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Table 1. The temporary and spatial variability of microbial communities in<br />

paleosols and modern surface soils.<br />

Burial places Aksay 1 Abganerovo 2 Malyaevka 2 Kolobovka 2<br />

Microbial biomass*<br />

MS 546 406 107 35<br />

PS 16-112 20-42 11-19 0.4-3<br />

Quantity of MS 66 57 17 44<br />

microorganisms** PS 8-48 4-47 7-10 25-27<br />

MS 74 58 66 70<br />

Populations of SA<br />

PS 74-97 21-58 28-66 69-77<br />

microorganisms<br />

MS 8 15 4 6<br />

of different NA<br />

PS 0-8 18-36 4-32 6-8<br />

trophic<br />

groups***<br />

MS 18 35 30 24<br />

RM<br />

PS 4-18 25-61 25-43 16-28<br />

MS – modern soil, PS – buried soil<br />

1 – chestnut soil,<br />

2 – light-chestnut soil<br />

SA – soil agar, NA – nitrite agar, RM – rich medium<br />

* - µg C/g soil ** - million cells/g soil, *** - %<br />

It should be noted, that pedogenesis reconstructions obtained on the base of<br />

microbiological methods are in full accord with those obtained with the help of<br />

traditional morphological-genetic analysis of the soils. Moreover, being more<br />

sensitive to soil-forming condition changes, the data of microbial community state<br />

allows to specify and work out in detail the morphological-genetic analysis data.<br />

Acknowledgements. This research was supported by the Russian Foundation for Basic<br />

Research and the Program of Presidium of RAS for Basic Research (directive 4)<br />

REFERENCES<br />

1.<br />

2.<br />

3.<br />

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E.R.M. (1997) Variability of Radiocarbon Ages of Individual Organic Compounds<br />

from Marine Sediments. Science. Vol.277. 796-799.<br />

Brockman F.J., Kieft T.L., Fredricson J.K., Bjornstad B.N., Shu-mei W. Li,<br />

Spangenburg W., Long P.E. (1992) Microbiology of Vadose Zone Paleosols in South-<br />

Central Washington State. Microbial Ecology. 23. 279-301.<br />

Marphenina O.E. Gorbatovskaya E.V. Gorlenko M.B. Microbial characteristics of<br />

cultural layers in medieval Russian archaeological sites. Pochvovedenie. 2001. Vol.70.<br />

855-859.<br />

45

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