Abstract

Granules isolated from the snail Helix aspersa and the shore crab Carcinus maenas have been studied by using scanning electron microscopy, powder X-ray diffraction and solid-state nuclear magnetic resonance (NMR). These amorphous deposits are largely based on pyrophosphate (P$\_{2}$O$\_{7}{}^{4-}$) and orthophosphate (PO$\_{4}{}^{3-}$) respectively. NMR indicates that water is evenly distributed throughout the pyrophosphate granules and that the PO$\_{4}{}^{3-}$ ions occupy distorted lattice sites. The $^{1}$H NMR spectra of the orthophosphate granules of desiccated and normal deposits indicate that water can move in and out of these solids. This movement is probably facilitated by the organic component, identified by $^{1}$H-$^{13}$C NMR, particularly in the crab granules. The distorted lattice, the presence of hydrated ions and the interactions with the organic matrix probably account for many of the properties of these solids and are relevant to the interpretation of their biological significance.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.