of Norman Wells, N.W.T., were investigated using palynomorph analysis indicating the presence of Upper Maastrichtian and Paleocene beds. The Upper Maastrichtian sections contain tv/o local palynostratigraphic zones correlative with Srivastava's Wodehouse...
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| Format: | Text |
| Language: | English |
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University of British Columbia
2011
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| Online Access: | https://dx.doi.org/10.14288/1.0052405 https://doi.library.ubc.ca/10.14288/1.0052405 |
| Summary: | Sedimentary strata near Tate Lake, south of Norman Wells, N.W.T., were investigated using palynomorph analysis indicating the presence of Upper Maastrichtian and Paleocene beds. The Upper Maastrichtian sections contain tv/o local palynostratigraphic zones correlative with Srivastava's Wodehousea spinata and Manci-corpus gibbus zones of the Edmonton and Battle Formations of Alberta, and other Maastrichtian formations in western North America. The Paleocene strata compare lithologically and palynologically with the Lower Fort Union Group of Montana and Wyoming, the post-Brazeau beds of the Alberta Foothills, the upper part of the Bonnet Plume Formation, N.W.T., and Tertiary coal deposits in Spitzbergen. A progressive cooling in climate from subtropical to warm temperate during Upper Maastrichtian times is indicated by the decrease in the number of angiosperm species and greater influx of gymnosperms and pteridophytes, A marked change in microflora and lithology at the Cretaceous-Tertiary boundary indicates ... |
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