Tachycitin, a 73-residue polypeptide having antimicrobial activity is present in the hemocyte of horseshoe crab (Tachypleus tridentatus). The first three-dimensional structure of invertebrate chitin-binding protein was determined for tachycitin using two-dimensional nuclear magnetic resonance spectroscopy. The measurements indicate that the structure of tachycitin is largely divided into N- and C-terminal domains; the former comprises a three-stranded beta-sheet and the latter a two-stranded beta-sheet following a short helical turn. The latter structural motif shares a significant tertiary structural similarity with the chitin-binding domain of plant chitin-binding protein. This result is thought to provide faithful experimental evidence to the recent hypothesis that chitin-binding proteins of invertebrates and plants are correlated by a convergent evolution process.

The backbone resonance assignments have been completed for the apo (¹H and ¹⁵N) and calcium‐loaded (¹H, ¹⁵N, and ¹³C) regulatory N‐domain of chicken skeletal troponin‐C (1–90), using multidimensional homonuclear and heteronuclear NMR spectroscopy. The chemical‐shift information, along with detailed NOE analysis and ³J_HNHα coupling constants, permitted the determination and quantification of the Ca²⁺‐induced secondary structural change in the N‐domain of TnC. For both structures, 5 helices and 2 short β‐strands were found, as was observed in the apo N‐domain of the crystal structure of whole TnC (Herzberg O, James MNG, 1988, J Mol Biol 203:761–779). The NMR solution structure of the apo form is indistinguishable from the crystal structure, whereas some structural differences are evident when comparing the 2Ca²⁺ state solution structure with the apo one. The major conformational change observed is the straightening of helix‐B upon Ca²⁺ binding. The possible importance and role of this conformational change is explored. Previous CD studies on the regulatory domain of TnC showed a significant Ca²⁺‐induced increase in negative ellipticity, suggesting a significant increase in helical content upon Ca²⁺ binding. The present study shows that there is virtually no change in α‐helical content associated with the transition from apo to the 2Ca²⁺ state of the N‐domain of TnC. Therefore, the Ca²⁺‐induced increase in ellipticity observed by CD does not relate to a change in helical content, but more likely to changes in spatial orientation of helices.

Antifreeze proteins (AFPs) are found in organisms ranging from fish to bacteria, where they serve different functions to facilitate survival of their host. AFPs that protect freeze-intolerant fish and insects from internal ice growth bind to ice using a regular array of well-conserved residues/motifs. Less is known about the role of AFPs in freeze-tolerant species, which might be to beneficially alter the structure of ice in or around the host. Here we report the 0.95-Å high-resolution crystal structure of a 223-residue secreted AFP from the snow mold fungus Typhula ishikariensis . Its main structural element is an irregular β-helix with six loops of 18 or more residues that lies alongside an α-helix. β-Helices have independently evolved as AFPs on several occasions and seem ideally structured to bind to several planes of ice, including the basal plane. A novelty of the β-helical fold is the nonsequential arrangement of loops that places the N- and C termini inside the solenoid of β-helical coils. The ice-binding site (IBS), which could not be predicted from sequence or structure, was located by site-directed mutagenesis to the flattest surface of the protein. It is remarkable for its lack of regularity and its poor conservation in homologs from psychrophilic diatoms and bacteria and other fungi.