Wyniki wyszukiwania

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Diatom biofacies in the SW Gulf of Gdansk and the Vistula Lagoon (the Southern Baltic Sea) as indicators of the basin evolution in the Middle and Late Holocene

100%

Witak M.

Oceanological and Hydrobiological Studies

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2013

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tom 42

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nr 1

2

Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik

Malacofauna in cave deposits of the Udorka valley (Krakow-Czestochowa Upland)

100%

Szymanek M., Krajcarz M. T., Krajcarz M., Sudol M.

Folia Malacologica

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2016

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tom 24

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nr 1

3

Tree stumps from the bottom of the Vistula Lagoon as indicators of water level changes in the Southern Baltic during the Late Holocene

100%

Leczynski L., Miotk-Szpiganowicz G., Zachowicz J., Uscinowicz S., Krapiec M.

Oceanologia

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2007

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tom 49

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nr 2

The Vistula Lagoon is situated along the south-eastern shore of the Gulf of Gdańsk and is linked with the gulf through the Strait of Baltiysk. Separated from the open sea by the Vistula Spit, the Vistula Lagoon is a shallow body of water with a mean depth of 3 m; the bottom is covered with a layer of mud several metres thick. This article presents a unique, newly discovered locality of tree stumps occurring in situ at the bottom of the Vistula Lagoon. The radiocarbon age of the alder stumps and the top of the peat in which they are rooted is Subboreal. The alder wood was dated to 4770±35 and 3295±35 years BP. The top layers of peat were dated to 4670±40, 4410±35 and 3690±35 years BP. The considerable scatter of the dates indicates the significance of erosional processes during marine transgressions. Radiocarbon dates and pollen analyses indicate that in the late Atlantic – early Subboreal periods, the water level of the Vistula Lagoon was about 3 m lower than it is today. The −2 m level was passed no earlier than c. 3500 years ago; the −1 m level was reached around 2000 years ago.

4

Mid-Holocene foraminiferal assemblages from marine shell-bearing moraines at Hornsund, South Spitsbergen

100%

Birkenmajer K., Luczkowska E.

Bulletin of the Polish Academy of Sciences. Earth Sciences

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1996

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tom 44

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nr 4

5

Dendrochronological pine scale [1622-1996 AD] for the Malopolska Area [South Poland]

100%

Szychowska-Krapiec E.

Bulletin of the Polish Academy of Sciences. Earth Sciences

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1997

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tom 45

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nr 1

6

A diatom record of Late Holocene environmental changes in the Gulf of Gdansk

80%

Witak M.

Oceanological Studies

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2000

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tom 29

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nr 2

7

Malacofauna of Late Holocene overbank deposits in Southern Poland

80%

Alexandrowicz S. W.

Bulletin of the Polish Academy of Sciences. Earth Sciences

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1996

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tom 44

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nr 4

Ograniczanie wyników

3 Bulletin of the Polish Academy of Sciences. Earth Sciences

1 Folia Malacologica

1 Oceanologia

1 Oceanological Studies

1 Oceanological and Hydrobiological Studies

2 Witak M.

1 Alexandrowicz S. W.

1 Birkenmajer K.

1 Krajcarz M.

1 Krajcarz M. T.

1 Krapiec M.

1 Leczynski L.

1 Luczkowska E.

1 Miotk-Szpiganowicz G.

1 Sudol M.

1 Szychowska-Krapiec E.

1 Szymanek M.

1 Uscinowicz S.

1 Zachowicz J.

1 2016

1 2013

1 2007

1 2000

1 1997

2 1996

Diatom biofacies in the SW Gulf of Gdansk and the Vistula Lagoon (the Southern Baltic Sea) as indicators of the basin evolution in the Middle and Late Holocene

Malacofauna in cave deposits of the Udorka valley (Krakow-Czestochowa Upland)

Tree stumps from the bottom of the Vistula Lagoon as indicators of water level changes in the Southern Baltic during the Late Holocene

Mid-Holocene foraminiferal assemblages from marine shell-bearing moraines at Hornsund, South Spitsbergen

Dendrochronological pine scale [1622-1996 AD] for the Malopolska Area [South Poland]

A diatom record of Late Holocene environmental changes in the Gulf of Gdansk

Malacofauna of Late Holocene overbank deposits in Southern Poland