Spatial distribution of benthic macrofauna in the Central Arctic Ocean

Permanent sea-ice cover and low primary productivity in the mostly ice-covered Central Arctic ocean basins result in significantly lower biomass and density of macrobenthos in the abyssal plains compared to the continental slopes. However, little is known on bathymetric and regional effects on the m...

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Published in:PLOS ONE
Main Authors: Vedenin, A., Gusky, M., Gebruk, A., Kremenetskaia, A., Rybakova, E., Boetius, A.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2018
Subjects:
Online Access:http://hdl.handle.net/21.11116/0000-0003-B88D-F
http://hdl.handle.net/21.11116/0000-0003-B88F-D
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spelling ftpubman:oai:pure.mpg.de:item_3031371 2023-08-20T04:03:55+02:00 Spatial distribution of benthic macrofauna in the Central Arctic Ocean Vedenin, A. Gusky, M. Gebruk, A. Kremenetskaia, A. Rybakova, E. Boetius, A. 2018 application/pdf http://hdl.handle.net/21.11116/0000-0003-B88D-F http://hdl.handle.net/21.11116/0000-0003-B88F-D unknown info:eu-repo/semantics/altIdentifier/doi/10.1371/journal.pone.0200121 http://hdl.handle.net/21.11116/0000-0003-B88D-F http://hdl.handle.net/21.11116/0000-0003-B88F-D info:eu-repo/semantics/openAccess PLOS ONE info:eu-repo/semantics/article 2018 ftpubman https://doi.org/10.1371/journal.pone.0200121 2023-08-01T23:54:42Z Permanent sea-ice cover and low primary productivity in the mostly ice-covered Central Arctic ocean basins result in significantly lower biomass and density of macrobenthos in the abyssal plains compared to the continental slopes. However, little is known on bathymetric and regional effects on the macrobenthos diversity. This study synthesizes new and available macrobenthos data to provide a baseline for future studies of the effects of Arctic change on macrofauna community composition in the Arctic basins. Samples collected during three expeditions (in 1993,2012 and 2015) at 37 stations on the slope of the Barents and Laptev Seas and in the abyssal of the Nansen and Amundsen Basins in the depth range from 38 m to 4381 m were used for a quantitative analysis of species composition, abundance and biomass. Benthic communities clustered in five depth ranges across the slope and basin. A parabolic pattern of species diversity change with depth was found, with the diversity maximum for macrofauna at the shelf edge at depths of 100-300 m. This deviates from the typical species richness peak at mid-slope depths of 1500-3000 m in temperate oceans. Due to the limited availability of standardized benthos data, it remains difficult to assess if and how the significant sea-ice loss observed in the past decade has affected benthic community composition. The polychaete Ymerana pteropoda and the bryozoan Nolella sp. were found for the first time in the deep Nansen and Amundsen Basins. Article in Journal/Newspaper Arctic Arctic Ocean laptev Sea ice Max Planck Society: MPG.PuRe Arctic Arctic Ocean PLOS ONE 13 10 e0200121
institution Open Polar
collection Max Planck Society: MPG.PuRe
op_collection_id ftpubman
language unknown
description Permanent sea-ice cover and low primary productivity in the mostly ice-covered Central Arctic ocean basins result in significantly lower biomass and density of macrobenthos in the abyssal plains compared to the continental slopes. However, little is known on bathymetric and regional effects on the macrobenthos diversity. This study synthesizes new and available macrobenthos data to provide a baseline for future studies of the effects of Arctic change on macrofauna community composition in the Arctic basins. Samples collected during three expeditions (in 1993,2012 and 2015) at 37 stations on the slope of the Barents and Laptev Seas and in the abyssal of the Nansen and Amundsen Basins in the depth range from 38 m to 4381 m were used for a quantitative analysis of species composition, abundance and biomass. Benthic communities clustered in five depth ranges across the slope and basin. A parabolic pattern of species diversity change with depth was found, with the diversity maximum for macrofauna at the shelf edge at depths of 100-300 m. This deviates from the typical species richness peak at mid-slope depths of 1500-3000 m in temperate oceans. Due to the limited availability of standardized benthos data, it remains difficult to assess if and how the significant sea-ice loss observed in the past decade has affected benthic community composition. The polychaete Ymerana pteropoda and the bryozoan Nolella sp. were found for the first time in the deep Nansen and Amundsen Basins.
format Article in Journal/Newspaper
author Vedenin, A.
Gusky, M.
Gebruk, A.
Kremenetskaia, A.
Rybakova, E.
Boetius, A.
spellingShingle Vedenin, A.
Gusky, M.
Gebruk, A.
Kremenetskaia, A.
Rybakova, E.
Boetius, A.
Spatial distribution of benthic macrofauna in the Central Arctic Ocean
author_facet Vedenin, A.
Gusky, M.
Gebruk, A.
Kremenetskaia, A.
Rybakova, E.
Boetius, A.
author_sort Vedenin, A.
title Spatial distribution of benthic macrofauna in the Central Arctic Ocean
title_short Spatial distribution of benthic macrofauna in the Central Arctic Ocean
title_full Spatial distribution of benthic macrofauna in the Central Arctic Ocean
title_fullStr Spatial distribution of benthic macrofauna in the Central Arctic Ocean
title_full_unstemmed Spatial distribution of benthic macrofauna in the Central Arctic Ocean
title_sort spatial distribution of benthic macrofauna in the central arctic ocean
publishDate 2018
url http://hdl.handle.net/21.11116/0000-0003-B88D-F
http://hdl.handle.net/21.11116/0000-0003-B88F-D
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
laptev
Sea ice
genre_facet Arctic
Arctic Ocean
laptev
Sea ice
op_source PLOS ONE
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1371/journal.pone.0200121
http://hdl.handle.net/21.11116/0000-0003-B88D-F
http://hdl.handle.net/21.11116/0000-0003-B88F-D
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1371/journal.pone.0200121
container_title PLOS ONE
container_volume 13
container_issue 10
container_start_page e0200121
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