Exhumed paleoplains of the Precambrian Shield of North America

1964 ◽  
Vol 262 (7) ◽  
pp. 817-857 ◽  
Author(s):  
J. W. Ambrose
1976 ◽  
Vol 13 (5) ◽  
pp. 697-703 ◽  
Author(s):  
M. Walters ◽  
P. M. Sheehan ◽  
P. J. Lespérance

Graptolites have been recovered from limestones at Lake Waswanipi, Québec, in an Ordovician outlier on the Precambrian Shield. These limestones were previously interpreted as Wilderness, Trenton, or Richmond in age. They are now assigned a middle Climacograptus spiniferus to C. pygmaeus Zone age, dating the transgression over this part of the shield. Associated megafossils, though poorly preserved, are described. Correlations are made with other graptolite-bearing carbonates in eastern and central North America.


1985 ◽  
Vol 63 (8) ◽  
pp. 1482-1493 ◽  
Author(s):  
K. H. Nicholls ◽  
J. F. Gerrath

Electron microscopy of silica scales was used in the identification of 13 taxa of the colonial chrysophyte Synura found in Ontario lakes and ponds, one of which has not been reported previously from North America (Synura spinosa f. longispina Petersen & Hansen). Two other taxa found in Ontario (Synura splendida Korshikov and Synura petersenii f. praefracta Asmund) have previously been reported only once from North America. One new combination is proposed (Synura leptorrhabda (Asmund) Nicholls) which provides for more consistent taxonomy of species in the Synura echinulata group (S. echinulata Korshikov, Synura mammillosa Takahashi, Synura multidentata (Balonov & Kuzmin) Péterfi & Momeu, and S. leptorrhabda). The systematics of other problematic taxa, including the related genus Chrysodidymus, are discussed. Samples containing Synura spp., previously implicated in 11 recent cases of "fishy" taste and odour in Ontario lakes, were reexamined by electron microscopy and found to be dominated by S. petersenii Korshikov. All affected sites were lakes of the Precambrian Shield (pH 5.7 – 7.5; alkalinity < 1 – 45 mg CaCO3/L). No evidence of obnoxious tastes or odours from other Synura species has been found.


2000 ◽  
Vol 37 (2-3) ◽  
pp. 165-181 ◽  
Author(s):  
A P Dickin

Ninety-eight new Nd-isotope analyses are presented for gneissic rocks from the Grenville Province. When combined with over 250 published Nd analyses and some unpublished analyses, these data can be used to establish a first-order crustal formation age map for most of the Grenville parautochthon and allochthonous polycyclic belt. In particular, the geographic extents of a juvenile Labradorian arc (Labradoria) and a juvenile 1.5 Ga arc (Quebecia) are defined, each with an area probably in excess of 100 000 km2. In addition, pre-1.75 Ga arcs are identified in Ontario (Barilia) and Labrador (Makkovikia). This work largely fills the last major gap in the continent-wide crustal formation age map of the Precambrian Shield of North America.


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