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Thresholds in past relative Humidity and Ecosystem Structure in Africa

Project description

Role of relative humidity in forest resilience in Africa

The EU-funded THrESholds project will identify thresholds in relative humidity (RH) that in the last 10 000 years triggered the transition from forest to savanna or made forest resilience possible in Africa. The researcher will apply a new RH proxy based on the triple oxygen isotope composition (17O-excess) of phytoliths, microscopic silica particles formed in plant tissues. The 17O-excess in the water cycle will be examined at a West African instrumented site to precisely quantify the fractionation at play. 17O-excess of phytoliths from four West and Central African Holocene lake sediment cores will also be analysed to reconstruct changes in RH. Vegetation structure and fire activity will be reconstructed from the same sediments, and the effect of reconstructed RH and fire activity trends on vegetation changes will be analysed.

Objective

Tropical forest and savanna are home to one-fifth of global human population. With ongoing global change, predicting how these biomes will respond to changing rainfall and relative humidity (RH) is of high priority. The overall aim of this project is to identify thresholds in RH that triggered in the past (last 10,000 years) the transition from forest to savanna and those that made forest resilience possible in Africa. I will use a new RH proxy, recently developed by the host laboratory, which is the triple oxygen isotope composition (17O-excess) of phytoliths. While calibrations were conducted in growth chambers, field applications are needed to precisely evaluate the accuracy of the proxy. I will examine the evolution of the 17O-excess in the water cycle and in grass and tree phytoliths, and quantify the isotopic fractionation at play, at a West African instrumented site. Then 17O-excess bias potentially brought by the contribution of phytoliths from lake shoreline vegetation to bulk sedimentary phytoliths will be quantified. Finally, I will analyse the 17O-excess of phytoliths from four West and Central African Holocene lacustrine sedimentary cores to reconstruct changes in RH. Vegetation structure and fire activity will be reconstructed from the same sediments. The effect of reconstructed RH and fire activity trends will be analyzed using time series cross-correlation and spectral analyses, and thresholds in RH identified using regime shifts analyses. These results will help to better understand the impacts of past climate change on tropical forest resilience. During this project, I will acquire new laboratory skills, develop the use of a new paleoclimate proxy, reinforce my scientific leadership and expand my career prospects in academia. I will bring my expertise in remote sensing analyses and biome management to the host laboratory. This project will also strengthen the European leadership in triple oxygen isotope analyses for paleoclimate reconstructions.

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Programme(s)

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Topic(s)

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Funding Scheme

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

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Call for proposal

Procedure for inviting applicants to submit project proposals, with the aim of receiving EU funding.

(opens in new window) H2020-MSCA-IF-2020

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Coordinator

CENTRE NATIONAL DE LA RECHERCHE SCIENTIFIQUE CNRS
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.

€ 176 946,28
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.

€ 196 707,84
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