Shifts in shell mineralogy and metabolism of Concholepas concholepas juveniles along the Chilean coast
Laura Ramajo A B F , Alejandro B. Rodríguez-Navarro C , Carlos M. Duarte A D , Marco A. Lardies E and Nelson A. Lagos B
+ Author Affiliations
- Author Affiliations
A Global Change Department, Instituto Mediterráneo de Estudios Avanzados (IMEDEA, CSIC-UIB), C/ Miquel Marqués 21, E-07190 Esporles, Islas Baleares, Spain.
B Centro de Investigación e Innovación para el Cambio Climático (CiiCC), Universidad Santo Tomás, Avenida Ejército 146, 8370003 Santiago, Chile.
C Departamento de Mineralogía y Petrología, Facultad de Ciencias, Universidad de Granada, Avenida Fuentenueva s/n, 18071 Granada, Spain.
D Red Sea Research Center, King Abdullah University of Science and Technology, Thuwal 23955-6900, Kingdom of Saudi Arabia.
E Facultad de Artes Liberales e Ingeniería y Ciencias, Universidad Adolfo Ibañez, Avenida Diagonal Las Torres 2640, 7041169 Santiago, Chile.
F Corresponding author. Laura Ramajo. Email: lramajo@imedea.uib-csic.es
Marine and Freshwater Research 66(12) 1147-1157 https://doi.org/10.1071/MF14232
Submitted: 5 August 2014 Accepted: 12 January 2015 Published: 7 May 2015
Abstract
Along the west coast of South America, from the tropical zone to the Patagonian waters, there is a significant latitudinal gradient in seawater temperature, salinity and carbonate chemistry. These physical–chemical changes in seawater induce morphological and physiological responses in calcifying organisms, which may alter their energy budget and calcification processes. In this study, we study the organism energy maintenance (i.e. metabolic rate) and mineralogical composition of the shell of the juvenile marine snails Concholepas concholepas (Gastropoda: Muricidae), collected from benthic populations located ~2000 km apart, varies across geographic regions along the Chilean coast. We found that in juvenile snails, the calcite : aragonite ratio in the pallial shell margin (i.e. newly deposited shell) increase significantly from northern to southern populations and this increase in calcite precipitation in the shell of juveniles snails was associated with a decrease in oxygen consumption rates in these populations. Our result suggests that calcite secretion may be favoured when metabolic rates are lowered, as this carbonate mineral phase might be less energetically costly for the organism to precipitate. This result is discussed in relation to the natural process such as coastal upwelling and freshwater inputs that promote geographic variation in levels of pH and carbonate saturation state in seawater along the Chilean coast.
Additional keywords: calcium carbonate, metabolism, ocean acidification, temperature.
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