Natural barriers disturb the ecosystems in northern Sweden’s rivers
Umea University
image:
Previous theories have assumed that water, sediment and plant seeds move freely downstream (top image). However, lakes and rapids can become natural barriers where water can be slowed down as well. The solid lines show high transport or dispersal, and the dotted lines show reduced transport due to natural barriers.
view moreCredit: Marlene Lahti
Rivers in northern Sweden do not always become wider or richer in species further downstream. Natural barriers shape the flow and stop plants from spreading, new research from Umeå University shows.
“Our results suggest that many foundational assumptions in river science may not apply here,” says Lina Polvi Sjöberg, Associate Professor at the Department of Ecology, Environment and Geoscience at Umeå University.
The rivers in northern Sweden flow through terrain shaped by the last Ice Age. The landscape is dotted with lakes and covered in sediment brought by the ice: sand, gravel and plenty of boulders. A news study from Umeå University shows that this creates natural barriers that disrupt the flow of water. It also hinders the transport of sediment and the dispersal of plant seeds. All of this affects both the shape of the streams and the mix of plant types found along the shores.
“We found that these landscapes are naturally fragmented, and that local conditions – such as sediment type and proximity to lakes – play a much larger role than previously thought,” says Lina Polvi Sjöberg.
Together with researcher Lovisa Lind, she studied two catchments in norther Sweden, Bjurbäcken and Hjuksån, located above and below the highest coastline after the last glaciation. Using maps and field studies, they analysed the shape of the streams and the plant life along several miles of the shores.
Their findings challenge widely accepted theories that streams become wider and more biologically diverse downstream. The researchers found no clear correlations between the drainage area and channel width, and no consistent increase in plant species diversity downstream within these medium-sized catchments.
“In the catchment below the former highest coastline, we did see slightly stronger patterns, likely due to finer sediments from the sea. But overall, the presence of lakes and coarse glacial deposits breaks up the expected downstream trends,” says Lina Polvi Sjöberg.
The study shows that lakes stop transport of plant seeds by water. This leads to more diversity in plant life between nearby parts of the rivers. The researchers also saw an unexpected pattern: that species density (the number of species in a given area) was constant – or even decreased – downstream.
These results will have an impact on river restoration in areas shaped by the Ice Age. In these fragmented systems, passive recovery – where plants recolonise naturally – will probably not succeed. Instead, active interventions such as planting and physically reshaping the stream channels might be necessary.
“Restoration strategies need to be adapted to these local realities,” says Lina Polvi Sjöberg.
Streams in northern Sweden that were affected by the last Ice Age are fragmented, with three main types of reaches: rapids with large boulders, flats in sand or peat, and lakes.
Credit
Marlene Lahti
The terrain in northern Sweden was shaped by the last Ice Age.
Credit
Richard Mason
The terrain in northern Sweden was shaped by the last Ice Age.
Credit
Lina Polvi Sjöberg
Journal
Communications Earth & Environment
Method of Research
Observational study
Subject of Research
Not applicable
Article Title
Disrupted geomorphic and biotic stream connectivity in paraglacial regions
Article Publication Date
1-Oct-2025
