scholarly journals Erratum to: On the Composition and Age of Taphofloras of the Krivorechenskaya Formation (Upper Cretaceous) of the Anadyr River Left Bank, Northeast Asia

2021 ◽  
Vol 29 (6) ◽  
pp. 765-765
Author(s):  
A. B. Herman ◽  
S. V. Shczepetov
2019 ◽  
Vol 18 (3) ◽  
pp. 62-73
Author(s):  
A. N. Chekha

Purpose. There are many archaeological sites located in the North Angara region. Although this territory has been investigated since 18th century, most intensive work was done during rescue archaeological works on Boguchany hydroelectric power station in 2008–2011. One of the valuable sources of artifacts is the Kutarey site. Our work contains a brief analysis of stone industries of the Kutarey River Mouth site. The main goal of this work is to apply technical and typological analysis to mark the specificity of the stone industries of layer 2 of the Kutarey River Mouth site in comparison with the results that had been previously published on layer 3 in the context of new data of this region in terms of ceramics complexes. We introduce a previously unpublished collection of stone artifacts of layer 2 of the Kutarey River Mouth site, which significantly extends the source base of the Neolithic and Bronze Age in this region. Results. The Kutarey River Mouth site is located on the left bank of the Angara River, 15 km down from the Kezhma village, on the right bank of the Kutarey River. The location was found in 1974 by N. I. Drozdov and his squad. The site was further investigated in 2008 and in 2010 by an IAE SB RAS squad (guided by A. N. Savin). Firstly, the site was determined as a Neolithic location, but as result of 2010 excavations three Neolithic-Middle Age cultural horizons were discovered. In the context of the difficulties connected with conducting investigations in this region, namely an open location, a low stratigraphy situation, a high extend of technogenic interruption, the materials of layer 3 are most perspective due to a high grade of saturation of the artifacts and minimal technogenic interruptions. These materials belong to the Neolithic and Paleometal Era. In order to clarify cultural and chronological specificity of this complex, it is necessary to analyze materials from layer 2. The stone industry of layer 2 is represented by retouching microblades, bladelets, tools for blades, flakes, scrapers including one microscraper, bifaces, several adzes, axes, and one piercing tool. Of special interest are blade points and trihedral and tetrahedral points. Conclusion. Our technical and typological analyses show that in comparison to layer 3, layer 2 is characterized by a small number of massive axes and adzes, no flints, few double scrapers, and only volume splitting tools aimed mainly at obtaining a small blade. Also, despite the fact that the core of the collection is the product of the hornstones of local origin, we observe a significant increase in the percentage of artifacts made of flint (13 %), which may indicate some new commodity strategies. The most interesting analogy can be traced with the dedicated Upper Kolyma Early Holocene complex, which contained blade points widely distributed in Northeast Asia and was present directly or indirectly in the materials from Chukotka (Verkhnetirsky IV and Nizhnechutinsky IV), Yakutia (Olbinski burial ground, Jubilee), Kamchatka (the Ushki I–IV layer, Avacha 1,9). This complex is believed to belong to specific Volbinsky traditions, which formed in the first half of the Holocene, about 8800–6000 years ago. It is also worth comparing these materials with other Kutarey sites – Sen’kin (Siniy) Kamen’, Ruchei Povarny, Gora Kutarey and adjacent territories.


2019 ◽  
Vol 27 (4) ◽  
pp. 424-441
Author(s):  
V. A. Marinov ◽  
S. E. Agalakov ◽  
I. N. Kosenko ◽  
O. S. Urman ◽  
E. A. Potapova ◽  
...  

Zootaxa ◽  
2010 ◽  
Vol 2499 (1) ◽  
pp. 21 ◽  
Author(s):  
MASSIMO OLMI ◽  
ALEXANDER P. RASNITSYN ◽  
ADALGISA GUGLIELMINO

New fossil taxa of Embolemidae and Dryinidae (Hymenoptera: Chrysidoidea) are described. For Embolemidae, Embolemopsis baissensis n. gen. n. sp. and Baissobius minutus n. sp., are described from Central Siberia, West Transbaikalia, left bank of Vitim River (facing downstream), Baissa, lake deposits from earlier Early Cretaceous (Neocomian stage) (130–140 mybp). For Dryinidae, Anteonopsis antiquus n. gen. n. sp., Bocchus ? cenomanianus n. sp. and Gonatopus ? cretacicus n. sp., are described from Siberia, Magadan Region, Obeschchayushchiyi, tuffaceous deposits from Upper Cretaceous (Cenomanian) (90–95 mybp); Deinodryinus ? aptianus n. sp., is described from Central Mongolia, Bayanhongor Aimag, 5–8 Km N Bon Tsagan Nuur Lake, from impressed in lake deposits of the Khurilt rock unit probably of Aptian (Early Cretaceous) (100–115 mybp). In addition, an unidentified fossil belonging to Deinodryinus ? or Dryinus ? is recorded from Russian Far East, Maritime Province, Velikaya Kema (later Earlier or early Middle Miocene) (about 30 mybp). The known species of Baissobius Rasnitsyn are reviewed and a key is presented.


2012 ◽  
pp. 9-19 ◽  
Author(s):  
Slobodan Knezevic ◽  
Ljupko Rundic ◽  
Meri Ganic

The largest single-pylon, cable-stayed bridge in the world was opened in Belgrade on January 1, 2012 and it passes over the tip of the Ada Ciganlija Island. Its monumentality, architectural design and construction innovations became a new symbol of Belgrade. Core samples from the boreholes drilled for the construction of the bridge revealed a relatively complex subsurface geological structure. An Upper Cretaceous-Paleogene flysch formation and Middle Miocene Sarmatian sediments were found near the surface on the right bank of the Sava River. However, at the tip of Ada Ciganlija, the Upper Cretaceous-Palaeogene flysch strata were found below several different Miocene and Quaternary units. In the deepest borehole DB-6, the flysch deposits were found at a depth of 80 meters. On the left bank of the Sava River in New Belgrade, only Upper Miocene Pannonian marls and Pleistocene and Holocene alluvial deposits were drilled. Based on a comparative analysis of the borehole sections and structural characteristics of the rocks, it could be concluded that the Pre-Quaternary units cascade subsided along sub-parallel faults towards N-NW.


Author(s):  
Andriy Bogucki ◽  
Olena Tomeniuk ◽  
Roman Dmytruk ◽  
Andriy Yatsyshyn

On the left bank of the Dnister River between the villages of Mezhyhirtsi and Dubivtsi (Halych district, Ivano-Frankivsk region, Ukraine) there are several large mechanized quarries, where raw materials (marl, limestone, gypsum) are mined for PJSC “Ivano-Frankivsk Cement”. It is quarries of limestones and marls of Dubivtsi Suite of the Upper Cretaceous in a lower part of a slope, and gypsum of Tyrassian Suite of the Neogene nearly in a watershed. The amplitude of maximum points of the relief above the Dnister River bed reaches 145 m and it varies in the range of 50-60 m above the oldest terraces of the Dnister River (Loyeva level), which are developed on it right bank (Dnister-Lukva interfluve). Well stratified thick (more than 20 m) Pleistocene loess-soil sequence covering almost all the Brunhes palaeomagnetic chron developed over the gypsum. In particular, it is worth noting that the covering series of sediments in the Mezhyhirtsi section does not lie on the alluvium of the Dnister, but directly on the bedrocks, i.e. outside the Dnister valley. The first general description of the Pleistocene loess-soil series in the Mezhyhirtsi section is given and the fossil malacofauna found in a number of horizons and sub-horizons is presented. There are almost all the stratigraphic horizons of the Pleistocene (from the upper horizon of the Upper Pleistocene loesses (MIS 2) to the palaeosol complex of Zahvizdia (MIS 17-21) and the sediments, which it was formed on) in the section. It is reasoned that the Mezhyhirtsi section requires a comprehensive study. It may become a key section for the Pleistocene of Halych-Dnister region – an area with a well-developed complex of Dnister terraces, a number of Upper and Middle Palaeolithic sites (Mezhyhirtsi, Yezupil I-IX, Kolodiiv, Mariampil I, V, Halych I, II and many others). There are many interdisciplinary studied sections of the Pleistocene deposits (for instance, the Kolodiiv section with a fossil Eem (Horokhiv) peatland or the Halych section with a 50-meter thick covering loess-soil series on the fifth (Halych) terrace of the Dnister River) in the region. The Mezhyhirtsi section is important because it contains the oldest part of the section of the Pleistocene in the Halych-Dnister region, as well as a few palaeobasins (above the Korshiv and Zahvizdia palaeosol complexes), the study of which may provide many new data for reconstruction of the palaeogeographical conditions of the Pleistocene within the Dnister valley and beyond it. Key words: Pleistocene, loess-soil series, key section, palaeobasin, the Matuyama-Brunhes boundary, Halych-Dnister region.


Island Arc ◽  
2000 ◽  
Vol 9 (4) ◽  
pp. 611-626 ◽  
Author(s):  
Shigeyuki Suzuki ◽  
Shizuo Takemura ◽  
Graciano P. Yumul ◽  
Sevillo D. David ◽  
Daniel K. Asiedu

10.1029/ft172 ◽  
1989 ◽  
Author(s):  
W. Burleigh Harris ◽  
Vernon J. Hurst ◽  
Paul G. Nystrom ◽  
Lauck W. Ward ◽  
Charles W. Hoffman ◽  
...  

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