scholarly journals The Linguistic Atlas of the East of Guilan on the Basis of Morphological Analysis (Lexical - Inflectional)

2016 ◽  
Vol 7 (1) ◽  
pp. 1166-1171
Author(s):  
Maryam Mahlouji Afshar ◽  
Iran Kalbassi
Keyword(s):  
Caspian Sea ◽  
Morphological Analysis ◽  
Field Method ◽  
Syntactic Analysis ◽  
The Caspian Sea ◽  
Principal Role ◽  
Language Varieties ◽  
Eastern Border ◽  
Morphological Differences ◽  
Guilan Province

This article, in line with “The National Project of the Dialectology”, aims to provide a linguistic atlas in the East of Guilan province. Due to the large number of speakers in the southern edge of the Caspian Sea and many differences between dialects and accents, this area has great importance linguistically and providing the linguistic atlas in representation and introduction of dialects in this land can be an important achievement to access the indigenous, cultural, social and historical studies among linguistics and persons who are interested in culture. In order to achieve this principal issue, there has been investigated the morphological differences and similarities (lexical - inflectional) of language varieties in the East of Guilan province with the standard Persian- even more than phonetic and syntactic analysis- and they can have the principal role in providing the linguistic atlas. So in this article, through presenting the morphological evidences (lexical - inflectional) and comparing them with standard Persian, there has been marked a dialect with different accents- the Guilaki dialect from the East of Guilan province and it has been depicted for linguistic atlas. The study was conducted by library and field method and by collecting data from a questionnaire consisting of 100 words and sampling from 20 villages in the East of Guilan province- from Astaneh Ashrafieh to the end of the eastern border of Guilan province (Chaboksar). The data obtained by each village has been considered in the tables related to each word and has been moved on the map of region after comparing with the standard Persian and finally the linguistic atlas has been made. To achieve genuine accents, the speakers of middle-aged who spent much of their life in the area have been helped and villages have been considered with more phonetic differences in accent.

The Boundaries of Caucasian Albania (4th Century BC – 3rd Century AD)

2021 ◽  
pp. 31
Author(s):  
Archil S. Balakhvantsev
Keyword(s):  
Caspian Sea ◽  
Balance Of Power ◽  
The Political ◽  
The Caspian Sea ◽  
Political Situation ◽  
Archaeological Data ◽  
Narrative Tradition ◽  
Eastern Border ◽  
To Come ◽  
High Degree

The issue of the borders of Caucasian Albania in the ancient period has long been discussed in the literature, and the inability of researchers from different countries to come to an agreed solution is explained not so much by the state of the sources as by the high degree of politicization of the problem. The only thing that unites the most disagreeing authors with each other is their resolute confidence in the invariability of the borders of Caucasian Albania throughout antiquity. However, we have no reason to speak of an “eternal and unchanging” border along the Kura, Aras or Alazani. Albania's borders were constantly changing in the wake of changes in the balance of power between it and its neighbors: Media Atropatena, Armenia and Iberia. In the future, the political situation in Transcaucasia and the configuration of borders were increasingly influenced by the struggle of the two superpowers of the Ancient World – the Rome and Iran – for domination in the Middle East. Thus, the establishment of the border between Armenia and Albania along the Kura is associated with the signing of the Nisibis peace between Diocletian and Narses. The only “eternal” was the eastern border along the Caspian Sea, but it also in the 4th–2nd centuries BC underwent major changes. Further clarification of the borders of Albania is possible only on the basis of an in-depth and honest analysis of the ancient narrative tradition and an ever-growing array of archaeological data, free from following the political conjuncture.

scholarly journals An Assessment of Heavy Metals in Coastal Sediments of the Caspian Sea, Guilan Province

2017 ◽  
Vol 8 (31) ◽  
pp. 27-34 ◽  
Author(s):  
Mohsen Mohammedi Galangash ◽  
Esa Solgi ◽  
Zahra Bozorgpanah
Keyword(s):  
Heavy Metals ◽  
Caspian Sea ◽  
Coastal Sediments ◽  
The Caspian Sea ◽  
Guilan Province

THE NUMBER AND QUALITATIVE CHARACTERISTICS OF FRY FISH IN SHALLOW COASTAL WATERS OF THE VOLGA IN THE SUMMER-AUTUMN PERIOD OF 2012

2017 ◽  
pp. 65-73
Author(s):  
Edward Vladimirovich Nikitin
Keyword(s):  
Fish Species ◽  
Coastal Waters ◽  
Caspian Sea ◽  
The Caspian Sea ◽  
Volga River ◽  
Commercial Fish ◽  
Autumn Period ◽  
Fish Juveniles ◽  
Qualitative Characteristics ◽  
Shallow Coastal Waters

Shallow coastal waters of the Volga river is a flooded feeding area for fish juveniles of nonmigratory fish species. There takes place annual downstream migration of fluvial anadromous fish species from spawning grounds of the Volga river to the Northern Caspian Sea. The most important factors determining the number and qualitative characteristics of fry fishes are the level of the Caspian Sea (currently having a tendency to the lowering), hydrological and thermal regimes of the Volga river. Researches were carried out in definite periods of time. In the summer-autumn period of 2012 fry fishes were presented by 19 species (13 of them were commercial species), which belonged to 9 families. The article gives data on all the commercial fish species. In the first decade of July the maximum number of fry fish was registered in the western part of the Volga outfall offshore - in box 247 (19.86 mln specimens/km2), in the eastern part - in box 142 (20.4 mln specimens/km2). The most populous were roach, red-eye, silver bream and bream; size-weight characteristics were better in the areas remoted from the Volga delta. In the third decade of July the quantitative indicators of fry fish on these areas decreased, size-weight characteristics greatly increased. In the second decade of October in the western part of the seaside there were registered increased pre-wintering concentrations of fish juveniles, their qualitative indicators increased, which is evidence to favorable feeding conditions in 2012.

On the type locality of the steppe ribbon racer, Psammophis lineolatus (Brandt, 1838) (Serpentes: Lamprophiidae)

2020 ◽  
Vol 324 (2) ◽  
pp. 262-272
Author(s):  
I.V. Doronin ◽  
T.N. Dujsebayeva ◽  
K.M. Akhmedenov ◽  
A.G. Bakiev ◽  
K.N. Plakhov
Keyword(s):  
Caspian Sea ◽  
Type Specimen ◽  
Type Locality ◽  
Eastern Coast ◽  
Zoological Museum ◽  
Western Coast ◽  
The Caspian Sea ◽  
Original Species ◽  
Academy Of Sciences ◽  
Made In

The article specifies the type locality of the Steppe Ribbon Racer. The holotype Coluber (Taphrometopon) lineolatus Brandt, 1838 is stored in the reptile collection of the Zoological Institute of the Russian Academy of Sciences (ZISP No 2042). Literature sources provide different information about the type locality. A mistake has been made in the title of the work with the original species description: the western coast of the sea was indicated instead of the eastern one. The place of capture was indicated as “M. Caspium” (Caspian Sea) on the label and in the reptile inventory book of the Zoological Museum of the Academy of Sciences. The specimen was sent to the museum by G.S. Karelin. The “1842” indicated on the labels and in the inventory book cannot be the year of capture of the type specimen, just as the “1837” indicated by A.M. Nikolsky. In 1837, Karelin was in Saint Petersburg and in 1842 in Siberia. Most likely, 1837 is the year when the collection arrived at the Museum, and 1842 is the year when the information about the specimen was recorded in the inventory book (catalog) of the Zoological Museum of the Academy of Sciences. In our opinion, the holotype was caught in 1932. From Karelin’s travel notes of the expedition to the Caspian Sea in 1832, follows that the snake was recorded in two regions adjacent to the eastern coast of the Caspian Sea – Ungoza Mountain (“Mangyshlak Mountains”) and site of the Western Chink of Ustyurt between Zhamanairakty and Kyzyltas Mountains (inclusive) on the northeast coast of Kaydak Sor (“Misty Mountains”). In our article, Karelin’s route to the northeastern coast of the Caspian Sea in 1832 and photographs of these localities are given. The type locality of Psammophis lineolatus (Brandt, 1838) should be restricted to the Mangystau Region of the Kazakhstan: Ungoza Mountain south of Sarytash Gulf, Mangystau (Mangyshlak) Penninsula (44°26´ N, 51°12´ E).

ICE CONDITIONS IN THE NORTH-WESTERN PART OF THE CASPIAN SEA IN THE MODERN PERIOD

2020 ◽  
Vol 19 (6) ◽  
pp. 4-17
Author(s):  
Nepomenko Leonid ◽  
◽  
Popova Natalia ◽  
Zubanov Stepan ◽  
Ostrovskaya Elena ◽  
...  
Keyword(s):  
Caspian Sea ◽  
The Caspian Sea ◽  
The North ◽  
Modern Period ◽  
Ice Conditions ◽  
North Western
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