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Planktonic foraminifera are present both in bottom sediments and surface waters on the shelf area averaging 400 metres in depth to the west of a line between Cape MClure and Cape Meecham, but in M'Clure Strait proper to the east of this line in the surface waters only. The evidence is used to suggest a slow net eastward movement of water from the ocean through MClure Strait in the past with increased rates at the present time. RÉSUMÉ. La circulation des eaux de surface dans certaines parties dedoi:10.14430/arctic3161 fatcat:l46vseirajfcnaixix7j2vph7q