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Glacier shrinkage is causing a 'green transition'

  • Glacier shrinkage is causing 'green transition'

Glacier-fed streams are undergoing a process of profound change, according to EPFL scientists in a paper appearing in Nature Geoscience. This conclusion is based on the expeditions to the world’s major mountain ranges by members of the Vanishing Glaciers project.

Microbial life will flourish in mountain streams because of ongoing glacier shrinkage. This is what a team of scientists from EPFL and Charles University, Prague, report in a paper published in Nature Geoscience. Their observations are based on samples collected from 154 glacier-fed streams worldwide as part of the EPFL-led Vanishing Glaciers project, which is funded by the NOMIS Foundation.

Glacier-fed streams are murky, raging torrents in the summer. Large quantities of glacial meltwater churn up rocks and sediment, allowing very little light to reach the streambed, while freezing temperatures and snow in other seasons provide little opportunity for a rich microbiome to develop. But, as glaciers shrink under the effects of global warming, the volume of water originating from glaciers is declining. That means the streams are becoming warmer, calmer, and clearer, giving algae and other microorganisms an opportunity to become abundant and to contribute more to local carbon and nutrient cycles. “We’re witnessing a process of profound change at the level of the microbiome in these ecosystems – nothing short of a ‘green transition’ because of the increased primary production,” says Tom Battin, a full professor at EPFL’s River Ecosystems Laboratory (RIVER).


Ten percent: that’s the amount of volume lost by Swiss glaciers in the past two years. Scientific models predict continued rapid melting in the coming decades unless climate measures are adopted. Find out, through our animated infographic, what Swiss glaciers might look like by 2100.
© 2024 EPFL / Emphase

Changing composition

In their paper, the scientists looked at the nutrients, such as nitrogen and phosphorus, in the stream water as well as the enzymes that microorganisms living in the streambed sediment produce in order to use these nutrients. Then, they looked at changes in both of these over a very large gradient of streams fed by glaciers that differ in size. “Glacier-fed-stream ecosystems generally have limited quantities of carbon and nutrients, particularly phosphorous,” explains Tyler Kohler, a former postdoc at RIVER and the paper’s lead author. “As glaciers shrink and the demand for phosphorus by algae and other microorganisms grows, phosphorus may become more limiting in high-mountain streams.” Hence phosphorus, a critical building block for life, will become even more rare in downstream ecosystems, including larger rivers and lakes, with yet unknown impacts for their food webs.

Advanced stage in Uganda

These findings are supported by a paper published in Royal Society Open Science in August 2023 by scientists from the Vanishing Glaciers project. In this study, the authors analyzed the microbiome of a small glacier-fed stream in the Rwenzori Mountains, in Uganda, where the “green transition” was already at an advanced stage. Here, the nutrient and enzyme composition was also much different, and algae were abundant. “What’s happening with the Rwenzori glacier gives us a glimpse of what Swiss glacier-fed streams will look like 30 or 50 years from now,” says Battin. One outcome of this change is that as glacier-fed streams host more microbial life, they will play a bigger role in biogeochemical cycles such as CO2 fluxes.

The RIVER team plans to build on this research. They are conducting a census of the microbial biodiversity in glacier-fed streams and, using various lines of genomic information, are exploring how diverse microorganisms are able to dwell in one of Earth’s most extreme freshwater ecosystems.

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