2024 marks the 140th anniversary of the beginning of the expeditions of the laboratory of the Botanical Garden of Moscow University under the supervision of Professor Ivan Nikolaevich Gorozhankin to study the Central Russian flora. The historical and scientific context of the studies of this traditional object for the Botanical Garden of Moscow University during the 18th – early 21st centuries is traced. It is shown how the long-term targeted field research by the staff of the laboratory of the Botanical Garden has contributed to a methodologically unified approach to the organization of the program for studying the flora of the Oka River basin allowed not only to expand the territorial coverage, going beyond the purely Moscow region, but also to significant contribute to the development of an important scientific problem, namely, the cognition of the phenomenon of the Oka River flora. Gorozhankin’s principle of systemic research of regional flora was successfully implemented at the end of the 20th century by scientists of the Botanical Garden of Moscow University in the study of the flora of Central Russia.

At the end of the 1960s a movement began for the preservation of Earth's biosphere — the common home for humanity and the receptacle of all life on Earth. This movement united the scientific communities of various countries for many years. 20 years later, at the International Symposium “Biosphere and Humanity. History and Modernity” the development and promotion of the ideas of Academician V.I. Vernadsky, the founder of the Earth’s Biosphere doctrine, were summed up.

The article continues the author’s series of publications on global Holocene activation. The research was carried out on the interface between geology and meteoritics within the context of the Earth pulsating expansion model, whereby the Earth began to evolve in a compression mode in the late Pleistocene. At the Pleistocene – Holocene boundary, the Earth was subjected to a massive pummeling of large asteroids and changed its orbit, moving closer to the Sun. From this time on, the compression increased sharply, crustal processes intensified causing an upsurge of continental orogeny, and global transgression intensified. Astroblemes are considered as constituents of the host geological systems. They are indicators of the onset of the Holocene activation. Evidence is presented of most of the known astroblemes being formed at the Pleistocene – Holocene boundary by a single stream of asteroids. Using astroblemes in South Africa and Eurasia as examples, their relationships were studied with Holocene orogenic systems – with their tectonics, volcanism, fluid dynamics, and drainage network. The global Holocene activation is shown to significantly change the natural environment, thereby triggering an unprecedented explosion in the development of human civilization.

The article, based on materials from the Moscow State University Archives, examines the activities of the Botanical Garden of Moscow University during the Great Patriotic War (1941–1945). Using a systematic approach, the article traces changes in the main parameters of the Botanical Garden’s structural and functional organization under the influence of adverse external factors. It is shown how, in the context of the crisis caused by the war, which led to a shortage of resources for scientific activities, the areas of research and educational work were transformed, and the composition and structure of the Botanical Garden’s plant collections, as well as the number and organizational structure of its scientific and auxiliary staff, changed. Special attention is paid to the personality of K.I. Meyer, who headed the Botanical Garden in 1940–1948.

The results of our research conducted at the junction of geology, speleology and archeology are presented. Every cave is considered as an integral part of the enclosing geological system. Representative examples show the nature of the interrelationships of caves with structures of the continental crust of Eurasia, Africa and North America. The research was performed within the framework of the pulsationally expanding Earth model. According to this model, at the Pleistocene–Holocene turn, our planet was bombarded by a stream of asteroids, after which it switched to a pulsed compression mode, with a sharp activation of orogeny at the Holocene beginning. At that time, caves with their Paleolithic–Neolithic cultural layers were deformed. Their deformations are considered as Holocene activation indicators.

The article traces milestones of the formation and development of sciadography in the Botanical Garden of Moscow University in the 19–20th centuries in the aspect of the history of science. In accordance with the logic of the development of scientific know­ledge, taxonomic ideas about the Umbelliferae were transformed as research methods improved. Studying of the Umbelliferae became a specialty of the Botanical Garden of Moscow University. The evolution of approaches to the construction of the system of this family of angiosperms is considered: from G.F. Hoffmann’s artificial system (early 19th century), based on comparative morphological data, to B.M. Kozo-Polyansky’s natural system (early 20th century), based on the principles of evolutionary morphology, and further, to phylogenetic systematics based on modern research methods and quantitative methods of data processing. This approach was developed by V.N. Tikhomirov and M.G. Pimenov, their colleagues and students (since the 1970s). January 2025 marks the 265th anniversary of the birth of G.F. Hoffmann (1760–1826) and the 135th anniversary of the birth of B.M. Kozo-Polyansky (1890–1957).

In the year of the 150^th anniversary of the famous Russian scientist Vladimir A. Barykin (1874–1939), an attempt is made to reconstruct the initial period of his scientific activity. Based on the documents from the State Archive of the Russian Federation and published sources, the pre-revolutionary stage in the life and work of V.A. Barykin is considered. The professional path of the scientist, his first scientific research, as well as participation in the Russian-Japanese and World War I are recreated. And although the flourishing of his scientific and organizational activities took place in the 1920s and 1930s, the pre-revolutionary period of his life was extremely busy with expeditions and research, becoming significant for the formation of a professional scientist and the definition of those research areas that he would develop later. The fruitful scientific activity of the scientist was interrupted in 1938, when he was arrested, and in 1939 he was shot during the repressions. Despite the rehabilitation of V.A. Barykin in 1955, no detailed publications about his life and scientific activity have appeared. This article attempts to fill in this research gap and honor the memory of the prominent Russian scientist in his jubilee year.

New data on the placoderm fish Plourdosteus livonicus (Eastman, 1896) from the Lower Frasnian deposits of the Mikhaylovsky Mine in the Kursk Region is described. These remains are currently housed at the Earth Science Museum of Lomonosov Moscow State University. The medio-dorsal plate from this locality allows reconstructing its form and proportion, as also early unknown anterior division of the bone. Only small fragments of medio-dorsal plates were formerly described and figured for P. livonicus from this and other localities in European Russia. So, the new data from the Mikhaylovsky Mine adds to the morphology information of this species. The medio-dorsals are of diagnostic significance and distinguish in the plourdosteids. The specimen from the Earth Science Museum’s collection is compared with the medio-dorsal plates of other Frasnian Plourdosteus species from the East-European platform.

The article discusses the results of our preliminary studies of Paleocene columnar stromatolites from the “Kamyshinskie Ushi” location, near the northwestern periphery of the town of Kamyshin. The morphology, composition and features of the buildings were studied. They can be attributed to the morphological type of columnar non-branching stromatolites; fan-shaped branching stromatolites are less common; their mineral composition differs little from the host rocks and consists mainly of quartz grains cemented by silicon oxide. Dark layers are much more saturated with ore inclusions. The concentration of chromium, molybdenum, wolfram, vanadium, cobalt and nickel in dark varieties increases noticeably, which confirms their stromatolite origin. The deposition settings of their formation remain controversial.

The exposition of the department "Natural Zones" in the Earth Science Museum of Moscow State University (25th floor, halls Nos 18–20) presents 15 full-scale exhibits of dry 3D fragments of biogeocenoses, namely: spotted tundra; forest tundra; swamps: flat-hummocky tundra, oligotrophic upland and mesotrophic lowland sedge; spruce-green grass; grass-grass and tipchak-grass steppes; subtropical mountain forest; alpine meadows; semi-deserts; deserts – clay, wormwood-solyanka and ilak belosaksaulnik on ridge sands; and savannas. These exhibits demonstrate the interaction of the main natural components characteristic of the respective climatic conditions (soils, flora, and fauna). The article gives a description of the animal species represented in the exposition based on a visual examination of zoological exhibits and a study of their nomenclature and taxonomic changes.

The article describes two groups of facies most widely represented in the collections of Lower Frasnian invertebrates of the Main Devonian Field in the Mining Museum (hardgrounds and pelecypod banks). The presence of three types of hardgrounds has been established, differing in the nature of the original bottom and the time of exposure of each hardground, and hence structural and textural features of rocks and systematic composition of oryctocenoses. The first type is crinoidal limestone with an extensive complex of sclerobionts and traces of bioerosion by Trypanites Mägdefrau, an uneven surface and a visually almost complete absence of impregnation. In hardgrounds of this type, three generations of sclerobionts are distinguished, namely: abiogenic substrates (first), incrustators of the remains of organisms of the first generation (second), and bioerosion organisms (third). The second type is micritic limestone with a smooth glass-type surface, a small complex of sclerobionts and traces of bioerosion by Trypanites Mägdefrau. The third type is pelecypod limestones with an uneven surface, isolated sclerobionts, numerous traces of bioerosion by Trypanites Mägdefrau and strong ferruginous impregnation. For the most widespread hardgrounds of the first type, the presence of specific taphofacies has been established, characterized by good preservation of organic remains of the first generation, an almost complete absence of organic remains of the second generation, and a complete absence of bioerodible organisms. The appearance of such taphofacies is due to the short exposure time of the hardground and the beginning of a rapid process of new accumulation immediately after the appearance of the first organisms of the second generation. The presence of such taphofacies emphasizes the importance of distinguishing taphofacies in certain paleofacies and certain types of oryctocenoses. In the oryctocenoses of pelecypod shells, three morphological and ethological types of cornulitids have been established. The most representative settlements of cornulithids were characteristic of calcareous clay soils with small areas of compacted bottom.

As part of MSU’s Strategic Development Programme, the Youth Museum initiative is currently under development as a mobile-network project. The project consists of a system of interacting nodes, comprising a central site on the MSU campus and a network of regional subdivisions. The proposal suggests the use of mobile field museum exhibitions as an effective mechanism of interaction. In recent years, the aforementioned system was experimentally tested within the “Flotilla of Floating Universities” scientific and educational expedition. This project comprises a set of interrelated research, educational, training, artistic, and other projects. The direct and active involvement of students and schoolchildren led to the development of creative methods for the traveling exhibitions «Ancient Lukomorye» and «Living Matter in Geospheres», as well as to the methods of joint empirical and information gathering for the development of central and regional «Youth Museum» clusters. Materials were collected to create pilot versions of exhibitions, educational collections and the launch of interactive platforms at Tambov State Technical University: «Cretaceous Beach» («Palaeoecological Sandbox»), «Page of the Stone Chronicle» («Dissecting Table of a Beginner Palaeoecologist»), and others. These exhibitions are designed to ensure that they can be used effectively in educational and outreach activities on a wide range of topics. Students and schoolchildren will have the opportunity to conduct small-scale individual and collaborative research projects of varying levels of complexity using the platform format.

The concept of biogeocenoses as structural units of the biosphere is reflected in the exposition of the department “Natural Zones” (Halls No. 18–20 on the 25^th floor) of the Moscow State University Museum of Earth Science: the interaction of the main natural components characteristic of the corresponding climatic conditions – soils, flora and fauna – is succinctly demonstrated. There are 15 full-scale exhibits of dry volumetric fragments of biogeocenoses: spotted tundra; forest tundra; swamps: flat-hummocky tundra, oligotrophic upland and mesotrophic lowland sedge; spruce-green grass; grass-grass and tipchak-grass steppes; subtropical mountain forest; alpine meadows; semi–deserts; deserts – clay, wormwood-solyanka and ilak belosaksaulnik on ridge sands; and savannas as well.

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.