DataSheet_1_Chemosynthetic and photosynthetic trophic support from cold seeps in Arctic benthic communities.docx

Benthic communities below the photic zone are largely reliant on the export of surface-water primary production and the flux of partially degraded organic matter to the seabed, i.e. pelagic−benthic coupling. Over the past decades, however, the role of chemosynthetically produced carbon in food webs...

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Main Authors: Emmelie K. L. Åström, Bodil A. Bluhm, Tine L. Rasmussen
Format: Dataset
Language:unknown
Published: 2022
Subjects:
Online Access:https://doi.org/10.3389/fmars.2022.910558.s001
https://figshare.com/articles/dataset/DataSheet_1_Chemosynthetic_and_photosynthetic_trophic_support_from_cold_seeps_in_Arctic_benthic_communities_docx/20510286
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record_format openpolar
spelling ftfrontimediafig:oai:figshare.com:article/20510286 2024-09-15T17:57:54+00:00 DataSheet_1_Chemosynthetic and photosynthetic trophic support from cold seeps in Arctic benthic communities.docx Emmelie K. L. Åström Bodil A. Bluhm Tine L. Rasmussen 2022-08-18T13:47:05Z https://doi.org/10.3389/fmars.2022.910558.s001 https://figshare.com/articles/dataset/DataSheet_1_Chemosynthetic_and_photosynthetic_trophic_support_from_cold_seeps_in_Arctic_benthic_communities_docx/20510286 unknown doi:10.3389/fmars.2022.910558.s001 https://figshare.com/articles/dataset/DataSheet_1_Chemosynthetic_and_photosynthetic_trophic_support_from_cold_seeps_in_Arctic_benthic_communities_docx/20510286 CC BY 4.0 Oceanography Marine Biology Marine Geoscience Biological Oceanography Chemical Oceanography Physical Oceanography Marine Engineering methane chemosynthesis food web benthos Svalbard Dataset 2022 ftfrontimediafig https://doi.org/10.3389/fmars.2022.910558.s001 2024-08-19T06:19:48Z Benthic communities below the photic zone are largely reliant on the export of surface-water primary production and the flux of partially degraded organic matter to the seabed, i.e. pelagic−benthic coupling. Over the past decades, however, the role of chemosynthetically produced carbon in food webs has been recognized in various habitats. Cold seeps are now known to be widespread across circumpolar Arctic shelves where natural release of hydrocarbons occurs at the seabed. Here, we investigated to what extent chemosynthesis-based carbon (CBC) enters the food web in a high latitude shelf-system. Specifically, we estimated the contributions of chemosynthesis-based carbon to primarily benthic invertebrate taxa from seeps at both shallow and deeper shelves and comparative non-seep areas in the Svalbard-Barents Sea region using bulk stable isotope-analysis of carbon and nitrogen. Our results show low δ 13 C values (-51.3 to -32.7 ‰) in chemosymbiotic siboglinids and several species of benthic, higher-trophic level, invertebrates (mainly polychaetes and echinoderms; -35.0 to -26.1‰) collected at cold seeps, consistent with assimilation of chemosynthesis-based carbon into the Arctic benthic food web. Using a two-component mixing equation, we demonstrate that certain species could derive more than 50% of their carbon from chemosynthesis-based carbon. These findings show that autochthonous chemosynthetic energy sources can contribute to supporting distinct groups of ‘background’ benthic taxa at these Arctic seep-habitats beyond microbial associations and chemosymbiotic species. Furthermore, we found a higher degree of chemosynthesis-based carbon in benthos at the deeper Barents Sea shelf seeps (>330 m) compared to seeps at the Western Svalbard shelf (<150 m water-depth), and we suggest this result reflects the differences in depth range, surface production and pelagic-benthic coupling. We detected large intra-species variations in carbon signatures within and across geographical locations and, combined with isotopic ... Dataset Barents Sea Svalbard Frontiers: Figshare
institution Open Polar
collection Frontiers: Figshare
op_collection_id ftfrontimediafig
language unknown
topic Oceanography
Marine Biology
Marine Geoscience
Biological Oceanography
Chemical Oceanography
Physical Oceanography
Marine Engineering
methane
chemosynthesis
food web
benthos
Svalbard
spellingShingle Oceanography
Marine Biology
Marine Geoscience
Biological Oceanography
Chemical Oceanography
Physical Oceanography
Marine Engineering
methane
chemosynthesis
food web
benthos
Svalbard
Emmelie K. L. Åström
Bodil A. Bluhm
Tine L. Rasmussen
DataSheet_1_Chemosynthetic and photosynthetic trophic support from cold seeps in Arctic benthic communities.docx
topic_facet Oceanography
Marine Biology
Marine Geoscience
Biological Oceanography
Chemical Oceanography
Physical Oceanography
Marine Engineering
methane
chemosynthesis
food web
benthos
Svalbard
description Benthic communities below the photic zone are largely reliant on the export of surface-water primary production and the flux of partially degraded organic matter to the seabed, i.e. pelagic−benthic coupling. Over the past decades, however, the role of chemosynthetically produced carbon in food webs has been recognized in various habitats. Cold seeps are now known to be widespread across circumpolar Arctic shelves where natural release of hydrocarbons occurs at the seabed. Here, we investigated to what extent chemosynthesis-based carbon (CBC) enters the food web in a high latitude shelf-system. Specifically, we estimated the contributions of chemosynthesis-based carbon to primarily benthic invertebrate taxa from seeps at both shallow and deeper shelves and comparative non-seep areas in the Svalbard-Barents Sea region using bulk stable isotope-analysis of carbon and nitrogen. Our results show low δ 13 C values (-51.3 to -32.7 ‰) in chemosymbiotic siboglinids and several species of benthic, higher-trophic level, invertebrates (mainly polychaetes and echinoderms; -35.0 to -26.1‰) collected at cold seeps, consistent with assimilation of chemosynthesis-based carbon into the Arctic benthic food web. Using a two-component mixing equation, we demonstrate that certain species could derive more than 50% of their carbon from chemosynthesis-based carbon. These findings show that autochthonous chemosynthetic energy sources can contribute to supporting distinct groups of ‘background’ benthic taxa at these Arctic seep-habitats beyond microbial associations and chemosymbiotic species. Furthermore, we found a higher degree of chemosynthesis-based carbon in benthos at the deeper Barents Sea shelf seeps (>330 m) compared to seeps at the Western Svalbard shelf (<150 m water-depth), and we suggest this result reflects the differences in depth range, surface production and pelagic-benthic coupling. We detected large intra-species variations in carbon signatures within and across geographical locations and, combined with isotopic ...
format Dataset
author Emmelie K. L. Åström
Bodil A. Bluhm
Tine L. Rasmussen
author_facet Emmelie K. L. Åström
Bodil A. Bluhm
Tine L. Rasmussen
author_sort Emmelie K. L. Åström
title DataSheet_1_Chemosynthetic and photosynthetic trophic support from cold seeps in Arctic benthic communities.docx
title_short DataSheet_1_Chemosynthetic and photosynthetic trophic support from cold seeps in Arctic benthic communities.docx
title_full DataSheet_1_Chemosynthetic and photosynthetic trophic support from cold seeps in Arctic benthic communities.docx
title_fullStr DataSheet_1_Chemosynthetic and photosynthetic trophic support from cold seeps in Arctic benthic communities.docx
title_full_unstemmed DataSheet_1_Chemosynthetic and photosynthetic trophic support from cold seeps in Arctic benthic communities.docx
title_sort datasheet_1_chemosynthetic and photosynthetic trophic support from cold seeps in arctic benthic communities.docx
publishDate 2022
url https://doi.org/10.3389/fmars.2022.910558.s001
https://figshare.com/articles/dataset/DataSheet_1_Chemosynthetic_and_photosynthetic_trophic_support_from_cold_seeps_in_Arctic_benthic_communities_docx/20510286
genre Barents Sea
Svalbard
genre_facet Barents Sea
Svalbard
op_relation doi:10.3389/fmars.2022.910558.s001
https://figshare.com/articles/dataset/DataSheet_1_Chemosynthetic_and_photosynthetic_trophic_support_from_cold_seeps_in_Arctic_benthic_communities_docx/20510286
op_rights CC BY 4.0
op_doi https://doi.org/10.3389/fmars.2022.910558.s001
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