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Instytut Archeolgoii i Etnologii Polskiej Akademii Nauk
Lacustrine sediments from the archaeological site at Dąbki are represented by detritus gyttja intercalated by shell-gyttja. The thickness of these sedim ents in the central part of the ancient lake reach over 7 m and in the near-shore part - about 2 m. The described sediments are mainly of M iddle H olocene age. All the species of molluscs noted in these sediments are known in the present-day fauna of Poland. The changes of assem blages reflect the evolution of the lake. In its early phase it was a low peat-bog passing into a flat water basin. In the next phase the lake developed and a gyttja with a rich fauna are deposited. During the late phase the basin are filled with sediments and strongly overgrown by reed passing into a peat-bog with small water bodies
oai:rcin.org.pl:60709 ; 0079-7138
IAiE PAN, call no. P III 149 ; IAiE PAN, call no. P III 272 ; IAiE PAN, call no. P III 353 ; click here to follow the link
Copyright-protected material. May be used within the limits of statutory user freedoms
Institute of Archaeology and Ethnology of the Polish Academy of Sciences
Library of the Institute of Archaeology and Ethnology of the Polish Academy of Sciences
Ministry of Science and Higher Education ; Activities popularizing science (DUN)
Feb 2, 2022
Dec 2, 2016
289
https://rcin.org.pl./publication/80060
Edition name | Date |
---|---|
Alexandrowicz, Stefan Witold, 1991, The malacofauna of the Holocene lacustrine sediments of Dąbki near Darłowo | Feb 2, 2022 |
Bogaczewicz-Adamczak, Bożena (1948– )
Ilkiewicz, Jolanta
Alexandrowicz, Stefan Witold (1930– )
Wirska-Parachoniak, Maria
Kozłowski, Stefan Karol (1938– )
Dzięczkowski, Andrzej
Libera, Jerzy