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Lab number
GSC-1199
Material dated
mammoth bone collagen; collagène osseux de mammouth
Taxa dated
mostly Mammuthus sp. (380 g, id. by C.S. Churcher)
Locality
right (south) bank of the Red Deer River, 590 m asl, 15 m above river level, 100 m below the general prairie level, just above the confluence with the South Saskatchewan River, southeastern Alberta
Map sheet
72 L/16
Submitter
A.M. Stalker
Date submitted
March 7, 0098
Normalized Age
14200 ± 1120
δ13C (per mil)
-19.4
Significance
palaeobiology, anomalous; paléobiologie, anormal
Context
CPR Pit, sand and gravel terrace, 2-4 m depth
Associated taxa
Mammalia: Mammuthus sp (see also GSC-1387)
Additional information
This date is anomalous in relation to glacial chronology, probably too young.
Comments
EfOm-VP, Empress: This Canadian Pacific Railway gravel pit contains abundant bones which were washed into place and thus were rounded, commonly damaged, and widely dispersed in coarse gravel. Stalker notes that the discrepancy between the two dates is unexplained, although GSC-1199 may have suffered contamination during collection by three persons; the sample was also soft, damp, and weathered, with modern rootlets that were removed during preparation. GSC-1387 appears more reliable, but both dates are substantially older than expected, and neither allows sufficient time for post-Classical Wisconsin incision of the large Red Deer valley. The possibility of the valley have been cut earlier must now be considered. In addition, the presence of a large, well developed fauna so close to the time of the Classical Wisconsin glaciation seems improbable. If GSC-1387 is correct, the fauna may have lived in a prolonged interval between two advances of Wisconsinan ice. Burns (1996: 110) takes a different view, suggesting that both dates are too young.

References