Belle, Simon
- Department of Aquatic Sciences and Assessment, Swedish University of Agricultural Sciences
- Estonian University of Life Sciences
Research article2018Peer reviewed
Belle, Simon; Freiberg, Rene; Poska, Anneli; Agasild, Helen; Alliksaar, Tiiu; Tonno, Ilmar
The study of lake sediments and archived biological remains is a promising approach to better understand the impacts of climate change on aquatic ecosystems. Small lakes have been shown to be strongly sensitive to past climate change, but similar information is lacking for large lakes. By identifying responses to climate change of carbon flows through benthic food web in two different sized lakes, we aimed to understand how lake morphometry can mediate the effects of climate change. We reconstructed the dynamics of phytoplankton community composition and carbon resources sustaining chironomid biomass during the Holocene from the combined analysis of sedimentary pigment quantification and carbon stable isotopic composition of subfossil chironomid head capsules (delta C-13(Hc)) in a large lake in the Baltic area (Estonia). Our results showed that chironomid biomass in the large lake was mainly sustained by phytoplankton, with no significant relationship between delta C-13(Hc) values and temperature fluctuations. We suggest that lake morphometry (including distance of the sampling zone to the shoreline, and lake volume for primary producers) mediates the effects of climate change, making large lakes less sensitive to climate change. Complementary studies are needed to better understand differences in organic matter dynamics in different sized lakes and to characterize the response of the aquatic carbon cycle to past climate change. 2018 Elsevier Ltd. All rights reserved.
Climate change; Benthic food web; Large lake; Carbon stable isotope; Subfossil chironomid
Quaternary Science Reviews
2018, Volume: 187, pages: 168-176
Publisher: PERGAMON-ELSEVIER SCIENCE LTD
SDG13 Climate action
Oceanography, Hydrology, Water Resources
DOI: https://doi.org/10.1016/j.quascirev.2018.03.027
https://res.slu.se/id/publ/95107