В № 20 «Записок ИИМК РАН» публикуются научные исследования, представленные на российскофинляндском симпозиуме «Торговля, обмен и взаимовлияния в доисторическое время и средневековье/ историческое время». В разделах «Новейшие открытия и разработки ИИМК РАН» и «Из истории науки» представлены статьи Н. Ф. Соловьёвой и А. В. Полякова, посвященные полевым открытиям на Йылгынлы-депе в Южном Туркменистане и анализу данных радиоуглеродного датирования фёдоровской культуры на Енисее, а также работа С. О. Ремизова, обобщающая информацию об изучении памятников каменного века Волгоградской обл.Издание адресовано археологам, культурологам, историкам, музееведам, студентам исторических факультетов вузов.The 20 th issue of the "Transactions of IHMC RAS" contains the Proceedings of the Russian-Finnish Symposium "Trade, Exchange and Contacts in Prehistory and in the Medieval/post-Medieval Times". The sections "Newest discoveries and developments" and "From the history of science" present the papers by N. F. Solovyova and A. V. Polyakov devoted to field discoveries at Ilgynly-depe in South Turkmenistan and to the analysis of radiocarbon dates obtained for the Fyodorovo culture on the Yenisei river, respectively, as well as the work by S. O. Remizov who summarizes the information about the Stone Age sites of the Volgograd oblast.The volume is intended for archaeologists, culturologists, historians, museum workers, and students of historical faculties.
The Sukhaya Mechetka is the most important Middle Paleolithic site in the Eastern Europe. The paper presents the analysis of the section, including its cultural layer, in the context of stratigraphy and paleogeography of the Lower Volga River region. The structure of the section represents 11 main stages of sedimentation and paleogeographic evolution of the site territory, which are closely related to global and regional changes in the climate and the level of the Caspian Sea. The base of the section reflects the stage of a river existence on the territory of the site that flowed into the Volga River estuary, formed by the Early Khazarian transgression of the Caspian Sea at the end of the Middle Pleistocene (MIS 6). A long continental period of evolution under multi-directional climate fluctuations of different amplitudes from the Mikulino interglacial (MIS 5e) till the Late Valdai glacial epoch (MIS 2) is reflected in the middle part of the section. The Late Khazarian and Hyrcanian transgressive basins (MIS 5), as well as the Paleo-Khvalynian stage (MIS 3) of the Caspian Sea did not reach the latitude of Sukhaya Mechetka. The stage of Early Khvalynian transgression (MIS 2, 16 190 ± 200 years ago) during the degradation of Ostashkovo glaciation is expressed in the upper part of the section. Three paleosoils have been found that reflect the warming periods of the MIS 5 stage and are related to its 5e, 5c and 5a sub-stages. The middle paleosoil contains a cultural layer assigned to the Micoquian/KMG community of Northern Eurasia. The climate was moderately warm during the Neanderthal settlement of the territory, steppe landscapes dominated the interfluve, and the forests grew in the balka. The Hyrcanian transgression of the Caspian Sea with an estuary in the Volga River valley predetermined a high erosion basis and the formation of a balka with a wide bottom and gentle banks. A permanent fresh watercourse attracted mammals which were an object of hunting for ancient men. All this, obviously, became a basis for the organization of settlement in the Sukhaya Mechetka balka. Correlation of the section with detailed studied loess-soil sections of the Lower Volga River region makes it possible to determine the age of its cultural horizon in between 97-110 thousand years ago.
The locations of the Stone Age on the Volgograd region territory have been known since the beginning of the XIX century. However, purposeful Stone Age sites explorations had only started after the Sukhaya Mechetka site was discovered by A.P. Koptev and M.N. Grischenko in 1951. The data accumulated on series of stratified sites in Volgograd Region makes it possible to outline two significant groups of them. One of the groups belongs to the Lower Volga basin. The other group is associated with the ramified network of gullies and ravines and multiple tributaries of the Don. The Don is the fourth longest river on the Russian Plain; its basin taken in the Volgograd Region is several times larger than the Volga basin taken in the area. The relatively flat landscape of the Don plain, saturated with small rivers, gullies and ravines, as well as stone raw materials available for mining, have been creating favorable conditions for human habitation since the Middle Paleolithic. The well-known Paleolithic and Mesolithic sites are found both in the watersheds and in the floodplain-terrace areas of the Middle Don. The near-mouth section of the Kurmoyarsky Aksai river – the Don tributary in Kotelnikovo District – and the surroundings of Kremenskaya village in Kletskaya District are standing out in terms of being studied. The stone industry detected in the lower layers of the multilayered site Schlyakh indicates that the Don plain was inhabited by people during the Middle to the Upper Paleolithic transition. The prospects of further searches for Stone Age sites in the Middle Don Basin had already been proven by the discovery of at least forty sites in previous decades. Further archaeological research will help to discover new stratified sites with impressive collections of stone and bone items, which will make it possible to draw analogies with synchronous sites in the territories adjacent to the Volgograd region.
The Sukhaya Mechёtka site, located on the northern outskirts of Volgograd, has attracted the attention of Paleolithic researchers since its discovery in 1951 by geologists A.I.Koptev and M.N. Grishchenko. The materials of the site - a collection of stone products currently kept at the MAE RAS, and chronostratigraphic information – can be considered as perfect by standards of open Paleolithic complexes. To a large extent, the site acquired such a significance due to the presence of the only one perfectly preserved cultural layer, which lies in clear stratigraphic conditions. Being densely overlapped with thick deposits, the site was preserved so well that it remained unaffected by the turbulent natural processes of the last glacial-interglacial macrocycle. Single-layer sites usually have a disadvantage comparing to multi-layer complexes in terms of the importance level of the tasks solved with their help. But the Sukhaya Mechёtka favorably differs from other sites by the measure of cultural layer being studied in the field and the potential for further studies. The stone assemblage and field documentation archives created by M.Z. Panichkina and S.N. Zamyatnin show a picture of the life of Middle Paleolithic hunters settlement taken at limited time interval. It is confirmed by preliminary results of planigraphic and technological analyzes performed with use of refitting. Sukhaya Mechёtka is a practically intact echo of an individual Neanderthal community’s life, as far as it’s possible for archaeological material of this age. However, the matter of the site’s chronology, and the time period of Sukhaya Mechёtka layer formation being determined in particular, are not completely resolved. The representations of the middle of the last century based on geological observations (Mikulino) need to be verified. The C14 dating method showed obviously an inadequately young age. OSL dating results are expected to be gained in the future.
In 2021, the Lower Volga Paleolithic research team of the IAET SB RAS, participating in the Interdisciplinary Lower Volga Expedition organized by the IIMK RAS, the study of the Sukhaya Mechetka Middle Paleolithic site located in the northern outskirts ofVolgograd City was continued. The research was aimed at studying the chronostratigraphic position of the cultural layer and reconstructing the paleoclimate during the Neanderthal habitation period. In 2021, an additional geological section was established to the west of the buffer zone of the excavation area to study the stratigraphy of the right-side slope of the Sukhaya Mechetka gully. In 2021 the upper part of SM 14-18 (SМ East) stratigraphic sequence has been completely excavated (26 m thick). The new SM West stratigraphic sequence was established in 155 m westwards. Preliminary correlation of the layers and paleosol horizons in these two profiles was carried out. Samples for palynological, micromorphological, physicochemical and phytholithic analyses with the purpose to correlate the two sequences have been collected. Sediments were sampled for OSL dating. Studies of the buried paleosol are extremely important for understanding the dynamics of the climatic changes during the cultural layer accumulation at Sukhaya Mechetka. Pedogenetic levels that have been revealed in 2021 are comparable to the buried paleosol identified at the site earlier in depths, continuity and features of pedogenesis. Texturally graded buried paleosol described here for the first time for the SM West sequence expand our understanding of the soil spatial inhomogeneity, and, consequently, conditions of human habitation. Results of the ongoing field investigation will allow determining the cultural-chronological position of Sukhaya Mechetka in the context of the Eastern and Central European Middle Paleolithic complexes for the first time.
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