The Holocene vegetation history of the Khibiny Mountains: implications for the post-glacial expansion of spruce and alder on the Kola Peninsula, northwestern Russia

• Published in: Journal of quaternary science 1999-02, Vol.14 (1), p.29-43
• Main Authors: Kremenetski, Constantin, Vaschalova, Tatiana, Sulerzhitsky, Leopold
• Format: Article
• Language: English
• Subjects: alder; climate; Holocene; Kola Peninsula; Picea; Pinus; Pinus sylvestris; pollen analysis; spruce
• ISSN: 0267-8179; 1099-1417
• DOI: 10.1002/(SICI)1099-1417(199902)14:1<29::AID-JQS396>3.0.CO;2-1

Pollen and peat botanical investigations of the Lutnermayok peat bog, Kola Peninsula, northwestern Russia, were carried out, and 21 surface pollen samples were studied. Combined with previous studies our data form the basis for the vegetation history over the last 7000 yr of the Khibiny Mountains. Pinus sylvestris was the dominant species between 7000 and 5000 yr BP and Picea obovata penetrated to the Khibiny Mountains ca. 5500/5300 yr BP. Since 4500 yr BP, Picea replaced Pinus in major parts of the area and dominated the forest cover. Picea immigrated to the Kola Peninsula after 7000 yr BP. There were two paths of spruce migration: from the southeast and the southwest. Grey alder, Alnusincana, immigrated to the Kola Peninsula from the southwest and northwest about ca. 8000 yr BP. Grey alder has been restricted to its modern range since 4000 yr BP. The range of vertical movement of the treeline in Khibiny Mountains during the last 700 yr was 240–260 m, which corresponds to an amplitude of summer temperature change of 2°C. Copyright © 1999 John Wiley & Sons, Ltd.