Ichnodiversity in the eastern Canadian Arctic in the context of polar microbioerosion patterns
Studies of marine microbioerosion in polar environments are scarce. They include our recent investigations of bioerosion traces preserved in sessile balanid skeletons from the Arctic Svalbard archipelago and the Antarctic Ross Sea. Here, we present results from a third study site, Frobisher Bay, in...
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Norwegian Polar Institute
2022
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Online Access: | https://doi.org/10.33265/polar.v41.8083 https://doaj.org/article/ee0a5bf3f277472887a9203715f23409 |
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fttriple:oai:gotriple.eu:oai:doaj.org/article:ee0a5bf3f277472887a9203715f23409 2023-05-15T14:03:53+02:00 Ichnodiversity in the eastern Canadian Arctic in the context of polar microbioerosion patterns Neele Meyer Max Wisshak Evan N. Edinger Kumiko Azetsu-Scott André Freiwald 2022-04-01 https://doi.org/10.33265/polar.v41.8083 https://doaj.org/article/ee0a5bf3f277472887a9203715f23409 en eng Norwegian Polar Institute 0800-0395 1751-8369 doi:10.33265/polar.v41.8083 https://doaj.org/article/ee0a5bf3f277472887a9203715f23409 undefined Polar Research, Vol 41, Pp 1-15 (2022) ichnotaxa trace fossil assemblage polar environment antarctic ichnocoenoses barnacles geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2022 fttriple https://doi.org/10.33265/polar.v41.8083 2023-01-22T17:53:07Z Studies of marine microbioerosion in polar environments are scarce. They include our recent investigations of bioerosion traces preserved in sessile balanid skeletons from the Arctic Svalbard archipelago and the Antarctic Ross Sea. Here, we present results from a third study site, Frobisher Bay, in the eastern Canadian Arctic, together with a synthesis of our current knowledge of polar bioerosion in both hemispheres. Barnacles from 62 to 94 m water depth in Frobisher Bay were prepared using the cast-embedding technique to enable visualization of microboring traces by scanning electron microscopy. In total, six ichnotaxa of traces produced by organotrophic bioeroders were found. All recorded ichnotaxa were also present in Mosselbukta, Svalbard, and most in the Ross Sea. Frobisher Bay contrasts with Mosselbukta in that it is a siliciclastic-dominated environment and shows a lower ichnodiversity, which may be accounted for by the limited bathymetrical range and a high turbidity and sedimentation rate. We evaluate potential key ichnotaxa for the cold-temperate and polar regions, of which the most suitable are Flagrichnus baiulus and Saccomorpha guttulata, and propose adapted index ichnocoenoses for the interpretation of palaeobathymetry accordingly. Together, the three studies allow us to make provisional considerations about the biogeographical distribution of polar microbioerosion traces reflecting the ecophysiological limits of their makers. Article in Journal/Newspaper Antarc* Antarctic Arctic Frobisher Bay Polar Research Ross Sea Svalbard Unknown Antarctic Arctic Frobisher Bay ENVELOPE(-66.581,-66.581,62.834,62.834) Mosselbukta ENVELOPE(15.955,15.955,79.891,79.891) Ross Sea Svalbard Svalbard Archipelago The Antarctic Polar Research 41 |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
fttriple |
language |
English |
topic |
ichnotaxa trace fossil assemblage polar environment antarctic ichnocoenoses barnacles geo |
spellingShingle |
ichnotaxa trace fossil assemblage polar environment antarctic ichnocoenoses barnacles geo Neele Meyer Max Wisshak Evan N. Edinger Kumiko Azetsu-Scott André Freiwald Ichnodiversity in the eastern Canadian Arctic in the context of polar microbioerosion patterns |
topic_facet |
ichnotaxa trace fossil assemblage polar environment antarctic ichnocoenoses barnacles geo |
description |
Studies of marine microbioerosion in polar environments are scarce. They include our recent investigations of bioerosion traces preserved in sessile balanid skeletons from the Arctic Svalbard archipelago and the Antarctic Ross Sea. Here, we present results from a third study site, Frobisher Bay, in the eastern Canadian Arctic, together with a synthesis of our current knowledge of polar bioerosion in both hemispheres. Barnacles from 62 to 94 m water depth in Frobisher Bay were prepared using the cast-embedding technique to enable visualization of microboring traces by scanning electron microscopy. In total, six ichnotaxa of traces produced by organotrophic bioeroders were found. All recorded ichnotaxa were also present in Mosselbukta, Svalbard, and most in the Ross Sea. Frobisher Bay contrasts with Mosselbukta in that it is a siliciclastic-dominated environment and shows a lower ichnodiversity, which may be accounted for by the limited bathymetrical range and a high turbidity and sedimentation rate. We evaluate potential key ichnotaxa for the cold-temperate and polar regions, of which the most suitable are Flagrichnus baiulus and Saccomorpha guttulata, and propose adapted index ichnocoenoses for the interpretation of palaeobathymetry accordingly. Together, the three studies allow us to make provisional considerations about the biogeographical distribution of polar microbioerosion traces reflecting the ecophysiological limits of their makers. |
format |
Article in Journal/Newspaper |
author |
Neele Meyer Max Wisshak Evan N. Edinger Kumiko Azetsu-Scott André Freiwald |
author_facet |
Neele Meyer Max Wisshak Evan N. Edinger Kumiko Azetsu-Scott André Freiwald |
author_sort |
Neele Meyer |
title |
Ichnodiversity in the eastern Canadian Arctic in the context of polar microbioerosion patterns |
title_short |
Ichnodiversity in the eastern Canadian Arctic in the context of polar microbioerosion patterns |
title_full |
Ichnodiversity in the eastern Canadian Arctic in the context of polar microbioerosion patterns |
title_fullStr |
Ichnodiversity in the eastern Canadian Arctic in the context of polar microbioerosion patterns |
title_full_unstemmed |
Ichnodiversity in the eastern Canadian Arctic in the context of polar microbioerosion patterns |
title_sort |
ichnodiversity in the eastern canadian arctic in the context of polar microbioerosion patterns |
publisher |
Norwegian Polar Institute |
publishDate |
2022 |
url |
https://doi.org/10.33265/polar.v41.8083 https://doaj.org/article/ee0a5bf3f277472887a9203715f23409 |
long_lat |
ENVELOPE(-66.581,-66.581,62.834,62.834) ENVELOPE(15.955,15.955,79.891,79.891) |
geographic |
Antarctic Arctic Frobisher Bay Mosselbukta Ross Sea Svalbard Svalbard Archipelago The Antarctic |
geographic_facet |
Antarctic Arctic Frobisher Bay Mosselbukta Ross Sea Svalbard Svalbard Archipelago The Antarctic |
genre |
Antarc* Antarctic Arctic Frobisher Bay Polar Research Ross Sea Svalbard |
genre_facet |
Antarc* Antarctic Arctic Frobisher Bay Polar Research Ross Sea Svalbard |
op_source |
Polar Research, Vol 41, Pp 1-15 (2022) |
op_relation |
0800-0395 1751-8369 doi:10.33265/polar.v41.8083 https://doaj.org/article/ee0a5bf3f277472887a9203715f23409 |
op_rights |
undefined |
op_doi |
https://doi.org/10.33265/polar.v41.8083 |
container_title |
Polar Research |
container_volume |
41 |
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1766274736344530944 |