The Heliconoides Modified Dissolution Index-HMDI: Do methane seepage environments affect the preservation state of Heliconoides inflatus?

Pteropods are holoplanktonic molluscs presently endangered because their fragile aragonitic shell is very sensitive to ocean acidification. The preservation of pteropods, and in particular of the mesopelagic Heliconoides (Limacina) inflatus, has been used to assess aragonite saturation state in Quat...

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Published in:Ecological Indicators
Main Authors: Beccari, Valentina, Almogi-Labin, Ahuva, Basso, Daniela, Panieri, Giuliana, Makovsky, Yizhaq, Neururer, Christoph, Hajdas, Irka, Spezzaferri, Silvia
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2023
Subjects:
Online Access:https://hdl.handle.net/10037/29268
https://doi.org/10.1016/j.ecolind.2023.110380
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author Beccari, Valentina
Almogi-Labin, Ahuva
Basso, Daniela
Panieri, Giuliana
Makovsky, Yizhaq
Neururer, Christoph
Hajdas, Irka
Spezzaferri, Silvia
author_facet Beccari, Valentina
Almogi-Labin, Ahuva
Basso, Daniela
Panieri, Giuliana
Makovsky, Yizhaq
Neururer, Christoph
Hajdas, Irka
Spezzaferri, Silvia
author_sort Beccari, Valentina
collection University of Tromsø: Munin Open Research Archive
container_start_page 110380
container_title Ecological Indicators
container_volume 152
description Pteropods are holoplanktonic molluscs presently endangered because their fragile aragonitic shell is very sensitive to ocean acidification. The preservation of pteropods, and in particular of the mesopelagic Heliconoides (Limacina) inflatus, has been used to assess aragonite saturation state in Quaternary sediments (Limacina Dissolution Index, LDX) as an inferred proxy for climatic changes. Three deep-sea cores retrieved in 2016 during the EUROFLEETS2 SEMSEEP cruise offshore Israel are investigated to assess the preservation degree of H. inflatus (d'Orbigny, 1835) in representative environments across the base of the southeastern Mediterranean margin (cold water coral, active seepage pockmark and deep sea channel areas). In some core intervals, yellowish, recrystallized internal molds of this species are present. They have been previously observed in the Eastern Mediterranean, but the nature and origin of their colour was never explained. Scanning Electron Microscopy (SEM), Energy Dispersive Spectroscopy (EDS) and Electron Backscatter Diffraction (EBSD) revealed that the recrystallized molds of the H. inflatus shells are formed by aragonite needles and high-Mg calcite crystals. The formation and preservation of these internal molds is induced by advective methane emissions, typically precipitating aragonite and High-Mg calcite phases close to the sediment–water interface. These molds were never used in previous applications of the LDX or in any existing ranking of pteropod preservation. Therefore, we have categorized these peculiar features combining previous pteropod ranking descriptions with the new observations to develop a modified biotic index (Heliconoides Modified Dissolution Index-HMDI). High values of the HMDI at the base of the pockmark core correspond to the interval where also active seepage-related features – e.g., bubble emissions, low-oxygen benthic foraminifera, chemosymbiotic molluscs, small fragments of authigenic carbonate crusts and slightly depleted δ 13 C values – occur, showing the ...
format Article in Journal/Newspaper
genre Ocean acidification
genre_facet Ocean acidification
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institution Open Polar
language English
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op_doi https://doi.org/10.1016/j.ecolind.2023.110380
op_relation Ecological Indicators
info:eu-repo/grantAgreement/EC/FP7-INFRASTRUCTURES/312762r/EU/New operational steps towards an alliance of European research fleets/EUROFLEETS2/
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doi:10.1016/j.ecolind.2023.110380
https://hdl.handle.net/10037/29268
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spelling ftunivtroemsoe:oai:munin.uit.no:10037/29268 2025-04-13T14:25:07+00:00 The Heliconoides Modified Dissolution Index-HMDI: Do methane seepage environments affect the preservation state of Heliconoides inflatus? Beccari, Valentina Almogi-Labin, Ahuva Basso, Daniela Panieri, Giuliana Makovsky, Yizhaq Neururer, Christoph Hajdas, Irka Spezzaferri, Silvia 2023-05-24 https://hdl.handle.net/10037/29268 https://doi.org/10.1016/j.ecolind.2023.110380 eng eng Elsevier Ecological Indicators info:eu-repo/grantAgreement/EC/FP7-INFRASTRUCTURES/312762r/EU/New operational steps towards an alliance of European research fleets/EUROFLEETS2/ FRIDAID 2149117 doi:10.1016/j.ecolind.2023.110380 https://hdl.handle.net/10037/29268 Attribution 4.0 International (CC BY 4.0) openAccess Copyright 2023 The Author(s) https://creativecommons.org/licenses/by/4.0 Journal article Tidsskriftartikkel Peer reviewed publishedVersion 2023 ftunivtroemsoe https://doi.org/10.1016/j.ecolind.2023.110380 2025-03-14T05:17:56Z Pteropods are holoplanktonic molluscs presently endangered because their fragile aragonitic shell is very sensitive to ocean acidification. The preservation of pteropods, and in particular of the mesopelagic Heliconoides (Limacina) inflatus, has been used to assess aragonite saturation state in Quaternary sediments (Limacina Dissolution Index, LDX) as an inferred proxy for climatic changes. Three deep-sea cores retrieved in 2016 during the EUROFLEETS2 SEMSEEP cruise offshore Israel are investigated to assess the preservation degree of H. inflatus (d'Orbigny, 1835) in representative environments across the base of the southeastern Mediterranean margin (cold water coral, active seepage pockmark and deep sea channel areas). In some core intervals, yellowish, recrystallized internal molds of this species are present. They have been previously observed in the Eastern Mediterranean, but the nature and origin of their colour was never explained. Scanning Electron Microscopy (SEM), Energy Dispersive Spectroscopy (EDS) and Electron Backscatter Diffraction (EBSD) revealed that the recrystallized molds of the H. inflatus shells are formed by aragonite needles and high-Mg calcite crystals. The formation and preservation of these internal molds is induced by advective methane emissions, typically precipitating aragonite and High-Mg calcite phases close to the sediment–water interface. These molds were never used in previous applications of the LDX or in any existing ranking of pteropod preservation. Therefore, we have categorized these peculiar features combining previous pteropod ranking descriptions with the new observations to develop a modified biotic index (Heliconoides Modified Dissolution Index-HMDI). High values of the HMDI at the base of the pockmark core correspond to the interval where also active seepage-related features – e.g., bubble emissions, low-oxygen benthic foraminifera, chemosymbiotic molluscs, small fragments of authigenic carbonate crusts and slightly depleted δ 13 C values – occur, showing the ... Article in Journal/Newspaper Ocean acidification University of Tromsø: Munin Open Research Archive Ecological Indicators 152 110380
spellingShingle Beccari, Valentina
Almogi-Labin, Ahuva
Basso, Daniela
Panieri, Giuliana
Makovsky, Yizhaq
Neururer, Christoph
Hajdas, Irka
Spezzaferri, Silvia
The Heliconoides Modified Dissolution Index-HMDI: Do methane seepage environments affect the preservation state of Heliconoides inflatus?
title The Heliconoides Modified Dissolution Index-HMDI: Do methane seepage environments affect the preservation state of Heliconoides inflatus?
title_full The Heliconoides Modified Dissolution Index-HMDI: Do methane seepage environments affect the preservation state of Heliconoides inflatus?
title_fullStr The Heliconoides Modified Dissolution Index-HMDI: Do methane seepage environments affect the preservation state of Heliconoides inflatus?
title_full_unstemmed The Heliconoides Modified Dissolution Index-HMDI: Do methane seepage environments affect the preservation state of Heliconoides inflatus?
title_short The Heliconoides Modified Dissolution Index-HMDI: Do methane seepage environments affect the preservation state of Heliconoides inflatus?
title_sort heliconoides modified dissolution index-hmdi: do methane seepage environments affect the preservation state of heliconoides inflatus?
url https://hdl.handle.net/10037/29268
https://doi.org/10.1016/j.ecolind.2023.110380