Abstract
We investigated oxygen and carbon isotopes
of bulk carbonate and of benthic freshwater
ostracods (Candona candida) in a sediment core of
Lago Piccolo di Avigliana that was previously analyzed
for pollen and loss-on-ignition, in order to
reconstruct environmental changes during the late
glacial and early Holocene. The depth–age relationship
of the sediment core was established using 14
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