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Mastogloia Sea
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Mastogloia Sea
The Mastogloia Sea (also Early Littorina Sea, Initial Littorina Sea) is one of the prehistoric stages of the Baltic Sea in its development after the last ice age. It is characterised by distinctive deposits of the calciferous shell of species of the diatom Mastogloia that were used for paleoenvironmental reconstructions. This transition took place at different times in different parts of the Baltic basin c. 9000 years ago following the Ancylus Lake stage and preceding the full Littorina Sea stage.
Towards its demise, the Ancylus Lake was falling, having partly eroded and scouring away at its new outlet at the Great Belt. It reached sea level c. 9800 years ago, making it the Mastogloia Sea.
At this time global sea level was rising rapidly due to the melting of vast tracts of the great ice age ice sheets. As a result, some sea (salt) water started to penetrate into the basin through the Danish Straits, mixing into the vast freshwater body. This led to the stage's slightly brackish conditions in the Baltic.
This phase of the body of water takes its name from the brackish water-dwelling diatom genus Mastogloia, the species of which are characteristic of the geological deposits of this stage. As fresh water lakes became part of the sea identification in the now marine deposits of Mastogloia smithii allow dating which is between 9.8 and 8.5 ka cal. BP. Periods of high salinity were associated with even more distinct deposits.
Continuing sea level rise during this stage deepened the straits connecting the body with the ocean, thus increasing the influx of salt water.
A great hydrographic shift occurred c. 9850 years ago, which corresponds to shifts in currents in the Skagerrak, Kattegat and the Norwegian Channel, as they transition to the modern circulation system in the eastern North Sea. This is a consequence of the opening, and deepening, of Strait of Dover and the Danish straits and increased Atlantic water inflow. Thereafter this caused the South Jutland Current. Between 9850 and 8550 years ago the body of water became brackish, starting from the southern parts closest to the ocean and spreading to its centre and finally the shallow, ice-prone, well-watered Gulf of Finland and Gulf of Bothnia.
The overwhelming by brackish water happened at different times at different places in the Baltic basin. As well as the Ancylus Lake there were isolated lake basins. Baltic relative sea levels were different when these events happened with factors such at land rebound and the level of the world ocean being important. Relative sea level data points show negative tendencies in the northern Baltic region and positive ones in the southern region. The initial event in the south western portion of the Baltic Basin at about 9.8 ka cal. BP was at 23 to 22 m (75 to 72 ft) below present sea level. About 9.5 to 9.1 ka cal. BP, the relative sea level at Lomtjärn in Ångermanland, northern Sweden was around 180 m (590 ft). More recently than this at 8.9 ka cal. BP the Usedom/Rügen islands region of Germany, was inundated by sea water when 16 m (52 ft) below sea level. The stable and low relative sea levels found in Haväng and Pärnu in the eastern Baltic suggest that sea-level rise in the world's oceans was not the only factor in the time of inundation by a connection to the world ocean.
The marine microfossil record in today's deepest part of the Baltic Sea shows before 7.1 ka cal. BP, the freshwater surface diatoms Aulacoseira islandica and Stephanodiscus neoastraea and other evidence of a low productivity ecosystem, with transient greater productivity in response to brackish conditions.
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Mastogloia Sea
The Mastogloia Sea (also Early Littorina Sea, Initial Littorina Sea) is one of the prehistoric stages of the Baltic Sea in its development after the last ice age. It is characterised by distinctive deposits of the calciferous shell of species of the diatom Mastogloia that were used for paleoenvironmental reconstructions. This transition took place at different times in different parts of the Baltic basin c. 9000 years ago following the Ancylus Lake stage and preceding the full Littorina Sea stage.
Towards its demise, the Ancylus Lake was falling, having partly eroded and scouring away at its new outlet at the Great Belt. It reached sea level c. 9800 years ago, making it the Mastogloia Sea.
At this time global sea level was rising rapidly due to the melting of vast tracts of the great ice age ice sheets. As a result, some sea (salt) water started to penetrate into the basin through the Danish Straits, mixing into the vast freshwater body. This led to the stage's slightly brackish conditions in the Baltic.
This phase of the body of water takes its name from the brackish water-dwelling diatom genus Mastogloia, the species of which are characteristic of the geological deposits of this stage. As fresh water lakes became part of the sea identification in the now marine deposits of Mastogloia smithii allow dating which is between 9.8 and 8.5 ka cal. BP. Periods of high salinity were associated with even more distinct deposits.
Continuing sea level rise during this stage deepened the straits connecting the body with the ocean, thus increasing the influx of salt water.
A great hydrographic shift occurred c. 9850 years ago, which corresponds to shifts in currents in the Skagerrak, Kattegat and the Norwegian Channel, as they transition to the modern circulation system in the eastern North Sea. This is a consequence of the opening, and deepening, of Strait of Dover and the Danish straits and increased Atlantic water inflow. Thereafter this caused the South Jutland Current. Between 9850 and 8550 years ago the body of water became brackish, starting from the southern parts closest to the ocean and spreading to its centre and finally the shallow, ice-prone, well-watered Gulf of Finland and Gulf of Bothnia.
The overwhelming by brackish water happened at different times at different places in the Baltic basin. As well as the Ancylus Lake there were isolated lake basins. Baltic relative sea levels were different when these events happened with factors such at land rebound and the level of the world ocean being important. Relative sea level data points show negative tendencies in the northern Baltic region and positive ones in the southern region. The initial event in the south western portion of the Baltic Basin at about 9.8 ka cal. BP was at 23 to 22 m (75 to 72 ft) below present sea level. About 9.5 to 9.1 ka cal. BP, the relative sea level at Lomtjärn in Ångermanland, northern Sweden was around 180 m (590 ft). More recently than this at 8.9 ka cal. BP the Usedom/Rügen islands region of Germany, was inundated by sea water when 16 m (52 ft) below sea level. The stable and low relative sea levels found in Haväng and Pärnu in the eastern Baltic suggest that sea-level rise in the world's oceans was not the only factor in the time of inundation by a connection to the world ocean.
The marine microfossil record in today's deepest part of the Baltic Sea shows before 7.1 ka cal. BP, the freshwater surface diatoms Aulacoseira islandica and Stephanodiscus neoastraea and other evidence of a low productivity ecosystem, with transient greater productivity in response to brackish conditions.