Throughout the Arctic, rivers transport fallen trees from forests to the ocean. As the river twists and turns, the logs can stack up, resulting in long-term carbon storage.
A new study has mapped the largest known woody deposit, covering 51 square kilometers (20 square miles) of the Mackenzie River Delta in Nunavut, Canada, and calculated that the logs store about 3.4 million tons (about 3.1 million metric tons) of carbon.
“To put that in perspective, that’s about two and a half million car emissions for a year,” said Alicia Sendrowski, a research engineer who led the study while at Colorado State University.
“That’s a sizeable amount of carbon,” she said, but it’s not a carbon pool we know much about. “We have great knowledge about carbon in other forms, like dissolved or particulate organic carbon, but not what we call ‘large carbon’ large wood.” That’s starting to change.
For decades, scientists have known that driftwood can move quickly in the Arctic, but they are just now beginning to calculate how much wood there is and how much carbon storage we fear losing due to climate change.
“The Arctic’s cold, often dry or icy conditions mean trees can be preserved for tens of thousands of years; a tree that fell a thousand years ago might look just as fresh as one that fell last winter,” Sendrowski said.
“There’s been a lot of work on fluxes of carbon from water and sediment, but we simply didn’t pay attention to the wood until very recently. This is a very young field of research that is developing quite fast,” said Virginia Ruiz-Villanueva, a fluvial geomorphologist at the University of Lausanne who was not involved in the study. “And it’s important to study this wood not only for the carbon cycle but in general for our understanding of how these natural fluvial systems work, how the rivers mobilize and distribute the wood.”
The Mackenzie River Delta is a “hotspot” of carbon storage thanks to incredibly carbon-rich soils, so the logs’ carbon storage makes up a relatively small fraction of the delta’s total carbon storage, which is around 3 quadrillion grams of carbon.Alicia Sendrowski
The findings were published in Geophysical Research Letters, a journal that publishes high-impact, short-format research with direct significance in the Earth and space disciplines.
Sendrowski and her colleagues concentrated on the Mackenzie River, which has very high-resolution photography and is known to contain enormous wood reserves, to obtain a sense of the logjams. Its delta is the third largest in the world by land area and drains about 20% of Canada. The team studied about 13,000 square kilometers (5,000 square miles) of delta in the biggest attempt to map woody deposits so far.
The researchers spent three weeks in the field measuring river driftwood with colleagues at Colorado State University, mapping logjams, and sampling the wood to date using radiocarbon dating.
Sendrowski used remote photography after fieldwork to detect wood at the river’s surface and estimate the area of the logjam. Based on her field observations, she approximated the volume of wood within the logjam and the amount of carbon it is storing.
Sendrowski found the deposit, comprising more than 400,000 miniature caches of wood, is storing about 3.4 million tons (3.1 million metric tons) of carbon. The largest single deposit, which covers around 20 American football fields, stores 7,385 tons (6,700 metric tons) of carbon alone.
“But because there are even more logs buried in soil, submerged underwater, and hidden from aerial imagery under vegetation, the total amount of carbon stored in the delta’s wood could be about twice as large,” she said.
“The Mackenzie River Delta is a “hotspot” of carbon storage thanks to incredibly carbon-rich soils,” Sendrowski said, “so the logs’ carbon storage makes up a relatively small fraction of the delta’s total carbon storage, which is around 3 quadrillion grams of carbon.”
“But we think it’s still important because as changes in the basin occur, like logging or damming, and as climate change alters precipitation patterns and warming, wood preservation will decrease. It’s a significant amount of carbon, so there’s a potentially significant loss of carbon storage,” she said.
The Mackenzie logjam also represents only one basin in the Arctic; at least a dozen deltas larger than 500 square kilometers dot the north, so massive woody deposits throughout the Arctic could add up to a significant carbon storage pool that we know nothing about.
The researchers were also curious about how long a tree can survive in the Arctic, which is crucial for modeling how “active” a carbon pool is, or how quickly material is transferred about.
While many of the trees they sampled began growing around or after 1950, some were much older, dating back to around 700 CE. (A study in the 1960s carbon-dated wood from a tree preserved in an icy mound to about 33,000 years ago.)
The Mackenzie River Delta was a good place to start.
“The exciting aspect for me isn’t just the scale, but also the potential to apply this to other places where large wood hasn’t been focused on,” Sendrowski said. “It’s a burgeoning field, she said, and there’s still much to be learned.”