Paleomagnetic measurements were conducted on discrete samples taken from advanced hydraulic piston corer (APC) and extended core barrel cores of Hole 1006A, part of the Bahamas Transect (Leg 166) of the Ocean Drilling Program (ODP). The Bahamas Transect consists of five ODP sites, moving from the basin (Site 1006) to the toe-of-slope (Site 1007) and up the lower slope (Sites 1003, 1004, and 1005) (Shipboard Scientific Party, 1997b). The purpose of the Hole 1006A paleomagnetic samples was to attempt to construct a magnetic reversal stratigraphy for sediments that comprise part of a deep-water current drift deposit. Shipboard measurements during Leg 166 (February-April 1996) were unable to determine a reversal stratigraphy for a number of reasons, including instrumentation problems, a possible radial overprint from the coring process, and the relatively weak nature of the magnetic remanence inherent in these types of sediments (see "Cautionary Note Regarding Cryogenic Magnetometer Data," in Shipboard Scientific Party, 1997a). We hoped that shore-based measurement of the discrete samples would overcome the instrument concerns and the severity of the suspected radial overprint remagnetization. To assess the nature of the magnetic remanence and determine if a reversal stratigraphy could be gleaned from the sediment record, we analyzed 778 discrete samples. The results are presented in this data report.