Figure F2. Age-depth curve for Hole 1082A. The paleomagnetic "model 1" (Shipboard Scientific Party, 1998) and two calcareous nannofossil datums (n1 = FO of Emiliania huxleyi; n2 = LO of Pseudoemiliania lacunosa) (Shipboard Scientific Party, 1998) are used. Geomagnetic polarity time scale (GPTS) after Cande and Kent (1995) and Berggren et al. (1995). Numbers (1-21) indicate radiolarian events (see Table T2).