scholarly journals Palaeobotanical record of the Eemian Interglacial succession at the Jagodne site (Garwolin Plain, central Poland)

2021 ◽  
Vol 65 (2) ◽  
Author(s):  
Aleksandra BOBER ◽  
Dorota BRZOZOWICZ ◽  
Danuta DRZYMULSKA ◽  
Marcin ŻARSKI ◽  
Magdalena SUCHORA
2018 ◽  
Vol 58 (2) ◽  
pp. 219-229
Author(s):  
Aleksandra Bober ◽  
Irena Agnieszka Pidek ◽  
Marcin Żarski

AbstractThe paper reports pollen analyses of 47 samples from palaeolake sediments at WH-15 Struga near Puznówka on the Garwolin Plain in central Poland. The pollen succession covers Late Saalian (MIS-6) and fully developed Eemian (MIS-5e) successions. The Late Saalian section is well developed (more than 2 m thick) and contains sub-zones reflecting the alternating dominance of steppe-tundra and boreal forest communities. The analysed Eemian succession is an uncommon succession described as a variant with early appearance and culmination of Tilia. In these terms, the successions of WH-15 Struga resemble those of sites of the Eemian interglacial known from the vicinity of Warsaw: Błonie, Warszawa-Żoliborz and Warszawa-Wola. The WH-15 Struga site is one of several recently discovered fossil sites of Eemian lakes on the Garwolin Plain, constituting the southern fragment of the extensive Eemian lakeland in the Polish Lowland.


2014 ◽  
Vol 54 (2) ◽  
pp. 279-304 ◽  
Author(s):  
Aleksandra Majecka

Abstract The vegetation of the Eemian interglacial and Early Vistulian glaciation was reconstructed on the basis of pollen analysis, biogenic and mineral-biogenic sediments from the Żabieniec Południowy locality. It was revealed that the present-day fossil reservoir was formerly a lake existing continuously from the decline of the Warta stadial (LG MPG) to the end of the Early Vistulian (EV4). The upper Plenivistulian age of top sediments, previously accepted on the basis of the radiocarbon date 24 200 ± 350 yrs BP (uncalibrated), was not confirmed by pollen analysis. In the pollen record from the nearby Żabieniec mire a break in biogenic accumulation corresponding to the Lower and Middle Plenivistulian was discovered. In view of the character of Plenivistulian morphogenesis in that area it appears that the deposits of both basins illustrate the development of one large melt-out depression during the whole postglacial period.


2013 ◽  
Vol 56 (2) ◽  
pp. 89-112
Author(s):  
Radomir Jaskuła ◽  
Anna Stępień ◽  
Przemysław Włodarczyk ◽  
Iwona Słowińska-Krysiak

Lethaia ◽  
2007 ◽  
Vol 40 (2) ◽  
pp. 139-151 ◽  
Author(s):  
MICHAŁ ZATOŃ ◽  
LOÏC VILLIER ◽  
MARIUSZ A. SALAMON

Boreas ◽  
2020 ◽  
Author(s):  
Daniela Müller ◽  
Rik Tjallingii ◽  
Mateusz Płóciennik ◽  
Tomi P. Luoto ◽  
Bartosz Kotrys ◽  
...  

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