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What Is This Indicator, and Why Is It Important?
This indicator will report the total amount of carbon stored
in soil and plants in grasslands and shrublands.
Carbon storage has become an important issue in international
negotiations on the management of greenhouse gas emissions,
because increased carbon storage can be useful in offsetting
emissions of carbon from fossil fuel burning and other sources.
The amount of carbon stored in grasslands and shrublands generally
changes very slowly. It may be affected by changes in fire
frequency, changes in grazing intensity, by the introduction
of non-native species, or by conversion of these lands to
other uses (like agriculture). In grasslands (including alpine
and arctic tundra), more than two-thirds of all carbon is
stored in the soil. This contrasts with forests, where significant
amounts of carbon are stored in trees (see Forest
Carbon Storage). Some grassland and shrubland soils normally
have low levels of stored carbon; however, at least globally,
they are thought to store about half as much carbon as is
stored by forests and as much as is stored in croplands.
Carbon in soilin the form of organic matter, or partially
decayed plant and animal matterhelps the soil hold water
and supply nutrients to plants; it also protects against erosion
and helps support a healthy and diverse set of microscopic
plants and animals. Soil carbon is indicative of soil fertility,
and some grassland soils are among the most fertile on earth.
Further, soil organic matter also stores nitrogen for hundreds
and even thousands of years. This helps limit the effect of
increasing atmospheric nitrogen deposition, by ensuring that
nitrogen does not leach into groundwater (see Nitrate
in Groundwater).
See also Farmlands Soil
Organic Matter.
Why Can't This Indicator Be Reported at This Time?
There are baseline estimates of soil carbon, but
there is no mechanism for regular monitoring of and reporting
on carbon storage.
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