H2020Individual fellowship2021–2023

WarmTraits · How does climate warming duration affect above- and belowground plant traits and overall tundra ecosystem functionality?

Horizon 2020 — Marie Skłodowska-Curie Actions

Duration
2021-05-01 → 2023-09-03
EU contribution
€207,312
Participants
1
Scheme
MSCA-IF

Lines connect the coordinator with its partners.

Results in brief

How does climate warming duration affect above- and belowground plant traits and overall tundra ecosystem functionality?

In the Arctic, climate change is causing tundra landscapes to warm at a rate twice that of the rest of the world. A key objective in ecology is to predict how climate warming will alter plant communities and to measure its impact on the ecosystem. Plant functional traits, such as plant height or leaf size, are measurable characteristics that reveal various strategies for competition with other plants and adaptation to climate change. For instance, variations in leaf thickness or nitrogen content have a significant influence on the carbon balance within ecosystems by directly affecting photosynthetic carbon uptake and the rates of microbial litter decomposition. As a result, plant traits establish a quantifiable connection between changes in vegetation and ecosystem processes that, in turn, have implications for the climate. As the tundra heats up, the vegetation absorbs more carbon dioxide through photosynthesis while microbial decomposition of soil carbon increasingly releases greenhouse gases into the atmosphere. Permafrost soils hold twice as much carbon as is currently present in the atmosphere. This raises significant concern regarding whether the tundra biome will act as net source or sink of atmospheric carbon, and consequently, whether it will exacerbate or mitigate future climate change. Ultimately, this hinges on the balance between plant carbon uptake and soil microbial decomposition losses. However, plants play a dual role—they not only sequester carbon but also regulate decomposition rates through changes in their leaf and root traits. Nevertheless, our understanding of how plants respond to long-term tundra warming in terms of their functional traits remains limited. In this project, my aim is to quantify the impact of climate warming duration on a comprehensive set of plant functional traits, both above- and belowground. To achieve this, I will take advantage of a unique opportunity to collect samples from a long-term field experiment. In this experiment, mini-greenhouses have been warming arctic tundra plots for durations of two, 12, and 22 years, respectively. Additionally, I will examine how plant responses to warming influence essential ecosystem functions, such as carbon and nitrogen mineralization rates, using stable isotopic labelling techniques. To enhance the project's impact, I plan to organize and host a field workshop. This workshop will not only educate students in the field of trait-based functional ecology but also provide them with valuable hands-on experience in field research methodologies. In doing so, I aim to efficiently collect project data while offering students invaluable research exposure and skill development. This project enhances our mechanistic understanding of how tundra ecosystems respond to prolonged climate warming, carrying direct implications for their feedback into the global climate system. The findings will assist researchers and modelers in refining climate change predictions, ultimately benefiting us all.

Data: CORDIS, © European Union

Project objective

Climate warming is changing vegetation across the Arctic tundra region. Warmer temperatures enhance plant photosynthetic uptake of atmospheric CO2 but warming also promotes microbial decomposition of the vast permafrost carbon pool, releasing greenhouse gases to the atmosphere in a positive feedback-loop. In addition to temperature, changes in plant composition also strongly affect carbon and nutrient cycling rates through species-specific differences in leaf and root characteristics. These so-called plant functional traits provide an essential link between vegetation change and ecosystem functionality, and understanding how climate warming affects tundra plant traits is therefore vital for accurately forecasting ecosystem impacts over the coming century.Climate-change manipulation experiments allow for process-based investigations into how ecosystems respond mechanistically to warming. However, lack of long-term experimental warming studies in the Arctic currently impedes our ability to predict future climate responses accurately over decadal time-scales because extrapolation of short-term data consistently leads to faulty long-term predictions. In WarmTraits, I will utilize a unique opportunity to destructively sample in a long-term experiment where greenhouses have warmed tundra plots for one, 11, and 21 years, respectively. Thereby, I will quantify the mechanistic effects of increasing climate-warming duration on a very comprehensive suite of above- and belowground plant functional traits. In addition, I will directly link functional trait changes to ecosystem functionality by measuring important ecosystem carbon and nitrogen cycling processes using stable isotope labelling. I have the required expertise in ecosystem ecology and biogeochemistry to implement the project objectives successfully, and my host’s expert knowledge ensures that I will receive top-tier research training in plant physiology and stable isotope techniques.

Original text from CORDIS.

Participants

  • KOBENHAVNS UNIVERSITET · KOBENHAVNCoordinatorDenmark

Links

Data: CORDIS, © European Union