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Table 12. Forest floor organic matter and nutrient concentrations for contrasting forest types (*). The amount of organic matter stored in the forest floor shows a large decrease with decreasing latitude reflecting the effect of temperature on decomposition rates. Coniferous forests within a given climatic regime contain greater oranic matter concentrations primarily as a result of the poorer litter quality associated with conifer litter.
Forest Type | n | Organic Matter | N | P | Ca | Mg | P |
| kg/ha |
Boreal Coniferous | 3 | 113720 | 617 | 109 | 360 | 140 | 115 |
Boreal Deciduous | 1 | 68772 | 548 | 99 | 489 | 139 | 79 |
Temperate Coniferous | 13 | 74881 | 681 | 70 | 206 | 53 | 60 |
Temperate Deciduous | 14 | 21625 | 377 | 53 | 205 | 28 | 25 |
Mediterranean Deciduous | 1 | 11400 | 125 | 10 | 361 | 20 | 4 |
Tropical Rain Forest | 4 | 6460 | 91 | 12 | 96 | 15 | 5 |
(*) Data for boreal, temperate and Mediterranean forest are from Cole and Rapp (1981); tropical forest from Edwards and Grubb (1982).
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