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Which consequence results when thermocline depth increases during upwelling?

A)Nutrient flux to surface declines
B)Surface salinity temporarily decreases
C)Plankton growth rates rapidly increase
D)Deep-water oxygen levels rise fastest

💡 Explanation

Reduced thermocline disruption limits nutrient replacement because density stratification inhibits convective overturn; this 'nutrient-pump' upwelling efficiency declines; therefore less nutrient transfer; rather than the plankton benefitting or the salinity decreasing in this thermal/depth increase situation.

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