Shungite is a new variety of natural carbonaceous rocks with carbon content (98-20%) depending on the particular deposit (Chebolaksha, Maksovo, Nigozero, Shunga, Zazhogino) in Karelia (Russia) [1]. The occurrence of the natural С 60 and С 70 fullerenes was proved first for Shungite [2]. Fullerene type formations from single C 60(70) to globules of ~10 nm in size were reported in this material. Disordered multilayer carbon globules of ~10 nm make separate elements supplemented in Shungite with the uniformly distributed SiO 2 , metal oxides, mica and other admixtures [3]. The supramolecular structure of the totality of the globules changes in the samples of different deposits, however, the main features of the carbon units remain unchanged [3]. The interest in Shungite stems from the possibility of its use in industry and medicine [1].The studies of the physical properties of Shungite are at the beginning stage [4,5], however, the specific features of this material have been already recognised. The first measurements of the magnetic susceptibility yield an intriguing result [6]: in Sh-I (98% of carbon) the change in χ d was similar to that corresponding to the appearance of superconductivity at 95 K in the fullerenes doped with Сu 2+ [7]. In this article we report the first EPR study of Shungite samples (Sh-III, 55-25% carbon and Sh-IV, 25-5%). The observed spectra definitely confirm the presence of electrical conductivity characteristic of metals, however, the properties of Shungite differ from both those of metals and those of graphite (and fullerenes). We have studied the Shungite samples from two deposits (Sh-III and Sh-IV). EPR measurements were carried on an X-band RADIO-PAN spectrometer in the 300-4.2 K temperature range.For the Sh-III sample of ∼3 × 1 × 0.5 mm 3 size a relatively week signal of the Dyson shape [8] was observed (Fig. 1a). It was characterized by the asymmetry parameter a/b varying from 2.40 to 2.25 depending on the angle between the constant magnetic field direction and the sample surface. At the same time, changes in the linewidth were insignificant, and ∆В eff was equal 1.99 ± 0.04 mT. After the sample grinding, the signal intensity increased more than ten times and became absolutely symmetric (∆В = 1.82 ± 0.05 mT; g-factor = 2.0019 ± 0.0002; Fig. 1b). Measurements of the fine-ground sample degassed in vacuum 2 × 10 -6 mm Hg on heating up to 200 °С, showed that the molecular oxygen usually adsorbed on the surface crystallites did not affect the EPR signal, as it was observed sometimes in a variety of graphites and carbon blacks [9].The temperature dependence of the EPR signal of Sh-III was studied both for powder and for the bulk sample. (Na + ) have been found in Sh-IV. Analysis of the EPR spectra has been made taking into consideration the properties of the conductive materials such as metals and graphite.