Table 8. Estimated annual Corg stocks in soils of different ecosystems.
Ecosystem | Soil/sediment Carbon Accumulation rate |
(g C m−2 y−1) | |
Tropical Forests | 2.3–2.5 |
Temp Forests | 1.4–12 |
Boreal Forests | 0.8–2.2 |
Temp grassland | 2.2 |
Temperate desert | 0.8 |
Tundra | 0.2–0.7 |
Posidonia oceanica | 6–175 |
Australian seagrasses | 1.0–66.5 * |
Soil/sediment Carbon Stock | |
(g C m−2) | |
Tropical montane | 6100 |
Tropical wet | 6100 |
Tropical moist | 5000 |
Tropical dry | 2200 |
Warm Temperate moist | 7600 |
Warm temperate dry | 2600 |
Cool temperate moist | 11600 |
Cool temperate dry | 4900 |
Boreal | 14900 |
Polar | 11800 |
Australian seagrasses | 1090 – 20140# |
P. oceanica | 10500–40000∧ |
Data from [67] except Australian seagrasses (this study) and P. oceanica (based on the range reported [5], [7], [42], [47].
∧Value assume sediment depth of 1 m, which is a conservative estimate for the higher values which are for Posidonia ecosystems with reported organic sediment depths of >2.5 m ([23] and Pers. Obs. for Oyster Harbour and Waychinicup Inlet in SW Australia; P. oceanica references as above).