This report aimed to investigate how chlorophyll-concentrations (Chl-a) in the water column and varved sediments were affected by changes in air temperature and precipitation and consequently how climate change will affect the sedimentation and productivity in boreal aquatic ecosystems. VRS (visible-reflectance-spectroscopy) was used to asses Chl-a and its derivates in sediment trap samples between 2002-2021 and in a series of freeze cores (1979-2021) from lake Nylandssjön, with annually laminated sediments. In order to evaluate how weather and climate change affected the sedimentation and productivity in the lake the results were compared with meteorological data from SMHI (Swedish Meteorological and Hydrological Institute) and Chl-a data from seperate depths in the water column. The results indicate that the majority of the yearly sedimentation occur either in May or June, where a higher cumulative amount of precipitation in May lead to a higher sedimentation rate in May (r=0,49; p=0,03). The amount of precipitation in spring also had a significant impact on the primary production in spring and summer (r=0,59; p=0,01; r=0,73; p=0,002). Water column Chl-a and spectrally inferred Chl-a in sediments show similar trends in concentrations with deeper water sampling, however, water column Chl-a displayed significant differences in values between various depths (p=0,0004). Consequently, climate change will much likely increase the productivity of boreal aquatic ecosystems within years and the amount of sedimentation that occurs between years due to higher temperatures. An increased amount of precipitation will also enhance the primary productivity and the transportation of allochthonous- and minerogenic material to the lake.

L’apport de sédiments fins au cours d’eau est un phénomène naturel mais qui sous les effets de l’anthropisation peut devenir excessif et conduire à perturber le fonctionnement de l’hydrosystème. Cet apport excessif provoque le colmatage du lit des rivières et peut perturber les échanges hydriques, les processus biogéochimiques et les communautés d’invertébrés benthiques et hyporhéiques. D’un point de vue méthodologique, la mesure de la conductivité hydraulique dans le substrat permet d’obtenir une image du niveau de colmatage de la zone hyporhéique et le pompage Bou Rouch permet d’étudier qualitativement la faune hyporhéique. D’un point de vue biologique, les effets du colmatage sont un peu plus importants pour l’hyporhéos que pour le benthos notamment au niveau de la richesse taxonomique, des assemblages faunistiques et des traits biologiques / Fine sediment input to the streambeds is a natural phenomenon but in addition to the effects of human impacts may become excessive and lead to disruption of the functioning of the hydrosystem. This excessive intake causes the clogging of river beds and can disrupt water exchange, biogeochemical processes and benthic and hyporheic invertebrate communities. From a methodological point of view, measurement of hydraulic conductivity in the substratum provides a realistic picture of the clogging level of the hyporheic zone and the Bou Rouch pump a good sampling for a qualitative study of the hyporheic fauna. From a biological point of view, the clogging effects on the hyporheos are higher compared to the benthos regarding taxonomic richness, changes in faunal assemblages and biological traits