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dc.contributor.authorBurdett, Heidi L.
dc.contributor.authorDonohue, Penelope J. C.
dc.contributor.authorHatton, Angela D.
dc.contributor.authorAlwany, Magdy A.
dc.contributor.authorKamenos, Nicholas A.
dc.date.accessioned2013-11-01T12:01:05Z
dc.date.available2013-11-01T12:01:05Z
dc.date.issued2013-05-28
dc.identifier.citationBurdett , 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.0064651en
dc.identifier.issn1932-6203
dc.identifier.otherPURE: 75923686
dc.identifier.otherPURE UUID: 07d76622-9d08-4bab-b2a8-5d50c6012a81
dc.identifier.otherWOS: 000319733000073
dc.identifier.otherScopus: 84878408233
dc.identifier.urihttp://hdl.handle.net/10023/4136
dc.descriptionThis 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.en
dc.description.abstractOceanic 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 may be more important benthic producers of dissolved DMS/P than corals. An increase in DMS/P concentrations during periods of low carbonate saturation state may become ecologically important in the future under an OA regime, impacting larval settlement and increasing atmospheric emissions of DMS.
dc.language.isoeng
dc.relation.ispartofPLoS Oneen
dc.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.en
dc.subjectGreat Barrier Reefen
dc.subjectOcean acidificationen
dc.subjectMarine macroalgaeen
dc.subjectElevated CO2en
dc.subjectAlgaeen
dc.subjectDMSPen
dc.subjectSeawateren
dc.subjectCalcificationen
dc.subjectDimethylsufideen
dc.subjectImpactsen
dc.subjectQ Scienceen
dc.subject.lccQen
dc.titleSpatiotemporal Variability of Dimethylsulphoniopropionate on a Fringing Coral Reef : The Role of Reefal Carbonate Chemistry and Environmental Variabilityen
dc.typeJournal articleen
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews.Earth and Environmental Sciencesen
dc.identifier.doihttps://doi.org/10.1371/journal.pone.0064651
dc.description.statusPeer revieweden


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