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ý.,,: V. ý ýý . - Nottingham eTheses - University of Nottingham

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(INA+ phenotype) bacteria are the most temperature-effective natural ice nuclei after ice<br />

itself (which nucleates at 0°C under standard conditions (Yank<strong>of</strong>sky et al., 1997)). There<br />

are a large number <strong>of</strong> other naturally occurring ice nucleators including detritus (Upper &<br />

Vali, 1995), spider silk (Murase et al., 2001) and soot particles (Gorbunov et al., 2001).<br />

The INA+ phenotype has been identified in three Gram negative genera: Erwina,<br />

Pseudomonas and Xanthomonas. The protein itself is homologous between the genera,<br />

forming a beta-helical structure which could interact with water through the repetitive<br />

TXT motif (Graether & Jia, 2001). Water molecules are arranged into an ice-like array as<br />

the membrane bound heteronucleator (INP) acts as a template that mimics the structure <strong>of</strong><br />

ice. INA+ bacteria are generally epiphytic and are <strong>of</strong>ten ubiquitous in agriculturally<br />

important crops. They play a significant role in causing frost damage by promoting ice<br />

formation at a higher temperature than would occur if normal super cooling temperatures<br />

(-4°C to-12°C) were allowed to occur, accounting for an excess <strong>of</strong> $1 billion in crop<br />

injury in the United States per year (Edwards et al., 1994). As a result <strong>of</strong> this, much<br />

research has been performed to elucidate the mechanism behind ice nucleation in an<br />

effort to control or prevent crop damage by these bacteria. Research into crop protection<br />

led to the marketing <strong>of</strong> a number <strong>of</strong> commercial products including those used in the<br />

prevention <strong>of</strong> frost (FrostbanTM), manufacture <strong>of</strong> snow (Snomax®), reduction <strong>of</strong> the<br />

incidence <strong>of</strong> fire blight (Blightban®) and as an aid for food concentration and texturing<br />

(Skirvin et al., 2000). For a comprehensive review <strong>of</strong> the history <strong>of</strong> ice nucleation and<br />

nucleation function please refer to Skirvin et al. (2000).<br />

1. S. 3.4 -<br />

Antifreeze proteins<br />

1.5.3.4.1- AFP structure and function<br />

Ice-nucleating proteins induce ice formation but anti-freeze proteins inhibit ice<br />

formation, and in some cases have been shown to inhibit the action <strong>of</strong> INPs (Parody-<br />

Morreale et al., 1988). Anti-freeze proteins (also known as thermal hysteresis proteins)<br />

are a structurally diverse class <strong>of</strong> proteins, which all have the ability to bind to the surface<br />

<strong>of</strong> ice and inhibit its recrystalisation (Yeh & Feeney, 1996; Davies & Sykes, 1997;<br />

Smaglik, 1998). They act at the surface <strong>of</strong> ice by lowering the freezing point below the<br />

melting point (Davies & Sykes, 1997; Knight & DeVries, 1994; Haymet et al., 1998), a<br />

10

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