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Geochemical and micropaleontological analyses were carried out on a 35cm box core (CR06-TCE) spanning the last 6000years in the Esquiman Channel, a northeast arm of the Laurentian Channel in the Gulf of St. Lawrence. A 0.6%% decrease of δ 18 O in benthic foraminifer Globobulimina auriculata shells characterizes the upper 10cm of the core and suggests a warming of the bottom waters. This...
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