Yvan Coquinot
Centre national de la recherche scientifique
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Featured researches published by Yvan Coquinot.
Science | 2011
Christopher S. Henshilwood; Francesco d’Errico; Karen L. van Niekerk; Yvan Coquinot; Zenobia Jacobs; Stein-Erik Lauritzen; Michel Menu; Renata García-Moreno
Early humans mixed and stored ochre pigments in shells 100,000 years ago, an indication of the emergence of higher planning. The conceptual ability to source, combine, and store substances that enhance technology or social practices represents a benchmark in the evolution of complex human cognition. Excavations in 2008 at Blombos Cave, South Africa, revealed a processing workshop where a liquefied ochre-rich mixture was produced and stored in two Haliotis midae (abalone) shells 100,000 years ago. Ochre, bone, charcoal, grindstones, and hammerstones form a composite part of this production toolkit. The application of the mixture is unknown, but possibilities include decoration and skin protection.
Journal of Analytical Atomic Spectrometry | 2011
Marie Radepont; Wout De Nolf; Koen Janssens; Geert Van der Snickt; Yvan Coquinot; Lizet Klaassen; Marine Cotte
Since antiquity, the red pigment mercury sulfide (α-HgS), called cinnabar in its natural form or vermilion red when synthetic, was very often used in frescoes and paintings, even if it was known to suffer occasionally from degradation. The paint hereby acquires a black or silver-grey aspect. The chemical characterization of these alteration products is rather challenging mainly because of the micrometric size and heterogeneity of the surface layers that develop and that are responsible for the color change. Methods such as electron microscopy, synchrotron-based microscopic X-ray fluorescence, microscopic X-ray absorption near edge spectroscopy, Raman microscopy and secondary ion microscopy have been previously employed to identify the (Hg- and S-) compounds present and to study their co-localization. Next to these, also microscopic X-ray diffraction (XRD) (either by making use of laboratory X-ray sources or when used at a synchrotron facility) allows the identification of the crystal phases that are present in degraded HgS paint layers. In this paper we employ these various forms of micro-XRD to analyze degraded red paint in different paintings and compare the results with other X-ray based methods. Whereas the elemental analyses of the degradation products revealed, next to mercury and sulfur, the presence of chlorine, X-ray diffraction allowed the identification, next to α-HgS, of the Hg and S-containing compound calomel (Hg2Cl2) but also of the Hg, S and Cl-containing minerals corderoite (α-Hg3S2Cl2) and kenhsuite (γ-Hg3S2Cl2). These observations are consistent with X-ray absorption spectroscopy measurements performed at the S- and Cl-edges.
Journal of Analytical Atomic Spectrometry | 2015
Marie Radepont; Yvan Coquinot; Koen Janssens; Jean-Jacques Ezrati; Wout De Nolf; Marine Cotte
The red pigment mercury sulfide, called cinnabar or vermilion, is well known to suffer from an alteration giving rise to a grey, grey-white or black color at the surface of degraded works of art. This phenomenon can dramatically affect the esthetical value of artworks. This work aims at assessing the factors (light, halides) influencing the instability of red mercury sulfide and understanding (by combining thermodynamic and experimental approaches) the chemical equilibria governing the formation and evolution of the different degradation compounds. From the thermodynamic study of the Hg–S–Cl–H2O system, it was concluded that Hg(0), Hg3S2Cl2, and Hg2Cl2 can be formed from the reaction of α-HgS with ClO(g). In the second part, the artificial ageing experiments presented were carried out on model samples following the conditions assessed in the first part, in order to reproduce natural ageing observed on red mercury sulfide. Similarly to degradation compounds detected on original works of art, mercury chlorine compounds such as calomel (Hg2Cl2) and corderoite (α-Hg3S2Cl2) were identified on the surface of α-HgS model samples, when exposed to light and a sodium hypochlorite solution. Sulfates were detected as well, and more particularly gypsum (CaSO4·2H2O) when Ca was originally present in the model sample. The relationship between color and composition is discussed as well.
Global and Planetary Change | 2009
Stéphane Desruelles; Eric Fouache; Attila Çiner; Rémi Dalongeville; Kosmas Pavlopoulos; Erdal Koşun; Yvan Coquinot; Jean-Luc Potdevin
Canadian Mineralogist | 2009
M. Naze-Nancy Masalehdani; Florias Mees; Michel Dubois; Yvan Coquinot; Jean-Luc Potdevin; Michel Fialin; Marie-Madeleine Blanc-Valleron
Geomorphologie-relief Processus Environnement | 2004
Stéphane Desruelles; Eric Fouache; Kosmas Pavlopoulos; Rémi Dalongeville; Jean-Pierre Peulvast; Yvan Coquinot; Jean-Luc Potdevin
Geomorphologie-relief Processus Environnement | 2004
Stéphane Desruelles; Eric Fouache; Kosmas Pavlopoulos; Rémi Dalongeville; Jean-Pierre Peulvast; Yvan Coquinot; Jean-Luc Potdevin
Geodinamica Acta | 2007
Stéphane Desruelles; Eric Fouache; Rémi Dalongeville; Kosmas Pavlopoulos; Jean-Pierre Peulvast; Yvan Coquinot; Jean-Luc Potdevin; Claire Hasenohr; Michèle Brunet; Robert Mathieu; Élisabeth Nicot
Techné | 2008
Hélène Salomon; Colette Vignaud; Yvan Coquinot; Sandrine Pagès-Camagna; Marie-Pierre Pomiès; Michel Menu; Michèle Julien; Francine David; Jean-Michel Geneste
Paléo: revue d'archéologie préhistorique | 2014
Francesco D'Errico; Christopher S. Henshilwood; Renata García-Moreno; Yvan Coquinot; Michel Menu; Zenobia Jacobs; Stein-Erik Lauritzen