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Both climate trends and short-term fluctuations affected algae–zooplankton interactions in a boreal lake during the late Holocene

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dc.contributor.authorBelle, Simon
dc.contributor.authorTõnno, Ilmar
dc.contributor.authorVrede, Tobias
dc.contributor.authorFreiberg, Rene
dc.contributor.authorNilsson, Jenny L.
dc.contributor.authorGoedkoop, Willem
dc.date.accessioned2023-03-31T06:57:04Z
dc.date.available2023-03-31T06:57:04Z
dc.date.issued2021
dc.description.abstract1. Most studies aiming to explore the response of algae and zooplankton trophic interactions to climate variability have only been focused on unidirectional and very shortterm trends in temperature changes. As a result, the non-stationary aspect of climate change (warming and cooling periods, frequencies) remains completely unstudied. 2. We studied elemental and stable isotope composition of sedimentary organic matter, photosynthetic pigments, and carbon stable isotope composition of Cladocera resting eggs in a sediment record covering the last c. 2,600 years. We examined how past climate change acting at different timescales affected algal biomass and community composition, and carbon assimilation by zooplankton in a boreal lake. 3. Our study revealed major effects of both long-term climate trends and shorter term fluctuations on algae–zooplankton interactions in a boreal lake. We found the main climate trends, in particular the Little Ice Age, induced algal biomass and community composition changes and drastic changes in carbon assimilation by zooplankton. Interestingly, we found that temperature fluctuations could also contribute to regulating algae–zooplankton interactions. Specifically, we observed drastic changes in sedimentary markers and stable isotope composition of zooplankton remains during the most recent period, suggesting a strong influence of ongoing anthropogenic change on algae–zooplankton interactions. 4. Our study confirms previous findings showing close long-term linkage between the temporal dynamics of zooplankton diet and planktonic algae, and that both climate trends and short-term fluctuations are key in regulating consumer– resource trophic interactions. 5. Novel approaches that combine high temporal resolution paleolimnological reconstructions and contemporary monitoring studies are needed to better understand climate change effects on algae–zooplankton interactions and lake food webs.eng
dc.description.abstractEesti Teadusagentuur, Grant/Award Number: PRG709 and PRG1167; Svenska Forskningsrådet Formas, Grant/Award Number: 2016-861; Oscar and Lilli Lamm Foundation.eng
dc.description.sponsorshipEesti Teadusagentuur, Grant/Award Number: PRG709 and PRG1167; Svenska Forskningsrådet Formas, Grant/Award Number: 2016-861; Oscar and Lilli Lamm Foundation.eng
dc.identifier.issn0046-5070
dc.identifier.publicationFreshwater Biology. 2021;66:2076–2085.eng
dc.identifier.urihttp://hdl.handle.net/10492/8016
dc.identifier.urihttps://doi.org/10.1111/fwb.13815
dc.publisherWiley
dc.rightsCreative Commons Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0) ; openAccesseng
dc.rights© 2021 The Authors.eng
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/
dc.subjectalgal pigmentseng
dc.subjectaquatic food webseng
dc.subjectcarbon stable isotopeeng
dc.subjectpaleolimnologyeng
dc.subjectsubfossil cladoceraeng
dc.subjectarticleseng
dc.titleBoth climate trends and short-term fluctuations affected algae–zooplankton interactions in a boreal lake during the late Holoceneeng
dc.typeArticleeng

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