Warmer atmospheric temperatures warm the soil and increase microbial and
chemical processes therein. Bellamy et al. (2005) studied changes in soil
carbon in England and Wales between 1978 and 2003 for over 6,000 locations and
found that all soils sampled are losing carbon, most likely due to global
warming. Their research has four major implications (Schulze and Freibauer,
2005):
Bellamy et al. (2005) calculated a mean rate of loss of soil carbon to be 0.6% per year. This represents about 13 million metric tonnes of carbon per year which is equivalent to 8% of the UK annual carbon dioxide emissions.
References
Bellamy, P. H., and Co-authors, 2005: Carbon losses from all soils across
England and Wales 1978-2003. Nature, 437, 245-248.
Schulze, E. D., and A. Freibauer, 2005: Carbon unlocked from soils.
Nature, 437, 205-206.