Auswahl der wissenschaftlichen Literatur zum Thema „Last glaciation (MIS3 à 2)“
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Zeitschriftenartikel zum Thema "Last glaciation (MIS3 à 2)"
Liakka, J., M. Löfverström und F. Colleoni. „The impact of the North American ice sheet on the evolution of the Eurasian ice sheet during the last glacial cycle“. Climate of the Past Discussions 11, Nr. 6 (10.11.2015): 5203–41. http://dx.doi.org/10.5194/cpd-11-5203-2015.
Der volle Inhalt der QuelleLiakka, Johan, Marcus Löfverström und Florence Colleoni. „The impact of the North American glacial topography on the evolution of the Eurasian ice sheet over the last glacial cycle“. Climate of the Past 12, Nr. 5 (25.05.2016): 1225–41. http://dx.doi.org/10.5194/cp-12-1225-2016.
Der volle Inhalt der QuelleVan Meerbeeck, C. J., H. Renssen und D. M. Roche. „How did Marine Isotope Stage 3 and Last Glacial Maximum climates differ? Perspectives from equilibrium simulations“. Climate of the Past Discussions 4, Nr. 5 (06.10.2008): 1115–58. http://dx.doi.org/10.5194/cpd-4-1115-2008.
Der volle Inhalt der QuelleVan Meerbeeck, C. J., H. Renssen und D. M. Roche. „How did Marine Isotope Stage 3 and Last Glacial Maximum climates differ? – Perspectives from equilibrium simulations“. Climate of the Past 5, Nr. 1 (05.03.2009): 33–51. http://dx.doi.org/10.5194/cp-5-33-2009.
Der volle Inhalt der QuellePloskov, A. N., A. V. Eliseev und I. I. Mokhov. „ENSEMBLE MODELLING OF ICE SHEET DYNAMICS IN THE LAST GLACIAL CYCLE“. Доклады Российской академии наук. Науки о Земле 510, Nr. 1 (01.05.2023): 99–105. http://dx.doi.org/10.31857/s2686739722602873.
Der volle Inhalt der QuelleZolnikov, I. D., I. C. Novikov, E. V. Deev, A. V. Panin und R. N. Kurbanov. „The Last Glaciation and Ice-Dammed Lakes in the South-East Altai“. Journal "Ice and snow" 63, Nr. 4 (01.10.2023): 639–51. http://dx.doi.org/10.31857/s207667342304018x.
Der volle Inhalt der QuelleLian, Olav B., und Stephen R. Hicock. „Lithostratigraphy and limiting optical ages of the Pleistocene fill in Fraser River valley near Clinton, south-central British Columbia“. Canadian Journal of Earth Sciences 38, Nr. 5 (01.05.2001): 839–50. http://dx.doi.org/10.1139/e00-103.
Der volle Inhalt der QuelleLehmkuhl, Frank, Michael Klinge, Henrik Rother und Daniela Hülle. „Distribution and timing of Holocene and late Pleistocene glacier fluctuations in western Mongolia“. Annals of Glaciology 57, Nr. 71 (Januar 2016): 169–78. http://dx.doi.org/10.3189/2016aog71a030.
Der volle Inhalt der QuelleGlushkova, O. Yu, und V. N. Smirnov. „Реконструкция масштабов и морфологических особенностей плейстоценовых оледенений на Северо-Востоке России“. Bulletin of the North-East Science Center, Nr. 2 (30.06.2021): 50–67. http://dx.doi.org/10.34078/1814-0998-2021-2-50-67.
Der volle Inhalt der QuelleShulmeister, James, Glenn D. Thackray, Tammy M. Rittenour und Olivia M. Hyatt. „Multiple glacial advances in the Rangitata Valley, South Island, New Zealand, imply roles for Southern Hemisphere westerlies and summer insolation in MIS 3 glacial advances“. Quaternary Research 89, Nr. 2 (22.02.2018): 375–93. http://dx.doi.org/10.1017/qua.2017.108.
Der volle Inhalt der QuelleDissertationen zum Thema "Last 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.
Der volle Inhalt der QuelleThe 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
Sandström, Sonja. „Central Asian ice-marginal moraines of the global last glacial maximum : An analysis of topographic features affecting the glaciation pattern in the Tian Shan and Altai mountains“. Thesis, Stockholms universitet, Institutionen för naturgeografi, 2018. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-155171.
Der volle Inhalt der QuelleCentral Asia Paleoglaciology Project
Buchteile zum Thema "Last glaciation (MIS3 à 2)"
Peterson, Jim A., S. Chandra und Christian Lundberg. „Landforms from the Quaternary glaciation of Papua New Guinea: an overview of ice extent during the Last Glacial Maximum“. In Developments in Quaternary Sciences, 313–19. Elsevier, 2004. http://dx.doi.org/10.1016/s1571-0866(04)80136-2.
Der volle Inhalt der QuelleRobinson, Beren W., und Dolph Schluter. „Natural Selection and the Evolution of Adaptive Genetic Variation in Northern Freshwater Fishes“. In Adaptive Genetic Variation In The Wild, 65–94. Oxford University PressNew York, NY, 2000. http://dx.doi.org/10.1093/oso/9780195121834.003.0003.
Der volle Inhalt der QuelleKonferenzberichte zum Thema "Last glaciation (MIS3 à 2)"
Solhjell, E., D. Moellenbeck, S. Yang und J. W. Lakeman. „Geotechnical Properties of Subglacial Till at Baltic Sea Offshore Wind Farm Sites“. In Offshore Technology Conference. OTC, 2024. http://dx.doi.org/10.4043/35172-ms.
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