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Problemy Osvoeniya Pustyn' (Problems of Desert Development) (4):42-48.
Volgograd (Stalingrad): Vserossijskij Naučhno-Issledovatel'skij i Institut Agrolesomelioracii (VNIALMI), 13 pp.
Genetic diagnostics of paleosols are based on the morphology of soil profiles, on the combination of the stable properties of microstructure and on the mineral composition of soils (taking into account diagenetic transformations).
As a result of spatial paleopedological reconstructions performed both at a level of the structure of soil cover (study of paleosols in the catena) and at the zonal-provincial level allowed to compile soil maps of Eastern Europe for the Mikulino Interglacial (125 ka BP), the Bryansk Interstadial (32 to 24 ka) and the Holocene climatic optimum (5.5 ka).
Geologie en Mijnbouw (Netherlands Journal of Geosciences) 91(1-2):111-128. Comptes rendus hebdomadaires des Séances de l'Académie des Sciences, Paris, Série II, 303(11):1025-1027.
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Vestnik sel'skokhoziaistvennoi nauki: ezhemesiachnyi nauchnyi zhurnal Ministerstva sel'skogo khoziaistva Kaz SSR (7):33-38. Parabeldünen am Wadi Howar; Besiedlung und Klima in neolithischer Zeit im Nordsudan (Parabolic dunes of Wadi Howar: settlement and climate in Neolithic period in northern Sudan). (in German)Gabrieli, J., Cozzi, G., Vallelonga, P., Schwikowski, M., Sigl, M., Eickenberg, J., Wacker, L., Boutron, C., Gäggeler, H., Cescon, P. Atmospheric Environment 45(3):587-593, doi:10.1016/j.atmosenv.20Gabrielli, P., Barbante, C.
