| 
 Reservoir  | 
 Be, kg  | 
 Be, kg/yr  | 
 Be concentration  | 
| 
 Mantle1  | 
 2 x 1017  | 
 
  | 
 
  | 
| 
 MORB source  | 
 
  | 
 
  | 
 0.02-0.03 ppm*  | 
| 
 Intraplate source  | 
 
  | 
 
  | 
 0.08-0.1 ppm*  | 
| 
 "Primitive mantle"  | 
 
  | 
 
  | 
 ~ 0.066 ppm*  | 
| 
 Oceans1  | 
 2.5 x 1011  | 
 
  | 
 0.2 pg/g (seawater)  | 
| 
 River inputs2  | 
 
  | 
 4 x 104  | 
 1.2 pg/g (river water)  | 
| 
 Aerosol inputs3  | 
 
  | 
 7-24 x 104 (?)  | 
 
  | 
| 
 Marine hydrothermal inputs4  | 
 
  | 
 1-5 x 104  | 
 0.1-0.4 ng/g (endmember vent fluids)  | 
| 
 Marine Sediments5  | 
 6 x 1014  | 
 
  | 
 1.5 ppm  | 
| 
 Continents1  | 
 3 x 1016  | 
 
  | 
 1.5 ppm  | 
| 
 Additions to ocean crust via MORB magmatism5  | 
 
  | 
 9.9 x 106  | 
 0.3 ppm (MORB)  | 
| 
 Sediment Subduction5  | 
 
  | 
 1.5 x 106  | 
 1.5 ppm (sediments)  | 
| 
 Additions to the continents via arc magmatism5  | 
 
  | 
 1.6 x 106  | 
 0.5 ppm (Arc basalts)  | 
*Inverse modeling results for MORB suites (Ryan and Langmuir 1988) and inferences from Be/Nd ratios.