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dc.contributor.authorTaranu, Zofia E.-
dc.contributor.authorGregory- Eaves, Irene-
dc.contributor.authorLeavitt, P. R.-
dc.contributor.authorBunting, L.-
dc.contributor.authorBuchaca, Teresa-
dc.contributor.authorCatalán, Jordi-
dc.contributor.authorDomaizon, Isabelle-
dc.contributor.authorGuilizzoni, Piero-
dc.contributor.authorLami, A.-
dc.contributor.authorMcGowan, S.-
dc.contributor.authorMoorhouse, Heather-
dc.contributor.authorMorabito, G.-
dc.contributor.authorPick, Frances R.-
dc.contributor.authorStevenson, Mark A.-
dc.contributor.authorThompson, Patrick L.-
dc.contributor.authorVinebrooke, Rolf D.-
dc.date.accessioned2015-03-18T08:50:06Z-
dc.date.available2015-03-18T08:50:06Z-
dc.date.issued2015-
dc.identifier.citationEcology Letters : doi: 10.1111/ele.12420 (2015)es_ES
dc.identifier.issn1461-023X-
dc.identifier.urihttp://hdl.handle.net/10261/112561-
dc.description10 páginas, 4 figuras.es_ES
dc.description.abstractIncreases in atmospheric temperature and nutrients from land are thought to be promoting the expansion of harmful cyanobacteria in lakes worldwide, yet to date there has been no quantitative synthesis of long-term trends. To test whether cyanobacteria have increased in abundance over the past ~ 200 years and evaluate the relative influence of potential causal mechanisms, we synthesised 108 highly resolved sedimentary time series and 18 decadal-scale monitoring records from north temperate-subarctic lakes. We demonstrate that: (1) cyanobacteria have increased significantly since c. 1800 CE, (2) they have increased disproportionately relative to other phytoplankton, and (3) cyanobacteria increased more rapidly post c. 1945 CE. Variation among lakes in the rates of increase was explained best by nutrient concentration (phosphorus and nitrogen), and temperature was of secondary importance. Although cyanobacterial biomass has declined in some managed lakes with reduced nutrient influx, the larger spatio-temporal scale of sedimentary records show continued increases in cyanobacteria throughout the north temperate-subarctic regions.es_ES
dc.description.sponsorshipThis project was funded by the Natural Sciences and Engineering Research Council of Canada (I.G.-E., P.R.L., F.P., R.D.V.), Fonds Qu eb ecois de Recherche sur la Nature et les Technologies (Z.E.T.), Canadian Foundation for Innovation (I.G.-E., P.R.L.), Canada Research Chair (P.R.L.), Fundaci o Bosch i Gimpera, Universitat de Barcelona (T.B.), EU project BIOMASS (T.B., J.C.), Catalan government (GECA, 2014SGR1249) (T.B., J.C.), Spanish government (NitroPir, CGL2010-19373) (J.C.), Nexdata Project (P.G., A.L., G.M.), EU INTERREG IIIA (S.M., M.A.S.), Cheshire Wildlife Trust and Natural England (S.M.), UK Environment Agency and Freshwater Biological Association (S.M.), Engineering and Physical Sciences Research Council and Environment Agency (H.M.), International Commission for the Protection of Italian Swiss Waters (P.G., A.L., G.M.), ‘IperRetro’ ANR VULNS- 005 (I.D.), SOERE OLA IS (I.D.) data collection by INRA, CIPEL, CISALB and SILA (I.D.), EDYTEM for the sediment core LDB09_P2-02 code IGSN : EDYLDB005 (I.D.), and the Alberta Ingenuity Water Research grant (P.L.T., R.D.V.).es_ES
dc.language.isoenges_ES
dc.publisherJohn Wiley & Sonses_ES
dc.rightsclosedAccesses_ES
dc.subjectPaleolimnologyes_ES
dc.subjectRegression treees_ES
dc.subjectAnthropocenees_ES
dc.subjectClimate changees_ES
dc.subjectCyanobacteriaes_ES
dc.subjectEutrophicationes_ES
dc.subjectLong-term trendses_ES
dc.subjectMeta-analysises_ES
dc.titleAcceleration of cyanobacterial dominance in north temperatesubarctic lakes during the Anthropocenees_ES
dc.typeArtículoes_ES
dc.identifier.doi10.1111/ele.12420-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttp://dx.doi.org/10.1111/ele.12420es_ES
dc.identifier.e-issn1461-0248-
dc.relation.csices_ES
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