Seawater pH, and not inorganic nitrogen source, affects pH at the blade surface of Macrocystis pyrifera: implications for responses of the giant kelp to future oceanic conditions

Ocean acidification (OA), the ongoing decline in seawater pH, is predicted to have wide-ranging effects on marine organisms and ecosystems. For seaweeds, the pH at the thallus surface, within the diffusion boundary layer (DBL), is one of the factors controlling their response to OA. Surface pH is co...

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Published in:Physiologia Plantarum
Main Authors: Fernandez, PA, Roleda, MY, Leal, PP, Hurd, CL
Format: Article in Journal/Newspaper
Language:unknown
Published: Blackwell Munksgaard 2017
Subjects:
Online Access:https://eprints.utas.edu.au/38953/
http://dx.doi.org/oi:10.1111/ppl.12478
id ftunivtasmania:oai:eprints.utas.edu.au:38953
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spelling ftunivtasmania:oai:eprints.utas.edu.au:38953 2023-05-15T17:50:43+02:00 Seawater pH, and not inorganic nitrogen source, affects pH at the blade surface of Macrocystis pyrifera: implications for responses of the giant kelp to future oceanic conditions Fernandez, PA Roleda, MY Leal, PP Hurd, CL 2017 https://eprints.utas.edu.au/38953/ http://dx.doi.org/oi:10.1111/ppl.12478 unknown Blackwell Munksgaard Fernandez, PA, Roleda, MY, Leal, PP and Hurd, CL orcid:0000-0001-9965-4917 2017 , 'Seawater pH, and not inorganic nitrogen source, affects pH at the blade surface of Macrocystis pyrifera: implications for responses of the giant kelp to future oceanic conditions' , Physiologia Plantarum, vol. 159, no. 1 , pp. 107-119 , doi:10.1111/ppl.12478 <http://dx.doi.org/10.1111/ppl.12478>. Macrocystis kelp ocean acidification nitrogen climate change Article PeerReviewed 2017 ftunivtasmania https://doi.org/10.1111/ppl.12478 2021-12-13T23:18:00Z Ocean acidification (OA), the ongoing decline in seawater pH, is predicted to have wide-ranging effects on marine organisms and ecosystems. For seaweeds, the pH at the thallus surface, within the diffusion boundary layer (DBL), is one of the factors controlling their response to OA. Surface pH is controlled by both the pH of the bulk seawater and by the seaweeds’ metabolism: photosynthesis and respiration increase and decrease pH within the DBL (pHDBL), respectively. However, other metabolic processes, especially the uptake of inorganic nitrogen (Ni; NO3− and NH4+) may also affect the pHDBL. Using Macrocystis pyrifera, we hypothesized that (1) NO3− uptake will increase the pHDBL, whereas NH4+ uptake will decrease it, (2) if NO3− is cotransported with H+, increases in pHDBL would be greater under an OA treatment (pH = 7.65) than under an ambient treatment (pH = 8.00), and (3) decreases in pHDBL will be smaller at pH 7.65 than at pH 8.00, as higher external [H+] might affect the strength of the diffusion gradient. Overall, Ni source did not affect the pHDBL. However, increases in pHDBL were greater at pH 7.65 than at pH 8.00. CO2 uptake was higher at pH 7.65 than at pH 8.00, whereas HCO3− uptake was unaffected by pH. Photosynthesis and respiration control pHDBL rather than Ni uptake. We suggest that under future OA, Macrocystis pyrifera will metabolically modify its surface microenvironment such that the physiological processes of photosynthesis and Ni uptake will not be affected by a reduced pH. Article in Journal/Newspaper Ocean acidification University of Tasmania: UTas ePrints Physiologia Plantarum 159 1 107 119
institution Open Polar
collection University of Tasmania: UTas ePrints
op_collection_id ftunivtasmania
language unknown
topic Macrocystis
kelp
ocean acidification
nitrogen
climate change
spellingShingle Macrocystis
kelp
ocean acidification
nitrogen
climate change
Fernandez, PA
Roleda, MY
Leal, PP
Hurd, CL
Seawater pH, and not inorganic nitrogen source, affects pH at the blade surface of Macrocystis pyrifera: implications for responses of the giant kelp to future oceanic conditions
topic_facet Macrocystis
kelp
ocean acidification
nitrogen
climate change
description Ocean acidification (OA), the ongoing decline in seawater pH, is predicted to have wide-ranging effects on marine organisms and ecosystems. For seaweeds, the pH at the thallus surface, within the diffusion boundary layer (DBL), is one of the factors controlling their response to OA. Surface pH is controlled by both the pH of the bulk seawater and by the seaweeds’ metabolism: photosynthesis and respiration increase and decrease pH within the DBL (pHDBL), respectively. However, other metabolic processes, especially the uptake of inorganic nitrogen (Ni; NO3− and NH4+) may also affect the pHDBL. Using Macrocystis pyrifera, we hypothesized that (1) NO3− uptake will increase the pHDBL, whereas NH4+ uptake will decrease it, (2) if NO3− is cotransported with H+, increases in pHDBL would be greater under an OA treatment (pH = 7.65) than under an ambient treatment (pH = 8.00), and (3) decreases in pHDBL will be smaller at pH 7.65 than at pH 8.00, as higher external [H+] might affect the strength of the diffusion gradient. Overall, Ni source did not affect the pHDBL. However, increases in pHDBL were greater at pH 7.65 than at pH 8.00. CO2 uptake was higher at pH 7.65 than at pH 8.00, whereas HCO3− uptake was unaffected by pH. Photosynthesis and respiration control pHDBL rather than Ni uptake. We suggest that under future OA, Macrocystis pyrifera will metabolically modify its surface microenvironment such that the physiological processes of photosynthesis and Ni uptake will not be affected by a reduced pH.
format Article in Journal/Newspaper
author Fernandez, PA
Roleda, MY
Leal, PP
Hurd, CL
author_facet Fernandez, PA
Roleda, MY
Leal, PP
Hurd, CL
author_sort Fernandez, PA
title Seawater pH, and not inorganic nitrogen source, affects pH at the blade surface of Macrocystis pyrifera: implications for responses of the giant kelp to future oceanic conditions
title_short Seawater pH, and not inorganic nitrogen source, affects pH at the blade surface of Macrocystis pyrifera: implications for responses of the giant kelp to future oceanic conditions
title_full Seawater pH, and not inorganic nitrogen source, affects pH at the blade surface of Macrocystis pyrifera: implications for responses of the giant kelp to future oceanic conditions
title_fullStr Seawater pH, and not inorganic nitrogen source, affects pH at the blade surface of Macrocystis pyrifera: implications for responses of the giant kelp to future oceanic conditions
title_full_unstemmed Seawater pH, and not inorganic nitrogen source, affects pH at the blade surface of Macrocystis pyrifera: implications for responses of the giant kelp to future oceanic conditions
title_sort seawater ph, and not inorganic nitrogen source, affects ph at the blade surface of macrocystis pyrifera: implications for responses of the giant kelp to future oceanic conditions
publisher Blackwell Munksgaard
publishDate 2017
url https://eprints.utas.edu.au/38953/
http://dx.doi.org/oi:10.1111/ppl.12478
genre Ocean acidification
genre_facet Ocean acidification
op_relation Fernandez, PA, Roleda, MY, Leal, PP and Hurd, CL orcid:0000-0001-9965-4917 2017 , 'Seawater pH, and not inorganic nitrogen source, affects pH at the blade surface of Macrocystis pyrifera: implications for responses of the giant kelp to future oceanic conditions' , Physiologia Plantarum, vol. 159, no. 1 , pp. 107-119 , doi:10.1111/ppl.12478 <http://dx.doi.org/10.1111/ppl.12478>.
op_doi https://doi.org/10.1111/ppl.12478
container_title Physiologia Plantarum
container_volume 159
container_issue 1
container_start_page 107
op_container_end_page 119
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