scholarly journals A Complex of the Early-Eleventh Century Finds from a Cistern in Quarter IX of Chersonese

Author(s):  
Larissa V. Sedikova ◽  
Stanislav G. Ryzhov

This paper discusses a complex of ceramic finds excavated from a cistern in quarter IX in the north-eastern area of Chersonese, which supplied water to a public bath at the first stage of its existence. Although the reasons why the cistern was covered with soil remain unclear, later on residential buildings appeared at this site. The finds published here comprised imported transport and table ceramic wares. The complex included brown-clay flat-handle transport pitchers, presumably from the Taman area; Günsenin I amphorae produced on the Marmara Sea coast to the south-west of Constantinople; Glazed White Ware II tableware (according to J. Hayes’ classification) and painted white-clay Polychrome Ware also produced in the vicinity of the Byzantine capital. A vessel with polished surface is probably connected with the manufacture of the Khazar Khanate circle. The questions of the chronology of specific pottery types nave been analysed with account to their modern dating. According to the combination of dates, the complex of finds from the cistern in question is attributable to the beginning of the eleventh century. An important role for the dating of the complex is played by the chronology of the white-clay polychrome ware clarified by G. Sanders and the absence of Günsenin II amphorae dating from the mid-eleventh to the early twelfth centuries. The ceramic ware from the infill of the cistern comprises only imported pieces and reflects the two directions of Cherson’s trade in the said period: first, Constantinople and its environs and second, the Azov Sea and Northern Caucasus area.

2021 ◽  
Vol 17 (1) ◽  
pp. 89-114
Author(s):  
Arsen L. Budaychiev

The main purpose of this article is a typological and chronological study of the handles of ceramic vessels originating from fairly well-studied sites of the Early Bronze Age of the Primorsky Lowland of Dagestan, including both settlements (Velikent II, Gemetyube I, II, Kabaz-Kutan I, II, Torpakh-kala), and and burial grounds (Velikent I (catacomb No. 8), II (catacomb No. 1), III (catacomb No. 1), Karabudakhkent II, Kayakent VI). The first handles in the North-Eastern Caucasus appeared on ceramic ware back in the Eneolithic era. During the early Bronze Age, handles became a characteristic part of ceramic dishes (bowls, containers, cups, vases) on the considered sites of Primorsky Dagestan. Functionally, they have a utilitarian, decorative, artistic and religious purpose. The handles are of four types, which are characteristic of certain forms of dishes: type 1 - horizontal tubular, type 2 - ribbon, type 3 - pseudo-handles, type 4 - hemispherical. The article provides a description of each type of pens, provides analogues on the sites of the Early Bronze Age both in the Northeast Caucasus and the adjacent regions of the Caucasus, including the territories of modern Iran, Turkey and Palestine and Israel, which were part of the distribution area of ​​the Kuro-Arak cultural and historical community ( including Khirbet-Kerak culture). The work identifies the most common and early, dating back to the Chalcolithic period, types of pens, discusses the issue of their chronology. This article is the first special work devoted to a typological and chronological analysis of ceramic vessel handles.


1969 ◽  
Vol 73 (704) ◽  
pp. 657-664 ◽  
Author(s):  
R. G. West

During the past two years the commercial airline operators and the travelling public alike have been forced to acknowledge the rapid increase in airport congestion. This problem is most marked in the North Eastern area of America at the present time but a similar situation will develop fairly soon at major airports in Europe. Even with the introduction of the airbus to scheduled services, the number of aircraft movements at conventional airports, within a given time period, will reach a maximum safe level. The restrictions are imposed partly by the large number of aircraft operations on each runway, and partly by Air Traffic Control safety limits.


Author(s):  
A. A. T. Sime ◽  
G. J. Cranmer

The genus Echinus is common throughout the entire northern North Sea. Echinus esculentus L. predominates in the shallow water off the eastern Scottish coast down to 100 m, while the small variety of Echinus acutus var. norvegicus (Düben and Koren) is rarely found in depths of less than 100 m and is most commonly located in the north-eastern area of the North Sea (Cranmer, 1985).


Author(s):  
Andrea Biondi

The article focuses on the analysis of seven Lombard weapons datable between the end of 6th and the 7th century C.E. and present in the Archaeological Museum of Fiesole, in the north-eastern area of Tuscany in Italy. These objects, only partially published, and coming both from the Lombard necropolis of Area Garibaldi and from unknown contexts, have been compared with similar materials on national scale of the 6th-7th century C.E. and represent a relevant term of archaeological analysis for the transition between Late Antiquity Era and Lombard domination in Fiesole.


Author(s):  
O. Podymov ◽  
O. Podymov ◽  
N. Kuzevanova ◽  
N. Kuzevanova ◽  
A. Khvorosch ◽  
...  

The work demonstrates the results of the 6-years complex ship-borne monitoring of coastal zone in the north-eastern part of the Black Sea, carried out by the Southern Branch of P.P.Shirshov Institute of Oceanology, RAS, on a marine cross-section at the Blue Bay (Gelendzhik) beam 1-2 times per month. Climatic changes and eutrophication exert a significant impact on the sea water at the coastal area. In case of the Black Sea these factors pile up with a permanent hydrogen sulphide contamination of the sea water below 80-200 meters depth (depending on the season and distance from the shore). Strong pycno-halocline at the depths from 70 to 160 meters, formed due to the inflow of high salinity water from the Marmara Sea, inhibits the mixing between the water layers and, as a result, also limits the oxygen transport into the deeper layers. The winter cooling reduces the pycno-halocline and enriches the top active layer, down to the cold intermediate layer (CIL), with oxygen and nutrients, which subsequently lead to a vernal phytoplankton bloom. Formation of the thermocline and upper quasi-homogeneous layer (UQL), caused by the water warming in spring, at large extent determines a thickness of phytoplankton-rich layer during the spring and summer seasons. The work demonstrates seasonal and interannual dynamics of the UQL, thermocline, CIL and hydrogen sulphide boundary position in the coastal zone of the north-eastern part of the Black Sea.


2015 ◽  
Vol 60 (2) ◽  
Author(s):  
Maria-Larisa Ivanescu ◽  
Dumitru Acatrinei ◽  
Ionuţ Pavel ◽  
Tatiana Sulesco ◽  
Liviu Miron

AbstractThe members of the Anopheles maculipennis complex have been incriminated for the transmission of the malaria in Europe, which was endemic until the middle of the century. The global warming and the intensification of the intercontinental travel constitute a risk of the re-emergence of the malaria in Europe, given the presence of the Anopheles vectors. The study has attempted the identification by using the PCR (Polymerase Chain Reaction) of the members of the Anopheles maculipennis complex from the North-eastern area of Romania from the city of Iaşi. In total there have been identified by using the PCR amplifying the ITS2 sequence of the ribosomal DNA, 217 specimens belonging to the complex of A. maculipennis among which: 58 A. atroparvus, 18 A. melanoon, 2 A. labranchiae, 52 A. maculipennis and 87 A. messeae. The ITS2 sequences of the ribosomal DNA have been compared to those of the species belonging to the A. maculipennis available in GenBank. The Species A. labranchiae is reported for the first time in Romania, being identified in the larval stage IV. The adaptation of a new species to the climatic conditions present in the North-eastern Romania, confirms the phenomenon of global warming and also the intensification of the travelling. As a result of the analysis of the A. labranchiae sequence, this one corresponds to the extent of 96% to the species from Italy, registered in GenBank, given the fact that a high number of the inhabitants of the municipality of Iaşi are working in this country.


2005 ◽  
Vol 19 (1) ◽  
pp. 59-77
Author(s):  
Elisenda Campmany Jané

Traditional studies of Catalan dialectology have always included the variety spoken in the North-eastern area in the group of dialects that have CV pronominal clitics instead of the innovative VC standard forms (e.g., me instead of em ‘me’). rt is also welI accepted that nowadays there is variation between CV and VC clitics, the latter being considered the result of the increasing influence of the standard. Our goa I is to check the scope of this variation and determine if there are internal factors that favour the shift to VC forms. Unlike previous studies, our description wilI not be based on data from questionnaires but on data from spontaneous texts recorded in two corpora: the Atles lingüístic del domini català, compiled in the 60s, and the Corpus Oral Dialectal, compiled in the 90s. The data unexpectedly show that, although there is a tendency towards the loss of CV clitics along the time, all the speakers, including the oldest ones, use more VC than CV forms, which cannot be entirely attributed to the influence of the standard. We conclude that VC clitics have a deep-rooted presence and are favoured by certain syntactic contexts that are welI determined by language universals.


Author(s):  
O. Podymov ◽  
O. Podymov ◽  
N. Kuzevanova ◽  
N. Kuzevanova ◽  
A. Khvorosch ◽  
...  

The work demonstrates the results of the 6-years complex ship-borne monitoring of coastal zone in the north-eastern part of the Black Sea, carried out by the Southern Branch of P.P.Shirshov Institute of Oceanology, RAS, on a marine cross-section at the Blue Bay (Gelendzhik) beam 1-2 times per month. Climatic changes and eutrophication exert a significant impact on the sea water at the coastal area. In case of the Black Sea these factors pile up with a permanent hydrogen sulphide contamination of the sea water below 80-200 meters depth (depending on the season and distance from the shore). Strong pycno-halocline at the depths from 70 to 160 meters, formed due to the inflow of high salinity water from the Marmara Sea, inhibits the mixing between the water layers and, as a result, also limits the oxygen transport into the deeper layers. The winter cooling reduces the pycno-halocline and enriches the top active layer, down to the cold intermediate layer (CIL), with oxygen and nutrients, which subsequently lead to a vernal phytoplankton bloom. Formation of the thermocline and upper quasi-homogeneous layer (UQL), caused by the water warming in spring, at large extent determines a thickness of phytoplankton-rich layer during the spring and summer seasons. The work demonstrates seasonal and interannual dynamics of the UQL, thermocline, CIL and hydrogen sulphide boundary position in the coastal zone of the north-eastern part of the Black Sea.


2003 ◽  
Vol 6 (1) ◽  
pp. 25-54 ◽  
Author(s):  
Sabine Reinhold

Ornaments, jewellery, personal equipment and weapons in graves can be defined as relicts of ancient costumes and weapon assemblages which are connected to the social identities of the buried persons. At several late Bronze Age and early Iron Age sites in the north Caucasus (Koban culture) large numbers of richly furnished graves allow the reconstruction of specific costume and armour groups. These can be related to factors which structured these communities into a ranked society. This article is based on the investigation of two cemeteries in Chechenia (north-eastern Caucasus) which demonstrate the change in social differentiation during the developed Iron Age. The article also includes a general discussion about the concepts of costumes and their potential for reconstructing social identities.


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