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dc.contributor.authorPacheco, J. P.
dc.contributor.authorAznarez, C.
dc.contributor.authorLevi, E. E.
dc.contributor.authorBaattrup-Pedersen, A.
dc.contributor.authorJeppesen, E.
dc.date.accessioned2023-08-31T07:59:04Z
dc.date.available2023-08-31T07:59:04Z
dc.date.issued2022-10-01
dc.identifier.citationHydrobiologia: 849 (17-18): 3889-3904 (2022)es_ES
dc.identifier.urihttp://hdl.handle.net/10810/62320
dc.description.abstractPeriphyton is a key primary producer in shallow lakes, sensitive to global warming and changes in nutrient balances. Reduced nitrogen availability due to accelerated denitrification at higher temperatures or in response to reduced N loadings aimed to reduce the eutrophication may affect periphyton biomass and composition, to compensate for the low N availability (e.g. promoting N2-fixing). We analysed periphyton responses to N decline in 12 eutrophic shallow lake mesocosms during one year of low N compared to high N, under three temperature scenarios: ambient, A2 IPCC scenario and A2 increased by 50%. We used two submerged macrophytes (Potamogeton crispus and Elodea canadensis) and artificial imitations of these as substrates for periphyton growth. Nitrogen decline increased periphyton biomass and induced compositional changes irrespective of season, plant type, and temperature. Periphyton biomass was negatively associated to phytoplankton and positively to plant complexity. Warmer scenarios negatively affected periphyton exclusively at high N loadings. Low N conditions were associated with lower periphyton taxonomic richness, lower N2-fixing cyanobacteria biovolume and increased biovolume of large-sized chlorophytes and non-N2-fixing cyanobacteria. Our results suggest that low N conditions promoted periphyton due to a more efficient use of nutrients and improved light conditions resulting from lower phytoplankton biomass and contrasting effects of temperature. © 2021, The Author(s), under exclusive licence to Springer Nature Switzerland AG.es_ES
dc.description.sponsorshipThis study was supported by the Sino-Danish Centre – Aarhus University, the University of the Chinese Academy of Sciences and the University of the Republic, Uruguay. E.J. was also supported by the TÜBITAK, BIDEB 2232 program (118C250). C.A. was supported by the Doctoral INPhINIT–INCOMING program, fellowship code (LCF/BQ/DI20/11780004), from “la Caixa” Foundation (ID 100010434). We thank Beibei Hao for her valuable assistance with the experimental design and Ann Lene Vigh and Kathrine Tabermann Uhrenholt for the field and lab assistance.es_ES
dc.language.isoenges_ES
dc.publisherHydrobiologiaes_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-sa/3.0/es/*
dc.subjectBenthic algaees_ES
dc.subjectDiazotrophic cyanobacteriaes_ES
dc.subjectOligotrophicationes_ES
dc.subjectPhytoplanktones_ES
dc.subjectPlant morphologyes_ES
dc.titlePeriphyton responses to nitrogen decline and warming in eutrophic shallow lake mesocosmses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.holder© The Authors.es_ES
dc.rights.holderAtribución-NoComercial-CompartirIgual 3.0 España*
dc.relation.publisherversionhttps://dx.doi.org/10.1007/s10750-021-04755-yes_ES
dc.identifier.doi10.1007/s10750-021-04755-y
dc.contributor.funderSino-Danish Centre – Aarhus University
dc.contributor.funderla Caixa” Foundation
dc.contributor.funderTÜBITAK
dc.contributor.funderUniversity of the Republic
dc.contributor.funderUniversity of the Chinese Academy of Sciences


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