A multi-millennial record of rock glacier ice chemistry (Lazaun, Italy)

Active rock glaciers—known as mixtures of unconsolidated debris with interstitial ice, ice lenses or a core of massive ice—are widespread indicators of mountain permafrost. The age of a frozen rock glacier core in the Central European Alps (Lazaun, Italy) was dated to about 10,000 years. Here we rep...

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Published in:Frontiers in Earth Science
Main Authors: Ulrike Nickus, Hansjörg Thies, Karl Krainer, Kathrin Lang, Volkmar Mair, David Tonidandel
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media S.A. 2023
Subjects:
Q
Ice
Online Access:https://doi.org/10.3389/feart.2023.1141379
https://doaj.org/article/f15b6049e8c143b7a6ffc52536299647
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spelling ftdoajarticles:oai:doaj.org/article:f15b6049e8c143b7a6ffc52536299647 2023-05-15T16:36:57+02:00 A multi-millennial record of rock glacier ice chemistry (Lazaun, Italy) Ulrike Nickus Hansjörg Thies Karl Krainer Kathrin Lang Volkmar Mair David Tonidandel 2023-03-01T00:00:00Z https://doi.org/10.3389/feart.2023.1141379 https://doaj.org/article/f15b6049e8c143b7a6ffc52536299647 EN eng Frontiers Media S.A. https://www.frontiersin.org/articles/10.3389/feart.2023.1141379/full https://doaj.org/toc/2296-6463 2296-6463 doi:10.3389/feart.2023.1141379 https://doaj.org/article/f15b6049e8c143b7a6ffc52536299647 Frontiers in Earth Science, Vol 11 (2023) alpine permafrost active rock glacier ice core ice chemistry Lazaun Science Q article 2023 ftdoajarticles https://doi.org/10.3389/feart.2023.1141379 2023-03-12T01:34:48Z Active rock glaciers—known as mixtures of unconsolidated debris with interstitial ice, ice lenses or a core of massive ice—are widespread indicators of mountain permafrost. The age of a frozen rock glacier core in the Central European Alps (Lazaun, Italy) was dated to about 10,000 years. Here we report on the chemical composition of the frozen Lazaun core. The ice containing part of the core extended from about 2.8 m down to 24 m depth and consisted of two lobes—both a mix of ice and debris, separated by more than 3 m thick almost ice-free layer. The two lobes of the core showed layers of high solute content and peak values of electrical conductivity exceeding 1,000 μS/cm, but they differed in acidity and metal concentration. High acidity (minimum pH of 4.15) and high levels of elements like nickel, cobalt, zinc, manganese, iron and aluminum characterized the upper lobe, while neutral to alkaline pH and low metal values prevailed in the bottom lobe. We attributed solutes accumulated in the ice matrix to the weathering of bedrock minerals, with peak values favored by the oxidation of pyrite, or by an enhanced reactive surface area in fine-grained sediment layers. The chemical composition of the ice core also revealed signals of prehistoric atmospheric deposition from different sources including wood combustion, metal ore mining, and large volcanic eruptions (Thera, Aniakchak II). To our knowledge, this is the first study that presents the chemical stratigraphy of an entire rock glacier ice core. Article in Journal/Newspaper Ice ice core permafrost Directory of Open Access Journals: DOAJ Articles Frontiers in Earth Science 11
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic alpine permafrost
active rock glacier
ice core
ice chemistry
Lazaun
Science
Q
spellingShingle alpine permafrost
active rock glacier
ice core
ice chemistry
Lazaun
Science
Q
Ulrike Nickus
Hansjörg Thies
Karl Krainer
Kathrin Lang
Volkmar Mair
David Tonidandel
A multi-millennial record of rock glacier ice chemistry (Lazaun, Italy)
topic_facet alpine permafrost
active rock glacier
ice core
ice chemistry
Lazaun
Science
Q
description Active rock glaciers—known as mixtures of unconsolidated debris with interstitial ice, ice lenses or a core of massive ice—are widespread indicators of mountain permafrost. The age of a frozen rock glacier core in the Central European Alps (Lazaun, Italy) was dated to about 10,000 years. Here we report on the chemical composition of the frozen Lazaun core. The ice containing part of the core extended from about 2.8 m down to 24 m depth and consisted of two lobes—both a mix of ice and debris, separated by more than 3 m thick almost ice-free layer. The two lobes of the core showed layers of high solute content and peak values of electrical conductivity exceeding 1,000 μS/cm, but they differed in acidity and metal concentration. High acidity (minimum pH of 4.15) and high levels of elements like nickel, cobalt, zinc, manganese, iron and aluminum characterized the upper lobe, while neutral to alkaline pH and low metal values prevailed in the bottom lobe. We attributed solutes accumulated in the ice matrix to the weathering of bedrock minerals, with peak values favored by the oxidation of pyrite, or by an enhanced reactive surface area in fine-grained sediment layers. The chemical composition of the ice core also revealed signals of prehistoric atmospheric deposition from different sources including wood combustion, metal ore mining, and large volcanic eruptions (Thera, Aniakchak II). To our knowledge, this is the first study that presents the chemical stratigraphy of an entire rock glacier ice core.
format Article in Journal/Newspaper
author Ulrike Nickus
Hansjörg Thies
Karl Krainer
Kathrin Lang
Volkmar Mair
David Tonidandel
author_facet Ulrike Nickus
Hansjörg Thies
Karl Krainer
Kathrin Lang
Volkmar Mair
David Tonidandel
author_sort Ulrike Nickus
title A multi-millennial record of rock glacier ice chemistry (Lazaun, Italy)
title_short A multi-millennial record of rock glacier ice chemistry (Lazaun, Italy)
title_full A multi-millennial record of rock glacier ice chemistry (Lazaun, Italy)
title_fullStr A multi-millennial record of rock glacier ice chemistry (Lazaun, Italy)
title_full_unstemmed A multi-millennial record of rock glacier ice chemistry (Lazaun, Italy)
title_sort multi-millennial record of rock glacier ice chemistry (lazaun, italy)
publisher Frontiers Media S.A.
publishDate 2023
url https://doi.org/10.3389/feart.2023.1141379
https://doaj.org/article/f15b6049e8c143b7a6ffc52536299647
genre Ice
ice core
permafrost
genre_facet Ice
ice core
permafrost
op_source Frontiers in Earth Science, Vol 11 (2023)
op_relation https://www.frontiersin.org/articles/10.3389/feart.2023.1141379/full
https://doaj.org/toc/2296-6463
2296-6463
doi:10.3389/feart.2023.1141379
https://doaj.org/article/f15b6049e8c143b7a6ffc52536299647
op_doi https://doi.org/10.3389/feart.2023.1141379
container_title Frontiers in Earth Science
container_volume 11
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