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Peat is an accumulation of partially decayed vegetation or organic matter. ... clear-cutting for horticultural peat (of which Sweden is an important producer in ...
Peat formation is a natural carbon sink; because the decomposition of the organic matter is slower than its production rate, the surplus accumulates as peat. Their stability has important implications for climate change; they are among the largest near-surface reserves of terrestrial organic carbon. [2]
Peat soils store over 600 Gt of carbon, more than the carbon stored in all other vegetation types, including forests. This substantial carbon storage represents about 30% of the world's soil carbon, underscoring their critical importance in the global carbon cycle. [5]
Tropical peat is a type of histosol that is found in tropical latitudes, including South East Asia, Africa, and Central and South America. [2] Tropical peat mostly consists of dead organic matter from trees instead of spaghnum which are commonly found in temperate peat. [ 3 ]
Peatland as an ecosystem is important for regulating soil quality. When the peat covering Sphagnum layer is degraded, the remaining bare peat soil releases sediment to water streams, which pollutes and reduces biodiversity of rivers and water reservoirs. [20] Additionally trough wind and water erosion carbon can be released if the peat is blank ...
A fen is a type of peat-accumulating wetland fed by mineral-rich ground or surface water. [1] [2] It is one of the main types of wetland along with marshes, swamps, and bogs. Bogs and fens, both peat-forming ecosystems, are also known as mires. [2] The unique water chemistry of fens is a result of the ground or surface water input.
Peat has been Ireland's staple fuel for centuries and as of 2005 it provided about 9% of the country's energy needs. [13] Peatlands cover approximately 17% of the area of Ireland, [14] and Bord na Móna (the "Peat Board") is a semi-state company charged with the mechanised harvesting of peat – extracting more than 4 million tonnes in 2014. [15]
Other species specialized in re-settling land which had been briefly deforested by flooding: Synchysidendron and Lepidodendron in mineral-soil areas and Lepidophloios in peat areas. Cordaites may have favored drier areas of the swamp. In the later part of this period tree ferns tended to take over from lycopsid trees.
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