Climate change-induced march of treelines halted by unsuitable soils: study

Climate change-induced march of treelines halted by unsuitable soils: study
University of Guelph researcher conducting field work on the Canadian Rockies. Credit: University of Guelph

New research from the University of Guelph is dispelling a commonly held assumption about climate change and its impact on forests in Canada and abroad.

It's long been thought that is enabling treelines to march farther uphill and northward. But it turns out that climate warming-induced advances may be halted by unsuitable soils.

It is an important finding for resource managers looking to preserve individual species or entire ecosystems.

"There's a common belief about the impacts of climate change," said U of G researcher Emma Davis. "It's actually a more complicated story than people believe."

Her studies are the first in southwestern Canada to test how factors such as may affect treeline advance.

Along with Prof. Ze'ev Gedalof, Davis, a recent Ph.D. graduate in the Department of Geography, Environment and Geomatics, looked at plant growth at higher altitudes than normal in the Canadian Rockies. Normally, travelling northward means a temperature drop of about 1 C every 130 kilometres, equivalent to climbing 65 to 100 metres up a mountainside.

Just as scientists expect climate-induced warming to enable more northerly movement of plants, they also predict the alpine treeline will climb warming mountain slopes.

Climate change-induced march of treelines halted by unsuitable soils: study
University of Guelph researcher Emma Davis in the field. Credit: University of Guelph

The U of G researchers grew spruce and fir seedlings at varying elevations beyond their current limits in four locations, including Jasper National Park in Alberta and Kootenay National Park in British Columbia. They also collected soil samples from the same areas in which to grow spruce seeds in growth chambers at the University.

Controlling for conditions such as variables, seed quality and predation allowed them to zero in on soil properties. They found that plants thriving below the treeline were hindered by soils beyond the existing range, although the scientists aren't sure why.

Gedalof said soils may inhibit seed germination, including changes to soil chemistry caused by vegetation or soil microbes or fungi. Climate warming may also inhibit germination or growth of seedlings by increasing surface temperatures or reducing winter snow days, leading to drier conditions.

The researchers suspect similar results would occur in other mountainous areas and at higher latitudes worldwide.

Their findings are good news for rare or threatened species that face potential competition from encroaching plants creeping up from below the treeline, said Gedalof, who runs the Climate and Ecosystem Dynamics Research Group on campus.

"We've bought some time to figure out how to preserve the alpine system."

At the same time, struggling to adapt to warmer conditions in their home range may face hurdles in migrating northward or higher on a mountainside if they encounter unsuitable soils.

That's important for ecologists looking to take advantage of favourable warming to encourage growth of economically and ecologically important plant species beyond their existing ranges, he said. "Non-climatic factors are clearly limiting changes."

The research was published recently in the journals Arctic, Antarctic and Alpine Research and Global Change Biology.

Explore further

Seedlings face uphill battle with climate change

More information: Emma L. Davis et al, Limited prospects for future alpine treeline advance in the Canadian Rocky Mountains, Global Change Biology (2018). DOI: 10.1111/gcb.14338

Soil properties as constraints to seedling regeneration beyond alpine treelines in the Canadian Rocky Mountains, Arctic, Antarctic and Alpine Research … 5625?needAccess=true

Journal information: Global Change Biology

Citation: Climate change-induced march of treelines halted by unsuitable soils: study (2018, July 12) retrieved 15 August 2022 from
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