Abstract

Peatlands are a significant component of the global carbon (C) cycle, yet despite their role as a long-term C sink throughout the Holocene, they are increasingly vulnerable to destabilization. Nowhere is this shift from sink to source happening more rapidly than in Southeast Asia, and nowhere else are the combined pressures of land-use change and fire on peatland ecosystem C dynamics more evident nor the consequences more apparent. This review focuses on the peatlands of this region, tracing the link between deforestation and drainage and accelerating C emissions arising from peat mineralization and fire. It focuses on the implications of the recent increase in fire occurrence for air quality, human health, ecosystem resilience and the global C cycle. The scale and controls on peat-driven C emissions are addressed, noting that although fires cause large, temporary peaks in C flux to the atmosphere, year-round emissions from peat mineralization are of a similar magnitude. The review concludes by advocating land management options to reduce future fire risk as part of wider peatland management strategies, while also proposing that this region's peat fire dynamic could become increasingly relevant to northern peatlands in a warming world.This article is part of the themed issue 'The interaction of fire and mankind'.

Highlights

  • Peatlands are a globally important carbon (C) pool

  • This review focuses on the peatlands of this region, tracing the link between deforestation and drainage and accelerating C emissions arising from peat mineralization and fire

  • In terms of both area (3.6 million km2 [3]) and C storage (400–600 Gt [4]), the most extensive peatlands are found in northern regions of the world, but there are significant deposits in the humid tropics. These tropical peatlands cover some 0.4 million km2 with a total C pool of 80–90 Gt [5]. Their greatest extent is in Southeast Asia (0.25 million km2; 69 Gt C), with 57 Gt C in Indonesian peatlands and a smaller 9 Gt C in Malaysia [5]

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Summary

Introduction

Peatlands are a globally important carbon (C) pool. While covering only approximately 3% of the Earth’s land surface, they contain an estimated 500– 700 Gt (i.e. Pg) of C, which is between 32 and 46% of the total soil C pool (approx. 1500 Gt [1]) and likely exceeding that contained in the world’s vegetation (500 Gt [2]). Most peat C has accumulated over long time periods; in northern peatlands, more than half was sequestered before 7000 years BP [4], while some tropical deposits had an earlier genesis prior to the Last Glacial Maximum (less than 18 000 years BP [9]) Despite their role as a long-term C sink throughout the Holocene, peat C pools are increasingly vulnerable to destabilization through a combination of climatic warming, land-use change and fire. Potential for further escalation of C loss as global warming accelerates into the future Nowhere is this shift from sink to source happening more rapidly than in insular Southeast Asia, and nowhere else are the combined pressures of landuse change and fire on peatland ecosystem C dynamics more evident nor the consequences more apparent. The review concludes by advocating land management options to reduce future fire risk while proposing that the knowledge that has developed on Southeast Asia’s peat fire dynamic could become increasingly relevant to northern peatlands that are subject to intensifying levels of human disturbance in a warming world

Peatlands as vulnerable carbon pools
Fire feedbacks to the climate system
Scaling up
In the firing line: managing and preventing peat fire
Conclusion
Meeting discussion
74. Zvyagintsev AM et al 2011 Air pollution over
Findings
55. Van Leeuwen TT et al 2014 Biomass burning fuel
Full Text
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