The Łanięta site with fossil lake deposits is situated just in front of the maximum extent of Vistulian Glaciation ice. Palynological analysis shows that lake accumulation lasted through the Eemian Interglacial and almost the whole Early Vistulian, the longest record of this time interval in this part of Poland. Two warm interstadial-rank oscillations (Brörup and Odderade) and two stadials have been distinguished during the Early Vistulian. The older of these is correlated with the Herning Stadial while younger one equates with the Rederstal Stadial of the German succession
During the maximum of the last glaciation the Vistula ice lobe was one of the key morphological elem...
Though the stratigraphical and palaeogeographical framework of the Quaternary in Poland is still to ...
Our high-resolution data of pollen and macrofossils from 2 cores taken from the Jagodne site (Garwol...
The stratigraphy and palaeogeography of Quaternary deposits under lying the Oleoenica Plain were inv...
Eemian Interglacial lacustrine sediments at Leszczyno are situated within the area of theWarta Glaci...
The borehole at Radówek (Łagów Lakeland, western Poland) was made during cartographic works for the ...
Abstract: Stratigraphy of the Vistulian glacial events in the southern part of the Lower Vistula re...
The Vistulian decline was a period of rapid environmental events. The authors correlated ages of the...
The buried and present-day Vistula valleys has developed along tectonic linear structures of NW-SE t...
Lake sediments of the Mazovian Interglacial were found in boreholes Kasyldów and Wola Okrzejska 48, ...
The paper presents the data on an Eemian-Late Glacial sedimentary sequence from the Zwierzyniec site...
In the upper part of the Lower Vistul0 fonnation in the Lower VistuJa Region and the Elbl~g Elevatio...
Palynologic analysis of biogenic sediments from the borehole at Krzyz6wki near Kolo indicated an inc...
Ice sheet of the Wartanian Glaciation and their deposits shaped the landscape of the Węgrów Basin. B...
Many terrestrial pollen profiles from Poland (and a few pollen records from other parts of Central E...
During the maximum of the last glaciation the Vistula ice lobe was one of the key morphological elem...
Though the stratigraphical and palaeogeographical framework of the Quaternary in Poland is still to ...
Our high-resolution data of pollen and macrofossils from 2 cores taken from the Jagodne site (Garwol...
The stratigraphy and palaeogeography of Quaternary deposits under lying the Oleoenica Plain were inv...
Eemian Interglacial lacustrine sediments at Leszczyno are situated within the area of theWarta Glaci...
The borehole at Radówek (Łagów Lakeland, western Poland) was made during cartographic works for the ...
Abstract: Stratigraphy of the Vistulian glacial events in the southern part of the Lower Vistula re...
The Vistulian decline was a period of rapid environmental events. The authors correlated ages of the...
The buried and present-day Vistula valleys has developed along tectonic linear structures of NW-SE t...
Lake sediments of the Mazovian Interglacial were found in boreholes Kasyldów and Wola Okrzejska 48, ...
The paper presents the data on an Eemian-Late Glacial sedimentary sequence from the Zwierzyniec site...
In the upper part of the Lower Vistul0 fonnation in the Lower VistuJa Region and the Elbl~g Elevatio...
Palynologic analysis of biogenic sediments from the borehole at Krzyz6wki near Kolo indicated an inc...
Ice sheet of the Wartanian Glaciation and their deposits shaped the landscape of the Węgrów Basin. B...
Many terrestrial pollen profiles from Poland (and a few pollen records from other parts of Central E...
During the maximum of the last glaciation the Vistula ice lobe was one of the key morphological elem...
Though the stratigraphical and palaeogeographical framework of the Quaternary in Poland is still to ...
Our high-resolution data of pollen and macrofossils from 2 cores taken from the Jagodne site (Garwol...