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Nyctemeral variations of magnesium intake in the calcitic layer of a Chilean mollusk shell (Concholepas concholepas, Gastropoda)
Lazareth C. E., Guzman N., Poitrasson F., Candaudap F., Ortlieb L.
Geochimica et Cosmochimica Acta Acta / Geochimica et Cosmochimica Acta Acta; Geochimica et Cosmochimica Acta Acta (England); Geochimica et Cosmochimica Acta Acta 71 (2007) 5369-5383 - http://hal.archives-ouvertes.fr/hal-00319310
Article in peer-reviewed journal
Sciences of the Universe/Earth Sciences
Nyctemeral variations of magnesium intake in the calcitic layer of a Chilean mollusk shell (Concholepas concholepas, Gastropoda)
Claire E. Lazareth 1, Nury Guzman 1, Franck Poitrasson 2, Frederic Candaudap 2, Luc Ortlieb 1
1:  Paléo-environnements tropicaux et variabilité climatique (PALEOTROPIQUE)
Institut de recherche pour le développement [IRD]
IRD Ile de France - 32 rue Henri Varagnat - 93143 Bondy Cedex
France
2:  Laboratoire des Mécanismes et Transfert en Géologie (LMTG)
http://www.lmtg.obs-mip.fr/
CNRS : UMR5563 – Observatoire Midi-Pyrénées – Université Paul Sabatier [UPS] - Toulouse III – Institut de recherche pour le développement [IRD] : UMR154
14 avenue Edouard Belin 31400 Toulouse
France
Mollusk shells are increasingly used as records of past environmental conditions, particularly for sea-surface temperature (SST) reconstructions. Many recent studies tackled SST (and/or sea-surface salinity) tracers through variations in the elementary (Mg and Sr) or stable isotope (?18O) composition within mollusk shells. But such attempts, which sometimes include calibration studies on modern specimens, are not always conclusive. We present here a series of Mg and Sr analyses in the calcitic layer of Concholepas concholepas (Muricidae, Gastropoda) with a very high time-resolution on a time window covering about 1 and a half month of shell formation, performed by Laser Ablation Inductively-Coupled Plasma Mass Spectrometry (LA-ICP-MS) and electron probe micro-analysis (EPMA). The selected specimen of this common Chilean gastropod was grown under controlled environmental conditions and precise weekly time-marks were imprinted in the shell with calcein staining. Strontium variations in the shell are too limited to be interpreted in terms of environmental parameter changes. In contrast, Mg incorporation into the shell and growth rate appear to change systematically between night and day. During the day, Mg is incorporated at a higher rate than at night and this intake seems positively correlated with water temperature. The nightly reduced Mg incorporation is seemingly related to metabolically controlled processes, formation of organic-rich shell increments and nocturnal feeding activity of the animals. The nyctemeral Mg changes in the C. concholepas shell revealed in this study might explain at least part of the discrepancies observed in previous studies on the use of Mg as a SST proxy in mollusk shells. In the case of C. concholepas, Mg cannot be used straightforwardly as a SST proxy.
English

Geochimica et Cosmochimica Acta Acta / Geochimica et Cosmochimica Acta Acta; Geochimica et Cosmochimica Acta Acta (England); Geochimica et Cosmochimica Acta Acta
international
2007-11
71
5369-5383