Modern data are clarifying tectonic transitions from continents to oceans. The importance of magmatic additions relative to mechanical extension varies between cases and through time based on observations of isolated margins and ridges. Magma poor spreading centers and magma rich continental margins are both well known. Here we present data to document the complete and continuous evolution from a magma rich Central Atlantic margin to a magma-starved ocean floor. Tectonic changes correlate with separation rate changes. Early Jurassic hotspot volcanism initially overwhelmed slow extension to build the Demerara Plateau at the eastern edge of the margin, but hotspot activity waned near the end of the Middle Jurassic. Normal spreading rates and normal thickness oceanic crust prevailed through most of the Oxfordian. Spreading slowed in the Kimmeridgian but magmatic addition slowed even more, evidenced by normal faults that offset the full oceanic crust and by outboard exhumed mantle.