Daniel Gerdeaux1, Elise Dufour. 1. INRA, Station d'hydrobiologie lacustre, 75 Avenue de Corzent, BP 511, 74203, Thonon-les-Bains, France. gerdeaux@thonon.inra.fr
Abstract
RATIONALE: Sequential analysis of otolith oxygen isotope (δ(18) O(oto) ) values was performed by classical mechanical microdrilling and dual inlet mass spectrometry to infer the timing of growth checks in pike (Esox lucius) scales from Lake Annecy (France). It indicated that the first check on scales occurs before the first winter of life of the fish. METHODS: Eleven fish caught in February and June 2008 were studied. Intra-individual isotopic profiles exhibit cyclic variations that are consistent with that of modeled δ(18) O(oto) values using variations in epilimnion temperature and otolith-specific isotope fractionation equations. The positions of growth checks on scales were compared with the periodic variations of δ(18) O(oto) values on otolith radii using an allometric relationship. RESULTS: All individuals presented at least one check deposited before the first winter. Deposition of some checks might be linked to a shift in fish diet or habitat or to catch-and-release induced stress. CONCLUSIONS: Although coupling between sequential analysis of δ(18) O(oto) values and observation of scale growth features has been shown to be useful, there are limitations in the methodology, especially for the growth-attenuated region of otoliths associated with older ages.
RATIONALE: Sequential analysis of otolith oxygen isotope (δ(18) O(oto) ) values was performed by classical mechanical microdrilling and dual inlet mass spectrometry to infer the timing of growth checks in pike (Esox lucius) scales from Lake Annecy (France). It indicated that the first check on scales occurs before the first winter of life of the fish. METHODS: Eleven fish caught in February and June 2008 were studied. Intra-individual isotopic profiles exhibit cyclic variations that are consistent with that of modeled δ(18) O(oto) values using variations in epilimnion temperature and otolith-specific isotope fractionation equations. The positions of growth checks on scales were compared with the periodic variations of δ(18) O(oto) values on otolith radii using an allometric relationship. RESULTS: All individuals presented at least one check deposited before the first winter. Deposition of some checks might be linked to a shift in fish diet or habitat or to catch-and-release induced stress. CONCLUSIONS: Although coupling between sequential analysis of δ(18) O(oto) values and observation of scale growth features has been shown to be useful, there are limitations in the methodology, especially for the growth-attenuated region of otoliths associated with older ages.