Marie-Curie fellow (Postdoctoral researcher)
Topics:
Methods:
Softwares and codes:
2022-Present Marie Skłodowska-Curie fellow, GFZ Helmholtz Centre Potsdam, Germany.
Study: Temperature and hydroclimate changes in the southern Levant during the Holocene, using fluid inclusions in halite from ICDP core 5017-1.
Host: Pr. Achim Brauer.
2022-2024 Visiting scholar, Binghamton University, State University of New York, NY, USA.
Host: Distinguished Pr. Tim K. Lowenstein
2021-2022 Azrieli postdoctoral fellow, Leon Charney school of marine sciences, Dr. Moses Strauss department of geosciences, University of Haifa, Israel.
Study: Reconstruction of late Pleistocene lake levels of the Dead Sea.
Host: Dr. Nicolas WALDMANN
2015-2019 PhD in Environmental Geosciences, University Lyon 1 Claude Bernard, France: “Turning halite fluid inclusions into accurate paleothermometers with Brillouin spectroscopy: development of a new method and application to the Last Interglacial in the Dead Sea”. Supervision: Dr. Véronique GARDIEN (LGL-TPE, University Lyon 1), Pr. Frédéric CAUPIN (ILM, University Lyon 1).
Diploma delivered 12/12/2019
2013-2014 Master of Science “Earth and Planets” at CRPG, Lorraine University, Nancy, France.
Diploma delivered 25/11/2014
2011-2014 Geologist-Engineer school at Ecole Nationale Supérieure de Géologie (ENSG), Nancy, France.
Diploma delivered 07/10/2014
01/09/2009 Classe préparatoire aux grandes écoles (« prep school ») “Biology, Chemistry, Physics and Earth Sciences”, Lycée Chateaubriand, Rennes
Marie Skłodowska-Curie fellowship CROSSROADS (Climate ReOrganizations at Synoptic Scale as Recorded in the Offshore Archives of the Dead Sea). During this project, I focus on the Holocene halite deposits of the deep -ICDP core 5017-1. Using Brillouin spectroscopy (University of Lyon), Laser Ablation Inductively Coupled Plasma Mass Spectrometry (LA-ICP-MS, Binghamton University) and chemical modelling with Phreeqc, I reconstruct the chemical composition of halite fluid inclusions. Because halite precipitates when the lake is fully mixed, the composition of the fluid inclusions provides us with the average chemical composition of the lake. In turn, the magnesium concentration can be used to reconstruct the volume, and using the bathymetric curve the lake level, of the Dead Sea throughout the Holocene. Using Nucleation-Assisted Microthermometry (University of Bergen) and halite fluid inclusion modelling with HaliBubble, I reconstruct the temperature of the lake throughout the Holocene. I develop a thermal model of the Dead Sea in order to interpret these water temperatures in terms of air temperature. The final goal of the project is to obtain a Holocene timeseries of air temperature and lake level to investigate the synoptic-scale changes in atmospheric circulation.