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| Funder | Swedish Research Council |
|---|---|
| Recipient Organization | Umeå University |
| Country | Sweden |
| Start Date | Jan 01, 2025 |
| End Date | Dec 31, 2028 |
| Duration | 1,460 days |
| Number of Grantees | 4 |
| Roles | Co-Investigator; Principal Investigator |
| Data Source | Swedish Research Council |
| Grant ID | 2024-05713_VR |
Forests and peatlands dominate contemporary terrestrial carbon stocks and impact radiative forcing throughexchange with the atmosphere.
Rising temperatures and C O concentrations influence the exchange fluxes ofthese ecosystems, but proxy- and satellite data and modelling give conflicting results, with serious consequencesfor the accuracy of climate model predictions.
We pioneer novel stable isotope methodology – isotopomerabundances, which constitute the unique isotope information contained in each individual molecular position of ametabolite.
Isotopomers allow us to link atmospheric biophysical controls to enzyme responses in plants,providing a powerful way of disentangling temperature and C O physiological effects on ecosystem functioning,and constraining process representations in models designed to project the evolution of biosphere carbon stocksunder global change scenarios.In this interdisciplinary collaboration we will: 1) Use manipulation experiments to identify and calibrateisotopomer signals for a set of tropical tree species and for Northern hemisphere Sphagnum mosses, andcomparing species with and without ability for N-fixation. 2) For both plant groups quantify - over the pastcentury - the interaction between “C O fertilization", temperature rise and plant N status. 3) Use the obtaineddata to update leaf metabolic representations in a globally benchmarked ecosystem model, using it to analysehistorical biospheric C fluxes and C balance changes
Umeå University
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