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* Institute of Biological Chemistry, Academia Sinica, Taipei 11529, Taiwan, and
Department of Biochemistry and
Department of Animal Biology, University of Illinois at Urbana-Champaign, Urbana, Illinois 61801 USA
Correspondence: Address reprint requests to Andrew H.-J. Wang, Institute of Biological Chemistry, Academia Sinica, Nankang, Taipei 11529, Taiwan. Tel.: 8-862-2788-1981; Fax: 8-862-2788-2043; E-mail: ahjwang{at}gate.sinica.edu.tw.
| ABSTRACT |
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| INTRODUCTION |
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All type III AFPs are highly homologous as indicated by the extensive amino acid sequence identity. As shown in Fig. 1,
50% of the amino acid residues are identical. Recently, the human genome sequencing project identified a domain in sialic acid synthase (SAS) to be homologous to type III AFPs (International Human Genome Sequencing Consortium, 2001
). This is the C-terminal domain (Baardsnes and Davies, 2001
), and its deletion results in loss of the SAS activity (Dr. Chun-Hung Lin, IBC, personal communication). All of the crystallographic studies on type III AFPs carried out so far employed the Atlantic ocean pout Macrozoarces americanus as the source organism. Most of these structures were determined using crystals that belonged to the orthorhombic space group P212121 and had similar cell dimensions. In the study by Yang et al. (1998)
a new monoclinic crystal form of P21 was also reported. In this paper we present an orthorhombic crystal structure of type III AFP, RD1 from the Antarctic eel pout, Lycodichthys dearborni, at a resolution of 0.62 Å. This is the highest resolution of all type III AFP crystal structures known, and it permitted the identification of many interesting fine-scale structural features of the AFP that could be associated with function.
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| MATERIALS AND METHODS |
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Two data sets were collected in the end, with resolution ranges of 500.96 Å and 1.20.62 Å. They were merged before use in the structural analysis. The wavelength was 0.6668 Å and the crystal-to-detector distance was 117 mm for both data sets, but the detector was placed at 2
= 0 and 30°, respectively. A scalar value of 474.65 was computed between 11,483 matched reflection pairs in the overlapped resolution range between 1.2 Å and 0.96 Å in the two data sets with an R-merge value of 18.5%, then 18,840 reflections in the low-resolution data set were added to the high-resolution data set by applying the scalar factor. The programs DENZO and SCALEPACK (Otwinowski and Minor, 1997
) were used for data processing. The integration procedures might not be fully optimized due to the ultra-high resolution nature of the data. Some errors might be introduced into the resultant structure factors. Relevant statistical numbers are listed in Table 1.
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The difference Fourier maps calculated at this stage began to show alternate conformations of several residues, and the model was modified accordingly (vide infra). Water molecules were included with a criterion of density level higher than 1.5
in the 2FOFC map. Several cases of split water were also observed. By employing SHELX-97, all hydrogen atoms were explicitly attached to the protein model with idealized geometry. Water molecules, however, were treated as oxygen atoms because the electron density maps did not allow precise identification of their associated hydrogen atoms. Six anisotropic temperature factors were allowed to vary for each nonhydrogen atom. Inasmuch as the protein atoms still assume full occupancies, water molecules were now allowed to refine with fractional occupancies. Using these additional constructs, usually performed for "small molecules" only, the R-values of high-resolution shells were improved significantly, and the refinement could subsequently be extended to 0.62 Å. Most individual nonhydrogen atoms were now seen as discrete spheres in the electron density maps, as shown in Fig. 2.
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For model analysis and comparison, the programs CCP4 (Collaborative Computational Project Number 4, 1994), PROCHECK (Laskowski et al., 1993
), GRASP (Nicholls et al., 1991
), and O were used. Three models from the Research Collaboratory for Structural Bioinformatics (RCSB) Protein Data Bank were used for comparison, including two orthorhombic structures and one monoclinic crystal structure at 1.25 Å, 1.15 Å, and 2.0 Å resolution, with access codes 1MSI, 1HG7, and 1OPS, respectively. The programs ALSCRIPT (Barton, 1993
), BOBSCRIPT (Esnouf, 1997
), MOLSCRIPT (Kraulis, 1991
), Raster3D (Merrit and Murphy, 1994
), and GRASP were employed in producing figures.
| RESULTS AND DISCUSSION |
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55° rotation about the C
C
axis. The side chains of four amino acid residues also show alternate conformations: Glu25, Met30, Met43, and Met56. Examples are presented in Fig. 4. There are three alternate nonhydrogen atoms in Glu25 (CD, OE1, and OE2) and Met56 (CG, SD, and CE), whereas Met30 and Met43 have a single methyl group in alternate conformations. All but two residues (Asn14 and Asn62) have their dihedral angles within the most favored regions as defined by PROCHECK. Both asparagines have the
L-like conformation ([
,
] = [72°, 8°] and [65°, 15°], respectively), which is normally found for a glycine residue in the third position of a type II turn (Richardson, 1981
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The RD1 model has root mean square deviations (RMSD) in bond lengths and angles of 0.012 Å and 2.1° from ideal values. These are typical of well-refined protein structures, despite the ultra-high resolution data used. Deviations of the parameters of the polypeptide chain are also within the normal range from ideal values. However, three residues show unusual geometry. First, the side chain of Leu10 has torsion angles of
1 = 180° and
2 = 300°, which is not favored. It is in contact with a nonpolar patch of Leu19, Ile37, and Pro38 on a symmetry-related molecule. Presumably, crystal-packing interactions of the side chains force Leu10 into such a special conformation (vide infra). Second, the peptide torsion angles of Met21Met22 (
= -165°) and Gln44Val45 (
= 168°) deviate by more than 10° from the ideal planar value. They are probably caused by preferred hydrogen bonds of the carbonyl oxygen atoms of Met21 and Gln44 with the backbone nitrogen atoms of Asn8 and Lys61, respectively. The optimized ON distances of 2.80 and 2.81 Å as well as exact alignment of the hydrogen bonds would be altered if the peptides were more planar.
For distribution analysis, the temperature factors of all atoms are converted to isotropic values (Table 1). Of the 490 nonhydrogen atoms in the protein model, 484 temperature factors are less than 20 Å2, and only six are between 20 and 30 Å2. These include the side-chain atoms CE and NZ of Lys2, OE1 of Glu35, OE2 of Glu36, NE2 of Gln44, and OE2 of Glu64. They are all on the protein surface and facing solvent. The average temperature factor of 530 hydrogen atoms in the model is 7.95 Å2. Seven of them are between 20 and 30 Å2, and three are between 30 and 40 Å2. These correspond to the hydrogen atoms attached to CE and NZ of Lys2, CE of the second conformer of Met30, and NE2 of Gln44. The water molecules have higher temperature factors, inasmuch as most (214) of them are between 5 and 25 Å2, and only six are between 30 and 40 Å2.
Residual electron densities and cavity
After extensive refinement, the R-value did not reduce to less than 10%, as usually required for "small molecule" crystals. This may due in part to scale problems with the disordered bulk solvent, which occupies about a quarter of the solvent space (vide infra). If the data were divided according to resolution, the linear scalar values between the observed and calculated structure factors showed a concave curve with a minimum of 0.959 located in the shell of 1.00.94 Å, whereas at both ends the scalar values were 1.168 and 1.146 for 502.5 Å and 0.640.62 Å shells, respectively. Although a bulk solvent model was employed in SHELX refinement, with the parameters g and U of 0.629 and 6.09, respectively, it seemed insufficient to overcome the scaling problem. On the other hand, although the fully unrestrained refinement was attempted, it did not yield a convergent and geometrically sensible model with lower R-values. It is possible that the full matrix least squares conjugate gradient method is not optimal for this particular case. At this stage of the refinement, it is probably not justified to proceed with the charge-density refinement procedure as yet.
Nevertheless, when the refined model is superimposed on the final FOFC difference Fourier map, some interesting features can be seen. These are probably a consequence of the atomic model used in refinement, which only adopts a spherical or ellipsoidal approach for calculating structure factors and does not take valence electrons and lone pairs into account. In Fig. 5 A, the map for a typical peptide bond is shown. Residual electron densities are seen, particularly about the peptide carbonyl oxygen which is more electronegative than other atoms. In Fig. 5 B, all of the ordered peptide bonds are superimposed and significant features about the oxygen atom come out clearly. In addition to the bond electrons of the carbonyl group, some possible densities for lone pairs of the oxygen atom also become visible. Bond electrons in the other three bonds between C
C, CN, and NC
can also be visualized with certainty. Beyond the C
atom, electron densities for other bonds, including both peptide and side-chain bonds, are concentrated in two regions, corresponding to two favored orientations of the adjacent peptide units.
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level, residual densities are seen for 144 bonds; if it is at 3-
level, 78 have corresponding densities; if it is at 4-
level, densities for only 20 bonds are seen. Of these 20 bonds, 11 belong to methionine and five belong to serine and threonine residues.
In the RD1 molecule there is a cavity that is not occupied by protein or solvent atoms and does not have residual density. It has a volume of 45 Å3 as calculated using GRASP and is surrounded by eight conserved nonpolar residues: Val5, Ala7, Ile11, Leu17, Met21, Met22, Val49, and Leu55, shown in Fig. 6. Such a cavity has not been reported for type III AFP before (Yang et al., 1998
; Antson et al., 2001
). However, in the monoclinic crystal structure (RCSB code 1OPS) a similar cavity of 22 Å3 can also be identified. The absence of a detectable cavity in both high-resolution orthorhombic structures with RCSB codes 1MSI and 1HG7 is probably due to the side chain of Leu55, which has alternate conformations. Apparently the cavity offers Leu55 more space and rotational freedom. Although the precise function of the cavity has not been determined, a possibility is to provide flexibilities of core hydrophobic side chains in the process of protein folding. We are currently making mutants in this region to investigate the effects of various side chains on the stability of RD1.
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41% solvent content (Matthews, 1968
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As mentioned above, all type III AFPs are highly homologous and have identical protein folds. If the RD1 molecule is superimposed on other type III AFPs, the difference in coordinates would be minimal. Upon comparison using the LSQ procedure of O with 1.0-Å matching criterion, the RMSD for RD1 and the 1HG7 models is 0.253 Å between 61 pairs of C
atoms. The RMSD for RD1 and 1MSI models is 0.279 Å between 63 pairs of C
atoms, and that for RD1 and 1OPS is 0.453 Å between 59 atom pairs. The model of 1OPS has larger deviations from other models, probably because it is in a different crystal form and the protein molecules are involved in different lattice contacts (vide infra). It has RMSD from the 1HG7 and 1MSI models of 0.445 and 0.385 Å for 62 and 60 atom pairs, respectively, whereas the RMSD between the latter two models is only 0.241 Å for 64 atom pairs. In addition to the N- and C-terminal ends, the regions of largest deviations are located about residues 2728 and 3839, with C
coordinate differences of
0.8 and 1.2 Å, respectively. These two loop regions are located at the margin of the two homologous motifs (Fig. 1), and are presumably less structurally constrained. In fact, both are involved in lattice contact interactions.
In the monoclinic crystal form, each AFP molecule makes lattice contacts with eight symmetry-related neighbors. Direct interactions are listed in Table 3. The first type of interface (A) involves four residues from each molecule, related by unit translation along the a-axis. It buries 143 and 145 Å2 surface areas on the two apposing molecules. The second type (B1) involves nine and ten residues and buries 385 and 352 Å2 on molecules related by (x,y,z) and (x, 1/2+y, -z); the third type (B2) involves four and two residues and buries 101 and 110 Å2 on molecules related by (x,y,z) and (x, 1/2+y, 1-z), respectively. The fourth type (C) involves five and four residues on molecules related by unit translation along the c-axis, and buries 176 and 208 Å2 surface areas, respectively. The total surface area buried by crystal contact is 1620 Å2 per molecule, which covers
44% of the molecular surface. As seen in Table 3, the side chains of Thr27, Asn28, and Gln39 all participate in specific hydrogen bonds with neighboring molecules.
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All orthorhombic crystal structures of type III AFPs have identical space group (P212121) and very similar unit-cell dimensions. In other words, they are quasi-isomorphous, irrespective of their different amino acid sequences. Nevertheless, the crystals of 1MSI and 1HG7 diffracted x rays to only 1.25 and 1.15 Å resolution, significantly lower as compared with RD1. The Vm and crystal contact areas are not very different and, again, these cannot explain the diffraction results. In fact, the residues involved in direct crystal contact interactions are mostly conserved (Table 2). In the 1HG7 structure, only three residues are different from RD1 in these regions: Arg23 (Lys), Ser24 (Ala), and Arg39 (Lys). Arg23 forms a conserved salt bridge with Asp58, and the CB atom of Ser24 also remains in contact with Pro12 whereas the OG atom is facing the bulk solvent. Arg39, however, makes quite different interactions. In 1HG7, there is a sulfate ion bound to the guanidium group of Arg39, and also to Thr28, Asn46, and Gly62 of two other symmetry-related molecules. In contrast, no sulfate molecule was observed in the RD1 crystal. The side chain of Lys39 in RD1 makes direct contact with Thr28 of a symmetry-related molecule, whereas in 1HG7 there is no such contact, and the side chain of Thr28 has alternate conformations. At interface C of 1HG7, the only direct interaction is between the terminal amino group and the carbonyl oxygen atoms of Arg39 and Val41. In addition, at interface B, the side chain of Leu10 in 1HG7 is not constrained into an unfavored conformation by lattice contact. Similar situations are seen in the 1MSI structure, but there is no sulfate ion and no alternate conformer for Thr28.
As mentioned above, the polypeptide termini of RD1 and the regions near residues 2728 and 3839 show largest RMSD in C
coordinates upon superposition with other models. It is not only because of the intrinsic peptide flexibility for lack of structural role, but also caused by tight crystal packing of the molecule. The more involved interactions at interfaces B and C may account for the superior quality of the orthorhombic RD1 crystal, which diffracts x rays very well and allows data collection at ultra-high resolution.
Solvent model and ice-binding surface
There are 240 water molecules in the refined model, but only 47 are well defined in the electron density maps. These include structural waters that each of them binds to at least one protein atom. An example is shown in Fig. 8 A, where one of the water molecules forms four hydrogen bonds with protein. This water molecule belongs to the first "good" category. The other waters in Fig. 8 A are not as well defined, judged by the lower fractional occupancies, but they still have corresponding densities in the map. These belong to the second "not-so-good" category that includes 122 of the total 240 waters. In Fig. 8 B, some water molecules at crystal contact are shown (and so is Leu10 discussed above). The three RD1 molecules are colored orange, green, and blue. The nature of this interface is nonpolar but five of the water molecules form a pentagon inside the hydrophobic pocket. Six of the eight waters shown here belong to the first category and two belong to the second.
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The remaining 71 of the 240 water molecules did not behave well upon refinement and belong to the third category. They were added according to the residual densities in the bulk solvent region because the presence of these waters somehow reduced both R and Rfree values, but actually do not have corresponding density level of more than 1.5
in the final 2FOFC map. This could be explained by the use of ammonium sulfate in crystallization, which resulted in a dense solvent background. The interstitial volume of solvent corresponds to
24,800 Å3 per unit cell. The 240 water molecules of the refined model occupy 18,000 Å3 (4500 Å3 per asymmetric unit) of the volume, leaving 6800 Å3 (1700 Å3 per asymmetric unit) void volume. Thus, the number of other disordered water molecules not included in the model is probably more than 60, as estimated using the existing solvent model.
When the crystal structure of the type III AFP was first determined (Jia et al., 1996
), it was proposed that the protein binds to ice by formation of hydrogen bonds. Later research suggested that additional interactions with hydrophobic side chains might also play an important role in ice binding (Yang et al., 1998
; Antson et al., 2001
). In Fig. 9, the structures of the IBS residues are compared, and they show minimal deviations from one another. The flat and mostly neutral surface on RD1, as shown in Fig. 10, is supposed to bind to a particular lattice plane of ice, presumably with a similar mechanism proposed by Jia et al. (1996)
, Yang et al. (1998)
, and Antson et al. (2001)
. The ice-binding surface of RD1 is composed of 11 residues, which are shown in Fig. 11 A. In the crystal structure of RD1, there are 44 ordered water molecules near the IBS, shown in Fig. 11 B. These are all within 4.0-Å distance from the ice-binding residues, including Gln9, Leu10, Pro12, Ile13, Asn14, Thr15, Ala16, Thr18, Ile20, Met21, and Gln44, and have corresponding densities of more than 2-
level in the final 2FOFC map. In cases of split waters, averaged coordinates are used. If they are superimposed on the 1HG7 model, 28 of the 44 waters have equivalents within 1.0 Å distance. If the matching criterion is 0.5 Å, 14 waters still have equivalents in both models. Among the 28 water molecules, 19 waters make 22 well-defined hydrogen bonds with the protein, including 17 bonds with backbone atoms and five bonds with the side-chain atoms of Gln9, Asn14, and Thr18. The remaining nine equivalent waters and the 16 unmatched waters are bound to other water molecules, which form a cage-like structure, as shown in Fig. 11 A. Similar results are obtained if the 1MSI model is used, with 22 pairs of water molecules matched by 1.0 Å distance. However, if the 1OPS model is compared, only six equivalent waters are found. They bind to the backbone atoms of Leu10, Ala16, Leu17, Ile20, and Leu51, and the side chain of Gln9. The distribution of these water molecules appears to be sporadic and featureless, and probably unrelated with any ice structure.
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| CONCLUSION |
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In summary, the structural refinement of biological macromolecules at such an ultra-high resolution is complex and challenging. Our results here illustrated that more work needs to be done to reach a satisfactory conclusion, not the least including: i) ample synchrotron beam time to collect many more data sets using newer generation of detectors and data processing protocols, ii) testing different refinement programs, and iii) treatment of imperfect models (bulk solvents, multiple conformers, etc.). This new work will be carried out in the future.
| ACKNOWLEDGEMENTS |
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This work was supported by grant NSF OPP 99-09841 to A.L.D. and C-H.C.C. from the National Science Foundation, United States, and grant NSC 90-2321-B-001-015 to A.H-J.W. from the National Science Council, Republic of China.
Submitted on June 10, 2002; accepted for publication September 25, 2002.
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