Variations in terrigenous input into the deep equatorial atlantic during the past 24,000 years.
Francois R, Bacon M P·Science (New York, N.Y.)
Estimates of terrigenous fluxes at three different water depths at two sites in the equatorial Atlantic by normalization against excess (230)Th flux indicate that the flux of terrigenous material to the seafloor was significantly higher during the last glacial period than it is today. Fluxes started to decrease during…