Basal foraminifera and gromiids (Protista) at the Håkon-Mosby Mud Volcano (Barents Sea slope)

We describe the occurrence of basal (‘primitive’) foraminifera and gromiids (a distinct taxon related to the foraminifera) in different bathyal habitats of the Håkon Mosby Mud Volcano (HMMV, Barents Sea). The foraminifera include two distinct groupings: (1) soft-shelled monothalamous foraminifera (‘...

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Published in:Marine Biodiversity
Main Authors: Gooday, Andrew J., Kamenskaya, Olga E., Soltwedel, Thomas
Format: Article in Journal/Newspaper
Language:unknown
Published: 2013
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/503439/
https://doi.org/10.1007/s12526-013-0148-5
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spelling ftnerc:oai:nora.nerc.ac.uk:503439 2023-05-15T15:38:48+02:00 Basal foraminifera and gromiids (Protista) at the Håkon-Mosby Mud Volcano (Barents Sea slope) Gooday, Andrew J. Kamenskaya, Olga E. Soltwedel, Thomas 2013-09 http://nora.nerc.ac.uk/id/eprint/503439/ https://doi.org/10.1007/s12526-013-0148-5 unknown Gooday, Andrew J. orcid:0000-0002-5661-7371 Kamenskaya, Olga E.; Soltwedel, Thomas. 2013 Basal foraminifera and gromiids (Protista) at the Håkon-Mosby Mud Volcano (Barents Sea slope). Marine Biodiversity, 43 (3). 205-225. https://doi.org/10.1007/s12526-013-0148-5 <https://doi.org/10.1007/s12526-013-0148-5> Publication - Article PeerReviewed 2013 ftnerc https://doi.org/10.1007/s12526-013-0148-5 2023-02-04T19:37:50Z We describe the occurrence of basal (‘primitive’) foraminifera and gromiids (a distinct taxon related to the foraminifera) in different bathyal habitats of the Håkon Mosby Mud Volcano (HMMV, Barents Sea). The foraminifera include two distinct groupings: (1) soft-shelled monothalamous foraminifera (‘allogromiids’, ‘saccamminids’ and ‘psammosphaerids’) and (2) brown organic-walled foraminifera (genera Conicotheca, Nodellum, Placopsilinella and Resigella). Samples were analysed from (1) the ‘hot centre’ of the volcano where fluid upflow was maximal; (2) smooth and structured muds in a ‘warm’ area of the centre where fluid upflow was reduced; (3) areas covered by Beggiatoa mats; (4) an area colonised by siboglinid polychaetes (‘pogonophores’); and (5) areas of ‘normal’ seafloor outside the volcano. Together, the studied organisms represented 57.8 % (‘normal’ seafloor; n = 418), 28.5 % (‘warm centre’; n = 122), and 26.4 % (Beggiatoa mats; n = 5) of all ‘live’ (stained) foraminifera in three samples (0–1 cm layer) that were sorted for all stained foraminifera. In total, the 17 samples examined yielded 21 ‘allogromiid’ (organic-walled), 25 ‘saccamminid’ (agglutinated) and 5 other morphospecies among the monothalamous foraminifera, as well as 5 ‘brown-walled’ and 5 gromiid morphospecies. Four taxa were identified to species (Conicotheca nigrans, Resigella moniliforme, R. polaris, Micrometula hyalinosphaera); another seven were assigned to the genera Bathyallogromia, Conqueria, Nodellum, Placopsilinella, Resigella, Tinogullmia and Vanhoeffenella. All others were undescibed at the genus level. Some species, notably ‘Saccamminid sp. 5’, C. nigrans and Nodellum sp., were distributed in sediment layers down to 5 cm depth, and sausage-shaped gromiids were also present in the deeper layers of some samples. The number of basal foraminiferal and gromiid morphospecies varied considerably from site to site. It was relatively high north of the volcano (42 morphospecies in 4 samples) and in the ‘warm centre’ (28 morphospecies in 2 ... Article in Journal/Newspaper Barents Sea Natural Environment Research Council: NERC Open Research Archive Barents Sea Marine Biodiversity 43 3 205 225
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language unknown
description We describe the occurrence of basal (‘primitive’) foraminifera and gromiids (a distinct taxon related to the foraminifera) in different bathyal habitats of the Håkon Mosby Mud Volcano (HMMV, Barents Sea). The foraminifera include two distinct groupings: (1) soft-shelled monothalamous foraminifera (‘allogromiids’, ‘saccamminids’ and ‘psammosphaerids’) and (2) brown organic-walled foraminifera (genera Conicotheca, Nodellum, Placopsilinella and Resigella). Samples were analysed from (1) the ‘hot centre’ of the volcano where fluid upflow was maximal; (2) smooth and structured muds in a ‘warm’ area of the centre where fluid upflow was reduced; (3) areas covered by Beggiatoa mats; (4) an area colonised by siboglinid polychaetes (‘pogonophores’); and (5) areas of ‘normal’ seafloor outside the volcano. Together, the studied organisms represented 57.8 % (‘normal’ seafloor; n = 418), 28.5 % (‘warm centre’; n = 122), and 26.4 % (Beggiatoa mats; n = 5) of all ‘live’ (stained) foraminifera in three samples (0–1 cm layer) that were sorted for all stained foraminifera. In total, the 17 samples examined yielded 21 ‘allogromiid’ (organic-walled), 25 ‘saccamminid’ (agglutinated) and 5 other morphospecies among the monothalamous foraminifera, as well as 5 ‘brown-walled’ and 5 gromiid morphospecies. Four taxa were identified to species (Conicotheca nigrans, Resigella moniliforme, R. polaris, Micrometula hyalinosphaera); another seven were assigned to the genera Bathyallogromia, Conqueria, Nodellum, Placopsilinella, Resigella, Tinogullmia and Vanhoeffenella. All others were undescibed at the genus level. Some species, notably ‘Saccamminid sp. 5’, C. nigrans and Nodellum sp., were distributed in sediment layers down to 5 cm depth, and sausage-shaped gromiids were also present in the deeper layers of some samples. The number of basal foraminiferal and gromiid morphospecies varied considerably from site to site. It was relatively high north of the volcano (42 morphospecies in 4 samples) and in the ‘warm centre’ (28 morphospecies in 2 ...
format Article in Journal/Newspaper
author Gooday, Andrew J.
Kamenskaya, Olga E.
Soltwedel, Thomas
spellingShingle Gooday, Andrew J.
Kamenskaya, Olga E.
Soltwedel, Thomas
Basal foraminifera and gromiids (Protista) at the Håkon-Mosby Mud Volcano (Barents Sea slope)
author_facet Gooday, Andrew J.
Kamenskaya, Olga E.
Soltwedel, Thomas
author_sort Gooday, Andrew J.
title Basal foraminifera and gromiids (Protista) at the Håkon-Mosby Mud Volcano (Barents Sea slope)
title_short Basal foraminifera and gromiids (Protista) at the Håkon-Mosby Mud Volcano (Barents Sea slope)
title_full Basal foraminifera and gromiids (Protista) at the Håkon-Mosby Mud Volcano (Barents Sea slope)
title_fullStr Basal foraminifera and gromiids (Protista) at the Håkon-Mosby Mud Volcano (Barents Sea slope)
title_full_unstemmed Basal foraminifera and gromiids (Protista) at the Håkon-Mosby Mud Volcano (Barents Sea slope)
title_sort basal foraminifera and gromiids (protista) at the håkon-mosby mud volcano (barents sea slope)
publishDate 2013
url http://nora.nerc.ac.uk/id/eprint/503439/
https://doi.org/10.1007/s12526-013-0148-5
geographic Barents Sea
geographic_facet Barents Sea
genre Barents Sea
genre_facet Barents Sea
op_relation Gooday, Andrew J. orcid:0000-0002-5661-7371
Kamenskaya, Olga E.; Soltwedel, Thomas. 2013 Basal foraminifera and gromiids (Protista) at the Håkon-Mosby Mud Volcano (Barents Sea slope). Marine Biodiversity, 43 (3). 205-225. https://doi.org/10.1007/s12526-013-0148-5 <https://doi.org/10.1007/s12526-013-0148-5>
op_doi https://doi.org/10.1007/s12526-013-0148-5
container_title Marine Biodiversity
container_volume 43
container_issue 3
container_start_page 205
op_container_end_page 225
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