FN Archimer Export Format PT J TI New insights into oyster high-resolution hinge growth patterns BT AF Huyghe, Dimitri de Rafelis, Marc Ropert, Michel Mouchi, Vincent Emmanuel, Laurent Renard, Maurice Lartaud, Franck AS 1:1,2;2:2;3:3;4:1,4;5:4;6:4;7:1; FF 1:;2:;3:PDG-ODE-LITTORAL-LERN;4:;5:;6:;7:; C1 Sorbonne Université, CNRS, Laboratoire d’Ecogéochimie des Environnements Benthiques, LECOB, Observatroire Océanologique de Banyuls, 66650 Banyuls‑sur‑Mer, France Géosciences Environnement Toulouse, CNRS, IRD, Université Paul Sabatier Toulouse 3, 14 Avenue Edouard Belin, 31400 Toulouse, France Ifremer, Laboratoire Environnement Ressource de Normandie, Avenue du General de Gaulle, BP 32, 14520 Port.en.Bessin, France Sorbonne Université, CNRS-INSU, Institut des Sciences de la Terre Paris, ISTeP, 75005 Paris, France C2 UNIV PARIS 06, FRANCE UNIV TOULOUSE, FRANCE IFREMER, FRANCE UNIV PARIS 06, FRANCE SI PORT-EN-BESSIN SE PDG-ODE-LITTORAL-LERN IN WOS Ifremer UPR copubli-france copubli-univ-france IF 2.05 TC 18 UR https://archimer.ifremer.fr/doc/00484/59601/85211.pdf LA English DT Article AB While oyster shells are one of the most common mollusks used for the analysis of (paleo)environmental and (paleo)climatic records based on geochemical proxies, high-resolution growth rate changes still need to be determined. Promising previous works are restricted to small portions of shell sections due to difficulties in continuous growth increment revelation. Based on a mark and recapture experiment of Magallana gigas specimens reared in an intertidal area of Normandy (France) for 22 months, and a sclerochronological approach using cathodoluminescence microscopy, this study provides the longest high-resolution record of growth increments in oyster shells to date. Different growth patterns were identified likely related to the oyster age. After age 1 year, the formation of growth increments follows an expected tide-related model, leading to the mineralization of ~ 2 calcitic increments per day, together with growth rate changes at lunar and semi-lunar periodicities, and a seasonal trend with occasional growth breaks during winter when temperatures fall below ~ 6 °C. However, for oysters younger than 1 year, i.e., before reaching their sexual maturity, the growth increment analysis reveals unconventional patterns. In this case, oysters’ growth is associated with either a large number (~ 5) or less than one increment per day depending on the period. This pattern is also associated with frequent growth cessations, although the growth rate of the shell is high at this period. Our results illustrate that the high-resolution sclerochronological approach is required for accurate paleoenvironmental reconstructions based on oyster shells. PY 2019 PD APR SO Marine Biology SN 0025-3162 PU Springer Nature VL 166 IS 4 UT 000460657700002 DI 10.1007/s00227-019-3496-2 ID 59601 ER EF