Seawater carbonate chemistry and abiotic and biotic interactions in the diffusive boundary layer of kelp blades ...

Seaweeds are able to modify the chemical environment at their surface, in a micro‐zone called the diffusive boundary layer (DBL), via their metabolic processes controlled by light intensity. Depending on the thickness of the DBL, sessile invertebrates such as calcifying bryozoans or tube‐forming pol...

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Main Authors: Noisette, Fanny, Hurd, Catriona L
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2018
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.885874
https://doi.pangaea.de/10.1594/PANGAEA.885874
id ftdatacite:10.1594/pangaea.885874
record_format openpolar
spelling ftdatacite:10.1594/pangaea.885874 2024-09-15T18:27:54+00:00 Seawater carbonate chemistry and abiotic and biotic interactions in the diffusive boundary layer of kelp blades ... Noisette, Fanny Hurd, Catriona L 2018 application/zip https://dx.doi.org/10.1594/pangaea.885874 https://doi.pangaea.de/10.1594/PANGAEA.885874 en eng PANGAEA https://dx.doi.org/10.1111/1365-2435.13067 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Benthos Chromista Coast and continental shelf Containers and aquaria 20-1000 L or < 1 m**2 Laboratory experiment Macroalgae Ochrophyta Other Other metabolic rates Primary production/Photosynthesis Single species South Pacific Temperate Ocean Acidification International Coordination Centre OA-ICC Publication Series of Datasets Collection article 2018 ftdatacite https://doi.org/10.1594/pangaea.88587410.1111/1365-2435.13067 2024-08-01T10:56:44Z Seaweeds are able to modify the chemical environment at their surface, in a micro‐zone called the diffusive boundary layer (DBL), via their metabolic processes controlled by light intensity. Depending on the thickness of the DBL, sessile invertebrates such as calcifying bryozoans or tube‐forming polychaetes living on the surface of the blades can be affected by the chemical variations occurring in this microlayer. Especially in the context of ocean acidification (OA), these microhabitats might be considered as a refuge from lower pH, because during the day photosynthesis temporarily raises the pH to values higher than in the mainstream seawater.We assessed the thickness and the characteristics of the DBL at two pH levels (today's average surface ocean pH 8.1 and a reduced pH predicted for the end of the century, pH 7.7) and seawater flows (slow, 0.5 and fast, >8 cm/s) on Ecklonia radiata (kelp) blades. Oxygen and pH profiles from the blade surface to the mainstream seawater were measured with O2 and pH ... Article in Journal/Newspaper Ocean acidification DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Benthos
Chromista
Coast and continental shelf
Containers and aquaria 20-1000 L or < 1 m**2
Laboratory experiment
Macroalgae
Ochrophyta
Other
Other metabolic rates
Primary production/Photosynthesis
Single species
South Pacific
Temperate
Ocean Acidification International Coordination Centre OA-ICC
spellingShingle Benthos
Chromista
Coast and continental shelf
Containers and aquaria 20-1000 L or < 1 m**2
Laboratory experiment
Macroalgae
Ochrophyta
Other
Other metabolic rates
Primary production/Photosynthesis
Single species
South Pacific
Temperate
Ocean Acidification International Coordination Centre OA-ICC
Noisette, Fanny
Hurd, Catriona L
Seawater carbonate chemistry and abiotic and biotic interactions in the diffusive boundary layer of kelp blades ...
topic_facet Benthos
Chromista
Coast and continental shelf
Containers and aquaria 20-1000 L or < 1 m**2
Laboratory experiment
Macroalgae
Ochrophyta
Other
Other metabolic rates
Primary production/Photosynthesis
Single species
South Pacific
Temperate
Ocean Acidification International Coordination Centre OA-ICC
description Seaweeds are able to modify the chemical environment at their surface, in a micro‐zone called the diffusive boundary layer (DBL), via their metabolic processes controlled by light intensity. Depending on the thickness of the DBL, sessile invertebrates such as calcifying bryozoans or tube‐forming polychaetes living on the surface of the blades can be affected by the chemical variations occurring in this microlayer. Especially in the context of ocean acidification (OA), these microhabitats might be considered as a refuge from lower pH, because during the day photosynthesis temporarily raises the pH to values higher than in the mainstream seawater.We assessed the thickness and the characteristics of the DBL at two pH levels (today's average surface ocean pH 8.1 and a reduced pH predicted for the end of the century, pH 7.7) and seawater flows (slow, 0.5 and fast, >8 cm/s) on Ecklonia radiata (kelp) blades. Oxygen and pH profiles from the blade surface to the mainstream seawater were measured with O2 and pH ...
format Article in Journal/Newspaper
author Noisette, Fanny
Hurd, Catriona L
author_facet Noisette, Fanny
Hurd, Catriona L
author_sort Noisette, Fanny
title Seawater carbonate chemistry and abiotic and biotic interactions in the diffusive boundary layer of kelp blades ...
title_short Seawater carbonate chemistry and abiotic and biotic interactions in the diffusive boundary layer of kelp blades ...
title_full Seawater carbonate chemistry and abiotic and biotic interactions in the diffusive boundary layer of kelp blades ...
title_fullStr Seawater carbonate chemistry and abiotic and biotic interactions in the diffusive boundary layer of kelp blades ...
title_full_unstemmed Seawater carbonate chemistry and abiotic and biotic interactions in the diffusive boundary layer of kelp blades ...
title_sort seawater carbonate chemistry and abiotic and biotic interactions in the diffusive boundary layer of kelp blades ...
publisher PANGAEA
publishDate 2018
url https://dx.doi.org/10.1594/pangaea.885874
https://doi.pangaea.de/10.1594/PANGAEA.885874
genre Ocean acidification
genre_facet Ocean acidification
op_relation https://dx.doi.org/10.1111/1365-2435.13067
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.88587410.1111/1365-2435.13067
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