Computed axial tomography (CAT-scan) gives a pseudo-3D representation
of sedimentary cores. Sediments may be described and numerically proce
ssed from digitized high resolution images. A 150 m long borehole was
drilled and sampled at Ile-aux-Coudres, middle estuary of the St. Lawr
ence, Quebec, and analysed by a tomodensitometer (CAT-scanner). This b
orehole represents mainly the Illinoian-Sangamonian transition series
(isotopic stage 5e, 130-80 kyr B.P.) of a post-glacial glacioisostatic
marine invasion and the subsequent regressive prodelta. Four represen
tative samples, 900 mm long, were chosen for analysis from a transitio
n zone between glacial and prodeltaic sediments. They have been descri
bed from tomographic longitudinal and transversal sections, from CT nu
mber series, and also from classical analysis such as grain size, orga
nic matter and carbonates. CT numbers reflect sedimentary characterist
ics and are closely linked to grain size and to organic matter. Carbon
ates are only weakly correlated, probably because of its low concentra
tion. Bed thickness and numerical processing of CT number series are u
sed to characterize lamina, and allow for depicting sub-annual, annual
and longer periodicities. Clay facies, fine and thick rhythmites, and
isolated diamicton beds were identified. From bottom to top, the firs
t sample contains homogeneous clay rhythmites, typical of a distal env
ironment; the second is composed of diamictons and thin, alternating l
ight-dark annual lamina sets; in the third sample, annual light-dark r
hythmites are slightly thicker and display subtle semi-annual cyclicit
ies; in the fourth sample, annual rhythmites are several centimetres i
n thickness and contain preserved sub-annual events, of possible seaso
nal cyclicity. This succession of facies and associated stratal period
icities may be typical of transgressive sedimentation in a basin such
as the St. Lawrence estuary during the transition from glacial to non-
glacial conditions.