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Which outcome results when subduction of oceanic crust halts?

A)Reduced mantle convection cell formation
B)Increased deep ocean water ventilation
C)Enhanced thermohaline ocean circulation
D)Decreased coastal upwelling intensity

💡 Explanation

Subduction cessation reduces pathways for cold crust to fuel mantle plumes, hence decreasing mantle convection cell formation because subduction drives cold material down, therefore the whole system slows with fewer plumes, rather than increasing ocean ventilation which needs active downwelling.

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