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Boron isotopes as pH proxy: A new look at boron speciation in deep-sea corals using B MAS NMR and EELS |
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| Authors: | Claire Rollion-Bard Dominique Blamart Grégory Tricot Jean-Pierre Cuif |
| Institution: | a Université de Lorraine, Centre de Recherches Pétrographiques et Géochimiques, CRPG-CNRS, 15 rue Notre Dame des Pauvres, 54500 Vandoeuvre-lès-Nancy, France b Laboratoire des Sciences du Climat et de l’Environnement, avenue de la Terrasse, 91198 Gif-sur-Yvette Cédex, France c Unité de Catalyse et de Chimie du Solide-UMR CNRS 8181, ENSCL-USTL F-59652 Villeneuve d’Ascq, France d Unité Matériaux et Transformations, Bât. C6, Université Lille 1, 59655 Villeneuve d’Ascq, France e UMR IDES, Interactions et Dynamique des Environnements de Surface, Bat. 504, Université Paris XI, 91405 Orsay Cédex, France |
| Abstract: | Dissolved boron in modern seawater occurs in the form of two species, trigonal boric acid B(OH)3 and tetrahedral borate ion  . One of the key assumption in the use of boron isotopic compositions of carbonates as pH proxy is that only borate ions,  , are incorporated into the carbonate. Here, we investigate the speciation of boron in deep-sea coral microstructures (Lophelia pertusa specimen) by using high field magic angle spinning nuclear magnetic resonance (11B MAS NMR) and electron energy-loss spectroscopy (EELS). We observe both boron coordination species, but in different proportions depending on the coral microstructure, i.e. centres of calcification versus fibres. These results suggest that careful sampling is necessary before performing boron isotopic measurements in deep-sea corals. By combining the proportions of B(OH)3 and  determined by NMR and our previous ion microprobe boron isotope measurements, we propose a new equation for the relation between seawater pH and boron isotopic composition in deep-sea corals. |
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