Evolution of the Baltic Sea
Pleistocene
Eemian Sea (130,000–115,000 BC)
Ice sheets and seas (115,000–12,600 BC)
Holocene
Baltic Ice Lake (12,600–10,300 BC)
Yoldia Sea (10,300–9,500 BC)
Ancylus Lake (9,500–8,000 BC)
Mastogloia Sea (8,000–7,500 BC)
Littorina Sea (7,500–4,000 BC)
Modern Baltic Sea (4,000 BC–present)

The Mastogloia Sea is one of the prehistoric stages of the Baltic Sea in its development after the last ice age. This took place c. 8000 years ago following the Ancylus Lake stage and preceding the Littorina Sea stage.[Note 1]

Overview

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. 8500 years ago, making it the Mastogloia Sea.[1][2]

At this time global sea level was rising rapidly due to the melting of vast tracts of the great ice age ice sheets.[3] 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.[4][5]

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. 8500 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.[6]

Between 8000 and 7000 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.

Successor

The phase of more saline conditions and higher sea level than today marks the Littorina Sea stage.[7]

The Mastogloia Sea stage thus is between the freshwater Ancylus Lake stage and the Littorina Sea stage.[8][9]

Disputed status

Many researchers have been unwilling to recognize the Mastogloia Sea as a separate stage in the development of the Baltic Sea, favouring including it in either the Ancylus Lake stage or the Littorina Sea stage.[10][11]

In stratigraphy of Baltic sediments the Mastogloia stage is difficult to detect, its sediments being visibly identical to those of the Ancylus Lake.[12][13] Even the fossil diatom content of the phase's sediments – cited by researchers as the key method of distinguishing deposits of different Baltic stages – is ambiguous, in many places showing no difference from that of Ancylus deposits, and at best including an admixture of Mastogloia diatoms in an otherwise typical Ancylus flora.[14] Deposits of the Littorina Sea phase show a drastic change both in the visible characteristics of the sediment and its diatoms.[15][16] Some academics prefer to include the phase as the early Littorina Sea stage, being the time after resumption of a marine (sea) connection.[17]

In spite of these objections, though, the concept of the phase persists in literature concerning the development of the Baltic Sea. It has been noted that it is useful in maintaining the clarity of the system, delimiting the period with undeniable if slight marine influence following the fall of the Ancylus Lake to sea level that pre-dates the great changes from the outset of the Littorina Sea stage.[18]

Notes

  1. ^ Dates used in this article are radiocarbon dating years before present (meaning, for so many historic papers tally with this, the year 1950 AD). As calendar years before present, all dates would be a few hundred years older.[clarification needed]

References

  1. ^ Björck 1995.
  2. ^ Donner 1995
  3. ^ (Fleming et al. 1998)
  4. ^ Donner 1995
  5. ^ Eronen 1974
  6. ^ Gyllencreutz, Richard (15 July 2005). "Late Glacial and Holocene paleoceanography in the Skagerrak from high-resolution grain size records". Palaeogeography, Palaeoclimatology, Palaeoecology. 222 (3–4). © 2005 Elsevier B.V: 344–369. Bibcode:2005PPP...222..344G. doi:10.1016/j.palaeo.2005.03.025.
  7. ^ Miettinen 2004
  8. ^ Donner 1995
  9. ^ Hyvärinen et al. 1988
  10. ^ Hyvärinen et al. 1988.
  11. ^ Miettinen 2002
  12. ^ Donner 1995
  13. ^ Eronen 1983
  14. ^ Eronen 1974
  15. ^ Donner 1995
  16. ^ Eronen 1974
  17. ^ Hyvärinen et al. 1988
  18. ^ Eronen 1983
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