The Influence of Carbonates in Parent Rocks on the Biological
Properties of Mountain Soils of the Northwest Caucasus Region

K. Sh. Kazeev, M. A. Kutrovskii, E. V. Dadenko, L. S. Vezdeneeva,
S. I. Kolesnikov, and V. F. Val’kov

Southern Federal University, ul. Bol’shaya Sadovaya 105/42, Rostov-on-Don, 344006 Russia

E-mail: kazeev@sfedu.ru

Received March 21, 2008

Abstract—The biological activity of different subtypes of soddy-calcareous soils (rendzinas) of the Northwest
Caucasus region was studied. In the Novorossiisk–Abrau-Dyurso region (dry subtropics), typical soddy-calcar-
eous soils with the high content of carbonates predominate; in the more humid conditions of the Lagonaki Pla-
teau (Republic of Adygeya), leached soddy-calcareous soils carbonate-free down to the parent rock are spread.
The number of microarthropods, the populations of fungi and bacteria, and the enzyme activity (catalase, dehy-
drogenase, and invertase) testify that the biological activity of these soils significantly differs. In the typical
soddy-calcareous soils of the dry subtropics, the content of carbonates does not affect the characteristics men-
tioned; in the more humid conditions of the West Caucasus region, the presence of carbonates in the parent
rocks intensifies the biological activity of the soddy-calcareous soils.

DOI: 10.1134/S1064229312030052


Pleiades Publishing home page | journal home page | top

If you have any problems with this server, contact webmaster.