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Nature 452, 56-61 (6 March 2008) | doi:10.1038/nature06636; Received 3 July 2007; Accepted 10 January 2008

Structure and metal exchange in the cadmium carbonic anhydrase of marine diatoms

Yan Xu1,4, Liang Feng2,4,5, Philip D. Jeffrey2,4, Yigong Shi2 & François M. M. Morel3

  1. Department of Ecology and Evolutionary Biology,
  2. Department of Molecular Biology,
  3. Department of Geosciences, Princeton University, New Jersey 08544, USA
  4. These authors contributed equally to this work.
  5. Present address: Laboratory of Molecular Neurobiology and Biophysics, Rockefeller University, New York 10065, USA.

Correspondence to: Yigong Shi2François M. M. Morel3 Correspondence and requests for materials should be addressed to F.M.M.M. (Email: morel@princeton.edu) or Y.S. (Email: yshi@princeton.edu).

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Carbonic anhydrase, a zinc enzyme found in organisms from all kingdoms, catalyses the reversible hydration of carbon dioxide and is used for inorganic carbon acquisition by phytoplankton. In the oceans, where zinc is nearly depleted, diatoms use cadmium as a catalytic metal atom in cadmium carbonic anhydrase (CDCA). Here we report the crystal structures of CDCA in four distinct forms: cadmium-bound, zinc-bound, metal-free and acetate-bound. Despite lack of sequence homology, CDCA is a structural mimic of a functional beta-carbonic anhydrase dimer, with striking similarity in the spatial organization of the active site residues. CDCA readily exchanges cadmium and zinc at its active site—an apparently unique adaptation to oceanic life that is explained by a stable opening of the metal coordinating site in the absence of metal. Given the central role of diatoms in exporting carbon to the deep sea, their use of cadmium in an enzyme critical for carbon acquisition establishes a remarkable link between the global cycles of cadmium and carbon.