The study, conducted by a team including University of Saskatchewan (USask) researchers, suggests that these faster-growing, less flammable deciduous forests may act as a stabilizing ‘firebreak’ against escalating fire patterns and nutrient loss in the region.
The study began in the wake of the dramatic 2004 fire season in Alaska when 6.7 million acres of forest burned—an area about five times the size of Prince Edward Island and seven times the long-term average. Historically, more than half of this forested terrain has been dominated by black spruce, but after fire, faster-growing aspen and birch are replacing some of these stands.
“In a region with only five common tree species, this study shows how changes in tree composition can dramatically alter patterns of carbon storage in boreal forests,” said Jill Johnstone, adjunct professor in biology at USask, researcher at University of Alaska-Fairbanks, and co-author of the study.
The team, made up of researchers from Northern Arizona University, the Center for Ecosystem Science and Society at NAU, the University of Alaska Fairbanks, Auburn University, and USask surveyed 75 black spruce stands that burned in 2004 and followed their recovery over the next 13 years. They also collected a range of data from trees and soils of different ages and burn severities to construct a chronosequence, a kind of scientific time-lapse that lets researchers fast-forward through a 100-year fire cycle to see how forests recover and change.
“In 2005, I thought that there was no way these forests could recover the carbon they lost in this fire,” said Michelle Mack, a professor of biology at Northern Arizona University and the lead author of the study. “The literature is full of papers suggesting deeper, more severe fires burn more carbon than can be replaced before the next fire. But not only did we see these deciduous trees make up for those losses, they did so rapidly.”
The team found that the new aspen and birch trees where the black spruce burned accumulated carbon and nitrogen more quickly than the spruce, storing most of it in their wood and leaves as opposed to the soil organic layer. And at the end of a projected 100-year cycle, the deciduous stands had recovered as much nitrogen as was lost to fire, and more carbon than was lost, resulting in an increase in the net ecosystem carbon balance. Calculating this balance is critical as scientists work to understand the way these northern forests are changing, and the effects of those changes on the global carbon picture.
“I was surprised that deciduous trees could replenish lost carbon so effectively and efficiently,” said Heather Alexander, an assistant professor of forest ecology at Auburn and one of the paper’s co-authors. “Even though considerable carbon is combusted and emitted into the atmosphere when black spruce forests burn severely, the deciduous trees that often replace them have an amazing ability to recapture and store carbon in their aboveground leaves and wood.”
“Carbon is just one piece of the puzzle,” said Mack, who noted deciduous forests have other important feedbacks, or interconnected effects, on climate. “We know these forests help cool regional climate, and we know that they are less ignitable, so fires are less likely to spread. Taken together, these effects create a relatively strong set of stabilizing climate feedbacks in the boreal forest.”
But there is a lot that researchers don’t know about the fate of deciduous boreal forests in a warmer world.
“As mature deciduous trees die, will they be replaced with trees with the same structure, composition, and carbon storage abilities?” Alexander asked. “And will they recover from fire with the same carbon storage capacities?”
“Shifts from slow-growing black spruce to fast-growing deciduous species could balance out the impacts of the intensifying fire regime in the boreal forest,” said Isla Myers-Smith, a global change ecologist at the University of Edinburgh who was not involved in the study. “But it remains to be seen how carbon gains balance losses in future with accelerated warming at high latitudes.”
Mack said continued climate warming may undo the carbon-sequestering gains these trees represent.
“The carbon should reside longer on the landscape because deciduous forests are less flammable. But flammability isn’t a constant. The climate will pass a threshold where things get so hot and dry, even deciduous forests will burn. So, one question we need to ask is, how strong will the mitigating effect of low flammability be, and how long will it last?”
Permafrost carbon also complicates the picture. Though many of the sites in this study did not have permafrost near the soil surface, the permanently frozen ground is found across the boreal biome. As it thaws, permafrost releases stores of carbon and methane, potentially offsetting the storage gains by deciduous trees, Mack said.
“We will eventually pass a temperature threshold where negative feedbacks aren't enough.”
The other members of the research team from USask were Johnstone’s former doctoral students Xanthe Walker, currently a post-doctoral fellow at Northern Arizona University, and Mélanie Jean, now assistant professor of biology at Université de Moncton.
This research was supported by Canada’s Natural Sciences and Engineering Research Council, the U.S. Department of Defense Strategic Environmental Research and Development Program, the NASA Arctic Boreal Vulnerability Experiment, the U.S. Joint Fire Sciences program, and the Bonanza Creek Long-term Ecological Research Program, a program of the U.S. National Science Foundation and the USDA Forest Service.
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