Ediacaran paleosols of the Gaskiers Formation lack large root traces, but show soil profile differentiation (clay enrichment and depletion of alkali and alkaline earth elements at the expense of feldspar and rock fragments) and diagnostic soil structures (blocky peds, argillans, sepic plasmic fabric...
In accordance with the stratigraphic position of this recently discovered diamictite horizon, we suggest it represents a glacial event within the Ediacaran Period, probably related to the Gaskiers Glaciation with an age of approximately 580 Ma (Bowring et al., 2003; Knoll et al., 2004)....
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Ediacaran paleosols of the Gaskiers Formation lack large root traces, but show soil profile differentiation (clay enrichment and depletion of alkali and alkaline earth elements at the expense of feldspar and rock fragments) and diagnostic soil structures (blocky peds, argillans, sepic plasmic fabric...
Glacially-influenced deep-marine sedimenta- tion of the late Precambrian Gaskiers Formation, Newfoundland, Canada. Sedimentology 36, 601e620.Eyles, N., and Eyles, C.H., 1989, Glacially-influenced deep-marine sedimenta- tion of the late Precambrian Gaskiers Formation, Newfoundland, Canada: ...
Radiometric and stratigraphic constraints on terminal Ediacaran (post-Gaskiers) glaciations and meta- zoan evolution. Precambrian Research 182, 402-412.Hebert, C.L., Kaufman, A.J., Penniston Dorland, S.C., and Martin, A.J., Radiometric and stratigraphic constraints on terminal Ediacaran (post...
Macrofossils of the inferred protistゞrade organism Palaeopascichnus linearis occur stratigraphically beneath glacial diamictites of the ~580 Ma, Gaskiers〆quivalent, Trinity 'facies' of the Rocky Harbour Formation on the Bonavista Peninsula of Newfoundland, Canada. These fossils significantly preヾ...
GRAVENOR, C.P., 1980, Heavy minerals and sedimentological studies on the glaciogenic Late Precambrian Gaskiers Formation of Newfoundland: Canadian Journal of Earth Sciences, v. 17, p. 1331-1341.gRAvenoR, C.P. 1980. Heavy minerals and sedimentological studies in the glaci- ogenic Late ...
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