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Guillaume Lawnizack PhD thesis

Stromatolites from Jussat cliff (Puy-de-Dôme, France)Roles of continental weathering and microbial activity on the evolution of lacustrine systems (Limagnes basin) in the context of late Eocene to early Miocene climate transitions (Project: LIMAGNES)

Started in october 2023

Supervisors: Pierre Pellenard & Emmanuelle Vennin

Funding: doctoral grant

 

Abstract

Cenozoic climate evolution and futures projections of global temperature and CO2 content from the GIEC (Westerhold et al., 2020). The red box shows the period during which the Limagnes basins were active and corresponds to the studied interval.In the modern context of climate change and associated biodiversity erosion, understanding past climate transitions is a key question to constrain climate models. The climatic transition that abruptly formed the Antarctic polar icecap during the Eocene/Oligocene transition (~34 Ma) characterizes the shift from Greenhouse to Icehouse global conditions. The record of extreme climatic disruptions in continental environments is still little studied, although it constitutes a major way to understand the carbon cycle. This PhD subject will investigate how climatic events from the late Eocene to the early Miocene are recorded in the Limagnes lacustrine system (Massif Central). An integrative multidisciplinary approach will combine analyses of facies/microfacies, mineralogy (including clay assemblages), and isotopic geochemistry (Hf-Nd combined isotopes), on outcrops and deep BRGM cores. The local tectonic context inducing rift basins governed by strong subsidence provides an exceptional opportunity to study the continuous evolution of lacustrine sedimentation from detrital deposits to microbial carbonates. The main objectives of this PhD focus on the effects of variations in continental weathering linked to hydrolysis conditions and the role of microbial activities on the lacustrine carbonate production.

 

Influence of climate and its variations on rock alteration and the sedimentary record (here focusing on Calcium, Bouton et al., 2019)Keywords

carbonates, weathering, paleoclimate, lacustrine, microbilaites

 

 

extrait:
lien_externe:
titre:
Les rôles de l'altération continentale et de l'activité microbienne sur l'évolution de systèmes lacustres (bassin des Limagnes) dans le contexte de transitions climatiques fin Éocène à début Miocène (Projet : LIMAGNES)
date_de_debut_these:
octobre 2023
nom:
Lawnizack
date_de_debut_these_numerique:
202310
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kc_raw_content:

Stromatolites from Jussat cliff (Puy-de-Dôme, France)Roles of continental weathering and microbial activity on the evolution of lacustrine systems (Limagnes basin) in the context of late Eocene to early Miocene climate transitions (Project: LIMAGNES)

Started in october 2023

Supervisors: Pierre Pellenard & Emmanuelle Vennin

Funding: doctoral grant

 

Abstract

Cenozoic climate evolution and futures projections of global temperature and CO2 content from the GIEC (Westerhold et al., 2020). The red box shows the period during which the Limagnes basins were active and corresponds to the studied interval.In the modern context of climate change and associated biodiversity erosion, understanding past climate transitions is a key question to constrain climate models. The climatic transition that abruptly formed the Antarctic polar icecap during the Eocene/Oligocene transition (~34 Ma) characterizes the shift from Greenhouse to Icehouse global conditions. The record of extreme climatic disruptions in continental environments is still little studied, although it constitutes a major way to understand the carbon cycle. This PhD subject will investigate how climatic events from the late Eocene to the early Miocene are recorded in the Limagnes lacustrine system (Massif Central). An integrative multidisciplinary approach will combine analyses of facies/microfacies, mineralogy (including clay assemblages), and isotopic geochemistry (Hf-Nd combined isotopes), on outcrops and deep BRGM cores. The local tectonic context inducing rift basins governed by strong subsidence provides an exceptional opportunity to study the continuous evolution of lacustrine sedimentation from detrital deposits to microbial carbonates. The main objectives of this PhD focus on the effects of variations in continental weathering linked to hydrolysis conditions and the role of microbial activities on the lacustrine carbonate production.

 

Influence of climate and its variations on rock alteration and the sedimentary record (here focusing on Calcium, Bouton et al., 2019)Keywords

carbonates, weathering, paleoclimate, lacustrine, microbilaites

 

 

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