Succession in the Hudson Bay Lowland, Northern Ontario, Canada

1996 ◽  
Vol 28 (2) ◽  
pp. 172 ◽  
Author(s):  
Lee F. Klinger ◽  
Susan K. Short
Keyword(s):  
Hudson Bay ◽  
Northern Ontario ◽  
Hudson Bay Lowland

scholarly journals Additions to the Vascular Flora of Ontario, Canada, from the Sutton Ridges, Hudson Bay Lowland Ecoregion

2011 ◽  
Vol 125 (3) ◽  
pp. 241 ◽  
Author(s):  
Michael J. Oldham ◽  
Samuel R. Brinker
Keyword(s):  
North America ◽  
Plant Species ◽  
Vascular Plant ◽  
Field Studies ◽  
Hudson Bay ◽  
Northern Ontario ◽  
Vascular Flora ◽  
Arctic Plants ◽  
Diapensia Lapponica ◽  
Hudson Bay Lowland

Field studies in the Hudson Bay Lowland ecoregion of northern Ontario during 2010 resulted in the discovery of four native vascular plant species not previously confirmed from the province: Arctic Bellflower (Campanula uniflora; Campanulaceae), Lapland Diapensia (Diapensia lapponica; Diapensiaceae), Alpine Azalea (Kalmia procumbens; Ericaceae), and Alpine Brook Saxifrage (Saxifraga rivularis; Saxifragaceae). These four species are widespread arctic plants occurring in both North America and Eurasia and were found on the Sutton Ridges, a Precambrian bedrock inlier surrounded by the extensive wetlands of the Hudson Bay Lowland.

scholarly journals Amino Acid Evidence Indicating Two or More Ages of Pre-Holocene Nonglacial Deposits In Hudson Bay Lowland, Northern Ontario

2007 ◽  
Vol 44 (3) ◽  
pp. 389-393 ◽  
Author(s):  
Philip H. Wyatt
Keyword(s):  
Amino Acid ◽  
Marine Sediments ◽  
Organic Material ◽  
Hudson Bay ◽  
Last Interglacial ◽  
Northern Ontario ◽  
Glacial Sediments ◽  
Hudson Bay Lowland

ABSTRACT Amino acid studies have identified pre-Holocene non-glacial sediments in the Hudson Lowland which are significantly younger than Bell Sea sediments of the Missinaibi Formation. This younger unit is represented by marine sediments on the Severn and Abitibi rivers. Buried organic material on Beaver River is correlated with the younger Severn and Abitibi river marine sediments based on amino acid evidence. Assuming that Bell Sea sediments are of last interglacial (130-120 ka) age, the younger nonglacial sediments may have been deposited late in 18O stage 5 (80-75 ka). Paleoecologic studies of the Beaver River organics indicate climate at least as warm as present.

MACROFOSSIL AND BIOMARKER RECORD FROM HUDSON BAY LOWLAND SOUTH RIDGE HOLLOW BOG, NORTHEAST ONTARIO

2016 ◽  
Author(s):  
Rebecca Snyder ◽  
◽  
Dorothy Peteet ◽  
Jonathan Nichols ◽  
Sarah Finkelstein ◽  
...  
Keyword(s):  
Hudson Bay ◽  
Hudson Bay Lowland

Analysis of Multi-Temporal ERS-1 SAR Data of Subarctic Tundra and Forest in the Northern Hudson Bay Lowland and Implications for Climate Studies

1999 ◽  
Vol 25 (1) ◽  
pp. 21-33 ◽  
Author(s):  
C.K. Duguay ◽  
W.R. Rouse ◽  
P.M. Lafleur ◽  
L.D. Boudreau ◽  
Y. Crevier ◽  
...  
Keyword(s):  
Hudson Bay ◽  
Multi Temporal ◽  
Hudson Bay Lowland ◽  
Sar Data ◽  
Climate Studies
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