Published March 2021 | Version v1
Journal article

Ecosystem maturity modulates greenhouse gases fluxes from artificial lakes

  • 1. Univ Lyon, Université Claude Bernard Lyon 1, CNRS, ENTPE, UMR 5023 LEHNA, F-69622 Villeurbanne (France)
  • 2. OFB, Direction de la Recherche et de l'Appui Scientifique, Aix-en-Provence (France)
  • 3. Pôle R&D "ECLA", Aix-en-Provence (France)
  • 4. Aix Marseille Univ., Universite de Toulon, CNRS, IRD, MIO UM 110, 13288 Marseille (France)
  • 5. Institute of Ecology and Biodiversity (IEB), Faculty of Sciences, Universidad de Chile, Santiago (Chile)
  • 6. Inrae, Aix Marseille Univ, RECOVER, Aix-en-Provence (France)
  • 7. UPS, CNRS, IRD, Université de Toulouse, UMR 5174, Laboratoire Évolution et Diversité Biologique (EDB), Université de Toulouse, 118 route de Narbonne, 31062 Toulouse (France)

Description

Highlights: • C cycling variability and its variability in artificial lakes have been overlooked. • We quantified gas fluxes in 11 gravel pit lakes across a gradient of ecosystem maturity. • Lakes ranged from heterotrophic to autotrophic as maturity increased. • Eutrophication turns lakes as CO2-sinks. • CH4 emissions and associated climate impacts increased with ecosystem maturity. Lentic ecosystems play a major role in the global carbon cycling but the understanding of the environmental determinants of lake metabolism is still limited, notably in small artificial lakes. Here the effects of environmental conditions on lake metabolism and CO2 and CH4 emissions were quantified in 11 small artificial gravel pit lakes covering a gradient of ecosystem maturity, ranging from young oligotrophic to older, hypereutrophic lakes. The diffusive fluxes of CO2 and CH4 ranged from −30.10 to 37.78 mmol m−2 d−1 and from 3.05 to 25.45 mmol m−2 d−1 across gravel pit lakes, respectively. Nutrients and chlorophyll a concentrations were negatively correlated with CO2 concentrations and emissions but positively correlated with CH4 concentrations and emissions from lakes. These findings indicate that, as they mature, gravel pit lakes switch from heterotrophic to autotrophic-based metabolism and hence turn into CO2-sinks. In contrast, the emission of CH4 increased along the maturity gradient. As a result, eutrophication occurring during ecosystem maturity increased net emissions in terms of climate impact (CO2 equivalent) due to the higher contribution of CH4 emissions. Overall, mean CO2equivalent emission was 7.9 g m−2 d−1, a value 3.7 and 4.7 times higher than values previously reported in temperate lakes and reservoirs, respectively. While previous studies reported that lakes represent emitters of C to the atmosphere, this study highlights that eutrophication may reverse lake contribution to global C budgets. However, this finding is to be balanced with the fact that eutrophication also increased CH4 emissions and hence, enhanced the potential impact of these ecosystems on climate. Implementing mitigation strategies for maintaining intermediate levels of maturity is therefore needed to limit the impacts of small artificial waterbodies on climate. This could be facilitated by their small size and should be planned at the earliest stages of artificial lake construction.

Availability note (English)

Available from http://dx.doi.org/10.1016/j.scitotenv.2020.144046

Additional details

Identifiers

DOI
10.1016/j.scitotenv.2020.144046;
PII
S004896972037577X;

Publishing Information

Journal Title
Science of the Total Environment
Journal Volume
760
Journal Page Range
vp.
ISSN
0048-9697
CODEN
STENDL

Optional Information

Copyright
Copyright (c) 2020 Elsevier B.V. All rights reserved.