Microanalysis of C and O isotopes of azooxanthellate and zooxanthellate corals by ion microprobe |
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Authors: | Rollion-Bard C Blamart D Cuif J-P Juillet-Leclerc A |
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Institution: | (1) BP 20, CRPG-CNRS, 15 rue Notre-Dame des Pauvres, 54500 Vandoeuvre-lès-Nancy, France;(2) Laboratoire des Sciences du Climat et de lEnvironnement, CEA-CNRS, Domaine du CNRS, Bat 12, 4 Avenue de la Terrasse, 91198 Gif-sur-Yvette Cédex, France;(3) Faculte des Sciences, Universite de Paris XI , Bat 504 Geologie, 91405 Orsay Cedex, France |
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Abstract: | We have determined the 18O and 13C values of azooxanthellate (Lophelia pertusa) and zooxanthellate (Porites lutea) corals at a micrometer scale using an ion microprobe (SIMS—secondary ion mass spectrometry). In P. lutea, centers of calcification are small (10 to 15 m) and difficult to locate during measurements. In L. pertusa, they are large (50 m) and arranged in lines of centers of calcification. Our results show that centers of calcification in L. pertusa have a restricted range of variation in 18O -2.8±0.3 (PDB)], and a larger range in 13C 14.3 to 10.9 (PDB)]. Surrounding skeletal fibers exhibit large isotopic variation both for C and O (up to 12), and 13C and 18O are positively correlated. The C and O isotopic compositions of the center of calcification deviate from this linear trend at the lightest 18O values of the surrounding fibers. Ion microprobe results on P. lutea demonstrate also a large range of variation for the 18O values (up to 10). No correlation is found with C isotopes that exhibit, in comparison with L. pertusa, a small range of variation (2). This variation of 18O at a micrometer scale is probably the result of two processes: (1) an isotopic equilibrium calcification with 1 pH unit variation in the calcification fluid as indicated by direct measurements of coelenteron pH in the coral Galaxea fascicularis (Al-Horani et al. 2003) and (2) a kinetic fractionation. The 13C apparent disequilibrium in P. lutea may be the result of mixing between metabolic CO2 (respiration) and dissolved inorganic carbon (DIC) coming directly from seawater. |
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Keywords: | Corals Oxygen isotopes Carbon isotopes Ion microprobe Porites lutea Lophelia pertusa |
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