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  5. Unprecedented Burning in Tropical Peatlands During the 20th Century Compared to the Previous Two Millennia.

Unprecedented Burning in Tropical Peatlands During the 20th Century Compared to the Previous Two Millennia.

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Resource type
Journal article
Creator (person)
Wang, Yuwan
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Feldpausch, Ted R.
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Swindles, Graeme T.
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Moss, Patrick
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McGowan, Hamish A.
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Sim, Thomas G.
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Morris, Paul J.
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Benfield, Adam
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Courtney‐Mustaphi, Colin
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Wahl, David
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Montoya, Encarni
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Githumbi, Esther
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Honorio Coronado, Eurídice N.
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Augustijns, Femke
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Verstraeten, Gert
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O' Donnell (Roe), Jess
Tibby, John
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Benavides, Juan C.
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Hapsari, K. Anggi
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Schittek, Karsten
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Mohamed Ramdzan, Khairun Nisha
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Bao, Kunshan
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Cole, Lydia E. S.
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Anderson, Lysanna
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Gałka, Mariusz
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Orijemie, Emuobosa Akpo
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Strobel, Paul
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Ramya Bala, Prabhakaran
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Dommain, René
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Marchant, Rob
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Sukumar, Raman
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Chawchai, Sakonvan
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Kavil, Sarath Pullyottum
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Mooney, Scott
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Kelly, Thomas J.
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Gao, Yang
Voulgarakis, Apostolos
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Boom, Arnoud
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Burton, Chantelle
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Berrio, Juan Carlos
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Ribeiro, Kelly
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Anderson, Liana O.
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Hardiman, Mark
Spater, Molly
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Page, Susan E.
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Gallego‐Sala, Angela V.
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Date published
March 17, 2026
Abstract
Tropical peatland wildfire incidence has risen in recent decades, driven by drainage for land use and intensified by severe droughts with global climate change. These disturbances have altered vegetation structure, disrupted ecosystem functioning, and increased carbon emissions, particularly in Southeast Asia. However, the long‐term history and characteristics of wildfires in tropical peatlands remain largely unknown. Here, we compiled fifty‐eight macro‐charcoal records from peatlands across the tropics, ranging from lowland forested to montane peatlands, to assess millennia‐scale changes and controlling factors of tropical peatland burning. We divided the datasets into four main sub‐regions: Neotropical, Afrotropical, Indomalayan and Australasian ecoregions to explore regional variability. Tropical peatlands had high burning levels between 0 and 850 , followed by a relatively low and stable period until a marked increase during the 20th century. The general trend in tropical peatland burning follows changes in global temperature, and climate variables that control the length and severity of drought events have a notable influence on peat burning before 1900 . During the 20th century, regional differences were observed, with declining fire trends in the Neotropical and Afrotropical regions and increasing fire trends in the Indomalayan and Australasian regions. This difference is likely attributable to human activities, and such intervention is also evident in palm swamps and hardwood swamps under similar wet, weakly seasonal climates. With the increase in anthropogenic pressures on peatlands and greater climate variability, future wildfires in peatlands are likely to become more frequent and widespread across all tropical ecoregions. Conservation and sustainable land‐use practices could be used to mitigate and control peatland burning and protect these carbon‐rich sinks.
Project(s)
Priority 4: Accelerated Taxonomy
Funder
Funder nameAwards
Global Challenges Research Fund
NE/T010401/1
Conselho Nacional de Desenvolvimento Científico e Tecnológico
409531/2021‐9
VLIRUOS
IUC project AMU ET2017IUC035A101
Fundação de Amparo à Pesquisa do Estado de São Paulo
FAPESP ‐ 2020/16457‐3
Leverhulme Trust
RPG‐2021‐354
Pontificia Universidad Católica del Ecuador
Ministry of Environment
University of Liverpool
Quandamooka Yoolooburrabee Aboriginal Corporation
Journal title
Global Change Biology
Volume
32
Issue
3
Article number
e70717
Publisher
John Wiley & Sons Ltd.
Place of publication
UK
ISSN
1354-1013
eISSN
1365-2486
Date accepted
August 13, 2025
Official URL
https://doi.org/10.1111/gcb.70717
Rights statement
In Copyright
Licence
https://creativecommons.org/licenses/by/4.0/
DOI
10.1111/gcb.70717
Keywords
Charcoal
Peatlands
Palaeoenvironment
Contemporary fire
Last two millennia
Paleofire
Holocene
Tropical peatlands
Additional information
IF = 12.1 (2024)
Managed by the British Library and supported by the AHRC

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