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dc.contributor.authorSantiago, Alvarez-Fernandez
dc.contributor.authorLennart T., Bach
dc.contributor.authorJan, Taucher
dc.contributor.authorUlf, Riebesell
dc.contributor.authorUlrich, Sommer
dc.contributor.authorAberle-Malzahn, Nicole
dc.contributor.authorCorinne P.D., Brussaard
dc.contributor.authorMaarten, Boersma
dc.date.accessioned2019-07-09T10:29:21Z
dc.date.available2019-07-09T10:29:21Z
dc.date.created2018-04-20T10:56:28Z
dc.date.issued2018
dc.identifier.citationProgress in Oceanography. 2018, 165 11-18.nb_NO
dc.identifier.issn0079-6611
dc.identifier.urihttp://hdl.handle.net/11250/2603888
dc.description.abstractIn situ mesocosm experiments on the effect of ocean acidification (OA) are an important tool for investigating potential OA-induced changes in natural plankton communities. In this study we combined results from various in-situ mesocosm studies in two different ocean regions (Arctic and temperate waters) to reveal general patterns of plankton community shifts in response to OA and how these changes are modulated by inorganic nutrient availability. Overall, simulated OA caused an increase in phytoplankton standing stock, which was more pronounced in smaller-sized taxa. This effect on primary producers was channelled differently into heterotroph primary consumers depending on the inorganic nutrient availability. Under limiting conditions, bacteria and micro-heterotrophs benefited with inconsistent responses of larger heterotrophs. During nutrient replete periods, heterotrophs were in general negatively affected, although there was an increase of some mesozooplankton developmental stages (i.e. copepodites). We hypothesize that changes in phytoplankton size distribution and community composition could be responsible for these food web responses.nb_NO
dc.language.isoengnb_NO
dc.publisherElseviernb_NO
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/deed.no*
dc.titlePlankton responses to ocean acidification: The role of nutrient limitationnb_NO
dc.typeJournal articlenb_NO
dc.typePeer reviewednb_NO
dc.description.versionacceptedVersionnb_NO
dc.source.pagenumber11-18nb_NO
dc.source.volume165nb_NO
dc.source.journalProgress in Oceanographynb_NO
dc.identifier.doi10.1016/j.pocean.2018.04.006
dc.identifier.cristin1580587
dc.description.localcode© 2018. This is the authors’ accepted and refereed manuscript to the article. Locked until 7.5.2020 due to copyright restrictions. This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/nb_NO
cristin.unitcode194,66,10,0
cristin.unitnameInstitutt for biologi
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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Attribution-NonCommercial-NoDerivatives 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivatives 4.0 Internasjonal