Eemian and Vistulian (Weichselian) paleoenvironmental changes: A multi-proxy study of sediments and mammal remains from the Ławy paleolake (Eastern Poland)

Hrynowiecka, Anna; Żarski, Marcin; Jakubowski, Gwidon; Nadachowski, Adam; Pawłowska, Kamilla; Pawłowski, Dominik; Szymanek, Marcin; Nast, Dariusz

doi:10.1016/j.quaint.2016.10.033

Cited by 14 publications

(2 citation statements)

References 33 publications

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“…Pollen records show a rather unstable environment with repeated changes from tundra-like grassland to forest-tundra and taiga vegetation (e.g. Duprat-Oualid et al, 2017;Engel et al 2010;Hrynowiecka et al, 2018;Kulesza et al, 2020;Maier et al, 2021;Sirocko et al, 2016;Van Andel and Tzedakis 1996;Gerlach et al, 1993;Szczepanek et al, 2007;Maier et al, 2021). The above-mentioned phenomena of cryoturbation and solifluction occurring during the colder phases of MIS 3 and at the transition to MIS 2 were recorded in the periglacial transformation of the soil complex, especially in the younger part.…”

Section: Loess Stratigraphymentioning

confidence: 99%

State‐of‐the‐art overview of the Loess Palaeolithic of Poland

Valde‐Nowak

Łanczont

2021

J Quaternary Science

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In Poland, loess mainly occurs in the southern part of the country, in the Polish Uplands, and on the northern foreland of the Sudetes and the Carpathians. Most of these sediments come from the time of the last glaciation-the Vistulian (Weichselian) glaciation. Thin covers of loess from the penultimate glaciation have been preserved in Upper Silesia. Only a few sites from the Middle Palaeolithic remain in the loess. In the eastern part of Poland loess creates profiles several metres high. Discoveries in this zone represent the cultural sequence from the transition from the Middle to Upper Palaeolithic. We know more traces of various cultures from the Upper Palaeolithic exist. The study attempts to synchronise profiles from selected archaeological open-air sites, outlines of the history of research on loess sites, and attempts to explain terminological and conceptual issues. The issue of loess in the cave site profiles will not be discussed in the article.

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Section: Loess Stratigraphymentioning

confidence: 99%

State‐of‐the‐art overview of the Loess Palaeolithic of Poland

Valde‐Nowak

Łanczont

2021

J Quaternary Science

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“…The high resolution chronostratigraphy of the paleo-lakes is a main research topic, which has been deeply studied by several authors [17][18][19][20][21][22][23][24][25][26][27]. In particular, the Ibate paleolake has shown a distal lacustrine environment with low-oxygen conditions in its bottom waters [17].…”

Section: Introductionmentioning

confidence: 99%