Glacial and Interglacial Stratigraphy, Hudson Bay Lowland

1968 ◽  
Author(s):  
B C Mcdonald
Keyword(s):  
Hudson Bay ◽  
Hudson Bay Lowland

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

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

Silurian stratigraphy of the Hudson Bay Lowland in Quebec

1986 ◽  
Vol 23 (3) ◽  
pp. 288-299 ◽  
Author(s):  
Sven Y. Larsson ◽  
Colin W. Stearn
Keyword(s):  
Drainage Basin ◽  
Hudson Bay ◽  
Storm Events ◽  
Benthic Assemblages ◽  
Coral Fauna ◽  
Nodular Limestone ◽  
Shallow Subtidal ◽  
Hudson Bay Lowland

Carbonates of late Llandoverian to Ludlovian age, divided into the Severn River, Ekwan River, and Kenogami River formations, crop out in the drainage basin of the Harricana River. The Severn River Formation consists of a succession of alternating wackestone and packstone beds 17.5 m thick. The packstones are ascribed to storm events and carry a deeper water fauna than the wackestones. The Ekwan River Formation is divided into four units: a barren dolostone at the base, sandy wackestones and packstones with a coral fauna, another barren dolomudstone, and at the top a unit of argillaceous, nodular limestone rich in leperditid ostracods. The units are ascribed to shallow subtidal, intertidal, and supratidal environments. Three benthic assemblages, characterized by ostracods, corals, rhynchonellids, and the brachiopods Brachyprion and Dalejina, are distinguished in order of increasing depth. Two transgressive events in Llandoverian C4 and C6 times are marked by coral-rich units in the Severn River and Ekwan River formations.

A woolly mammoth (Proboscidea, Mammuthus primigenius) molar from the Hudson Bay Lowland of Manitoba

1988 ◽  
Vol 25 (6) ◽  
pp. 933-938 ◽  
Author(s):  
Erik Nielsen ◽  
C. S. Churcher ◽  
G. E. Lammers
Keyword(s):  
Depositional Environment ◽  
River Sediments ◽  
Hudson Bay ◽  
Tree Line ◽  
Mammuthus Primigenius ◽  
Early Form ◽  
Enamel Thickness ◽  
Hudson Bay Lowland ◽  
Woolly Mammoth

The first fossil mammal from the Hudson Bay Lowland of Manitoba, a molar from the woolly or Siberian mammoth, Mammuthus primigenius, is described from near Bird. A lophar index of 9.0 and an enamel thickness of 1.5–2.3 mm allow the tooth to be assigned to an early form of the species. Although in situ provenance of the molar is unknown, it is likely that the molar derives from Early Wisconsinan or Sangamon sediments that outcrop in the area. A boreal steppe or steppe–tundra environment is indicated by the presence of woolly mammoth, supporting a depositional environment north of the then tree line previously established for the Nelson River sediments.

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