Influence of modern environmental gradients on foraminiferal faunas in the inner Kongsfjorden (Svalbard)
International audience Kongsfjorden (Svalbard archipelago) is subjected to strong environmental gradients creating high physical and geochemical stress on benthic faunas. The present study aims at understanding the environmental drivers governing benthic foraminifera in the innermost part of the fjo...
Published in: | Marine Micropaleontology |
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Main Authors: | , , , , , , , |
Other Authors: | , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2022
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Subjects: | |
Online Access: | https://hal.science/hal-04306327 https://hal.science/hal-04306327/document https://hal.science/hal-04306327/file/Fossileetal_31Aug2021.pdf https://doi.org/10.1016/j.marmicro.2022.102117 |
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Open Polar |
collection |
Portail des publications scientifiques de l’Université d’Angers (HAL) |
op_collection_id |
ftunivangershal |
language |
English |
topic |
Benthic foraminifera Bioindicators Tidewater glacier Arctic Fjord hydrology [SDE]Environmental Sciences |
spellingShingle |
Benthic foraminifera Bioindicators Tidewater glacier Arctic Fjord hydrology [SDE]Environmental Sciences Fossile, Eleonora Nardelli, Maria Pia Howa, Hélène Baltzer, Agnès Poprawski, Yohann Baneschi, Ilaria Doveri, Marco Mojtahid, Meryem Influence of modern environmental gradients on foraminiferal faunas in the inner Kongsfjorden (Svalbard) |
topic_facet |
Benthic foraminifera Bioindicators Tidewater glacier Arctic Fjord hydrology [SDE]Environmental Sciences |
description |
International audience Kongsfjorden (Svalbard archipelago) is subjected to strong environmental gradients creating high physical and geochemical stress on benthic faunas. The present study aims at understanding the environmental drivers governing benthic foraminifera in the innermost part of the fjord. Surface sediments from 9 stations were sampled during August 2018 along a transect starting at ca. 2 km from the tidewater glacier Kronebreen and ending 12 km seaward. Three biozones were identified in response to disturbances linked to the proximity of the Kronebreen front (i.e., high water turbidity, freshwater, and sediment inputs, reduced organic fluxes). Close to the terminus (proximal biozone), few stress-tolerant and glacier proximal species were present (i.e., Capsammina bowmanni and Cassidulina reniforme). At about 6-8 km from the front (medial biozone), reduced turbidity, and increased organic fluxes, resulted in a higher diversity, and a high abundance of the phytodetritus-indicator Nonionellina labradorica. Relatively high diversity persisted until 12 km from the front due to higher organic inputs and reduced stressful conditions. The distal biozone was dominated by the Atlantic Water (AW) indicator Adercotryma glomeratum, in coherence with the presence of warm and salty AW detected far inside the fjord. Physical stress related to the glacier dynamics appears to favour the establishment of opportunistic species close to the terminus, whereas reduced disturbance away from the glacier induces the establishment of diverse assemblages. Our results show that benthic foraminifera may be effective bioindicators to monitor the long-term retreat of tidewater glaciers induced by climate change in Kongsfjorden. |
author2 |
Laboratoire de Planétologie et Géosciences UMR_C 6112 (LPG) Le Mans Université (UM)-Université d'Angers (UA)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Nantes université - UFR des Sciences et des Techniques (Nantes univ - UFR ST) Nantes Université - pôle Sciences et technologie Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ)-Nantes Université - pôle Sciences et technologie Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ) Université d'Angers (UA) Nantes Université (Nantes Univ) Littoral, Environnement, Télédétection, Géomatique (LETG - Nantes ) Université de Brest (UBO)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Littoral, Environnement, Télédétection, Géomatique UMR 6554 (LETG) Université de Brest (UBO)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut de Géographie et d'Aménagement Régional de l'Université de Nantes (Nantes Univ - IGARUN) Nantes Université - pôle Humanités Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ)-Nantes Université - pôle Humanités Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ)-Institut de Géographie et d'Aménagement Régional de l'Université de Nantes (Nantes Univ - IGARUN) CNR Istituto di Geoscienze e Georisorse Pisa (IGG-CNR) National Research Council of Italy |
format |
Article in Journal/Newspaper |
author |
Fossile, Eleonora Nardelli, Maria Pia Howa, Hélène Baltzer, Agnès Poprawski, Yohann Baneschi, Ilaria Doveri, Marco Mojtahid, Meryem |
author_facet |
Fossile, Eleonora Nardelli, Maria Pia Howa, Hélène Baltzer, Agnès Poprawski, Yohann Baneschi, Ilaria Doveri, Marco Mojtahid, Meryem |
author_sort |
Fossile, Eleonora |
title |
Influence of modern environmental gradients on foraminiferal faunas in the inner Kongsfjorden (Svalbard) |
title_short |
Influence of modern environmental gradients on foraminiferal faunas in the inner Kongsfjorden (Svalbard) |
title_full |
Influence of modern environmental gradients on foraminiferal faunas in the inner Kongsfjorden (Svalbard) |
title_fullStr |
Influence of modern environmental gradients on foraminiferal faunas in the inner Kongsfjorden (Svalbard) |
title_full_unstemmed |
Influence of modern environmental gradients on foraminiferal faunas in the inner Kongsfjorden (Svalbard) |
title_sort |
influence of modern environmental gradients on foraminiferal faunas in the inner kongsfjorden (svalbard) |
publisher |
HAL CCSD |
publishDate |
2022 |
url |
https://hal.science/hal-04306327 https://hal.science/hal-04306327/document https://hal.science/hal-04306327/file/Fossileetal_31Aug2021.pdf https://doi.org/10.1016/j.marmicro.2022.102117 |
genre |
Arctic Climate change Foraminifera* glacier Kongsfjord* Kongsfjorden Svalbard Tidewater |
genre_facet |
Arctic Climate change Foraminifera* glacier Kongsfjord* Kongsfjorden Svalbard Tidewater |
op_source |
ISSN: 0377-8398 Marine Micropaleontology https://hal.science/hal-04306327 Marine Micropaleontology, 2022, 173, pp.102117. ⟨10.1016/j.marmicro.2022.102117⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.marmicro.2022.102117 hal-04306327 https://hal.science/hal-04306327 https://hal.science/hal-04306327/document https://hal.science/hal-04306327/file/Fossileetal_31Aug2021.pdf doi:10.1016/j.marmicro.2022.102117 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1016/j.marmicro.2022.102117 |
container_title |
Marine Micropaleontology |
container_volume |
173 |
container_start_page |
102117 |
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1799475635392872448 |
spelling |
ftunivangershal:oai:HAL:hal-04306327v1 2024-05-19T07:36:30+00:00 Influence of modern environmental gradients on foraminiferal faunas in the inner Kongsfjorden (Svalbard) Fossile, Eleonora Nardelli, Maria Pia Howa, Hélène Baltzer, Agnès Poprawski, Yohann Baneschi, Ilaria Doveri, Marco Mojtahid, Meryem Laboratoire de Planétologie et Géosciences UMR_C 6112 (LPG) Le Mans Université (UM)-Université d'Angers (UA)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Nantes université - UFR des Sciences et des Techniques (Nantes univ - UFR ST) Nantes Université - pôle Sciences et technologie Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ)-Nantes Université - pôle Sciences et technologie Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ) Université d'Angers (UA) Nantes Université (Nantes Univ) Littoral, Environnement, Télédétection, Géomatique (LETG - Nantes ) Université de Brest (UBO)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Littoral, Environnement, Télédétection, Géomatique UMR 6554 (LETG) Université de Brest (UBO)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut de Géographie et d'Aménagement Régional de l'Université de Nantes (Nantes Univ - IGARUN) Nantes Université - pôle Humanités Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ)-Nantes Université - pôle Humanités Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ)-Institut de Géographie et d'Aménagement Régional de l'Université de Nantes (Nantes Univ - IGARUN) CNR Istituto di Geoscienze e Georisorse Pisa (IGG-CNR) National Research Council of Italy 2022-05 https://hal.science/hal-04306327 https://hal.science/hal-04306327/document https://hal.science/hal-04306327/file/Fossileetal_31Aug2021.pdf https://doi.org/10.1016/j.marmicro.2022.102117 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.marmicro.2022.102117 hal-04306327 https://hal.science/hal-04306327 https://hal.science/hal-04306327/document https://hal.science/hal-04306327/file/Fossileetal_31Aug2021.pdf doi:10.1016/j.marmicro.2022.102117 info:eu-repo/semantics/OpenAccess ISSN: 0377-8398 Marine Micropaleontology https://hal.science/hal-04306327 Marine Micropaleontology, 2022, 173, pp.102117. ⟨10.1016/j.marmicro.2022.102117⟩ Benthic foraminifera Bioindicators Tidewater glacier Arctic Fjord hydrology [SDE]Environmental Sciences info:eu-repo/semantics/article Journal articles 2022 ftunivangershal https://doi.org/10.1016/j.marmicro.2022.102117 2024-04-26T01:41:29Z International audience Kongsfjorden (Svalbard archipelago) is subjected to strong environmental gradients creating high physical and geochemical stress on benthic faunas. The present study aims at understanding the environmental drivers governing benthic foraminifera in the innermost part of the fjord. Surface sediments from 9 stations were sampled during August 2018 along a transect starting at ca. 2 km from the tidewater glacier Kronebreen and ending 12 km seaward. Three biozones were identified in response to disturbances linked to the proximity of the Kronebreen front (i.e., high water turbidity, freshwater, and sediment inputs, reduced organic fluxes). Close to the terminus (proximal biozone), few stress-tolerant and glacier proximal species were present (i.e., Capsammina bowmanni and Cassidulina reniforme). At about 6-8 km from the front (medial biozone), reduced turbidity, and increased organic fluxes, resulted in a higher diversity, and a high abundance of the phytodetritus-indicator Nonionellina labradorica. Relatively high diversity persisted until 12 km from the front due to higher organic inputs and reduced stressful conditions. The distal biozone was dominated by the Atlantic Water (AW) indicator Adercotryma glomeratum, in coherence with the presence of warm and salty AW detected far inside the fjord. Physical stress related to the glacier dynamics appears to favour the establishment of opportunistic species close to the terminus, whereas reduced disturbance away from the glacier induces the establishment of diverse assemblages. Our results show that benthic foraminifera may be effective bioindicators to monitor the long-term retreat of tidewater glaciers induced by climate change in Kongsfjorden. Article in Journal/Newspaper Arctic Climate change Foraminifera* glacier Kongsfjord* Kongsfjorden Svalbard Tidewater Portail des publications scientifiques de l’Université d’Angers (HAL) Marine Micropaleontology 173 102117 |