Andrei A Andreev

Datos Biográficos

ID10709461
NOMBREAndrei A Andreev
NOMBRESAndrei A
APELLIDOAndreev
FIRMAANDREEV A A
VERIFICADONo
TOTAL DE OBRAS5
TOTAL DE CITAS0
TOTAL COMO AUTOR5
TOTAL COMO EDITOR0
PRIMER AÑO DE PUBLICACIÓN1998
AÑO MÁS RECIENTE DE PUBLICACIÓN2007
ÍNDICE H0

  • Environmental changes in the northern Altai during the last millennium documented in Lake Teletskoye pollen record

    Open AccessAndrei Andreev, Andrei A Andreev et al.ARTICLEQuaternary Research2007

    A high-resolution pollen record from Lake Teletskoye documents the climate-related vegetation history of the northern Altai Mountain region during the last millennium. Siberian pine taiga with Scots pine, fir, spruce, and birch dominated the vegetation between ca. AD 1050 and 1100. The climate was similar to modern. In the beginning of the 12th century, birch and shrub alder increased. Lowered pollen concentrations and simultaneous peaks in herbs…

  • Middle Weichselian environments on western Yamal Peninsula, Kara Sea based on pollen records

    Open AccessAndrei Andreev, Andrei A Andreev et al.ARTICLEQuaternary Research2006

    Pollen data from two sections from a coastal cliff on the western Yamal Peninsula (69 ° 43.27′N, 66 ° 48.80′E) document the environmental history during the Karginsky (Middle Weichselian) interstadial. Low pollen concentrations, high amounts of redeposited pollen, and relatively high presence of Artemisia pollen characterize sediments deposited at about 33,000 14 C yr B.P. Grass-sedge plant associations with few other herbs occupied the area duri…

  • Late Pleistocene and Holocene Vegetation and Climate on the Taymyr Lowland, Northern Siberia

    Open AccessAndrei Andreev, Andrei A Andreev et al.ARTICLEQuaternary Research2002

    Pollen records from perennially frozen sequences provide vegetation and climate reconstruction for the last 48,000 14 C years in the central part of Taymyr Peninsula. Open larch forest with Alnus fruticosa and Betula nana grew during the Kargin (Middle Weichselian) Interstade, ca. 48,000–25,000 14 C yr B.P. The climate was generally warmer and wetter than today. Open steppe-like communities with Artemisia , Poaceae, Asteraceae, and herb tundralik…

  • Holocene Treeline History and Climate Change Across Northern Eurasia

    Open AccessGlen M Macdonald, Andrei A Velichko et al.ARTICLEQuaternary Research2000

    Radiocarbon-dated macrofossils are used to document Holocene treeline history across northern Russia (including Siberia). Boreal forest development in this region commenced by 10,000 yr B.P. Over most of Russia, forest advanced to or near the current arctic coastline between 9000 and 7000 yr B.P. and retreated to its present position by between 4000 and 3000 yr B.P. Forest establishment and retreat was roughly synchronous across most of northern …

  • Present‐day and mid‐Holocene biomes reconstructed from pollen and plant macrofossil data from the former Soviet Union and Mongolia

    Open AccessPavel E Tarasov, Thompson Webb Iii et al.ARTICLEJournal of Biogeography1998

    Fossil pollen data supplemented by tree macrofossil records were used to reconstruct the vegetation of the Former Soviet Union and Mongolia at 6000 years. Pollen spectra were assigned to biomes using the plant‐functional‐type method developed by Prentice et al . (1996). Surface pollen data and a modern vegetation map provided a test of the method. This is the first time such a broad‐scale vegetation reconstruction for the greater part of northern…