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East Siberian Sea
Arctic Report Card 2018 Effects of Persistent Arctic Warming Continue to Mount
Pleistocene-Holocene Permafrost of the East Siberian Eurasian Arctic Shelf
Multi-Year Distributions of Dissolved Barium in the Canada Basin And
Crustal Architecture of the East Siberian Arctic Shelf and Adjacent Arctic Ocean Constrained by Seismic Data and Gravity Modeling Results
The Degradation of Coastal Permafrost and the Organic Carbon Balance of the Laptev and East Siberian Seas
Wetlands in Russia
Denisenko, N. V., 2011. Bryozoans of the East Siberian
Arctic Report Card 2020 the Sustained Transformation to a Warmer, Less Frozen and Biologically Changed Arctic Remains Clear
Russian-German Cooperation in the Siberian Shelf Seas: Geo-System Laptev-Sea
7 Laptev Sea
Freshwater Transport Between the Kara, Laptev, and East-Siberian Seas (Fig
Background on Vladivostok and the Soviet Far East
The Arctic—M
Russian Travels Including Russian Americana & Pacific
Change in Sediment Provenance on the Inner Slope of the Chukchi Rise and Their Paleoenvironmental Implications
Landscapes, Faces, and Memories: Eskimo Photography of Aleksandr Forshtein, 1927–1929
Sedimentary Record from the Canada Basin, Arctic Ocean: Implications for Late to Middle Pleistocene Glacial History
CDOM Optical Properties and DOC Content in the Largest Mixing Zones of the Siberian Shelf Seas
Top View
The Biogeochemistry of the East Siberian Sea and Its Impact on the Upper Waters of the Deep Arctic Ocean
Iucn Technical Evaluation Natural System of Wrangel
Carbon Mineralization in Laptev and East Siberian Sea Shelf and Slope Sediment
Chukotsky Autonomous Okrug Russian E a S 737,000 Sq
Atlas of Marine and Coastal Biological Diversity of the Russian Arctic
Deglacial Sea-Level History of the East Siberian Sea Margin Thomas M
The Ocean Carbon Cycle in the Western Arctic Ocean: Distributions and Air-Sea Fluxes of Carbon Dioxide.Oceanography 24(3):186–201
Ancient Tales of Chukotka
The Summer Hydrography and Surface Circulation of the East Siberian Shelf Sea*
The Dominant Role of the East Siberian Sea in Driving the Oceanic Flow Through the Bering
U.S. Department of the Interior Open-File Report 96-727
The IUCN/NRDC Workshop to Identify Areas of Ecological and Biological
Middle Cretaceous to Eopleistocene Sequences on the New Siberian Islands: an Approach to Interpret Offshore Seismic
East Siberian Sea, an Arctic Region of Very High Biogeochemical Activity
East Siberian Sea: LME #56
Arctic Biogeography
Carbon Mineralization in Laptev and East Siberian Sea Shelf and Slope Sediment Volker Brüchert1,3, Lisa Bröder2,3, Joanna E. S
Circumpolar Arctic Tundra Vegetation Change Is Linked to Sea Ice Decline
Circum-Arctic Mineralogy & Pan-Arctic
East Siberian Sea, an Arctic Region of Very High Biogeochemical Activity
High Biolability of Ancient Permafrost Carbon Upon Thaw Jorien E
East Siberian Sea, an Arctic Region of Very High Biogeochemical Activity
Ecologically Or Biologically Significant Marine Areas (Ebsas) Special Places in the World’S Oceans
Organic Matter Across Subsea Permafrost Thaw Horizons on the East Siberian Arctic Shelf
8 East Siberian Sea
Geology of the Shelves Surrounding the New Siberian Islands, Russian Arctic
The Arctic—M
Seas of the Arctic Ocean