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Статья посвящена вопросу территории расселения "крайне южных селькупов".
Монография посвящена исследованию обжитого нарымскими селькупами пространства на разных уровнях его проявления: освоенная территория проживания, пространство поселения, пространство внутри и около жилища.
Kniha vyšla v Moskvě roku 1967 / The book was published in Moscow in 1967 / Книга была издана в Москве в 1967 году.
В статье дан анализ топонимов (названий поселений), упомянутых Г. Миллером в 1740 г. на р. Шудельке, и сделаны выводы относительно расселения локальных групп селькупов в бассейне этой реки.
Спелеология и спелестология. №1
Гаршин Д.И., Долотов Ю.А., Неходцев В.А. Обзор верхней части Среднепронского спелестологического района (на границе Тульской и Рязанской областей) // Спелеология и спелестология. – Набережные Челны. 2022. №1: 114-125THE MID-PRONYA SPELESTOLOGICAL REGION UPPER PART OVERVIEW (ALONG THE TULA AND RYAZAN REGIONS BORDER) In July, 2021 the Tethys caving club surveyed an area in the upper reaches of the Pronya, along the Tula and Ryazan regions border. An underground limestone quarry fragment, found near Osanovo village, is described in this paper along with the area around it. A brief overview of underground quarrying nearby and spelestological zoning are also proposed. Early Carboniferous limestones were mainly mined in the described part of the Pronya valley. Based on historical facts, the authors consider that the quarries could not exist in the Pronya upper reaches until the late 17th – early 18th centuries. The limestone quarrying was started with large construction works of 17th century defensive structures, the Ivanovsky canal and the Tula Arms Plant in the 18th century and continued with cement plants working in the late 19th century. According to known sources, only rather small peasant quarries producing limestone for local needs, existed in the described territory until the early 20th century. The Osanovskaya-1 underground cavity is a small chamber, remained from a large limestone mine, most part of which was destroyed by open-pit quarries near Osanovo village. Keywords: Quarries, Oka limestones, the Pronya valley upper reaches, the Osanovskaya-1 mine fragment
Archaeological Sites of the Dniester Region / Археологические памятники Приднестровья
L. V. Subbotin, S. N. Razumov, V. S. Sinika. Semyonovka Barrows / Л.В. Субботин, С.Н. Разумов, В.С. Синика. Семёновские курганы2017 •
This book contains a presentation and analysis of materials obtained during archaeological study of barrows near Semyonovka village, Belgorod-Dnestrovsky district, Odessa region. The value of these sources lies in the breadth of prehistoric and historical cultures of the region that existed in this territory from the Early Bronze Age to the Sarmatian time. The book is meant for archaeologists, historians, university professors and students, and anyone interested in the ancient history of the region. Работа посвящена публикации и анализу материалов, полученных в результатеархеологических исследований курганов у с. Семёновка Белгород-Днестровскогорайона Одесской области. Ценность этих источников заключена в широте охватадоисторических и исторических культур региона, существовавших на этой территории от раннего бронзового века до сарматского времени. Для археологов, историков, этнографов, преподавателей вузов и студентов, а также всех, кто интересуется древней историей края.
St. Petersburg 2012
Процесс культурогенеза начальной поры позднего бронзового века Волго—Уральского региона (вопросы хронологии, периодизации, историографии). Самара
Основные этапы развития щитковых псалиев Северной Евразии (в соавт. с Кузнецов П.Ф.)2014 •
Для Западно-Сибирской равнины характерно широкое распространение больших меандрирующих палеорусел позднеледникового возраста. Они обнаружены во всех ландшафтных зонах, кроме тундры Ямала. На востоке равнины ширина позднеледниковых рек превосходила ширину современных русел в 2–3 раза, в центральной части – в 3–5 раз. В бассейнах Тобола и Ишима это соотношение достигало 10/1. Основной причиной формирования столь крупных рек была значительная сезонная неравномерность стока с максимальными расходами воды, превышающими современные.
The paper is a response to recent claims that the materials of Susiluola (Wolf cave) in Finland and Byzovaya in the northern Urals in Russia should be regarded as Middle Paleolithic and are thus indicative of the Neanderthal presence near the polar circle. The first-hand examination of the material from Susiluola leads to the conclusion that it does not contain any indisputable artifacts. As to Byzovaya, the old and widely held view that it is an Early Upper Paleolithic assemblage seems to fit the available archaeological and chronometric evidence much better than a recently proposed hypothesis of the Middle Paleolithic status of the site. The authors suggest that the archaic appearance of the Byzovaya typology and technology may rather be due to a specific function of this site, situated in direct proximity to a mammoth cemetery. Like the other sites of the kind (Shestakovo, Yana), it could have been devoted (at least partly) to the exploitation of mammoth remains (corpse dismembering, tusk extraction and initial processing, etc.).
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