Constraining calcium isotope fractionation (delta Ca-44/40) in modern and fossil scleractinian coral skeleton - Université Pierre et Marie Curie Accéder directement au contenu
Article Dans Une Revue Chemical Geology Année : 2013

Constraining calcium isotope fractionation (delta Ca-44/40) in modern and fossil scleractinian coral skeleton

Résumé

The present study investigates the influence of environmental (temperature, salinity) and biological (growth rate, inter-generic variations) parameters on calcium isotope fractionation (delta Ca-44/40) in scleractinian coral skeleton to better constrain this record. Previous studies focused on the delta Ca-44/40 record in different marine organisms to reconstruct seawater composition or temperature, but only few studies investigated corals. This study presents measurements performed on modern corals from natural environments (from the Maldives for modem and from Tahiti for fossil corals) as well as from laboratory cultures (Centre Scientifique de Monaco). Measurements on Porites sp., Acropora sp., Montipora verrucosa and Stylophora pistillata allow constraining inter-generic variability. Our results show that the fractionation of delta Ca-44/40 ranges from 0.6 to 0.1%., independent of the genus or the environmental conditions. No significant relationship between the rate of calcification and delta Ca-44/40 was found. The weak temperature dependence reported in earlier studies is most probably not the only parameter that is responsible for the fractionation. Indeed, sub-seasonal temperature variations reconstructed by delta O-18 and Sr/Ca ratio using a multi-proxy approach, are not mirrored in the coral's delta Ca-44/40 variations. The intergeneric variability and intrageneric variability among the studied samples are weak except for S. pistillate, which shows calcium isotopic values increasing with salinity. The variability between samples cultured at a salinity of 40 is higher than those cultured at a salinity of 36 for this species. The present study reveals a strong biological control of the skeletal calcium isotope composition by the polyp and a weak influence of environmental factors, specifically temperature and salinity (except for S. pistillate). Vital effects have to be investigated in situ to better constrain their influence on-the calcium isotopic signal. If vital effects could be extracted from the isotopic signal, the calcium isotopic composition of coral skeletons could provide reliable information on the calcium composition and budget in ocean. (c) 2012 Elsevier B.V. All rights reserved.

Domaines

Océanographie

Dates et versions

hal-03502640 , version 1 (26-12-2021)

Identifiants

Citer

Chloe Pretet, Elias Samankassou, Thomas Felis, Stephanie Reynaud, Florian Boehm, et al.. Constraining calcium isotope fractionation (delta Ca-44/40) in modern and fossil scleractinian coral skeleton. Chemical Geology, 2013, 340, pp.49-58. ⟨10.1016/j.chemgeo.2012.12.006⟩. ⟨hal-03502640⟩
26 Consultations
0 Téléchargements

Altmetric

Partager

Gmail Facebook X LinkedIn More