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Legacies of Indigenous land use and cultural burning in the Bolivian Amazon rainforest ecotone

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posted on 2025-08-01, 14:03 authored by SY Maezumi, S Elliott, M Robinson, CJ Betancourt, J Gregorio de Souza, D Alves, M Grosvenor, L Hilbert, DH Urrego, WD Gosling, J Iriarte
The southwestern Amazon Rainforest Ecotone (ARE) is the transitional landscape between the tropical forest and seasonally flooded savannahs of the Bolivian Llanos de Moxos. These heterogeneous landscapes harbour high levels of biodiversity and some of the earliest records of human occupation and plant domestication in Amazonia. While persistent Indigenous legacies have been demonstrated elsewhere in the Amazon, it is unclear how past human-environment interactions may have shaped vegetation composition and structure in the ARE. Here, we examine 6000 years of archaeological and palaeoecological data from Laguna Versalles (LV), Bolivia. LV was dominated by stable rainforest vegetation throughout the Holocene. Maize cultivation and cultural burning are present after ca 5700 cal yr BP. Polyculture cultivation of maize, manioc and leren after ca 3400 cal yr BP predates the formation of Amazonian Dark/Brown Earth (ADE/ABE) soils (approx. 2400 cal yr BP). ADE/ABE formation is associated with agroforestry indicated by increased edible palms, including Mauritia flexuosa and Attalea sp., and record levels of burning, suggesting that fire played an important role in agroforestry practices. The frequent use of fire altered ADE/ABD forest composition and structure by controlling ignitions, decreasing fuel loads and increasing the abundance of plants preferred by humans. Cultural burning and polyculture agroforestry provided a stable subsistence strategy that persisted despite pronounced climate change and cultural transformations and has an enduring legacy in ADE/ABE forests in the ARE. This article is part of the theme issue 'Tropical forests in the deep human past'.

Funding

792197

ERC_Adv834514)

ERC_Cog616179

European Commission

European Research Council (ERC)

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© 2022 The Author(s). Published by the Royal Society. All rights reserved.

Notes

This is the author accepted manuscript. The final version is available from the Royal Society via the DOI in this record Data accessibility: Supplementary data to this article can be found online in the publicly available Neotoma database (www.neotomadb.org) and Global Charcoal database (www.gpwg.org/gpwgdb. html) once these data are published.

Journal

Philosophical Transactions of the Royal Society B: Biological Sciences

Publisher

Royal Society

Place published

England

Version

  • Accepted Manuscript

Language

en

FCD date

2022-03-09T15:02:20Z

FOA date

2022-03-09T15:13:40Z

Citation

Vol. 377, No. 1849, article 20200499

Department

  • Archaeology and History

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