Pub Date : 2022-12-30DOI: 10.34078/1814-0998-2022-4-94-103
A. Lebedintsev
The article presents results of archaeological survey conducted by G. A. Pytlyakov, the Lecturer of the Yakut State Pedagogical Institute, in the Oymyakonsky District of Yakutia in 1955. The works under discussion resulting in the discovery of materials related to the Yakut first-settlers in the territory: remains of balagan-type housing structures, traces of urasa-type temporary portable dwellings, ground burials, and petroglyphs. It has been noted that the economy and material culture of the Upper Indigirka Yakuts had a number of features determined by harsh natural conditions of the region. An opinion has been expressed that, in the past, the Oymyakon yakuts were not engaged in cattle breeding, as their settlements were located in the places neither convenient nor suitable for cattle breeding. It has been assumed that the Ingigirka basin may have a certain potential for searching other petroglyphs.
本文介绍了雅库特国立教育学院讲师G. A. Pytlyakov于1955年在雅库特奥伊米亚孔斯基区进行的考古调查的结果。讨论中的工作导致发现了与该地区第一批雅库特定居者有关的材料:巴拉干式房屋结构的遗迹，urasa式临时移动住宅的痕迹，地面埋葬和岩画。已经指出，上英迪吉尔卡雅库特的经济和物质文化具有该地区恶劣的自然条件所决定的若干特点。有一种意见认为，过去奥伊米亚康雅库特人不从事养牛，因为他们的定居点位于既不方便也不适合养牛的地方。据推测，Ingigirka盆地可能具有寻找其他岩画的潜力。
{"title":"Археологические исследования Г.А.Пытлякова в Оймяконском районе Якутии","authors":"A. Lebedintsev","doi":"10.34078/1814-0998-2022-4-94-103","DOIUrl":"https://doi.org/10.34078/1814-0998-2022-4-94-103","url":null,"abstract":"The article presents results of archaeological survey conducted by G. A. Pytlyakov, the Lecturer of the Yakut State Pedagogical Institute, in the Oymyakonsky District of Yakutia in 1955. The works under discussion resulting in the discovery of materials related to the Yakut first-settlers in the territory: remains of balagan-type housing structures, traces of urasa-type temporary portable dwellings, ground burials, and petroglyphs. It has been noted that the economy and material culture of the Upper Indigirka Yakuts had a number of features determined by harsh natural conditions of the region. An opinion has been expressed that, in the past, the Oymyakon yakuts were not engaged in cattle breeding, as their settlements were located in the places neither convenient nor suitable for cattle breeding. It has been assumed that the Ingigirka basin may have a certain potential for searching other petroglyphs.","PeriodicalId":341033,"journal":{"name":"Bulletin of the North-East Science Center","volume":"117 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-12-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"116237426","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-12-30DOI: 10.34078/1814-0998-2022-4-10-23
A. S. Biakov
The article discussed the duration of existence and the rate of formation for Permian bivalve species and genera in Northeast Asia. It has been established that the species existed averagely for 2-5 million years; and the genera, for 10-20 million years. The vast majority of long-lived taxa characterize the Early Permian (Asselian-Middle Artinskian) assemblages. The proportion of long-lived species that existed for over 10 million years exceeds 25 % of all bivalve species existing on this stage. Since the end of the Artinskian (and even more so since the Kungurian), the number of relatively short-lived species increased significantly. The possible reason for this phenomenon might have been an increase in the frequency of manifestation of geobiospheric, mainly extinction (Biakov, 2012a), events, resulted from an increase in the Earth endogenous activity, and expressed in the manifestation of volcanic activity of various nature and the deep fluids impact on the biota. A long time interval, covering almost the entire Lower Permian and characterized by a relatively calm course of geological history, was replaced by an interval with sharp upheavals manifested, which also affected the development of the entire biota, including bivalves. The rate of taxa formation is also associated with geobiospheric events and is controlled primarily by extinction events.
{"title":"Продолжительность существования и скорость образования видов и родов двустворчатых моллюсков в перми Северо-Востока Азии","authors":"A. S. Biakov","doi":"10.34078/1814-0998-2022-4-10-23","DOIUrl":"https://doi.org/10.34078/1814-0998-2022-4-10-23","url":null,"abstract":"The article discussed the duration of existence and the rate of formation for Permian bivalve species and genera in Northeast Asia. It has been established that the species existed averagely for 2-5 million years; and the genera, for 10-20 million years. The vast majority of long-lived taxa characterize the Early Permian (Asselian-Middle Artinskian) assemblages. The proportion of long-lived species that existed for over 10 million years exceeds 25 % of all bivalve species existing on this stage. Since the end of the Artinskian (and even more so since the Kungurian), the number of relatively short-lived species increased significantly. The possible reason for this phenomenon might have been an increase in the frequency of manifestation of geobiospheric, mainly extinction (Biakov, 2012a), events, resulted from an increase in the Earth endogenous activity, and expressed in the manifestation of volcanic activity of various nature and the deep fluids impact on the biota. A long time interval, covering almost the entire Lower Permian and characterized by a relatively calm course of geological history, was replaced by an interval with sharp upheavals manifested, which also affected the development of the entire biota, including bivalves. The rate of taxa formation is also associated with geobiospheric events and is controlled primarily by extinction events.","PeriodicalId":341033,"journal":{"name":"Bulletin of the North-East Science Center","volume":"62 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-12-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"121340513","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-09-30DOI: 10.34078/1814-0998-2022-3-25-40
V. Y. Kungurova
The materials, obtained from previous (1972-2019) studies of over 300 km of the coastal land strip in Southwestern Kamchatka and the adjoining underwater slope of the Sea of Okhotsk (in the interfluve of the Bolshaya and the Kikhchik rivers) were analyzed. Gold-rich zones (> 60 mg/m3) in the form of subparallel lenses, oriented along the sea shoreline, were identified between 6.3-30 m isobaths in the shallow marine shelf zone. The gold content of the submarine coastal slope correlated directly with the sediments of the upper coastal zone. Higher gold concentrations (up to hundreds of mg/m3) were detected in Holocene marine sediments of the shallow marine shelf in sampling intervals 0 to 2.0 m. They are mostly confined either to the upper, steepest part of the submarine slope or to the first or second terraced level. These are the areas of the most active impact, near the shorelines (modern and submerged), within which glacial and water-glacial formations are often exposed by erosion. Most of the gold concentrate halos related to ancient shorelines, the western boundary of which lies within 25-30 m isobaths, and to paleovalleys, identified by seismoacoustic profiling. In paleovalleys, flooded by the sea and buried under marine sediments, alluvial placers similar to Tikhangou in Primorsky Krai may be revealed. The most promising within the investigated territory was the area of underwater coastal slope within the Severnaya Mitoga - Utka - Khomutina interfluve, between 5.3-30 m isobaths, where concentrate halos with considerable gold concentrations from 60 to 500-1186 mg/m3 had been revealed.
{"title":"О золотоносности мелководной зоны шельфа Юго-Западной Камчатки","authors":"V. Y. Kungurova","doi":"10.34078/1814-0998-2022-3-25-40","DOIUrl":"https://doi.org/10.34078/1814-0998-2022-3-25-40","url":null,"abstract":"The materials, obtained from previous (1972-2019) studies of over 300 km of the coastal land strip in Southwestern Kamchatka and the adjoining underwater slope of the Sea of Okhotsk (in the interfluve of the Bolshaya and the Kikhchik rivers) were analyzed. Gold-rich zones (> 60 mg/m3) in the form of subparallel lenses, oriented along the sea shoreline, were identified between 6.3-30 m isobaths in the shallow marine shelf zone. The gold content of the submarine coastal slope correlated directly with the sediments of the upper coastal zone. Higher gold concentrations (up to hundreds of mg/m3) were detected in Holocene marine sediments of the shallow marine shelf in sampling intervals 0 to 2.0 m. They are mostly confined either to the upper, steepest part of the submarine slope or to the first or second terraced level. These are the areas of the most active impact, near the shorelines (modern and submerged), within which glacial and water-glacial formations are often exposed by erosion. Most of the gold concentrate halos related to ancient shorelines, the western boundary of which lies within 25-30 m isobaths, and to paleovalleys, identified by seismoacoustic profiling. In paleovalleys, flooded by the sea and buried under marine sediments, alluvial placers similar to Tikhangou in Primorsky Krai may be revealed. The most promising within the investigated territory was the area of underwater coastal slope within the Severnaya Mitoga - Utka - Khomutina interfluve, between 5.3-30 m isobaths, where concentrate halos with considerable gold concentrations from 60 to 500-1186 mg/m3 had been revealed.","PeriodicalId":341033,"journal":{"name":"Bulletin of the North-East Science Center","volume":"37 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-09-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"115032893","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-09-30DOI: 10.34078/1814-0998-2022-3-73-84
E. A. Nesterova, N. N. Nikolaeva, E. S. Petukhova
The article presents the results of analyzing characteristics of burying mammoth fauna animal remains. The finds coordinates were linked to the engineering-geological map of the Republic of Sakha (Yakutia) (1:1 500 000). Extensive literary data describing the burials taphonomy are taken into account. It has been found that most of the finds were buried in deposits of small fractions (loess-like loams, sandy loams, sands) characteristic for the edoma (ice complex) providing the unique preservation for bone and soft tissues of animals.
{"title":"Анализ особенностей захоронения остатков животных мамонтовой фауны и ископаемой мамонтовой кости","authors":"E. A. Nesterova, N. N. Nikolaeva, E. S. Petukhova","doi":"10.34078/1814-0998-2022-3-73-84","DOIUrl":"https://doi.org/10.34078/1814-0998-2022-3-73-84","url":null,"abstract":"The article presents the results of analyzing characteristics of burying mammoth fauna animal remains. The finds coordinates were linked to the engineering-geological map of the Republic of Sakha (Yakutia) (1:1 500 000). Extensive literary data describing the burials taphonomy are taken into account. It has been found that most of the finds were buried in deposits of small fractions (loess-like loams, sandy loams, sands) characteristic for the edoma (ice complex) providing the unique preservation for bone and soft tissues of animals.","PeriodicalId":341033,"journal":{"name":"Bulletin of the North-East Science Center","volume":"90 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-09-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"125142510","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-09-30DOI: 10.34078/1814-0998-2022-3-3-15
I. V. Brynko, T. I. Mikhalitsyna, I. L. Vedernikov, A. S. Biakov
The article discusses the results of studying the material composition of Permian terrigenous deposits in the Dzhigdali, Gizhiga, and Khivach formations in the southeastern part of the Omolon massif. The obtained data interpretation is based on the petrographic research and widely used petrochemical and discriminant paleogeodynamic diagrams. The lithochemical study showed that the deposits had accumulated under conditions of a moderately warm climate with some cooling episodes in the active continental margin settings. Clastic material entered the sedimentary basin from several provenance areas: the Permian Okhotsk-Taigonos volcanic arc, the Precambrian basement of the Omolon massif, and volcanic rock fields of the Kedon series.
{"title":"Новые данные о составе пермских терригенных отложений Омолонского массива (Северо-Восток России): значение для палеогеографии и геодинамических реконструкций","authors":"I. V. Brynko, T. I. Mikhalitsyna, I. L. Vedernikov, A. S. Biakov","doi":"10.34078/1814-0998-2022-3-3-15","DOIUrl":"https://doi.org/10.34078/1814-0998-2022-3-3-15","url":null,"abstract":"The article discusses the results of studying the material composition of Permian terrigenous deposits in the Dzhigdali, Gizhiga, and Khivach formations in the southeastern part of the Omolon massif. The obtained data interpretation is based on the petrographic research and widely used petrochemical and discriminant paleogeodynamic diagrams. The lithochemical study showed that the deposits had accumulated under conditions of a moderately warm climate with some cooling episodes in the active continental margin settings. Clastic material entered the sedimentary basin from several provenance areas: the Permian Okhotsk-Taigonos volcanic arc, the Precambrian basement of the Omolon massif, and volcanic rock fields of the Kedon series.","PeriodicalId":341033,"journal":{"name":"Bulletin of the North-East Science Center","volume":"100 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-09-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"122694449","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-09-30DOI: 10.34078/1814-0998-2022-3-120-126
O. S. Favstritskaya
The author of the article considered the experience of urbanization of the regions of the Far North-East of Russia. The transformations taking place with urban settlements in the Magadan Oblast and the Chukotka Autonomous Okrug under the influence of socio-economic factors were analyzed.
{"title":"Российский опыт пространственной трансформации региональных экономических систем: урбанизация Крайнего Северо-Востока России","authors":"O. S. Favstritskaya","doi":"10.34078/1814-0998-2022-3-120-126","DOIUrl":"https://doi.org/10.34078/1814-0998-2022-3-120-126","url":null,"abstract":"The author of the article considered the experience of urbanization of the regions of the Far North-East of Russia. The transformations taking place with urban settlements in the Magadan Oblast and the Chukotka Autonomous Okrug under the influence of socio-economic factors were analyzed.","PeriodicalId":341033,"journal":{"name":"Bulletin of the North-East Science Center","volume":"23 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-09-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"114104497","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-09-30DOI: 10.34078/1814-0998-2022-3-63-72
A. Lozhkin, P. Anderson
A palynological record obtained from El'gygytgyn Lake sediments, which spans the 1.244-1.304 million years (Ma) interval of the Calabrian Stage, shows repeated changes in the plant communities of Arctic Chukotka. These variations in the vegetation further suggest a dominance of interstadial and interglacial climates. Eight pollen zones were distinguished within this interval. According to the working age model for the composite El'gygytgyn core, these pollen zones correspond to marine oxygen isotope stages (MIS) 40, 39, and 38. The upper boundary of MIS 38 coincides with magnetic event the Cobb Mountain (1.240 Ma), which is one of the main chronological landmarks used in creating the core's chronology. The features of modern pollen-spore spectra obtained from the water-sediment interface within the lake aided in reconstructing both the local and regional paleovegetation. The consistent presence of Larix pollen throughout the 1.244-1.304 Ma interval indicates that even under the severest climatic conditions Larix forest-tundra persisted on the Anadyr Plateau and near El'gygytgyn Lake. This pattern differs sharply from that seen in the Middle and Late Pleistocene when herb-dominated tundra characterized the glacial intervals in the Arctic. The spore-pollen spectra further show that the warmest climatic conditions occurred during MIS 39. The data from the 1.244-1.304 Ma interval represent the last step in completing the Quaternary vegetation history from this unique site in Arctic Siberia.
{"title":"Vegetation Response to Climate Change during the Middle Calabrian in Arctic Chukotka","authors":"A. Lozhkin, P. Anderson","doi":"10.34078/1814-0998-2022-3-63-72","DOIUrl":"https://doi.org/10.34078/1814-0998-2022-3-63-72","url":null,"abstract":"A palynological record obtained from El'gygytgyn Lake sediments, which spans the 1.244-1.304 million years (Ma) interval of the Calabrian Stage, shows repeated changes in the plant communities of Arctic Chukotka. These variations in the vegetation further suggest a dominance of interstadial and interglacial climates. Eight pollen zones were distinguished within this interval. According to the working age model for the composite El'gygytgyn core, these pollen zones correspond to marine oxygen isotope stages (MIS) 40, 39, and 38. The upper boundary of MIS 38 coincides with magnetic event the Cobb Mountain (1.240 Ma), which is one of the main chronological landmarks used in creating the core's chronology. The features of modern pollen-spore spectra obtained from the water-sediment interface within the lake aided in reconstructing both the local and regional paleovegetation. The consistent presence of Larix pollen throughout the 1.244-1.304 Ma interval indicates that even under the severest climatic conditions Larix forest-tundra persisted on the Anadyr Plateau and near El'gygytgyn Lake. This pattern differs sharply from that seen in the Middle and Late Pleistocene when herb-dominated tundra characterized the glacial intervals in the Arctic. The spore-pollen spectra further show that the warmest climatic conditions occurred during MIS 39. The data from the 1.244-1.304 Ma interval represent the last step in completing the Quaternary vegetation history from this unique site in Arctic Siberia.","PeriodicalId":341033,"journal":{"name":"Bulletin of the North-East Science Center","volume":"18 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-09-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"123168176","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-09-30DOI: 10.34078/1814-0998-2022-3-56-62
О. А. Balandin, N. Peshkov, O. Sokolova, V. S. Sokolova
Coarse soils are reliable foundations. However, in the presence of sand-clay aggregate cryogenic processes develop in them, which has a negative impact on engineering structures functioning. The research aims in assessing the heaving hazard of coarse soils with different percentages of the sand-clay aggregate. Such soils were field-tested in Zabaikalsky Krai. As a result, the optimum conditions of cryogenic frost heave were determined for them and a statistical model was compiled to assess their heaving hazard.
{"title":"Оценка пучинистости крупно-обломочных грунтов с суглинистым заполнителем (Забайкальский край)","authors":"О. А. Balandin, N. Peshkov, O. Sokolova, V. S. Sokolova","doi":"10.34078/1814-0998-2022-3-56-62","DOIUrl":"https://doi.org/10.34078/1814-0998-2022-3-56-62","url":null,"abstract":"Coarse soils are reliable foundations. However, in the presence of sand-clay aggregate cryogenic processes develop in them, which has a negative impact on engineering structures functioning. The research aims in assessing the heaving hazard of coarse soils with different percentages of the sand-clay aggregate. Such soils were field-tested in Zabaikalsky Krai. As a result, the optimum conditions of cryogenic frost heave were determined for them and a statistical model was compiled to assess their heaving hazard.","PeriodicalId":341033,"journal":{"name":"Bulletin of the North-East Science Center","volume":"18 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-09-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"122970966","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-09-30DOI: 10.34078/1814-0998-2022-3-101-105
O. M. Orlovskaya, N. Е. Dokuchaev, G. I. Atrashkevich, A. N. Lazutkin
Parasitization of the trematode Plagiorchis koreanus Ogata, 1938 in the Siberian Bat (Myotis sibiricus Kastschenko, 1905) in the Northern Priokhotye (Magadan Oblast) with a possibility of the parasite life cycle realization in the regional freshwater ecosystems has been established for the first time. This is the first registration of P. koreanus in the Siberian Bat in Northeast Asia. An illustrated description of adult flukes is given.
{"title":"Трематода Plagiorchis koreanus (Plagiorchiidae) от сибирской ночницы (Myotis sibiricus) из Северного Приохотья (Магаданская область)","authors":"O. M. Orlovskaya, N. Е. Dokuchaev, G. I. Atrashkevich, A. N. Lazutkin","doi":"10.34078/1814-0998-2022-3-101-105","DOIUrl":"https://doi.org/10.34078/1814-0998-2022-3-101-105","url":null,"abstract":"Parasitization of the trematode Plagiorchis koreanus Ogata, 1938 in the Siberian Bat (Myotis sibiricus Kastschenko, 1905) in the Northern Priokhotye (Magadan Oblast) with a possibility of the parasite life cycle realization in the regional freshwater ecosystems has been established for the first time. This is the first registration of P. koreanus in the Siberian Bat in Northeast Asia. An illustrated description of adult flukes is given.","PeriodicalId":341033,"journal":{"name":"Bulletin of the North-East Science Center","volume":"414 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-09-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"134237324","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-09-30DOI: 10.34078/1814-0998-2022-3-106-111
A. Lebedintsev
The articles presents information on the study of the Sanga-Talon burial ground, performed by the Kolyma archaeological team from the North-East Interdisciplinary Research Institute of the USSR Academy of Sciences in the zone of flooding by the reservoir of the Kolyma hydroelectric power plant, in 1971-1972. The burial ground was found near the settlement of Sanga-Talon, on a 7-8 meter terrace, on the left of the mouth of the Obo Creek (right tributary of the Kolyma River). It is assumed that the Yakut burial ground indicates the exploration of this part of the Kolyma valley by the Yakuts in the 18th century. The data on the Yakut settling in the northeast direction along the Kolyma River and its tributaries are presented. The discovery of the Yakut burial ground near the settlement of Sanga-Talon is of certain scientific interest, since the Yakut exploration of this part of the Kolyma valley has not been sufficiently studied.
{"title":"Исследование якутского Санга-Талонского могильника на Верхней Колыме","authors":"A. Lebedintsev","doi":"10.34078/1814-0998-2022-3-106-111","DOIUrl":"https://doi.org/10.34078/1814-0998-2022-3-106-111","url":null,"abstract":"The articles presents information on the study of the Sanga-Talon burial ground, performed by the Kolyma archaeological team from the North-East Interdisciplinary Research Institute of the USSR Academy of Sciences in the zone of flooding by the reservoir of the Kolyma hydroelectric power plant, in 1971-1972. The burial ground was found near the settlement of Sanga-Talon, on a 7-8 meter terrace, on the left of the mouth of the Obo Creek (right tributary of the Kolyma River). It is assumed that the Yakut burial ground indicates the exploration of this part of the Kolyma valley by the Yakuts in the 18th century. The data on the Yakut settling in the northeast direction along the Kolyma River and its tributaries are presented. The discovery of the Yakut burial ground near the settlement of Sanga-Talon is of certain scientific interest, since the Yakut exploration of this part of the Kolyma valley has not been sufficiently studied.","PeriodicalId":341033,"journal":{"name":"Bulletin of the North-East Science Center","volume":"170 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-09-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"132725964","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
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