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...

Full description

Bibliographic Details
Published in:Physiologia Plantarum
Main Authors: Fernandez, PA, Roleda, MY, Leal, PP, Hurd, CL
Format: Article in Journal/Newspaper
Language:English
Published: Blackwell Munksgaard 2017
Subjects:
Online Access:http://dx.doi.org/oi:10.1111/ppl.12478
https://doi.org/10.1111/ppl.12478
http://www.ncbi.nlm.nih.gov/pubmed/27293117
http://ecite.utas.edu.au/112297
id ftunivtasecite:oai:ecite.utas.edu.au:112297
record_format openpolar
spelling ftunivtasecite:oai:ecite.utas.edu.au:112297 2023-05-15T17:51:48+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 http://dx.doi.org/oi:10.1111/ppl.12478 https://doi.org/10.1111/ppl.12478 http://www.ncbi.nlm.nih.gov/pubmed/27293117 http://ecite.utas.edu.au/112297 en eng Blackwell Munksgaard http://dx.doi.org/10.1111/ppl.12478 Fernandez, PA and Roleda, MY and Leal, PP and 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, Physiologia Plantarum, 159, (1) pp. 107-119. ISSN 0031-9317 (2017) [Refereed Article] http://www.ncbi.nlm.nih.gov/pubmed/27293117 http://ecite.utas.edu.au/112297 Biological Sciences Plant Biology Phycology (incl. Marine Grasses) Refereed Article PeerReviewed 2017 ftunivtasecite https://doi.org/10.1111/ppl.12478 2019-12-13T22:12:35Z 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 (pH DBL ), respectively. However, other metabolic processes, especially the uptake of inorganic nitrogen (N i NO 3 − and NH 4 + ) may also affect the pH DBL . Using Macrocystis pyrifera , we hypothesized that (1) NO 3 − uptake will increase the pH DBL , whereas NH 4 + uptake will decrease it, (2) if NO 3 − is cotransported with H + , increases in pH DBL would be greater under an OA treatment (pH=7.65) than under an ambient treatment (pH=8.00), and (3) decreases in pH DBL 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, N i source did not affect the pH DBL . However, increases in pH DBL were greater at pH 7.65 than at pH 8.00. CO 2 uptake was higher at pH 7.65 than at pH 8.00, whereas HCO 3 − uptake was unaffected by pH. Photosynthesis and respiration control pH DBL rather than N i uptake. We suggest that under future OA, Macrocystis pyrifera will metabolically modify its surface microenvironment such that the physiological processes of photosynthesis and N i uptake will not be affected by a reduced pH. Article in Journal/Newspaper Ocean acidification eCite UTAS (University of Tasmania) Physiologia Plantarum 159 1 107 119
institution Open Polar
collection eCite UTAS (University of Tasmania)
op_collection_id ftunivtasecite
language English
topic Biological Sciences
Plant Biology
Phycology (incl. Marine Grasses)
spellingShingle Biological Sciences
Plant Biology
Phycology (incl. Marine Grasses)
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 Biological Sciences
Plant Biology
Phycology (incl. Marine Grasses)
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 (pH DBL ), respectively. However, other metabolic processes, especially the uptake of inorganic nitrogen (N i NO 3 − and NH 4 + ) may also affect the pH DBL . Using Macrocystis pyrifera , we hypothesized that (1) NO 3 − uptake will increase the pH DBL , whereas NH 4 + uptake will decrease it, (2) if NO 3 − is cotransported with H + , increases in pH DBL would be greater under an OA treatment (pH=7.65) than under an ambient treatment (pH=8.00), and (3) decreases in pH DBL 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, N i source did not affect the pH DBL . However, increases in pH DBL were greater at pH 7.65 than at pH 8.00. CO 2 uptake was higher at pH 7.65 than at pH 8.00, whereas HCO 3 − uptake was unaffected by pH. Photosynthesis and respiration control pH DBL rather than N i uptake. We suggest that under future OA, Macrocystis pyrifera will metabolically modify its surface microenvironment such that the physiological processes of photosynthesis and N i 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 http://dx.doi.org/oi:10.1111/ppl.12478
https://doi.org/10.1111/ppl.12478
http://www.ncbi.nlm.nih.gov/pubmed/27293117
http://ecite.utas.edu.au/112297
genre Ocean acidification
genre_facet Ocean acidification
op_relation http://dx.doi.org/10.1111/ppl.12478
Fernandez, PA and Roleda, MY and Leal, PP and 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, Physiologia Plantarum, 159, (1) pp. 107-119. ISSN 0031-9317 (2017) [Refereed Article]
http://www.ncbi.nlm.nih.gov/pubmed/27293117
http://ecite.utas.edu.au/112297
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
_version_ 1766159047810088960