Ice-related environmental changes in Arctic fjords : new insights from benthic foraminifera

Climate change threatens polar regions with major consequences on ice-related dynamics and linked ecosystems. Predictions of future sea ice cover and glacier retreat rely on paleoenvironmental reconstructions (through proxies’ application) to extend the instrumental period and thus reduce models’ un...

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Main Author: Fossile, Eleonora
Other Authors: Bio-Indicateurs Actuels et Fossiles (BIAF), Université d'Angers (UA), Université d'Angers, Hélène Howa, Meryem Mojtahid, Maria-Pia Nardelli
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: HAL CCSD 2022
Subjects:
Online Access:https://theses.hal.science/tel-04089929
https://theses.hal.science/tel-04089929/document
https://theses.hal.science/tel-04089929/file/pdffix_these_FOSSILE.pdf
id ftccsdartic:oai:HAL:tel-04089929v1
record_format openpolar
spelling ftccsdartic:oai:HAL:tel-04089929v1 2023-06-11T04:09:21+02:00 Ice-related environmental changes in Arctic fjords : new insights from benthic foraminifera Changements environnementaux liés à la dynamique de la glace dans les fjords de l’Arctique : nouvelles connaissances apportées par les foraminifères benthiques Fossile, Eleonora Bio-Indicateurs Actuels et Fossiles (BIAF) Université d'Angers (UA) Université d'Angers Hélène Howa Meryem Mojtahid Maria-Pia Nardelli 2022-05-04 https://theses.hal.science/tel-04089929 https://theses.hal.science/tel-04089929/document https://theses.hal.science/tel-04089929/file/pdffix_these_FOSSILE.pdf en eng HAL CCSD NNT: 2022ANGE0008 tel-04089929 https://theses.hal.science/tel-04089929 https://theses.hal.science/tel-04089929/document https://theses.hal.science/tel-04089929/file/pdffix_these_FOSSILE.pdf info:eu-repo/semantics/OpenAccess https://theses.hal.science/tel-04089929 Earth Sciences. Université d'Angers, 2022. English. ⟨NNT : 2022ANGE0008⟩ Sea ice Polynya Tidewater glacier Bioindicators Proxy Svalbard Polynie Glacier côtier Bioindicateurs [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/doctoralThesis Theses 2022 ftccsdartic 2023-05-06T22:45:20Z Climate change threatens polar regions with major consequences on ice-related dynamics and linked ecosystems. Predictions of future sea ice cover and glacier retreat rely on paleoenvironmental reconstructions (through proxies’ application) to extend the instrumental period and thus reduce models’ uncertainty. This PhD thesis aimed to develop and test ecological proxies for sea ice formation and glacier melting using benthic foraminifera. In the Storfjorden “sea ice factory”, foraminiferal responses to brine presence (i.e., CO2-enriched waters released during sea ice formation processes) were investigated. The ratio between Agglutinated and Calcareous (A/C) foraminifera was proposed as potential proxy for brine persistence, because of the brine-induced dissolution on calcareous foraminiferal shells. Although the A/C signal was affected by taphonomic processes, the differences between areas of brine persistence and those with intermittent influence was preserved, thus supporting the proxy. Likewise, foraminiferal responses to steep environmental gradients (e.g., water salinity and turbidity, organic fluxes) created by tidewater glacier dynamics in summer, were investigated in Kongsfjorden. The glacier induced disturbance resulted in the establishment of different foraminiferal assemblages and increased taxonomic and functional diversity with increased distance from the glacier front. A combination of diversity metrics was proposed as potential proxy for glacier retreat and its effectiveness was tested on a sedimentary archive covering the last 60 years. The two proxies proposed here are therefore applicable in any similar Arctic environments. Le changement climatique menace les régions polaires avec des conséquences majeures sur la dynamique des glaces et les écosystèmes associés. Les simulations de fonte glaciaire reposent sur des reconstitutions paléo environnementales, qui complètent les mesures directes sur la période actuelle pour réduire l'incertitude des prévisions. Des proxies basés sur l’écologie des ... Doctoral or Postdoctoral Thesis Arctic Climate change Foraminifera* glacier Glacier côtier Kongsfjord* Kongsfjorden Sea ice Storfjorden Svalbard Tidewater Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Arctic Svalbard
institution Open Polar
collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
language English
topic Sea ice
Polynya
Tidewater glacier
Bioindicators
Proxy
Svalbard
Polynie
Glacier côtier
Bioindicateurs
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
spellingShingle Sea ice
Polynya
Tidewater glacier
Bioindicators
Proxy
Svalbard
Polynie
Glacier côtier
Bioindicateurs
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Fossile, Eleonora
Ice-related environmental changes in Arctic fjords : new insights from benthic foraminifera
topic_facet Sea ice
Polynya
Tidewater glacier
Bioindicators
Proxy
Svalbard
Polynie
Glacier côtier
Bioindicateurs
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
description Climate change threatens polar regions with major consequences on ice-related dynamics and linked ecosystems. Predictions of future sea ice cover and glacier retreat rely on paleoenvironmental reconstructions (through proxies’ application) to extend the instrumental period and thus reduce models’ uncertainty. This PhD thesis aimed to develop and test ecological proxies for sea ice formation and glacier melting using benthic foraminifera. In the Storfjorden “sea ice factory”, foraminiferal responses to brine presence (i.e., CO2-enriched waters released during sea ice formation processes) were investigated. The ratio between Agglutinated and Calcareous (A/C) foraminifera was proposed as potential proxy for brine persistence, because of the brine-induced dissolution on calcareous foraminiferal shells. Although the A/C signal was affected by taphonomic processes, the differences between areas of brine persistence and those with intermittent influence was preserved, thus supporting the proxy. Likewise, foraminiferal responses to steep environmental gradients (e.g., water salinity and turbidity, organic fluxes) created by tidewater glacier dynamics in summer, were investigated in Kongsfjorden. The glacier induced disturbance resulted in the establishment of different foraminiferal assemblages and increased taxonomic and functional diversity with increased distance from the glacier front. A combination of diversity metrics was proposed as potential proxy for glacier retreat and its effectiveness was tested on a sedimentary archive covering the last 60 years. The two proxies proposed here are therefore applicable in any similar Arctic environments. Le changement climatique menace les régions polaires avec des conséquences majeures sur la dynamique des glaces et les écosystèmes associés. Les simulations de fonte glaciaire reposent sur des reconstitutions paléo environnementales, qui complètent les mesures directes sur la période actuelle pour réduire l'incertitude des prévisions. Des proxies basés sur l’écologie des ...
author2 Bio-Indicateurs Actuels et Fossiles (BIAF)
Université d'Angers (UA)
Université d'Angers
Hélène Howa
Meryem Mojtahid
Maria-Pia Nardelli
format Doctoral or Postdoctoral Thesis
author Fossile, Eleonora
author_facet Fossile, Eleonora
author_sort Fossile, Eleonora
title Ice-related environmental changes in Arctic fjords : new insights from benthic foraminifera
title_short Ice-related environmental changes in Arctic fjords : new insights from benthic foraminifera
title_full Ice-related environmental changes in Arctic fjords : new insights from benthic foraminifera
title_fullStr Ice-related environmental changes in Arctic fjords : new insights from benthic foraminifera
title_full_unstemmed Ice-related environmental changes in Arctic fjords : new insights from benthic foraminifera
title_sort ice-related environmental changes in arctic fjords : new insights from benthic foraminifera
publisher HAL CCSD
publishDate 2022
url https://theses.hal.science/tel-04089929
https://theses.hal.science/tel-04089929/document
https://theses.hal.science/tel-04089929/file/pdffix_these_FOSSILE.pdf
geographic Arctic
Svalbard
geographic_facet Arctic
Svalbard
genre Arctic
Climate change
Foraminifera*
glacier
Glacier côtier
Kongsfjord*
Kongsfjorden
Sea ice
Storfjorden
Svalbard
Tidewater
genre_facet Arctic
Climate change
Foraminifera*
glacier
Glacier côtier
Kongsfjord*
Kongsfjorden
Sea ice
Storfjorden
Svalbard
Tidewater
op_source https://theses.hal.science/tel-04089929
Earth Sciences. Université d'Angers, 2022. English. ⟨NNT : 2022ANGE0008⟩
op_relation NNT: 2022ANGE0008
tel-04089929
https://theses.hal.science/tel-04089929
https://theses.hal.science/tel-04089929/document
https://theses.hal.science/tel-04089929/file/pdffix_these_FOSSILE.pdf
op_rights info:eu-repo/semantics/OpenAccess
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