Abstract
Modern climate in western Norway shows a strong west–east gradient in oceanicity–continentality (coast to inner
fjord) and altitudinal temperature gradients that control the regional and altitudinal zonation of vegetation. To
discover if similar gradients existed during the Lateglacial and early Holocene, plant-macrofossil analyses were
made from five lacustrine sediment sequences in the Nordfjord–A˚
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