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The Hateg basin, South Carpathians, Romania, contains a thick sequence of Maastrichtian continental deposits from which a rich dinosaur an mammal fauna is known. Field data as well as mineralogical and stable isotope analyses from three representative profiles were integrated in order to reconstruct environmental conditions during Maastrichtian time. Tu tea quarry is characterized by the presence of well drained calcisols, with smectite (montmorillonite) as the main clay component. Along the profile, the delta(18)O and delta(13)C isotopic compositions of calcretes show a small variation, of up to 0.9 parts per thousand. The profile along the Barbat Valley shows preponderantly calcisols, the main clay mineral being smectite, with subordinate illite and chlorite. The oxygen isotopic compositions of calcretes are similar to 0.5 parts per thousand lighter than those from Tu tea. The soils are interpreted as having formed under more humid conditions and they are similar to those situated at the bottom of the sequence developed along Sibisel Valley. The abundant smectite from the Tustea and Barbat Valley deposits, as well the presence of good developed soils, reflects palaeoenvironmental conditions predominantly controlled by climate. Preliminary magneto stratigraphic data along the Sibisel Valley section indicate that sedimentation started at the end of chron C32n. All other palaeomagnetic sites distributed upstream, as far as the upper limit of this formation, have only reversed polarity and the corresponding time interval is probably chron C31r, Along this valley, the sequence shows a general coarsening upward trend. The palaeosol type changes from calcisol- to vertisol-dominated sequences. The soils are moderate to weakly developed. The mineralogical composition of the clay fraction also changes, from smectite- to illite and chlorite-dominated. These features points towards unstable tectonic conditions and higher uplift rates of the surrounding area within chron C31r. Towards the top of the sequence, the oxygen and carbon isotopic composition of calcretes become 1 and similar to 2 parts per thousand lighter, respectively. These changes indicate a transition from generally semi-arid towards more humid and possible cooler conditions and correlate with the worldwide trend for chron 31r.