From a hydrological point of view, active caves are a series of connected conduits which drain water through an aquifer. Water tends to choose the easiest way through the system but different geological and morphological barriers act as flow restrictions. The number and characteristics of restrictions depends on the particular speleogenetic environment, which is a function of geological, geomorphological, climatological and hydrological settings. We present some theoretical background of open surface and some possible scenarios.
COBISS.SI-ID: 27826221
In caves microorganisms inhabit distinct habitats where they develop various interactions. As an evidence of microbial activity several features can be identified. Microorganisms are involved both in lithogenic and litholitic processes. Besides heterotrophs in caves autotrophic organisms can be also expected. Especially bacteria, as the most diverse group, offer immense biotechnological and bioremediation potential.
COBISS.SI-ID: 28262189