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dc.contributor.authorTittensor, DP
dc.contributor.authorBaco, AR
dc.contributor.authorBrewin, PE
dc.contributor.authorClark, MR
dc.contributor.authorConsalvey, M
dc.contributor.authorHall‐Spencer, J
dc.contributor.authorRowden, AA
dc.contributor.authorSchlacher, T
dc.contributor.authorStocks, KI
dc.contributor.authorRogers, AD
dc.date.accessioned2013-02-22T20:40:33Z
dc.date.available2013-02-22T20:40:33Z
dc.date.issued2009-06
dc.identifier.issn0305-0270
dc.identifier.issn1365-2699
dc.identifier.urihttp://hdl.handle.net/10026.1/1415
dc.description.abstract

<jats:title>Abstract</jats:title><jats:p><jats:bold>Aim </jats:bold> Globally, species distribution patterns in the deep sea are poorly resolved, with spatial coverage being sparse for most taxa and true absence data missing. Increasing human impacts on deep‐sea ecosystems mean that reaching a better understanding of such patterns is becoming more urgent. Cold‐water stony corals (Order Scleractinia) form structurally complex habitats (dense thickets or reefs) that can support a diversity of other associated fauna. Despite their widely accepted ecological importance, records of scleractinian corals on seamounts are patchy and simply not available for most of the global ocean. The objective of this paper is to model the global distribution of suitable habitat for stony corals on seamounts.</jats:p><jats:p><jats:bold>Location </jats:bold> Seamounts worldwide.</jats:p><jats:p><jats:bold>Methods </jats:bold> We compiled a database containing all accessible records of scleractinian corals on seamounts. Two modelling approaches developed for presence‐only data were used to predict global habitat suitability for seamount scleractinians: maximum entropy modelling (Maxent) and environmental niche factor analysis (ENFA). We generated habitat‐suitability maps and used a cross‐validation process with a threshold‐independent metric to evaluate the performance of the models.</jats:p><jats:p><jats:bold>Results </jats:bold> Both models performed well in cross‐validation, although the Maxent method consistently outperformed ENFA. Highly suitable habitat for seamount stony corals was predicted to occur at most modelled depths in the North Atlantic, and in a circumglobal strip in the Southern Hemisphere between 20° and 50° S and shallower than around 1500 m. Seamount summits in most other regions appeared much less likely to provide suitable habitat, except for small near‐surface patches. The patterns of habitat suitability largely reflect current biogeographical knowledge. Environmental variables positively associated with high predicted habitat suitability included the aragonite saturation state, and oxygen saturation and concentration. By contrast, low levels of dissolved inorganic carbon, nitrate, phosphate and silicate were associated with high predicted suitability. High correlation among variables made assessing individual drivers difficult.</jats:p><jats:p><jats:bold>Main conclusions </jats:bold> Our models predict environmental conditions likely to play a role in determining large‐scale scleractinian coral distributions on seamounts, and provide a baseline scenario on a global scale. These results present a first‐order hypothesis that can be tested by further sampling. Given the high vulnerability of cold‐water corals to human impacts, such predictions are crucial tools in developing worldwide conservation and management strategies for seamount ecosystems.</jats:p>

dc.format.extent1111-1128
dc.format.mediumUndetermined
dc.languageen
dc.language.isoen
dc.publisherWiley
dc.subjectConservation biogeography
dc.subjectdistribution
dc.subjectENFA
dc.subjecthabitat suitability
dc.subjectmaximum entropy
dc.subjectmodelling
dc.subjectniche
dc.subjectScleractinia
dc.subjectseamount
dc.subjectstony coral
dc.titlePredicting global habitat suitability for stony corals on seamounts
dc.typejournal-article
dc.typeJournal Article
plymouth.author-urlhttps://www.webofscience.com/api/gateway?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000266242800011&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=11bb513d99f797142bcfeffcc58ea008
plymouth.issue6
plymouth.volume36
plymouth.publication-statusPublished
plymouth.journalJournal of Biogeography
dc.identifier.doi10.1111/j.1365-2699.2008.02062.x
plymouth.organisational-group/Plymouth
plymouth.organisational-group/Plymouth/Faculty of Science and Engineering
plymouth.organisational-group/Plymouth/Faculty of Science and Engineering/School of Biological and Marine Sciences
plymouth.organisational-group/Plymouth/PRIMaRE Publications
plymouth.organisational-group/Plymouth/REF 2021 Researchers by UoA
plymouth.organisational-group/Plymouth/REF 2021 Researchers by UoA/UoA07 Earth Systems and Environmental Sciences
plymouth.organisational-group/Plymouth/Research Groups
plymouth.organisational-group/Plymouth/Research Groups/Marine Institute
plymouth.organisational-group/Plymouth/Users by role
plymouth.organisational-group/Plymouth/Users by role/Academics
dc.identifier.eissn1365-2699
dc.rights.embargoperiodNot known
rioxxterms.versionofrecord10.1111/j.1365-2699.2008.02062.x
rioxxterms.licenseref.urihttp://www.rioxx.net/licenses/all-rights-reserved
rioxxterms.typeJournal Article/Review


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