Abstract

This is the first study exploring skeletal mechanical properties in temperate corals. The variation of skeletal mechanical properties with distance from the aboral pole, coral age, and population was investigated in the corals Balanophyllia europaea (zooxanthellate) and Leptopsammia pruvoti (non-zooxanthellate), collected at three sites along a wide latitudinal gradient. Mechanical properties were measured by nanoindentation, a technique applied here in detail for the first time to a scleractinian. In both species, a reduction of Young’s modulus was observed toward the oral pole, which is the youngest part of the skeleton. Skeletons of B. europaea increased their Young’s modulus with age, unlike L. pruvoti. Only the zooxanthellate species showed reduced Young’s modulus in southern populations, coherently with the observed reduced skeletal bulk density and porosity with SST (decreasing latitude) in B. europaea, and with the lack of correlations with SST and latitude for skeletal bulk density and porosity in L. pruvoti. These results support previous hypotheses on differences in the skeletal mechanical properties of these two coral species in relation to the observed variations of skeletal bulk density and porosity with temperature/latitude, which may have consequences related to the envisaged seawater warming of next decades.

Highlights

  • Sea surface temperature (SST) is one of the main factors that determine coral reef development (Kleypas et al 1999), and it strictly depends on latitude (Kain 1989)

  • The present study focuses on these two common scleractinian corals of the Mediterranean Sea: B. europaea (Risso, 1826) and L. pruvoti Lacaze-Duthiers, 1897, aiming to investigate the variations of coral skeletal mechanical properties

  • The study of skeletal mechanical properties was divided into three analyses to assess the hardness and Young’s modulus trends according to: (1) the skeletal zone, (2) the age class of the individuals, and (3) the population

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Summary

Introduction

Sea surface temperature (SST) is one of the main factors that determine coral reef development (Kleypas et al 1999), and it strictly depends on latitude (Kain 1989). The rate of climate change is accelerating, and the average surface temperature of the oceans is likely to increase by 1.1–6.4 °C during the current century (Solomon et al 2007). The magnitude of temperature change is expected to be greater in temperate areas than in tropical ones (Solomon et al 2007). In the Mediterranean Sea, the current rate of warming averages 0.04 °C per yr (Dıaz-Almela et al 2007), twice than in the global ocean (Vargas-Yanez et al 2007). The coralligenous community, which is one of the most diverse in the Mediterranean Sea (*1,700 species) (Ballesteros 2006) and where suspension feeders are

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