Spatiotemporal Variability of Dimethylsulphoniopropionate on a Fringing Coral Reef : The Role of Reefal Carbonate Chemistry and Environmental Variability

This research was financially supported by a NERC studentship (NE/H525303/1) to HB, a University of Glasgow Mobility Scholarship to HB and PD and a Royal Society of Edinburgh/Scottish Government Fellowship (RSE 48701/1) and Carnegie Trust for the Universities of Scotland grant to NK. The funders had...

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Published in:PLoS ONE
Main Authors: Burdett, Heidi L., Donohue, Penelope J. C., Hatton, Angela D., Alwany, Magdy A., Kamenos, Nicholas A.
Other Authors: University of St Andrews. Earth and Environmental Sciences
Format: Article in Journal/Newspaper
Language:English
Published: 2013
Subjects:
Q
Online Access:http://hdl.handle.net/10023/4136
https://doi.org/10.1371/journal.pone.0064651
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spelling ftstandrewserep:oai:research-repository.st-andrews.ac.uk:10023/4136 2023-07-02T03:33:21+02:00 Spatiotemporal Variability of Dimethylsulphoniopropionate on a Fringing Coral Reef : The Role of Reefal Carbonate Chemistry and Environmental Variability Burdett, Heidi L. Donohue, Penelope J. C. Hatton, Angela D. Alwany, Magdy A. Kamenos, Nicholas A. University of St Andrews. Earth and Environmental Sciences 2013-11-01T12:01:05Z application/pdf http://hdl.handle.net/10023/4136 https://doi.org/10.1371/journal.pone.0064651 eng eng PLoS One Burdett , H L , Donohue , P J C , Hatton , A D , Alwany , M A & Kamenos , N A 2013 , ' Spatiotemporal Variability of Dimethylsulphoniopropionate on a Fringing Coral Reef : The Role of Reefal Carbonate Chemistry and Environmental Variability ' , PLoS One , vol. 8 , no. 5 , e64651 , pp. 1-8 . https://doi.org/10.1371/journal.pone.0064651 1932-6203 PURE: 75923686 PURE UUID: 07d76622-9d08-4bab-b2a8-5d50c6012a81 WOS: 000319733000073 Scopus: 84878408233 http://hdl.handle.net/10023/4136 https://doi.org/10.1371/journal.pone.0064651 © 2013 Burdett et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. Great Barrier Reef Ocean acidification Marine macroalgae Elevated CO2 Algae DMSP Seawater Calcification Dimethylsufide Impacts Q Science SDG 14 - Life Below Water Q Journal article 2013 ftstandrewserep https://doi.org/10.1371/journal.pone.0064651 2023-06-13T18:25:21Z This research was financially supported by a NERC studentship (NE/H525303/1) to HB, a University of Glasgow Mobility Scholarship to HB and PD and a Royal Society of Edinburgh/Scottish Government Fellowship (RSE 48701/1) and Carnegie Trust for the Universities of Scotland grant to NK. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript. Oceanic pH is projected to decrease by up to 0.5 units by 2100 (a process known as ocean acidification, OA), reducing the calcium carbonate saturation state of the oceans. The coastal ocean is expected to experience periods of even lower carbonate saturation state because of the inherent natural variability of coastal habitats. Thus, in order to accurately project the impact of OA on the coastal ocean, we must first understand its natural variability. The production of dimethylsulphoniopropionate (DMSP) by marine algae and the release of DMSP's breakdown product dimethylsulphide (DMS) are often related to environmental stress. This study investigated the spatiotemporal response of tropical macroalgae (Padina sp., Amphiroa sp. and Turbinaria sp.) and the overlying water column to natural changes in reefal carbonate chemistry. We compared macroalgal intracellular DMSP and water column DMSP+DMS concentrations between the environmentally stable reef crest and environmentally variable reef flat of the fringing Suleman Reef, Egypt, over 45-hour sampling periods. Similar diel patterns were observed throughout: maximum intracellular DMSP and water column DMS/P concentrations were observed at night, coinciding with the time of lowest carbonate saturation state. Spatially, water column DMS/P concentrations were highest over areas dominated by seagrass and macroalgae (dissolved DMS/P) and phytoplankton (particulate DMS/P) rather than corals. This research suggests that macroalgae may use DMSP to maintain metabolic function during periods of low carbonate saturation state. In the reef system, seagrass and macroalgae ... Article in Journal/Newspaper Ocean acidification University of St Andrews: Digital Research Repository PLoS ONE 8 5 e64651
institution Open Polar
collection University of St Andrews: Digital Research Repository
op_collection_id ftstandrewserep
language English
topic Great Barrier Reef
Ocean acidification
Marine macroalgae
Elevated CO2
Algae
DMSP
Seawater
Calcification
Dimethylsufide
Impacts
Q Science
SDG 14 - Life Below Water
Q
spellingShingle Great Barrier Reef
Ocean acidification
Marine macroalgae
Elevated CO2
Algae
DMSP
Seawater
Calcification
Dimethylsufide
Impacts
Q Science
SDG 14 - Life Below Water
Q
Burdett, Heidi L.
Donohue, Penelope J. C.
Hatton, Angela D.
Alwany, Magdy A.
Kamenos, Nicholas A.
Spatiotemporal Variability of Dimethylsulphoniopropionate on a Fringing Coral Reef : The Role of Reefal Carbonate Chemistry and Environmental Variability
topic_facet Great Barrier Reef
Ocean acidification
Marine macroalgae
Elevated CO2
Algae
DMSP
Seawater
Calcification
Dimethylsufide
Impacts
Q Science
SDG 14 - Life Below Water
Q
description This research was financially supported by a NERC studentship (NE/H525303/1) to HB, a University of Glasgow Mobility Scholarship to HB and PD and a Royal Society of Edinburgh/Scottish Government Fellowship (RSE 48701/1) and Carnegie Trust for the Universities of Scotland grant to NK. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript. Oceanic pH is projected to decrease by up to 0.5 units by 2100 (a process known as ocean acidification, OA), reducing the calcium carbonate saturation state of the oceans. The coastal ocean is expected to experience periods of even lower carbonate saturation state because of the inherent natural variability of coastal habitats. Thus, in order to accurately project the impact of OA on the coastal ocean, we must first understand its natural variability. The production of dimethylsulphoniopropionate (DMSP) by marine algae and the release of DMSP's breakdown product dimethylsulphide (DMS) are often related to environmental stress. This study investigated the spatiotemporal response of tropical macroalgae (Padina sp., Amphiroa sp. and Turbinaria sp.) and the overlying water column to natural changes in reefal carbonate chemistry. We compared macroalgal intracellular DMSP and water column DMSP+DMS concentrations between the environmentally stable reef crest and environmentally variable reef flat of the fringing Suleman Reef, Egypt, over 45-hour sampling periods. Similar diel patterns were observed throughout: maximum intracellular DMSP and water column DMS/P concentrations were observed at night, coinciding with the time of lowest carbonate saturation state. Spatially, water column DMS/P concentrations were highest over areas dominated by seagrass and macroalgae (dissolved DMS/P) and phytoplankton (particulate DMS/P) rather than corals. This research suggests that macroalgae may use DMSP to maintain metabolic function during periods of low carbonate saturation state. In the reef system, seagrass and macroalgae ...
author2 University of St Andrews. Earth and Environmental Sciences
format Article in Journal/Newspaper
author Burdett, Heidi L.
Donohue, Penelope J. C.
Hatton, Angela D.
Alwany, Magdy A.
Kamenos, Nicholas A.
author_facet Burdett, Heidi L.
Donohue, Penelope J. C.
Hatton, Angela D.
Alwany, Magdy A.
Kamenos, Nicholas A.
author_sort Burdett, Heidi L.
title Spatiotemporal Variability of Dimethylsulphoniopropionate on a Fringing Coral Reef : The Role of Reefal Carbonate Chemistry and Environmental Variability
title_short Spatiotemporal Variability of Dimethylsulphoniopropionate on a Fringing Coral Reef : The Role of Reefal Carbonate Chemistry and Environmental Variability
title_full Spatiotemporal Variability of Dimethylsulphoniopropionate on a Fringing Coral Reef : The Role of Reefal Carbonate Chemistry and Environmental Variability
title_fullStr Spatiotemporal Variability of Dimethylsulphoniopropionate on a Fringing Coral Reef : The Role of Reefal Carbonate Chemistry and Environmental Variability
title_full_unstemmed Spatiotemporal Variability of Dimethylsulphoniopropionate on a Fringing Coral Reef : The Role of Reefal Carbonate Chemistry and Environmental Variability
title_sort spatiotemporal variability of dimethylsulphoniopropionate on a fringing coral reef : the role of reefal carbonate chemistry and environmental variability
publishDate 2013
url http://hdl.handle.net/10023/4136
https://doi.org/10.1371/journal.pone.0064651
genre Ocean acidification
genre_facet Ocean acidification
op_relation PLoS One
Burdett , H L , Donohue , P J C , Hatton , A D , Alwany , M A & Kamenos , N A 2013 , ' Spatiotemporal Variability of Dimethylsulphoniopropionate on a Fringing Coral Reef : The Role of Reefal Carbonate Chemistry and Environmental Variability ' , PLoS One , vol. 8 , no. 5 , e64651 , pp. 1-8 . https://doi.org/10.1371/journal.pone.0064651
1932-6203
PURE: 75923686
PURE UUID: 07d76622-9d08-4bab-b2a8-5d50c6012a81
WOS: 000319733000073
Scopus: 84878408233
http://hdl.handle.net/10023/4136
https://doi.org/10.1371/journal.pone.0064651
op_rights © 2013 Burdett et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
op_doi https://doi.org/10.1371/journal.pone.0064651
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