Formation of chiral morphologies through selective binding of amino acids to calcite surface steps

被引:603
作者
Orme, CA [1 ]
Noy, A
Wierzbicki, A
McBride, MT
Grantham, M
Teng, HH
Dove, PM
DeYoreo, JJ
机构
[1] Lawrence Livermore Natl Lab, Dept Chem & Mat Sci, Livermore, CA 94551 USA
[2] Univ S Alabama, Dept Chem, Mobile, AL 36688 USA
[3] Virginia Polytech Inst & State Univ, Dept Geol Sci, Blacksburg, VA 24061 USA
[4] George Washington Univ, Dept Earth & Environm Sci, Washington, DC 20052 USA
关键词
D O I
10.1038/35081034
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Many living organisms contain biominerals and composites with finely tuned properties, reflecting a remarkable level of control over the nucleation, growth and shape of the constituent crystals(1-6). Peptides and proteins play an important role in achieving this control(1,7,8). But the general view that organic molecules affect mineralization through stereochemical recognition, where geometrical and chemical constraints dictate their binding to a mineral, seems difficult to reconcile(4) with a mechanistic understanding, where crystallization is controlled by thermodynamic and kinetic factors(9). Indeed, traditional crystal growth models emphasize the inhibiting effect of so-called 'modifiers' on surface-step growth, rather than stereochemical matching to newly expressed crystal facets. Here we report in situ atomic force microscope observations and molecular modelling studies of calcite growth in the presence of chiral amino acids that reconcile these two seemingly divergent views. We rnd that enantiomer-specific binding of the amino acids to those surface-step edges that offer the best geometric and chemical rt changes the step-edge free energies, which in turn results in macroscopic crystal shape modifications. Our results emphasize that the mechanism underlying crystal modification through organic molecules is best understood by considering both stereochemical recognition and the effects of binding on the interfacial energies of the growing crystal.
引用
收藏
页码:775 / 779
页数:6
相关论文
共 34 条
[11]   ATOMIC CHARGES DERIVED FROM ELECTROSTATIC POTENTIALS - A DETAILED STUDY [J].
CHIRLIAN, LE ;
FRANCL, MM .
JOURNAL OF COMPUTATIONAL CHEMISTRY, 1987, 8 (06) :894-905
[12]   GENERAL PARAMETERIZED SCF MODEL FOR FREE-ENERGIES OF SOLVATION IN AQUEOUS-SOLUTION [J].
CRAMER, CJ ;
TRUHLAR, DG .
JOURNAL OF THE AMERICAN CHEMICAL SOCIETY, 1991, 113 (22) :8305-8311
[13]   AM1-SM2 AND PM3-SM3 PARAMETERIZED SCF SOLVATION MODELS FOR FREE-ENERGIES IN AQUEOUS-SOLUTION [J].
CRAMER, CJ ;
TRUHLAR, DG .
JOURNAL OF COMPUTER-AIDED MOLECULAR DESIGN, 1992, 6 (06) :629-666
[14]   AN SCF SOLVATION MODEL FOR THE HYDROPHOBIC EFFECT AND ABSOLUTE FREE-ENERGIES OF AQUEOUS SOLVATION [J].
CRAMER, CJ ;
TRUHLAR, DG .
SCIENCE, 1992, 256 (5054) :213-217
[15]   The role of Mg2+ as an impurity in calcite growth [J].
Davis, KJ ;
Dove, PM ;
De Yoreo, JJ .
SCIENCE, 2000, 290 (5494) :1134-1137
[16]  
Didymus J.M., 1991, P267
[17]   CONSTRUCTION AND MORPHOGENESIS OF THE CHIRAL ULTRASTRUCTURE OF COCCOLITHS FROM THE MARINE ALGA EMILIANIA-HUXLEYI [J].
DIDYMUS, JM ;
YOUNG, JR ;
MANN, S .
PROCEEDINGS OF THE ROYAL SOCIETY B-BIOLOGICAL SCIENCES, 1994, 258 (1353) :237-245
[18]   SURFACE-STRUCTURE DETERMINATION BY X-RAY-DIFFRACTION [J].
FEIDENHANSL, R .
SURFACE SCIENCE REPORTS, 1989, 10 (03) :105-188
[19]   Surface speciation of calcite observed in situ by high-resolution X-ray reflectivity [J].
Fenter, P ;
Geissbühler, P ;
DiMasi, E ;
Srajer, G ;
Sorensen, LB ;
Sturchio, NC .
GEOCHIMICA ET COSMOCHIMICA ACTA, 2000, 64 (07) :1221-1228
[20]  
HONESS AP, 1937, 35 PENNS STAT COLL M, P667