EarthRef.org Reference Database (ERR) -- Podkovyrov et al. 1998

The Karatau Group of the Southern Urals furnishes an opportunity to reveal the C-isotopic composition for the major part of the Upper Riphean in a single type succession comprising, according to radiometric and paleontological evidence, both the lower and upper horizons of this unit (1000 +/- 50-650 +/- 20 Ma). In the studied sections, the group is dominated by carbonate deposits, which in terms of cathodoluminescent, geochemical and isotopic-geochemical data can be considered insignificantly altered and retaining the primary C-isotopic signature. Limestones of the lower Katav Subformation, lowermost in the carbonate succession of the group, show the descending trend of delta(13)C values from 4.4 down to -0.8 parts per thousand PDB, whereas limestones of the upper Katav Subformation and the lower part of the overlying lower Inter Subformation demonstrate the ascending trend up to 3.9 parts per thousand with three positive excursions. The upper part of the lower Inter limestones is characterized by low positive values of delta(13)C and the upper Inter limestones, by the low negative values. Limestones and dolomites of the overlying Min'yar Formation display the largest for the Karatau Group range of delta(13)C variations from -2.2 to 5.9 parts per thousand with four peaks. The Uk Formation limestones, which terminate the Karatau carbonate succession, show again the low positive values of delta(13)C. Variations of delta(13)C in the Karatau Group are basically consistent with the general Upper Riphean trend. However, contrary to other Upper Riphean sections, the Karatau Group is devoid of long intervals characterized by high (>6 parts per thousand) values and demonstrates much smaller delta(13)C range. These distinctions may be due to significant stratigraphic hiatuses in the Karatau carbonate succession.