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N.L. Gerbilsky’s Scientific School of Ecological Histophysiology: on the 125th anniversary of his birthday
80 years ago, two biologists in the USSR, simultaneously and independently, began researching the mechanisms of hormone production by nerve cells, i.e., the processes of neurosecretion. These were L.B. Levinson from Moscow State University, who was engaged in cytochemical studies of neurosecretion in insects and amphibians, and N.L. Gerbilsky from Leningrad State University (LSU), who studied the structure of two parts of the fish brain (hypothalamus and pituitary gland), and the functions of their hormones (neurohormones) to regulate the processes of vital activity of the body and its adaptation to changing environmental conditions. This fundamental research area worked alongside major foreign scientific schools of neuroendocrinology, E. and B. Sharer, R. Collin, R. Gauppa, B. Hanstra, G. Russi, and M. Mosinger. The work was also of applied importance, in particular, under the leadership of N.L. Gerbilsky, the role of hypothalamic and pituitary hormones in migration and spawning processes in bony and sturgeon fish, who were threatened with extinction due to the start of the construction of hydroelectric power plants in the 1920–1930s. This scientific field has revealed the relationship between the morphofunctional organization of the nervous, endocrine and reproductive systems in animals and ecological features of their species and was called “ecological histophysiology”. The result of N.L. Gerbilsky’s research was the development of a technique for obtaining hormones produced in the fish brain and then injecting them to other individuals to stimulate their reproductive processes in the practice of fish farming. The purpose of this article is to show the contribution of N.L. Gerbilsky and his students to the development of biotechnical methods for managing migration behavior and spawning in bony and sturgeon fish species.
SILICATIZATION OF CULTURAL LAYER SOILS IN ARCHAEOLOGICAL EXCAVATIONS
The preservation and in situ museumification of archaeological objects of stratigraphic sections of cultural layer soils, whose value depends on the integrity and intactness, is a complex and underdeveloped problem. This is due to some specific properties of these soils, such as the heterogeneity of soil composition both vertically and horizontally; the diversity of inclusions, the uneven compressibility of the strata, the ability to self-compact from their weight, changes in hydrogeological conditions, soil soaking and the decomposition of organic inclusions. As a result, these soils are the most unfavorable in artificial stabilization. In the study, a wide range of soils of the cultural layer from various places with stabilization plans were examined. Our analysis of the deposits made it possible to separate these soils by geochemical features which have the highest impact on the intensity of the chemical solution’s interaction processes with the mineral component of the soil.
This chemical solution is in a family of silicate compositions with surfactants of the amide class. These organic liquid glass hardeners activate the skeletal part of the soil and provide the complete mobilization of the main cementing substance (silica gel). Pilot tests of various modifications of organo-silicate solutions were carried out at the sites of Chersonesos (Sevastopol), Tanais (Rostov region), Moscow, etc. The soils ranged from sandy to loamy with various inclusions (building stone, ceramics, bones, fish scales, shells, ash, soot, plant roots, etc.). Soil stabilization was carried out by injecting chemical solutions of various densities with the use of vertical and horizontal injections. An important finding of the work was that forming a new soil mass with improved properties was determined by the composition, properties of the soil and injection solutions, the distance from the injector and the depth of the stabilized area.
For the first time in Russia, at the center of Moscow, it was possible to preserve the soil mass in situ of the cultural layer of the 16–17th centuries and exhibit it for 32 years to visitors in the underground archaeological museum.