Drill sites recovered from the South Atlantic by the Deep Sea Drilling Proj
ect provide excellent magnetostratigraphies for the time-interval of polari
ty chrons C33r through C28n (83-62.5 Ma: Cande & Kent time-scale). Cyclic p
atterns of carbonate sedimentation, with a mean repeat time of ca. 20 ka, c
an be correlated between sites. The cycles show the full hierarchy of eccen
tricity amplitude modulations that would be expected of precessional orbita
l forcing. A significant modulation component exists at ca. 400 ka, which i
n all likelihood matches the modern 404 ka repeat time for eccentricity. Th
is modulation pattern may provide the 'tuning fork' for tying cyclical sedi
mentation to the most stable astronomical eccentricity period. A ca. 2.5 Ma
modulation also emerges that seems surprisingly similar to the modern long
-wavelength eccentricity modulation of precessional amplitude, which should
average 2.425 Ma. Results of 'cyclochronology' of polarity chrons C29n-C31
n suggest that the Cande & Kent time-scale will need to be revised to allow
for a more gentle change in South Atlantic sea-floor spreading than modell
ed by those authors.