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PDBsum entry 3bob
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Enzyme class:
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E.C.4.2.1.1
- carbonic anhydrase.
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Reaction:
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hydrogencarbonate + H+ = CO2 + H2O
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hydrogencarbonate
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+
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H(+)
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=
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CO2
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+
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H2O
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Cofactor:
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Zn(2+)
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Molecule diagrams generated from .mol files obtained from the
KEGG ftp site
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DOI no:
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Nature
452:56-61
(2008)
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PubMed id:
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Structure and metal exchange in the cadmium carbonic anhydrase of marine diatoms.
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Y.Xu,
L.Feng,
P.D.Jeffrey,
Y.Shi,
F.M.Morel.
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ABSTRACT
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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.
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Selected figure(s)
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Figure 1.
Figure 1: Structure of the second CA repeat of CDCA1 (CDCA1-R2).
a, Overall structure of the Cd-bound CDCA1-R2. Two lobes of
the structure are coloured blue and green. Cd is highlighted in
red, and Cd-coordinating residues are coloured yellow. b,
Comparison of the active site conformation between CDCA-R2
(green) and
-CA (blue). The active site residues in CDCA-R2 and -CA
are coloured yellow and orange, respectively. Hydrogen bonds are
represented by red dashed lines. Cd and the water ligand are
shown in large and small red spheres, respectively. (A stereo
view is shown in Supplementary Fig. 1b.) c, Comparison of Cd-
and Zn-coordination in CDCA1-R2. Metal coordination and hydrogen
bonds are indicated by red and green dashed lines, respectively;
numbers indicate bond lengths in Å. W1–W3, water
molecules. Structural images were prepared using MOLSCRIPT^44
and GRASP^45.
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Figure 3.
Figure 3: Structure of CDCA1-R2 bound to substrate analogue
acetate. a, A close-up view of the region around acetate. The
F[o] - F[c] electron density map surrounding acetate was
calculated using simulated annealing with the omission of
acetate and was contoured at 5 .
b, A close-up view of the active site conformation. Metal
coordination and hydrogen bonds are indicated by red and green
dashed lines, respectively. Relevant distances are indicated
(Å). c, A hydrophobic channel traverses through CDCA1-R2.
Cd is highlighted in red. Acetate is shown in yellow. The
conserved hydrophobic residues that line the channel are shown
in magenta. (Stereo views of a and b are shown in Supplementary
Fig.
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The above figures are
reprinted
by permission from Macmillan Publishers Ltd:
Nature
(2008,
452,
56-61)
copyright 2008.
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Figures were
selected
by an automated process.
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Literature references that cite this PDB file's key reference
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PubMed id
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Reference
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B.M.Hopkinson,
C.L.Dupont,
A.E.Allen,
and
F.M.Morel
(2011).
Efficiency of the CO2-concentrating mechanism of diatoms.
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Proc Natl Acad Sci U S A,
108,
3830-3837.
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C.T.Supuran
(2011).
Carbonic anhydrase inhibition with natural products: novel chemotypes and inhibition mechanisms.
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Mol Divers,
15,
305-316.
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F.Carta,
A.Innocenti,
R.A.Hall,
F.A.Mühlschlegel,
A.Scozzafava,
and
C.T.Supuran
(2011).
Carbonic anhydrase inhibitors. Inhibition of the β-class enzymes from the fungal pathogens Candida albicans and Cryptococcus neoformans with branched aliphatic/aromatic carboxylates and their derivatives.
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Bioorg Med Chem Lett,
21,
2521-2526.
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F.Pannetier,
G.Ohanessian,
and
G.Frison
(2011).
Comparison between α- and β-carbonic anhydrases: can Zn(His)3(H2O) and Zn(His)(Cys)2(H2O) sites lead to equivalent enzymes?
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Dalton Trans,
40,
2696-2698.
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J.A.Cuesta-Seijo,
M.S.Borchert,
J.C.Navarro-Poulsen,
K.M.Schnorr,
S.B.Mortensen,
and
L.Lo Leggio
(2011).
Structure of a dimeric fungal α-type carbonic anhydrase.
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FEBS Lett,
585,
1042-1048.
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J.A.Tamames,
and
M.J.Ramos
(2011).
Metals in proteins: cluster analysis studies.
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J Mol Model,
17,
429-442.
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J.R.Reinfelder
(2011).
Carbon concentrating mechanisms in eukaryotic marine phytoplankton.
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Ann Rev Mar Sci,
3,
291-315.
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O.Amata,
T.Marino,
N.Russo,
and
M.Toscano
(2011).
Catalytic activity of a ζ-class zinc and cadmium containing carbonic anhydrase. Compared work mechanisms.
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Phys Chem Chem Phys,
13,
3468-3477.
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C.A.Ohlin,
E.M.Villa,
J.R.Rustad,
and
W.H.Casey
(2010).
Dissolution of insulating oxide materials at the molecular scale.
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Nat Mater,
9,
11-19.
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J.G.Ferry
(2010).
The gamma class of carbonic anhydrases.
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Biochim Biophys Acta,
1804,
374-381.
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L.Syrjänen,
M.Tolvanen,
M.Hilvo,
A.Olatubosun,
A.Innocenti,
A.Scozzafava,
J.Leppiniemi,
B.Niederhauser,
V.P.Hytönen,
T.A.Gorr,
S.Parkkila,
and
C.T.Supuran
(2010).
Characterization of the first beta-class carbonic anhydrase from an arthropod (Drosophila melanogaster) and phylogenetic analysis of beta-class carbonic anhydrases in invertebrates.
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BMC Biochem,
11,
28.
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M.Smiri,
A.Chaoui,
N.Rouhier,
C.Kamel,
E.Gelhaye,
J.P.Jacquot,
and
E.El Ferjani
(2010).
Cadmium induced mitochondrial redox changes in germinating pea seed.
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Biometals,
23,
973-984.
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K.J.Waldron,
J.C.Rutherford,
D.Ford,
and
N.J.Robinson
(2009).
Metalloproteins and metal sensing.
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Nature,
460,
823-830.
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K.J.Waldron,
and
N.J.Robinson
(2009).
How do bacterial cells ensure that metalloproteins get the correct metal?
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Nat Rev Microbiol,
7,
25-35.
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R.S.Rowlett,
C.Tu,
J.Lee,
A.G.Herman,
D.A.Chapnick,
S.H.Shah,
and
P.C.Gareiss
(2009).
Allosteric site variants of Haemophilus influenzae beta-carbonic anhydrase.
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Biochemistry,
48,
6146-6156.
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PDB codes:
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S.Elleuche,
and
S.Pöggeler
(2009).
Beta-carbonic anhydrases play a role in fruiting body development and ascospore germination in the filamentous fungus Sordaria macrospora.
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PLoS ONE,
4,
e5177.
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A.Moya,
S.Tambutté,
A.Bertucci,
E.Tambutté,
S.Lotto,
D.Vullo,
C.T.Supuran,
D.Allemand,
and
D.Zoccola
(2008).
Carbonic anhydrase in the scleractinian coral Stylophora pistillata: characterization, localization, and role in biomineralization.
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J Biol Chem,
283,
25475-25484.
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F.M.Morel
(2008).
The co-evolution of phytoplankton and trace element cycles in the oceans.
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Geobiology,
6,
318-324.
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J.F.Domsic,
B.S.Avvaru,
C.U.Kim,
S.M.Gruner,
M.Agbandje-McKenna,
D.N.Silverman,
and
R.McKenna
(2008).
Entrapment of Carbon Dioxide in the Active Site of Carbonic Anhydrase II.
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J Biol Chem,
283,
30766-30771.
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PDB codes:
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R.E.Mirams,
S.J.Smith,
K.S.Hadler,
D.L.Ollis,
G.Schenk,
and
L.R.Gahan
(2008).
Cadmium(II) complexes of the glycerophosphodiester-degrading enzyme GpdQ and a biomimetic N,O ligand.
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J Biol Inorg Chem,
13,
1065-1072.
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The most recent references are shown first.
Citation data come partly from CiteXplore and partly
from an automated harvesting procedure. Note that this is likely to be
only a partial list as not all journals are covered by
either method. However, we are continually building up the citation data
so more and more references will be included with time.
Where a reference describes a PDB structure, the PDB
codes are
shown on the right.
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}
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