Weichselian history of the Fennoscandian ice sheet in southern Sweden and the southwestern Baltic Basin

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Weichselian history of the Fennoscandian ice sheet in southern Sweden and the southwestern Baltic Basin. / Anjar, Johanna; Adrielsson, Lena; Larsen, Nicolaj Krog; Möller, Per; Barth, Kilian.

In: Boreas, Vol. 43, No. 3, 2014, p. 608-626.

Research output: Contribution to journalJournal articleResearchpeer-review

Harvard

Anjar, J, Adrielsson, L, Larsen, NK, Möller, P & Barth, K 2014, 'Weichselian history of the Fennoscandian ice sheet in southern Sweden and the southwestern Baltic Basin', Boreas, vol. 43, no. 3, pp. 608-626. https://doi.org/10.1111/bor.12048

APA

Anjar, J., Adrielsson, L., Larsen, N. K., Möller, P., & Barth, K. (2014). Weichselian history of the Fennoscandian ice sheet in southern Sweden and the southwestern Baltic Basin. Boreas, 43(3), 608-626. https://doi.org/10.1111/bor.12048

Vancouver

Anjar J, Adrielsson L, Larsen NK, Möller P, Barth K. Weichselian history of the Fennoscandian ice sheet in southern Sweden and the southwestern Baltic Basin. Boreas. 2014;43(3):608-626. https://doi.org/10.1111/bor.12048

Author

Anjar, Johanna ; Adrielsson, Lena ; Larsen, Nicolaj Krog ; Möller, Per ; Barth, Kilian. / Weichselian history of the Fennoscandian ice sheet in southern Sweden and the southwestern Baltic Basin. In: Boreas. 2014 ; Vol. 43, No. 3. pp. 608-626.

Bibtex

@article{7a18b994a0a04a1db075ea2eb2c71eab,
title = "Weichselian history of the Fennoscandian ice sheet in southern Sweden and the southwestern Baltic Basin",
abstract = "This study presents the Weichselian stratigraphy on Kriegers Flak in the southwestern Baltic Sea, and correlates it to new sections in southernmost Sweden and to previously published stratigraphic sequences from SW Sk{\aa}ne. A total of four Weichselian advances are identified based on our correlations. The oldest till, observed only on Kriegers Flak, is dated to the Early or Middle Weichselian and tentatively correlated to the Ristinge advance, previously identified in Denmark. It is overlain by three interstadial sediment units, starting with brackish clay and followed by terrestrial and lacustrine deposits, which have been dated to 42-36ka, and finally by glaciolacustrine clay dated to 28.5-26ka. After 30ka, the Fennoscandian ice sheet advanced through the Baltic Basin and into the coastal areas of southernmost Sweden where the Allarp Till was deposited, followed by a deglaciation sequence. The uppermost tills, the Dalby Till and the Lund till, were deposited during the LGM advance and the subsequent re-advances through the Baltic Basin. Based on the new evidence it has been possible to identify and date a Middle and Late Weichselian till succession in southern Sweden and provide a strong correlation to the established glacial stratigraphies in Sweden and Denmark.",
author = "Johanna Anjar and Lena Adrielsson and Larsen, {Nicolaj Krog} and Per M{\"o}ller and Kilian Barth",
year = "2014",
doi = "10.1111/bor.12048",
language = "English",
volume = "43",
pages = "608--626",
journal = "Boreas",
issn = "0300-9483",
publisher = "Wiley-Blackwell",
number = "3",

}

RIS

TY - JOUR

T1 - Weichselian history of the Fennoscandian ice sheet in southern Sweden and the southwestern Baltic Basin

AU - Anjar, Johanna

AU - Adrielsson, Lena

AU - Larsen, Nicolaj Krog

AU - Möller, Per

AU - Barth, Kilian

PY - 2014

Y1 - 2014

N2 - This study presents the Weichselian stratigraphy on Kriegers Flak in the southwestern Baltic Sea, and correlates it to new sections in southernmost Sweden and to previously published stratigraphic sequences from SW Skåne. A total of four Weichselian advances are identified based on our correlations. The oldest till, observed only on Kriegers Flak, is dated to the Early or Middle Weichselian and tentatively correlated to the Ristinge advance, previously identified in Denmark. It is overlain by three interstadial sediment units, starting with brackish clay and followed by terrestrial and lacustrine deposits, which have been dated to 42-36ka, and finally by glaciolacustrine clay dated to 28.5-26ka. After 30ka, the Fennoscandian ice sheet advanced through the Baltic Basin and into the coastal areas of southernmost Sweden where the Allarp Till was deposited, followed by a deglaciation sequence. The uppermost tills, the Dalby Till and the Lund till, were deposited during the LGM advance and the subsequent re-advances through the Baltic Basin. Based on the new evidence it has been possible to identify and date a Middle and Late Weichselian till succession in southern Sweden and provide a strong correlation to the established glacial stratigraphies in Sweden and Denmark.

AB - This study presents the Weichselian stratigraphy on Kriegers Flak in the southwestern Baltic Sea, and correlates it to new sections in southernmost Sweden and to previously published stratigraphic sequences from SW Skåne. A total of four Weichselian advances are identified based on our correlations. The oldest till, observed only on Kriegers Flak, is dated to the Early or Middle Weichselian and tentatively correlated to the Ristinge advance, previously identified in Denmark. It is overlain by three interstadial sediment units, starting with brackish clay and followed by terrestrial and lacustrine deposits, which have been dated to 42-36ka, and finally by glaciolacustrine clay dated to 28.5-26ka. After 30ka, the Fennoscandian ice sheet advanced through the Baltic Basin and into the coastal areas of southernmost Sweden where the Allarp Till was deposited, followed by a deglaciation sequence. The uppermost tills, the Dalby Till and the Lund till, were deposited during the LGM advance and the subsequent re-advances through the Baltic Basin. Based on the new evidence it has been possible to identify and date a Middle and Late Weichselian till succession in southern Sweden and provide a strong correlation to the established glacial stratigraphies in Sweden and Denmark.

U2 - 10.1111/bor.12048

DO - 10.1111/bor.12048

M3 - Journal article

AN - SCOPUS:84901917707

VL - 43

SP - 608

EP - 626

JO - Boreas

JF - Boreas

SN - 0300-9483

IS - 3

ER -

ID: 235140490