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- W2008359763 abstract "Three palaeolakes at elevations from 44 m a.s.l. to 30 m a.s.l. all have marine sediments in the lower part of the sequences, with lacustrine sediments above. The highest lake was isolated from the sea approximately 12,400 years ago, and the lowest 11,100 years ago. The lacustrine sedimentary sequence is so similar in these lakes and many other palaeolakes that we propose formal lithostratigraphical units. Climatic changes were the most important cause for changes in the sediment composition. The earliest vegetation was dominated by grass and herbs, especially Rumex and Oxyria. Later in the Allerød the flora was more diversified, but a tree-less vegetation, still covered large areas. Open birch forests were established on favourable localities approx. 11,600 years ago. Tree birch probably survived in the area during the Younger Dryas. Low sedimentation rates during the Younger Dryas suggests slow erosion on land, and a continuous vegetation cover, which was dominated by herbs and Salix. An Older Dryas climatic deterioration was not detected. In the Preboreal a Juniperus maximum occurs after the Betula rise, in contrast to the sequence in Denmark and Germany. Pinus is supposed to have immigrated from the east, through Sweden." @default.
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- W2008359763 date "1988-01-01" @default.
- W2008359763 modified "2023-09-27" @default.
- W2008359763 title "Late weichselian/early holocene pollen-and lithostratigraphy in lakes in the ålesund area, western Norway" @default.
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- W2008359763 doi "https://doi.org/10.1016/0034-6667(88)90033-4" @default.
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