| Popis: |
This thesis utilizes high resolution charcoal analysis and charcoal morphology to reconstruct fire history for Prince Rupert Harbour (PRH), British Columbia between ~13,200 and 3500 cal BP. Home to the North Coast Tsimshian, PRH is an ideal study location for evaluating demographic and related environmental patterns for its extensive and well-studied archaeological record yet it lacks local paleoenvironmental data. I use this fire history to: produce one line of localized palaeoecological data, assess variation in charcoal accumulation rates (CHAR) compared against regional and semi-local paleoclimate records, determine whether or not the presence of an anthropogenic signal exists in the charcoal record, and test the relationship between natural charcoal accumulation rates and demographic models for the PRH region between 6000 and 3500 cal BP. Results indicate that fire frequency and intensity were low with just fourteen potential fire events in the DIL CHAR record, 9 in Zone 2 (13,200-6000 cal BP) and 4 in Zone 1 (6000-3500 cal BP). Zone 2 peaks could not be confidently separated from the background signal and are interpreted with caution. Peaks charcoal morphology in Zone 1 in suggest local, low intensity fires. The data suggests that no extreme fluctuation in climate as seen through fire regime occurred over the 11,000-year record, and while there is no correlation between demography and CHAR such that an anthropogenic driver could be posited, the only fire events confidently identified occurred after the earliest known villages formed. I suggest that additional fire histories capturing the past 3500 years when PRH saw significant demographic growth will be necessary and fruitful for understanding the human impact, if any, on the fire regime of the Prince Rupert Harbour region. |
