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Characterization of a Ca(II)-, Mineral-Interactive Poly- electrolyte Sequence from the Adhesive Elastomeric Biomineralization Protein, Lustrin A Brandon A. Wustman, James C. Weaver, Daniel E. Morse, and John Spencer Evans* Langmuir 2003, 19, 9373-9381. In the Materials and Methods section under the subheading Crystal Growth Interaction Experiments, the actual polypeptide concentration range utilized in the geologic calcite overgrowth experiments should read as 1.1 × 10 -6 , 3.3 × 10 -6 , 1.7 × 10 -5 , 3.3 × 10 -5 , 1.7 × 10 -5 , and 3.3 × 10 -4 M. Under the subheading, Solid-State 1 H Magic-Angle Spinning (MAS) NMR Spectroscopy, the concentration of D4 polypeptide utilized in this assay should read as 3.3 × 10 -4 M. Likewise, in the Results section, the polypeptide con- centrations reported in the legend to Figure 6 require correction. The correct figure legend and polypeptide concentrations are presented below. Figure 6. Scanning electron micrographs of calcium carbonate overgrowth on the {104} cleavage plane of geological calcite in the presence of (A) No peptide added (negative control); (B) Poly-L-Asp, 3.3 × 10 -5 M; (C) Poly- L-Glu, 3.3 × 10 -5 M; (D) AP24-1 model peptide, 1.7 × 10 -5 M; (E) D4 model peptide, 3.3 × 10 -6 M. Spacebar in each figure represents 1 μm, magnification ) 5000×. LA0361621 10.1021/la0361621 Published on Web 12/06/2003 Rheology, Cryogenic Transmission Electron Spectroscopy, and Small-Angle Neutron Scattering of Highly Viscoelastic Wormlike Micellar Solutions Vania Croce,* Terence Cosgrove,* Geoff Maitland, Trevor Hughes, and Go ¨ran Karlsson Langmuir 2003, 19, 8536-8541. This paper was published with an error in the title. The correct title and byline are given below: Rheology, Cryogenic Transmission Electron Microscopy, and Small-Angle Neutron Scattering of Highly Viscoelastic Wormlike Micellar Solutions Vania Croce* and Terence Cosgrove* School of Chemistry, University of Bristol, Cantock’s Close, Bristol BS8 1TS, U.K. Geoff Maitland and Trevor Hughes Schlumberger Cambridge Research, High Cross, Madingley Road, Cambridge CB3 0EL, U.K. Go ¨ran Karlsson Department of Physical Chemistry, Uppsala University, Box 579, Uppsala S-75123, Sweden LA0304114 10.1021/la0304114 Published on Web 12/03/2003 277 Langmuir 2004, 20, 277-277 10.1021/la0361621 CCC: $27.50 © 2004 American Chemical Society Published on Web 12/06/2003

Characterization of a Ca(II)-, Mineral-Interactive Polyelectrolyte Sequence from the Adhesive Elastomeric Biomineralization Protein, Lustrin A

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Page 1: Characterization of a Ca(II)-, Mineral-Interactive Polyelectrolyte Sequence from the Adhesive Elastomeric Biomineralization Protein, Lustrin A

Characterization of a Ca(II)-, Mineral-Interactive Poly-electrolyte Sequence from the Adhesive ElastomericBiomineralization Protein, Lustrin ABrandon A. Wustman, James C. Weaver, Daniel E.Morse, and John Spencer Evans* Langmuir 2003, 19,9373-9381.

In the Materials and Methods section under thesubheading Crystal Growth Interaction Experiments, theactual polypeptide concentration range utilized in thegeologic calcite overgrowth experiments should read as1.1 × 10-6, 3.3 × 10-6, 1.7 × 10-5, 3.3 × 10-5, 1.7 × 10-5,and 3.3 × 10-4 M. Under the subheading, Solid-State 1HMagic-Angle Spinning (MAS) NMR Spectroscopy, theconcentration of D4 polypeptide utilized in this assayshould read as 3.3 × 10-4 M.

Likewise, in the Results section, the polypeptide con-centrations reported in the legend to Figure 6 requirecorrection. The correct figure legend and polypeptideconcentrations are presented below.Figure 6. Scanning electron micrographs of calciumcarbonate overgrowth on the {104} cleavage plane ofgeological calcite in the presence of (A) No peptide added(negative control); (B) Poly-L-Asp, 3.3 × 10-5 M; (C) Poly-L-Glu, 3.3 × 10-5 M; (D) AP24-1 model peptide, 1.7 × 10-5

M; (E) D4 model peptide, 3.3 × 10-6 M. Spacebar in eachfigure represents 1 µm, magnification ) 5000×.

LA0361621

10.1021/la0361621Published on Web 12/06/2003

Rheology, Cryogenic Transmission ElectronSpectroscopy, and Small-Angle Neutron Scattering ofHighly Viscoelastic Wormlike Micellar Solutions

Vania Croce,* Terence Cosgrove,* Geoff Maitland,Trevor Hughes, and Goran Karlsson Langmuir 2003, 19,8536-8541.

This paper was published with an error in the title. Thecorrect title and byline are given below:

Rheology, Cryogenic Transmission ElectronMicroscopy, and Small-Angle Neutron

Scattering of Highly Viscoelastic WormlikeMicellar Solutions

Vania Croce* and Terence Cosgrove*

School of Chemistry, University of Bristol, Cantock’sClose, Bristol BS8 1TS, U.K.

Geoff Maitland and Trevor Hughes

Schlumberger Cambridge Research, High Cross,Madingley Road, Cambridge CB3 0EL, U.K.

Goran Karlsson

Department of Physical Chemistry, Uppsala University,Box 579, Uppsala S-75123, Sweden

LA0304114

10.1021/la0304114Published on Web 12/03/2003

277Langmuir 2004, 20, 277-277

10.1021/la0361621 CCC: $27.50 © 2004 American Chemical SocietyPublished on Web 12/06/2003