Paleolimnology of the Maya Region /

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Paleolimnology of the Maya Region /
Brenner, Mark, 1952-
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Ihis allows tor the persistence in the basin of some Terminal Classic habitation, or use of the catchment by some of Yaxha's Postclassic inhabitants. In any case, the ^itegrated postcollapse population density at Sacnab accounts for only about 10% of the total integrated Maya period population oensity in the basin.
The rate of phosphorus accumulation on the lake floor attributable to human activity was calculateu by subtracting the baseline rate from the Maya zone rate. Assuming sediment accumu
...lation to be uniform over the basin bottom, the disturbance phosphorus accumulation rate was multiplied by the lake area and 2600 years of Maya time. This computation produced a figure equal to the entire oisturbance-generatea phosphorus load on the lake bottom. To calculate the number of person-years necessary to produce this phosphorus input, the load was expressed in kg and divided by the proposed per capita loading rate (0.5kg*person-year-l). ihis procedure was used to compute the number of riparian person-years necessary to generate the disturbance load at Sacnab and Macanche.

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