Supplementary information files for Increased North Atlantic dust deposition linked to Holocene Icelandic glacier fluctuations ...

Supplementary files for article Increased North Atlantic dust deposition linked to Holocene Icelandic glacier fluctuationsMineral dust concentrations are coupled to climate over glacial-interglacial cycles with increased dust deposition occurring during major cold phases over the last ~100 ka. Holoc...

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Main Authors: Stewart, Helena, Bradwell, Tom, Bullard, Joanna, D. McCulloch, Robert, Millar, Ian
Format: Dataset
Language:unknown
Published: Loughborough University 2023
Subjects:
Online Access:https://dx.doi.org/10.17028/rd.lboro.23966415
https://repository.lboro.ac.uk/articles/dataset/Supplementary_information_files_for_Increased_North_Atlantic_dust_deposition_linked_to_Holocene_Icelandic_glacier_fluctuations/23966415
id ftdatacite:10.17028/rd.lboro.23966415
record_format openpolar
spelling ftdatacite:10.17028/rd.lboro.23966415 2023-10-01T03:57:52+02:00 Supplementary information files for Increased North Atlantic dust deposition linked to Holocene Icelandic glacier fluctuations ... Stewart, Helena Bradwell, Tom Bullard, Joanna D. McCulloch, Robert Millar, Ian 2023 https://dx.doi.org/10.17028/rd.lboro.23966415 https://repository.lboro.ac.uk/articles/dataset/Supplementary_information_files_for_Increased_North_Atlantic_dust_deposition_linked_to_Holocene_Icelandic_glacier_fluctuations/23966415 unknown Loughborough University https://hdl.handle.net/2134/20936392 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Geology not elsewhere classified Archaeology not elsewhere classified Dataset dataset 2023 ftdatacite https://doi.org/10.17028/rd.lboro.23966415 2023-09-04T14:02:36Z Supplementary files for article Increased North Atlantic dust deposition linked to Holocene Icelandic glacier fluctuationsMineral dust concentrations are coupled to climate over glacial-interglacial cycles with increased dust deposition occurring during major cold phases over the last ~100 ka. Holocene records suggest considerable spatial and temporal variability in the magnitude, frequency and timing of dust peaks that reflects regional or local drivers of dust emissions and transport. Here, we present stratigraphical, geochemical and isotopic evidence for dust deposition from two high-resolution peat sequences 200 km apart in northern Scotland spanning the last c. 8200 years. εNd isotope data suggest the dominant minerogenic dust source switches between a low latitude (likely Saharan) and a high latitude, Icelandic source. Marked peaks in increased minerogenic dust deposition at: c. 5.4–5.1, 4.0–3.9, 2.8–2.6, 1.0 and 0.3 ka BP occur against a backdrop of low dust deposition during the mid-Holocene (c. ... Dataset North Atlantic 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 unknown
topic Geology not elsewhere classified
Archaeology not elsewhere classified
spellingShingle Geology not elsewhere classified
Archaeology not elsewhere classified
Stewart, Helena
Bradwell, Tom
Bullard, Joanna
D. McCulloch, Robert
Millar, Ian
Supplementary information files for Increased North Atlantic dust deposition linked to Holocene Icelandic glacier fluctuations ...
topic_facet Geology not elsewhere classified
Archaeology not elsewhere classified
description Supplementary files for article Increased North Atlantic dust deposition linked to Holocene Icelandic glacier fluctuationsMineral dust concentrations are coupled to climate over glacial-interglacial cycles with increased dust deposition occurring during major cold phases over the last ~100 ka. Holocene records suggest considerable spatial and temporal variability in the magnitude, frequency and timing of dust peaks that reflects regional or local drivers of dust emissions and transport. Here, we present stratigraphical, geochemical and isotopic evidence for dust deposition from two high-resolution peat sequences 200 km apart in northern Scotland spanning the last c. 8200 years. εNd isotope data suggest the dominant minerogenic dust source switches between a low latitude (likely Saharan) and a high latitude, Icelandic source. Marked peaks in increased minerogenic dust deposition at: c. 5.4–5.1, 4.0–3.9, 2.8–2.6, 1.0 and 0.3 ka BP occur against a backdrop of low dust deposition during the mid-Holocene (c. ...
format Dataset
author Stewart, Helena
Bradwell, Tom
Bullard, Joanna
D. McCulloch, Robert
Millar, Ian
author_facet Stewart, Helena
Bradwell, Tom
Bullard, Joanna
D. McCulloch, Robert
Millar, Ian
author_sort Stewart, Helena
title Supplementary information files for Increased North Atlantic dust deposition linked to Holocene Icelandic glacier fluctuations ...
title_short Supplementary information files for Increased North Atlantic dust deposition linked to Holocene Icelandic glacier fluctuations ...
title_full Supplementary information files for Increased North Atlantic dust deposition linked to Holocene Icelandic glacier fluctuations ...
title_fullStr Supplementary information files for Increased North Atlantic dust deposition linked to Holocene Icelandic glacier fluctuations ...
title_full_unstemmed Supplementary information files for Increased North Atlantic dust deposition linked to Holocene Icelandic glacier fluctuations ...
title_sort supplementary information files for increased north atlantic dust deposition linked to holocene icelandic glacier fluctuations ...
publisher Loughborough University
publishDate 2023
url https://dx.doi.org/10.17028/rd.lboro.23966415
https://repository.lboro.ac.uk/articles/dataset/Supplementary_information_files_for_Increased_North_Atlantic_dust_deposition_linked_to_Holocene_Icelandic_glacier_fluctuations/23966415
genre North Atlantic
genre_facet North Atlantic
op_relation https://hdl.handle.net/2134/20936392
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.17028/rd.lboro.23966415
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