<p>Paleomagnetic measurements provide very important methods to study the evolution of and variations in the Earth&#8217;s magnetic field throughout time. A vital tool used in paleomagnetism are natural magnetic minerals, such as the titanomagnetite (<em>TM</em>) solid solution series (Fe<sub>3-<em>x</em></sub>Ti<em><sub>x</sub></em>O<sub>4</sub>, 0 &#8804; <em>x</em> &#8804; 1). The main source of magnetic information in <em>TM</em>s is the thermal remanent magnetisation (<em>TRM</em>) they retain whilst being cooled below their Curie temperature (<em>T<sub>C</sub></em>) during their formation.</p><p>The key factor determining the <em>T<sub>C</sub>&#160; </em>is the composition. However, recent studies on natural and synthetic TM powders [1,2,3] have shown that their <em>T<sub>C</sub>&#160; </em>is also heavily influenced by their thermal history. Annealing various natural and synthetic <em>TM</em> powders at temperatures between 300&#176;C and 425&#176;C for timescales of hours to months resulted in changes in their <em>T<sub>C</sub>&#160; </em>of up to 150&#176;C.</p><p>The accuracy of many paleomagnetic measuring techniques, such as geomagnetic paleointensity estimates and paleomagnetic paleothermometry, depends on the exact knowledge of the Curie temperature. Changes in <em>T<sub>C</sub>&#160; </em>of such a considerable extend could deeply impact those techniques or even render them doubtable. So far, vacancy-mediated chemical clustering at the octahedral site of the <em>TM</em> structure has been postulated as the mechanism causing this phenomenon [2,3]. To further investigate the underlying processes, we synthesised a large (~6.5 mm diameter;&#160; ~27 mm length) <em>TM</em> single crystal using an optical floating zone furnace. Via SEM-EDX techniques it was established that the crystal was homogenous over its whole length with a composition of&#160; Fe<sub>2.64</sub>Ti<sub>0.36</sub>O<sub>4</sub>. Using a Physical Properties Measurement System (<em>PPMS</em>) the Curie temperatures of several pieces of the crystal were determined after different annealing treatments. For the first time it has been possible to detect systematic changes in <em>T<sub>C</sub>&#160; </em>with annealing in a <em>TM</em> single crystal.</p><p>Additionally within the scope of this project it was possible to determine the relationship between the extend of change in <em>T<sub>C</sub>&#160; </em>and the microstructure for polycrystalline samples.</p><p>&#160;</p><p>[1] Bowles, J. A., Jackson, M. J., Berqu&#243;, T. S., Solheid, P. A. and Gee, J. S. (2013), Nature Communications, 4, 1916. https://doi:10.1038/ncomms2938</p><p>[2] Jackson, M. J., and Bowles, J. A. (2018), J. Geophys. Res., 123, 1-20. https://doi:10.1002/2017JB015193</p><p>[3] Bowles, J. A., Lappe, S.&#8208;C. L. L., Jackson, M. J., Arenholz, E., & van der Laan, G. (2019). Geochem. Geophy. Geosy. 20. https://doi.org/10.1029/2019GC008217</p>