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- W2077081719 abstract "A thin, impure limestone was found in situ on Precambrian bedrock at latitude 70°36.6′ N and longitude 75°20′ W some 26 km northwest of the Barnes Ice Cap. The unit consists of undulating laminations composed of alternating fine- and coarse-grained sediment, which are interpreted as a series of algal mats or algal-laminated sediments. An analysis of enclosed palynomorphs indicates the presence of Ulmus, Taxodiutm, Liriodendron, Carpinus, and Engelhardtia plus other genera. On the basis of the microflora a Paleogene age is assigned to the unit. The climate at that time was warm-temperate and the environment suggested is a freshwater marsh or swamp. The outcrop is restricted to a single hill summit and its location suggests considerable Neogene geomorphological activity, primarily river-cutting associated with vertical movements along the western margin of the Davis Strait/Baffin Bay Tift." @default.
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- W2077081719 date "1972-03-01" @default.
- W2077081719 modified "2023-09-27" @default.
- W2077081719 title "An Early Tertiary Outcrop in North-Central Baffin Island, Northwest Territories, Canada: Environment and Significance" @default.
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- W2077081719 doi "https://doi.org/10.1139/e72-019" @default.
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