In order to examine the effects of chemical composition on thermal expansion in the pyroxene mineral group, X-ray diffraction data have been collected from room temperature to ~925 °C on a chemically diverse group of thirteen pyroxenes, including four orthorhombic and nine monoclinic samples. Additionally, resulting unit-cell volumes computed from the XRD data have proven to be good tests for a large number of thermal expansion models; the physical model by Kroll and coworkers and the empirical one by Fei have been found to be especially useful. Modeling also has allowed the connection of present data, collected at temperatures above 25 °C, to the volume data of other workers for much lower temperatures, well below 0° C, and also extrapolation of values for volume and thermal expansion well beyond the measurement range. We have found for orthopyroxenes that Fe 2+-Mg 2+ substitution has little effect on thermal expansion coefficients for volume. For clinopyroxenes, however, greater thermal expansion occurs in Ca 2+-(diopside, augite, hedenbergite, johannsenite) than in Li +-(spodumene) or Na +-bearing members (jadeite, aegirine, kosmochlor). Present data support the observation that differences in volume thermal This is the peer-reviewed, final accepted version for American Mineralogist, published by the Mineralogical Society of America. The published version is subject to change. Cite as Authors (Year) Title. American Mineralogist, in press.