Montane forest root growth and soil
organic layer depth as potential factors stabilizing Cenozoic global change (pages 983 — 990)
Montane forest root growth and soil
organic layer depth as potential factors stabilizing Cenozoic global change (pages 983 — 990) Christopher E. Doughty, Lyla L. Taylor, Cecile A. J. Girardin, Yadvinder Malhi and David J. Beerling
Not exact matches
According to her, the research included four of the five functionally distinct carbon pools whose study is recommended by the United Nations (UN) Intergovernmental Panel on Climate Change (IPCC): aboveground biomass (live plants), dead
organic matter, leaf litter (
layer that contains a combination of fragments of leaves, branches and other decomposing
organic matter) and soil (up to 30 centimeters (cm) in
depth).