In the biomineralization process, a number of Pro‐rich proteins participate in the formation of three‐dimensional supramolecular structures. One such protein superfamily, the Pro,Gly‐rich sea urchin intracrystalline spicule matrix proteins, form protein–protein supramolecular assemblies that modify the microstructure of the inorganic mineral phase (calcite) within embryonic sea urchin spicules and adult sea urchin spines. These proteins represent a useful model for understanding Pro sequence usage and the resulting generation of extended or “open” structures for protein–protein and/or protein–crystal recognition. In the sea urchin spicule matrix protein, SM50 (Strongylocentrotus purpuratus), there exists an unusual 20‐residue Pro,Asn‐containing repeat, PNNPNNPNPNNPNNPNNPNP, which links the upstream 15‐residue C‐terminal domain and the downstream 211‐residue β‐spiral repeat domain. To define the structural preferences of this 20‐residue repeat, we created a 20‐residue N‐ and C‐terminal “capped” peptidomimetic of this sequence. Using far‐uv CD dichroism, CHα and α‐15N conformational shifts, 3JNH‐CHα coupling constants, sequential dNN(i, i + 1) rotating frame nuclear Overhauser effect connectivities, dαN(i, i + 1)/dNN(i, i + 1) intensity ratios, amide temperature shift coefficients, amide solvent exchange, and simulated annealing refinement protocols, we have determined that this 20‐residue repeat motif adopts an extended “twist” structure consisting of turn‐ and coil‐like regions. These findings are consistent with previous studies, which have shown that Pro‐rich tandem repeats adopt extended, flexible structures in solution. We hypothesize that this 20‐residue repeat may fulfill the role of a mineral‐binding domain, a protein–protein docking domain, or as an internal “molecular spacer” for the SM50 protein during spicule biocomposite formation. © 2000 John Wiley & Sons, Inc. Biopoly 54: 464–475, 2000