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. 2012 Feb 16;109(10):3699-3704. doi: 10.1073/pnas.1109243109

Fig. 1.

Fig. 1.

Fracture surfaces of a sea urchin spine shown at different magnifications under SEM (A)–(D). The spine was fractured perpendicular to its growth direction which corresponds to the crystallographic c-axis. Note: (C) is area bounded by white box in (B) and (D) is area bounded by white box in (C)