Research Results on Ecological Hazard Objects in Abrosimov Bay (Novaya Zemlya,Kara Sea)

Oceanology - The article presents results of field research on environmental assessment in Abrosimov Bay (Yuzhny Island of Novaya Zemlya) in connection with the existing RW disposal sites in this...     

Development of Technology for Integrated Instrumental Underwater Observations Related to Russian Arctic Ecosystems

Oceanology - Abstract—The article touches upon methodological problems of studying the underwater fauna, plant, and micro- and mesorelief of the near-bottom zone of the Russian Arctic seas in...     

Upper Campanian-lower Maastrichtian sections of the northwestern Rostov region. Article 1. Description, paleontological assemblages, and lithobiostratigraphy

Four upper Campanian-lower Maastrichtian reference sections are described in the Glubokaya and Kalitva river basins and in the Znamenka 1-A Borehole located in the northwestern Rostov region. The sections are composed of the upper Campanian Kagal??nik, Belgorod, Pavlovka, Sukhodol and lower Maastrichtian Efremovo-Stepanovka formations. They are characterized by successive stratigraphically significant macro- and microfossil assemblages: belemnites, calcareous nannoplankton, benthic foraminifers, and radiolarians. The Pavlovka and, particularly, Sukhodol formations contain a specific assemblage of coarsely-agglutinated benthic foraminifers. The first data obtained on radiolarians in upper Campanian-lower Maastrichtian sections of the northwestern Rostov region revealed four assemblages, two of which were previously unknown from Upper Cretaceous sediments of the East European Platform. Most sections enclose a hiatus at the base of the Sukhodol Formation, which comprises two upper Campanian benthic foraminiferal zones. The problem of recognition of the lower Maastrichtian boundary on the East European Platform is considered in accordance with international GSSP requirements.     

Thermodynamic properties of CoCr2O4: specific heat and magnetic entropy

We present the temperature dependence of the specific heat of CoCr₂O₄ between 2.08 K and 306 K in zero magnetic field. The lattice component can be described by the Komada–Westrum model with a characteristic temperature Θ_KW = 541 K. The entropy of the magnetic component amounts to 33.51 J mol^?1 K^?1 at T = 298.15 K, in good agreement with the magnetic entropy of Co²⁺ and Cr³⁺ ions with completely quenched orbital moments. We compare our results with data available in literature.     

Hydrophysical and morpholithodynamic processes in the Onega River’s estuary

New data on the Onega River estuary’s hydrological and morpholithodynamic regimes are presented. The river’s bottom structure and soil lithology are described on the basis of field sonar survey materials. Proceeding from the analysis of the hydrographic maps, the dynamics of the Onega River’s mouth bar is tracked over the period of 1830–2000.     

Generation of the 2018 Tsunami on Sulawesi Island: Possible Sources

Doklady Earth Sciences - Numerical simulation of a tsunami from September 28, 2018, on Sulawesi Island (Indonesia) is carried out. It is shown that the observed distribution of tsunami heights...     

Morphostructures and Sedimentary Cover Structure of the Inner Shelf of Western Crimea

Oceanology - The article presents the results of geophysical and geomorphological works on the western shelf of the Crimean Peninsula (Yevpatoriya–Balaklava). The sedimentary sequence...     

Technology for bottom relief and sedimentation surveys of White-Sea river estuaries

Experimental bottom relief survey technology and investigation results are presented. Investigations were conducted over about six years at several White-Sea river estuaries onboard the R/V Ecolog. Geomorphology data was obtained using an instrument complex that included an MKS, Microsound side scan sonar, AP-5 acoustic profiler, and LMS-350 echo sounder. ECHOGRAPH and WINRASTR original software was used for data gathering and processing.     

Manifestation of marine and riverine factors in the tide and ebb phases along the white sea coasts of different configuration

The peculiarities of the distributional patterns of the water temperature, salinity, current velocities, particulate matter concentration, bottom contour, and zooplankton abundance were studied in relation to the marine-riverine interactions and tide/ebb phases for coast lines of different configurations in the White Sea during the cruises of the R/V Ekolog (August of 2006 and 2007). A significant difference in the manifestation of the combined effect of the marine and riverine impacts (the estuarine concave relief) and only the marine impact (the open-sea straight-line portion) was observed, which results in both variations in the sea water level and the distributional patterns of the suspended matter and the zooplankton.