The Development of the Baltic Sea Basin During the Last 130 ka

  • Thomas Andrén
  • Svante Björck
  • Elinor Andrén
  • Daniel Conley
  • Lovisa Zillén
  • Johanna Anjar
Part of the Central and Eastern European Development Studies (CEEDES) book series (CEEDES)


During the Eemian interglacial 130–115 ka BP, the hydrology of the Baltic Sea was significantly different from the Holocene. A pathway between the Baltic basin and the Barents Sea through Karelia existed during the first ca. 2.5 ka of the interglacial. Both sea surface temperature and salinity of the SW Eemian Baltic Sea were much higher, ca. 6°C and 15‰, respectively, than at present. A first early Weichselian Scandinavian ice advance is recorded in NW Finland during marine isotope stage (MIS) 4 and the first Baltic ice lobe advance into SE Denmark is dated to 55–50 ka BP. From the last glacial maximum that was reached ca. 22 ka BP, the ice sheet retreated northward with a few still-stands and readvances; however, by ca. 10 ka BP the entire basin was deglaciated. Weak inflows of saline water were registered in the southern and central Baltic Sea ca. 9.8 ka BP with full brackish marine conditions reached at ca. 8 ka BP and the maximum Holocene salinity was recorded between 6 and 4 ka BP. The present Baltic Sea is characterized by a marked halocline preventing the vertical water exchange resulting in hypoxic bottom conditions in the deeper part of the basin.


Baltic Sea Eemian Scandinavian ice sheet Weichselian Baltic Ice Lake Yoldia Sea Ancylus Lake Littorina Sea Hypoxia 


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Copyright information

© Springer-Verlag Berlin Heidelberg 2011

Authors and Affiliations

  • Thomas Andrén
    • 1
  • Svante Björck
    • 2
  • Elinor Andrén
    • 1
  • Daniel Conley
    • 2
  • Lovisa Zillén
    • 2
  • Johanna Anjar
    • 2
  1. 1.School of Life Sciences, Södertörn UniversityHuddingeSweden
  2. 2.Department of Earth and Ecosystem Sciences, Division of Geology, Quaternary SciencesLund UniversityLundSweden

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