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dc.contributor.authorMaezumi, Y
dc.contributor.authorWhitney, B
dc.contributor.authorMayle, F
dc.contributor.authorGregorio de Souza, J
dc.contributor.authorIriarte, J
dc.date.accessioned2017-12-18T10:09:12Z
dc.date.issued2017-12-14
dc.description.abstractA 50,000-year-old sediment core record from Laguna Chaplin is reanalyzed to explore potential paleoecological methods to detect the extent of pre-Columbian disturbance in the Bolivian Amazon. High-resolution (sub-centennial) macrocharcoal data are analyzed using statistical algorithm software including Regime Shift Detection and CHAR Analysis to detect changes in past fire regimes. These data are compared with existing charcoal records from throughout the Bolivian lowlands to provide a regional scale context of past biomass burning. During the mid-Holocene, changes in precipitation are the dominant driver of fire activity and biomass burning at Laguna Chaplin and across the Bolivian lowlands. During the late Holocene, increased fire activity across ecosystems ranging from fire-adapted to fire-intolerant forests is attributed to the apex of pre-Columbian activity. These data suggest human-caused ignitions during the late Holocene are the driving factor of regional scale fire activity in the Bolivian lowlands. After ca. 650 cal yr BP, there is an increase in biomass burning and fire frequency synchronous with the expansion of Moraceae/Urticaceae pollen (>50%) at Laguna Chaplin. This occurs during the time-transgressive southward expansion of the rainforest boundary, during the apex of pre-Columbian activity in the region. The increase in biomass burning at Laguna Chaplin is reflected at other sites in the region with known human occupation histories. The presence of Zea mays ca. 970 to 170 cal yr BP indicates maize cultivation is practiced in the immediate vicinity surrounding Laguna Chaplin. The simultaneous increase in fire activity with the expansion of the less flammable humid rainforest vegetation suggests human fire management practices. These data are interpreted as the use of frequent, low severity, human-caused fires to clear the croplands from encroaching rainforest vegetation. Despite evidence of pre-Columbian fire management during the late Holocene, vegetation and fire data indicate the extent of human-landscape modification and fire management at Laguna Chaplin, is not enough to inhibit the climate-driven regional forest expansion of the savanna-rainforest ecotonal boundary to its most southern extent in the last 50,000 years. This study demonstrates the utility of applying a multi-proxy, high-resolution paleoecological method to disentangle climate and pre-Columbian disturbance in the Bolivian Amazon.en_GB
dc.description.sponsorshipFunding for research is supported in part by the ERC-PAST (Pre-Columbian Amazon-Scale Transformations) European Research Council (616179) awarded to JI. We thank Jonas Gregorio de Souza for the regional map. Special thanks to Tom Thompson and Chase Adams for their editorial assistance and to the anonymous reviewers for their comments and suggestions. Funding for FM to core Laguna Chaplin in 1998 is provided by a Royal Society Research Grant and a Royal Society Study Visit grant. We thank Tim Killeen and the Museo de Historia Natural “Noel Kempff Mercado”, Santa Cruz, Bolivia, for providing logistical support, and in particular Lupita Sanchez and local guides (e.g., Juan Surubi) from the village of Florida for assistance with coring the site.en_GB
dc.identifier.citationVol. 3, pp. 1 - 14en_GB
dc.identifier.doi10.1016/j.quaint.2017.11.053
dc.identifier.urihttp://hdl.handle.net/10871/30708
dc.language.isoenen_GB
dc.publisherElsevieren_GB
dc.rights.embargoreasonPublisher's policy.en_GB
dc.rights© 2017 Elsevier Ltd and INQUA. All rights reserved.en_GB
dc.subjectPaleofireen_GB
dc.subjectCharcoalen_GB
dc.subjectPre-Columbianen_GB
dc.subjectFire managementen_GB
dc.subjectMaize cultivationen_GB
dc.subjectBolivian Amazonen_GB
dc.titleReassessing climate and pre-Columbian drivers of paleofire activity in the Bolivian Amazonen_GB
dc.typeArticleen_GB
dc.identifier.issn1040-6182
dc.descriptionThis is the author accepted manuscript. The final version is available from Elsevier via the DOI in this record.en_GB
dc.identifier.journalQuaternary Internationalen_GB


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