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Late Quaternary of Antarctica
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GLACIATIONS | Late Quaternary of Antarctica
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Late Quaternary Glaciation of Antarctica☆
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GLACIATIONS | Late Quaternary of Antarctica
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The history of the Barents Sea Ice Sheet ‐ state of the art and current research...
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Glacial and environmental history of Severnaya Zemlya, Siberian high arctic, dur...
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Glacial history of the Antarctic Peninsula since the Last Glacial Maximum - a sy...
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Late Quaternary glacial and climatic history of the Antarctica ‐ state of the ar...
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Late Quaternary glacial and climatic history of the Arctic ‐ state of the art an...
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Late Quaternary marine-based Kara Sea ice sheets: review of terrestrial stratigr...
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The Preboreal oscillation around the Nordic Seas : Terrestrial and lacustrine re...
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Quaternary glacial and sea-level history of Severnaya Zemlya, Siberian high arct...
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Glacial and climate history of the Antarctic Peninsula since the Last Glacial Ma...
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The Preboreal oscillation around the Nordic Seas: terrestrial and lacustrine res...
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Late Weichselian history of relative sea level changes in Iceland during a colla...
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Late Weichselian history of relative sea level changes in Iceland during a colla...
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Holocene and pre-Holocene temporary disappearance of the George VI Ice Shelf, An...
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Holocene deglaciation and climate history of the northern Antarctic Peninsula re...
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A detailed record of relative sea‐level change during the last deglaciation of n...
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Middle Weichselian environments on western Yamal Peninsula, Kara Sea based on po...
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Geology
Paleontology
Ecology, Evolution, Behavior and Systematics
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Geomorphology and Regolith and Landscape Evolution
Iceland
Islandia
Oceanography
Physical Geography and Environmental Geoscience
Weichselian
Weichseliense
deglaciación
deglaciation
ice sheet
manto de hielo
nivel del mar
sea level
western yamal peninsula
Anthropocene
Archeology
Arctic
Chronology
Climate Research
Diatoms
Earth and Related Environmental Sciences
Earth-Surface Processes
Environmental Sciences
GB Physical geography
Geovetenskap och miljövetenskap
Glacial records
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