scholarly journals Stone Kurgans of the Southern Urals, “Irendyk-Kryktyn Group of Nomads” and “Settled Down Sako-Sarmatians”

Author(s):  
Vitaliy Vasilev

Based on the available archaeological material, the article covers a number of issues related to the kurgans of nomads from the middle of the 1st millennium BC within the sub-mountain zone of the Bashkir Trans-Urals, embankments of which were built using stone. The author analyses the representativeness of archaeological records, provides typological and chronological attribution of the burial complexes. Previously these materials allowed to identify the “Irendyk-Kryktyn nomadic group” which existed in the considered landscape zone. According to the author, the investigated stone kurgans are divided into two groups. The first one might be dated back to the Saka Age (VII-VI centuries BC), the second one belongs to the Savromatian-Sarmatian period (not earlier that the mid of V-IV centuries BC). Within the existing chronology there is no explanation for the time gap between those periods. Hereby, this fact may indicate the presence of two culturally unrelated nomadic groups. The analysis of the archaeological material allows us to say that the signs of the burial rite, which are typical for the monuments of the foothill strip of the Bashkir Trans-Ural (Irendyk-Kryktyn group), are widespread far beyond this landscape zone, and are common for nomads who left stone kurgans in the steppe part of the region on both sides of the Ural Ridge. Furthermore, the author draws attention to the existing statement about the process of sedentarization of nomads of this region in the middle of the 1st millennium BC. The study of the source base on this issue shows that single finds of ceramic in “settlements” of nomads are their common locations. Settlement monuments in the mountainous Urals and steppe Trans-Urals, where few fragments of Kenotkel and Gafurian tableware were found, demonstrate the lack of dwellings, tools and remnants of handicraft production. This fact testifies to the temporary or episodic nature of the appearance of small groups of population at such monuments, and is not associated with nomads. Moreover, the sedentarization of nomads in the northern marginal zone is not confirmed by either historical or ethnographic sources. The article contains materials to supplement the archaeological records for studying issues related to stone kurgans.

Author(s):  
Nikita Savelev ◽  

The article presents an analysis of the burial rite and chronology of the Gumarovo cemetery, located on the border of the steppe and mountain-steppe zones of the Southern Urals, at the southern tip of the almost completely forested low plateau Zilair (Russia, Orenburg oblast, right bank of the Sakmara River). The cemetery consists of 5 stone kurgans, explored in 1979–1980 by an expedition led by R.B. Ismagilov. A burial of Early Scythian time was revealed in one of the kurgans (the so-called “Bolshoy Gumarovskiy”, “Big Gumarovo”), and immediately became widely known among researchers. The cemetery itself belongs to a later time, also known as “Sauromatian” time. Based on the chronological indicators and simultaneous occurrence of accompanying inventory categories, it is determined that the cemetery dates back to the end of the 5th – beginning of the 4th centuries BC and existed for a very short time. The burial rite features of the Gumarovo kurgans (stone mounds, wide oval graves, sloping walls, circular chamber graves, heads of the deceased oriented to the west and the east) indicate that it belongs to a special “Mugodzharian” group of nomads from the Southern Urals steppes eastern part. The origin of this group of nomads is associated with the migration of the Northern and Central Kazakhstan nomads to the steppes of the Orsk-Ilek interfluve, i.e. to the west of the Mugodzhar ridge; with their long-lasting interaction with the local population of the Sauromatian (proved by Blumenfeld and East Aral complexes) and Early Sarmatian time; as well as assimilating part of the Early Saka appearance population, which occupied the steppes of the Southern Trans-Urals in the 7th – 6th centuries BC. It is shown that it is the “Mugodzharian” features that make the kurgans in the eastern part of the Southern Urals steppes significantly specific.


Author(s):  
Svetlana Sharapova ◽  

The article deals with the antiquity of Sargat culture of forest-steppe in the Trans-Urals and Western Siberia. The established concepts of chronological framework cover the interval from the 5th century BC to 4th-5th centuries AD. Recent studies, both in the main territory and outside the Sargat area, provide evidences for clarifying the upper chronological boundary of the culture. The bright Late Sarmatian appearance of some Sargat burial complexes allows to consider Late Sarmatian finds of the Southern Urals as a reference; rich material has been accumulated on them, as well as detailed chronology.Late Sargathian monuments are found only in two regions - Tobol and Ishim rivers basins. The proposed correction is based on archaeological material which is external data (relative chronology) towards radiocarbon analysis (absolute chronology). In the archaeological collections of Sargat burials there are no any artifacts, the beginning of the period of existence of which falls on the 3rd century AD. There is no such evidence in the settlements either. Furthermore, judging by the available materials, the number of such complexes is small and the inventory is quite poor. The article gives a detailed analysis of burials from seven kurgan cemeteries located in Tobol and Ishim rivers basins, which might be attributed to the latest group marking the upper chronological boundary. In the second half of the 3rd century AD, the main features of the Sargat culture are fading and blurred, besides, it is absent in most of the forest-steppe territory to the east of the Urals. In conclusion the author suggests that if the assumptions are correct, the disappearance of the bright expressive complexes that defined the image of the Sargat social and cultural system, looks quite sharp. The Sargat monuments of the 4th century AD and later are not found across vast forest-steppe territory.


Author(s):  
A. O. Khotylev ◽  
N. B. Devisheva ◽  
Al. V. Tevelev ◽  
V. M. Moseichuk

Within the Western slope of the Southern Urals, there are plenty of basite dyke complexes of Riphean to Vendian among Precambrian terrigenous-carbonate formations. In metamorphic formations of the Taratash complex (Archean to Early Proterozoic, the northern closure of the Bashkirian meganticlinorium) there was observed the andesitic dyke with isotopic age of 71±1 Ma (U-Pb SHRIMP II on zircons) and near Bakal two bodies of gabbroids with zircons of similar ages were found. These are the first evidence of possible Mezozoic magmatism in this region.


2017 ◽  
Vol 212 (12) ◽  
pp. 48-50
Author(s):  
Ju.P. Gorichev ◽  
◽  
A.N. Davydychev ◽  
A.Yu. Kulagin ◽  
◽  
...  

2012 ◽  
pp. 109-134
Author(s):  
P. S. Shirokikh ◽  
A. M. Kunafin ◽  
V. B. Martynenko

The secondary birch and aspen forests of middle stages of succession of the central elevated part of the Southern Urals are studied. 4 subassociations, 1 community, and 7 variants in the alliances of Aconito-Piceion and Piceion excelsae are allocated. It is shown that the floristic composition of aspen and birch secondary forests in the age of 60—80 years is almost identical to the natural forests. However, a slight increase the coenotical role of light-requiring species of grasslands and hemiboreal forests in the secondary communities of the class Brachypodio-Betuletea was noticed as well as some reduction of role the shade-tolerant species of nemoral complex and species of boreal forests of the class Vaccinio-Piceetea. Dominant tree layer under the canopy of secondary series is marked by an active growth of natural tree species.


2002 ◽  
pp. 42-62 ◽  
Author(s):  
A. I. Solomeshch ◽  
V. B. Martynenko ◽  
O. Yu. Zhigunov

Xerophillous pine-larch forests of the Southern Ural have been described as a new alliance Caragano fruti­cis—Pinion sylvestris. They occur on steep slopes of upper parts of mountain ridges with poorely developed stony soils. Alliance asigned to the class Brachypodio pinnati—Betuletea pendulae, order Chamaecytiso ruthe­nici—Pinetalia sylvestris. Associations Carici caryophyl­leae—Pinetum sylvestris and Ceraso fruticis—Pinetum sylvestris with four subassociations are described. Eco­logical and floristical peculiarities of new alliance in comparison with another alliances of the order Cha­maecytiso-Pinetalia and with siberian class Rhytidio rugosi—Laricetea sibiricae have been discussed.


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