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  • The geologic basis for a reconstruction of a grounded ice sheet in McMurdo Sound, Antarctica, at the Last Glacial Maximum
  • Glacial and paleoclimatic history of the Ross ice drainage system of Antarctica. Special issue
  • The overall results in this paper afford a background for interpreting the glacial chronology of eastern Taylor Valley and for reconstructing a grounded ice sheet in the overall Ross Embayment at the Last Glacial Maximum (LGM)
  • Map of vegetation during the last glacial maximum in Japan
  • Carte ; Datation radiocarbone ; Dernier maximum glaciaire ; Géographie de l'Asie ; Japon ; Macrofossile ; Palynologie ; Paléobiogéographie ; Paléobotanique ; Pléistocène supérieur ; Pléniglaciaire ; Quaternaire zones moyennes
  • A vegetation map reconstructed for the Japanese Archipelago (based upon pollen data from 28 sites and plant macrofossil data from 33 sites) at the time of last glacial maximum shows that coniferous forests covered extensive areas of the land. Boreal
  • Fast-flowing outlet glaciers of the Last Glacial Maximum Patagonian Icefield
  • Cartography ; Chile ; Glacial flow ; Glacier ; LANDSAT ; Lateglacial ; Numerical model ; Palaeo-environment ; Patagonia ; Remote sensing
  • Glacial geomorphology around the Northern Patagonian Icefield indicates that a number of fast-flowing outlet glaciers drained the icefield during the Last Glacial Maximum. Here, a detailed regional map of glacial landforms around the Northern
  • of the Northern Patagonian Icefield at the Last Glacial Maximum is not accurately represented in existing numerical ice-sheet models.
  • Alpine evidence for atmospheric circulation patterns in Europe during the Last Glacial Maximum
  • the atmospheric circulation and associated precipitation patterns responsible for the ice buildup in the Alps during the last glaciation and 2) an explanation for the nonsynchronous maximum glacial extents in the Alps, the Pyrénées, and the surrounding low
  • The AA. present a reconstruction of the late Quaternary paleoclimate history in central Europe with special emphasis on the period of ice buildup following the last (Eemian) interglaciation. Special attention is focused on 1) reconstructing
  • Environments of aeolian deposition in south-central Nebraska during the Last Glacial Maximum
  • Aeolian features ; Glacial features ; Loess ; Magnetic susceptibility ; Nebraska ; Permafrost ; Quaternary ; Stratigraphy ; United States of America
  • The Peoria Loess of south-central Nebraska, deposited approximately during the Last Glacial Maximum, can be subdivided into three zones: an upper laminated loess and a lower massive loess, separated by a dark gley zone in which bison bones
  • Cosmogenic nuclide chronology of pre-last glacial maximum moraines at Lago Buenos Aires, 46°S, Argentina
  • In this paper, exposure ages are presented for glacial deposits older than the last glacial maximum. The chronology demonstrates that a major mountain glaciation occurred during marine oxygen isotope stage 6 in Patagonia and indicates
  • Reconstruction of the Ross ice drainage system, Antarctica, at the Last Glacial Maximum
  • Glacial and paleoclimatic history of the Ross ice drainage system of Antarctica. Special issue
  • The AA. present a revised reconstruction of the Ross ice drainage system of Antarctica at th Last Glacial Maximum (LGM) based on a recent convergence of terrestrial and marine data. The Ross drainage system includes all ice flowlines that enter
  • Circulation in the Gulf of Mexico during the last glacial maximum 18000 years ago
  • Lors du dernier maximum glaciaire (il y a 18000 ans), les eaux de surface du Golfe du Mexique étaient plus froides et plus salées, et décrivaient un mouvement anticyclonique. (JRV).
  • Last glacial maximum in China: comparison between land and sea
  • As a result of the sea-level drop at the last glacial maximum, the size and configurations of the Chinas Seas changed greatly. This paper is an attempt to compare the available paleoenvironmental data yielded by deposits of the China mainland
  • Absence of last glacial maximum records in lowlan tropical forests
  • Environmental conditions of the lowland tropical forests during the last glacial maximum (LGM) between ca 20,000 and 18,000 C 14 yr B.P., are reevaluated in terms of dating control and lithology analyzed in seven pollen records from South America
  • Extent and timing of the last glacial maximum in Southwestern Alaska
  • The AA. report here on stratigraphic sections relevant to the timing of the last glacial maximum (LGM) in southwestern Alaska, the region between Cook Inlet and Unimak Island, including the Kodiak archipelago. This work has concentrated
  • Paleoproductivity evolution off central Chile from the Last Glacial Maximum to the Early Holocene
  • A geochemical and paleontological reconstruction of paleoproductivity, upwelling intensity and sea surface temperature (SST) off central Chile at 35°S reveals marked changes from the Last Glacial Maximum (LGM) through the Early Holocene. The AA
  • Cosmogenic radionuclide evidence for the limited extent of last glacial maximum glaciers in the Tanggula Shan of the central Tibetan Plateau
  • Cosmogenic radionuclide (CRN) exposure ages provide evidence for the limited extent of last glacial maximum glaciers in the Tanggula Shan, central Tibetan Plateau. The most extensive advances occurred during or before marine oxygen isotope stage 6
  • Alps (The) ; Geomorphology ; Glacial features ; Glaciation ; Glacier advance ; Palaeo-environment ; Pleistocene ; Slovenia ; Topography
  • The article deals with glacial remains from the last glacial maximum in the Logar Valley (Kamnik-Savinja Alps). The AA. tried to reinterpret the findings written so far and to prepare a new proposal of the circumference of the last glacial maximum
  • in this area. The numerical analysis was based on the findings gained with field work. According to the findings, the maximum glacier extent was drawn and a three-dimensional reconstruction of the topography of the surface was created. - (IKR)
  • Spatial and temporal variations in the thermodynamics since the Last Glacial Maximum at Jutulstraumen drainage basin, East Antarctica
  • Antarctica ; Glacial flow ; Ice sheet ; Model ; Spatial variation ; Thermal regime ; Watershed
  • Modèle d'écoulement de glace thermodynamique. Application au Jutulstraumen. Modélisation de la dynamique et des changements thermiques depuis le dernier maximum glaciaire. Elévations et vitesses simulées et mesurées aujourd'hui.
  • New radiometric and geomorphologic evidences of a last glacial maximum older than 18 ka in SW European mountains : the exemple of Redes Natural Park (Cantabrian Mountains, NW Spain)
  • Asturias ; C 14 dating ; Comparative study ; Geochronology ; Glacial features ; Glacier fluctuation ; Lateglacial ; Periglacial features ; Pyrénées ; Quaternary ; Spain
  • of glacier evolution established in the Pyrénées, with a glacial maximum phase for the last glacial period older than 18 ka.
  • The aim of this work is to date glacial events in Redes Natural Park, in order to establish if the timing of these events is similar to comparable events in the Pyrénées. The chronological data presented in this work are consistent with the model
  • The Last Glacial Maximum on Spitsbergen, Svalbard
  • Arctic Ocean;Arctic Region ; C14 dating ; Glacial features ; Marine sediment ; Paleo-environment ; Quaternary ; Stratigraphy ; Svalbard
  • The main aim of this paper is to contribute to a resolution of the described controversy on the limit of the last glacier, and to provide an improved description and interpretation of the late Weichselian glaciation on western Svalbard
  • Paleoecology of central Kentucky since the Last Glacial Maximum
  • Climatic variation ; Glacial features ; Holocene ; Kentucky ; Paleo-ecology ; Palynology ; Pollen diagrams ; Quaternary ; United States
  • In this paper, the AA. present paleoecological data from Jackson Pond, Kentucky, which is located 190 km south of the full-glacial limit of the Laurentide Ice Sheet and the sediments of which continuously span the past 20,000 radiocarbon years
  • maximum, dated between 30 000 and 11 000 B.P., was relatively cold and dry compared with the warmer, more humid climate of the Holocene and the interstade preceding the last glacial maximum. General atmospheric circulation models for the polar latitudes
  • at the time of the last glacial maximum show an intensification of the southern westerlies, apparently a result of the expansion of ice cover in Antarctica.
  • Late-Quaternary paleoecological and glacial evidence from the higher latitudes of the Southern Hemisphere implies overall uniformity of large-scale glacial and interglacial climatic fluctuations for the past 40 000 yr. Climate of the last glacial
  • Topographic and climatic influences on accelerated loess accumulation since the last glacial maximum in the palouse, Pacific Northwest, USA
  • Accumulation rate ; Aeolian features ; Glacial surge ; Loess ; Oregon ; Palaeo-environment ; Palaeoclimate ; Pleistocene ; Quaternary ; Tephrochronology ; United States of America
  • provide an ideal test of the topographic trap model of Mason et al. (1999) and in so doing provide insight into timing of loess deposition since the last glacial maximum (LGM)
  • This paper evaluates the roles that Juniper and Cold Springs Canyons have played in the distribution and thickness of loess in the southwestern Palouse. These topographic features and their associated glacial outburst flood and eolian deposits