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Meromictic stratification and geochemical gradients in a flooded abandoned apatite and mica mine (Quebec, Canada)
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DOI：10.1016/j.apgeochem.2026.106962.png)
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Abstract
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• Stable meromictic stratification with distinct oxic and anoxic layers. • Microbial sulfate reduction occurs in the chemocline and monimolimnion. • Accumulation of solutes in the monimolimnion, including phosphorus and nitrogen. • Lake morphometry likely responsible for meromixis. • Potential model site for flooded apatite and mica pit lakes in Canada.
Keywords:
Flooded mine
Open-pit lake
Meromictic lake
Lake stratification
Stable isotopes
Geochemistry
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