@misc{Alexandrowicz_Stefan_Witold_The_1991,
 author={Alexandrowicz, Stefan Witold},
 volume={38},
 copyright={Rights Reserved - Free Access},
 address={Wrocław},
 journal={Przegląd Archeologiczny},
 howpublished={online},
 year={1991},
 publisher={Instytut Archeolgoii i Etnologii Polskiej Akademii Nauk},
 language={eng},
 abstract={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},
 type={Text},
 title={The malacofauna of the Holocene lacustrine sediments of Dąbki near Darłowo},
 URL={http://www.rcin.org.pl/iae/Content/60709/PDF/WA308_80060_PIII149_The-malacofauna-of-t_I.pdf},
 keywords={late Mesolithic – Poland, molluscs remains, Dąbki, Darłowo commune (Poland)},
}