Syn-pandemic Fire Suppression in the Tropical Americas During European Conquest

A new reconstruction of the biomass burning history of the tropical Americas during the past 5 millennia documents the expansion of fire use by Mesoamerican and Amazonian agriculturalists and a subsequent period of fire suppression beginning ~500 years BP. Fire suppression is synchronous with the collapse of the American indigenous population during European conquest. The present work synthesizes microscopic charcoal accumulation records preserved in lake, bog, and basin sediments from 14 sites in Central America and equatorial South America to reconstruct regional variation in charcoal accumulation rates, averaged over 200-year increments, relative to the mean rate of regional charcoal accumulation during the past 5 millennia. This study builds upon prior fire history reconstructions by synthesizing a substantially greater number of stratigraphic charcoal accumulation sequences to resolve features of the Late Holocene biomass burning record in the tropical Americas. We find that between ~5000 and ~4000 years BP, charcoal accumulation generally persisted at rates >1 standard deviation (s.d.) below the 5-millennium mean. Subsequently charcoal accumulation rates fluctuated until ~3000 years BP and then increased, maintaining an average level >0.5 s.d. above the 5-millenium mean until ~500 years BP. After ~500 years BP, charcoal accumulation rates dropped to values below the 5000-year mean and remained suppressed for the next several centuries. The variation in charcoal accumulation rates over the past 5000 years reflects both climatic and anthropogenic factors affecting the regional fire history of the tropical Americas. The transition to above-average charcoal accumulation rates after 3000 years BP is synchronous with a trend toward a drier climate in the circum-Caribbean region and expanding forest clearance and cultivation by Mesoamerican and Amazonian societies. The subsequent, prolonged period of enhanced biomass burning between ~3000 and ~500 years BP is punctuated by three intervals of low charcoal accumulation, reflecting intermittent episodes of fire-suppression lasting <200 years. The latest and most pronounced of these low-fire intervals occurs at ~1100 years BP and corresponds to the Classic Maya collapse. The persistence of low charcoal accumulation rates for several centuries after ~500 years BP is parsimoniously explained by a reduction of agriculture-related biomass burning due to syn-pandemic population collapse. During European conquest, pandemics killed ~90% of the indigenous American population, estimated to represent ~20% of the 16^{th} century global population. The suppression of biomass burning after ~500 years BP is a unique feature of the fire history of Central and equatorial South America relative to other regions of the globe, where rates of charcoal accumulation are typically >0.2 s.d. above their Holocene mean values. Syn-pandemic fire suppression in the tropical Americas is associated with massive regional reforestation and sequestration of carbon into the terrestrial biosphere, which contributed to the ~2% global reduction in atmospheric CO2 levels and the 0.1 per mil increase in δ13C of atmospheric CO2 from 1500 to 1700 A.D.