Suspended particulate matter within the Kaliningrad coastal zone: distribution, transport, composition
... the suspensions, including colonies of cyanobacteria, diatoms and dinoflagellates. The suspended matter composition changes from the Sambia Peninsula toward to the Curonian Spit: iron content rises along with a decrease in total number of mineral particles.
Bubnova E. S
the Baltic Sea, suspended particulate matter, sediment transport, mineral composition, abrasion, deposition, human activity
32-39
On the benthic foraminifera species of Alabaminella weddellensis and Epistominella exigua in paleo-oceanologic reconstructions
... analysis // Palaeontologia Electronica. 2001. Vol. 4. № 1. P. 1—9.
15. Hecker B. Photographic evidence for the rapid flux of particles to the sea floor and their transport down the continental slope // Deep Sea Research. Part A. 1990. Vol. 37. № 12.... ... 161—177.
19. Licari L. N., Mackensen A. Benthic foraminifera off West Africa (1°N to 32°S): Do live assemblages from the topmost sediment reliably record environmental variability? // Marine Micropaleontology. 2005. Vol. 55, № 3. P. 205—233.
20. Licari ...
Total suspended matter in the Gdansk deep at oxygenated / anoxic conditions in 2018—2023
... conditions. Semi-enclosed water bodies, such as the shallow Baltic Sea, play a key role in the global carbon cycle. Carbon-containing particles, both organic and inorganic, settle within the total suspended matter, making it important to understand the patterns ... ... mixed coastal zone, the suspended matter is transported to the Gdańsk Deep, where benthic nepheloid layers indicate complex sedimentation conditions, suggesting that this area cannot be considered a simple carbon sink. Intermediate nepheloid layers form ...
The The Variability of Bottom Friction Velocity and the Suspended Particle Propagation along the Pathway of Saline Inflow into the Baltic Sea
... identified processes prevalent in the bottom layer dynamics at specific points on the pathway of the inflow waters propagation in the Baltic Sea. An analysis of the variability of bottom friction velocity made it possible to estimate the likelihood of bottom sediment resuspension at these points and to predict propagation pathways.
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