Evidence of ameliorated Middle Weichselian climate and sub-arctic environment in the western Baltic region: coring lake sediments at Klintholm, Møn, Denmark

Michael Houmark-Nielsen; Ole Bennike; Geoffrey Lemdahl; Christoph Lüthgens

doi:10.1111/bor.12159

Evidence of ameliorated Middle Weichselian climate and sub-arctic environment in the western Baltic region: coring lake sediments at Klintholm, Møn, Denmark

Michael Houmark-Nielsen, Ole Bennike, Geoffrey Lemdahl, Christoph Lüthgens

3 Citations (Scopus)

Abstract

Coring through glaciotectonically stacked Quaternary sediments situated below sea level on the island of Møn, Denmark, recovered a succession of interstadial sediments of Middle Weichselian age. Plant and animal remains including insects found in laminated sand and mud indicate deposition in a lake surrounded by dwarf shrubs, herbs, mosses and rare trees. The insect fauna indicates a mean July temperature of 8-12 °C, suggesting an arctic to sub-arctic environment, while winter temperatures around -8 to -22 °C suggest periglacial conditions with permafrost. Luminescence dating of sediment samples gave ages from 48-29 ka, and radiocarbon dating indicates deposition of plant fragments between 45 and 36 ka BP. The fossil assemblage from Møn shows close resemblance to those from other sites with similar ages found in the vicinity of the western Baltic Basin.

Original language	English
Journal	Boreas
Volume	45
Issue number	2
Pages (from-to)	347-359
Number of pages	13
ISSN	0300-9483
DOIs	https://doi.org/10.1111/bor.12159
Publication status	Published - 1 Apr 2016

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title = "Evidence of ameliorated Middle Weichselian climate and sub-arctic environment in the western Baltic region: coring lake sediments at Klintholm, M{\o}n, Denmark",

abstract = "Coring through glaciotectonically stacked Quaternary sediments situated below sea level on the island of M{\o}n, Denmark, recovered a succession of interstadial sediments of Middle Weichselian age. Plant and animal remains including insects found in laminated sand and mud indicate deposition in a lake surrounded by dwarf shrubs, herbs, mosses and rare trees. The insect fauna indicates a mean July temperature of 8-12 °C, suggesting an arctic to sub-arctic environment, while winter temperatures around -8 to -22 °C suggest periglacial conditions with permafrost. Luminescence dating of sediment samples gave ages from 48-29 ka, and radiocarbon dating indicates deposition of plant fragments between 45 and 36 ka BP. The fossil assemblage from M{\o}n shows close resemblance to those from other sites with similar ages found in the vicinity of the western Baltic Basin.",

author = "Michael Houmark-Nielsen and Ole Bennike and Geoffrey Lemdahl and Christoph L{\"u}thgens",

year = "2016",

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doi = "10.1111/bor.12159",

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volume = "45",

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TY - JOUR

T1 - Evidence of ameliorated Middle Weichselian climate and sub-arctic environment in the western Baltic region

T2 - coring lake sediments at Klintholm, Møn, Denmark

AU - Houmark-Nielsen, Michael

AU - Bennike, Ole

AU - Lemdahl, Geoffrey

AU - Lüthgens, Christoph

PY - 2016/4/1

Y1 - 2016/4/1

N2 - Coring through glaciotectonically stacked Quaternary sediments situated below sea level on the island of Møn, Denmark, recovered a succession of interstadial sediments of Middle Weichselian age. Plant and animal remains including insects found in laminated sand and mud indicate deposition in a lake surrounded by dwarf shrubs, herbs, mosses and rare trees. The insect fauna indicates a mean July temperature of 8-12 °C, suggesting an arctic to sub-arctic environment, while winter temperatures around -8 to -22 °C suggest periglacial conditions with permafrost. Luminescence dating of sediment samples gave ages from 48-29 ka, and radiocarbon dating indicates deposition of plant fragments between 45 and 36 ka BP. The fossil assemblage from Møn shows close resemblance to those from other sites with similar ages found in the vicinity of the western Baltic Basin.

AB - Coring through glaciotectonically stacked Quaternary sediments situated below sea level on the island of Møn, Denmark, recovered a succession of interstadial sediments of Middle Weichselian age. Plant and animal remains including insects found in laminated sand and mud indicate deposition in a lake surrounded by dwarf shrubs, herbs, mosses and rare trees. The insect fauna indicates a mean July temperature of 8-12 °C, suggesting an arctic to sub-arctic environment, while winter temperatures around -8 to -22 °C suggest periglacial conditions with permafrost. Luminescence dating of sediment samples gave ages from 48-29 ka, and radiocarbon dating indicates deposition of plant fragments between 45 and 36 ka BP. The fossil assemblage from Møn shows close resemblance to those from other sites with similar ages found in the vicinity of the western Baltic Basin.

U2 - 10.1111/bor.12159

DO - 10.1111/bor.12159

M3 - Journal article

SN - 0300-9483

VL - 45

SP - 347

EP - 359

JO - Boreas

JF - Boreas

IS - 2

ER -

Evidence of ameliorated Middle Weichselian climate and sub-arctic environment in the western Baltic region: coring lake sediments at Klintholm, Møn, Denmark

Abstract

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