TY - JOUR
T1 - Unprecedented burning in tropical peatlands during the 20th century compared to the previous two millennia
T2 - Tropical peatland burning through time
AU - Wang, Yuwan
AU - Feldpausch , Ted
AU - Swindles, Graeme
AU - Moss, Patrick
AU - McGowan, Hamish
AU - Sim, Thomas
AU - Morris, Paul
AU - Benfield, Adam
AU - Courtney-Mustaphi, Colin
AU - Wahl, David
AU - Montoya, Encarni
AU - Githumbi, Esther
AU - Honorio Coronado, Euridice
AU - Augustijns, Femke
AU - Verstraeten, Gert
AU - O'Donnell (Roe), Jess
AU - Tibby, John
AU - Benavides, Juan
AU - Hapsari, K. Anggi
AU - Schittek, Karsten
AU - Ramdzan, Khairun Nisha Mohamed
AU - Bao, Kunshan
AU - Cole, Lydia
AU - Anderson, Lysanna
AU - Gałka, Mariusz
AU - Emuobosa Akpo, Orijemie
AU - Strobel, Paul
AU - Ramya Bala, Prabhakaran
AU - Dommain, Rene
AU - Marchant, Rob
AU - Sukumar, Raman
AU - Chawchai, Sakonvan
AU - Pullyottum Kavil, Sarath
AU - Mooney, Scott
AU - Kelly, Thomas
AU - Gao, Yang
AU - Voulgarakis, Apostolos
AU - Boom, Arnoud
AU - Burton, Chantelle
AU - Carlos Berrio, Juan
AU - Ribeiro, Kelly
AU - Anderson, Liana
AU - Hardiman, Mark
AU - Spater, Molly
AU - Page, Susan
AU - Gallego-Sala, Angela
PY - 2025/5/27
Y1 - 2025/5/27
N2 - 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 led to significant 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 higher burning levels between 0 and 850 CE, 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 CE. During the last century (1900-2000 CE), regional variability was observed, with declining fire trends in the Neotropical and Afrotropical regions and upward trends in the Indomalayan and Australasian regions. This difference is likely to be attributed to human activities and human intervention is also seen in palm swamps and hardwood swamps under similar climatic settings. 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 are needed to mitigate and control peatland burning and protect these carbon-rich sinks.
AB - 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 led to significant 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 higher burning levels between 0 and 850 CE, 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 CE. During the last century (1900-2000 CE), regional variability was observed, with declining fire trends in the Neotropical and Afrotropical regions and upward trends in the Indomalayan and Australasian regions. This difference is likely to be attributed to human activities and human intervention is also seen in palm swamps and hardwood swamps under similar climatic settings. 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 are needed to mitigate and control peatland burning and protect these carbon-rich sinks.
KW - Tropical peatland
KW - Contemporary fire
KW - Paleofire
KW - Charcoal
KW - Palaeoenvironment
KW - Last two millennia
KW - UKRI
KW - NERC
KW - NE/N011570/1
KW - NE/R017980/1
KW - NE/W001691/1
KW - NE/V018760/2
KW - NE/T010401/1
M3 - Article
SN - 1354-1013
JO - Global Change Biology
JF - Global Change Biology
ER -