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Programme des sessions > Recherche par auteur > Régnier Edouard

A new 33 000 years long record at the Lago Grande di Monticchio (Basilicate, Italy): Overview of new tephrochronology, cores scan XRF and CT-scan analyses.
Adrien Maignan  1@  , Sébastien Nomade  2@  , Alison Pereira  3@  , Jérémy Jacob  4@  , Giada Fernandez  5, 6@  , Lorenzo Monaco  7, 5  , Biagio Giaccio  7  , Paul Albert  8  , Molly Flynn  8  , Maurizio Petrelli  9@  , Giulia Fisauli  9  , Alessandro Musu  9  , Claude Lemilbeau  10@  , Vincent Scao  11@  , Laurent Augustin  12@  , Alain De Moya  13@  , Trevor Popp  14@  , Edouard Régnier  1@  
1 : Laboratoire des Sciences du Climat et de l'Environnement
CEA, CNRS : UMR182, Université de Versailles-Saint Quentin en Yvelines
2 : Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette]
Université de Versailles Saint-Quentin-en-Yvelines, Commissariat à l'énergie atomique et aux énergies alternatives, Institut National des Sciences de l'Univers, Université Paris-Saclay, Centre National de la Recherche Scientifique, Université de Versailles Saint-Quentin-en-Yvelines : UMR8212, Commissariat à l'énergie atomique et aux énergies alternatives : DRF/LSCE, Institut National des Sciences de l'Univers : UMR8212, Centre National de la Recherche Scientifique : UMR8212
3 : Géosciences Paris Saclay
Institut National des Sciences de l'Univers, Université Paris-Saclay, Centre National de la Recherche Scientifique, Centre National de la Recherche Scientifique : UMR8148, Université Paris-Saclay : UMR8148, Institut National des Sciences de l'Univers : UMR8148
4 : Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette]
Université de Versailles Saint-Quentin-en-Yvelines, Commissariat à l'énergie atomique et aux énergies alternatives, Institut National des Sciences de l'Univers, Université Paris-Saclay, Centre National de la Recherche Scientifique, Université de Versailles Saint-Quentin-en-Yvelines : UMR8212, Commissariat à l'énergie atomique et aux énergies alternatives : DRF/LSCE, Institut National des Sciences de l'Univers : UMR8212, Centre National de la Recherche Scientifique : UMR8212
5 : "Sapienza" University of Rome, Dipartimento di Scienze della Terra
6 : Instituto di geologia ambientale e geoingeneria, CNR
7 : Istituto di Geologia Ambientale e Geoingegneria
8 : Department of Geography [Swansea]
9 : Department of Physics and Geology, University of Perugia, Perugia, Italy
10 : Institut des Sciences de la Terre d'Orléans  (ISTO)  -  Site web
CNRS : UMR7327, Université d'Orléans, BRGM
Campus Géosciences 1A, rue de la Férollerie 45071 Orléans cedex 2 -  France
11 : Laboratoire des Sciences du Climat et de l'Environnement  (LSCE)
CEA, CNRS, Université de Versailles-Saint Quentin en Yvelines
Université Paris-Saclay, 91191 Gif-sur-Yvette -  France
12 : Division technique INSU/SDU
Centre National de la Recherche Scientifique
13 : Carottage Continental France  (CCF)
CNRS
14 : UAR Observatoire des Sciences de l'Univers de Grenoble
CNRS

In 2023, a new coring was carried out in paleoenvironmental well-known archive of the Lago Grande di Monticchio (Basilicata, Italy). This archive is famous for containing dozens of tephra layers originated from the Campanian volcanic province. Two sister cores (MONTI23-II) were extracted at a lake depth of 6m, side by side and staggered in depth, using the U-NID-90-PO corer and the Uvitech Platform of the DT-INSU (France). A continuous composite core of 17.6 m covering the last 33 000 years was constructed, constituting a high potential archive for studying the paleoenvironmental changes occurred during this period covering the last deglaciation and the entire Holocene.

In this contribution we present millimeter resolution XRF and CTScan measurements provided all along the core that enabled the creation of a digital twin of each section, allowing a sub-millimetric match between them. We also discuss the chemical and lithological variations observed along the core. Regarding palaeoclimatic issues, the last deglaciation is here well expressed (3m) characterized by an increase of the carbon content in the sediment, that jumps between about 5 % during last glacial maximum (LGM) to about 30% at the beginning the Holocene. One other interested discovery is the drastic change in the chemistry of the sediments, lasting 300 years (40 cm), during the Middle Ages linked to the building of Sant'Ippolito abbey and following other human activities around the lake.

The combined XRF and CT scan images also bring significant information regarding the tephra layers preservations, deformation and potential reworking along the core. We also performed major elements analyses on 57 volcanic horizons on glass shards. We also obtained trace elements for 24 of them.

Finally, thanks to the geochemical identification of these tephra and direct 14C (on seed and macro plants remains) and 40Ar/39Ar (on single grains K-feldspars) dating, we created a Bayesian model for the core enabling us to construct the most accurate chronology for this environmental archive done so far.

All these new data will be compared with previous works published for this lake Monticchio, especially with pollen data already available (Allen et al., 2009).


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