A partial skeleton of an adult male walrus (Odobenus rosmarus) was exc
avated from a raised beach on the Labrador coast, near the present com
munity of Forteau. Bone collagen from the specimen has been radiocarbo
n dated at about 11 500 yr BP. Fossil pollen, dinoflagellates, diatoms
, sponges, echinoderms, barnacles, foraminifers and ostracodes from sa
ndy clay surrounding the specimen are considered in terms of their pal
eoenvironmental implications. Presuming the bone date is correct, paly
nological and molluscan data suggest that the walrus skeleton was rewo
rked and redeposited by a receding sea some 10 300 to 10 400 years ago
, when sparse tundra vegetation evidently bordered on a glaciomarine e
nvironment.