AUTHOR=Feldpausch Ted R. , Carvalho Lidiany , Macario Kita D. , Ascough Philippa L. , Flores César F. , Coronado Eurídice N. Honorio , Kalamandeen Michelle , Phillips Oliver L. , Staff Richard A. 

TITLE=Forest Fire History in Amazonia Inferred From Intensive Soil Charcoal Sampling and Radiocarbon Dating

JOURNAL=Frontiers in Forests and Global Change

VOLUME=Volume 5 - 2022

YEAR=2022

URL=https://www.frontiersin.org/journals/forests-and-global-change/articles/10.3389/ffgc.2022.815438

DOI=10.3389/ffgc.2022.815438

ISSN=2624-893X

ABSTRACT=Fire has a historical role in tropical forests related to past climate and ancient land use spanning the Holocene; however, it is unclear from charcoal records how fire varied at different spatiotemporal scales and what sampling strategies are required to determine fire history and their effects. We evaluated fire variation in structurally intact, terra-firme Amazon forests with no recent fire history, by intensive soil charcoal sampling from three replicate soil pits in sites in Guyana and northern and southern Peru. We used radiocarbon (14C) measurement to assess 1) locally, how the timing of fires represented in our sample varied across the surface of forest plots and with soil depth, 2) basin-wide, how the age of fires varies across climate and environmental gradients, and 3) how many samples are appropriate when applying the 14C approach to assess the date of last fire. Considering all 14C dates (n=33), the most recent fires occurred at a similar time at each of the three sites (median ages: 728-851 cal years BP), indicating that in terms of fire, these forests could be considered old-growth. The number of unique fire events ranged from 1 to 4 per pit and from 4 to 6 per site. Based upon our sampling strategy, the N-Peru site--with the highest annual precipitation--had the most fire events. Median fire return intervals varied 455-2950 cal yrs BP among sites. Based on available dates, at least three samples (1 from the top of each of 3 pits) is required if the sampling is to have a reasonable likelihood of capturing the most recent fire for forests with no history of a recent fire. The fire return interval for two of the sites was shorter than the time since the last fire, suggesting these forests have recently undergone a longer fire-free period, on average, than in the past. Our analysis from terra-firme forest soils helps to improve understanding of changes in fire regime, information necessary to evaluate post-fire legacies on modern vegetation and soil and to calibrate models to predict forest response to fire under climate change.