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dc.contributorYang, Yan
dc.contributor.authorHolding, Johnna
dc.contributor.authorDuarte, Carlos M.
dc.contributor.authorSanz-Martín, Marina
dc.contributor.authorMesa, E
dc.contributor.authorArrieta, J M
dc.contributor.authorChierici, Melissa
dc.contributor.authorHendriks, Iris
dc.contributor.authorGarcía-Corral, L S
dc.contributor.authorRegaudie-de-Gioux, A
dc.contributor.authorDelgado, A
dc.contributor.authorReigstad, M
dc.contributor.authorWassmann, P
dc.contributor.authorAgusti, Susana
dc.coverage.spatialgeoLocationBox: 78.08 9.34 79.72 13.47
dc.date.accessioned2017-06-06T08:02:23Z
dc.date.available2017-06-06T08:02:23Z
dc.date.issued2016
dc.identifier.citationHolding, J., Duarte, C. M., Sanz-Martín, M., Mesa, E., Arrieta, J. M., Chierici, M., … Agustí, S. (2016). Temperature dependence of CO2-enhanced primary production in the European Arctic Ocean, supplement to: Holding, Johnna; Duarte, Carlos M; Sanz-Martín, Marina; Mesa, E; Arrieta, J M; Chierici, Melissa; Hendriks, Iris; García-Corral, L S; Regaudie-de-Gioux, A; Delgado, A; Reigstad, M; Wassmann, P; Agustí, Susana (2015): Temperature dependence of CO2-enhanced primary production in the European Arctic Ocean. Nature Climate Change, 5(12), 1079-1082 [Data set]. PANGAEA - Data Publisher for Earth & Environmental Science. https://doi.org/10.1594/pangaea.860530
dc.identifier.doi10.1594/PANGAEA.860530
dc.identifier.urihttp://hdl.handle.net/10754/624160
dc.description.abstractThe Arctic Ocean is warming at two to three times the global rate and is perceived to be a bellwether for ocean acidification. Increased CO2 concentrations are expected to have a fertilization effect on marine autotrophs, and higher temperatures should lead to increased rates of planktonic primary production. Yet, simultaneous assessment of warming and increased CO2 on primary production in the Arctic has not been conducted. Here we test the expectation that CO2-enhanced gross primary production (GPP) may be temperature dependent, using data from several oceanographic cruises and experiments from both spring and summer in the European sector of the Arctic Ocean. Results confirm that CO2 enhances GPP (by a factor of up to ten) over a range of 145-2,099?µatm; however, the greatest effects are observed only at lower temperatures and are constrained by nutrient and light availability to the spring period. The temperature dependence of CO2-enhanced primary production has significant implications for metabolic balance in a warmer, CO2-enriched Arctic Ocean in the future. In particular, it indicates that a twofold increase in primary production during the spring is likely in the Arctic.
dc.formattext/tab-separated-values
dc.format.extent700 data points
dc.language.isoeng
dc.publisherPANGAEA - Data Publisher for Earth & Environmental Science
dc.rightsCreative Commons Attribution 3.0 Unported (CC-BY)
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/
dc.titleTemperature dependence of CO2-enhanced primary production in the European Arctic Ocean, supplement to: Holding, Johnna; Duarte, Carlos M; Sanz-Martín, Marina; Mesa, E; Arrieta, J M; Chierici, Melissa; Hendriks, Iris; García-Corral, L S; Regaudie-de-Gioux, A; Delgado, A; Reigstad, M; Wassmann, P; Agustí, Susana (2015): Temperature dependence of CO2-enhanced primary production in the European Arctic Ocean. Nature Climate Change, 5(12), 1079-1082
dc.typeDataset
dc.contributor.departmentBiological and Environmental Sciences and Engineering (BESE) Division
dc.contributor.departmentMarine Science Program
dc.contributor.departmentRed Sea Research Center (RSRC)
kaust.personDuarte, Carlos M.
kaust.personAgusti, Susana
dc.type.resourceSupplementary Dataset
dc.relation.isdocumentedbyURL:https://cran.r-project.org/package=seacarb
dc.relation.issupplementtoDOI:10.1038/NCLIMATE2768
dc.date.collected2010-06-23
dc.date.collected2014-05-23
display.relations<b> Is Supplement To:</b> <br/> <ul><li><i>[Article]</i> <br/> Temperature dependence of CO2-enhanced primary production in the European Arctic Ocean 2015, 5 (12):1079 Nature Climate Change. DOI: <a href="https://doi.org/10.1038/NCLIMATE2768">10.1038/NCLIMATE2768</a> HANDLE: <a href="http://hdl.handle.net/10754/596052">10754/596052</a></li></ul>


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Creative Commons Attribution 3.0 Unported (CC-BY)
Except where otherwise noted, this item's license is described as Creative Commons Attribution 3.0 Unported (CC-BY)