Fine-scale nutrient and carbonate system dynamics around cold-water coral reefs in the northeast Atlantic

Ocean acidification has been suggested as a serious threat to the future existence of cold-water corals (CWC). However, there are few fine-scale temporal and spatial datasets of carbonate and nutrients conditions available for these reefs, which can provide a baseline definition of extant conditions...

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Published in:Scientific Reports
Main Authors: Findlay, Helen S., Hennige, Sebastian J., Wicks, Laura C., Navas, Juan Moreno, Woodward, E. Malcolm S., Roberts, J. Murray
Format: Text
Language:English
Published: Nature Publishing Group 2014
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3895924
http://www.ncbi.nlm.nih.gov/pubmed/24441283
https://doi.org/10.1038/srep03671
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author Findlay, Helen S.
Hennige, Sebastian J.
Wicks, Laura C.
Navas, Juan Moreno
Woodward, E. Malcolm S.
Roberts, J. Murray
author_facet Findlay, Helen S.
Hennige, Sebastian J.
Wicks, Laura C.
Navas, Juan Moreno
Woodward, E. Malcolm S.
Roberts, J. Murray
author_sort Findlay, Helen S.
collection PubMed Central (PMC)
container_issue 1
container_title Scientific Reports
container_volume 4
description Ocean acidification has been suggested as a serious threat to the future existence of cold-water corals (CWC). However, there are few fine-scale temporal and spatial datasets of carbonate and nutrients conditions available for these reefs, which can provide a baseline definition of extant conditions. Here we provide observational data from four different sites in the northeast Atlantic that are known habitats for CWC. These habitats differ by depth and by the nature of the coral habitat. At depths where CWC are known to occur across these sites the dissolved inorganic carbon ranged from 2088 to 2186 μmol kg−1, alkalinity ranged from 2299 to 2346 μmol kg−1, and aragonite Ω ranged from 1.35 to 2.44. At two sites fine-scale hydrodynamics caused increased variability in the carbonate and nutrient conditions over daily time-scales. The observed high level of variability must be taken into account when assessing CWC sensitivities to future environmental change.
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genre Northeast Atlantic
Ocean acidification
genre_facet Northeast Atlantic
Ocean acidification
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op_doi https://doi.org/10.1038/srep03671
op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3895924
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op_rights Copyright © 2014, Macmillan Publishers Limited. All rights reserved
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This work is licensed under a Creative Commons Attribution 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by/3.0/
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spelling ftpubmed:oai:pubmedcentral.nih.gov:3895924 2025-01-16T23:50:31+00:00 Fine-scale nutrient and carbonate system dynamics around cold-water coral reefs in the northeast Atlantic Findlay, Helen S. Hennige, Sebastian J. Wicks, Laura C. Navas, Juan Moreno Woodward, E. Malcolm S. Roberts, J. Murray 2014-01-20 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3895924 http://www.ncbi.nlm.nih.gov/pubmed/24441283 https://doi.org/10.1038/srep03671 en eng Nature Publishing Group http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3895924 http://www.ncbi.nlm.nih.gov/pubmed/24441283 http://dx.doi.org/10.1038/srep03671 Copyright © 2014, Macmillan Publishers Limited. All rights reserved http://creativecommons.org/licenses/by/3.0/ This work is licensed under a Creative Commons Attribution 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by/3.0/ CC-BY Article Text 2014 ftpubmed https://doi.org/10.1038/srep03671 2014-01-26T01:42:34Z Ocean acidification has been suggested as a serious threat to the future existence of cold-water corals (CWC). However, there are few fine-scale temporal and spatial datasets of carbonate and nutrients conditions available for these reefs, which can provide a baseline definition of extant conditions. Here we provide observational data from four different sites in the northeast Atlantic that are known habitats for CWC. These habitats differ by depth and by the nature of the coral habitat. At depths where CWC are known to occur across these sites the dissolved inorganic carbon ranged from 2088 to 2186 μmol kg−1, alkalinity ranged from 2299 to 2346 μmol kg−1, and aragonite Ω ranged from 1.35 to 2.44. At two sites fine-scale hydrodynamics caused increased variability in the carbonate and nutrient conditions over daily time-scales. The observed high level of variability must be taken into account when assessing CWC sensitivities to future environmental change. Text Northeast Atlantic Ocean acidification PubMed Central (PMC) Scientific Reports 4 1
spellingShingle Article
Findlay, Helen S.
Hennige, Sebastian J.
Wicks, Laura C.
Navas, Juan Moreno
Woodward, E. Malcolm S.
Roberts, J. Murray
Fine-scale nutrient and carbonate system dynamics around cold-water coral reefs in the northeast Atlantic
title Fine-scale nutrient and carbonate system dynamics around cold-water coral reefs in the northeast Atlantic
title_full Fine-scale nutrient and carbonate system dynamics around cold-water coral reefs in the northeast Atlantic
title_fullStr Fine-scale nutrient and carbonate system dynamics around cold-water coral reefs in the northeast Atlantic
title_full_unstemmed Fine-scale nutrient and carbonate system dynamics around cold-water coral reefs in the northeast Atlantic
title_short Fine-scale nutrient and carbonate system dynamics around cold-water coral reefs in the northeast Atlantic
title_sort fine-scale nutrient and carbonate system dynamics around cold-water coral reefs in the northeast atlantic
topic Article
topic_facet Article
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3895924
http://www.ncbi.nlm.nih.gov/pubmed/24441283
https://doi.org/10.1038/srep03671