18 results on '"Bréhéret, Jean-Gabriel"'
Search Results
2. The earliest unambiguous Neanderthal engravings on cave walls: La Roche-Cotard, Loire Valley, France
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Marquet, Jean-Claude, primary, Freiesleben, Trine Holm, additional, Thomsen, Kristina Jørkov, additional, Murray, Andrew Sean, additional, Calligaro, Morgane, additional, Macaire, Jean-Jacques, additional, Robert, Eric, additional, Lorblanchet, Michel, additional, Aubry, Thierry, additional, Bayle, Grégory, additional, Bréhéret, Jean-Gabriel, additional, Camus, Hubert, additional, Chareille, Pascal, additional, Egels, Yves, additional, Guillaud, Émilie, additional, Guérin, Guillaume, additional, Gautret, Pascale, additional, Liard, Morgane, additional, O’Farrell, Magen, additional, Peyrouse, Jean-Baptiste, additional, Thamó-Bozsó, Edit, additional, Verdin, Pascal, additional, Wojtczak, Dorota, additional, Oberlin, Christine, additional, and Jaubert, Jacques, additional
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- 2023
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3. The earliest unambiguous Neanderthal engravings on cave walls:La Roche-Cotard, Loire Valley, France
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Marquet, Jean Claude, Freiesleben, Trine Holm, Thomsen, Kristina Jørkov, Murray, Andrew Sean, Calligaro, Morgane, Macaire, Jean Jacques, Robert, Eric, Lorblanchet, Michel, Aubry, Thierry, Bayle, Grégory, Bréhéret, Jean Gabriel, Camus, Hubert, Chareille, Pascal, Guillaud, Émilie, Guérin, Guillaume, Gautret, Pascale, Liard, Morgane, O’Farrell, Magen, Peyrouse, Jean Baptiste, Thamó-Bozsó, Edit, Verdin, Pascal, Wojtczak, Dorota, Oberlin, Christine, Jaubert, Jacques, Marquet, Jean Claude, Freiesleben, Trine Holm, Thomsen, Kristina Jørkov, Murray, Andrew Sean, Calligaro, Morgane, Macaire, Jean Jacques, Robert, Eric, Lorblanchet, Michel, Aubry, Thierry, Bayle, Grégory, Bréhéret, Jean Gabriel, Camus, Hubert, Chareille, Pascal, Guillaud, Émilie, Guérin, Guillaume, Gautret, Pascale, Liard, Morgane, O’Farrell, Magen, Peyrouse, Jean Baptiste, Thamó-Bozsó, Edit, Verdin, Pascal, Wojtczak, Dorota, Oberlin, Christine, and Jaubert, Jacques
- Abstract
Here we report on Neanderthal engravings on a cave wall at La Roche-Cotard (LRC) in central France, made more than 57±3 thousand years ago. Following human occupation, the cave was completely sealed by cold-period sediments, which prevented access until its discovery in the 19th century and first excavation in the early 20th century. The timing of the closure of the cave is based on 50 optically stimulated luminescence ages derived from sediment collected inside and from around the cave. The anthropogenic origin of the spatially-structured, non-figurative marks found within the cave is confirmed using taphonomic, traceological and experimental evidence. Cave closure occurred significantly before the regional arrival of H. sapiens, and all artefacts from within the cave are typical Mousterian lithics; in Western Europe these are uniquely attributed to H. neanderthalensis. We conclude that the LRC engravings are unambiguous examples of Neanderthal abstract design.
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- 2023
4. Dynamics of nonmigrating mid-channel bar and superimposed dunes in a sandy-gravelly river (Loire River, France)
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Wintenberger, Coraline L., Rodrigues, Stéphane, Claude, Nicolas, Jugé, Philippe, Bréhéret, Jean-Gabriel, and Villar, Marc
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- 2015
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5. Fluvial islands: First stage of development from nonmigrating (forced) bars and woody-vegetation interactions
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Wintenberger, Coraline L., Rodrigues, Stéphane, Bréhéret, Jean-Gabriel, and Villar, Marc
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- 2015
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6. New data on middle Turonian tuffeaux of southern Touraine and on their ammonites faunas
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Amédro, Francis, Robaszynski, Francis, Châtelier, Hervé, Ferchaud, Patrice, Matrion, Bertrand, Bréhéret, Jean-Gabriel, Biogéosciences [UMR 6282] [Dijon] (BGS), Université de Bourgogne (UB)-AgroSup Dijon - Institut National Supérieur des Sciences Agronomiques, de l'Alimentation et de l'Environnement-Centre National de la Recherche Scientifique (CNRS), Département Mines-Géologie, Faculté polytechnique de Mons, Université de Mons (UMons)-Université de Mons (UMons), GéoHydrosystèmes COntinentaux (GéHCO EA6293), Université de Tours, Laffont, Rémi, and Université de Tours (UT)
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Romaniceras (Y.) ornatissimum zone ,ammonites ,tuffeaux ,correlations ,zone à Romaniceras (Y.) ornatissimum ,Turonian Stratotype ,[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/Paleontology ,Stratotype Turonien ,[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology ,corrélations - Abstract
The knowledge of the Turonian stratotype, “from Saumur till Montrichard“, along the Loire and the Cher valleys waspublished in 2018 by Amédro et alii. Since then, the study of recent collecting of ammonites in southern Touraine provided significant informationto state more precisely the Turonian zonation. New outcrops are described at Bourgueil, Chinon, Loudun, Usseau, Sossay,Marigny-Marmande, Séligny and Ports-sur-Vienne where the following formations were recognized: the Amboise Chalk, the tuffeaux ofArdilliers, of Saumur, of Bourré and the Tuffeau Jaune de Touraine.In these southern countries, it is pointed out that: (1) more than the upper half of the Amboise Chalk appears like the Tuffeaude Saumur facies which at least develops till Châtellerault and contains the “Liron” marker level; (2) the upper part of the Tuffeau deBourré shows numerous firmgrounds; (3) the tempestites at the base of the Tuffeau Jaune de Touraine delivered an original ammoniteassociation where a new species, Romaniceras (R.) marigniacum, occurs with R. ornatissimum in the higher part of the R. ornatissimumzone (Tm 3); (4) consequently, the base of the Tuffeau Jaune de Touraine starts in the Middle Turonian and not in the Upper Turonian asit was traditionally admitted., Les connaissances relatives au Turonien stratotypique qui s’étend « depuis Saumur jusqu’à Montrichard » ont été publiées en2018 par Amédro et alii et concernent des localités réparties dans les vallées de la Loire et du Cher. L’étude de nouvelles récoltes d’ammonitesen Touraine méridionale apporte des compléments significatifs quant à la zonation de l’étage. De nouveaux affleurements sontdécrits à Bourgueil, Chinon, Loudun, Usseau, Sossay, Marigny-Marmande, Séligny et Ports-sur-Vienne où sont reconnues les formationsde la Craie d’Amboise, des Tuffeaux des Ardilliers, de Saumur, de Bourré et du Tuffeau Jaune de Touraine.Il est montré dans ces régions méridionales que : (1) plus de la moitié supérieure de la Craie d’Amboise se trouve sous le facièsdu Tuffeau de Saumur, ce dernier se développant au moins jusqu’à Châtellerault, avec le niveau repère « Liron » ; (2) la partie supérieuredu Tuffeau de Bourré comporte de nombreux arrêts de sédimentation avec firmgrounds ; (3) les tempestites de la base du Tuffeau Jaunede Touraine livrent une association d’ammonites inédite où une nouvelle espèce, Romaniceras (R.) marigniacum, coexiste avec R. ornatissimumau sommet de la zone du même nom (Tm 3) ; (4) ainsi, la base du Tuffeau Jaune de Touraine commence dans le Turonien moyenet non dans le Turonien supérieur comme il était traditionnellement admis.
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- 2020
7. The geological regional natural reserve of Pontlevoy (Loir-et-Cher, France): presentation and new data on the Miocene formations south of Blois
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Macaire, Jean-Jacques, Le Doussal, Claude, Hinschberger, Florent, Bréhéret, Jean-Gabriel, Sen, Sevket, GéoHydrosystèmes COntinentaux (GéHCO EA6293), Université de Tours (UT), Centre de Recherche en Paléontologie - Paris (CR2P), Muséum national d'Histoire naturelle (MNHN)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Région Centre - Val de Loire et Conseil Départemental du Loir-et-Cher, Hinschberger, Florent, and Université de Tours
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stratigraphie ,[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] ,[SDU.STU] Sciences of the Universe [physics]/Earth Sciences ,faille décrochante ,[SDU.STU]Sciences of the Universe [physics]/Earth Sciences ,[SDU.STU.GP] Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] ,[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/Paleontology ,paléontologie ,patrimoine géologique ,sédimentologie ,[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology ,Miocène - Abstract
The Geological Regional Natural Reserve (GRNR) of Pontlevoy, inaugurated in 2018, comprises two ancient quarries (theFour à Chaux quarry and the Hauts de la Plaine Saint-Gilles quarry). It shows the main Miocene formations, overlaying one on theother, which are characteristic of the area located between the Loire and the Cher valleys at the South of Blois: Aquitanian “Calcaire deBeauce”, Burdigalian “Sables et marnes du Blésois” and Langhian “Falun du Blésois”, the two last formations being fossiliferous. Aftera brief synthesis on the Miocene formations of this area, we present sedimentological data on the outcropping formation of the GRNRand results of new paleontological excavations in the “Sables et marnes du Blésois” of the reserve. The geophysical prospection usingelectrical conductivity method as well as borings and core drillings, performed before the preservation works in the area located betweenthe two quarries showed (1) a new fluvial formation filling a deep channel cut in the Langhian falun; this fluvial formation can be datedof the Serravalian or the Upper Miocene, and (2) a senestral strike-slip fault, also regarding to the east, which affects the whole Mioceneformations., La Réserve Naturelle Régionale Géologique (RNRG) de Pontlevoy inaugurée en 2018 comprend deux anciennes carrières (carrièredu Four à Chaux et carrière du Haut de la Plaine Saint-Gilles). On peut y observer en superposition stratigraphique les principalesformations miocènes du secteur situé entre Loire et Cher au sud de Blois : Calcaire de Beauce de l’Aquitanien, Sables et marnes duBlésois du Burdigalien et Faluns du Blésois du Langhien, les deux dernières étant fossilifères. Après une brève synthèse sur les formationsmiocènes de la région, sont présentées ici des données sédimentologiques sur les formations visibles dans la RNRG et les résultats denouvelles fouilles paléontologiques dans les Sables et marnes du Blésois de la réserve. La prospection géophysique par conductivité électrique,ainsi que les sondages et forages carottés effectués entre les deux carrières avant l’aménagement de la réserve, ont révélé (1) laprésence d’une nouvelle formation fluviatile comblant un profond chenal incisé dans le falun langhien ; cette formation peut être rapportéeau Serravallien ou au Miocène supérieur et (2) la présence d’une faille à regard est et décrochement sénestre affectant l’ensemble desformations miocènes.
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- 2020
8. The prehistoric site of la Roche-Cotard IV (Indre-et-Loire, France):A middle and upper Pleistocene sequence, reference for the Val-de-Loire in Touraine
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Marquet, Jean Claude, Macaire, Jean Jacques, Bayle, Grégory, Peyrouse, Jean Baptiste, Guillaud, Émilie, Aubry, Thierry, Liard, Morgane, Bréhéret, Jean Gabriel, Jørkov Thomsen, Kristina, Holm Freiesleben, Trine, Thamóné-Bozsó, Édit, Guérin, Guillaume, and Murray, Andrew S.
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Neanderthal ,Lithic industry ,Middle Paleolithic ,Palaeoenvironment ,Upper Pleistocene ,Archaeozoology ,Loire river - Abstract
The prehistoric site of La Roche-Cotard (LRC) is located on the right bank slope of the Loire Valley, a little upstream of Langeais in Indre-et-Loire. The site was made accessible by extensive material collection in 1846. The main cave, LRC I, was excavated in 1912: it contained a middle Paleolithic industry and digital traces were discovered in 1975 and validated in 2008. The resumption of excavations on the site since 2008 has highlighted a powerful 11 meter section with 22 distinct layers, the lower part of which fills a shelter: locus LRC IV, very close to LRC I. The stratigraphy combines from the bottom to the top, karstic inputs, fluvial and eolian sands from the Loire valley and slope deposits. Indices of anthropic occupation (lithic industry, burned bones) attest to the occupation of this space. Numerous radiocarbon and OSL ages make it possible to chronologically constrains this filling between the limit of the isotopic stages 7 and 6 (layer 22 - 169 ka) and the end of stage 3 (layer 2 - 25 ka). The locus has given rise to a multidisciplinary study as complete as possible (sedimentology and micromorphology, small and large vertebrate faunas, lithic industry...). These data provide new information on the palaeoenvironmental evolution of the region, which is poorly known in this time range. The geometry and the age of the deposits lead to the hypothesis that the main cave LRC I was impenetrable by Homo sapiens at least starting from the beginning of the isotopic stage 3 (60 ka) and thus that the parietal productions with symbolic character of the cave are most likely to be attributed to Neanderthal man.
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- 2019
9. Comparaison entre le Turonien du Saumurois et de la Touraine
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Amédro , Francis, Robaszynski , Francis, Bréhéret , Jean-Gabriel, Biogéosciences [UMR 6282] [Dijon] (BGS), Université de Bourgogne (UB)-AgroSup Dijon - Institut National Supérieur des Sciences Agronomiques, de l'Alimentation et de l'Environnement-Centre National de la Recherche Scientifique (CNRS), Département Mines-Géologie, Université de Mons (UMons), GéoHydrosystèmes COntinentaux (GéHCO EA6293), Université de Tours (UT), F. Amédro, B. Matrion & F. Robaszynski, P. De Wever & A. Cornée, Laffont, Rémi, Biogéosciences [Dijon] ( BGS ), Université de Bourgogne ( UB ) -AgroSup Dijon - Institut National Supérieur des Sciences Agronomiques, de l'Alimentation et de l'Environnement-Centre National de la Recherche Scientifique ( CNRS ), Université de Mons ( UMons ), GéoHydrosystèmes COntinentaux ( GéhCO EA6293 ), and Université de Tours
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[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy ,[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy ,[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy ,ComputingMilieux_MISCELLANEOUS - Abstract
7 pages; National audience
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- 2018
10. Les affleurements de la Touraine (partie orientale du stratotype)
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Amédro, Francis, Robaszynski, Francis, Bréhéret, Jean-Gabriel, Le Doussal, Claude, Matrion, Bertrand, Biogéosciences [Dijon] ( BGS ), Université de Bourgogne ( UB ) -AgroSup Dijon - Institut National Supérieur des Sciences Agronomiques, de l'Alimentation et de l'Environnement-Centre National de la Recherche Scientifique ( CNRS ), Département Mines-Géologie, Université de Mons ( UMons ), GéoHydrosystèmes COntinentaux ( GéhCO EA6293 ), Université de Tours, F. Amédro, B. Matrion & F. Robaszynski, P. De Wever & A. Cornée, Biogéosciences [UMR 6282] [Dijon] (BGS), Université de Bourgogne (UB)-AgroSup Dijon - Institut National Supérieur des Sciences Agronomiques, de l'Alimentation et de l'Environnement-Centre National de la Recherche Scientifique (CNRS), Université de Mons (UMons), GéoHydrosystèmes COntinentaux (GéHCO EA6293), Université de Tours (UT), and Laffont, Rémi
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[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy ,[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy ,[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy ,ComputingMilieux_MISCELLANEOUS - Abstract
17 pages; National audience
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- 2018
11. A Hydrothermal-Sedimentary Context for the Origin of Life
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Westall, Frances, Hickman-Lewis, Keyron, Hinman, Nancy, Gautret, Pascale, Campbell, Kathleen, Bréhéret, Jean-Gabriel, Foucher, Frédéric, Hubert, Axelle, Sorieul, Stephanie, Dass, Avinash Vicholous, Kee, Terence, Georgelin, Thomas, Brack, André, Centre de biophysique moléculaire (CBM), Université d'Orléans (UO)-Institut National de la Santé et de la Recherche Médicale (INSERM)-Centre National de la Recherche Scientifique (CNRS)-Institut de Chimie du CNRS (INC), Institut des Sciences de la Terre d'Orléans - UMR7327 (ISTO), Centre National de la Recherche Scientifique (CNRS)-Université d'Orléans (UO)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers en région Centre (OSUC), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Bureau de Recherches Géologiques et Minières (BRGM) (BRGM), Biogéosystèmes Continentaux - UMR7327, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)-Centre National de la Recherche Scientifique (CNRS)-Université d'Orléans (UO)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers en région Centre (OSUC), School of Environment [Auckland, New Zealand], University of Auckland [Auckland], GéoHydrosystèmes COntinentaux (GéHCO EA6293), Université de Tours (UT), Centre d'Etudes Nucléaires de Bordeaux Gradignan (CENBG), Université Sciences et Technologies - Bordeaux 1-Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3)-Centre National de la Recherche Scientifique (CNRS), School of Chemistry [Leeds], University of Leeds, Laboratoire de Réactivité de Surface (LRS), Institut de Chimie du CNRS (INC)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), CNRS-MI-2014, ANR-09-BLAN-0219,ARCHAEMAT(2009), Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)-Observatoire des Sciences de l'Univers en région Centre (OSUC), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)-Observatoire des Sciences de l'Univers en région Centre (OSUC), Université de Tours, Université d'Orléans (UO)-Institut National de la Santé et de la Recherche Médicale (INSERM)-Institut de Chimie du CNRS (INC)-Centre National de la Recherche Scientifique (CNRS), Université Sciences et Technologies - Bordeaux 1 (UB)-Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3)-Centre National de la Recherche Scientifique (CNRS), Vuillaume, Isabelle, and Blanc - - ARCHAEMAT2009 - ANR-09-BLAN-0219 - Blanc - VALID
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Geologic Sediments ,Earth, Planet ,Silicates ,[CHIM] Chemical Sciences ,Origin of Life ,Temperature ,Water ,[CHIM]Chemical Sciences ,Volcanic Eruptions ,Research Articles - Abstract
Critical to the origin of life are the ingredients of life, of course, but also the physical and chemical conditions in which prebiotic chemical reactions can take place. These factors place constraints on the types of Hadean environment in which life could have emerged. Many locations, ranging from hydrothermal vents and pumice rafts, through volcanic-hosted splash pools to continental springs and rivers, have been proposed for the emergence of life on Earth, each with respective advantages and certain disadvantages. However, there is another, hitherto unrecognized environment that, on the Hadean Earth (4.5–4.0 Ga), would have been more important than any other in terms of spatial and temporal scale: the sedimentary layer between oceanic crust and seawater. Using as an example sediments from the 3.5–3.33 Ga Barberton Greenstone Belt, South Africa, analogous at least on a local scale to those of the Hadean eon, we document constant permeation of the porous, carbonaceous, and reactive sedimentary layer by hydrothermal fluids emanating from the crust. This partially UV-protected, subaqueous sedimentary environment, characterized by physical and chemical gradients, represented a widespread system of miniature chemical reactors in which the production and complexification of prebiotic molecules could have led to the origin of life. Key Words: Origin of life—Hadean environment—Mineral surface reactions—Hydrothermal fluids—Archean volcanic sediments. Astrobiology 18, 259–293.
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- 2018
12. Le site préhistorique de la Roche‑Cotard IV (Indre-et-Loire, France) : une séquence du pléistocene moyen et supérieur, référence pour le val de Loire tourangeau
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Marquet, Jean‑Claude, primary, Macaire, Jean‑Jacques, additional, Bayle, Grégory, additional, Peyrouse, Jean‑Baptiste, additional, Guillaud, Émilie, additional, Aubry, Thierry, additional, Liard, Morgane, additional, Bréhéret, Jean‑Gabriel, additional, Jørkov Thomsen, Kristina, additional, Freiesleben, Trine Holm, additional, Thamoné‑Bozso, Édit, additional, Guérin, Guillaume, additional, and Murray, Andrew S., additional
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- 2019
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13. Pierres, mortiers et parements de la tour des Minimes au regard du compte de construction de 1495-1496, des investigations archéologiques et des analyses pétrographiques
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Gaugain , Lucie, Bréhéret , Jean-Gabriel, Mechling , Jean-Michel, Prigent , Daniel, Centre d'études supérieures de la Renaissance UMR 7323 (CESR), Ministère de la Culture et de la Communication (MCC)-Université de Tours (UT)-Centre National de la Recherche Scientifique (CNRS), GéoHydrosystèmes COntinentaux (GéHCO EA6293), Université de Tours (UT), Institut Jean Lamour (IJL), Université de Lorraine (UL)-Institut de Chimie du CNRS (INC)-Centre National de la Recherche Scientifique (CNRS), Archéologie, Terre, Histoire, Sociétés [Dijon] (ARTeHiS), Centre National de la Recherche Scientifique (CNRS)-Université de Bourgogne (UB)-Ministère de la Culture et de la Communication (MCC), Centre d'études supérieures de la Renaissance ( CESR ), Centre National de la Recherche Scientifique ( CNRS ) -Université de Tours-Ministère de la Culture et de la Communication ( MCC ), GéoHydrosystèmes COntinentaux ( GéhCO EA6293 ), Université de Tours, Institut Jean Lamour ( IJL ), Université de Lorraine ( UL ) -Centre National de la Recherche Scientifique ( CNRS ), Archéologie, Terre, Histoire, Sociétés [Dijon] ( ARTeHiS ), Ministère de la Culture et de la Communication ( MCC ) -Université de Bourgogne ( UB ) -Centre National de la Recherche Scientifique ( CNRS ), Ministère de la Culture et de la Communication (MCC)-Université de Tours-Centre National de la Recherche Scientifique (CNRS), Institut de Chimie du CNRS (INC)-Université de Lorraine (UL)-Centre National de la Recherche Scientifique (CNRS), and Ministère de la Culture et de la Communication (MCC)-Université de Bourgogne (UB)-Centre National de la Recherche Scientifique (CNRS)
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accounts ,[SHS.ARCHI]Humanities and Social Sciences/Architecture, space management ,architecture ,Pierres de taille ,[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory ,Tour des Minimes ,archaeology ,building site ,bond ,Comptes de construction ,Pétrographie ,Château d'Amboise (Indre-et-Loire) ,petrography ,[ SHS.ARCHI ] Humanities and Social Sciences/Architecture, space management ,Mortiers ,15e siècle ,[ SHS.ARCHEO ] Humanities and Social Sciences/Archaeology and Prehistory ,tuffeau ,mortar - Abstract
International audience; Charles VIII (1483-1498) construction period in the castle at Amboise took place from 1492 to 1498. In 1495-1496, an account book was written mainly about the well-preserved Tour des Minimes, a tower one could climb up on horseback. A comparative study of the building, along with the account book, cut stones (petrography and statistics), mortars (grain size distribution and lime) and the whitewash jointing, requires a specific methodology and a constant dialogue between architectural historians, geologists, and archaeologists. The research enables to identify the name of the stones and the technical vocabulary used at the end of the middle ages. Moreover, it proves that achief stone dresser probably worked on the tower, and that the building site was likely to have been split into several centresand workshops; and it also reveals the rhythm of work to have been intense, since for the tower only, more than 15m of vaulted masonry had been created. All this have been allowed thanks to workers with an empirical knowledge of materials, the high quality of the chosen materials and the remarkable implementation they did. It resulted in an outstanding genuine edifice in which four revolutions and a half climb around an openwork newel.; Le chantier de Charles VIII (1483-1498) au château d’Amboise se déroula entre 1492 et 1498. L’année 1495-1496 est documentée par un livre de compte concernant notamment la tour cavalière des Minimes, aujourd’hui bien conservée. L’étude croisée du bâti, du livre de compte, des pierres de taille (pétrographie et statistique), des mortiers (granulométrie et analyses de la chaux) et du badigeon recouvrant les joints a nécessité la mise en place d’une méthodologie précise, demandant de continuels échanges entre historiens de l’architecture, géologues et archéologues. Ces investigations permettent d’identifier les dénominations des pierres et le vocabulaire technique en usage à la fin du Moyen Âge. Mais bien au-delà, elles démontrent l’intervention probable d’un appareilleur, l’organisation du chantier régi en plusieurs pôles et ateliers, ainsi que son rythme très soutenu puisque, pour la seule tour, plus de 15 m de maçonneries voûtées furent élevées. Ce fut possible grâce à la connaissance empirique des matériaux qu’avaient les hommes œuvrant à la construction, à la qualité des matériaux employés et à la remarquable mise en œuvre qui en fut faite. Il en résulte un ouvrage hors du commun, d’une rare audace où quatre révolutions et demie de voûtes d’ogives montent autour d’un noyau creux.
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- 2017
14. Biosignatures on Mars: What, Where, and How? Implications for the Search for Martian Life
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Westall, Frances, Foucher, Frédéric, Bost, Nicolas, Bertrand, Marylène, Loizeau, Damien, Vago, Jorge L., Kminek, Gerhard, Gaboyer, Frédéric, Campbell, Kathleen A., Bréhéret, Jean-Gabriel, Gautret, Pascale, Cockell, Charles S., Centre de biophysique moléculaire (CBM), Université d'Orléans (UO)-Institut National de la Santé et de la Recherche Médicale (INSERM)-Centre National de la Recherche Scientifique (CNRS)-Institut de Chimie du CNRS (INC), Conditions Extrêmes et Matériaux : Haute Température et Irradiation (CEMHTI), Centre National de la Recherche Scientifique (CNRS)-Institut de Chimie du CNRS (INC)-Université d'Orléans (UO), Agence Spatiale Européenne (ESA), European Space Agency (ESA), School of Environment, University of Auckland [Auckland], GéoHydrosystèmes COntinentaux (GéHCO EA6293), Université de Tours, Institut des Sciences de la Terre d'Orléans - UMR7327 (ISTO), Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)-Observatoire des Sciences de l'Univers en région Centre (OSUC), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS), SUPA School of Physics and Astronomy [Edinburgh], University of Edinburgh, CNRS -MI-2014, LE STUDIUM Orléans Région Centre, ANR-09-BLAN-0219,ARCHAEMAT(2009), European Project: 607297,EC:FP7:SPA,FP7-SPACE-2013-1,MASE(2014), European Project: 280168,EC:FP7:ERC,ERC-2011-StG_20101014,E-MARS(2011), Université d'Orléans (UO)-Institut National de la Santé et de la Recherche Médicale (INSERM)-Institut de Chimie du CNRS (INC)-Centre National de la Recherche Scientifique (CNRS), Université d'Orléans (UO)-Institut de Chimie du CNRS (INC)-Centre National de la Recherche Scientifique (CNRS), Agence Spatiale Européenne = European Space Agency (ESA), Université de Tours (UT), Centre National de la Recherche Scientifique (CNRS)-Université d'Orléans (UO)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers en région Centre (OSUC), and Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)
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[SDU]Sciences of the Universe [physics] - Abstract
International audience; The search for traces of life is one of the principal objectives of Mars exploration. Central to this objective is theconcept of habitability, the set of conditions that allows the appearance of life and successful establishment ofmicroorganisms in any one location. While environmental conditions may have been conducive to the appearanceof life early in martian history, habitable conditions were always heterogeneous on a spatial scale andin a geological time frame. This ‘‘punctuated’’ scenario of habitability would have had important consequencesfor the evolution of martian life, as well as for the presence and preservation of traces of life at a specificlanding site. We hypothesize that, given the lack of long-term, continuous habitability, if martian life developed,it was (and may still be) chemotrophic and anaerobic. Obtaining nutrition from the same kinds of sourcesas early terrestrial chemotrophic life and living in the same kinds of environments, the fossilized traces of thelatter serve as useful proxies for understanding the potential distribution of martian chemotrophs and theirfossilized traces. Thus, comparison with analog, anaerobic, volcanic terrestrial environments (Early Archean>3.5–3.33 Ga) shows that the fossil remains of chemotrophs in such environments were common, althoughsparsely distributed, except in the vicinity of hydrothermal activity where nutrients were readily available.Moreover, the traces of these kinds of microorganisms can be well preserved, provided that they are rapidlymineralized and that the sediments in which they occur are rapidly cemented. We evaluate the biogenicity ofthese signatures by comparing them to possible abiotic features. Finally, we discuss the implications of differentscenarios for life on Mars for detection by in situ exploration, ranging from its non-appearance, throughpreserved traces of life, to the presence of living microorganisms. Key Words: Mars—Early Earth—Anaerobicchemotrophs—Biosignatures—Astrobiology missions to Mars. Astrobiology 15, 998–1029.
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- 2015
15. Programme, AGES (Ancient Geomorphological EvolutionS) / Évolutions géomorphologiques anciennes de lʼhydrosystème ligérien. Rapport intermédiaire
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Castanet, C., Arthuis, Rémy, Bréhéret, Jean-Gabriel, Carcaud, Nathalie, Cubizolle, Hervé, Dumont, Annie, Garcia, Jean-Pierre, Garderes, P., Piana, Julienne, Trément, Frédéric, and Gilbert, Patrick
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[SHS.ENVIR] Humanities and Social Sciences/Environmental studies ,[SHS.GEO] Humanities and Social Sciences/Geography - Published
- 2015
16. The fate of Salicaceae seedlings related to the dynamics of alluvial bars during floods: differentiating bed erosion, uprooting and burying
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Wintenberger, Coraline, Rodrigues, Stéphane, Bréhéret, Jean-Gabriel, Jugé, Philippe, Villar, Marc, Université Francois Rabelais [Tours], Unité de recherche Amélioration, Génétique et Physiologie Forestières (AGPF), and Institut National de la Recherche Agronomique (INRA)
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[SDE.MCG]Environmental Sciences/Global Changes ,[SDE.ES]Environmental Sciences/Environmental and Society - Abstract
International audience; Riparian vegetation is a key factor of the morphological evolution of river. In Europe, riparian Salicaceae is declining following the loss of potential recruitment areas associated with river management. As an exception for lowland rivers, the Loire River (France) shows, in its middle reaches, an efficient sexual regeneration of Populus nigra and Salix alba on bare sediments deposited during flood events. In the literature, the influence of hydrological patterns as a key factor of the seedlings survival is well documented. Some studies focused on seedlings ability to withstand flood constraints and detailed the effect of duration and intensity of floods but few studies characterized precisely the processes applied on seedlings. As a working hypothesis, we consider that three types of flood stresses can induce mortality of seedlings: (i) uprooting by drag applied on the seedlings without sediment erosion, (ii) erosion of the recruited areas and (iii) burying. The distinction of these three processes allows identifying the importance of survival factors due to a strong sediment dynamics (e.g. erosion height > root height) or to the anchorage and resprouting ability. The main issues are: what are the governing processes (type and intensity) determining survival or death of seedlings and which factor (fluvial dynamics vs. own characteristics of seedlings) controls their survival? In-situ measurements were performed on a forced alluvial bar (20.000 m2) to detail the bar dynamics (bathymetry, topography, scour/fill processes, grain size surveys, flow velocity) and to survey the associated recruitment. On 48 plots (1.410 m2) the density, height and species (P. nigra and S. alba) were surveyed the year of recruitment (after dry period) and the next year after flood period. We highlight the following phases of processes during floods. The erosion of substrate dominates at the beginning of the rising limb. The erosion or uprooting processes depend of the balance between available bed shear stress and sediment size. Then the deposit occurs on the back of the bar before the peak discharge and protects them against uprooting by burying during the higher energy of flow. At the end of the falling limb, sediments are reworked, decreasing the burying height of seedlings and allowing possible uprooting (drag) or erosion of sediments.
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- 2014
17. Biosignatures on Mars: What, Where, and How? Implications for the Search for Martian Life
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Westall, Frances, primary, Foucher, Frédéric, additional, Bost, Nicolas, additional, Bertrand, Marylène, additional, Loizeau, Damien, additional, Vago, Jorge L., additional, Kminek, Gerhard, additional, Gaboyer, Frédéric, additional, Campbell, Kathleen A., additional, Bréhéret, Jean-Gabriel, additional, Gautret, Pascale, additional, and Cockell, Charles S., additional
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- 2015
- Full Text
- View/download PDF
18. Archean (3.33 Ga) microbe-sediment systems were diverse and flourished in a hydrothermal context
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Westall, Frances, primary, Campbell, Kathleen A., additional, Bréhéret, Jean Gabriel, additional, Foucher, Frédéric, additional, Gautret, Pascale, additional, Hubert, Axelle, additional, Sorieul, Stéphanie, additional, Grassineau, Nathalie, additional, and Guido, Diego M., additional
- Published
- 2015
- Full Text
- View/download PDF
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