Literatura académica sobre el tema "Dernière glaciation (MIS3 à 2)"
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Artículos de revistas sobre el tema "Dernière glaciation (MIS3 à 2)"
Painchaud, Alain, J. M. M. Dubois y Q. H. J. Gwyn. "Déglaciation et émersion des terres de l’ouest de l’île d’Anticosti, golfe du Saint-Laurent, Québec". Géographie physique et Quaternaire 38, n.º 2 (29 de noviembre de 2007): 93–111. http://dx.doi.org/10.7202/032545ar.
Texto completoLehmkuhl, Frank, Michael Klinge, Henrik Rother y Daniela Hülle. "Distribution and timing of Holocene and late Pleistocene glacier fluctuations in western Mongolia". Annals of Glaciology 57, n.º 71 (enero de 2016): 169–78. http://dx.doi.org/10.3189/2016aog71a030.
Texto completoGodbout, Julie y Jean Bousquet. "Les génomes du pin gris et du pin tordu, témoins des bouleversements climatiques passés". Foresterie 138, n.º 1 (6 de enero de 2014): 32–44. http://dx.doi.org/10.7202/1021041ar.
Texto completoHare, F. Kenneth. "Recent Climatological Research in Labrador Ungava". Cahiers de géographie du Québec 10, n.º 19 (12 de abril de 2005): 5–12. http://dx.doi.org/10.7202/020560ar.
Texto completoPrichonnet, Gilbert, Ghismond Martineau y Louis Bisson. "Les dépôts quaternaires de la région de Chibougamau, Québec". Géographie physique et Quaternaire 38, n.º 3 (29 de noviembre de 2007): 287–304. http://dx.doi.org/10.7202/032569ar.
Texto completoScourse, J. D. "The timing and magnitude of the British–Irish Ice Sheet between Marine Isotope Stages 5d and 2: implications for glacio‐isostatic adjustment, high relative sea levels and ‘giant erratic’ emplacement". Journal of Quaternary Science, 12 de marzo de 2024. http://dx.doi.org/10.1002/jqs.3611.
Texto completoTesis sobre el tema "Dernière glaciation (MIS3 à 2)"
Pallier, Céline. "De l’enregistrement sédimentaire en milieu karstique à la taphonomie des sites archéologiques du Paléolithique supérieur (MIS 3-MIS 2) : les apports de la grotte du Mas d’Azil et de la vallée de l’Arize (Pyrénées, France)". Electronic Thesis or Diss., Toulouse 2, 2021. http://www.theses.fr/2021TOU20011.
Texto completoThe Mas d'Azil cave, crossed by the Arize river, has preserved evidence of the hydrosedimentary dynamics of the last glacial cycle, which conditioned both human occupation during the Upper Palaeolithic and the conservation of archaeological remains. Thus, how can the study of such a sedimentary recorder answer the question of the archaeological gaps of the last ice age?Hiatuses, either chronological or spatial, are observed in the cave's occupations. What significance can be attributed to them : absence of humans or differential conservation? At the transition MIS 3-MIS 2, a phase of sedimentary aggradation has constrained occupation in the cave, while playing a major role in the conservation or erosion of the remains. It allowed the partial conservation of the Aurignacian levels that it covers, but made the cave inaccessible for several millennia. Finally, the geomorphological study allows a very precise reflection on the organisation of space, access and movement of the populations inside the cave during the recent Middle Magdalenian.The cave also provides information on the hydrosedimentary dynamics and paleoclimatic conditions on the scale of the Arize valley. The phenomena observed inside the cave have been recorded outside in a degraded way, but correlation hypotheses remain possible between the recordings in the cave and in the Arize valley. The Mas d'Azil cave is therefore a very high-resolution recorder of hydrosedimentary responses resulting from climatic fluctuations, particularly during the last glacial cycle. Through the archaeological evidence inserted in its geomorphological context, this cave underlines the importance of the differential taphonomy of the archaeological remains and makes it possible to interpret them, from the scale of the site to that of the valleys of the northern Pyrenean foothills