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

Project description

A closer look at how climate warming affects tundra plant traits

There are no trees in the Arctic tundra region. The climate is cold and windy, and rainfall is rare. Covered in snow for much of the year, climate warming is changing vegetation. While warmer temperatures enhance plant photosynthetic uptake of atmospheric CO2, they also promote microbial decomposition of the vast permafrost carbon pool. This releases greenhouse gases to the atmosphere in a positive feedback loop. The EU-funded WarmTraits project will study how climate warming will affect tundra plant traits. To forecast ecosystem impacts, the project will conduct a long-term experiment where greenhouses have warmed tundra plots for 1, 11 and 21 years. It will also quantify the mechanistic effects of increasing climate warming duration on a suite of above- and belowground plant functional traits.

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.

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MSCA-IF - Marie Skłodowska-Curie Individual Fellowships (IF)

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Call for proposal

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(opens in new window) H2020-MSCA-IF-2019

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Coordinator

KOBENHAVNS UNIVERSITET
Net EU contribution

Net EU financial contribution. The sum of money that the participant receives, deducted by the EU contribution to its linked third party. It considers the distribution of the EU financial contribution between direct beneficiaries of the project and other types of participants, like third-party participants.

€ 207 312,00
Address
NORREGADE 10
1165 KOBENHAVN
Denmark

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Region
Danmark Hovedstaden Byen København
Activity type
Higher or Secondary Education Establishments
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Total cost

The total costs incurred by this organisation to participate in the project, including direct and indirect costs. This amount is a subset of the overall project budget.

€ 207 312,00
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