Seeking the Sources of Dust: Geochemical and Magnetic Studies on “Cryodust” in Glacial Cores from Southern Spitsbergen (Svalbard, Norway)
Natural mineral particulate matter deposited from aerosols and trapped in glaciers—herein defined as “cryodust”—may be an excellent indicator of atmospheric circulation, if terrestrial sources of dust can be identified. In this study, we analyzed the composition of cryodust in shallow ice cores take...
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ftmdpi:oai:mdpi.com:/2073-4433/11/12/1325/ 2023-08-20T04:06:43+02:00 Seeking the Sources of Dust: Geochemical and Magnetic Studies on “Cryodust” in Glacial Cores from Southern Spitsbergen (Svalbard, Norway) Marek Lewandowski Monika A. Kusiak Tomasz Werner Adam Nawrot Barbara Barzycka Michał Laska Bartłomiej Luks agris 2020-12-07 application/pdf https://doi.org/10.3390/atmos11121325 EN eng Multidisciplinary Digital Publishing Institute Aerosols https://dx.doi.org/10.3390/atmos11121325 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 11; Issue 12; Pages: 1325 Svalbard Spitsbergen glacier core mineralogy magnetism dust sources aerosol Text 2020 ftmdpi https://doi.org/10.3390/atmos11121325 2023-08-01T00:36:58Z Natural mineral particulate matter deposited from aerosols and trapped in glaciers—herein defined as “cryodust”—may be an excellent indicator of atmospheric circulation, if terrestrial sources of dust can be identified. In this study, we analyzed the composition of cryodust in shallow ice cores taken from five glaciers in Southern Spitsbergen (Svalbard Archipelago, Northern Norway). The chemical composition, magnetic properties and radiogenic ages of individual grains were measured, where possible, to provide indicators of source areas. To identify mineral and rock fragments, solid particulates were examined by Scanning Electron Microscope fitted with a backscattered electron and Energy Dispersive Spectroscopic detectors. An Electron MicroProbe was employed for the U-Th-Pb chemical dating of monazite grains. Magnetic measurements comprised analyses of magnetic susceptibility (κ) vs. temperature (T) variations and determination of magnetic hysteresis parameters. Monazite ages span 445–423 Ma, consistent with mineral growth during the Caledonian orogeny. Caledonian rocks are exposed in the Nordaustlandet area of North-Eastern Svalbard, and this is the most probable source for monazite grains. Magnetic analyses show a predominance of ferrous (FeII) over ferric (FeIII) phases, consistent with a lack of input from subtropical sources. The results from both methods are consistent with local sources of dust from exposures in the Svalbard archipelago. Text glacier glacier Nordaustlandet Northern Norway Svalbard Spitsbergen MDPI Open Access Publishing Nordaustlandet ENVELOPE(22.400,22.400,79.800,79.800) Norway Svalbard Svalbard Archipelago Atmosphere 11 12 1325 |
institution |
Open Polar |
collection |
MDPI Open Access Publishing |
op_collection_id |
ftmdpi |
language |
English |
topic |
Svalbard Spitsbergen glacier core mineralogy magnetism dust sources aerosol |
spellingShingle |
Svalbard Spitsbergen glacier core mineralogy magnetism dust sources aerosol Marek Lewandowski Monika A. Kusiak Tomasz Werner Adam Nawrot Barbara Barzycka Michał Laska Bartłomiej Luks Seeking the Sources of Dust: Geochemical and Magnetic Studies on “Cryodust” in Glacial Cores from Southern Spitsbergen (Svalbard, Norway) |
topic_facet |
Svalbard Spitsbergen glacier core mineralogy magnetism dust sources aerosol |
description |
Natural mineral particulate matter deposited from aerosols and trapped in glaciers—herein defined as “cryodust”—may be an excellent indicator of atmospheric circulation, if terrestrial sources of dust can be identified. In this study, we analyzed the composition of cryodust in shallow ice cores taken from five glaciers in Southern Spitsbergen (Svalbard Archipelago, Northern Norway). The chemical composition, magnetic properties and radiogenic ages of individual grains were measured, where possible, to provide indicators of source areas. To identify mineral and rock fragments, solid particulates were examined by Scanning Electron Microscope fitted with a backscattered electron and Energy Dispersive Spectroscopic detectors. An Electron MicroProbe was employed for the U-Th-Pb chemical dating of monazite grains. Magnetic measurements comprised analyses of magnetic susceptibility (κ) vs. temperature (T) variations and determination of magnetic hysteresis parameters. Monazite ages span 445–423 Ma, consistent with mineral growth during the Caledonian orogeny. Caledonian rocks are exposed in the Nordaustlandet area of North-Eastern Svalbard, and this is the most probable source for monazite grains. Magnetic analyses show a predominance of ferrous (FeII) over ferric (FeIII) phases, consistent with a lack of input from subtropical sources. The results from both methods are consistent with local sources of dust from exposures in the Svalbard archipelago. |
format |
Text |
author |
Marek Lewandowski Monika A. Kusiak Tomasz Werner Adam Nawrot Barbara Barzycka Michał Laska Bartłomiej Luks |
author_facet |
Marek Lewandowski Monika A. Kusiak Tomasz Werner Adam Nawrot Barbara Barzycka Michał Laska Bartłomiej Luks |
author_sort |
Marek Lewandowski |
title |
Seeking the Sources of Dust: Geochemical and Magnetic Studies on “Cryodust” in Glacial Cores from Southern Spitsbergen (Svalbard, Norway) |
title_short |
Seeking the Sources of Dust: Geochemical and Magnetic Studies on “Cryodust” in Glacial Cores from Southern Spitsbergen (Svalbard, Norway) |
title_full |
Seeking the Sources of Dust: Geochemical and Magnetic Studies on “Cryodust” in Glacial Cores from Southern Spitsbergen (Svalbard, Norway) |
title_fullStr |
Seeking the Sources of Dust: Geochemical and Magnetic Studies on “Cryodust” in Glacial Cores from Southern Spitsbergen (Svalbard, Norway) |
title_full_unstemmed |
Seeking the Sources of Dust: Geochemical and Magnetic Studies on “Cryodust” in Glacial Cores from Southern Spitsbergen (Svalbard, Norway) |
title_sort |
seeking the sources of dust: geochemical and magnetic studies on “cryodust” in glacial cores from southern spitsbergen (svalbard, norway) |
publisher |
Multidisciplinary Digital Publishing Institute |
publishDate |
2020 |
url |
https://doi.org/10.3390/atmos11121325 |
op_coverage |
agris |
long_lat |
ENVELOPE(22.400,22.400,79.800,79.800) |
geographic |
Nordaustlandet Norway Svalbard Svalbard Archipelago |
geographic_facet |
Nordaustlandet Norway Svalbard Svalbard Archipelago |
genre |
glacier glacier Nordaustlandet Northern Norway Svalbard Spitsbergen |
genre_facet |
glacier glacier Nordaustlandet Northern Norway Svalbard Spitsbergen |
op_source |
Atmosphere; Volume 11; Issue 12; Pages: 1325 |
op_relation |
Aerosols https://dx.doi.org/10.3390/atmos11121325 |
op_rights |
https://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.3390/atmos11121325 |
container_title |
Atmosphere |
container_volume |
11 |
container_issue |
12 |
container_start_page |
1325 |
_version_ |
1774717999357362176 |