Late Weichselian (fluvio-)aeolian sediments and Holocene drift-sands of the classic type locality in Twente (E Netherlands): a high-resolution dating study using optically stimulated luminescence
The Late Weichselian and Holocene (fluvio-)aeolian sands of the type locality Lutterzand in the E Netherlands have been the focus of many palaeoclimatic, palaeoenvironmental and geochronological studies. In the present study, an accurate and detailed chronological framework has been established usin...
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2013
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ftvuamstcris:oai:research.vu.nl:publications/db41505d-c2d7-4e63-b1a6-3158bd706857 2024-09-30T14:41:16+00:00 Late Weichselian (fluvio-)aeolian sediments and Holocene drift-sands of the classic type locality in Twente (E Netherlands): a high-resolution dating study using optically stimulated luminescence Vandenberghe, D.A.G. Derese, C. Kasse, C. Van den haute, P. 2013 https://research.vu.nl/en/publications/db41505d-c2d7-4e63-b1a6-3158bd706857 https://doi.org/10.1016/j.quascirev.2013.02.009 https://hdl.handle.net/1871.1/db41505d-c2d7-4e63-b1a6-3158bd706857 eng eng https://research.vu.nl/en/publications/db41505d-c2d7-4e63-b1a6-3158bd706857 info:eu-repo/semantics/restrictedAccess Vandenberghe , D A G , Derese , C , Kasse , C & Van den haute , P 2013 , ' Late Weichselian (fluvio-)aeolian sediments and Holocene drift-sands of the classic type locality in Twente (E Netherlands): a high-resolution dating study using optically stimulated luminescence ' , Quaternary Science Reviews , vol. 68 , pp. 96-113 . https://doi.org/10.1016/j.quascirev.2013.02.009 /dk/atira/pure/sustainabledevelopmentgoals/life_below_water name=SDG 14 - Life Below Water article 2013 ftvuamstcris https://doi.org/10.1016/j.quascirev.2013.02.009 2024-09-05T00:23:22Z The Late Weichselian and Holocene (fluvio-)aeolian sands of the type locality Lutterzand in the E Netherlands have been the focus of many palaeoclimatic, palaeoenvironmental and geochronological studies. In the present study, an accurate and detailed chronological framework has been established using radiocarbon and optically stimulated luminescence dating. Additionally, the sedimentological characteristics of the fluvio-aeolian and aeolian sequences have been reinvestigated.Four main phases of (fluvio)aeolian sedimentation have been differentiated in the Lutterzand sections, consistent with the Late Pleniglacial, the pre-Allerød Lateglacial, the Late Dryas, and the Late Holocene. From at least 25.2 ± 1.9 ka up to 19.9 ± 1.6 ka, the area was marked by a transition from fluvial to aeolian deposition under continuous permafrost conditions (Older Coversand I). The Beuningen Gravel Bed is considered as the lithostratigraphic marker for permafrost degradation, shallow channelling and aeolian deflation associated with the formation of a desert pavement. Localised fluvial sedimentation in shallow channels took place in two phases, a first from ~20 ka to ~23 ka, and a second at around 16 ka; the desert pavement formed in between ~16 ka and ~14 ka, but probably shortly after 16 ka. The aeolian sediments overlying the Beuningen Gravel Bed were deposited as sand sheets and low dunes, and yielded ages between 15.8 ± 1.4 ka and 12.2 ± 0.9 ka. Although the OSL ages seem to point to fairly continuous coversand sedimentation during the Lateglacial, the intercalated Usselo Soil allows distinguishing a pre-Allerød phase (resulting in the Older Coversand II and the Younger Coversand I between 15.8 ± 1.4 ka and 12.3 ± 1.0 ka) from a post-Allerød phase (with deposition of the Younger Coversand II between 13.6 ± 1.1 ka and 12.2 ± 0.9 ka). During the major part of the Holocene, (podzol) soil formation occurred in the top of the aeolian sediments. Probably due to human activities, local erosion of the upper part of the Lateglacial ... Article in Journal/Newspaper permafrost Vrije Universiteit Amsterdam (VU): Research Portal Quaternary Science Reviews 68 96 113 |
institution |
Open Polar |
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Vrije Universiteit Amsterdam (VU): Research Portal |
op_collection_id |
ftvuamstcris |
language |
English |
topic |
/dk/atira/pure/sustainabledevelopmentgoals/life_below_water name=SDG 14 - Life Below Water |
spellingShingle |
/dk/atira/pure/sustainabledevelopmentgoals/life_below_water name=SDG 14 - Life Below Water Vandenberghe, D.A.G. Derese, C. Kasse, C. Van den haute, P. Late Weichselian (fluvio-)aeolian sediments and Holocene drift-sands of the classic type locality in Twente (E Netherlands): a high-resolution dating study using optically stimulated luminescence |
topic_facet |
/dk/atira/pure/sustainabledevelopmentgoals/life_below_water name=SDG 14 - Life Below Water |
description |
The Late Weichselian and Holocene (fluvio-)aeolian sands of the type locality Lutterzand in the E Netherlands have been the focus of many palaeoclimatic, palaeoenvironmental and geochronological studies. In the present study, an accurate and detailed chronological framework has been established using radiocarbon and optically stimulated luminescence dating. Additionally, the sedimentological characteristics of the fluvio-aeolian and aeolian sequences have been reinvestigated.Four main phases of (fluvio)aeolian sedimentation have been differentiated in the Lutterzand sections, consistent with the Late Pleniglacial, the pre-Allerød Lateglacial, the Late Dryas, and the Late Holocene. From at least 25.2 ± 1.9 ka up to 19.9 ± 1.6 ka, the area was marked by a transition from fluvial to aeolian deposition under continuous permafrost conditions (Older Coversand I). The Beuningen Gravel Bed is considered as the lithostratigraphic marker for permafrost degradation, shallow channelling and aeolian deflation associated with the formation of a desert pavement. Localised fluvial sedimentation in shallow channels took place in two phases, a first from ~20 ka to ~23 ka, and a second at around 16 ka; the desert pavement formed in between ~16 ka and ~14 ka, but probably shortly after 16 ka. The aeolian sediments overlying the Beuningen Gravel Bed were deposited as sand sheets and low dunes, and yielded ages between 15.8 ± 1.4 ka and 12.2 ± 0.9 ka. Although the OSL ages seem to point to fairly continuous coversand sedimentation during the Lateglacial, the intercalated Usselo Soil allows distinguishing a pre-Allerød phase (resulting in the Older Coversand II and the Younger Coversand I between 15.8 ± 1.4 ka and 12.3 ± 1.0 ka) from a post-Allerød phase (with deposition of the Younger Coversand II between 13.6 ± 1.1 ka and 12.2 ± 0.9 ka). During the major part of the Holocene, (podzol) soil formation occurred in the top of the aeolian sediments. Probably due to human activities, local erosion of the upper part of the Lateglacial ... |
format |
Article in Journal/Newspaper |
author |
Vandenberghe, D.A.G. Derese, C. Kasse, C. Van den haute, P. |
author_facet |
Vandenberghe, D.A.G. Derese, C. Kasse, C. Van den haute, P. |
author_sort |
Vandenberghe, D.A.G. |
title |
Late Weichselian (fluvio-)aeolian sediments and Holocene drift-sands of the classic type locality in Twente (E Netherlands): a high-resolution dating study using optically stimulated luminescence |
title_short |
Late Weichselian (fluvio-)aeolian sediments and Holocene drift-sands of the classic type locality in Twente (E Netherlands): a high-resolution dating study using optically stimulated luminescence |
title_full |
Late Weichselian (fluvio-)aeolian sediments and Holocene drift-sands of the classic type locality in Twente (E Netherlands): a high-resolution dating study using optically stimulated luminescence |
title_fullStr |
Late Weichselian (fluvio-)aeolian sediments and Holocene drift-sands of the classic type locality in Twente (E Netherlands): a high-resolution dating study using optically stimulated luminescence |
title_full_unstemmed |
Late Weichselian (fluvio-)aeolian sediments and Holocene drift-sands of the classic type locality in Twente (E Netherlands): a high-resolution dating study using optically stimulated luminescence |
title_sort |
late weichselian (fluvio-)aeolian sediments and holocene drift-sands of the classic type locality in twente (e netherlands): a high-resolution dating study using optically stimulated luminescence |
publishDate |
2013 |
url |
https://research.vu.nl/en/publications/db41505d-c2d7-4e63-b1a6-3158bd706857 https://doi.org/10.1016/j.quascirev.2013.02.009 https://hdl.handle.net/1871.1/db41505d-c2d7-4e63-b1a6-3158bd706857 |
genre |
permafrost |
genre_facet |
permafrost |
op_source |
Vandenberghe , D A G , Derese , C , Kasse , C & Van den haute , P 2013 , ' Late Weichselian (fluvio-)aeolian sediments and Holocene drift-sands of the classic type locality in Twente (E Netherlands): a high-resolution dating study using optically stimulated luminescence ' , Quaternary Science Reviews , vol. 68 , pp. 96-113 . https://doi.org/10.1016/j.quascirev.2013.02.009 |
op_relation |
https://research.vu.nl/en/publications/db41505d-c2d7-4e63-b1a6-3158bd706857 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1016/j.quascirev.2013.02.009 |
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