Cold-seep ostracods from the western Svalbard margin: direct palaeo-indicator for methane seepage?

Source at https://doi.org/10.5194/jm-37-139-2018 Despite their high abundance and diversity, microfossil taxa adapted to a particular chemosynthetic environment have rarely been studied and are therefore poorly known. Here we report on an ostracod species, Rosaliella svalbardensis gen. et sp. nov.,...

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Published in:Journal of Micropalaeontology
Main Authors: Yasuhara, Moriaki, Sztybor, Kamila, Rasmussen, Tine Lander, Okahashi, Hisayo, Sato, Runa, Tanaka, Hayato
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2018
Subjects:
Online Access:https://hdl.handle.net/10037/12098
https://doi.org/10.5194/jm-37-139-2018
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author Yasuhara, Moriaki
Sztybor, Kamila
Rasmussen, Tine Lander
Okahashi, Hisayo
Sato, Runa
Tanaka, Hayato
author_facet Yasuhara, Moriaki
Sztybor, Kamila
Rasmussen, Tine Lander
Okahashi, Hisayo
Sato, Runa
Tanaka, Hayato
author_sort Yasuhara, Moriaki
collection University of Tromsø: Munin Open Research Archive
container_issue 1
container_start_page 139
container_title Journal of Micropalaeontology
container_volume 37
description Source at https://doi.org/10.5194/jm-37-139-2018 Despite their high abundance and diversity, microfossil taxa adapted to a particular chemosynthetic environment have rarely been studied and are therefore poorly known. Here we report on an ostracod species, Rosaliella svalbardensis gen. et sp. nov., from a cold methane seep site at the western Svalbard margin, Fram Strait. The new species shows a distinct morphology, different from other eucytherurine ostracod genera. It has a marked similarity to Xylocythere, an ostracod genus known from chemosynthetic environments of wood falls and hydrothermal vents. Rosaliella svalbardensis is probably an endemic species or genus linked to methane seeps. We speculate that the surface ornamentation of pore clusters, secondary reticulation, and pit clusters may be related to ectosymbiosis with chemoautotrophic bacteria. This new discovery of specialized microfossil taxa is important because they can be used as an indicator species for past and present seep environments (http: //zoobank.org/urn:lsid:zoobank.org:pub:6075FF30-29D5-4DAB-9141-AE722CD3A69B).
format Article in Journal/Newspaper
genre Arctic
Fram Strait
Svalbard
Svalbard margin
genre_facet Arctic
Fram Strait
Svalbard
Svalbard margin
geographic Svalbard
geographic_facet Svalbard
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op_doi https://doi.org/10.5194/jm-37-139-2018
op_relation Journal of Micropalaeontology
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spelling ftunivtroemsoe:oai:munin.uit.no:10037/12098 2025-04-13T14:11:23+00:00 Cold-seep ostracods from the western Svalbard margin: direct palaeo-indicator for methane seepage? Yasuhara, Moriaki Sztybor, Kamila Rasmussen, Tine Lander Okahashi, Hisayo Sato, Runa Tanaka, Hayato 2018-01-05 https://hdl.handle.net/10037/12098 https://doi.org/10.5194/jm-37-139-2018 eng eng Copernicus Publications Journal of Micropalaeontology info:eu-repo/grantAgreement/RCN/SFF/223259/Norway/Centre for Arctic Gas Hydrate, Environment and Climate/CAGE/ FRIDAID 1536430 https://hdl.handle.net/10037/12098 openAccess VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Marin geologi: 466 VDP::Mathematics and natural science: 400::Geosciences: 450::Marine geology: 466 Journal article Tidsskriftartikkel Peer reviewed 2018 ftunivtroemsoe https://doi.org/10.5194/jm-37-139-2018 2025-03-14T05:17:57Z Source at https://doi.org/10.5194/jm-37-139-2018 Despite their high abundance and diversity, microfossil taxa adapted to a particular chemosynthetic environment have rarely been studied and are therefore poorly known. Here we report on an ostracod species, Rosaliella svalbardensis gen. et sp. nov., from a cold methane seep site at the western Svalbard margin, Fram Strait. The new species shows a distinct morphology, different from other eucytherurine ostracod genera. It has a marked similarity to Xylocythere, an ostracod genus known from chemosynthetic environments of wood falls and hydrothermal vents. Rosaliella svalbardensis is probably an endemic species or genus linked to methane seeps. We speculate that the surface ornamentation of pore clusters, secondary reticulation, and pit clusters may be related to ectosymbiosis with chemoautotrophic bacteria. This new discovery of specialized microfossil taxa is important because they can be used as an indicator species for past and present seep environments (http: //zoobank.org/urn:lsid:zoobank.org:pub:6075FF30-29D5-4DAB-9141-AE722CD3A69B). Article in Journal/Newspaper Arctic Fram Strait Svalbard Svalbard margin University of Tromsø: Munin Open Research Archive Svalbard Journal of Micropalaeontology 37 1 139 148
spellingShingle VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Marin geologi: 466
VDP::Mathematics and natural science: 400::Geosciences: 450::Marine geology: 466
Yasuhara, Moriaki
Sztybor, Kamila
Rasmussen, Tine Lander
Okahashi, Hisayo
Sato, Runa
Tanaka, Hayato
Cold-seep ostracods from the western Svalbard margin: direct palaeo-indicator for methane seepage?
title Cold-seep ostracods from the western Svalbard margin: direct palaeo-indicator for methane seepage?
title_full Cold-seep ostracods from the western Svalbard margin: direct palaeo-indicator for methane seepage?
title_fullStr Cold-seep ostracods from the western Svalbard margin: direct palaeo-indicator for methane seepage?
title_full_unstemmed Cold-seep ostracods from the western Svalbard margin: direct palaeo-indicator for methane seepage?
title_short Cold-seep ostracods from the western Svalbard margin: direct palaeo-indicator for methane seepage?
title_sort cold-seep ostracods from the western svalbard margin: direct palaeo-indicator for methane seepage?
topic VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Marin geologi: 466
VDP::Mathematics and natural science: 400::Geosciences: 450::Marine geology: 466
topic_facet VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Marin geologi: 466
VDP::Mathematics and natural science: 400::Geosciences: 450::Marine geology: 466
url https://hdl.handle.net/10037/12098
https://doi.org/10.5194/jm-37-139-2018