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Journal articles on the topic 'Féodalité – France – Ardennes (France)'

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Published: 4 June 2021

Last updated: 1 February 2022

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1

Niort, Jean-François. "Aspects juridiques du régime seigneurial en Nouvelle-France." Revue générale de droit 32, no. 3 (January 20, 2015): 443–526. http://dx.doi.org/10.7202/1028080ar.

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Si l’on a abondamment traité du régime seigneurial canadien et souligné son importance, rares sont les études juridiques d’ensemble qui lui ont été consacrées. L’entreprise est difficile, notamment parce qu’elle se heurte à la notion de féodalité, susceptible de plusieurs acceptions. Si, en ce sens, le régime seigneurial en Nouvelle-France ne relève guère de la féodalité politique, qui est disparue en Métropole à l’époque de la colonisation, il s’inscrit dans la féodalité au sens d’organisation socio-économique instaurant des rapports de domination de cette nature entre le seigneur et les habitants. Or, ces rapports s’expriment juridiquement, essentiellement à travers la Coutume de Paris, applicable en Nouvelle-France, bien que complétée par une législation royale et locale spécifique. Il s’agit plus précisément des « droits seigneuriaux », et parmi ceux-ci les droits dits « utiles » (détenant une valeur économique). Ces droits seigneuriaux peuvent être distingués en fonction de leur nature plutôt « privée » (seigneurie foncière) ou « publique » (seigneurie banale), correspondant aux deux « facettes » de la seigneurie complète, l’aspect « public » étant le plus révélateur de la dimension fiscale du régime seigneurial, puisque les droits en relevant n’ont pas de fondement contractuel. Utilisant ce cadre de référence, on présentera les droits seigneuriaux en Nouvelle-France, en cherchant à souligner leurs spécificités vis-à-vis de leur modèle juridique d’origine. On étudiera donc successivement les droits seigneuriaux attachés à la seigneurie « foncière » (cens et rentes, « lods et ventes » ), puis ceux relevant de la seigneurie « banale » (droits de justice, de banalité, de pêche et de chasse), avant d’évoquer les droits « conventionnels » (droits de corvée, de retrait, ainsi que les servitudes et les réserves). On proposera finalement une réflexion sur la possibilité d’une synthèse générale du régime seigneurial canadien.

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2

SINTUBIN, Manuel, and Stefan HELSEN. "Conodont deformation in the Naux limestone (Ardennes, France)." Geologica Belgica 1, no. 1-4 (January 31, 1998): 41–48. http://dx.doi.org/10.20341/gb.2014.005.

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To date conodont deformation has rarely been applied in a quantitative strain analysis. Using the exceptional collection of deformed Pa (Platform) elements of Ozarkodina remscheidensis remscheidensis (Ziegler, 1960), sampled - without information about their in situ orientation - in the Gedinnian Naux Limestone (Ardenne, France), an attempt is made to use deformed conodont elements as strain markers. Preliminary results show that the strain, suffered by these conodont elements, is relatively low compared to strains measured in the adjacent pelitic and conglomeratic formations. Several deformation patterns can be recognised, indicating shortening or angular shear deformation. However, the applicability of deformed conodont elements as quantitative strain markers remains still to be proven, due mainly to the problem of determining their in situ orientation.

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3

van Viersen, Allart Philip. "New Middle Devonian trilobites from Vireux-Molhain (Ardennes, northern France)." Senckenbergiana lethaea 86, no. 1 (June 2006): 63–75. http://dx.doi.org/10.1007/bf03043635.

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4

Robion, Philippe, Catherine Kissel, Dominique Frizon de Lamotte, Jean Pierre Lorand, and Jean Claude Guézou. "Magnetic mineralogy and metamorphic zonation in the Ardennes Massif (France-Belgium)." Tectonophysics 271, no. 3-4 (April 1997): 231–48. http://dx.doi.org/10.1016/s0040-1951(96)00268-5.

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5

Thevenard, Frédéric, Marc Philippe, and Georges Barale. "Le delta hettangien de la Grandville (Ardennes, France): Étude paléobotanique et paléoécologique." Geobios 28, no. 2 (1995): 145–62. http://dx.doi.org/10.1016/s0016-6995(95)80221-5.

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6

Augot, D., D. Muller, J. M. Demerson, F. Boué, C. Caillot, and F. Cliquet. "Dynamics of Puumala virus infection in bank voles in Ardennes department (France)." Pathologie Biologie 54, no. 10 (December 2006): 572–77. http://dx.doi.org/10.1016/j.patbio.2006.07.039.

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7

Sauvage, F., C. Penalba, P. Vuillaume, F. Boue, D. Coudrier, D. Pontier, and M. Artois. "Puumala hantavirusInfection in Humans and in the Reservoir Host, Ardennes Region, France." Emerging Infectious Diseases 8, no. 12 (December 2002): 1509–11. http://dx.doi.org/10.3201/eid0812.010518.

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8

Afonso, Eve, Marie-Lazarine Poulle, Melissa Lemoine, Isabelle Villena, Dominique Aubert, and Emmanuelle Gilot-Fromont. "Prevalence of Toxoplasma gondii in small mammals from the Ardennes Region, France." Folia Parasitologica 54, no. 4 (December 1, 2007): 313–14. http://dx.doi.org/10.14411/fp.2007.041.

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9

Castel, Guillaume, Elodie Monchatre-Leroy, Marc López-Roig, Séverine Murri, Mathilde Couteaudier, Franck Boué, Denis Augot, et al. "Puumala Virus Variants Circulating in Forests of Ardennes, France: Ten Years of Genetic Evolution." Pathogens 10, no. 9 (September 9, 2021): 1164. http://dx.doi.org/10.3390/pathogens10091164.

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In Europe, Puumala virus (PUUV) transmitted by the bank vole (Myodes glareolus) is the causative agent of nephropathia epidemica (NE), a mild form of haemorrhagic fever with renal syndrome. In France, very little is known about the spatial and temporal variability of the virus circulating within bank vole populations. The present study involved monitoring of bank vole population dynamics and PUUV microdiversity over a ten-year period (2000–2009) in two forests of the Ardennes region: Elan and Croix-Scaille. Ardennes region is characterised by different environmental conditions associated with different NE epidemiology. Bank vole density and population parameters were estimated using the capture/marking/recapture method, and blood samples were collected to monitor the overall seroprevalence of PUUV in rodent populations. Phylogenetic analyses of fifty-five sequences were performed to illustrate the genetic diversity of PUUV variants between forests. The pattern of the two forests differed clearly. In the Elan forest, the rodent survival was higher, and this limited turn-over resulted in a lower seroprevalence and diversity of PUUV sequences than in the Croix-Scaille forest. Uncovering the links between host dynamics and virus microevolution is improving our understanding of PUUV distribution in rodents and the NE risk.

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10

Groves-Kirkby, C. J., A. R. Denman, P. S. Phillips, R. G. M. Crockett, and J. M. Sinclair. "Comparison of seasonal variability in European domestic radon measurements." Natural Hazards and Earth System Sciences 10, no. 3 (March 26, 2010): 565–69. http://dx.doi.org/10.5194/nhess-10-565-2010.

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Abstract. Analysis of published data characterising seasonal variability of domestic radon concentrations in Europe and elsewhere shows significant variability between different countries and between regions where regional data is available. Comparison is facilitated by application of the Gini Coefficient methodology to reported seasonal variation data. Overall, radon-rich sedimentary strata, particularly high-porosity limestones, exhibit high seasonal variation, while radon-rich igneous lithologies demonstrate relatively constant, but somewhat higher, radon concentrations. High-variability regions include the Pennines and South Downs in England, Languedoc and Brittany in France, and especially Switzerland. Low-variability high-radon regions include the granite-rich Cornwall/Devon peninsula in England, and Auvergne and Ardennes in France, all components of the Devonian-Carboniferous Hercynian belt.

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11

Buffetaut, Eric. "An early azhdarchid pterosaur from the Lower Cretaceous of the eastern Paris basin." Bulletin de la Société Géologique de France 183, no. 6 (December 1, 2012): 525–28. http://dx.doi.org/10.2113/gssgfbull.183.6.525.

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Abstract A pterosaur vertebra from the Early Cretaceous (Albian) Sables verts of Grandpré (Ardennes, northeastern France) is characterised by its elongation, its very low neural arch confluent with the centrum, and the presence of a tuba vertebralis. It is referred to the family Azhdarchidae and is one of the earliest well-attested records of this group. The pterosaur diversity of the Sables verts is higher than previously recognised.

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12

Vulin, Johann, Séverine Murri, Sarah Madrières, Maxime Galan, Caroline Tatard, Sylvain Piry, Gabriele Vaccari, et al. "Isolation and Genetic Characterization of Puumala Orthohantavirus Strains from France." Pathogens 10, no. 3 (March 16, 2021): 349. http://dx.doi.org/10.3390/pathogens10030349.

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Puumala orthohantavirus (PUUV) causes a mild form of haemorrhagic fever with renal syndrome (HFRS) called nephropathia epidemica (NE), regularly diagnosed in Europe. France represents the western frontier of the expansion of NE in Europe with two distinct areas: an endemic area (north-eastern France) where PUUV circulates in rodent populations, with the detection of many human NE cases, and a non-endemic area (south-western France) where the virus is not detected, with only a few human cases being reported. In this study, we describe the different stages of the isolation of two PUUV strains from two distinct French geographical areas: Ardennes (endemic area) and Loiret (non-endemic area). To isolate PUUV efficiently, we selected wild bank voles (Myodes glareolus, the specific reservoir of PUUV) captured in these areas and that were seronegative for anti-PUUV IgG (ELISA) but showed a non-negligible viral RNA load in their lung tissue (qRT-PCR). With this study design, we were able to cultivate and maintain these two strains in Vero E6 cells and also propagate both strains in immunologically neutral bank voles efficiently and rapidly. High-throughput and Sanger sequencing results provided a better assessment of the impact of isolation methods on viral diversity.

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13

Mulligan, Timothy, and Florian K. Rothbrust. "Guderian's XIXth Panzer Corps and the Battle of France: Breakthrough in the Ardennes, May 1940." German Studies Review 15, no. 1 (February 1992): 164. http://dx.doi.org/10.2307/1430072.

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14

Schaal, Caroline, and Henri-Georges Naton. "Contribution of archaeobotany to understand taphonomic phenomena. The case of a Preboreal palaeochannel of Autrecourt-et-Pourron (Ardennes, France)." BSGF - Earth Sciences Bulletin 192 (2021): 6. http://dx.doi.org/10.1051/bsgf/2021003.

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Palaeoecology, through the analysis of the interactions between environmental factors and ecosystems, refines the knowledge of the structuring process of plant communities and helps to understand the complexity of past environments. However, it is necessary to analyse the taphonomic phenomena (deposition, conservation, degradation) affecting plant macrofossil assemblages in order to perform relevant palaeoecological analyses. Indeed, plant macrofossils may be under or over-represented in carpological assemblages, depending on the resistance of their cell membranes and the sedimentary condition deposits. For this reason, it is necessary to estimate the representative quality of the conserved part as a source of information. Like all archaeological documents, the plant archives are distorted by the processes of formation of the sedimentary levels and, ignore the diagenetic history of the sedimentary layers could lead to wrong palaeoecological interpretations. To this aim, we analysed plant macrofossils contained in the wet sediments of a Meuse palaeochannel (Autrecourt-et-Pourron, Ardennes, France). This archaeobotanical study of an oxbow lake dated to the Preboreal (11.7–10.7 ka cal. BP), provides a reference of a taphonomic referential according to a hierarchy of organic remain preservations. This framework successfully helped the palaeoecological interpretations of the Autrecourt-et-Pourron off-site, and it has brought robustness to environmental history reconstruction of the early Holocene in the Ardennes Meuse.

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15

Saint-Martin, Caroline, Moustapha Dramé, Sandrine Dabakuyo, Lukshe Kanagaratnam, Patrick Arveux, and Claire Schvartz. "Overdiagnosis of thyroid cancer in the Marne and Ardennes Departments of France from 1975 to 2014." Annales d'Endocrinologie 78, no. 1 (February 2017): 27–32. http://dx.doi.org/10.1016/j.ando.2016.07.005.

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16

Saint-Martin, C., M. Dram, S. Dabakuyo, L. Kanagaratnam, P. Arveux, and C. Schvartz. "Over diagnosis of thyroid cancer in the Marne and Ardennes departments of France from 1975 to 2014." Annales d'Endocrinologie 77, no. 4 (September 2016): 263. http://dx.doi.org/10.1016/j.ando.2016.07.083.

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17

Méaudre, Jean-Charles, Vincent Le Quellec, Pierre-Marie Guihard, Guillaume Blanchet, and Florian Téreygeol. "Counterfeiting at Le Clos-Paul in Charleville-Mézières (Ardennes, France). Reconstruction trial of a complex chaîne opératoire." Journal of Archaeological Science: Reports 36 (April 2021): 102858. http://dx.doi.org/10.1016/j.jasrep.2021.102858.

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18

Xu, Changhai, Jean Louis Mansy, Peter Van Den Haute, Francois Guillot, Zuyi Zhou, Jun Chen, and Johan De Grave. "Late- and post-Variscan evolution of the Ardennes in France and Belgium: constraints from apatite fission-track data." Geological Society, London, Special Publications 324, no. 1 (2009): 167–79. http://dx.doi.org/10.1144/sp324.13.

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19

AUGOT, D., F. SAUVAGE, F. BOUE, M. BOULOY, M. ARTOIS, J. M. DEMERSON, B. COMBES, et al. "Spatial and temporal patterning of bank vole demography and the epidemiology of the Puumala hantavirus in northeastern France." Epidemiology and Infection 136, no. 12 (March 6, 2008): 1638–43. http://dx.doi.org/10.1017/s0950268808000423.

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SUMMARYEpidemiological data from bank voles,Myodes glareolus, naturally infected by the hantavirus Puumala (PUUV) were collected by a capture–mark–recapture protocol from 2000 to 2002 in the French department of Ardennes. Four monitored trapping sites were established in two forests located in two cantons (Flize and Monthermé). We captured 912 bank voles corresponding to 557 different individuals during 8820 trapping nights for an overall trapping success of 10·34%. The average PUUV seroprevalence was 22·4%. Characteristics of the system reported in North European countries are confirmed in France. PUUV seroprevalence and abundance of rodents appeared weakly linked. Adult voles were more frequently antibody-positive, but no difference between sexes was established. Anti-PUUV seropositive voles were captured and high seroprevalence was observed from both forests, without human infection reported in Flize canton during the study. One site among the four exhibited peculiar infection dynamics, where vole weight and infection risk were negatively correlated.

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20

Poupeau, François-Mathieu, and Fabien Schlosser. "La régulation de la filière bois énergie dans les Ardennes françaises." Articles 29, no. 2 (January 7, 2011): 3–28. http://dx.doi.org/10.7202/045153ar.

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Filière longtemps marginale, le bois énergie a connu une croissance vigoureuse depuis une dizaine d’années, soutenue par l’engagement de plus en plus actif de la France en faveur des énergies renouvelables. En prenant l’exemple du département des Ardennes, nous montrons dans cet article comment ce développement s’est accompagné d’un certain nombre de tensions, en partie nouvelles, qui, à défaut de mettre cette filière en péril, posent aujourd’hui question tant pour les entreprises du secteur que pour les pouvoirs publics. Ces tensions tournent, pour l’essentiel, autour de la mobilisation des ressources en bois. Alors qu’à sa création le bois énergie était conçu comme une activité d’appoint pour les scieurs, son développement récent l’a fait entrer dans une nouvelle ère, plus industrielle, qui nécessite l’accès à des ressources plus importantes et plus diversifiées. Il en résulte une concurrence accrue entre les usages du bois et un risque de « fuite » de cette matière première vers d’autres territoires, du fait notamment de la multiplication des projets. Ces tensions, qui sont aujourd’hui exacerbées par l’injonction à remplir les objectifs européens, placent les enjeux de connaissance et de partage de l’information au coeur de l’activité régulatrice de l’État.

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21

Barthélemy, Dominique. "La Théorie Féodale à l'Épreuve de L'Anthropologie (note critique)." Annales. Histoire, Sciences Sociales 52, no. 2 (April 1997): 321–41. http://dx.doi.org/10.3406/ahess.1997.279569.

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Un préjugé ancien dévalorise la « période féodale », c'est-à-dire la France et l'Europe des 10e et 11e siècles, ou à partir de « l'an mil ». Une théorie sous-jacente dissuade trop d'historiens, prétendument empiriques, d'y voir aucune sorte d'esprit public ou d'autorité régulatrice. De quoi surprendre et même choquer un esprit teinté d'anthropologie ! Et n'y a-t-il pas aussi quelque arbitraire dans les récits d'une édification de « l'État », aux 12e et 13e siècles, « par la féodalité », c'est-à-dire en récupérant ou détournant des principes réputés « féodaux » ? Il est bien temps ensuite, aux époques ultérieures, d'opposer les « résidus féodaux » à la « modernisation par l'État », dans les intrigues que l'on tisse ou les tableaux que l'on brosse… Le livre de Susan Reynolds détruit allègrement tout cela. On ne peut qu'applaudir tout d'abord, tant la critique est forte et convaincante. Mais on se demande ensuite si elle ne va pus trop loin.

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22

Lefèvre, David, Jean Heim, Etienne Gilot, and Jacques Mouthon. "Evolution des environnements sédimentaires et biologiques à l'Holocène dans la plaine alluviale de la Meuse (Ardennes, France). Premiers résultats." Quaternaire 4, no. 1 (1993): 17–30. http://dx.doi.org/10.3406/quate.1993.1987.

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23

Souffi, Bénédicte, Colas Guéret, Charlotte Leduc, Anne Gebhardt, Cécile Foucher, Sylvain Griselin, Caroline Hamon, Jacques Pélegrin, and Aurélie Salavert. "Nouvelles données chronoculturelles et palethnographiques sur le Mésolithique des VIIIe et VIe millénaires dans le Nord de la France : le site de « la Culotte » à Remilly-les-Pothées (Ardennes, France)." Bulletin de la Société préhistorique française 115, no. 3 (2018): 531–65. http://dx.doi.org/10.3406/bspf.2018.14922.

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24

Souffi, Bénédicte, Colas Guéret, Charlotte Leduc, Anne Gebhardt, Cécile Foucher, Sylvain Griselin, Caroline Hamon, Jacques Pélegrin, and Aurélie Salavert. "Nouvelles données chronoculturelles et palethnographiques sur le Mésolithique des VIIIe et VIe millénaires dans le Nord de la France : le site de « la Culotte » à Remilly-les-Pothées (Ardennes, France)." Bulletin de la Société préhistorique française 115, no. 3 (2018): 531–65. http://dx.doi.org/10.3406/bspf.2018.14922.

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25

Helsen, S., and P. Kønigshof. "Conodont thermal alteration patterns in Palaeozoic rocks from Belgium, northern France and western Germany." Geological Magazine 131, no. 3 (May 1994): 369–86. http://dx.doi.org/10.1017/s0016756800011122.

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AbstractIn this paper thermal patterns based on conodont Colour Alteration Indices (CAI) have been studied in the Devonian and Carboniferous rocks from Belgium, northern France and western Germany. Four maps (with the exception of the southeastern Rheinisches Schiefergebirge) have been compiled for the investigated area: one for the Eifelian and Givetian, a second for the Frasnian, another for the Famennian and one for the Tournaisian and Viséan. Conodonts have not been found in Cambrian rocks from Belgium and northern France and as they are scarce in the Ordovician to Lower Devonian formations of this area, it was impossible to integrate these CAI data into an isograd map. In Germany (in the eastern Rheinisches Schiefergebirge) only a few CAI values for the Lower Devonian strata are available. In contrast to the Ardennes where in general conodonts show CAI values of 3.0–5.0, indices in areas adjacent to the Anglo-Brabant Massif, e.g. in the western Namur Synclinorium and in the Eifel Hills, range between 1.5 and 2.0. Slightly higher values occur in the Campine Basin north of the Anglo-Brabant Massif. By comparison with CAI data from Belgium, conodont colour alteration indices from the same stratigraphic horizons in some areas of the northern and eastern Rheinisches Schiefergebirge are up to one index higher. In most areas of the Rheinisches Schiefergebirge the level of metamorphism corresponds to the anchizone. Regional variations in CAI data appear to be related to buried intrusions and associated hydrothermal activity. In the southeastern Rheinisches Schiefergebirge CAI data are not completely consistent but it is possible to discern an increase in coalification from the north to the south. High index values in the southern Rheinisches Schiefergebirge are believed to result from regional metamorphism and heating related to numerous intrusive bodies.

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Robion, Philippe, Dominique Frizon de Lamotte, Catherine Kissel, and Charles Aubourg. "Tectonic versus mineralogical contribution to the magnetic fabrics of epimetamorphic slaty rocks: an example from the Ardennes Massif (France-Belgium)." Journal of Structural Geology 17, no. 8 (August 1995): 1111–24. http://dx.doi.org/10.1016/0191-8141(95)00002-u.

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27

Grimm, Matthias C. "Frasnian inarticulate Brachiopoda of the Büdesheim Syncline (Eifel/Germany), of the Saxony Vogtland (Germany) and the Ardennes (Belgium and Northern France)." Senckenbergiana lethaea 77, no. 1-2 (April 1998): 73–85. http://dx.doi.org/10.1007/bf03043735.

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28

van Nieukerken, Erik J., Steve Wullaert, Bong-Woo Lee, and Rudolf Bryner. "Antispilina ludwigi Hering, 1941 (Lepidoptera, Heliozelidae) a rare but overlooked European leaf miner of Bistorta officinalis (Polygonaceae): new records, redescription, biology and conservation." Nota Lepidopterologica 44 (April 23, 2021): 99–121. http://dx.doi.org/10.3897/nl.44.63848.

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We record Antispilina ludwigi Hering, 1941 newly for France: Massif Central and Jura, Belgium: Ardennes and Switzerland: Jura and Alps, from many localities at middle elevations. All records were based on leafmines, often with larvae, in Snake-root, Bistorta officinalis Delarbre (Polygonaceae) and adults were reared from several localities. The species inhab its poor grasslands, moor habitats and heathland with relatively large hostplants. As the habitat is declining, and also other lepidopteran species feeding on this host are in decline, we expect that despite the new findings, this species is also declining and should preferably be monitored together with host specialist butterflies, such as Boloria eunomia (Esper, 1799) and Lycaena helle (Denis & Schiffermüller, 1775). During the period that the mines are present, the species is easy to record, even after the larvae have left the mines. The species is redescribed and diagnosed.

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29

Guislain, Marie-Hélène, Francis Raoul, Patrick Giraudoux, Marie-Eve Terrier, Guillaume Froment, Hubert Ferté, and Marie-Lazarine Poulle. "Ecological and biological factors involved in the transmission of Echinococcus multilocularis in the French Ardennes." Journal of Helminthology 82, no. 2 (June 2008): 143–51. http://dx.doi.org/10.1017/s0022149x08912384.

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AbstractIn order to identify the respective importance of the ecological and biological factors involved in the transmission of Echinococcus multilocularis, we estimated grassland vole intermediate host (Microtus sp. and Arvicola terrestris) population densities, in relation to the diet of the definitive host (red fox, Vulpes vulpes) and with the prevalence of E. multilocularis in the fox population. The study was conducted in the Ardennes, north-eastern France, which is an area with a high incidence of alveolar echinococcosis. Surface index methods showed that Microtus was the most abundant intermediate host in the area. Furthermore, Microtus was present in one-third of the 144 faeces and 98 stomach content samples examined and represented more than two-thirds of the rodent occurrences. Red fox predation on Microtus was significantly correlated with Microtus relative abundance. In contrast, the relative abundance of A. terrestris was very low. This species, as well as Clethrionomys glareolus and Apodemus sp., was little consumed. E. multilocularis prevalence in foxes was determined from carcasses and reached 53% (95% confidence interval 45–61%). Intensity of infection varied from 2 to 73,380 worms per fox, with 72% of the sampled worm burden harboured by 8% of the sampled foxes. The selected explanatory variables (sex, year, age class, health and nutritional condition, and season) failed to predict prevalence rate and worm burden. The high prevalence rate in foxes indicates the possibility of intense E. multilocularis transmission, apart from periods, or in landscapes, favourable to large population outbreaks of grassland rodents.

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Schaal, Caroline, Henri-Georges Naton, Pascale Ruffaldi, Salomé Granai, Guillaume Jamet, Olivier Brun, and Émilie Gauthier. "Palaeoecological response to Greenlandian (Early Holocene) climatic changes: Insight from an abandoned-channel sequence of the Meuse River at Autrecourt-et-Pourron (Ardennes, France)." Palaeogeography, Palaeoclimatology, Palaeoecology 557 (November 2020): 109937. http://dx.doi.org/10.1016/j.palaeo.2020.109937.

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31

Szaniawski, Rafal, Marek Lewandowski, Jean-Louis Mansy, Olivier Averbuch, and Frederic Lacquement. "Syn-folding remagnetization events in the French-Belgium Variscan thrust front as markers of the fold-and-thrust belt kinematics." Bulletin de la Société Géologique de France 174, no. 5 (September 1, 2003): 511–23. http://dx.doi.org/10.2113/174.5.511.

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Abstract New paleomagnetic studies have been carried out within the Ardennes segment of the N France - S Belgium Variscan fold-and-thrust belt to set constraints on the fold-thrust belt kinematics and reveal the casual relationships between vertical-axis rotations and major strike deviated zones localised along the general trend of the belt. Magnetite-bearing Devonian and Carboniferous limestones yielded two characteristic, secondary components of the natural remanent magnetization : a low temperature component recorded most probably during the late stages of folding and a high temperature component, acquired during incipient stages of deformation. Both post- and synfolding magnetizations were identified in the Lower Devonian hematite bearing sandstones. Ages of magnetization, inferred from the analysis of characteristic remanence inclinations compared to the reference curves for the stable parts of the Old Red Sandstones Continent (ORC), suggest the previous remagnetization event to be due to the burial of sedimentary rocks under the thick molassic foreland basin of Namurian-Westphalian age and the second to the final out-of-sequence activation of the thrust front in Stephanian times. Irrespective of the age of the magnetizations, orientations of paleomagnetic directions are dominantly governed by second-order structural trends. Clockwise rotations are observed in relatively narrow zones featuring deviated orientations of fold axes, other sites show paleomagnetic directions akin to those known from the ORC. We interpret this feature as a result of local transpressive deformations and related rotations, which occurred at lateral borders of propagating thrust-sheets. The latter deformation zones are suggested to be controlled by deep-seated discontinuities inherited from the Devonian Rheno-hercynian basin development. The Ardennes thrust belt was thus not rotated as a whole unit with respect to the ORC after the Namurian, preserving the initial orientation of the continental margin.

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Gibot-Leclerc, S., C. Reibel, and S. Legros. "First Report of Branched Broomrape (Phelipanche ramosa) on Celeriac (Apium graveolens) in Eastern France." Plant Disease 98, no. 9 (September 2014): 1286. http://dx.doi.org/10.1094/pdis-02-14-0148-pdn.

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Branched broomrape, Phelipanche ramosa (L.) Pomel (syn. Orobanche ramosa L.), is a chlorophyll-lacking, obligate root parasitic plant that infests Brassicaceae, Solanaceae, and legumes (3). In western France, P. ramosa has invaded oilseed rape fields since the 1990s, causing significant yield losses (1). This crop has now become the primary host for the parasite, along with buckwheat (Fagopyrum esculentum L.), hemp (Cannabis sativa L.), and tobacco (Nicotania tabacum L.). In September 2013, a field survey indicated that a celeriac (Apium graveolens L. var. Prinlz) crop on clay soil in the Champagne-Ardennes region (48°20′19″ N, 04°01′57″ E, 140 m above sea level, eastern France) was infested with branched broomrape where hemp had been grown 4 years before. The celeriac field was planted to wheat (Triticum aestivum L.) in 2012 in rotation with lentils (Lens culinaris Medik.) in 2011. About 2% of the total celeriac field was infested and the estimated yield losses were approximately 25% for this infested area. The host symptoms observed were a slower growth of celeriac, along with leaf chlorosis, lower fruit production, and numerous abortions. The infestation of the celeriac crop was confirmed by verifying the attachment of branched broomrape to the celeriac roots. Broomrape plant heights were between 4.5 and 21 cm. The stems were erect, branched, frail, rather hairy, and bulging. Scale leaves were limited to 4 to 10 mm long, thick, acuminate, alternate scales. The flowers were numerous (between 4 and 51) and were 8.3 to 14.5 mm long. They were borne in the axils of scaly bracts. They had an irregular, curved shape, and a light mauve color. They did not have distinct peduncles and were grouped in rather long floral scapes during advanced flowering. The corolla tube was 10 to 15 mm long and its restricted part stood higher than the divisions of the calyx. It had ciliate, if not hairy, lobes. The calyx was more or less hairy, zygomorphous, with four lobes, and 6 to 8 mm long. Two bracteoles were situated on either side of the calyx. The four stamens observed were didynamous and borne 4 to 5 mm above the corolla base. The dorsifixed bilocularis, longitudinally dehiscent anthers were glabrous or covered with a fine down along sutures. Georges Sallé, (retired) Professor of Botanics at the University Pierre et Marie Curie, Paris, confirmed the identity of P. ramosa based on morphological characteristics (1). Celeriac infection by branched broomrape was confirmed using a developed assay (2). P. ramosa infecting celeriac roots was described by counting the numbers of individuals having reached ontogenic stages according to Gibot-Leclerc et al. (2). To our knowledge, this is the first study reporting P. ramosa infection on celeriac in eastern France. Since celeriac is produced in rotation with lentils, branched broomrape could pose a serious threat to production of these crops. References: (1) M. Blamey and C. Grey-Wilson. La Flore d'Europe Occidentale. Edition Flammarion, Paris, 2003. (2) S. Gibot-Leclerc et al. Flora 207:512, 2012. (3) M. C. Press and G. K. Phoenix. New Phytol. 166:737, 2005.

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VAN VIERSEN, Allart P., Peter TAGHON, and Benedikt MAGREAN. "Early Middle Devonian trilobites and events in the Nismes – Vireux-Molhain area, southern border of the Dinant Synclinorium (Belgium, northern France)." Geologica Belgica 22, no. 1-2 (2019): 7–33. http://dx.doi.org/10.20341/gb.2019.001.

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Well-preserved trilobite specimens are recorded from Eifelian strata between the villages of Nismes (southern Belgium) and Vireux-Molhain (northern France). In the area of study the lower Eifelian Vieux Moulin Member of the Jemelle Formation crops out. The diversified trilobite associations of this unit occur in dark shales and siltstones during a deepening phase and replace the comparatively poorly diversified trilobite fauna of the underlying Eau Noire Formation. This overturn of the local trilobite fauna might, in part, be considered a regional expression of the globally recognised Choteč Event. A marked influx of exotic trilobites in the Vieux Moulin Member is provisionally referred to the local Vieux Moulin Event. Trilobite diversity peaked in the middle Eifelian part (Chavées Member) of the Jemelle Formation before drastically dropping in the upper part of this formation. The manifestations in the Ardennes of the eastern North American Bakoven and Stony Hollow Events can neither be confirmed nor rejected based on the currently available data. New taxa from the early Eifelian part of the Jemelle Formation in the area of study are Asteropyge boeckae sp. nov., Asteropyge eonia sp. nov., Asteropyge filoxenia sp. nov., Cyphaspis insolata sp. nov., Cyphaspis iuxta sp. nov., Diademaproetus pertinax sp. nov., Geesops icovellaunae sp. nov., Gerastos kesselaeri sp. nov., Kettneraspis eftychia sp. nov., Pedinopariops ceuthonymus sp. nov., Pedinopariops richterianus geminus ssp. nov., Scabriscutellum archinalae sp. nov., Septimopeltis akatastasia sp. nov. and Tropidocoryphe insciens sp. nov. Our material includes exceptionally rare, well-preserved specimens from the famous “Mur des douaniers” locality near Vireux-Molhain. Additionally, Astycoryphe rugocauda sp. nov. is described from the lower Eifelian Couvin Formation (southern Belgium) and Gerastos silvicultrix sp. nov. from the uppermost Emsian Heisdorf Formation (German Eifel).

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Thiry, Médard, Florence Quesnel, Johan Yans, Robert Wyns, Anne Vergari, Hervé Theveniaut, Régine Simon-Coinçon, et al. "Continental France and Belgium during the early Cretaceous: paleoweatherings and paleolandforms." Bulletin de la Société Géologique de France 177, no. 3 (May 1, 2006): 155–75. http://dx.doi.org/10.2113/gssgfbull.177.3.155.

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Abstract During the early Cretaceous, successive tectonic phases and several sea level falls resulted in the emersion of the main part of western Europe and the development of thick “lateritic” weathering. This long period of continental evolution ended with the Upper Cretaceous transgressions. During this period, the exposed lands displayed a mosaic of diverse morphologies and weathered landscapes. Bauxites are the most spectacular paleoweathering features, known for long in southern France. Recently, new residual outcrops have been identified, trapped in the karstic depressions of the Grands Causses. Other bauxitic formations, containing gibbsite, have also been recognised, occurring with the Clay-with-Jurassic-cherts in the southeastern border of the Paris Basin. These bauxitic formations overlay Jurassic limestone and are buried beneath Upper Cretaceous marine deposits. The recognition of bauxites up north into the southern Paris Basin significantly widens the extension of the Lower Cretaceous bauxitic paleolandscapes. On the Hercynian basements thick kaolinitic weathering mantles occur. They have been classically ascribed to the Tertiary. The first datings of these in situ paleosoils, by means of paleomagnetism and/or radiogenic isotopes, record especially early Cretaceous ages. This is the case for the “Siderolithic” formations on the edges of the French Massif Central, but also for the kaolinitic profiles in the Belgian Ardennes. In the Flanders, the Brabant basement is deeply kaolinised beneath the Upper Cretaceous cover. These paleosoils show polygenetic evolutions. The relief of these basement paleolandscapes may have been significant. There where probably high scarps (often of tectonic origin) reaching 200 m in elevation or beyond, as well as wide surfaces with inselbergs, as in the present day landscapes of tropical Africa and South America. On the Jurassic limestone platforms occur diverse kaolinitic and ferruginous weathering products. Around the Paris Basin they show various facies, ranging from kaolinitic saprolites to ferricretes. Due to the lack of sedimentary cover, the age of these ferruginous and kaolinitic weathering products has been debated for long, most often allocated to the Siderolithic sensu lato (Eocene-Oligocene). Recent datings by paleomagnetism have enabled to date them (Borne de Fer in eastern Paris Basin) back also to the early Cretaceous (130 ± 10 Ma). These wide limestone plateaus show karstified paleolandforms, such as vast closed and flat depressions broken by conical buttes, but also deep sinkholes in the higher areas of the plateaus and piedmonts. The depth of the karst hollows may be indicative of the range of relative paleoelevations. Dissolution holes display seldom contemporaneous karst fillings, thus implying that the karstland had not a thick weathering cover or that this cover had been stripped off before or by the late Cretaceous transgression. Nevertheless, some areas, especially above chert-bearing Jurassic limestone or marl, show weathering products trapped in the karst features or as a thick weathering mantle. In the Paris Basin, the Wealden gutter looked like a wide floodplain in which fluvio-deltaic sands and clays were deposited and on which paleosoils developed during times of non-deposition. The edges of the gutter were shaped as piedmonts linked up with the upstream basement areas. The rivers flowing down to the plain deposited lobes of coarse fluvial sands and conglomerates. The intensity of the weathering, the thickness of the profiles and their maturation are directly dependent on the duration of the emersion and the topographic location relative to the gutter. Near the axis of the gutter, where emersion was of limited duration, the paleoweathering features are restricted to rubefaction and argillization of the Lower Cretaceous marine formations. On the other hand, on the borders of the basin and on the Hercynian basement, where emersion was of longer duration, the weathering profiles are thicker and more intensively developed. The inventory of the Lower Cretaceous paleoweathering features shows the complexity of the continental history of this period. Moreover, the preserved weathering products are only a part of this long lasting period, all the aspects relative to erosion phases are still more difficult to prove and to quantify. In this domain, apatite fission tracks thermochronology (AFTT) can be helpful to estimate the order of magnitude of denudation. Residual testimonies and subsequent transgressions may enable to estimate relative elevations, but in return, we presently have no reliable tool to estimate absolute paleoelevations. In the work presented here, the inventory enabled to draw a continental paleogeographic map showing the nature of the weathering mantles and the paleolandscape features, just as paleoenvironments and paleobathymetry presently appear on marine paleogeographic maps. For the future, the challenge is to make progress in dating the paleoweathering profiles and especially in the resolution of these datings, in order to correlate precisely the continental records with the different events which trigger them (eustatism, climate, regional and global geodynamics). The final goal will be to build up a stratigraphic scale of the “continental geodynamic and climatic events” in parallel with “sequential stratigraphy” in the marine realm.

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Lacquement, F., O. Averbuch, J. L. Mansy, R. Szaniawski, and M. Lewandowski. "Transpressional deformations at lateral boundaries of propagating thrust-sheets: the example of the Meuse Valley Recess within the Ardennes Variscan fold-and-thrust belt (N France–S Belgium)." Journal of Structural Geology 27, no. 10 (October 2005): 1788–802. http://dx.doi.org/10.1016/j.jsg.2005.05.017.

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Narkiewicz, Katarzyna, and Pierre Bultynck. "The Upper Givetian (Middle Devonian) Subterminus Conodont Zone in North America, Europe and North Africa." Journal of Paleontology 84, no. 4 (July 2010): 588–625. http://dx.doi.org/10.1017/s0022336000058352.

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Late Givetian and early Frasnian conodont communities with Icriodus subterminus have been revised on the basis of collections from Iowa (USA), the Boulonnais and the Ardennes (northern France and Belgium), the Radom-Lublin area and Holy Cross Mountains (Poland), and the Ma'der-Tafilalt region (southeast Morocco). As a result an Icriodus subterminus Zone with a threefold subdivision is defined. The three subzones correspond approximately to the “Lower and Upper subterminus Fauna” and the “insita Fauna” commonly used in N America for the study of shallow-water platform carbonate successions.The base of the subterminus Zone corresponds to a level within the uppermost part of the hermanni Zone; the top is characterized by the occurrence of the earliest Ancyrodella taxa, Montagne Noire Zones MN 1 and the base of MN 2 or slightly above the base of the falsiovalis Zone.The diagnosis of Icriodus subterminus is amended and two morphotypes are recognized. The stratigraphic range of the alpha morphotype is confined to an interval between the uppermost part of the hermanni Zone and the top of the MN 3 Zone; the beta morphotype may range into the MN 6 Zone.The holotype of Icriodus subterminus from the North Liberty beds in Iowa is most likely a specimen that was reworked from the Cedar Valley Limestone. Icriodus cedarensis and Icriodus tafilaltensis are described as new species, and the diagnoses of Icriodus excavatus and Icriodus expansus are amended. Between the Icriodus difficilis and Icriodus symmetricus zones, an Icriodus expansus Zone is defined.

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Madrières, Sarah, Caroline Tatard, Séverine Murri, Johann Vulin, Maxime Galan, Sylvain Piry, Coralie Pulido, et al. "How Bank Vole-PUUV Interactions Influence the Eco-Evolutionary Processes Driving Nephropathia Epidemica Epidemiology—An Experimental and Genomic Approach." Pathogens 9, no. 10 (September 25, 2020): 789. http://dx.doi.org/10.3390/pathogens9100789.

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In Europe, Puumala virus (PUUV) is responsible for nephropathia epidemica (NE), a mild form of hemorrhagic fever with renal syndrome (HFRS). Despite the presence of its reservoir, the bank vole, on most of French territory, the geographic distribution of NE cases is heterogeneous and NE endemic and non-endemic areas have been reported. In this study we analyzed whether bank vole-PUUV interactions could partly shape these epidemiological differences. We performed crossed-experimental infections using wild bank voles from French endemic (Ardennes) and non-endemic (Loiret) areas and two French PUUV strains isolated from these areas. The serological response and dynamics of PUUV infection were compared between the four cross-infection combinations. Due to logistical constraints, this study was based on a small number of animals. Based on this experimental design, we saw a stronger serological response and presence of PUUV in excretory organs (bladder) in bank voles infected with the PUUV endemic strain. Moreover, the within-host viral diversity in excretory organs seemed to be higher than in other non-excretory organs for the NE endemic cross-infection but not for the NE non-endemic cross-infection. Despite the small number of rodents included, our results showed that genetically different PUUV strains and in a lesser extent their interaction with sympatric bank voles, could affect virus replication and diversity. This could impact PUUV excretion/transmission between rodents and to humans and in turn at least partly shape NE epidemiology in France.

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Buchsenschutz, Olivier. "Stéphane Verger, Rites et espaces en pays celte et méditerranéen. Étude comparée à partir du sanctuaire d’Acy-Romance (Ardennes, France) Rome, École française de Rome, «Collection de l’École française de Rome-276», 2000, 356 p." Annales. Histoire, Sciences Sociales 57, no. 3 (June 2002): 722–24. http://dx.doi.org/10.1017/s0395264900034880.

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Cirier, Aude. "Pierre Bonnassie (éd.). Fiefs et féodalité dans l’Europe méridionale (Italie, France du Midi, péninsule Ibérique) du Xe au XIIIe siècle. Actes du colloquede Conques, 6-8 juillet 1998. Toulouse, CNRS/Université de Toulouse-Le Mirail, «Méridiennes », 2002, 465 p." Annales. Histoire, Sciences Sociales 58, no. 6 (December 2003): 1393–94. http://dx.doi.org/10.1017/s0395264900022137.

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A. Orban, Myriam. "Des huguenots en Provence orientale (1558-1594)." Revue d'histoire du protestantisme 5, no. 2-3 (December 18, 2020): 181–96. http://dx.doi.org/10.47421/rhp5_2-3_181-196.

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Si l’engagement de la grande noblesse (les Guise, Bourbons, Montmorency, Coligny, Condé) dans les guerres de religion est relaté dans les livres d’histoire, la noblesse de second ordre est moins connue, et l’historiographie ignore largement les grands seigneurs de la Provence orientale qui adhérèrent à la Réforme. Parmi cette noblesse du sud-est de la France, et notamment celle possédant fiefs dans les actuels départements des Alpes-Maritimes, du Var et des Alpes-de-Haute-Provence, on peut citer des Castellane, des Oraison, des Grasse, des Grimaldi de Beuil, et des Villeneuve auxquels est consacrée cette étude. Dès 1550, les évêchés sont affaiblis par la simonie, les questions d’argent et les procès pour conserver leurs droits temporels. L’abbaye de Lérins, dont le rayonnement a décliné suite à la gestion calamiteuse sous le régime de la commende, est devenue un foyer calviniste. Des moines ont été chassés. Quelques évêques ont abjuré publiquement, d’autres sympathisent plus ou moins ouvertement avec les huguenots. Mais, le mouvement réformé ne prend véritablement racine au sein de la noblesse qu’à partir de 1559, avec la fin des guerres d’Italie et le retour des barons sur leurs terres. Certains ont été en contact avec les Allemands luthériens et en reviennent convertis à la doctrine de la « nouvelle foi ». Protégés par le gouverneur de Provence, Claude de Tende, les Grasse et les Lascaris, les Villeneuve ont entraîné parentèle, gentilshommes et notables et créé de petites communautés qui accueillent des pasteurs venus de Genève. Des partis se créent, qui brouillent la légendaire solidarité nobiliaire. Les guérillas mettent tout le pays à feu et à sang. En 1569, le baron de Vence Claude de Villeneuve, son frère Honoré de Villeneuve-Tourrettes-lès-Vence et son oncle Jean de Villeneuve-Thorenc acquièrent, lors d’enchères, des terres et les droits associés mise en vente par l’évêque Louis Grimaldi de Beuil afin de payer les décimes réclamées par la royauté pour subvenir aux guerres de religion. Il semble que leur arrière-pensée soit de reconstituer leur fief, ce qui assurerait, grâce à une alliance avec les Grasse et les Villeneuve-les-Fayence, un vaste territoire protestant. Lors de la guerre proprement provençale entre carcistes et razats, ils font de Saint-Martin-la-Pelote, Saint-Laurent-la-Bastide et le Canadel (notamment) des bastions fortifiés pour accueillir les protestants et leurs troupes. Ces guerres ont fait des ravages parmi les seigneurs. Beaucoup sont morts au combat, les autres se sont ruinés et n’ont plus les moyens d’entretenir un ministre réformé. Quand en 1589 Henri IV devient roi de France, de nombreux barons se soumettent à lui pour obtenir son pardon. Ils n’ont plus de soutien et les abjurations commencent. La fin des guerres de religion dans le sud-est provençal marque aussi celle de l’esprit de patriotisme provençal et celle de la féodalité politique et militaire, tandis que les évêques tridentins cherchent à récupérer les terres vendues par leurs prédécesseurs aux Villeneuve. Néanmoins, la Réforme protestante est bien établie dans une partie de la population. Au XVIIe siècle, les évêques des diocèses de Vence et de Grasse s’attachent lors de visites pastorales à repérer les protestants et à faire appliquer par les vicaires et les curés les préceptes de la Contre-Réforme.

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Stead, Ian. "J.-G. Rozoy. Les Celtes en Champagne: les Ardennes au second Age du Fer: le Mont Troté, les Rouliers. 1 Étude. 2 Description. 758 pages, 101 colour and 507 black-and-white illustrations, 167 tables. 1988 [1986-71]. Charleville-Mézières (Mémoires de la Société Archéologique Champenoise 4): ISBN 2-902788-10-X paperback 350FF (from J.-G. Rozoy, 26 rue du Petit-Bois, F 08000 Charleville-Mézières, France)." Antiquity 62, no. 236 (September 1988): 622. http://dx.doi.org/10.1017/s0003598x00075001.

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Stoddart, Simon. "Late Iron Age sacred space in western Europe - Alexander Smith. The differential use of constructed sacred space in southern Britain, from the late Iron Age to the 4th century AD (British Archaeological Reports British series 318). 278 pages, 25 figures, 79 maps. 2001. Oxford: Archaeopress; 1-84171-213-2 paperback £35. - Stéphane Verger (ed.). Rites et espaces en pays celte et méditerranéen: étude comparée à partir du sanctuaire d'Acy-Romance (Ardennes, France) (Collection de l'École française de Rome 276). i+357 pages, 130 figures, 6 tables. 2000. Rome: École française de Rome; 2-7283-0601-X (ISSN 0223-5099) paperback." Antiquity 76, no. 294 (December 2002): 1143–44. http://dx.doi.org/10.1017/s0003598x00092073.

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Audren, Frédéric. "L’ethnologie juridique au Collège de France : le cours de Jacques Flach sur les Institutions primitives (1892-1904)." Clio@Themis, no. 15 (March 30, 2021). http://dx.doi.org/10.35562/cliothemis.552.

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Cette contribution présente le cours sur les institutions primitives dispensé par l’historien du droit Jacques Flach au Collège de France entre 1892 et 1904. Elle insiste sur la singularité de son approche historique et comparative. Soucieux d’étudier les institutions en contexte, il propose une interprétation inédite de la féodalité, ambitionne d’écrire une histoire globale du droit et cherche à restituer l’altérité institutionnelle des sociétés primitives. Flach est ainsi l’un des premiers à enseigner en France l’anthropologie sociale et juridique.

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Hansmann, Yves, and Aurélie Velay. "TBE in France." Tick-borne encephalitis - The Book, May 24, 2021. http://dx.doi.org/10.33442/26613980_12b12-4.

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The first human case of tick-borne encephalitis virus (TBEV) infection in France was reported in 1968 in Alsace, an eastern region next to the German border: a gamekeeper working in a forest near Strasbourg.1 Between 1970 and 1974, an extensive research survey confirmed the presence of TBEV in ticks and rodents in this French region. Eight percent of adult tick batches collected were infected (Ixodes ricinus) by the TBEV. Tick collection occurred in a forest near Strasbourg, the main city in the region. Nymphs were more rarely infected (1.6% of the collected lots).1 These data were confirmed in 2011 in Alsace in Guebwiller’s Valley, a middle altitude forest, with identification of western (European) subtype TBEV (TBEV-EU). The infection rate still remains low: TBEV was detected only in the I. ricinus nymphs (2.48%) that were collected during May; however, not in those collected during the other spring or summer months. In a more recent study, Bestehorn et al., collected ticks (953 male, 856 female adult ticks and 2,255 nymphs) in endemic foci in the upper Rhine region in France and Germany between 2016, 2017 and 2018 by flagging2. The minimal infection rate (MIR) of the collected ticks in the Foret de la Robertsau (France) was estimated to 0,11% (1 nymph/944 ticks). The isolated and sequenced TBEV strain from Foret de la Robertsau (F) is related to circulating TBEV isolates from eastern Bavaria and the Czech Republic. In the French department Alsace, there are today at least two independent TBEV strains circulating: the historical Alsace strain isolated in 1971 and the newly identified strain from Foret de la Robertsau. Other wooded regions (Ardennes) were explored for TBEV in ticks, but without evidence of virus infection.

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BUFFETAUT, Eric, Bernard GIBOUT, and Danielle DROUIN. "A pterosaur from the Toarcian (Early Jurassic) of the Ardennes (northeastern France)." Carnets de géologie (Notebooks on geology), le (2010). http://dx.doi.org/10.4267/2042/32427.

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Goemaere, Eric, Cécile Millier, Pierre-Yves Declercq, Gilles Fronteau, and Roland Dreesen. "Legends of the Ardennes Massif, a Cross-Border Intangible Geo-cultural Heritage (Belgium, Luxemburg, France, Germany)." Geoheritage 13, no. 2 (March 13, 2021). http://dx.doi.org/10.1007/s12371-021-00549-9.

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Goemaere, Eric, Cécile Millier, Pierre-Yves Declercq, Gilles Fronteau, and Roland Dreesen. "Correction to: Legends of the Ardennes Massif, a Cross-Border Intangible Geo-cultural Heritage (Belgium, Luxemburg, France, Germany)." Geoheritage 13, no. 2 (April 6, 2021). http://dx.doi.org/10.1007/s12371-021-00556-w.

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RENAUD, Jean-Pierre, Jean-François PICARD, Claudine RICHTER, Arnaud LEGOUT, and Claude NYS. "Amendements calco-magnésiens et fonctionnement écologique : bilan des expériences conduites dans l’Est de la France (massif vosgien et Ardennes)." Revue Forestière Française, no. 3 (2009). http://dx.doi.org/10.4267/2042/30103.

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BUFFETAUT, Eric, Bernard GIBOUT, Isabelle LAUNOIS, and Claude DELACROIX. "The sauropod dinosaur Cetiosaurus OWEN in the Bathonian (Middle Jurassic) of the Ardennes (NE France): insular, but not dwarf." Carnets de géologie (Notebooks on geology), Livres (2011). http://dx.doi.org/10.4267/2042/43897.

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William C. Parcell1. "ABSTRACT: Correlation of Upper Jurassic Carbonate and Reef Facies Across the Burgundy and Ardennes Platforms, Eastern Paris Basin, France." AAPG Bulletin 86 (2002). http://dx.doi.org/10.1306/3fef4735-1741-11d7-8645000102c1865d.

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