Ecology of stone-encrusting organisms in the Greenland Sea—a review

The Arctic is one of the most rapidly warming regions on Earth. This area is therefore very suitable for conducting studies focused on the influence of climate change on the biota. Marine communities of coastal waters are particularly sensitive to the current environmental changes (e.g., ice-scour i...

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Published in:Polar Research
Main Author: Kuklinski, Piotr
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 2009
Subjects:
Online Access:https://polarresearch.net/index.php/polar/article/view/2825
https://doi.org/10.3402/polar.v28i2.6114
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spelling ftjpolarres:oai:journals.openacademia.net:article/2825 2023-05-15T15:11:22+02:00 Ecology of stone-encrusting organisms in the Greenland Sea—a review Kuklinski, Piotr 2009-08-01 application/pdf https://polarresearch.net/index.php/polar/article/view/2825 https://doi.org/10.3402/polar.v28i2.6114 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/2825/6452 https://polarresearch.net/index.php/polar/article/view/2825 doi:10.3402/polar.v28i2.6114 Copyright (c) 2018 Polar Research Polar Research; Vol. 28 No. 2 (2009); 222-237 1751-8369 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2009 ftjpolarres https://doi.org/10.3402/polar.v28i2.6114 2021-11-11T19:13:21Z The Arctic is one of the most rapidly warming regions on Earth. This area is therefore very suitable for conducting studies focused on the influence of climate change on the biota. Marine communities of coastal waters are particularly sensitive to the current environmental changes (e.g., ice-scour intensity); understanding how community structure changes in response to local perturbations is thus important for providing an insight into how future communities may respond to climate change. This review focuses on the fauna colonizing stones of the Greenland Sea. It summarizes the current state of knowledge about the ecology of organisms inhabiting these substrata across a range of depths, from the intertidal to deeper parts of the continental shelf. In the intertidal zone, no stable or developed assemblage on the rocks is visible. The intertidal zone seems to be fully controlled by physical forces. In contrast, below the intertidal zone a rich and abundant fauna starts to appear on these substrata. Both biotic (e.g., competitive interactions) and abiotic (e.g., ice scour, size of the rock) processes seem to shape stone assemblages in the subtidal zone, yet their influence varies with depth. For example, the abundance of encrusting organisms decreases with depth, as does the intensity of competitive interactions. However, species richness on rocks seems to be in general higher in the deeper parts of the shelf. Possible scenarios of climate change influence on the encrusting biota, gaps in our knowledge about the ecology of stonedwelling faunal assemblages, as well as possible directions of future research, are discussed. Article in Journal/Newspaper Arctic Climate change Greenland Greenland Sea Polar Research Polar Research (E-Journal) Arctic Greenland Polar Research 28 2
institution Open Polar
collection Polar Research (E-Journal)
op_collection_id ftjpolarres
language English
description The Arctic is one of the most rapidly warming regions on Earth. This area is therefore very suitable for conducting studies focused on the influence of climate change on the biota. Marine communities of coastal waters are particularly sensitive to the current environmental changes (e.g., ice-scour intensity); understanding how community structure changes in response to local perturbations is thus important for providing an insight into how future communities may respond to climate change. This review focuses on the fauna colonizing stones of the Greenland Sea. It summarizes the current state of knowledge about the ecology of organisms inhabiting these substrata across a range of depths, from the intertidal to deeper parts of the continental shelf. In the intertidal zone, no stable or developed assemblage on the rocks is visible. The intertidal zone seems to be fully controlled by physical forces. In contrast, below the intertidal zone a rich and abundant fauna starts to appear on these substrata. Both biotic (e.g., competitive interactions) and abiotic (e.g., ice scour, size of the rock) processes seem to shape stone assemblages in the subtidal zone, yet their influence varies with depth. For example, the abundance of encrusting organisms decreases with depth, as does the intensity of competitive interactions. However, species richness on rocks seems to be in general higher in the deeper parts of the shelf. Possible scenarios of climate change influence on the encrusting biota, gaps in our knowledge about the ecology of stonedwelling faunal assemblages, as well as possible directions of future research, are discussed.
format Article in Journal/Newspaper
author Kuklinski, Piotr
spellingShingle Kuklinski, Piotr
Ecology of stone-encrusting organisms in the Greenland Sea—a review
author_facet Kuklinski, Piotr
author_sort Kuklinski, Piotr
title Ecology of stone-encrusting organisms in the Greenland Sea—a review
title_short Ecology of stone-encrusting organisms in the Greenland Sea—a review
title_full Ecology of stone-encrusting organisms in the Greenland Sea—a review
title_fullStr Ecology of stone-encrusting organisms in the Greenland Sea—a review
title_full_unstemmed Ecology of stone-encrusting organisms in the Greenland Sea—a review
title_sort ecology of stone-encrusting organisms in the greenland sea—a review
publisher Norwegian Polar Institute
publishDate 2009
url https://polarresearch.net/index.php/polar/article/view/2825
https://doi.org/10.3402/polar.v28i2.6114
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre Arctic
Climate change
Greenland
Greenland Sea
Polar Research
genre_facet Arctic
Climate change
Greenland
Greenland Sea
Polar Research
op_source Polar Research; Vol. 28 No. 2 (2009); 222-237
1751-8369
op_relation https://polarresearch.net/index.php/polar/article/view/2825/6452
https://polarresearch.net/index.php/polar/article/view/2825
doi:10.3402/polar.v28i2.6114
op_rights Copyright (c) 2018 Polar Research
op_doi https://doi.org/10.3402/polar.v28i2.6114
container_title Polar Research
container_volume 28
container_issue 2
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