Deposit-feeding of Nonionellina labradorica (foraminifera) from an Arctic methane seep site and possible association with a methanotroph

Several foraminifera are deposit feeders that consume organic detritus (dead particulate organic material with entrained bacteria). However, the role of such foraminifera in the benthic food web remains understudied. Foraminifera feeding on methanotrophic bacteria, which are 13 C-depleted, may cause...

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Published in:Biogeosciences
Main Authors: Schmidt, Christiane, Geslin, Emmanuelle, Bernhard, Joan M., LeKieffre, Charlotte, Svenning, Mette Marianne, Roberge, Helene, Schweizer, Magali, Panieri, Giuliana
Format: Text
Language:English
Published: 2022
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Online Access:https://doi.org/10.5194/bg-19-3897-2022
https://bg.copernicus.org/articles/19/3897/2022/
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spelling ftcopernicus:oai:publications.copernicus.org:bg98656 2023-05-15T14:31:46+02:00 Deposit-feeding of Nonionellina labradorica (foraminifera) from an Arctic methane seep site and possible association with a methanotroph Schmidt, Christiane Geslin, Emmanuelle Bernhard, Joan M. LeKieffre, Charlotte Svenning, Mette Marianne Roberge, Helene Schweizer, Magali Panieri, Giuliana 2022-08-30 application/pdf https://doi.org/10.5194/bg-19-3897-2022 https://bg.copernicus.org/articles/19/3897/2022/ eng eng doi:10.5194/bg-19-3897-2022 https://bg.copernicus.org/articles/19/3897/2022/ eISSN: 1726-4189 Text 2022 ftcopernicus https://doi.org/10.5194/bg-19-3897-2022 2022-09-05T16:22:56Z Several foraminifera are deposit feeders that consume organic detritus (dead particulate organic material with entrained bacteria). However, the role of such foraminifera in the benthic food web remains understudied. Foraminifera feeding on methanotrophic bacteria, which are 13 C-depleted, may cause negative cytoplasmic and/or calcitic δ 13 C values. To test whether the foraminiferal diet includes methanotrophs, we performed a short-term (20 h) feeding experiment with Nonionellina labradorica from an active Arctic methane-emission site (Storfjordrenna, Barents Sea) using the marine methanotroph Methyloprofundus sedimenti and analysed N. labradorica cytology via transmission electron microscopy (TEM). We hypothesised that M. sedimenti would be visible post-experiment in degradation vacuoles, as evidenced by their ultrastructure. Sediment grains (mostly clay) occurred inside one or several degradation vacuoles in all foraminifers. In 24 % of the specimens from the feeding experiment degradation vacuoles also contained bacteria, although none could be confirmed to be the offered M. sedimenti . Observations of the apertural area after 20 h incubation revealed three putative methanotrophs, close to clay particles, based on bacterial ultrastructural characteristics. Furthermore, we noted the absence of bacterial endobionts in all examined N. labradorica but confirmed the presence of kleptoplasts, which were often partially degraded. In sum, we suggest that M. sedimenti can be consumed via untargeted grazing in seeps and that N. labradorica can be generally classified as a deposit feeder at this Arctic site. Text arctic methane Arctic Barents Sea Foraminifera* Storfjordrenna Copernicus Publications: E-Journals Arctic Barents Sea Storfjordrenna ENVELOPE(17.000,17.000,76.000,76.000) Biogeosciences 19 16 3897 3909
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Several foraminifera are deposit feeders that consume organic detritus (dead particulate organic material with entrained bacteria). However, the role of such foraminifera in the benthic food web remains understudied. Foraminifera feeding on methanotrophic bacteria, which are 13 C-depleted, may cause negative cytoplasmic and/or calcitic δ 13 C values. To test whether the foraminiferal diet includes methanotrophs, we performed a short-term (20 h) feeding experiment with Nonionellina labradorica from an active Arctic methane-emission site (Storfjordrenna, Barents Sea) using the marine methanotroph Methyloprofundus sedimenti and analysed N. labradorica cytology via transmission electron microscopy (TEM). We hypothesised that M. sedimenti would be visible post-experiment in degradation vacuoles, as evidenced by their ultrastructure. Sediment grains (mostly clay) occurred inside one or several degradation vacuoles in all foraminifers. In 24 % of the specimens from the feeding experiment degradation vacuoles also contained bacteria, although none could be confirmed to be the offered M. sedimenti . Observations of the apertural area after 20 h incubation revealed three putative methanotrophs, close to clay particles, based on bacterial ultrastructural characteristics. Furthermore, we noted the absence of bacterial endobionts in all examined N. labradorica but confirmed the presence of kleptoplasts, which were often partially degraded. In sum, we suggest that M. sedimenti can be consumed via untargeted grazing in seeps and that N. labradorica can be generally classified as a deposit feeder at this Arctic site.
format Text
author Schmidt, Christiane
Geslin, Emmanuelle
Bernhard, Joan M.
LeKieffre, Charlotte
Svenning, Mette Marianne
Roberge, Helene
Schweizer, Magali
Panieri, Giuliana
spellingShingle Schmidt, Christiane
Geslin, Emmanuelle
Bernhard, Joan M.
LeKieffre, Charlotte
Svenning, Mette Marianne
Roberge, Helene
Schweizer, Magali
Panieri, Giuliana
Deposit-feeding of Nonionellina labradorica (foraminifera) from an Arctic methane seep site and possible association with a methanotroph
author_facet Schmidt, Christiane
Geslin, Emmanuelle
Bernhard, Joan M.
LeKieffre, Charlotte
Svenning, Mette Marianne
Roberge, Helene
Schweizer, Magali
Panieri, Giuliana
author_sort Schmidt, Christiane
title Deposit-feeding of Nonionellina labradorica (foraminifera) from an Arctic methane seep site and possible association with a methanotroph
title_short Deposit-feeding of Nonionellina labradorica (foraminifera) from an Arctic methane seep site and possible association with a methanotroph
title_full Deposit-feeding of Nonionellina labradorica (foraminifera) from an Arctic methane seep site and possible association with a methanotroph
title_fullStr Deposit-feeding of Nonionellina labradorica (foraminifera) from an Arctic methane seep site and possible association with a methanotroph
title_full_unstemmed Deposit-feeding of Nonionellina labradorica (foraminifera) from an Arctic methane seep site and possible association with a methanotroph
title_sort deposit-feeding of nonionellina labradorica (foraminifera) from an arctic methane seep site and possible association with a methanotroph
publishDate 2022
url https://doi.org/10.5194/bg-19-3897-2022
https://bg.copernicus.org/articles/19/3897/2022/
long_lat ENVELOPE(17.000,17.000,76.000,76.000)
geographic Arctic
Barents Sea
Storfjordrenna
geographic_facet Arctic
Barents Sea
Storfjordrenna
genre arctic methane
Arctic
Barents Sea
Foraminifera*
Storfjordrenna
genre_facet arctic methane
Arctic
Barents Sea
Foraminifera*
Storfjordrenna
op_source eISSN: 1726-4189
op_relation doi:10.5194/bg-19-3897-2022
https://bg.copernicus.org/articles/19/3897/2022/
op_doi https://doi.org/10.5194/bg-19-3897-2022
container_title Biogeosciences
container_volume 19
container_issue 16
container_start_page 3897
op_container_end_page 3909
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