Tree taxa immigration to the eastern Baltic region, southeastern sector of Scandinavian glaciation during the Late-glacial period (14,500-1,700?cal. b.p.)
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- 作者：Leeli Amon (1)
Siim Veski (1)
Jüri Vassiljev (1) - 关键词：Late ; glacial vegetation ; Macrofossil ; Immigration ; Tree line ; Eastern Baltic
- 刊名：Vegetation History and Archaeobotany
- 出版年：2014
- 出版时间：May 2014
- 年：2014
- 卷：23
- 期：3
- 页码：207-216
- 全文大小：2,102 KB
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Siim Veski (1)
Jüri Vassiljev (1)
1. Institute of Geology at Tallinn University of Technology, Ehitajate tee 5, 19086, Tallinn, Estonia - ISSN：1617-6278
文摘
The eastern Baltic region is situated in the southeastern part of the area which was covered by the last Scandinavian glaciation. Four well-dated sediment profiles from sites distributed along a ~330-km north–south transect were analysed for their macrofossil contents. The immigration of tree taxa during the Late-glacial (LG) period, which was the time of environmental change from tundra to woodland in previously glaciated areas, can be determined from these data. The pioneer vegetation in the study area was treeless dwarf shrub tundra with various dominant taxa. The so-called Aller?d hemispheric warming permitted the Post-glacial immigration of trees into the southern part of the eastern Baltic region; however, these most probably disappeared during the following cold period, the Younger Dryas/GS-1. The local presence of Betula sect. Albae, Pinus sylvestris, Populus tremula and Picea abies during the LG period in the southern part of the region was confirmed. The northern part of the area presumably remained treeless for the entire LG period. Therefore, until the beginning of the Holocene, the tree line in the eastern Baltic region did not reach beyond 58°N.