Abstract. Thermal transformations of kaolinite of different degree of crystallinity have been monitored by 27A1 and 298i high-resolution NMR with magic-angle spinning (MAS NMR), X-ray diffraction, Fourier transform infrared, atomic absorption spectrophotometry and thermogravimetric analysis. NMR shows differences in the dehydroxylation process of kaolinites with different degree of crystallinity and reveals the presence of short-range order in metakaolinite. 29Si NMR spectra acquired with a 30 s recycle delay of poorly and highly crystalline samples heated at 480 and 500 ~ C, respectively, contain three distinct signals; we discuss their assignment in the light of experiments involving leaching of the samples with aqueous KOH. Ca. 40% of Si sites retain their original Q3 symmetry just above the onset of dehydroxylation and the Q4 environment is present showing that a small amount of amorphous silica has already segregated. The spectrum of samples treated at 1000~ C contains a signal at -110 ppm (from Q* silicons) and a faint resonance, from mullite, at ca. -87 ppm.298i NMR also shows that cristobalite germs are already present at 950-1000 ~ C. The 27A1 MAS NMR spectra of metakaolinite reveal the presence of 4-, 5-and 6-coordinated A1. Changes in the three A1 populations as a function of temperature have been monitored quantitatively. Below 800 ~ C, 4-and 5-coordinated A1 appears at the expense of 6-coordinated A1, but above 800 ~ C the amount of 6-coordinated A1 increases again. We suggest a dehydroxylation scheme which accounts for the presence of 4-and 5-coordinated A1. Above 900-950~ C the latter signal is no longer present in the 27A1 NMR spectra and new 4-and 6-coordinated A1 species (mullite and 7-alumina) appear. We propose new ideas for the structure of metakaolinite.