Dolotov, YS et al. (2009): Mineral and chemical composition of surface bottom sediments from the Onega Bay, White Sea. doi:10.1594/PANGAEA.726931, Supplement to:Dolotov, Yury S; Filatov, NN; Shevchenko, Vladimir P; Petrov, MP; Tolstikov, AV; Zdorovennov, RE; Platonov, AV; Filippov, Alexander S; Bushuev, KL; Kutcheva, IP; Denisenko, Nina V; Stein, Ruediger; Saukel, Cornelia (2008): Multidisciplinary studies in Onega Bay of the White Sea and the estuary of the Onega River during the summer period. Oceanology, 48(2), 255-267, doi:10.1134/S0001437008020136
The distribution of temperature and salinity, current velocities, suspended particulate matter, bottom sediments, bottom morphology, and planktonic and benthic organisms during the summer period are studied in the estuary of the large Onega River and coastal areas of the Onega Bay (White Sea) influenced by interacting marine and riverine factors.