“…Below 100 °C, DTA curves showed an endothermic peak weakly indicating low amounts of absorbed water. The occurrence of otavite was confirmed by a broad endothermic peak between about 370 and 460 °C due to the decomposition of CdCO 3 into CdO under atmospheric pressure [ 73 , 74 ]. In the same temperature range the polyenes’ decomposition also occurred [ 67 , 75 ].…”