Holocene vegetation and climate dynamics of the boreal alpine ecotone of northwestern Fennoscandia

• Published in: Journal of Quaternary Science
• Main Authors: Jensen, Christin, Vorren, Karl‐Dag
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2008
• Subjects: Dividalen; Skrubben; Fennoscandia
• Online Access: http://dx.doi.org/10.1002/jqs.1155; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.1155; https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.1155

Abstract Climate change with respect to summer temperature throughout the Holocene is inferred from oscillations in the local Pinus sylvestris , Alnus incana and Betula pubescens forest‐lines, as recorded by fossil pollen and plant macrofossils in lake sediments at four altitudinal levels. Mt Skrubben (848 m a.s.l.), in Dividalen, was deglaciated down to below 280 m a.s.l. during 10 800–10 300 cal. yr BP. Betula pubescens established 10100 cal. yr BP at 280 m a.s.l. and expanded up to near the summit during the next 700 years. Birch woodland prevailed on the mountain plateau until 3300 cal. yr BP. Local Pinus sylvestris stands are recorded up to 400 m a.s.l. at 8450 cal. yr BP and >548 m a.s.l. about 8160 cal. yr BP. Alnus incana expanded from 400 to nearly 790 m a.s.l. during the period 7900–7600 cal. yr BP. The maximum forest distribution lasted until ca. 6000 cal. yr BP. Marked climatic deteriorations caused lowering of the forest‐lines around 4600 and 3000 cal. yr BP. Reconstruction of the summer temperature indicated mean July temperatures at 400 m a.s.l. of 1.5–3°C above the present during the period of maximum forest expansion, whereas >3°C above the present temperature at 548 m a.s.l. This is in accordance with other regional temperature reconstructions from northern Europe. Copyright © 2008 John Wiley & Sons, Ltd.