Please use this identifier to cite or link to this item: https://hdl.handle.net/1959.11/15874
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dc.contributor.authorHurd, Catriona Len
dc.contributor.authorCornwall, Christopher Een
dc.contributor.authorCurrie, Kimen
dc.contributor.authorHepburn, Christopher Den
dc.contributor.authorMcGraw, Christinaen
dc.contributor.authorHunter, Keith Aen
dc.contributor.authorBoyd, Philip Wen
dc.date.accessioned2014-10-14T15:32:00Z-
dc.date.issued2011-
dc.identifier.citationGlobal Change Biology, 17(10), p. 3254-3262en
dc.identifier.issn1365-2486en
dc.identifier.issn1354-1013en
dc.identifier.urihttps://hdl.handle.net/1959.11/15874-
dc.description.abstractAnthropogenically mediated decreases in pH, termed ocean acidification (OA), may be a major threat to marine organisms and communities. Research has focussed mainly on tropical coral reefs, but temperate reefs play a no less important ecological role in colder waters, where OA effects may first be manifest. Herein, we report that trends in pH at the surface of three ecologically important cold-water calcifiers (a primary producer and herbivores), under a range of fluid flows, differ substantially from one another, and for two of the three calcifiers, the pH, during darkness, is lower than the mean projected pH due to OA for the surface waters of the global ocean beyond the year 2100. Using micro-electrodes, we show that each calcifier had a different pH gradient between its surface and mainstream seawater, i.e. within the diffusion boundary layer (DBL) that appears to act as an environmental buffer to mainstream pH. Abalone encountered only mainstream seawater pH, whereas pH at the sea urchins' surface was reduced by ~0.35 units. For coralline algae, pH was ~0.5 units higher in the light and ~0.35 units lower under darkness than in ambient mainstream seawater. This wide range of pH within the DBL of some calcifiers will probably affect their performance under projected future reductions in pH due to OA. Differing exposure to a range of surface pH may result in differential susceptibility of calcifiers to OA. Such fluctuations are no doubt regulated by the interplay of water movement, morphology and metabolic rates (e.g. respiration, calcification and/or photosynthesis). Our study, by considering physics (flow regime), chemistry (pH gradients vs. OA future projections) and biology (trophic level, physiology and morphology), reveals that predicting species-specific responses and subsequent ecosystem restructuring to OA is complex and requires a holistic, eco-mechanical, approach.en
dc.languageenen
dc.publisherWiley-Blackwell Publishing Ltden
dc.relation.ispartofGlobal Change Biologyen
dc.titleMetabolically induced pH fluctuations by some coastal calcifiers exceed projected 22nd century ocean acidification: a mechanism for differential susceptibility?en
dc.typeJournal Articleen
dc.identifier.doi10.1111/j.1365-2486.2011.02473.xen
dc.subject.keywordsMarine and Estuarine Ecology (incl Marine Ichthyology)en
dc.subject.keywordsEnvironmental Chemistry (incl Atmospheric Chemistry)en
local.contributor.firstnameCatriona Len
local.contributor.firstnameChristopher Een
local.contributor.firstnameKimen
local.contributor.firstnameChristopher Den
local.contributor.firstnameChristinaen
local.contributor.firstnameKeith Aen
local.contributor.firstnamePhilip Wen
local.subject.for2008060205 Marine and Estuarine Ecology (incl Marine Ichthyology)en
local.subject.for2008039901 Environmental Chemistry (incl Atmospheric Chemistry)en
local.subject.seo2008960305 Ecosystem Adaptation to Climate Changeen
local.subject.seo2008960308 Effects of Climate Change and Variability on New Zealand (excl. Social Impacts)en
local.profile.schoolSchool of Science and Technologyen
local.profile.emailcmcgraw@une.edu.auen
local.output.categoryC1en
local.record.placeauen
local.record.institutionUniversity of New Englanden
local.identifier.epublicationsrecordune-20141012-205732en
local.publisher.placeUnited Kingdomen
local.format.startpage3254en
local.format.endpage3262en
local.peerreviewedYesen
local.identifier.volume17en
local.identifier.issue10en
local.title.subtitlea mechanism for differential susceptibility?en
local.contributor.lastnameHurden
local.contributor.lastnameCornwallen
local.contributor.lastnameCurrieen
local.contributor.lastnameHepburnen
local.contributor.lastnameMcGrawen
local.contributor.lastnameHunteren
local.contributor.lastnameBoyden
dc.identifier.staffune-id:cmcgrawen
local.profile.roleauthoren
local.profile.roleauthoren
local.profile.roleauthoren
local.profile.roleauthoren
local.profile.roleauthoren
local.profile.roleauthoren
local.profile.roleauthoren
local.identifier.unepublicationidune:16111en
local.identifier.handlehttps://hdl.handle.net/1959.11/15874en
dc.identifier.academiclevelAcademicen
local.title.maintitleMetabolically induced pH fluctuations by some coastal calcifiers exceed projected 22nd century ocean acidificationen
local.output.categorydescriptionC1 Refereed Article in a Scholarly Journalen
local.search.authorHurd, Catriona Len
local.search.authorCornwall, Christopher Een
local.search.authorCurrie, Kimen
local.search.authorHepburn, Christopher Den
local.search.authorMcGraw, Christinaen
local.search.authorHunter, Keith Aen
local.search.authorBoyd, Philip Wen
local.uneassociationUnknownen
local.year.published2011en
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