Sea urchin spines are porous, single crystal Mg-rich calcite [(Mg, Ca)(CO3)
] with a three dimensional meshwork architecture. The crystallographic orie
ntation of large (similar to 10 cm in length) spines from Heterocentrotus t
rigonarius was determined using the X-ray back-reflection Laue technique; t
he long axis of all spines is parallel to the [00.1] direction of calcite.
The internal structure was studied using SEM and TEM. The macropore structu
re dominated the SEM images, whereas many small (similar to 80 nm) protein
occlusions can be observed within the single crystal spines using TEM. The
spines appeared crystallographically perfect in the TEM. The bend strengths
of a group of spines were also determined and varied between similar to 13
and 41 MPa. (C) 2000 Kluwer Academic Publishers.