A5010842725- Marine and environmental studies
- Geology and Paleoclimatology Research
- Geological Studies and Exploration
- Methane Hydrates and Related Phenomena
- Ancient and Medieval Archaeology Studies
- Isotope Analysis in Ecology
- Food Industry and Aquatic Biology
- Arctic and Antarctic ice dynamics
- Climate change and permafrost
- Aquatic and Environmental Studies
- Cryospheric studies and observations
- Soil and Environmental Studies
- Coastal and Marine Dynamics
- Marine Biology and Ecology Research
- Oceanographic and Atmospheric Processes
- Arctic and Russian Policy Studies
- Geotechnical and Geomechanical Engineering
- Hydrocarbon exploration and reservoir analysis
- Geological and Geochemical Analysis
- Polar Research and Ecology
- Coastal and Marine Management
- Indigenous Studies and Ecology
- Bryophyte Studies and Records
- Geological formations and processes
- Archaeology and ancient environmental studies
Lomonosov Moscow State University
2014-2024
Moscow State University
2015-2023
Arctic and Antarctic Research Institute
2019
Considerable interannual differences were observed in river water and sea-ice meltwater inventory values derived from d18O salinity data the Eurasian Basin along continental margin of Laptev Sea summers 1993 1995, 2005 2006 during Nansen Amundsen Basins Observational system (NABOS) expeditions. The annually different pattern inventories remain closely linked for all years studied, which indicates that source regions transport mechanisms both formation are largely similar over relatively...
Fossil ostracod assemblages were investigated in five AMS 14 C ‐dated cores from various water depths of the L aptev and K ara seas ranging upper continental slope (270 m) to present‐day shelf depth (40 m). Six fossil distinguished. These represent varying environmental conditions at N orth S iberian margin since about 18 ka. In reflect gradual transition an estuarine brackish‐water environment modern marine 12.3 ka, as induced by regional early H olocene transgression. The core dates back...
The palynological method was used to study a 455 cm thick marine sediment sequence, which overlies the Moscovian moraine in Bychye-2 section on Pyoza River (Arkhangel’sk region). pollen records obtained allowed us make palynozonal subdivision of and trace plant cover transformations that occurred northeastern White Sea region during Boreal transgression. When comparing established local palynozones with regional subdivisions reference sections Bychye-1, located 5 km upstream from site, Peski...
Abstract The paper deals with results of geological and geophysical study the East Siberian Sea coastal areas are reported. Research activities started in 2018 frame State Geological Mapping Project (GK-1000/3) continued 2022 under support Russian Science Foundation. A seismo-stratigraphic scheme Quaternary sediment sequence has been compiled, a conception paleogeographical evolution Late Pleistocene–Holocene proposed.