10Be contents of late Cenozoic sediments from Sites 720, 722, and 728 in the western Arabian Sea

Abstract

Differences in scavenging intensity and upwelling in the water column, must account for the variations in the initial 10Be input into the sediments from Holes 728A and 722A, whereas differences in sediment character and sedimentation rate can explain the variances between Holes 722A, 728A, and 720A. -from Authors