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Par Collection Par Auteur- BELLO, R. L. (1)
- BROGOWSKI, Z. (1)
- CREAGER, J. S. (1)
- ECHOLS, R. J. (1)
- FLEMMING, N. C., (Editeur scientifique) (1)
- HOLMES, M. L. (1)
- MASTERS, P. M., (Editeur scientifique) (1)
- HEUSSER, C. J. (1)
- KOWALKOWSKI, A. (1)
- McMANUS, D. A. (1)
- NIMIS, P. L. (1)
- ROUSE, W. R. (1)
- TSUKADA, M. (1)
- 1983 (6)
- Geography of polar regions (4)
- Alaska ; Amérique du Nord ; Arctique ; Carbone 14 ; Datation ; Datation radiocarbone ; Détroit de Bering ; Estuaire ; Fond sous-marin ; Foraminifère benthique ; Géographie des régions polaires ; Holocène ; Littoral ; Mer de Tchoukotsk ; Milieu marin ; Niveau marin ; Pacifique, îles ; Paléo-environnement ; Paléobiogéographie ; Paléoclimatologie ; Paléofaune ; Plate-forme continentale ; Pléistocène supérieur ; Quaternaire marin ; Quaternaire supérieur ; Stratigraphie ; Sédimentologie (1)
- Alaska ; Arctique ; Dynamique de la végétation ; Etats-Unis ; Géographie des régions polaires ; Holocène ; Palynologie ; Paléobiogéographie ; Paléoflore ; Quaternaire zones froides ; Sédimentologie ; Toundra (1)
- Climat continental ; Cryoclastie ; Exoscopie ; Géographie physique ; Géomorphologie climatique ; Khangai ; Microscope électronique à balayage ; Mongolie ; Montagne ; Prairie ; Périglaciaire ; Quartz ; Sol ; Steppe ; Thermoclastie ; Toundra (1)
- Geography of Asia (1)
- Gradient latitudinal ; Géographie de l'Asie ; Japon ; Palynologie ; Paléobiogéographie ; Paléoclimatologie ; Paléotempérature ; Pléistocène supérieur ; Quaternaire zones moyennes (1)
- Physical geography (1)
- Features of cryogenic environment in soils of continental tundra and arid steppe on the southern Khangai slope under electron microscope (1)
- Holocene vegetation history of the Prince William Sound region, south-central Alaska (1)
- The Holocene transgression on the Arctic flank of Beringia: Chukchi Valley to Chukchi Estuary to Chukchi Sea in Quaternary coastlines and marine archaeology: Towards the prehistory of land bridges and continental shelves. (1)
- The radiation balance of typical terrain units in the Low Arctic (1)
- Vegetation and climate during the last glacial maximum in Japan (1)
- Vegetation history during the Holocene is interpreted from the pollen and sedimentary records of nine sections of peat deposits located in sedge tundra at sites in the northern and northwestern parts of the Prince William Sound region. Basal
- radiocarbon ages of the deposits are between 10,015 and 580 yr B.P. Modern surface pollen data from these and 25 additionnal sites, ranging from lowlands to an altitude of 675 m in the alpine tundra, were used to aid in the interpretation of the fossil records.
- 1983
- Structure and floristic composition of a high arctic tundra : Ny Alesund (Svalbard archipelago)
- 1983
- Features of cryogenic environment in soils of continental tundra and arid steppe on the southern Khangai slope under electron microscope
- 1983
- Churchill, Manitoba, from May through August, 1982. The terrain types were upland tundra, upland open spruce forest, lowland peat and moss vegetation, and lowland swamp covered with sedge grass.
- 1983
- The Japanese Archipelago was almost entirely covered by coniferous forests during the last glacial maximum. Northern Hokkaido was distinguished by coniferous parkland and tundra vegetation, while southern Hokkaido and northernmost Honsku were
- 1983
- steppe-tundra valley to a shallow, partly ice-covered estuary. A broader, more continuously ice-covered estuary became an embayment of the Arctic ocean. At about 14,400 yr B. P., the rising sea level finally opened the last strait. (P. A. Pirazzoli).
- 1983