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. 2013 Sep 5;8(9):e73748. doi: 10.1371/journal.pone.0073748

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).