Peatlands Flashcards
Tropical peatlands
- 11% of total peatland area
- 56% in SE Asia
- One of the highest carbon densities of all ecosystems
- 20% of C from peatland soils
- 5-6% of global soil C
- High peat accumulation rates (6-13 mm yr-1)
- Been forming since 3,000 to 13,000 years before present
- Peat thickness > 20 m, average 5 m
Boreal peatlands
- One of the most studied wetland types
- Vast areas in temperate climates
- Mainly located in Canada, Northern Europe, and Russia
- Some in Argentina and New Zealand
Boreal peatlands
Unique biota
- Carnivorous plants
- Mosses dominate
- Sphagnum - the keystone species, environmental engineer
Boreal peatlands
Economic importance
- Agriculture (71% of German peatlands)
- Forestry
- Energy and heat (Fuel for heat and power)
- Horticultural substrate (Berry production, Sphagnum farming)
- Other uses (Whiskey, balneology)
Boreal peatlands
Successional patterns
•Paludufication
–Development of peat over previously less wet mineral ground
–Dominant process
•Terrestrialization (Infilling)
–Peat develops on the margins of lakes, ponds, or slow-flowing rivers
see slide 22-31
PEATLANDS - Fen VS Bogs
HYDROLOGY
FEN
Geogenous – other hydr. flows besides P
BOGS
Ombrogenous - “rain-fed”
PEATLANDS - Fen VS Bogs
BIOGEOCHEMISTRY
FEN
Minerotrophic - rich in nutrients, pH 4.3-7
BOGS
Ombrotrophic - poor in nutrients, acidic pH 3.8
PEATLANDS - Fen VS Bogs
VEGETATION
FEN
More diverse, grasses, sedges and brown mosses
BOGS
Ericaceous shrubs, woolgrass, Sphagnum