Synthetic magnetic anomaly profile computed using Modmag(R1W) with the following input model parameters; top of magnetic source layer is 6.0 km, bottom of magnetic source layer is 6.5 km, remanent inclination = -81.2°, and remanent declination = 0.0°. Magnetic anomaly identifications were made using new high quality magnetic data in the Bruce Rise area (90°-115°E) collected by Russian Antarctic Expeditions 49 and 50 in 2004-2005. The total magnetic field was recorded in these surveys by a differential magnetometer to 0.01 nT accuracy. New magnetic anomaly identifications were also made for data collected during Geoscience Australia cruises 228 and 229 (S3-S6). Our new identifications were integrated with earlier identifications of Tikku and Cande (R6. References R1. Mendel V., M. Munschy, D. Sauter, Computers & Geosciences 31, 589 (2005). R2. O'Brien P., S. Stanley, R. Parums, in Antarctica: Contributions to Global Earth Sciences D. K. Fütterer, D. Damaske, G. Kleinschmidt, H. Miller, F. Tessensohn, Eds. (Springer-Verlag, Berlin, 2006) pp. 341-347. R3. H. M. J. Stagg et al., “Geological framework of the continental margin in the region of the Australian Antarctic Territory” (Geoscience Australia Record 2005). R4. J. B. Colwell, H. M. J. Stagg, N. G. Direen, G. Bernardel, I. Borissova, in Antarctica: Contributions to Global Earth Sciences D. K. Fütterer, D. Damaske, G. Kleinschmidt, H. Miller, F. Tessensohn, Eds. (Springer-Verlag, Berlin, 2006) pp. 327-340. R5. D. I. Close, H. M. J. Stagg, P. E. O'Brien, Marine Geology 239, 33 (2007). R6. Tikku A. A., S. C. Cande, Journal of Geophysical Research 104, 661 (1999).