“…We can mention the measurements of 1) natural single crystals of olivine Mg 1.8 Fe 0.2 SiO 4 in the UV-mid-IR spectral range at temperatures from 300 to 1700 K (Shankland et al, 1979) and olivine Mg 1.8 Fe 0.2 SiO 4 and enstatite MgSiO 3 in the mid-IR range at temperatures from 10 to 973 K (Zeidler et al, 2015), 2) oxides, such as Al 2 O 3 , MgAl 2 O 4 , and SiO 2 , in the mid-IR range from 300 to 900 K (Zeidler et al, 2013), 3) silicon in the UV-VIS range from room temperature up to 800 K (Weakliem and Redfield, 1979;Jellison and Modine, 1994) , 4) amorphous magnesium silicate smokes (Hallenbeck et al, 1998) and amorphous Mg-rich pyroxene particles (Brucato et al, 1999) embedded after annealing at temperatures between 1000 and 1300 in KBr pellets and measured ex situ in the mid-IR spectral range, and crystalline silicates produced by high-temperature (~1000 K) annealing of amorphous silicates, such as MgSiO 3 , Mg 2 SiO 4 , and Fe 2 SiO 4 (Fabian et al, 2000;Roskosz et al, 2011;Sabri et al, 2014). Having in mind possible carbon-rich exoplanetary atmospheres (Helling et al, 2017), it is worth to mention also high-temperature measurements of carbonaceous species, such as hydrogenated amorphous carbon films (Chou, 1992), diamond-like carbon films (Akkerman et al, 1996;Cheng et al, 1997), and nano-crystalline carbon in silicon oxycarbide (Rosenburg et al, 2018).…”