Abstract

The data file presents information on the quantitative taxa distribution for plant macrofossils in the Holocene sediment cores of mires in the Kaliningrad region (Russian Federation, South-Eastern Baltic Region), as well as 24 radiocarbon dates (14C). The dataset contains percentages of 51 most common (more than 1%) taxa in 1361 samples of 45 sediment cores. These data provide information on environmental development and evolution of the azonal wetland vegetation in the south-eastern part of the Baltic region during the Holocene.

Highlights

  • Quantitative data on plant macrofossil distribution in the holocene sediment cores of mires in the Kaliningrad region, Russian Federation (South-Eastern Baltic)

  • The data file contains the quantitative information on relative content (%) of the abundant (>1% of concentration) plant macro-remnants the in the Holocene sediment cores from peatlands in the Kaliningrad region

  • The plant macro-remnants is a basic substrate of the peat sediments which have generally no hiatuses

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Summary

Data Article

Quantitative data on plant macrofossil distribution in the holocene sediment cores of mires in the Kaliningrad region, Russian Federation (South-Eastern Baltic). The data file presents information on the quantitative taxa distribution for plant macrofossils in the Holocene sediment cores of mires in the Kaliningrad region (Russian Federation, South-Eastern Baltic Region), as well as 24 radiocarbon dates (14C). The dataset contains percentages of 51 most common (more than 1%) taxa in 1361 samples of 45 sediment cores These data provide information on environmental development and evolution of the azonal wetland vegetation in the south-eastern part of the Baltic region during the Holocene. The data file contains the quantitative information on relative content (%) of the abundant (>1% of concentration) plant macro-remnants (identified to species or genus) the in the Holocene sediment cores from peatlands in the Kaliningrad region. The plant macro-remnants is a basic substrate of the peat sediments which have generally no hiatuses

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Maloye Olenye terrestrializing lake
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