Unprecedented Burning in Tropical Peatlands During the 20th Century Compared to the Previous Two Millennia.
Name
Global_Change_Biology_-_2026_-_Wang_-_Unprecedented_Burning_in_Tropical_Peatlands_During_the_20th_Century_Compared_to_the.pdf
Description
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Size
8.7 MB
Format
Adobe PDF
Checksum (CRC64NVME)
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Resource type
Journal article
Creator (person)
Wang, Yuwan
Feldpausch, Ted R.
Swindles, Graeme T.
Moss, Patrick
McGowan, Hamish A.
Sim, Thomas G.
Morris, Paul J.
Benfield, Adam
Courtney‐Mustaphi, Colin
Wahl, David
Montoya, Encarni
Githumbi, Esther
Honorio Coronado, Eurídice N.
Augustijns, Femke
Verstraeten, Gert
O' Donnell (Roe), Jess
Tibby, John
Benavides, Juan C.
Hapsari, K. Anggi
Schittek, Karsten
Mohamed Ramdzan, Khairun Nisha
Bao, Kunshan
Cole, Lydia E. S.
Anderson, Lysanna
Gałka, Mariusz
Orijemie, Emuobosa Akpo
Strobel, Paul
Ramya Bala, Prabhakaran
Dommain, René
Marchant, Rob
Sukumar, Raman
Chawchai, Sakonvan
Kavil, Sarath Pullyottum
Mooney, Scott
Kelly, Thomas J.
Gao, Yang
Voulgarakis, Apostolos
Boom, Arnoud
Burton, Chantelle
Berrio, Juan Carlos
Ribeiro, Kelly
Anderson, Liana O.
Hardiman, Mark
Spater, Molly
Page, Susan E.
Gallego‐Sala, Angela V.
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 name | Awards |
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
Rights statement
In Copyright
Additional information
IF = 12.1 (2024)