4.7 Article

In situ measurements of oxygen isotopic composition in deep-sea coral, Lophelia pertusa: Re-examination of the current geochemical models of biomineralization

Journal

GEOCHIMICA ET COSMOCHIMICA ACTA
Volume 74, Issue 4, Pages 1338-1349

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.gca.2009.11.011

Keywords

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Funding

  1. European Commission [ERAS-CT-2003-980409]
  2. ANR [ANR-06-BLAN-0233]
  3. Agence Nationale de la Recherche (ANR) [ANR-06-BLAN-0233] Funding Source: Agence Nationale de la Recherche (ANR)

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We present ion microprobe measurements of oxygen isotopic compositions in the deep-sea coral Lophelia pertusa. Compared to bulk skeletal aragonite fibres, the EMZ (early mineralization zone), near the inside of the calyx, was systematically depleted in (18)O. Rayleigh fractionation from a semi-closed fluid reservoir does not explain this and other geochemical differences. Furthermore, pH values estimated from skeletal delta(11)B data are inconsistent with the idea that EMZ (or centres of calcification) (18)O depletion reflects a more alkaline calcification environment. Our data, combined with microstructural and geochemical observations, indicate that the aragonitic fibres and EMZ are formed by a compartmentalized mineralization calicoblastic ectoderm, which exerts strong biological control on the composition of the skeleton. Hence, we propose a new model whereby amorphous calcium carbonates (ACC) are precursors to the EMZ, whereas the fibre precipitation is probably governed by kinetic processes. (C) 2009 Elsevier Ltd. All rights reserved.

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