Oxygen Isotope Studies on Sea Ice in the Gulf of St. Lawrence

The fractionation of oxygen isotopes between sea ice and sea water in samples collected from the Gulf of St. Lawrence indicated that sea ice is enriched in its O 18 :O 16 ratio with respect to coexisting sea water. Sources of sea ice in the Gulf of St. Lawrence may be identified on the basis of O 18...

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Bibliographic Details
Published in:Journal of the Fisheries Research Board of Canada
Main Authors: Tan, F. C., Fraser, W. D.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1976
Subjects:
Online Access:http://dx.doi.org/10.1139/f76-182
http://www.nrcresearchpress.com/doi/pdf/10.1139/f76-182
Description
Summary:The fractionation of oxygen isotopes between sea ice and sea water in samples collected from the Gulf of St. Lawrence indicated that sea ice is enriched in its O 18 :O 16 ratio with respect to coexisting sea water. Sources of sea ice in the Gulf of St. Lawrence may be identified on the basis of O 18 :O 16 measurements.