Hemipelagic, sediment drift deposits have been discovered and mapped on the
Antarctic Peninsula shelf in 300-500 m water depth. The drift located adja
cent to Andvord Bay covers 44.5 km(2) and exhibits continuous and discontin
uous parallel reflections that conform to peaks and valleys in the acoustic
basement as observed in deep-tow boomer and sparker seismic records. This
style of drift deposit is a common feature of deep oceanic sediments, but i
s not normally found in continental shelf environments. Measured sedimentat
ion rates of 1-3 mm/yr on the Andvord drift indicate that the total 40 m dr
ift thickness observed in the seismic records is probably postglacial. The
drift contrasts with the basin-fill style of sedimentation that is normally
associated with the Antarctic continental shelf and may play an important
role in the carbon cycle. On the basis of an isopach map of drift sediments
and previously published core information, the rate of carbon accumulation
in the Andvord drift is estimated to be about 1.7 g/cm(2)/k.y., which is c
omparable to the highest rates reported for the southwestern Ross Sea.