Transgression Related Holocene Coastal Glendonites from Historic Sites

This study examines the occurrence of glendonite along coastlines since 1825, which have been previously referred to under different names such as Pseudogaylussite, Fundylite, and Kool Hoot across eleven sites. By utilising element ratios and 14C radiometric dating techniques, we establish a more ac...

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Published in:Minerals
Main Authors: Bo Schultz, Jennifer Huggett, Bas van de Schootbrugge, Clemens V. Ullmann, Mathias C. Broch
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/min13091159
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spelling ftmdpi:oai:mdpi.com:/2075-163X/13/9/1159/ 2023-10-01T03:57:12+02:00 Transgression Related Holocene Coastal Glendonites from Historic Sites Bo Schultz Jennifer Huggett Bas van de Schootbrugge Clemens V. Ullmann Mathias C. Broch agris 2023-08-31 application/pdf https://doi.org/10.3390/min13091159 eng eng Multidisciplinary Digital Publishing Institute Crystallography and Physical Chemistry of Minerals & Nanominerals https://dx.doi.org/10.3390/min13091159 https://creativecommons.org/licenses/by/4.0/ Minerals Volume 13 Issue 9 Pages: 1159 Pseudogaylussite Glendonite Ikaite Text 2023 ftmdpi https://doi.org/10.3390/min13091159 2023-09-03T23:54:55Z This study examines the occurrence of glendonite along coastlines since 1825, which have been previously referred to under different names such as Pseudogaylussite, Fundylite, and Kool Hoot across eleven sites. By utilising element ratios and 14C radiometric dating techniques, we establish a more accurate chronology for these varied sites ranging from 10 to 1 thousand years before the present (Ky BP). Sites include tidal flats, coastal barrier islands, and Wadden Sea environments. While some sites still exist, others are only known through publications and museum collections. Our research expands upon previous findings by presenting petrographic evidence that correlates with glendonite formation. Through the examination of the Olenitsa site on the Kola Peninsula, we demonstrate that marine bioclasts enclosed within concretions surrounding glendonites provide temporal context, suggesting that these outcrops were formed during a single event under changing conditions. Notably, certain sediment structures at selected sites indicate the occurrence of cold-water ice-raft storm events and the presence of drop stones. Furthermore, our paper explores the association of historic coastal sites with the formation of ikaite, highlighting the limitations of relying solely on geochemistry and isotopic analysis for interpretation. Intriguingly, we observe that pseudomorphs are abundant in specific areas but absent in adjacent regions with similar environmental, physical, and chemical conditions. No apparent connection is found between volcanic dust cloud-induced cold spells and glendonite. The distribution of coastal glendonites is more likely related to periods of climatic cooling through other means. We show that radiometric dating with 14C provides an indication of age, but the results can be erroneous due to the inclusion of older carbon sources in the analysis. The oldest locations discussed in this study are Kool Hoot (Alaska) and the river Clyde (Scotland), and the youngest glendonites discussed are from the Bay of ... Text kola peninsula Alaska MDPI Open Access Publishing Kola Peninsula Barrier Islands ENVELOPE(-92.283,-92.283,62.784,62.784) Olenitsa ENVELOPE(35.321,35.321,66.470,66.470) Minerals 13 9 1159
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic Pseudogaylussite
Glendonite
Ikaite
spellingShingle Pseudogaylussite
Glendonite
Ikaite
Bo Schultz
Jennifer Huggett
Bas van de Schootbrugge
Clemens V. Ullmann
Mathias C. Broch
Transgression Related Holocene Coastal Glendonites from Historic Sites
topic_facet Pseudogaylussite
Glendonite
Ikaite
description This study examines the occurrence of glendonite along coastlines since 1825, which have been previously referred to under different names such as Pseudogaylussite, Fundylite, and Kool Hoot across eleven sites. By utilising element ratios and 14C radiometric dating techniques, we establish a more accurate chronology for these varied sites ranging from 10 to 1 thousand years before the present (Ky BP). Sites include tidal flats, coastal barrier islands, and Wadden Sea environments. While some sites still exist, others are only known through publications and museum collections. Our research expands upon previous findings by presenting petrographic evidence that correlates with glendonite formation. Through the examination of the Olenitsa site on the Kola Peninsula, we demonstrate that marine bioclasts enclosed within concretions surrounding glendonites provide temporal context, suggesting that these outcrops were formed during a single event under changing conditions. Notably, certain sediment structures at selected sites indicate the occurrence of cold-water ice-raft storm events and the presence of drop stones. Furthermore, our paper explores the association of historic coastal sites with the formation of ikaite, highlighting the limitations of relying solely on geochemistry and isotopic analysis for interpretation. Intriguingly, we observe that pseudomorphs are abundant in specific areas but absent in adjacent regions with similar environmental, physical, and chemical conditions. No apparent connection is found between volcanic dust cloud-induced cold spells and glendonite. The distribution of coastal glendonites is more likely related to periods of climatic cooling through other means. We show that radiometric dating with 14C provides an indication of age, but the results can be erroneous due to the inclusion of older carbon sources in the analysis. The oldest locations discussed in this study are Kool Hoot (Alaska) and the river Clyde (Scotland), and the youngest glendonites discussed are from the Bay of ...
format Text
author Bo Schultz
Jennifer Huggett
Bas van de Schootbrugge
Clemens V. Ullmann
Mathias C. Broch
author_facet Bo Schultz
Jennifer Huggett
Bas van de Schootbrugge
Clemens V. Ullmann
Mathias C. Broch
author_sort Bo Schultz
title Transgression Related Holocene Coastal Glendonites from Historic Sites
title_short Transgression Related Holocene Coastal Glendonites from Historic Sites
title_full Transgression Related Holocene Coastal Glendonites from Historic Sites
title_fullStr Transgression Related Holocene Coastal Glendonites from Historic Sites
title_full_unstemmed Transgression Related Holocene Coastal Glendonites from Historic Sites
title_sort transgression related holocene coastal glendonites from historic sites
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/min13091159
op_coverage agris
long_lat ENVELOPE(-92.283,-92.283,62.784,62.784)
ENVELOPE(35.321,35.321,66.470,66.470)
geographic Kola Peninsula
Barrier Islands
Olenitsa
geographic_facet Kola Peninsula
Barrier Islands
Olenitsa
genre kola peninsula
Alaska
genre_facet kola peninsula
Alaska
op_source Minerals
Volume 13
Issue 9
Pages: 1159
op_relation Crystallography and Physical Chemistry of Minerals & Nanominerals
https://dx.doi.org/10.3390/min13091159
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/min13091159
container_title Minerals
container_volume 13
container_issue 9
container_start_page 1159
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