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TitleSiliceous microfossils and agglutinated foraminifera from the Upper Cretaceous Smoking Hills and Mason River formations in the Smoking Hills area, Northwest Territories
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LicencePlease note the adoption of the Open Government Licence - Canada supersedes any previous licences.
AuthorDiaz, J F; Galloway, J MORCID logo; Bringué, MORCID logo; Pedersen, P K; Grasby, S EORCID logo
SourceGeological Survey of Canada, Open File 8716, 2020, 21 pages, https://doi.org/10.4095/325466 Open Access logo Open Access
Image
Year2020
PublisherNatural Resources Canada
Documentopen file
Lang.English
Mediaon-line; digital
File formatpdf
ProvinceNorthwest Territories
NTS97C/06; 97C/13
AreaSmoking Hills; Horton River; Cape Bathurst; Franklin Bay; Canadian Arctic
Lat/Long WENS-127.0000 -126.9667 69.4833 69.4500
Lat/Long WENS-127.1167 -127.1167 69.9833 69.9667
Subjectspaleontology; stratigraphy; Nature and Environment; Science and Technology; Upper Cretaceous; Maastrichtian; Campanian; micropaleontology; microfossils; diatoms; fossil assemblages; fossil distribution, strata; fossil lists; fossil zones; type sections; bedrock geology; lithology; sedimentary rocks; mudstones; jarosite; sandstones; field work; correlations; Smoking Hills Formation; Mason River Formation; Foraminifera; Radiolarians; Silicoflagellates; Sponges; Spicules; Horton-Anderson Plains; Sverdrup Basin; Western Interior Seaway; Phanerozoic; Mesozoic; Cretaceous
Illustrationslocation maps; tables; stratigraphic columns
ProgramGEM2: Geo-mapping for Energy and Minerals TransGEM
Released2020 04 23
AbstractFive microfossil groups are herein described from the Upper Cretaceous Smoking Hills and Mason River formations in the Horton River area (Northwest Territories). Microfossil assemblages from the Smoking Hills Formation are dominated by radiolarians and foraminifera whereas the Mason River Formation mainly contains diatoms, silicoflagellates, and sponge spicules. These microfossil groups have been reported before in these units and age-equivalent strata from the Canadian Arctic except for radiolarians. The radiolarian assemblage described in this study represents one of the most diverse and abundant assemblages reported in Campanian-Maastrichtian rocks in North America and can be used to reconstruct the climatic, paleoceanographic, and paleobiogeographic conditions that took place at the end of the Cretaceous Period. This Open File documents the stratigraphic occurrence of the microfossil types.
Summary(Plain Language Summary, not published)
Five microfossil groups are described from the Upper Cretaceous Smoking Hills and Mason River formations in the Horton River area (Northwest Territories): radiolarians, foraminifera, diatoms, silicoflagellates, and sponge spicules. The radiolarian assemblage described in this study represents one of the most diverse and abundant assemblages reported in Upper Cretaceous rocks from North America. These microfossils can be used for stratigraphic investigations and to reconstruct the environmental conditions during the end of the Cretaceous Period.
GEOSCAN ID325466

 
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