In January and May 1999, interface sediments were sampled within the Nazare
Canyon, a large submarine canyon that deeply indents the western Iberian c
ontinental margin (NE Atlantic) at around 39 degrees 35N. Excess Th-234 pro
files were established with high resolution to calculate inventories and bi
oturbation coefficients. A northern transect at 42 degreesN is briefly pres
ented as a reference for the Western Iberian margin. Synthesis of these: pa
rameters is used to examine short-term deposition within the Nazare Canyon.
Th-234(xs) was always detected with significant activities on surface in m
ost of the samples. Along the reference transect and in the adjacent area,
surface Th-234 excesses are about 10-20 dpm g(-1) . In contrast, Th-234(xs)
reaches very high levels (up to 170 dpm g(-1)) in the canyon. There is a l
arge range of variability in inventories and bioturbation rates, in relatio
n with depth and location. These results show a preferential deposition in
the canyon and focus in the upper and middle part of the canyon. On a month
ly time scale the Nazare Canyon appears as a significant locus of sedimenta
tion for the Western Iberian margin. (C) 2001 Elsevier Science B.V. All rig
hts reserved.