Connecting caddisworm silk structure and mechanical properties: combined infrared spectroscopy and mechanical analysis
The underwater silk of an aquatic casemaking caddisfly larvae ( Hesperophylax occidentalis) is viscoelastic, and displays distinct yield behaviour, large strain cycle hysteresis and near complete recovery of its initial strength and stiffness when unloaded. Yield followed by a stress plateau has been attributed to sequential rupture of serial Ca 2+ -cross-linked phosphoserine (pS) β-domains. Spontaneous recovery has been attributed to refolding of the Ca 2+ /pS domains powered by an elastic network. In this study, native Ca 2+ ions were exchanged with other metal ions, followed by combined mechanical and FTIR analysis to probe the contribution of pS/metal ion complexes to silk mechanical properties. After exchange of Ca 2+ with Na + , the fibres are soft elastomers and the infrared spectra are consistent with C v3 symmetry of the – groups. Multivalent metal ions decreased the – symmetry and the symmetric stretching modes ( v s ) split in a manner characteristic of ordered phosphate compounds, such as phosphate minerals and lamellar bilayers of phosphatidic acid lipids. Integrated intensities of the v s bands, indicative of the metal ion's effect on transition dipole moment of the P–O bonds, and thereby the strength of the phosphate metal complex, increased in the order: Na + < Mg 2+ < Sr 2+ < Ba 2+ < Ca 2+ < Eu 3+ < La 3+ < Zn 2+ < Fe 2+ . With a subset of the metal ion series, the initial stiffness and yield stress of metal ion-exchanged fibres increased in the same order: establishing the link between phosphate transition dipole moments and silk fibre strength.