USA — UO-led study of last 2,000 years of charcoal evidence suggests human impacts have curtailed fires in most areas
Climate has been implicated by a new study as a major driver of wildfires in the last 2,000 years. But human activities, such as land clearance and fire suppression during the industrial era (since 1750) have created large swings in burning, first increasing fires until the late 1800s, and then dramatically reducing burning in the 20th century.
The study by a nine-member team from seven institutions — led by Jennifer R. Marlon, a doctoral student in geography department at the University of Oregon — appears online ahead of regular publication in the journal Nature Geoscience. The team analyzed 406 sedimentary charcoal records from lake beds on six continents.
A 100-year decline in wildfires worldwide — from 1870 to 1970 — was recorded despite increasing temperatures and population growth, researchers found. “Based on the charcoal record,” Marlon said, “we believe the reduction in the amount of biomass burned during those 100 years can be attributed to a global expansion of agriculture and intensive grazing of livestock that reduced fuels plus general landscape fragmentation and fire-management efforts.”
Above a 2006 wildfire burns boreal forests in the Yukon Flats, central Alaska. The photo was taken by Phil Higuera.Observations of increased burning associated with global warming and fuel build-up during the past 30 years, however, are not yet included in the sediment record.
Charcoal levels have drawn attention during the past 25 years because these data can track wildfire activity — both incidence and severity — over long time periods, providing information when similar data from satellites or fire-scarred trees do not exist. This study is among early efforts to analyze charcoal records for widespread patterns and trends over such a long period.
The importance of the data presented by Marlon’s team is put into perspective of overall information about the history of wildfires in a “News & Views” article, also appearing online, written by Andrew C. Scott, an earth sciences researcher at the University of London.
During the last 2,000 years, fire activity was highest between 1750 and 1870. “This was a period when several factors combined to generate conditions favorable to wildfires,” Marlon said. “Population growth and European colonization caused massive changes in land cover, and human-induced increases in atmospheric carbon dioxide concentrations may have started to increase biomass levels and fuels.”
A photo by shows a post-wildfire view of the 1996 Charlton burn near Waldo Lake in the central Oregon Cascades. Photo: Jennifer Marlon.From A.D. 1 to about 1750, wildfires worldwide declined from earlier years, probably resulting from a long-term global cooling trend that offset any possible influence of population growth and related land-use changes. Researchers pointed to charcoal evidence in western North America as an example of this trend. Similar records also were found in Central America and tropical areas of South America. In the western U.S. and in Asia, researchers noted, “initial colonization may have been marked by an increased use of fire for land clearance.
Subsequently, expansion of intensive agriculture and grazing, as well as forest management activities, likely reduced wildfire activity, Marlon said. “Our results strongly suggest that climate change has been the main driver of global biomass burning for the past two millennia,” the researchers concluded. “The decline in biomass burning after A.D. 1870 is opposite to the expected effect of rising carbon dioxide and rapid warming, but contemporaneous with an unprecedentedly high rate of population increase.”
The eight co-authors with Marlon were: Patrick J. Bartlein and Daniel G. Gavin, professors in the geography department and members of theEnvironmental Change Research Group; C. Carcaillet of the Centre for Bio-Archaeology and Ecology in Montpellier, France; S.P. Harrison and I.C. Prentice, both of the University of Bristol in the United Kingdom; P.E. Higuera of Montana State University in Bozeman, Mont.; F. Joos of the Physics Institute and Oeschger Centre for Climate Change Research in Bern, Switzerland; and Mitchell .J. Power of the University of Utah in Salt Lake City and a curator at the Utah Museum of Natural History.
The National Science Foundation in the United States and Natural Environment Research Council in the United Kingdom funded the research.
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