Lagoon sediments in the central part of the Vistula spit: geochronology, sedimentary environment and peculiarities of geological settings

• Autorzy: Bitinas A. , Boldyrev V. , Damušyte A. , Grigiene A. , Vaikutiene A. , Žaromskis R.
• Języki publikacji: EN

Abstrakty

EN

Lagoon gyttja layers occurring in anomalously high position (up to 2.5 m above the present-day sea level) are known from the central part of the Vistula Spit (Kaliningrad region of the Russian Federation). Complex investigations of lagoon sediments (gyttja, sand), including radiocarbon (14C) dating as well as mollusc, pollen and diatom analyses, have been carried out in 2004–2005. The results of these investigations indicate that the lagoon sediments were deposited in the Late Subboreal–Early Subatlantic period in a shallow freshwater, overgrown basin periodically influenced by brackish water. The anomalously high level of the lagoon gyttja is determined by neotectonic activity of Earth’s crust blocks.

Słowa kluczowe

EN

gyttja; lagoon sediments; neotectonics; Vistula Spit; Baltic Sea

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Polish Geological Institute Special Papers
• Rocznik: 2008
• Tom: Vol. 23
• Strony: 9--20
• Opis fizyczny: bibliogr. 27 poz., rys., wykr.

Twórcy

autor

Bitinas A.

autor

Boldyrev V.

autor

Damušyte A.

autor

Grigiene A.

autor

Vaikutiene A.

autor

Žaromskis R.

• Geological Survey or Lithuania, 35 Konarskio St, 03123 Vilnius, Lithuania,

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