scholarly journals Polychaete genus Pholoe (Polychaeta: Pholoidae) in the north-east region of the Barents Sea

2021 ◽  
Vol 12 (3-2021) ◽  
pp. 88-97
Author(s):  
K.K. Moskvin ◽  
Keyword(s):  
Barents Sea ◽  
Size Structure ◽  
Novaya Zemlya Archipelago ◽  
North West ◽  
Novaya Zemlya ◽  
North East ◽  
The North ◽  
East Region ◽  
The Barents Sea ◽  
Franz Josef Land

The paper describes species composition, distribution and biology of the polychaeta genus Pholoe in the north-east region of the Barents Sea (between Franz Josef Land and north-west coast of Novaya Zemlya archipelago). One species of the genu s was identified based on the reviewed morphological descriptions – Pholoe assimilis. The highest values of population density (1130 specimens/m2) and biomass (570 mg/m2) were registered in comparatively warm coastal waters of Novaya Zemlya archipelago. Pholoe assimilis’ population size structure based on the dorsal width of the fifth chaetiger was investigated for the first time. Size-frequency histograms indicate presence of at least four size classes.

Co, Hf, Ce, Cr, Th, and REE systematics of modern bottom sediments of the Barents sea

2019 ◽  
Vol 485 (2) ◽  
pp. 207-211
Author(s):  
A. V. Maslov ◽  
N. V. Politova ◽  
V. P. Shevchenko ◽  
N. V. Kozina ◽  
A. N. Novigatsk ◽  
...  
Keyword(s):  
Bottom Sediments ◽  
Barents Sea ◽  
Western Coast ◽  
Novaya Zemlya ◽  
The North ◽  
The Barents Sea ◽  
Franz Josef Land ◽  
Pechora River ◽  
Marine Areas ◽  
Bottom Grab

The Co, Hf, Ce, Cr, Th, and REE systematics are analyzed for modern sediments collected by a bottom grab during the 67th and 68th cruises of R/V “Akademik Mstislav Keldysh” and samples taken in the Barents Sea bays and inlets. Our results indicate that most modern bottom sediments are composed of fine silicoclastic material enhanced with a suspended matter of the North Cape current, which erodes the western coast of Scandinavia, and due to bottom erosion of some marine areas, as well as erosion of rock complexes of the Kola Peninsula, Novaya Zemlya, and Franz Josef Land (local provenances). Material from Spitsbergen also probably played a certain role. In the southern part of the Barents Sea, clastic material is supplied by the Pechora River.

Rare and trace elements in modern bottom sediments of the Barents sea. Nd, Pb and Sr isotopic composition

2021 ◽  
pp. 444-472
Author(s):  
A.V. Maslov ◽  
◽  
N.V. Politova ◽  
N.V. Kozina ◽  
A.B. Kuznetzov ◽  
...  
Keyword(s):  
Bottom Sediments ◽  
Surface Sediments ◽  
Barents Sea ◽  
Positive Correlation ◽  
Novaya Zemlya ◽  
The North ◽  
The Barents Sea ◽  
Franz Josef Land ◽  
Central Regions ◽  
Moderate Positive Correlation

The article presents a brief lithological description of the modern bottom sediments of the Barents Sea, selected in the 67th voyage of the R/V “Akademik Mstislav Keldysh” at the polygons: 1) “Pechora Sea”; 2) “Western slope of Kaninskoe shoal”; 3) “Central Barents Sea (Shtokman area)”; 4) “Russkaya Gavan’ fjord”; 5) “Medvezhinsky Trench”; 6) in the area to the south of Spitsbergen; 7) “Kola meridian”; 8) “Spitsbergen – Franz Josef Land archipelago”; 9) “Cambridge Strait”. The distribution of Cr, Ni, Cu, Zn, Cd, and Pb in samples of bottom sediments (pelitic, aleurite-pelitic and sandy-aleuritic-pelitic ooze) is compared with the background concentrations and contents of these elements in the Post-Archean Average Shale (PAAS). The data obtained are consistent with the notion that the distribution of heavy metals and other elements in the bottom sediments is controlled primarily by the global geochemical background. The relationship of the Sc, V, Cr, Ni, Y, Zr, Nb, Mo, Hf, Th, U and rare-earth elements concentrations with content of fine pelite (< 0.001 mm) fraction and organic carbon (Corg) is considered. It was found that most of these elements are characterized by a moderate positive correlation with the amount of fine pelite fraction in samples. By the magnitude of the correlation coefficient with the Corg content, all elements are attributed into three groups: (1) with moderate positive correlation, (2) weak positive correlation, (3) practically not pronounced correlation. The distribution in the bottom sediments of the Barents Sea of the element-indicators of the source rocks composition (Sc, Th, Co, Cr, La and Sm), as well as of rare earths, make it possible to consider that the majority of bottom sediments is mature in geochemical terms material, the sources of which were rocks of the Kola Peninsula and Spitsbergen (?). The bottom sediments of the Cambridge Strait are represented by geochemically less mature material, which, apparently, entered the sea as a result of erosion of the Franz Josef Land archipelago rocks. The established isotopic characteristics (εNd, 207Pb/206Pb and 87Sr/86Sr) of 17 samples of surface sediments suggest that the main contribution to the formation of bottom deposits of the central regions of the Barents Sea is made by rocks of the mainland part located in the influence zone of the North Cape Current. Archipelagos and islands (Franz Josef Land, Novaya Zemlya, etc.) that frame the Barents Sea supply a relatively small amount of clastic material that is carried by Arctic currents. The values of εNd and 87Sr/86Sr in the surface sediments of the central part of the Barents Sea and in the ice-rafted sediments carried by the Transpolar Drift showed a significant difference. This suggests that the contribution of such material to the formation of surface sediments of the Barents Sea is relatively small

Evaluation of the modern geoecological state of the fjords of the eastern Barents sea

2021 ◽  
pp. 899-943
Author(s):  
V.A. Shakhverdov ◽  
◽  
D.V. Ryabchuk ◽  
M.A. Spiridonov ◽  
V.A. Zhamoida ◽  
...  
Keyword(s):  
Bottom Sediments ◽  
Industrial Development ◽  
Barents Sea ◽  
Chemical Elements ◽  
Environmental Damage ◽  
North West ◽  
Geochemical Zoning ◽  
The North ◽  
The Barents Sea ◽  
Main Components

A brief analysis of the history of environmental geological study of the Barents Sea is given. It shows that at the beginning of industrial development the geological environment was characterized by a low level of disturbance and pollution. On example of the Kola Bay, an assessment of the current environmental geological conditions of the fjords in the eastern part of the Barents Sea is given. Seismic-acoustic studies confirm the predominantly tectonic origin of the bay and the hazardous spread of gravitational rocks movement within the coastal slopes. The background geochemical characteristics of recent bottom sediments are quantified. It is shown that geochemical zoning of the bottom of the bay is a consequence of both natural and anthropogenic processes. According to the content of Cu, Zn, As, Cd, Pb, Hg and hexane-soluble petroleum products (PP) in the bottom sediments, the characteristics of various areas were obtained. It is shown that the distribution of PP and several other pollutants in the main components of aquatic and coastal geosystems is a leading element of the environmental monitoring system, quantitative assessment of anthropogenic impact and accumulated environmental damage. Active economic activity within the southern leg of the Kola Bay, as well as the naval bases, significantly affects the distribution of chemical elements. The data concerning distribution of chemical elements forms in bottom sediments are given that suggest a high probability of secondary pollution of the bottom water when the physicochemical conditions of sedimentation processes change. A comparative analysis showed that bottom sediments of the Kola Bay are characterized by the highest concentration of chemical elements in the North-West Region of the Russian Federation.

scholarly journals Features of the Distribution of Chlorophyll-a Concentration along the Western Coast of the Novaya Zemlya Archipelago in Spring

Water ◽  
2021 ◽  
Vol 13 (24) ◽  
pp. 3648
Author(s):  
Pavel R. Makarevich ◽  
Veronika V. Vodopianova ◽  
Aleksandra S. Bulavina ◽  
Pavel S. Vashchenko ◽  
Tatiana G. Ishkulova
Keyword(s):  
Chlorophyll A ◽  
Barents Sea ◽  
Western Coast ◽  
Novaya Zemlya Archipelago ◽  
Chlorophyll A Concentration ◽  
Novaya Zemlya ◽  
The Barents Sea ◽  
High Concentrations ◽  
First Time ◽  
Arctic Surface

In spring 2016, the thermohaline characteristics of water masses and the distribution of chlorophyll-a concentration in the pelagic zone of the eastern part of the Barents Sea were studied. For the first time, in the conditions of an abnormally warm year and the absence of ice cover, a complex of hydrobiological works was carried out on a section crossing the Barents Sea from south to north along the western coast of the Novaya Zemlya archipelago. High concentrations of chlorophyll-a > 1 ˂ 6 mg/m3 at all stations of the transect indicate a stage of spring bloom in the successional cycle of microalgae. Significant differences in the content of chlorophyll-a in waters of various origins were revealed. The highest concentrations of chlorophyll-a corresponded to Arctic surface water (5.56 mg/m3). Slightly lower values were observed in the transformed Atlantic waters of the Novozemelskoe and Kolguevo–Pechorskoe currents (3.53 ± 0.97–3.71 ± 1.04 mg/m3), and the lowest was in the Barents waters (1.24 ± 0.84–1.45 ± 1.13 mg/m3).

scholarly journals Les pêches de l’URSS dans l’Atlantique du Nord-Est et l’élargissement des zones de pêche exclusive

2005 ◽  
Vol 18 (1) ◽  
pp. 107-126
Author(s):  
François Carré
Keyword(s):  
Barents Sea ◽  
East Atlantic ◽  
North East ◽  
The North ◽  
The Barents Sea ◽  
Average Production ◽  
Capelin Mallotus Villosus ◽  
Access Rights ◽  
The Baltic ◽  
Almost All

After the last war, the USSR set it self to increase the development of its ocean fisheries from its two North-East Atlantic seaboards on the Barents Sea and the Baltic. With a modernized fleet and almost complete freedom on the seas, its catch increased six fold between 1950 and 1976, going from 0,4 to 2,5 million tons per year, and Soviet fishermen could be found roaming on all the seas bordering Europe. However, as from 1977, this expansion was fiercely curtailed when coastal nations, including the USSR, established the 200-mile exclusive economic zone (EEZ) or mere exclusive fishing zone (EFZ), each being alloted almost all of its living resource s. More fishing grounds were lost by the USSR than gained, to the point where production suddenly fell in 1977 and it had to turn to fish of lesser quality, often used for industrial purposes, such as the Capelin (Mallotus villosus) and the blue Whiting (Micromesistius poutassou) which today make up to 60 % of all its catch off Northern Europe. The Soviet authorities reacted with flexibility and diversity, namely by increased fishing in the national exclusive zone, particularly in the Barents Sea, through negotiations leading to access rights to foreign waters, particularly those of Norway and the Faeroe Islands, and through a policy whereby it could purchase unprocessed fish from some members of the EEC. Thus Russian factory ships came to the British coasts to process mackerel delivered to them at sea by English and Scottish fishermen. It is through such a strategy of diversification, various examples of which may be found around the world, that the Soviets have succeeded in regaining grounds lost in 1977 and in reaching an average production of 1,7 million tons from 1977 to 1983 in the North-East Atlantic, this being 3 to 4 % less than that of 1970-76, notwithstanding the few purchases of fish made directly at sea.

Diet of snow crab in the Barents Sea and macrozoobenthic communities in its area of distribution

2020 ◽  
Author(s):  
Denis V Zakharov ◽  
Igor E Manushin ◽  
Tatiana B Nosova ◽  
Natalya A Strelkova ◽  
Valery A Pavlov
Keyword(s):  
Barents Sea ◽  
Benthic Communities ◽  
Stomach Contents ◽  
Snow Crab ◽  
Feeding Intensity ◽  
Novaya Zemlya Archipelago ◽  
Novaya Zemlya ◽  
The Barents Sea ◽  
The Pacific ◽  
Almost All

Abstract This article investigates the diet of the snow crab (Chionoecetes opilio) and its feeding intensity in the Barents Sea. Data show that snow crab has a diverse diet that includes almost all types of benthic invertebrates living in the Barents Sea. There are differences between the diets of females and males and of juveniles and adults. Juveniles and females typically occupy shallow areas with communities of bivalve molluscs, while males typically live deeper on slopes and depressions where polychaetes and crustaceans are the most abundant groups. Stomach contents were analysed to determine the species composition and frequency of occurrence of various benthic taxa. Consumption of food was estimated and compared with data from the Russian seas of the Pacific region. The total annual consumption of macrozoobenthos by snow crab was calculated in accordance with its current distribution in the Barents Sea. Snow crab consumes at least 30 000 tonnes of benthos annually, which amounts to 0.1–0.2% of the total macrozoobenthic biomass in the investigated area. The population of snow crab causes the largest impact on the benthic communities in the northeastern part of the Barents Sea and near the south side of the Novaya Zemlya archipelago.

Marsh vegetation in the north-east of Malozemelskaya tundra

2011 ◽  
pp. 45-69 ◽  
Author(s):  
N. V. Matveyeva ◽  
O. V. Lavrinenko
Keyword(s):  
Barents Sea ◽  
European Part ◽  
Russian Arctic ◽  
Marsh Vegetation ◽  
North East ◽  
The North ◽  
The Barents Sea ◽  
First Time ◽  
Different Levels

For the first time on the north-east of Malozemelskaya tundra at the coast of the Barents Sea the following 5 associations — Puccinellietum phryganodis Hadač 1946 (with subassociations inops Thannheiser, Willers 1988 ex Hofmann 1969 and caricetosum subspatheceае Thannheiser, Willers 1988 nom. nud).; Caricetum subspathaceae Hadač 1946 with subass. Inops Molenaar 1974 and arctanthemetosum hultenii subass. nov. (with variants inops var. nov. and typicum var. nov.); Caricetum glareosae Molenaar 1974 (as a geographical vicariant Calamagrostis deschampsioides vic. nov.) (with subassociations typicum and festucetosum rubrae); Scirpeto—Hippuridetum tetraphyllae Nordh. 1954 (inops subass. nov.), and the Dupontia psilosantha com. type that belong to the three alliance of the Glauco-Puccinellietalia order of the Juncetea maritime class are described with the Braun-Blanquet approach. A provisional ass. Parnassio palustris—Salicetum reptantis ass. nov. prov. represented the transitional vegetation between marshes and tundras belongs to the Scheuchzerio—Caricetea fuscae class. This shows that syntaxa of different levels known previously for various territories outside of the Russian Arctic are rather common at least in its European part. The comparison of the classification units of both Braun-Blanquet and Russian dominant systems (used by A. I. Leskov in the same region in the first half of the last century) has demonstrated a large correspondence in between and the absence of the insuperable barrier between two approaches.

Charles Bénard's first expedition to Novaya Zemlya, 1908

Polar Record ◽  
1987 ◽  
Vol 23 (146) ◽  
pp. 511-529 ◽  
Author(s):  
William Barr
Keyword(s):  
Barents Sea ◽  
Medical Officer ◽  
The South ◽  
Novaya Zemlya ◽  
The North ◽  
The Barents Sea

ABSTRACTIn the summer of 1908 the Mission Océanographique Arctique Française sailed from Dunkirk aboard the ketch Jacques Cartier. Sponsored by the Société d'Océanographie du Golfe de Gascogne and led by Charles Bénard, its major aims were to study the fisheries potential of the Barents Sea, to explore Gusinaya Zemlya on the south island of Novaya Zemlya, to chart and sound the bays and straits of that area, to carry out geological investigations, and to make a traverse of Matochkin Shar, which bisects Novaya Zemlya. The expedition established itself at Belush'ya Guba, from where Bénard and his companions explored much of Gusinaya Zemlya and surveyed, sounded and charted the adjacent waters. An attempt at crossing the south island, made by the medical officer Candiotti, was unsuccessful. Later, accompanied by the Russian geologist Vladimir Aleksandrovich Rusanov, Candiotti sailed through Matochkin Shar and made the first crossing of the north island, from Neznayemyy Zaliv to Krestovaya Guba. The expedition ended on rather a sour note: Bénard abandoned his ship and crew at Arkhangel'sk, leaving the organizing committee with the problems of unravelling the mess and repatriating the crew.

scholarly journals Ice gouging on the arctic shelf of Russia

2019 ◽  
Vol 59 (3) ◽  
pp. 466-468
Author(s):  
S. L. Nikiforov ◽  
R. A. Ananiev ◽  
N. V. Libina ◽  
N. N. Dmitrevskiy ◽  
L. I. Lobkovskii
Keyword(s):  
Deep Water ◽  
Barents Sea ◽  
The Arctic ◽  
Natural Phenomena ◽  
Novaya Zemlya ◽  
The Barents Sea ◽  
Franz Josef Land ◽  
Eastern Shelf ◽  
Almost All ◽  
Perennial Ice

The results of recent geological and geophysical expeditions indicate the activation of hazardous natural phenomena associated with ice gouging and represent geohazard for almost all activities, including operation of the Northern Sea Route. Within the Barents Sea and the western part of the Kara Sea, the modern ice gouging is mainly associated with icebergs which are formed as a result of the destruction of the glaciers of Novaya Zemlya, the Spitsbergen archipelago and Franz Josef Land, while on the eastern shelf it is caused by the destruction of seasonal or perennial ice fields. Fixed furrows can be divided into modern coastal gouges or deep water ploughmarks. All deep water gouges within the periglacial and glacial shelf are of paleogeographical origin, but with different mechanisms of action on the seabed. These furrows were formed by floating ice on the periglacial shelf. On the glacial shelf deep water ploughmarks were formed by large icebergs, which could carry out the gouging even on the continental slope and deep-sea ridges of the Arctic Ocean.

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