1,2Kokin O.V., 1,2Arkhipov V.V., 1,3Meshcheryakov N.I., 4Ananiev R.A., 5Slukovsky Z.I., 1Sukhikh E.A.

THE ICE-GOUGING LANDFORMS INVESTIGATION OF THE SOUTH-WESTERN PART OF KARA SEA AND THE NORTH-EASTERN PART OF THE BARENTS SEA IN THE 51ST CRUISE OF THE R/V "ACADEMIK BORIS PETROV" 

Relief and Quaternary deposits of the Arctic, Subarctic and North-West Russia. Issue 9.

Download *pdf

doi: 10.24412/2687-1092-2022-9-123-127

1 Geological Institute, Russian Academy of Sciences, Moscow, Russia,

2 Lomonosov Moscow State University, Faculty of Geography, Moscow, Russia

3 Murmansk Marine Biological Institute, Russian Academy of Sciences, Murmansk, Russia

4 Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia

5 Institute of North Industrial Ecology Problems, Kola Science Center of the RAS, Apatity, Russia 

 

     

Abstract. The preliminary results of the relief and sediments of the ice-gouging landforms study of the southwestern part of the Kara Sea and the north-eastern part of the Barents Sea, carried out during the 51st cruise of the R/V “Akademik Boris Petrov”, are presented. The survey of the ice-gouging landforms was carried out at 16 sites, on which ice gouges with depth of up to 10,0 m and up to 450 m wide were recorded. The maximum length of the ice gouges was 11.1 km. The core of bottom sediments are taken both directly from the bottom of the ice gouges and from an undisturbed background surface for comparative dating of the ice-gouging relief using the content of the non-equilibrium 210Pb, anthropogenic 137Cs and heavy metals (Pb, Sb, Cd, Tl, Bi). The ice-gouging landforms investigation was supported by the Russian Scientific Fund (project 21-77-20038).

Keywords: ice gouges, bottom topography survey, multibeam echo sounder, bottom sediment cores, East-Novaya Zemlya trough

 


 

 

REFERENCES:

Kokin O.V., Arkhipov V.V., Maznev S.V., Meshcheriakov N.I. The ice-gouging landforms investigation of the south-western part of the Kara sea in the 52nd cruise of the R/V "Academik Nikolay Strakhov" // Relief and Quaternary deposits of the Arctic, Subarctic and North-West Russia. 2021. Issue 8. P. 97-100. doi: 10.24412/2687-1092-2021-8-97-100

Meshcheryakov N.I., Usyagina I.S., Arkhipov V.V., Maznev, S.V., Kokin O.V. The first results of determining the absolute age of the ice-exaration furrow in the area of the Baidaratskaya Bay of the Kara Sea // Second All-Russian Scientific Conference “Geochronology of the Quaternary Period: Instrumental Methods for Dating Recent Deposits”, 2022. P. 56. (In Russ.)

Mironyuk S.G., Ivanova A.A. Micro- and mesorelief of the glacial shelf of the Western Arctic Seas in the light of new data // Bulletin of the Commission for the Study of the Quaternary Period. 2018. No. 76. P. 41–58. (In Russ.)

Nikiforov S.L., Sorokhtin N.O., Ananiev R.A. et al. Research in Barents and Kara Seas during Cruise 52 of the R/V Akademik Nikolaj Strakhov // Oceanology. 2022. Vol. 62. Is. 3. P. 433–434. doi:10.1134/S0001437022030079

Rybalko A.E., Mironyuk S.G., Roslyakov A.G., Kolyubakin A.A., Solovieva M.A., Terekhina Ya.E., Tokarev M.Yu. New signs of glaciation in the Kara Sea: mega-scale glacial lineation in the East-Novozemelsky trench // Relief and Quaternary deposits of the Arctic, Subarctic and North-West Russia. 2020. Issue 7. P. 175-181. doi:10.24411/2687-1092-2020-10727

 

 

Cite this article:

Kokin O.V., Arkhipov V.V., Meshcheryakov N.I., Ananiev R.A., Slukovsky Z.I., Sukhikh E.A. 2022. The ice-gouging landforms investigation of the south-western part of Kara sea and the north-eastern part of the Barents sea in the 51st cruise of the R/V "Academik Boris Petrov" // Relief and Quaternary deposits of the Arctic, Subarctic and North-West Russia. Issue 9. P. 123-127. doi: 10.24412/2687-1092-2022-9-123-127

 



eXTReMe Tracker


Flag Counter

Яндекс.Метрика

Hosted by uCoz