Nitrate δ15N and δ18O profiles were measured across the North Atlantic.
Partial assimilation in the Southern Ocean raises the δ15N of intermediate waters.
Sinking N in the low latitudes lowers intermediate depth δ18O but not δ15N.
Lowest δ15N in western thermocline does not require greater N fixation in west.
δ15N difference between northward and southward flows as a measure of N fixation.