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Decomposition of plant litter and cellulose in the tundras of the Taymyr peninsula
  • Decomposition of plant litter and cellulose in the tundras of the Taymyr peninsula
Holocene vegetation history of the Prince William Sound region, south-central Alaska
  • 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.
Zur Okologie der Tundra Zentralspitzbergens L'écologie de la toundra du Spitzberg central
  • Zur Okologie der Tundra Zentralspitzbergens L'écologie de la toundra du Spitzberg central
Validation of a model of the effect of tundra vegetation on soil temperatures
  • Validation of a model of the effect of tundra vegetation on soil temperatures
Structure and floristic composition of a high arctic tundra : Ny Alesund (Svalbard archipelago)
  • Structure and floristic composition of a high arctic tundra : Ny Alesund (Svalbard archipelago)
Die mesoklimatische Verteilung von Lufttemperatur und Niederschlag über der hocharktischen Tundra von Axel Heiberg Island, N.W.T., Kanada Répartition mésoclimatique de la température atmosphérique et des précipitations sur la toundra arctique de l'île Axel Heiberg, N.W.T., Canada
  • Die mesoklimatische Verteilung von Lufttemperatur und Niederschlag über der hocharktischen Tundra von Axel Heiberg Island, N.W.T., Kanada Répartition mésoclimatique de la température atmosphérique et des précipitations sur la toundra arctique de
Remnants of Viking age tundra in Spitsbergen and Northern Scandinavia
  • Remnants of Viking age tundra in Spitsbergen and Northern Scandinavia
The radiation balance of typical terrain units in the Low Arctic
  • 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.
Man's impact on tundra ecosystems
  • Man's impact on tundra ecosystems
Pollen analysis of a late Pliocene and early Pleistocene section from the Gubik Formation of Arctic Alaska
  • similar to that of present-day. Pollen floras from the overlying fluvial strata, of early or middle Pleistocene age, record predominantly herbaceous taxa indicating tundra conditions probably more severe than those of the present day. These deposits were
Effects of storm surges on the Beaufort sea coast, Northern Alaska
  • In 1970, a major storm surge caused by gale-force westerly winds inundated low-lying tundra plains and deltas as for as 5000 m inland and left a driftwood line as much as 3.4 m above normal sea level along the Beaufort Sea coast of Alaska
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.
  • 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).
Pollen analysis of the 1973 ice core from Devon Island glacier, Canada
  • were blown a minimum of 1000 km from low arctic shrub tundra and adjacent subarctic Picea (spruce) forest| these areas were dominated by the arctic air mass during the summer pollinating season. During the Wisconsinan-early Holocene, glacier ice
Canyon Creek: a late Pleistocene vertebrate locality in interior Alaska
  • sp. cf. O. dalli (mountain sheep), Canis sp. cf. C. lupus (wolf), Lepus sp. cf. L. othus or L. arcticus (tundra hare), and Rangifer sp. (caribou). This assemblage suggests an open landscape in which trees and tall shrubs were either absent or confined
Srednevaldajskoe more-ozero na zapade Bol'sezemel'skoj tundry. (Le lac-mer du Valdaï moyen dans l'ouest de la Bol'sezemel'skaja toundra)
  • Arctique ; Bol'sezemel'skaja tundra ; Diatomée ; Dépôt quaternaire ; Flore fossile ; Géographie des régions polaires ; Paléobiogéographie ; Paléogéographie ; Quaternaire glaciations ; Rossijskaja SFSR ; Sédimentologie ; URSS d'Europe ; Variation