scholarly journals Geology, Keskarrah Bay area, District of Mackenzie, Northwest Territories

1988 ◽  
Author(s):  
J B Henderson
1981 ◽  
Vol 59 (12) ◽  
pp. 2360-2364 ◽  
Author(s):  
G. F. Rogers ◽  
J. C. Roff ◽  
D. H. Lynn

Tintinnids were numerically dominant in plankton samples collected from Chesterfield Inlet, Northwest Territories, in September 1978. Thirteen species were identified, 11 of which are new records for the Hudson Bay area. Tintinnopsis fimbriata and T. angusta were the most numerous tintinnids in the upper estuary at salinities below 24‰; their cell numbers were significantly positively correlated to temperature. Parafavella denticulata was the most abundant species in marine waters but it penetrated the estuary to salinities as low as 4‰. Cell numbers and volumes of P. denticulata were significantly positively correlated to salinity and negatively to chlorophyll; this species appeared to act as an almost conservative indicator of marine influence in this estuary. The distributions of the two Tintinnopsis species were not so readily explained, but maximum numbers of T. fimbriata and T. angusta corresponded to a phytoplankton maximum at station 29 in the middle estuary.


1999 ◽  
Author(s):  
S Hanmer ◽  
H A Sandeman ◽  
S Tella ◽  
J J Ryan ◽  
T Hadlari ◽  
...  

1985 ◽  
Vol 22 (4) ◽  
pp. 630-637 ◽  
Author(s):  
A. L. Washburn ◽  
Minze Stuiver

New radiocarbon dates from the University of Washington's Quaternary Isotope Laboratory are given for Cornwallis Island, Northwest Territories, Canada, and these and other radiocarbon dates for the area are assembled in a diagram, including the envelope of a tentative emergence curve. Most of the new dates are derived from surface collections but appear to represent a consistent altitude–age relationship confirming the pattern of previously published dates for the general region.The oldest of the new Holocene dates on marine shells indicate that the Resolute Bay area began emerging by at least 9700 years BP. The highest well developed marine strandlines recognized to date are at an altitude of ca. 105 m. However, the postglacial marine limit is probably some 10 m or more higher. As in adjacent regions, early postglacial emergence was initially rapid, of the order of an average 8.3 m/100 years for the first recorded 75 m, then slowed to an average 0.5 m/100 years for the last 40 m.


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