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Below the upper peat layers, a 1 m-thick layer of white sand yielded two MSA lithic assemblages in association with faunal remains dated to between 30.8 ± 0.7 ka and >45 ka.
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The upper peat pool is where the model simulates heterotrophic respiration.
We model a slight annual C sink from the upper peat to the deep peat; however, these values are a major source of uncertainty.
The transfer of C from the upper peat to the deep peat layer is denoted in the model as the "Peat Carbon Accumulation" rate and is the mechanism for long-term C storage.
Similarly, the long-term peat accumulation rate, where a small proportion of C flows from the upper peat layer to the deep peat layer can be a sensitive variable for total ecosystem C over a long simulation period.
The South One consumed 80% of the above-ground living biomass (Fig. 9), and 50% of the upper peat layer.
Free convection takes place at the up side of the upper plate and forced convection below the upper plate.
2, 15, and 30 km, below the upper plate interface.
The acrotelm, or upper peat layer (0 40 cm depth), is periodically occupied by water, and has a higher yield, a higher permeability and a faster decomposition rate than the deep peat layer.
Saturated hydraulic conductivity (Ksat) of the lagg's upper peat layer resembles that of bog environments, but quickly reduces with depth, impeding vertical water flow.
Below ground stocks include: dead root, upper peat and deep peat.
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