Bulletin of the Geological Society of Finland (Dec 1994)

Late Pleistocene pollen flora with Larix from till-covered esker at Hietamäki, Ostrobothnia, western Finland

  • B. Eriksson,
  • R. Kujansuu

DOI
https://doi.org/10.17741/bgsf/66.2.001
Journal volume & issue
Vol. 66, no. 2
pp. 53 – 66

Abstract

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A till-covered layer of clay, fine sand and organic-bearing silt was found at Hietamäki near Haapajärvi, Ostrobothnia (Pohjanmaa), western Finland. The organic-bearing silt layer is an infill sediment in a dead ice hollow within a glaciofluvial formation interpreted as an esker. The esker is covered by till, at the base of which is a layer or lense of clay 1.5 m thick. On the basis of pollen content, the layers of clay and organic-bearing silt were deposited during the Eemian interglacial stage. Pinus-Picea-Larix forests mixed with Betula and Alnus possibly represent a regressive phase of the late Eemian vegetational development, when thermophile trees had already withdrawn from the area.

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