Table 3.
Revised biome C inventories if the root C pool (CR) of each biome is increased according to assumption (ii) and table 2, from those in table 1.
| biome | plant C (Pg) | ||||||
|---|---|---|---|---|---|---|---|
| above | below | total | soil Ca (Pg) | biome C (Pg) | C sinkb (Pg yr−1) | C sink increasec (%) | |
| CA | CR | CV | CS | CB | S | ||
| tropical forest | 266 | 123 | 389 | 214 | 602 | 0.72 | 9 |
| temperate forest | 109 | 49 | 159 | 153 | 312 | 0.37 | 7 |
| Boreal forest | 42 | 25 | 67 | 338 | 405 | 0.49 | 3 |
| Mediterranean shrubland | 8 | 14 | 22 | 71 | 94 | 0.11 | 6 |
| tropical savanna and grassland | 55 | 39 | 94 | 247 | 342 | 0.41 | 5 |
| temperate grassland | 2 | 6 | 8 | 176 | 185 | 0.22 | 1 |
| deserts | 5 | 8 | 13 | 159 | 172 | 0.21 | 2 |
| tundra | 1 | 2 | 3 | 115 | 118 | 0.14 | 1 |
| crops | 4 | 1 | 4 | 11 | 15 | 0.02 | 2 |
| total | 492 | 268 | 759 | 1485 | 2244 | 2.69 | 5 |
Soil C is calculated for a depth of 1 m (Saugier et al. 2001), see table 1.
Increases in the C sink are expressed as percentages of those in table 1.