[On the similarity in the effects of different cryopreservation conditions on the growth and development of plants].

The morphological characteristics of 35 wild plant species were studied after freezing of seeds under the conditions of deep, fast, and programmed freezing (-196 degrees C) and non-deep freezing (-10 degrees C). The seeds were stored frozen for a month. The seeds of all the species were characterized by a low humidity.

[Effect of freezing of seeds on the morphological characteristics of four pink species].

The effect of non-deep freezing (-10 degrees C) and deep freezing (-196 degrees C) on the morphological characteristics of four pink species was investigated. It was shown that the growth and development of plants after cryopreservation changed insignificantly. Rather stable characteristics (diameter of flower, the number of cauline nodes, and root length) did not change.

[The investigation of the influence of cryopreservation and inbreeding on the variability of morphological characteristics of the evening-primrose biennial (Oenothera biennis L.)].

The effect of deep freezing of seeds at -196 degrees C (-320.8 degrees Fahrenheit) and inbreeding on the morphological characteristics of the evening-primrose biennal (Oenothera biennis L.), such as the size of plant parts and the amount of fruits, cauline nodes, and generative and vegetative shoots was investigated.

[The possible contribution of late pleistocene biota to biodiversity in present permafrost zone].

During the last decade a wide range of biological objects, which have preserved their viability for tens and hundreds of thousands of years, was found in the samples of permafrost sediments from North-East Eurasia. Among them are bacteria, fungi, algae, moss spores, seeds of higher plants, protists. Along with physiological mechanisms of cryoconservation and constant low temperature of great importance for long-term preservation of biological objects in permafrost layers are ways of burying the organisms and conditions that prevail before the transition of sediments to the permafrost state.