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  • Glacial and vegetational history of the Southern Lake District of Chile
  • Andes ; Antarctica ; Argentina ; C 14 dating ; Chile ; Ice core ; Lateglacial ; Moraine ; New Zealand ; Ocean circulation ; Oxygen 18 ; Palaeo-environment ; Palaeoclimate ; Palaeoclimatology ; Palynology ; Quaternary ; Southern hemisphere
  • Andes ; Antarctique ; Argentine ; Carotte de glace ; Chili ; Circulation océanique ; Datation C 14 ; Hémisphère Sud ; Moraine ; Nouvelle-Zélande ; Oxygène 18 ; Palynologie ; Paléo-environnement ; Paléoclimat ; Paléoclimatologie ; Quaternaire
  • Combined glacial geologic and palynologic data from the Chilean Andes and New Zealand Southern Alps highlight features of middle latitude Southern Hemisphere paleoclimate through the Last Glacial Maximum, LGM, and the last termination. Discussion
  • Glacial geomorphologic maps of Llanquihue drift in the area of the southern Lake District, Chile
  • Glacial and vegetational history of the Southern Lake District of Chile
  • project to establish a paleoclimate reconstruction of the last glacial cycle in the middle latitudes of the Southern Hemisphere. They show the lobate shape and low surface slopes of the former piedmont glaciers that, at the last glacial maximum, spread
  • The AA. present 4 glacial geomorphic maps of Llanquihue drift in the region of the southern Lake District, Seno Reloncaví, and the eastern half of northern Isla Grande de Chiloé, Chile. These maps form the basis of an interdisiplinary research
  • Paleoecology of the southern Chilean Lake District-Isla Grande de Chiloé during middle-late Llanquihue glaciation and deglaciation
  • Glacial and vegetational history of the Southern Lake District of Chile
  • The paleoecological studies of the Southern Lake District-Isla Grande de Chiloé were undertaken to develop from high-resolution reconstruction of late Pleistocene vegetation: 1) presence, associations, and migratory movement of plant taxa; 2
  • ) climatic parameters that surround stades and interstades of middle and late Llanquihue glaciation; and 3) a standard for demonstrating late Pleistocene intrahemispheric and polar hemispheric relationships and dynamic forcing of climatic events.