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.,...
Published in: | Journal of Micropalaeontology |
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Main Authors: | , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2018
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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 |
id | ftunivtroemsoe:oai:munin.uit.no:10037/12098 |
institution | Open Polar |
language | English |
op_collection_id | ftunivtroemsoe |
op_container_end_page | 148 |
op_doi | https://doi.org/10.5194/jm-37-139-2018 |
op_relation | 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 |
op_rights | openAccess |
publishDate | 2018 |
publisher | Copernicus Publications |
record_format | openpolar |
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 |