Pre-Columbian Fire Management Linked to Refractory Black Carbon Emissions in the Amazon

Anthropogenic climate change—combined with increased human-caused ignitions—is leading to increased wildfire frequency, carbon dioxide emissions, and refractory black carbon (rBC) aerosol emissions. This is particularly evident in the Amazon rainforest, where fire activity has be...

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Main Authors: Monica M. Arienzo, S. Yoshi Maezumi, Nathan J. Chellman, Jose Iriarte
Format: Article
Language:English
Published: MDPI AG 2019-05-01
Series:Fire
Subjects:
Online Access:https://www.mdpi.com/2571-6255/2/2/31
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author Monica M. Arienzo
S. Yoshi Maezumi
Nathan J. Chellman
Jose Iriarte
author_facet Monica M. Arienzo
S. Yoshi Maezumi
Nathan J. Chellman
Jose Iriarte
author_sort Monica M. Arienzo
collection DOAJ
description Anthropogenic climate change—combined with increased human-caused ignitions—is leading to increased wildfire frequency, carbon dioxide emissions, and refractory black carbon (rBC) aerosol emissions. This is particularly evident in the Amazon rainforest, where fire activity has been complicated by the synchronicity of natural and anthropogenic drivers of ecological change, coupled with spatial and temporal heterogeneity in past and present land use. One approach to elucidating these factors is through long-term regional fire histories. Using a novel method for rBC determinations, we measured an approximately 3500-year sediment core record from Lake Caranã in the eastern Amazon for rBC influx, a proxy of biomass burning and fossil fuel combustion. Through comparisons with previously published records from Lake Caranã and regional evidence, we distinguished between local and regional rBC emission sources demonstrating increased local emissions of rBC from ~1250 to 500 calendar years before present (cal yr BP), coinciding with increased local-scale fire management during the apex of pre-Columbian activity. This was followed by a regional decline in biomass burning coincident with European contact, pre-Columbian population decline, and regional fire suppression associated with the rubber boom (1850−1910 CE), supporting the minimal influence of climate on regional burning at this time. During the past century, rBC influx has rapidly increased. Our results can serve to validate rBC modeling results, aiding with future predictions of rBC emissions and associated impacts to the climate system.
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spelling doaj.art-b996a8fc9aaf4f76b98052b9f7cc02582022-12-22T02:15:00ZengMDPI AGFire2571-62552019-05-01223110.3390/fire2020031fire2020031Pre-Columbian Fire Management Linked to Refractory Black Carbon Emissions in the AmazonMonica M. Arienzo0S. Yoshi Maezumi1Nathan J. Chellman2Jose Iriarte3Division of Hydrologic Sciences, Desert Research Institution, Reno, NV 89512, USADepartment of Geography and Geology, University of the West Indies Mona, Kingston, JamaicaDivision of Hydrologic Sciences, Desert Research Institution, Reno, NV 89512, USADepartment of Archaeology, University of Exeter, Exeter EX4 4QE, UKAnthropogenic climate change—combined with increased human-caused ignitions—is leading to increased wildfire frequency, carbon dioxide emissions, and refractory black carbon (rBC) aerosol emissions. This is particularly evident in the Amazon rainforest, where fire activity has been complicated by the synchronicity of natural and anthropogenic drivers of ecological change, coupled with spatial and temporal heterogeneity in past and present land use. One approach to elucidating these factors is through long-term regional fire histories. Using a novel method for rBC determinations, we measured an approximately 3500-year sediment core record from Lake Caranã in the eastern Amazon for rBC influx, a proxy of biomass burning and fossil fuel combustion. Through comparisons with previously published records from Lake Caranã and regional evidence, we distinguished between local and regional rBC emission sources demonstrating increased local emissions of rBC from ~1250 to 500 calendar years before present (cal yr BP), coinciding with increased local-scale fire management during the apex of pre-Columbian activity. This was followed by a regional decline in biomass burning coincident with European contact, pre-Columbian population decline, and regional fire suppression associated with the rubber boom (1850−1910 CE), supporting the minimal influence of climate on regional burning at this time. During the past century, rBC influx has rapidly increased. Our results can serve to validate rBC modeling results, aiding with future predictions of rBC emissions and associated impacts to the climate system.https://www.mdpi.com/2571-6255/2/2/31black carbonmacrocharcoaleastern Amazonpre-Columbianfire activity
spellingShingle Monica M. Arienzo
S. Yoshi Maezumi
Nathan J. Chellman
Jose Iriarte
Pre-Columbian Fire Management Linked to Refractory Black Carbon Emissions in the Amazon
Fire
black carbon
macrocharcoal
eastern Amazon
pre-Columbian
fire activity
title Pre-Columbian Fire Management Linked to Refractory Black Carbon Emissions in the Amazon
title_full Pre-Columbian Fire Management Linked to Refractory Black Carbon Emissions in the Amazon
title_fullStr Pre-Columbian Fire Management Linked to Refractory Black Carbon Emissions in the Amazon
title_full_unstemmed Pre-Columbian Fire Management Linked to Refractory Black Carbon Emissions in the Amazon
title_short Pre-Columbian Fire Management Linked to Refractory Black Carbon Emissions in the Amazon
title_sort pre columbian fire management linked to refractory black carbon emissions in the amazon
topic black carbon
macrocharcoal
eastern Amazon
pre-Columbian
fire activity
url https://www.mdpi.com/2571-6255/2/2/31
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AT nathanjchellman precolumbianfiremanagementlinkedtorefractoryblackcarbonemissionsintheamazon
AT joseiriarte precolumbianfiremanagementlinkedtorefractoryblackcarbonemissionsintheamazon