TY  - JOUR
AU  - Chauvaud Laurent, Thébault Julien
PY  - 2011//
TI  - Whats Hiding Behind Ontogenetic 13C Variations in Mollusk Shells? New Insights from the Great Scallop (Pecten maximus)
JO  - ESTUARIES AND COASTS
SP  - 211
EP  - 220
VL  - 34
IS  - 2
PB  - Springer-Verlag
KW  - Scallop shells
KW  - Carbon isotopes
KW  - Phytoplankton
KW  - Ontogeny
KW  - Proxy
KW  -
N2  - Mollusk shells contain geochemical information about environmental conditions that prevailed at the time of formation. We investigated ontogenetic and seasonal variations of δ13C in calcitic shells of Pecten maximus. Ontogenetic variations of δ13Cshell in three large specimens collected in Norway, France, and Spain exhibited a similar linear decrease with increasing shell height. We removed this linear drift (detrending). These three residual time series displayed variations that could be linked to environmental fluctuations. To check it, we reanalyzed the isotopic datasets of Lorrain et al. (Journal of Experimental Marine Biology and Ecology 275:47–61, 2002, Geochimica et Cosmochimica Acta 68:3509–3519, 2004), who worked on three scallops harvested in 2000 in the bay of Brest (France), a well-monitored ecosystem. Lowest values of δ13Cshell detrended were recorded in all shells in late spring–early summer, most likely reflecting corresponding variations in food availability. Our results indicate that ontogenetic and seasonal variations of δ13Cshell cannot be used as a proxy for past δ13CDIC variations but should be considered as promising tools for ecophysiological studies.
SN  - 1559-2723
UR  - http://dx.doi.org/10.1007/s12237-010-9267-4
N1  - exported from refbase (http://publi.ipev.fr/polar_references/show.php?record=1472), last updated on Mon, 01 Jul 2024 22:01:36 +0200
ID  - ChauvaudLaurent2011
ER  -