Relevant bibliographies by topics / Glaciations du Quaternaire

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Glaciations du Quaternaire'

Author: Grafiati
Published: 4 June 2021
Last updated: 2 February 2022

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Journal articles on the topic "Glaciations du Quaternaire"

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Delmas, Magali, Marc Calvet, Yanni Gunnell, Régis Braucher, and Didier Bourlès. "Les glaciations quaternaires dans les Pyrénées ariégeoises : approche historiographique, données paléogéographiques et chronologiques nouvelles." Quaternaire, no. 23/1 (March 1, 2012): 61–85. http://dx.doi.org/10.4000/quaternaire.6091.

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Lebuis, J., and P. P. David. "La stratigraphie et les événements du Quaternaire de la partie occidentale de la Gaspésie, Québec." Dynamique et paléogéographie de l’inlandsis laurentidien 31, no. 3-4 (2011): 275–96. http://dx.doi.org/10.7202/1000278ar.

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Une cartographie des dépôts meubles de la Gaspésie a permis d’identifier des unités lithostratigraphiques dont les noms formels sont proposés. Il existe des preuves pour deux glaciations distinctes représentées par des tills séparés par des intervalles de sédiments glacio-lacustres. La dernière glaciation a subi une inversion du sens de l’écoulement glaciaire et a permis la mise en place d’un troisième till, auquel est associé un diamicton glacio-marin déposé lors du vêlage des glaciers dans l’estuaire du Saint-Laurent. Enfin un quatrième till est dû à l’activité de calottes glaciaires confiné
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Hétu, Bernard, and James T. Gray. "Le modelé glaciaire du centre de la Gaspésie septentrionale, Québec." Géographie physique et Quaternaire 39, no. 1 (2007): 47–66. http://dx.doi.org/10.7202/032584ar.

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RÉSUMÉLe relief du centre de la Gaspésie septentrionale a grandement été modifié au cours des événements glaciaires du Quaternaire, mais l'érosion glaciaire s'est montrée très sélective. Les éléments du paysage les plus touchés sont les vallées et, dans une moindre mesure, les escarpements séparant les plateaux. Les vallées ont été surcreusées dans leur partie aval, parfois même sous le niveau de la mer. De plus, elles ont été calibrées et élargies, ce qui s'est traduit par l'apparition de parois abruptes, d'éperons tronqués et de vallées affluentes suspendues. Par ailleurs, la majorité des va
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Stauch, Georg, and Frank Lehmkuhl. "Quaternary glaciations in the Verkhoyansk Mountains, Northeast Siberia." Quaternary Research 74, no. 1 (2010): 145–55. http://dx.doi.org/10.1016/j.yqres.2010.04.003.

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AbstractGeomorphological mapping revealed five terminal moraines in the central Verkhoyansk Mountains. The youngest terminal moraine (I) was formed at least 50 ka ago according to new IRSL (infrared optically stimulated luminescence) dates. Older terminal moraines in the western foreland of the mountains are much more extensive in size. Although the smallest of these older moraines, moraine II, has not been dated, moraine III is 80 to 90 ka, moraine IV is 100 to 120 ka, and the outermost moraine V was deposited around 135 ka. This glaciation history is comparable to that of the Barents and Kar
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Fulton, R. J., E. Irving, and P. M. Wheadon. "Stratigraphy and paleomagnetism of Brunhes and Matuyama (>790 ka) Quaternary deposits at Merritt, British Columbia." Canadian Journal of Earth Sciences 29, no. 1 (1992): 76–92. http://dx.doi.org/10.1139/e92-009.

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A succession of Quaternary deposits in the Merritt basin of south-central British Columbia contains evidence for four glaciations and two interglaciations. Paleomagnetic signatures in these sediments are of three types: normal polarity, proposed to have been acquired during the Brunhes Normal Polarity Chron; reversed polarity, proposed to have been acquired during the Matuyama Reversed Polarity Chron; and reversed polarity (Matuyama age) all but obscured by a normally magnetized overprint (Brunhes age).Reversely magnetized deposits at the base of the succession include glacial lacustrine depos
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Ramadhin, Christine, and Chuixiang Yi. "ESD Ideas: Why are glaciations slower than deglaciations?" Earth System Dynamics 11, no. 1 (2020): 13–16. http://dx.doi.org/10.5194/esd-11-13-2020.

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Abstract. The Earth's climate during the Quaternary is dominated by short warm interglacials and longer cold glaciations paced by external forcings such as changes in insolation. Although not observed in the solar radiation changes, the time series of the cycles display asymmetry since transitions to full glacial conditions are slower than the termination of glaciations. Here an idea is proposed for the slower transition by identifying and describing two negative sea ice feedbacks dominant during the glaciation process that could serve as a control on the intermediate stage and decrease the pa
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Dortch, Jason M., Lewis A. Owen, and Marc W. Caffee. "Quaternary glaciation in the Nubra and Shyok valley confluence, northernmost Ladakh, India." Quaternary Research 74, no. 1 (2010): 132–44. http://dx.doi.org/10.1016/j.yqres.2010.04.013.

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AbstractThree glacial stages (Deshkit 1, Deshkit 2 and Dishkit 3 glacial stages) are identified in the Nubra and Shyok valleys in northernmost Ladakh, northwest India, on the basis of geomorphic field mapping, remote sensing, and 10Be terrestrial cosmogenic nuclide surface exposure dating. The glacial stages date to ∼ 45 ka (Deshkit 1 glacial stage), ∼ 81 ka (Deshkit 2 glacial stage) and ∼ 144 ka (Deshkit 3 glacial stage). A mean equilibrium line altitude depression of ∼ 290 m for the Deshkit 1 glacial stage was calculated using the area accumulation ratio, toe-to-headwall ratio, area–altitude
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Barendregt, R. W., J. S. Vincent, E. Irving, and J. Baker. "Magnetostratigraphy of Quaternary and late Tertiary sediments on Banks Island, Canadian Arctic Archipelago." Canadian Journal of Earth Sciences 35, no. 2 (1998): 147–61. http://dx.doi.org/10.1139/e97-094.

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Sediments approximately 50 m thick from Banks Island (Canadian Arctic Archipelago) contain one of the longest terrestrial records of Pleistocene climate changes in North America. Samples have been obtained from 126 horizons distributed among four localitites, of which 116 horizons yielded acceptable paleomagnetic data. In sediments of the Matuyama Reversed Zone, there are recorded at least two and possibly as many as five full continental glaciations, two interglacial intervals, and a nonglacial interval at the beginning which is considered preglacial. Subzones attributable to the Olduvai and
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Locke, William W. "The late Quaternary geomorphic and paleoclimatic history of the Cape Dyer area, easternmost Baffin Island, N.W.T." Canadian Journal of Earth Sciences 24, no. 6 (1987): 1185–98. http://dx.doi.org/10.1139/e87-114.

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The Cape Dyer area of easternmost Baffin Island was isolated from the Laurentide Ice Sheet by the fiords of Cumberland Peninsula. Accordingly, the glacial chronology at Cape Dyer is that of local ice only and is indicative of the local climate throughout the late Quaternary. Six drift units, representing three periods of restricted glaciation and three of expanded glaciation, are present. Beyond the most distal drift is an area that has not been modified by glaciation.The expanded glaciations were dated through correlation on the bases of moraine morphology, soil development, and amino-acid ra
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DOTSENKO, Valeriy, and Ibragim KERIMOV. "ABOUT THE REASONS OF CLIMATE WARMING BASED ON STUDYING THE HISTORY OF QUATERNARY GLACIOSES OF THE CAUCASUS (ON THE EXAMPLE OF THE INTERDURCHIE TEREK AND THE ANDIAN KOISU)." Sustainable Development of Mountain Territories 12, no. 3 (2020): 461–71. http://dx.doi.org/10.21177/1998-4502-2020-12-3-461-471.

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The Greater Caucasus experienced repeated glaciation during the Quaternary (early, middle, upper Pleistocene, late Glacial, and late Holocene), which occurred under changing climatic conditions and differentiated tectonic movements. These glaciations, of course, are associated with changes in terrain, the formation of new deposits, transgressions and regressions of the Caspian Sea, changes in vegetation and soil types, so the problem of glaciation affects all earth Sciences to varying degrees. The study of Quaternary glaciation, especially Holocene glaciation, is currently relevant for underst
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Dissertations / Theses on the topic "Glaciations du Quaternaire"

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Delmas, Magali. "Chronologie et impact géomorphologique des glaciations quaternaires dans l'est des Pyrénées." Phd thesis, Université Panthéon-Sorbonne - Paris I, 2009. http://tel.archives-ouvertes.fr/tel-00519194.

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L'objectif de cette étude est d'évaluer la part de l'empreinte glaciaire dans les paysages de la haute montagne aux latitudes moyennes. Peut-on transposer au Quaternaire la très grande efficacité de l'érosion glaciaire mesurée actuellement dans certaines montagnes et faire de cet agent le principal acteur de la morphogenèse ? Doit-on au contraire constater une forte résilience des paléoformes tertiaires et donc la faiblesse relative de l'érosion glaciaire ? Le domaine est-pyrénéen offre un terrain privilégié en raison du fort contraste nord-sud qui caractérise l'emprise spatiale et l'impact gé
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Delmas, Magali Danielle. "Chronologie et impact géomorphologique des glaciations quaternaires dans l'est des Pyrénées." Paris 1, 2009. http://www.theses.fr/2009PA010644.

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L'objectif de cette étude est d'évaluer la part de I'empreinte glaciaire dans les paysages de la haute montagne aux latitudes moyennes. Le domaine est-pyréneen offre un terrain privilégié en raison du fort contraste qui caractérise I'emprise spatiale et I'impact géomorphologique des paléoenglacements quaternaires. Deux axes de recherche complémentaires structurent ce travail. Le premier concerne la chronologie et la paléogéographie des glaciations quaternaires. La production de 81 datations lOBe fournissent une nouvelle vision du cycle würmien et contribuent au débat sur le caractère synchrone
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Ducassou, Emmanuelle. "Évolution du système turbiditique profond du Nil au cours du Quaternaire récent." Bordeaux 1, 2006. http://www.theses.fr/2006BOR13263.

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Ce travail, basé sur l’analyse et l’interprétation de prélèvements (carottes kullenberg et calypso) calibrées avec des données acoustiques (sismique 3,5 kHz et multifaisceaux), propose une reconstruction du fonctionnement sédimentaire récent (derniers 250 ka) du système turbiditique profond du Nil (STPN). Pour cela, une étude stratigraphique détaillée et basée sur plusieurs outils a été nécessaire pour dater des séries sédimentaires riches en événements gravitaires et s’étendant sur plusieurs cycles glaciaire/interglaciaire. C’est l’établissement d’une écostratigraphie basée sur les assemblage
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Smyčka, Jan. "Origine évolutive et diversification de la flore des montagnes européennes." Thesis, Université Grenoble Alpes (ComUE), 2019. https://thares.univ-grenoble-alpes.fr/2019GREAV031.pdf.

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Les biotas de montagne à travers le monde sont riches en espèces, mais aussi en espèces endémiques, ce qui suggère que des processus spécifiques de diversification et de survie ont été impliqués dans leur formation. Dans ma thèse, je me concentre sur la dynamique et les moteurs de la diversification végétale dans les montagnes européennes - un système montagneux qui n'est pas l'un des points chauds de la diversité les plus riches du monde, mais qui est remarquablement riche dans le contexte régional, surtout étant donné son histoire glaciaire récente. On a beaucoup écrit sur la diversification
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Pawley, Steven Michael. "Quaternary Glaciations of North and West Norfolk." Thesis, Royal Holloway, University of London, 2006. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.430784.

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Benabdellouahed, Massinissa. "La Seine fluviatile plio-quaternaire en baie de Seine : évolution morphologique et sédimentaire (rôle du substratum géologique et des cycles climato-eustatiques)." Phd thesis, Université de Caen, 2011. http://tel.archives-ouvertes.fr/tel-00660489.

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La baie de Seine forme aujourd'hui une vaste dépression marine d'environ 5 000 km 2 , située entre la Manche centrale au Nord, le Cotentin à l'Ouest et le Bassin parisien au Sud et à l'Est. Les nouvelles données sismiques THR (2007-2009) couplées aux données de dragages (2009) acquises en baie de Seine pour la thèse, ont permis de réviser la carte géologique du substratum de la Baie de Seine, d'établir les liens entre ce substratum et la Seine périglaciaire plio-quaternaire et de proposer pour cette dernière un nouveau modèle de dépôt et d'évolution. Le substratum géologique de la baie de Sein
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Rae, Alaric Campbell. "Late Quaternary glaciation in Southwest Ireland." Thesis, Coventry University, 2004. http://curve.coventry.ac.uk/open/items/03055be6-aad0-4313-d72e-1dac2156f221/1.

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During the last main phase of glaciations (26-13kaBP) an ice cap developed in south west Ireland and ice, from a dispersal centre in the vicinity of Kenmare, flowed north and diverged on the southern slopes of the Macgillycuddy’s Reeks. On these slopes, a weathering limit separates ice-moulded bedrock, on low ground, from frost-weathered terrain above. Assessment of bedrock dilation joint characteristics, Schmidt hammer R-value data, clay-sized mineral contents and magnetic properties of basal soil samples confirms significant contrasts in the degree of weathering above and below this limit. T
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Hein, Andrew S. "Quaternary glaciations in the Lago Pueyrredón Valley, Argentina." Thesis, University of Edinburgh, 2009. http://hdl.handle.net/1842/3858.

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This thesis develops a better knowledge of the extent and timing of glaciations in southern Argentina throughout the Quaternary. It provides a detailed understanding of successive major glacial outlet lobes in the Lago Pueyrredón valley. The glacial and glaciofluvial deposits in the valley, as elsewhere in the region, are extremely well-preserved and reflect punctuated glacial advances between ~ 1.1 Ma and ~ 17 ka. Several intermediate glaciations are undated, constrained by the limited time frame of radiocarbon age dating, the limited potential volcanic sites for K-Ar or 40Ar/39Ar age dating,
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Demory, François. "Paleomagnetic dating of climatic events in Late Quaternary sediments of Lake Baikal (Siberia)." Phd thesis, Universität Potsdam, 2004. http://opus.kobv.de/ubp/volltexte/2005/181/.

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Der Baikalsee ist ein ideales Klimaarchiv für die Mitte Eurasiens. In dieser Arbeit wurde gesteinsmagnetische und paleomagnetische Analysen an hemipelagischen Sequenzen von vier Lokationen analysiert. Die Kerne erreichen ein Alter von maximal 300 ky. In Kombination mit TEM, XRD, XRF und geochemischen Analysen zeigt die gesteinsmagnetische Studie, dass detritischer Magnetit das magnetische Signal der glazialen Sedimente dominiert. Die magnetischen Signale der interglazialen Sedimente wurden durch diagenetische Prozesse verändert. Mittels HIRM können Hämatit und Goethit quantifiziert werden. Di
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Hughes, Philip David. "Quaternary glaciation in the Pindus Mountains, Northwest Greece." Thesis, University of Cambridge, 2004. https://www.repository.cam.ac.uk/handle/1810/273442.

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Geomorphological and geological evidence for former Quaternary glaciation has been mapped n the Pindus Mountains of Northwest Greece. the dynamics and chronology of glaciation in this area has been established through sedimentological analysis, soil analysis and Uranium-series dating. Four glacial events are recorded in the sedimentological and geomorphological records. The more extensive recorded glaciation pre-dates 350,000 years BP and was characterised by extensive valley glaciers and ice-fields. A second glaciation occurred prior to the last interglacial, before <i>ca</i>. 127,000 years B
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Books on the topic "Glaciations du Quaternaire"

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Quaternary glaciations - extent and chronology: A closer look. Elsevier, 2011.

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Weidick, Anker. Quaternary glaciation history and glaciology of Jakobshavn Isbrae and the Disko Bugt region, West Greenland: A review. Geological Survey of Denmark and Greenland, 2007.

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1948-, Ehlers Jürgen, and Gibbard Philip L. 1949-, eds. Quaternary glaciations: Extent and chronology. Elsevier, 2004.

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Quaternary glaciations in the southern hemisphere. Pergamon, 1990.

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Memoirs on Quaternary glaciation in China. Geological Pub. House, 1991.

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-. Quaternary Glaciation in the Mediterranean Mountains. Geological Society, 2017.

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Quaternary Glaciations - Extent and Chronology - A Closer Look. Elsevier, 2011. http://dx.doi.org/10.1016/c2009-0-20217-0.

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Gibbard, P. L., and J. Ehlers. Quaternary Glaciations - Extent and Chronology, Volume 2: Part I: Europe (Developments in Quaternary Sciences). Elsevier Science, 2004.

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Gibbard, P. L., and J. Ehlers. Quaternary Glaciations - Extent and Chronology, Volume 2: Part II: North America (Developments in Quaternary Sciences). Elsevier Science, 2004.

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Quaternary Glaciations Extent and Chronology - Part III: South America, Asia, Africa, Australasia, Antarctica. Elsevier, 2004. http://dx.doi.org/10.1016/s1571-0866(04)x8106-9.

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Book chapters on the topic "Glaciations du Quaternaire"

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Ehlers, Jürgen, and Philip Gibbard. "Quaternary Glaciation." In Encyclopedia of Earth Sciences Series. Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2642-2_423.

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Zhou, Shangzhe, Jijun Li, Jingdong Zhao, Jie Wang, and Jingxiong Zheng. "Quaternary Glaciations." In Developments in Quaternary Sciences. Elsevier, 2011. http://dx.doi.org/10.1016/b978-0-444-53447-7.00070-2.

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Seltzer, Geoffrey O. "Late Quaternary Glaciation of the Tropical Andes." In The Physical Geography of South America. Oxford University Press, 2007. http://dx.doi.org/10.1093/oso/9780195313413.003.0011.

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The effects of climate change are intrinsic features of Earth’s landscapes, and South America is no exception. Abundant evidence bears witness to the changes that have shaped the continent over time—from the glacial tillites inherited from late Paleozoic Gondwana to recent terrigenous sediments and life forms trapped in alluvial, lacustrine, and nearby marine deposits. Preeminent among this evidence are the landforms and sediments derived from the late Cenozoic glaciations of the Andes, which have been the focus of so much recent and ongoing research. Because South America has long been a mainly tropical and subtropical continent, most of it escaped the direct effects of these glaciations. Nevertheless, portions of the continent extend sufficiently far poleward and rise high enough to attract snowfall and promote glaciers today. Glaciers were more emphatically present during Pliocene and Pleistocene cold stages, and it is their legacies that provide information about the changing environments of those times, and more especially of the past 30,000 years. There is evidence for glaciation in the tropical and extratropical Andes as early as Pliocene time (Clapperton, 1993). In southern South America, along the eastern side of the Patagonian Andes, Mercer (1976) dated a series of basalts interbedded with glacial tills that suggest multiple glacial advances after ~3.6 Ma (million years before present). In the La Paz Valley, Bolivia, volcanic ashes dated by K/Ar (potassium/argon) methods are interbedded with glacial tills indicative of at least two phases of glaciation in the late Pliocene, at 3.27 and 2.20 Ma (Clapperton, 1979, 1993). This evidence for early glaciation in disparate parts of the Andes indicates that portions of the cordillera were high enough and climatic variations were great enough in the Pliocene for glaciers to form long before the cold episodes of the Pleistocene. Glacial deposits in Ecuador, Perú, and Bolivia provide evidence for climate variability in tropical South America in the recent geological past. In the late Pleistocene, glacier equilibrium-line altitudes were as much as 1,200 m lower than they are today on the eastern slopes of the Andes, indicative of a significant depression in mean annual temperature in the tropics at maximum glaciation (e.g., Klein et al., 1999).
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Ehlers, J., V. Astakhov, P. L. Gibbard, Ó. Ingólfsson, J. Mangerud, and J. I. Svendsen. "GLACIATIONS | Early Quaternary." In Encyclopedia of Quaternary Science. Elsevier, 2007. http://dx.doi.org/10.1016/b0-44-452747-8/00123-x.

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Assine, Mario Luis, and Lucas Verissimo Warren. "Pre-Quaternary Glaciations." In Encyclopedia of Geology. Elsevier, 2021. http://dx.doi.org/10.1016/b978-0-12-409548-9.12497-2.

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Ehlers, J., V. Astakhov, P. L. Gibbard, J. Mangerud, and J. I. Svendsen. "GLACIATIONS | Late Pleistocene Glaciations in Europe." In Encyclopedia of Quaternary Science. Elsevier, 2007. http://dx.doi.org/10.1016/b0-44-452747-8/00127-7.

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Ehlers, J., and P. L. Gibbard. "GLACIATIONS | Overview." In Encyclopedia of Quaternary Science. Elsevier, 2013. http://dx.doi.org/10.1016/b978-0-444-53643-3.00128-x.

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Ehlers, J., and P. L. Gibbard. "GLACIATIONS | Overview." In Encyclopedia of Quaternary Science. Elsevier, 2007. http://dx.doi.org/10.1016/b0-44-452747-8/00121-6.

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Coronato, A., and J. Rabassa. "GLACIATIONS | Middle Pleistocene Glaciations in the Southern Hemisphere." In Encyclopedia of Quaternary Science. Elsevier, 2013. http://dx.doi.org/10.1016/b978-0-444-53643-3.00125-4.

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Ehlers, J., P. L. Gibbard, and P. D. Hughes. "Quaternary Glaciations and Chronology." In Past Glacial Environments. Elsevier, 2018. http://dx.doi.org/10.1016/b978-0-08-100524-8.00003-8.

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Conference papers on the topic "Glaciations du Quaternaire"

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Owen, Lewis A. "QUATERNARY GLACIATION OF TIBET AND THE BORDERING MOUNTAINS." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-297498.

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Orr, Elizabeth. "QUATERNARY GLACIATION OF STOK, NORTHERN ZANSKAR RANGE, TRANSHIMALAYA, NORTHERN INDIA." In 50th Annual GSA North-Central Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016nc-275093.

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Carson, Eric C., Elizabeth G. Ceperley, and J. Elmo Rawling. "THE ROLE OF QUATERNARY GLACIATIONS IN REORGANIZING THE OHIO AND UPPER MISSISSIPPI RIVERS." In Joint 52nd Northeastern Annual Section and 51st North-Central Annual GSA Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017ne-290220.

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Yi, Chaolu. "QUATERNARY GLACIATION SEQUENCES FROM MIS 10 TO HOLOCENE IN CENTRAL TIBETAN PLATEAU." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-316945.

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Laabs, Benjamin J., and Jeffrey S. Munroe. "LATE QUATERNARY GLACIATION OF THE NORTHERN GREAT BASIN: CHRONOLOGY, CLIMATE, AND KEY QUESTIONS." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-334107.

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Li, Yingkui, Yixin Chen, Gengnian Liu, Mei Zhang, and Zhijiu Cui. "TIMING AND EXTENT OF LATE QUATERNARY GLACIATIONS ON THE NORTHERN SLOPES OF MT. SHISHAPANGMA, MONSOONAL HIMALAYAS." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-300837.

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Lapo, Kristiana, and Doug Clark. "TIMING AND PALEOCLIMATIC SIGNIFICANCE OF QUATERNARY GLACIATION IN THE THREE-FINGERED JACK REGION, OREGON HIGH CASCADES." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-302500.

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Peng, Xu, Gengnian Liu, Yixin Chen, and Zhijiu Cui. "TIMING AND EXTENT OF LATE QUATERNARY GLACIATIONS IN THE COGARBU VALLEY, EASTERN HIMALAYA ALONG THE CHINA-BHUTAN BORDER, INVESTIGATED USING 10BE SURFACE EXPOSURE DATING." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-297290.

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Reports on the topic "Glaciations du Quaternaire"

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Clague, J. J. Chapitre 12: Glaciation et Sédimentation Quaternaires. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/134100.

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Clague, J. J. Chapter 12: Quaternary Glaciation and Sedimentation. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/134099.

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Pelletier, B. R., P. R. Hill, P. J. Mudie, and S. M. Blasco. Late Quaternary glaciation and sea level history. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/126961.

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Andrews, J. T. Nature de la Dernière Glaciation au Canada [Chapitre 8: Géodynamique Quaternaires au Canada]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131629.

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Andrews, J. T. Nature of the Last Glaciation in Canada [Chapter 8: Quaternary Geodynamics in Canada]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131628.

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Jackson, L. E. Quaternary geology and terrain inventory, Foothills and adjacent plains, southwestern Alberta: some new insights into the last two glaciations. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/193645.

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Funder, S. Evolution Climatique, Glaciation et Circulation Océanique [Chapitre 13: Le Quaternaire Des Regions Extraglaciaire Du Groenland Et Des Plates-Formes Continentales Adjacentes]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131820.

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Funder, S. Development of Climate, Glaciation, and Oceanographic Circulation [Chapter 13: Quaternary Geology of the Ice-Free areas and Adjacent Shelves of Greenland]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131819.

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