Holocene pollen stratigraphy and bog development in the western part of the Kola Peninsula, Russia

Pollen and macrofossil investigations and radiocarbon datings were carried out at a bog in the Khibiny mountains and the northernmost bog in European Russia on the Rybachiy Peninsula (69°98'N) on the western part of the Kola Peninsula. Peat accumulation on the Kola Peninsula started at c . 8500...

Full description

Bibliographic Details
Published in:Boreas
Main Authors: KREMENETSKI, CONSTANTIN, VASCHALOVA, TATIANA, GORIACHKIN, SERGEI, CHERKINSKY, ALEXANDR, SULERZHITSKY, LEOPOLD
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1997
Subjects:
Barents Sea
Kola Peninsula
Khibiny
Rybachiy
kola peninsula
Rybachiy Peninsula
Tundra
Online Access:http://dx.doi.org/10.1111/j.1502-3885.1997.tb00656.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1997.tb00656.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1997.tb00656.x
Description
Summary:Pollen and macrofossil investigations and radiocarbon datings were carried out at a bog in the Khibiny mountains and the northernmost bog in European Russia on the Rybachiy Peninsula (69°98'N) on the western part of the Kola Peninsula. Peat accumulation on the Kola Peninsula started at c . 8500–7500 BP. Pinus sylvestris reached its present northern limit on the peninsula by 7000 BP, while 6000–5000/4500 BP was a time of maximal progress of birch forest tundra up to the Barents Sea shoreline. Alnus ineana grew up to the Rybachiy Peninsula c . 40 km north of its present‐day northern limit. By c , 5500/5300 BP Picen ohovata had immigrated to the Khibiny mountains. After 5000/4500 BP the forested area had retreated in the northern part of the Kola Peninsula and the tundra belt bordering the Barents Sea shore was formed. By 3500 BP spruce had reached its modern northern limit.

Similar Items