What Lies Beneath
Researchers dig for answers on earthworms and carbon
- By Joshua Brown
What lies beneath
Researchers dig for answers on earthworms and carbon
by Joshua Brown
The humble earthworm is really anything but that in Vermont forests. They are both “keystone species”—critters that control an ecosystem and have a disproportionate impact on other species—and invasive. There are sixteen earthworm species reported in Vermont, and none of them are native.
Consider the earthworm’s profile raised. What’s more, these creatures who are tipping the balance in Northern Forest ecosystems may also have a role in global climate change. Finding answers on this front drives a research project led by Don Ross, professor of plant and soil science, and a team of colleagues.
That work brings the scientists to a hillside in the Hinesburg Town Forest one summer day, where five students dig a hole in the ground. Surrounding them, a stand of youngish trees—paper birch, sugar maple, white ash—forms a pleasing green glow. The trees are reclaiming a farm field abandoned in the 1930s. Each tree, as it grows, sucks in carbon dioxide from the air, converting some of it into leaves and wood. In other words, a forest stores carbon from the atmosphere that would otherwise contribute to the greenhouse effect—and global warming.
But for all the carbon being stored in these trees aboveground, a roughly equal amount of carbon is stored belowground. And that’s where the earthworms come in.
Graduate student Meghan Knowles holds up a clump of soil. “Most of this is earthworm poop, because this is such a highly invaded site,” she says. “Most of this soil has been processed by earthworms.” Then she teases apart the clump. “We’re sifting through the litter to try to find earthworms, and then we’re going to look for middens—mounds—that are an indication of deep burrowing species,” she says.
On the edge of the hole, a thin layer of leaves on the top surface is visible, and then an even mix of blackish-brown soil goes down into the darkness. “Look at this patch,” say Josef Gorres, professor of plant and soil science, “there’s this leaf layer and then we’re straight into the top mineral layer.” Yes, Dr. Watson, worms have been here. In a forest like this without worms, there would first be a “duff layer,” which is a spongy, bouncy layer above the deeper mineral soils, “and this just doesn’t exist in here anymore,” says Gorres. The worms have, literally, eaten it.
This efficient decomposition is why home gardeners love earthworms: they break down organic matter, releasing nutrients. But in a Vermont forest they’re not so benign, since in breaking down that organic matter they redistribute carbon throughout the soil, changing the basic layering of forest floors—and the tree and understory species that depend on this system. “A lot of plants that use the duff layer as a germination medium or a seed bank will no longer be around,” says Gorres.
The worms also release carbon dioxide as they eat, adding to the forest’s carbon emissions. It might seem that earthworms are all villain in the drama that is the global carbon cycle. But not so fast, the UVM scientists say.
“When the earthworms first invade, they change things dramatically and there is a big carbon loss and change in the forest floor,” says Don Ross, holding up three different species on his hand. As these earthworms move through the soil, they’re ingesting mineral particles along with organic particles, glomming them together inside their digestive track. And “when they poop,” says Knowles, “they produce what we call an aggregate.”
Over time, it seems, these soil aggregates might physically protect the organic carbon inside them, forming a barrier to the microorganisms that could otherwise break it down. “So the question is,” Gorres asks, over the long run, “do earthworms create a negative balance or positive balance on carbon?”
Part of this research project—sponsored by the Northeastern States Research Cooperative, and exploring eighteen forest plots across Vermont—aims to answer that question. “Earthworms create these stable aggregate structures,” says Knowles. “And so I’m trying to quantitatively distinguish between what earthworms are creating and what is already here, to figure out if earthworms are increasing that physical protection of carbon.”
Recent studies in the Northern Forest have shown that land use changes—like agricultural abandonment or intensive tree harvesting—can dramatically change the amount of carbon stored in that land’s soils. Much of the Northern Forest that was previously tilled farmland is currently gaining stored carbon. But what was the soil carbon like before European settlement? And how much does the current earthworm invasion threaten these gains? It’s hard to say.
“The presumption is that the first agricultural immigrants brought earthworms with them,” says historical ecologist Charlie Cogbill, one of the scientists on this project, “but we don’t know where the baseline is without worms.”
In any case, both Cogbill and Don Ross say, land use history had a huge effect on the current status of the forest, and also, probably, on whether an area has earthworms today. The eighteen plots the team is studying intensively have widely varying amounts of belowground carbon—and preliminary data show about half of them appear to have earthworms in them. That variability likely reflects differing land use histories. “Many of the forests here developed in the presence of earthworms, when ag land was abandoned,” Gorres says. “That is likely to be quite different than a forest that has regenerated from a stand that was timber harvested and did not have any earthworms.”
There are many variables of soil type, specific type and intensity of land use practice, microclimate and others that make each site different. “In Vermont and New England, the earthworm distribution is very patchy,” says Gorres. “In some places, earthworms are abundant. Then step three meters in another direction, and there is a complete forest floor and no earthworms. Why is that? Nobody has really been able to answer that.”
This project may not be able to answer that question either, but it does seek to broadly survey the extent of the worm invasion across Vermont—and to better understand how the interaction between earthworm activity and land use history influences the amount of carbon in the soil.
Human-generated carbon—and its capture—is starting to develop into big business. Around the world, various types of carbon markets are emerging in the effort to slow and regulate climate change. Credits in these markets generally depend on being able to show that carbon is being sequestered out of the atmosphere—and held long-term. But belowground carbon is nearly impossible to include in these markets, or other mitigation efforts, because it’s hard to measure.
“Forest soil carbon is poorly understood, and so it’s often not counted or even removed from some forest carbon protocols,” says Cecilia Danks, a social scientist in UVM’s Rubenstein School of Environment and Natural Resources. “I’ve been brought in to this earthworm project to try to figure out: is there a carbon market connection?” This research effort aims to move toward a better accounting of carbon in the Northern Forest, and perhaps, Danks hopes, the chance for Vermont forestland owners to get a return on the carbon stored below their feet, even carbon passing through the bowel of an invasive earthworm.