Temat: oxbow deposits - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: Early Yistulian deposits at Świnna Poręba, western Outer Carpathians (Southern Poland)
Autorzy:: Bińka, Krzysztof
Grzybowski, Krzysztof
Powiązania:: https://bibliotekanauki.pl/articles/2026787.pdf
Data publikacji:: 2001
Wydawca:: Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:: Carpathians
Early Vistulian
pollen
alluvia
oxbow deposits
Opis:: Alluvial and oxbow deposits preserved 18 m above the Skawa River valley floor are related to the Early Vistulian. Pollen analysis of the two mainly terrestrial profiles revealed a boreal forest succession. The age of the deposits is discussed.
Źródło:: Studia Quaternaria; 2001, 18; 11-16
1641-5558
2300-0384
Pojawia się w:: Studia Quaternaria
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 2.

Tytuł:: Younger Dryas Cladocera assemblages from two valley mires in central Poland and their potential significance for climate reconstructions
Autorzy:: Pawłowski, Dominik
Powiązania:: https://bibliotekanauki.pl/articles/94461.pdf
Data publikacji:: 2012
Wydawca:: Uniwersytet im. Adama Mickiewicza w Poznaniu
Tematy:: Younger Dryas
Cladocera
oxbow-lake deposits
valley mire
climate
local conditions
młodszy dryas
złoża
starorzecze
torfowisko
klimat
warunki lokalne
Opis:: Two sections of sediment from small oxbow-lake infillings located in different river valleys in central Poland were studied by cladoceran analysis in order to examine the response of aquatic ecosystems to the Younger Dryas. Lithological and geochemical records, as well as chydorid (Chydoridae) ephippia analysis were also used to reconstruct Younger Dryas climate trends. A high concentration of cladocerans, as well as the presence of Cladocera taxa preferring warmer water, was found. It is likely that local processes in the oxbow lakes were important, because the presence of warm-preferring taxa was also related to their habitats and their development. Yet local environmental forces, such as the influence of the rivers, habitat modification, macrophyte abundance, and eutrophication, were not only major factors to affect the Cladocera diversity in the Younger Dryas. The observation of changes in the composition and concentration of Cladocera in oxbow-lake infillings indicates that most of the changes occurred in response to climate changes.
Źródło:: Geologos; 2012, 18, 4; 237-249
1426-8981
2080-6574
Pojawia się w:: Geologos
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 3.

Tytuł:: Middle Pleistocene fluvial, lacustrine and glaciolacustrine sediments of the Czyżów and Kuców Formations (Kuców 9, 10 and 16 sections), Bełchatów outcrop, central Poland – the problem of stratigraphical interpretation
Autorzy:: Krzyszkowski, Dariusz
Wachecka-Kotkowska, Lucyna
Nita, Małgorzata
Wieczorek, Dariusz
Powiązania:: https://bibliotekanauki.pl/articles/2025048.pdf
Data publikacji:: 2021
Wydawca:: Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:: lake deposits
fluvial deposits
oxbow
Mazovian
Ferdynandovian
Kleszczów Graben
central Poland
Opis:: The article presents results of research of three sections (Kuców 9, 10 and 16). Two of them record fluvial and lacustrine interglacial sediments and the third, cold-stage glaciolacustrine sediments. They were formed inside the Miocene – Pliocene syncline depressions in a central part of the southern horst within the Kleszczów Graben. Fluvial and lacustrine deposits of the Middle Pleistocene Interglacial (Mazovian or Ferdynandovian in the Czyżów Formation) are described from the Kuców 9 and 10 sections. Their sediments are located in marginal parts of a buried river valley and within an oxbow palaeolake, then covered by glaciofluvial deposits of the Ławki (Early Saalian) and Rogowiec (Late Saalian) Formations. The Kuców 16 section comprises ice-dam sandy lithofacies (Kuców Formation, Elsterian) of a marginal part in a proglacial lake. Two pollen diagrams of K65/15 and Kuców 9 sections represent the Mazovian (Holsteinian) succession, although in the Kuców 9 section some features are typical for the Ferdinandovian succession.
Źródło:: Studia Quaternaria; 2021, 38, 1; 53-66
1641-5558
2300-0384
Pojawia się w:: Studia Quaternaria
Dostawca treści:: Biblioteka Nauki

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