Eutrophication and Geochemistry Drive Pelagic Calcite Precipitation in Lakes

Autor: Margot Sepp, Biel Obrador, Hares Khan, Rafael Marcé, Alo Laas
Přispěvatelé: Centre for Limnology
Rok vydání: 2021
Předmět:
0106 biological sciences
Ecologia dels llacs
lcsh:Hydraulic engineering
010504 meteorology & atmospheric sciences
Geography
Planning and Development

alkalinity
Context (language use)
Aquatic Science
01 natural sciences
Biochemistry
chemistry.chemical_compound
lcsh:Water supply for domestic and industrial purposes
calcite precipitation
lcsh:TC1-978
Dissolved organic carbon
medicine
Ecosystem
lake carbon budge
calcite saturation
0105 earth and related environmental sciences
Water Science and Technology
geochemistry
Calcite
lcsh:TD201-500
010604 marine biology & hydrobiology
Pelagic zone
Eutrophication
medicine.disease
6. Clean water
Oceanography
Geochemistry
eutrophication
chemistry
Eutrofització
13. Climate action
lake carbon budget
articles
Environmental science
Geoquímica
Saturation (chemistry)
Lake ecology
metabolism
Calcification
primary production
Zdroj: Water
Volume 13
Issue 5
Dipòsit Digital de la UB
Universidad de Barcelona
Water, Vol 13, Iss 597, p 597 (2021)
ISSN: 2073-4441
DOI: 10.3390/w13050597
Popis: Pelagic calcification shapes the carbon budget of lakes and the sensitivity of dissolved inorganic carbon (DIC) responses to lake metabolism. This process, being tightly linked to primary production, needs to be understood within the context of summer eutrophication which is increasing due to human stressors and global change. Most lake carbon budget models do not account for calcification because the conditions necessary for its occurrence are not well constrained. This study aims at identifying ratios between calcification and primary production and the drivers that control these ratios in freshwater. Using in situ incubations in several European freshwater lakes, we identify a strong relationship between calcite saturation and the ratio between calcification and net ecosystem production (NEP) (p-value <
0.001, R2 = 0.95). NEP-induced calcification is a short-term process that is potentiated by the increase in calcite saturation occurring at longer time scales, usually reaching the highest levels in summer. The resulting summer calcification event has effects on the DIC equilibria, causing deviations from the metabolic 1:1 stoichiometry between DIC and dissolved oxygen (DO). The strong dependency of the ratio between NEP and calcification on calcite saturation can be used to develop a suitable parameterization to account for calcification in lake carbon budgets.
Databáze: OpenAIRE