» Articles » PMID: 22279247

The Human Dimension of Fire Regimes on Earth

Abstract

Humans and their ancestors are unique in being a fire-making species, but 'natural' (i.e. independent of humans) fires have an ancient, geological history on Earth. Natural fires have influenced biological evolution and global biogeochemical cycles, making fire integral to the functioning of some biomes. Globally, debate rages about the impact on ecosystems of prehistoric human-set fires, with views ranging from catastrophic to negligible. Understanding of the diversity of human fire regimes on Earth in the past, present and future remains rudimentary. It remains uncertain how humans have caused a departure from 'natural' background levels that vary with climate change. Available evidence shows that modern humans can increase or decrease background levels of natural fire activity by clearing forests, promoting grazing, dispersing plants, altering ignition patterns and actively suppressing fires, thereby causing substantial ecosystem changes and loss of biodiversity. Some of these contemporary fire regimes cause substantial economic disruptions owing to the destruction of infrastructure, degradation of ecosystem services, loss of life, and smoke-related health effects. These episodic disasters help frame negative public attitudes towards landscape fires, despite the need for burning to sustain some ecosystems. Greenhouse gas-induced warming and changes in the hydrological cycle may increase the occurrence of large, severe fires, with potentially significant feedbacks to the Earth system. Improved understanding of human fire regimes demands: (1) better data on past and current human influences on fire regimes to enable global comparative analyses, (2) a greater understanding of different cultural traditions of landscape burning and their positive and negative social, economic and ecological effects, and (3) more realistic representations of anthropogenic fire in global vegetation and climate change models. We provide an historical framework to promote understanding of the development and diversification of fire regimes, covering the pre-human period, human domestication of fire, and the subsequent transition from subsistence agriculture to industrial economies. All of these phases still occur on Earth, providing opportunities for comparative research.

Citing Articles

Extreme Fire Spread Events Burn More Severely and Homogenize Postfire Landscapes in the Southwestern United States.

McFarland J, Coop J, Balik J, Rodman K, Parks S, Stevens-Rumann C Glob Chang Biol. 2025; 31(2):e70106.

PMID: 40007450 PMC: 11862873. DOI: 10.1111/gcb.70106.


Advancing terrestrial ecology by improving cross-temporal research and collaboration.

Azevedo-Schmidt L, Landrum M, Spoth M, Brocchini N, Hamley K, Mereghetti A Bioscience. 2025; 75(1):15-29.

PMID: 39911156 PMC: 11791528. DOI: 10.1093/biosci/biae108.


Seasonal spatial-temporal trends of vegetation recovery in burned areas across Africa.

Maillard O, Ribeiro N, Armstrong A, Ribeiro-Barros A, Andrew S, Amissah L PLoS One. 2025; 20(2):e0316472.

PMID: 39899503 PMC: 11790127. DOI: 10.1371/journal.pone.0316472.


Flame-forged divergence? Ancient human fires and the evolution of diurnal and nocturnal lineages in moorish geckos.

Fulgione D, Russo D, Rivieccio E, Maselli V, Avallone B, Mondanaro A iScience. 2025; 28(2):111715.

PMID: 39898051 PMC: 11783447. DOI: 10.1016/j.isci.2024.111715.


Molecular composition and the impact of fuel moisture content on fresh primary organic aerosol emissions during laboratory combustion of Ponderosa pine needles.

Jaoui M, Urbanski S, Long R, Landis M Environ Chem. 2024; 20(8):319-338.

PMID: 39502471 PMC: 11534018. DOI: 10.1071/en23013.


References
1.
Cochrane M . Fire science for rainforests. Nature. 2003; 421(6926):913-9. DOI: 10.1038/nature01437. View

2.
Crisp M, Burrows G, Cook L, Thornhill A, Bowman D . Flammable biomes dominated by eucalypts originated at the Cretaceous-Palaeogene boundary. Nat Commun. 2011; 2:193. DOI: 10.1038/ncomms1191. View

3.
Page S, Siegert F, Rieley J, Jaya A, Limin S . The amount of carbon released from peat and forest fires in Indonesia during 1997. Nature. 2002; 420(6911):61-5. DOI: 10.1038/nature01131. View

4.
Cochrane , Alencar , Schulze , Souza Jr , Nepstad , LEFEBVRE . Positive feedbacks in the fire dynamic of closed canopy tropical forests . Science. 1999; 284(5421):1832-5. DOI: 10.1126/science.284.5421.1832. View

5.
Van der Werf G, Dempewolf J, Trigg S, Randerson J, Kasibhatla P, Giglio L . Climate regulation of fire emissions and deforestation in equatorial Asia. Proc Natl Acad Sci U S A. 2008; 105(51):20350-5. PMC: 2629304. DOI: 10.1073/pnas.0803375105. View