A bottom sediment core with a length of about 8 m sampled in the eastern Ka
ra Sea near the entrance to the Vil'kitskii Strait was studied. An age mode
l was constructed based on four C-14 datings obtained using the acceleratin
g mass spectrometry method. The results of the grain-size, chemical, minera
logical, and foraminiferal analyses were adjusted to the model. A paleocean
ological interpretation of the data under consideration together with the p
aleoclimatic data on Bolshevik Island, located in the neighborhood, was per
formed.