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Academic literature on the topic 'Ichnologie – Cussac, Grotte de (Dordogne)'
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Journal articles on the topic "Ichnologie – Cussac, Grotte de (Dordogne)"
Jaubert, Jacques, Catherine Ferrier, Valérie Feruglio, et al. "La grotte de Cussac (Dordogne)." Les Nouvelles de l'archéologie, no. 154 (December 16, 2018): 16–24. http://dx.doi.org/10.4000/nda.5152.
Full textAujoulat, Norbert, Jean-Michel Geneste, Christian Archambeau, Marc Delluc, Henri Duday, and Dominique Gambier. "La grotte ornée de Cussac (Dordogne). Observations liminaires1." Paléo, no. 13 (December 14, 2001): 9–18. http://dx.doi.org/10.4000/paleo.919.
Full textAujoulat, Norbert, Jean-Michel Geneste, Christian Archambeau, Marc Delluc, Henri Duday, and Dominique Gambier. "La grotte ornée de Cussac - Le Buisson-de-Cadouin (Dordogne) : premières observations." Bulletin de la Société préhistorique française 99, no. 1 (2002): 129–37. http://dx.doi.org/10.3406/bspf.2002.12612.
Full textDissertations / Theses on the topic "Ichnologie – Cussac, Grotte de (Dordogne)"
Ledoux, Lysianna. "L’ichnologie préhistorique et les traces d’activités au sein des cavités ornées : les grottes de Fontanet (Ariège) et de Cussac (Dordogne)." Thesis, Bordeaux, 2019. http://www.theses.fr/2019BORD0010.
Full textTracks, which are among the most fragile and underestimated archaeological remains, represent a valuable source of information on site frequentation. In the past few years, they were widely studied in open air contexts. However, their analysis in caves, a context in which their study reached its peak between the 1970s and the early 2000s, is much less common. Recently, interest towards ichnology in subterranean environments re-emerged among prehistorians, and the study of tracks in several decorated caves was resumed. Our study is part of this dynamic and aims to contribute to research on tracks from the karst register and to participate in the renewal of the discipline in Prehistory. We study the footprints of the caves of Fontanet (Ariège) and Cussac (Dordogne), focusing firstly on their formation and conservation over time, and secondly on their contribution to the understanding of the subterranean environment appropriation by human in the Palaeolithic.Through observations, inventories, in situ measurements and ex situ work based on three-dimensional imaging tools, we conducted a morphological and morphometric study of fossil tracks. In addition, we have developed an experimental approach to understand the various factors that may have influenced the morphology of footprints at the time of their formation and since their formation. This multidisciplinary and interdisciplinary approach makes it possible to affirm the uniqueness of the Fontanet and Cussac caves from an ichnological, archaeological and geomorphological point of view and at the same time reveals similar behaviours that can be found throughout the Paleolithic period. The profile of individuals who have frequented these two cavities gradually takes shape. We propose several hypotheses concerning their behaviour and activities in this confined and naturally constraining space and contribute to the discussions relating to the function of these two cavities
Peyraube, Nicolas. "Apports des équilibres calco-carboniques et du carbone 13 pour l’étude de l’air et des écoulements d’eau dans la zone non saturée du karst : application au système karstique perché de la grotte de Cussac (Dordogne, France)." Thesis, Bordeaux 1, 2011. http://www.theses.fr/2011BOR14283/document.
Full textThe protection of Cussac engraved cave, discovered in 2000, is based upon the comprehension of itsrelationship with the karstic system and flow conditions in the unsaturated zone (UZ) understanding.Cussac site gives access to several springs from different parts of the UZ and a small saturated area.The cave itself is accessible and allows interception of flow inside the karst environment. Aerologicparameters including CO2 partial pressure (pCO2) and temperature of the cave have been monitoredsince 2003 to build a simple model of its relations with external atmosphere air and UZ air.A first part of the work is dedicated to the characterisation of the flows by a monitoring since 2008 ofwater chemistry and dynamics. This part lead to a Cussac perched aquifer functioning general scheme.To complete these classical investigations we wished to define hydrologic and aerologic flows in karstaquifers using one of its specificity: interdependency of gaseous, liquid and solid phases.Exchanges between rock, water and pCO2 of the UZ are estimated using calco-carbonic equilibriumequations. Functioning scheme is enriched by a conceptual view of flow conditions and a localisationin the karst of the CO2 dissolution or evasion and carbonate dissolution or precipitation process.Precisions on pCO2 evolution in UZ and in the particular environment of the cave are given by d13C.Unsaturated Zone CO2 isotopic composition is estimated from d13C measurement in water. This needto take in account total dissolved inorganic carbon variations process