Not exact matches
They
store carbon
in soil and biomass which has massive implications for climate
change, but they also hold back and release various
nutrients which have effects on natural areas as well as agricultural yield.
As shown
in part «b»
in Wieder et al.'s figure, the terrestrial carbon
store over the 21st Century
changes from a net sink of 125 GtC to a net source of 156 GtC once
nutrient constraints are imposed.
Other effects like temperature - dependent CO2 solubility
in ocean water, carbon
stored in the land biosphere, weathering rates, and ocean
nutrient inventories may help explain the rest of glacial − interglacial
changes in atmospheric pCO2 (26, 27).