Reworking of Mesozoic clayey material in the northwestern part of the Barents Sea

1975 ◽  
Vol 18 (1) ◽  
pp. M29-M34 ◽  
Author(s):  
K. Björlykke ◽  
A. Elverhøi
2020 ◽  
Vol 29 (1) ◽  
pp. 128-137
Author(s):  
I.O. Nekhaev ◽  
E.N. Krol

A taxonomic review of the genus Anatoma Woodward, 1859 in the Eurasian Arctic seas is presented. The new species A. golikovi sp. nov. is described from the northwestern part of the Barents Sea. The species differs from all other Arctic and North Atlantic Anatoma in having a flat spire. We consider Anatoma schioettei Høisæter et Geiger, 2011, syn. nov., a junior synonym of A. crispata (Fleming, 1828). Anatoma schanderi Høisæter et Geiger, 2011 is recorded for the first time from the Siberian seas.


Polar Record ◽  
1965 ◽  
Vol 12 (81) ◽  
pp. 703-708 ◽  
Author(s):  
Jenö Nagy

Svalbard comprises the islands between longs 10 to 35° E and between lats 74 to 81° N. The largest of these islands is Vestpitsbergen, followed by Nordaustlandet, Edgeøya, Barentsøya and Bjørnøya. The archipelago lies in the northwestern part of the Barents-Kara shelf. To south and east the continental shelf is covered by the shallow waters of the Barents Sea, whilst to the north and west the shelf falls away rapidly into the Arctic Basin and the Greenland Sea.


Author(s):  
Valeriy G. Yakubenko ◽  
Anna L. Chultsova

Identification of water masses in areas with complex water dynamics is a complex task, which is usually solved by the method of expert assessments. In this paper, it is proposed to use a formal procedure based on the application of the method of optimal multiparametric analysis (OMP analysis). The data of field measurements obtained in the 68th cruise of the R/V “Academician Mstislav Keldysh” in the summer of 2017 in the Barents Sea on the distribution of temperature, salinity, oxygen, silicates, nitrogen, and phosphorus concentration are used as a data for research. A comparison of the results with data on the distribution of water masses in literature based on expert assessments (Oziel et al., 2017), allows us to conclude about their close structural similarity. Some differences are related to spatial and temporal shifts of measurements. This indicates the feasibility of using the OMP analysis technique in oceanological studies to obtain quantitative data on the spatial distribution of different water masses.


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