Figure F6. Bio-Ba mass accumulation rate as a function of paleolatitude for (A) Site 1218 and (B) Site 1219. Note the high Bio-Ba flux at the paleoequator and the anomalous accumulation at 40 Ma, corresponding to carbonate accumulation event 3 (CAE-3).

Figure F6. Bio-Ba mass accumulation rate as a function of paleolatitude for (A) Site 1218 and (B) Site 1219. Note the high Bio-Ba flux at the paleoequator and the anomalous accumulation at 40 Ma, corresponding to carbonate accumulation event 3 (CAE-3).