The net inputs of silicic acid (dissolved silica) to the world ocean h
ave been revised to 6.1 +/- 2.0 teramoles of silicon per year (1 teram
ole = 10(12) moles). The major contibution (about 80 percent) comes fr
om rivers, whose world average silicic acid concentration is 150 micro
molar, These inputs are reasonably balanced by the net ouputs of bioge
nic silica of 7.1 +/- 1.8 teramoles of silicon per year in modern mari
ne sediments, The gross production of biogenic silica (the transformat
ion of dissolved silicate to particulate skeletal material) in surface
waters was estimated to be 240 +/- 40 teramoles of silicon per year,
and the preservation ratio (opal accumulation in sediment/gross produc
tion in surface waters) averages 3 percent. In the world ocean the res
idence time of silicon, relative to total biological uptake in surface
waters, is about 400 years.