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dc.rights.licenseopenen_US
dc.contributor.authorRODRIGUEZ LOPEZ, Lien
dc.contributor.authorLAMI, Andrea
dc.contributor.authorEL OUAHABI, Meriam
dc.contributor.authorFAGEL, Nathalie
dc.contributor.authorALVAREZ, Denisse
dc.contributor.authorGONZALEZ-RODRIGUEZ, Lisdelys
dc.contributor.authorSCHMIDT, Sabine
IDREF: 131836129
dc.contributor.authorURRUTIA, Roberto
dc.date.accessioned2022-11-23T08:25:50Z
dc.date.available2022-11-23T08:25:50Z
dc.date.issued2022-03-01
dc.identifier.issn2213-3054en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/170348
dc.description.abstractEnInteractions among climate change, ozone depletion, and ultraviolet radiation affect aquatic ecosystems. Meteorological and biological monitoring is often too brief, however, to record the magnitudes of past changes in ultraviolet fluxes and their effects. This study presents an analysis of fossil pigments and environmental conditions in the oligotrophic Laja Lake in the Chilean Andes over a 60-year period. The age of the sediment core was determined using high-efficiency gamma spectrometry and dated with lead-210 (210Pb). Analysis of the total and specific fossil pigments from a sediment core utilized a combination of analytical methods, spectrophotometry, and high-performance liquid chromatography. Environmental variables, such as stratospheric ozone concentration, temperature, precipitation, and ultraviolet radiation explained changes in the fossil pigment scytonemin. Results showed that low cloud cover over the high mountain lake predominated, with high ultraviolet radiation and temperature values during summer months. The most abundant group was Bacillariophyceae (diatoms). The highest concentrations of the pigments (canthaxanthin echinenone, myxoxanthophyll, aphanizophyll zeaxanthin and scytonemin) that represent the cyanobacteria groups were found in the upper part of the core (cm 0–15). The trend analysis further suggested that the influence of environmental features enabled generation of ultraviolet radiation-shielding pigment in the algae communities in the high mountain lake.This study advances understanding of the interactive effects of climate change, ozone depletion, and ultraviolet radiation on aquatic ecosystems. Fossil pigments proved to be good indicators of lake-ecosystem response to climate/environmental changes, which are necessary for predicting possible effects of future climate change.
dc.language.isoENen_US
dc.subject.enEnvironmental changes
dc.subject.enPhotosynthetic pigments
dc.subject.enSediments
dc.subject.enUltraviolet radiation
dc.title.enFossil pigments and environmental conditions in the oligotrophic Laja Lake in the Chilean Andes
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.ancene.2022.100321en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalAnthropoceneen_US
bordeaux.volume37en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
hal.identifierhal-03866993
hal.version1
hal.date.transferred2022-11-23T08:25:53Z
hal.exporttrue
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Anthropocene&rft.date=2022-03-01&rft.volume=37&rft.eissn=2213-3054&rft.issn=2213-3054&rft.au=RODRIGUEZ%20LOPEZ,%20Lien&LAMI,%20Andrea&EL%20OUAHABI,%20Meriam&FAGEL,%20Nathalie&ALVAREZ,%20Denisse&rft.genre=article


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