Decomposition
- carbon sink that mitigates global warming
Slow decomposition of mosses allows the mosses to contribute significantly
to the Arctic carbon sink. By photosynthesis, they "fix" carbon from the
atmosphere to organic compounds and by slow decomposition they help trap
the carbon instead quickly releasing them back to the atmosphere. It
is estimated that northern peatlands contain 120,000x106 tonnes
of carbon, equivalent to 24 years' emission from fossil fuels at the present
rate, and more than 50% of emissions since 1860, with half derived from
Sphagnum and a further component from other mosses. Annual carbon fixation
by slowly decomposing mosses in peatlands and boreal forests was estimated
as 6.5% of current emissions from fossil fuels. Therefore, mosses in the
Arctic region serves as a buffer for alleviating global warming.
Considering that the mosses in many regions of Alaska has already been disturbed
by urban development and oil exploitation, the value of mosses in ANWR arouses
much concern at the present.