A Stratigraphical-Sedimentological Study of the Last Interglacial Period in the Central Nordic Seas on the Basis of XRF Core Scanning

Abstract: The recognition of specific geological time intervals is one of the major issues when establishing the stratigraphies of marine sediment cores. The automatic XRF core scanning method provides a fast and non-destructive method to precisely identify a given time interval and its changeable s...

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Main Authors: Kolling, Henriette, Bauch, A Henning
Format: Article in Journal/Newspaper
Language:English
Published: Alfred-Wegener-Institut für Polar- und Meeresforschung und Deutsche Gesellschaft für Polarforschung  2017
Subjects:
Online Access:https://dx.doi.org/10.2312/polarforschung.87.1.15
https://www.tib.eu/suchen/id/awi:f825f2eb3a8d08a3808a5de8320bce3cde31097b
id ftdatacite:10.2312/polarforschung.87.1.15
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spelling ftdatacite:10.2312/polarforschung.87.1.15 2023-05-15T17:24:20+02:00 A Stratigraphical-Sedimentological Study of the Last Interglacial Period in the Central Nordic Seas on the Basis of XRF Core Scanning Kolling, Henriette Bauch, A Henning 2017 application/pdf https://dx.doi.org/10.2312/polarforschung.87.1.15 https://www.tib.eu/suchen/id/awi:f825f2eb3a8d08a3808a5de8320bce3cde31097b en eng Alfred-Wegener-Institut für Polar- und Meeresforschung und Deutsche Gesellschaft für Polarforschung  Alfred-Wegener-Institut für Polar- und Meeresforschung und Deutsche Gesellschaft für Polarforschung Earth Science Earth sciences and geology article-journal Electronic Resource ScholarlyArticle JournalArticle 2017 ftdatacite https://doi.org/10.2312/polarforschung.87.1.15 2022-04-01T17:57:47Z Abstract: The recognition of specific geological time intervals is one of the major issues when establishing the stratigraphies of marine sediment cores. The automatic XRF core scanning method provides a fast and non-destructive method to precisely identify a given time interval and its changeable sedi- mentation histories. To test the applicability of XRF core scanning to recog- nize such periods, we studied in detail sedimentation processes across the last interglacial climate cycle (MIS 5e) on unsampled sediment core section from the central Nordic Seas – an area of high interest for paleoceanographic reconstructions. To further ground truth the XRF scanning results the core was sampled and the contents of iceberg-rafted debris (IRD) and shards of tephra were quantified. On that basis we identified Ti/Ca ratios as a potential indicator for IRD depositional peaks, and Ca as indicator of high biogenic carbonate production. Two well-known tephras from MIS 5e, Midt-RHY and 5e-low/Bas-IV, could be identified based on specific elemental content, such as Si, Ti, Zr, and Rb. By cross-core correlations using Ca-content and IRD-counts, the iceberg-free interval with enhanced deposition of biogenic carbonate lasted for about 9 ky, with a return of significant iceberg presence around 115 ka, notifying the onset of the last glacial inception. According to the age model applied we could further define the age of the 5e-Midt-RHY tephra at ~121.5 ka and of the 5e-low/Bas-IV at ~125.5 ka. : Polarforschung Article in Journal/Newspaper Nordic Seas DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Earth Science
Earth sciences and geology
spellingShingle Earth Science
Earth sciences and geology
Kolling, Henriette
Bauch, A Henning
A Stratigraphical-Sedimentological Study of the Last Interglacial Period in the Central Nordic Seas on the Basis of XRF Core Scanning
topic_facet Earth Science
Earth sciences and geology
description Abstract: The recognition of specific geological time intervals is one of the major issues when establishing the stratigraphies of marine sediment cores. The automatic XRF core scanning method provides a fast and non-destructive method to precisely identify a given time interval and its changeable sedi- mentation histories. To test the applicability of XRF core scanning to recog- nize such periods, we studied in detail sedimentation processes across the last interglacial climate cycle (MIS 5e) on unsampled sediment core section from the central Nordic Seas – an area of high interest for paleoceanographic reconstructions. To further ground truth the XRF scanning results the core was sampled and the contents of iceberg-rafted debris (IRD) and shards of tephra were quantified. On that basis we identified Ti/Ca ratios as a potential indicator for IRD depositional peaks, and Ca as indicator of high biogenic carbonate production. Two well-known tephras from MIS 5e, Midt-RHY and 5e-low/Bas-IV, could be identified based on specific elemental content, such as Si, Ti, Zr, and Rb. By cross-core correlations using Ca-content and IRD-counts, the iceberg-free interval with enhanced deposition of biogenic carbonate lasted for about 9 ky, with a return of significant iceberg presence around 115 ka, notifying the onset of the last glacial inception. According to the age model applied we could further define the age of the 5e-Midt-RHY tephra at ~121.5 ka and of the 5e-low/Bas-IV at ~125.5 ka. : Polarforschung
format Article in Journal/Newspaper
author Kolling, Henriette
Bauch, A Henning
author_facet Kolling, Henriette
Bauch, A Henning
author_sort Kolling, Henriette
title A Stratigraphical-Sedimentological Study of the Last Interglacial Period in the Central Nordic Seas on the Basis of XRF Core Scanning
title_short A Stratigraphical-Sedimentological Study of the Last Interglacial Period in the Central Nordic Seas on the Basis of XRF Core Scanning
title_full A Stratigraphical-Sedimentological Study of the Last Interglacial Period in the Central Nordic Seas on the Basis of XRF Core Scanning
title_fullStr A Stratigraphical-Sedimentological Study of the Last Interglacial Period in the Central Nordic Seas on the Basis of XRF Core Scanning
title_full_unstemmed A Stratigraphical-Sedimentological Study of the Last Interglacial Period in the Central Nordic Seas on the Basis of XRF Core Scanning
title_sort stratigraphical-sedimentological study of the last interglacial period in the central nordic seas on the basis of xrf core scanning
publisher Alfred-Wegener-Institut für Polar- und Meeresforschung und Deutsche Gesellschaft für Polarforschung 
publishDate 2017
url https://dx.doi.org/10.2312/polarforschung.87.1.15
https://www.tib.eu/suchen/id/awi:f825f2eb3a8d08a3808a5de8320bce3cde31097b
genre Nordic Seas
genre_facet Nordic Seas
op_rights Alfred-Wegener-Institut für Polar- und Meeresforschung und Deutsche Gesellschaft für Polarforschung
op_doi https://doi.org/10.2312/polarforschung.87.1.15
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