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Development of a Litorina Bay at Epoo, near Porvoo, southern Finland
Author(s) -
H. Haila,
Kaarina SarmajaKorjonen,
A. Uutela
Publication year - 1991
Publication title -
bulletin of the geological society of finland
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.4
H-Index - 24
eISSN - 1799-4632
pISSN - 0367-5211
DOI - 10.17741/bgsf/63.2.004
Subject(s) - geology , peat , radiocarbon dating , holocene , bay , shore , brackish water , sea level , oceanography , altitude (triangle) , sediment , diatom , quaternary , physical geography , geomorphology , paleontology , archaeology , geography , salinity , geometry , mathematics
HAILA, HEIKKI, SARMAJA-KORJONEN, KAARINA and UUTELA, ANNELI, 1991: Development of a Litorina Bay at Epoo, near Porvoo, southern Finland. Bull. Geol. Soc. Finland 63, Part 2, 105—119. A sediment sequence at Epoo, municipality of Porvoo, on the South coast of Finland, altitude 25 m a.s.l., was studied for Holocene shoreline displacement in the Baltic Sea basin. The sediment sequence is made up of sand, clay-gyttja and drift peat deposited during the Ancylus and Litorina stages of the Baltic Sea. Two cores of clay-gyttja with an intervening sand layer were analysed for diatoms and pollen. The composition of the diatom flora changes from typical fresh-water species of the Ancylus Lake to brackish-water flora indicating transition to the Litorina Sea. The sequence shows a gradual change of a group of separate islands in the Ancylus Lake to larger complexes of dry land because of uplift. As two necks of land were formed, the site developed into a sheltered brackish-water bay, and drift peat accumulated. A radiocarbon age of 6130 ± 50 yr BP obtained from the top of the drift peat links the shore with the Litorina regression. The shore displacement history of the Helsinki-Porvoo area is discussed.

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