Based on some previously unpublished archival materials, the biography of Lecturer at Kazan University S.I. Limanova-Kolosova (1899–?), a little-known Russian microbiologist, was restored for the first time. Seraphima Ivanovna Kolosova (née Limanova) was born in the family of a veterinarian and received a natural science education at Kazan University. Since the beginning of the 1920s, she started working at the Botanical Laboratory under the guidance of Professor A.P. Ponomarev, who at that time was actively developing the microbiological lead. The works of S.I. Limanova-Kolosova were devoted to analysis of the microflora of various reservoirs in Tatarstan and neighboring regions. Her research was accompanied by lectures on general microbiology, aquatic and soil micro biology, technical microbiology and fermentation physiology. The scientific works of S.I. Limanova-Kolosova have allowed microbiological topics to take root within the walls of Kazan University and gave a further impetus to the development of this lead.

May of 2026 marks the 150th anniversary of the outstanding biologist and geo­grapher, theorist and historian of science, Academician, Moscow University graduate Leo S. Berg (1876–1950), who became famous during his life as the greatest ichthyologist in our country. He published numerous papers with descriptions of single fish species, as well as general monographs on the ichthyofauna of our country and its regions. He also focused on fishing, domestic aquaculture and zoogeographical zoning by ichthyofauna. The article discusses L.S. Berg’s research on palaeontology, which began during his expeditions to the Aral Sea in 1899–1906. He studied the Meso-Cenozoic deposits of the Aral coastline and their fossil fauna. Since the 1930s, Leo Berg continued his palaeoichthyological research, studying in detail the Late Paleozoic, Mesozoic and Cenozoic actinopterygian and other fishes. He described a number of fossil taxa of ichthyofauna and critically revised the system of fossil agnathans and fishes. The article provides brief biographical information of L.S. Berg, one of the classics of world ichthyology in the 20th century.

This study establishes the authorship of the geological term “eluvium” and traces its evolution in geological and soil sciences. It confirms the priority of H. Trautschold (1817–1902) as the original author of this term, supported by analysis of his works from the 1870s. The term was first introduced by him in 1872. The article demonstrates that the modern interpretation of the term “eluvium” shows a high degree of correlation with H. Trautschold’s classical definition. The development of the concept of eluvium and ideas about eluvial processes is traced through the works of prominent Russian soil scientists – N.M. Sibirtsev, V.V. Dokuchaev, V.I. Vernadsky, B.B. Polynov, V.R. Williams, and N.P. Remezov. V.V. Dokuchaev systematized the concept of eluvium into a coherent framework: definition of eluvium → eluvial processes → stages and phases of eluvial rock transformations. He emphasized that “although these products are sometimes altered beyond recognition of the parent rock which they originated from, a genetic connection between them always persists.” Particular significance lies in the incorporation of the biogeochemical aspect into the concept of eluvium through the works of N.P. Remezov, who established biological accumulation of elements exceeding their removal during eluvial processes. This allowed eluvium formation to be viewed not as a purely abiotic process but as a phenomenon involving living organisms. The article reveals the historical continuity of scientific ideas in the hypothesis of the origin of the Russian Plain: H. Trautschold → V.V. Dokuchaev → B.B. Polynov → V.A. Kovda. H. Trautschold was the first to propose that the Russian Plain formed from deposits lying on top, which were influenced for millennia by atmospheric precipitation, initiating the concept of eluvial origin of plains. This idea was later reflected in the works of V.V. Dokuchaev and B.B. Polynov, and subsequently in V.A. Kovda’s hypothesis regarding the fluvioglacial origin of the Russian Plain. Our analysis confirms that the term “eluvium” is a fundamental concept uniting geology, geomorphology, geochemistry, and soil science, and its evolution reflects the advancement of understanding regarding the genesis of surface deposits and soils.

Having started his biogeochemical studies in 1916, V.I. Vernadsky revealed that the generally accepted opinion about the origin of life from inert matter had no scientific sources. But all data of biology and paleontology indicate that all life comes from life (Francesco Redi’s principle). Vernadsky found convincing evidence of biogenesis in the state of biological space–time, which allowed him to describe the biosphere as a planetary shell, actually forming other geospheres. Vernadsky’s concept of the planetary role of living matter is currently gaining overriding and fundamental importance for all Earth sciences.

The problem of atmospheric electric field disturbances during geomagnetic field variations still has no clear solution. The article analyzes available data from magnetometers and atmospheric electricity stations during the supersubstorm of April 5, 2010, which developed against the background of a moderate magnetic storm (/Dst/ ~ 80 nT). Comparison of fluxmeter and magnetometer data has shown unexpectedly strong variations in the vertical electric field Ez with a range of up to several hundred V/m (“electric storm”) during intense magnetic disturbances. Although the Ez disturbance observed worldwide roughly coincided with the magnetic storm, the coherence between the geomagnetic and electrical variations and the electrical variations between themselves was low. This event does not fit into modern concepts of atmospheric electric field disturbances by ionospheric currents.

The old hypothesis by Academician V.I. Vernadsky of the biosphere being a geological force to build the surface and immediate interior of our planet is indirectly supported based on statistical data. According to occurrence data on findings of all known animal specimens and according to some characteristics of the tectonic activity of the Earth, the presence of several previously unknown cycles shortening from cycle to cycle (approx. By a factor of 1.51) over about a billion years, is substantiated. This leads to an idea of a cause-and-effect relationship between these two different categories of cycles. The influence of tectonics on biota, to one degree or another, has long been known. However, due to the mentioned cycles being rather accelerated, it is difficult to imagine that such strong acceleration in the tectonic cycles could arise due to some intra-tectonic causes, whereas the accelerated nature of biotic evolution due to some intrabiotic causes is quite possible. So, a conclusion arises of the mentioned contracting tectonic cycles being modulated by biota. Possible mechanisms of such influence are hypothesized, their clarification requiring additional research. This conclusion is revolutionary for geology and reveals biotic evolution’s previously unknown role as an active creator of global tectonic (cyclic) processes at a new, quantitative level, which is also revolutionary for evolutionary biology. But, regardless of these conclusions, the mentioned decreasing cyclicity is of interest itself, for the first time (statistically) speaking about the accelerated nature of evolution over such vast time periods.

The ecological status of the city of Moscow was assessed using two test kits, namely, a display based on luminescent bacteria and a lichen photobiont indicator. The toxicity of tree bark in lichen ecotops was estimated by a biotest method. Changes in the cell diameters of lichen photobionts were evaluated. Evidence has been obtained of a permanent detrimental effect of chronic contamination on the specific community of the lichen test system used and possible recent contamination by the use of our bacterial luminescence test system.

A new three-stage method for assessing the CO₂ balance in plant communities was formulated. The methodology includes not only taking into account the absorption of C-CO₂ during plantation vegetation, but also the processes occuring when using wood. In managed forests, when calculating the carbon balance, it is necessary to take into account the release of CO₂ not only at direct, but also at indirect consumption of technical energy for laying plantations, caring for them, and felling for final use. As a model, the consumption of technical energy in cultivating natural and genetically modified forms of aspen Populus tremula L. was calculated. The large role of indirect expenditure of technical energy in the C-CO₂ balance in forest plantations is shown. The use of a genetically modified clone of aspen significantly increases the productivity of plantations and CO₂ absorption from the atmosphere compared to its natural form. On a long time scale the final amount of CO₂ runoff from the atmosphere depends not only on the area of forests and their productivity, but also on the way of using wood. There is a highly effective way of using forest plantations to regulate the carbon dioxide content in the atmosphere, which is currently little paid attention, namely, the so-called substitution effect. Replacing energy-intensive materials (reinforced concrete, plastic, metal, and brick) with wood may be one of the main ways for the positive impact of forests on the CO₂ content in the atmosphere. The use of wood biomass from thinning, wood processing wastes, short-rotation forests for heat and power generation is a great reserve for replacing fossil hydrocarbons. The forest area needs to be expanded to increase wood production to replace energy-intensive building materials and generate biofuels.