H2020Individual fellowship2021–2023

THrESholds · Thresholds in past relative Humidity and Ecosystem Structure in Africa

Horizon 2020 — Marie Skłodowska-Curie Actions

Duration
2021-09-01 → 2023-08-31
EU contribution
€176,946
Participants
1
Scheme
MSCA-IF

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Results in brief

Thresholds in past relative Humidity and Ecosystem Structure in Africa

Tropical forests and savannas, vital for one-fifth of global human population, face challenges in predicting their responses to changing conditions like rainfall and relative humidity. These ecosystems function as alternative stable states due to feedback loops involving fire and vegetation. Understanding the thresholds in environmental conditions that trigger transitions between these vegetation states is crucial, but current data is limited due to the extended timescales involved. Fossil records in lake sediments spanning millennia offer valuable data, though their use presents methodological challenges, particularly when reconstructing variables like vegetation, rainfall, and RH. The present project aimed to address these limitations by participating to the development of a quantitative RH proxy based on the triple oxygen isotope analysis of phytoliths and identifying the RH thresholds responsible for transitions between forests and savannas in Africa over the past 5,000 years. Historically, the ecological dynamics of these ecosystems were not adequately considered in vegetation models, leading to mismanagement strategies such as fire suppression and afforestation in savannas. These strategies, while aimed at mitigating climate change, have adverse effects on biodiversity and local populations. To address this, it is essential to integrate the long-term ecological functioning of tropical forests and savannas into vegetation models, making the quantification of RH thresholds critical.

Data: CORDIS, © European Union

Project 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.

Original text from CORDIS.

Participants

  • CENTRE NATIONAL DE LA RECHERCHE SCIENTIFIQUE CNRS · ParisCoordinatorFrance

Links

Data: CORDIS, © European Union