Topics Covered Courtesy of Science/AAAS QUASI INSIDE This millimeter-sized fragment revealed a mix of minerals, including khatyrkite and cupalite that contain quasicrystalline grains.

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In the 25 years since quasiperiodic crystals were first proposed to exist, scientists have observed and studied more than 100 examples of these oddly ordered materials. All of them were synthesized in laboratories—until now.

An international research team has found a quasicrystal in a naturally occurring mineral sample originating in Russia (Science 2009, 324, 1306). The finding broadens the range of natural atomic structures and could provide clues that lead scientists to synthesize new kinds of quasicrystals.

Quasicrystals are ordered solids that lack periodicity, meaning their structures cannot be depicted by a geometric pattern of atoms that repeats in three dimensions at fixed intervals—a description of ordinary crystals. Typically built from multicomponent alloys, quasicrystals often exhibit five- or 10-fold rotational symmetry, a condition that's theoretically forbidden in conventional crystallography.

After years of searching, Luca Bindi of the Museum of Natural History, in Florence, Italy, and Princeton University's Paul J. Steinhardt and coworkers Peter J. Lu and Nan Yao discovered fivefold symmetry in micrometer-sized quasicrystal grains in samples of khatyrkite and cupalite. The Al-Cu-Fe-based mineral specimens in the Florence museum are reported to have come from the Koryak Mountains in Russia.

"Only because of Luca's stubborn determination and willingness to test every part of the sample was the quasicrystal found. It's a miracle, really," Steinhardt says.