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AGU: Geophysical Research Letters

 

Keywords

  • biomineralization
  • coral
  • NanoSIMS

Index Terms

  • Oceanography: Biological and Chemical: Geochemistry
  • Oceanography: Biological and Chemical: Chemical tracers
  • Biogeosciences: Isotopic composition and chemistry
  • Biogeosciences: Instruments and techniques
  • Biogeosciences: Paleoclimatology and paleoceanography

Abstract

Strontium-86 labeling experiments show spatially heterogeneous skeletal formation in the scleractinian coral Porites porites

Fanny Houlbrèque

Geological and Environmental Sciences, Stanford University, Stanford, California, USA

Marine Environment Laboratories, International Atomic Energy Agency, Principality of Monaco, Monaco

Anders Meibom

Laboratoire de Minéralogie et Cosmochimie du Muséum (LMCM), UMS NanoAnalyses 2679, Muséum National D'Histoire Naturelle, Paris, France

Jean-Pierre Cuif

UMR8148, IDES, Université Paris XI, Orsay, France

Jaroslaw Stolarski

Instytut Paleobiologii PAN, Warszawa, Poland

Yves Marrocchi

Laboratoire de Minéralogie et Cosmochimie du Muséum (LMCM), UMS NanoAnalyses 2679, Muséum National D'Histoire Naturelle, Paris, France

Christine Ferrier-Pagès

Centre Scientifique de Monaco, Principality of Monaco, Monaco

Isabelle Domart-Coulon

Département Milieux et Peuplements Aquatiques, UMR5178, Muséum National d'Histoire Naturelle, Paris, France

Robert B. Dunbar

Geological and Environmental Sciences, Stanford University, Stanford, California, USA

This paper presents the results of an effort to label calcium carbonates formed by marine organisms with stable isotopes to obtain information about the biomineralization processes. The growing skeleton of the scleractinian coral Porites porites was labeled three times with enhanced abundances of 86Sr. The distribution of 86Sr in the skeleton was imaged with the NanoSIMS ion microprobe with a spatial resolution of ∼200 nm and combined with images of the skeletal ultra-structure. Importantly, the distribution of the 86Sr label in the P. porites skeleton was found to be strongly heterogeneous. This constrains the physical dimensions of the hypothetical Extracellular Calcifying Fluid (ECF) reservoir at the surface of the growing skeleton, which is implicit in most geochemical models for coral biomineralization. These new experimental capabilities allow for a much more detailed view of the growth dynamics for a wide range of marine organisms that biomineralize carbonate structures.

Received 24 November 2008; accepted 14 January 2009; published 19 February 2009.

Citation: Houlbrèque, F., A. Meibom, J.-P. Cuif, J. Stolarski, Y. Marrocchi, C. Ferrier-Pagès, I. Domart-Coulon, and R. B. Dunbar (2009), Strontium-86 labeling experiments show spatially heterogeneous skeletal formation in the scleractinian coral Porites porites, Geophys. Res. Lett., 36, L04604, doi:10.1029/2008GL036782.

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