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A chronology of depositional coastal landforms of the Baltic Sea : Luminescence dating of sandy sediments and patterns of human settlement at the ancient Ventspils Lagoon

Kalińska, Edyta LU ; Breijers, Edijs ; Alexanderson, Helena LU orcid ; Krievāns, Māris and Bērziņš, Valdis (2022) In Estuarine, Coastal and Shelf Science 279.
Abstract

The ancient Ventspils Lagoon is an area where human settlements have been located on former coastal landforms and sediments. However, the chronology of its development has so far not been studied in detail. Since the ancient lagoon is dominated by sand deposition, optically stimulated luminescence dating (OSL) was used to determine when the ancient coast was formed. Twenty-one OSL samples gave a wide age range, between 8.57 ± 0.65 ka and 73.8 ± 8.3 ka. Twelve of the ages fall in the Late Glacial and Holocene and document the development of the lagoon between the Baltic Ice Lake stage (∼16 ka) and the Littorina Sea stage (∼8 ka). The new dates correspond to some extent with previously modelled shorelines for the Ventspils Lagoon and to... (More)

The ancient Ventspils Lagoon is an area where human settlements have been located on former coastal landforms and sediments. However, the chronology of its development has so far not been studied in detail. Since the ancient lagoon is dominated by sand deposition, optically stimulated luminescence dating (OSL) was used to determine when the ancient coast was formed. Twenty-one OSL samples gave a wide age range, between 8.57 ± 0.65 ka and 73.8 ± 8.3 ka. Twelve of the ages fall in the Late Glacial and Holocene and document the development of the lagoon between the Baltic Ice Lake stage (∼16 ka) and the Littorina Sea stage (∼8 ka). The new dates correspond to some extent with previously modelled shorelines for the Ventspils Lagoon and to radiocarbon ages from archaeological sites in the area. One date, 16.0 ± 1.3 ka, falls in the period before the Baltic Ice Lake and represents either a very early Baltic Ice Lake stage or, less likely, the Venta glacial lake prior to the Baltic Ice Lake. One date, 5.09 ± 0.42, is likely underestimated. Seven samples yielded dates between 21.5 ± 1.5 ka and 73.8 ± 8.3 ka, which corresponds to the Early and Middle Weichselian in the Baltic region. The samples in this latter group are likely overestimating the true age due to insufficient exposure to sunlight during deposition.

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author
; ; ; and
organization
publishing date
type
Contribution to journal
publication status
published
subject
keywords
Ancylus, Baltic ice lake, Baltic sea, Littorina, Mesolithic, Neolithic, OSL dating, Radiocarbon dating, Shorelines
in
Estuarine, Coastal and Shelf Science
volume
279
article number
108135
publisher
Elsevier
external identifiers
  • scopus:85142125276
ISSN
0272-7714
DOI
10.1016/j.ecss.2022.108135
language
English
LU publication?
yes
id
899f6345-e96d-480a-9e0f-83a853771e18
date added to LUP
2022-12-28 13:59:30
date last changed
2025-03-08 00:45:45
@article{899f6345-e96d-480a-9e0f-83a853771e18,
  abstract     = {{<p>The ancient Ventspils Lagoon is an area where human settlements have been located on former coastal landforms and sediments. However, the chronology of its development has so far not been studied in detail. Since the ancient lagoon is dominated by sand deposition, optically stimulated luminescence dating (OSL) was used to determine when the ancient coast was formed. Twenty-one OSL samples gave a wide age range, between 8.57 ± 0.65 ka and 73.8 ± 8.3 ka. Twelve of the ages fall in the Late Glacial and Holocene and document the development of the lagoon between the Baltic Ice Lake stage (∼16 ka) and the Littorina Sea stage (∼8 ka). The new dates correspond to some extent with previously modelled shorelines for the Ventspils Lagoon and to radiocarbon ages from archaeological sites in the area. One date, 16.0 ± 1.3 ka, falls in the period before the Baltic Ice Lake and represents either a very early Baltic Ice Lake stage or, less likely, the Venta glacial lake prior to the Baltic Ice Lake. One date, 5.09 ± 0.42, is likely underestimated. Seven samples yielded dates between 21.5 ± 1.5 ka and 73.8 ± 8.3 ka, which corresponds to the Early and Middle Weichselian in the Baltic region. The samples in this latter group are likely overestimating the true age due to insufficient exposure to sunlight during deposition.</p>}},
  author       = {{Kalińska, Edyta and Breijers, Edijs and Alexanderson, Helena and Krievāns, Māris and Bērziņš, Valdis}},
  issn         = {{0272-7714}},
  keywords     = {{Ancylus; Baltic ice lake; Baltic sea; Littorina; Mesolithic; Neolithic; OSL dating; Radiocarbon dating; Shorelines}},
  language     = {{eng}},
  publisher    = {{Elsevier}},
  series       = {{Estuarine, Coastal and Shelf Science}},
  title        = {{A chronology of depositional coastal landforms of the Baltic Sea : Luminescence dating of sandy sediments and patterns of human settlement at the ancient Ventspils Lagoon}},
  url          = {{http://dx.doi.org/10.1016/j.ecss.2022.108135}},
  doi          = {{10.1016/j.ecss.2022.108135}},
  volume       = {{279}},
  year         = {{2022}},
}