State of research on the Late Glacial and Holocene fluvial history in the Vistula river valley. (Etat des recherches sur l'évolution hydrologique de la vallée de la Vistule, pendant le Tardiglaciaire et l'Holocène)

Author(s):  
L. Starkel
2012 ◽  
Vol 63 (4) ◽  
pp. 50-60 ◽  
Author(s):  
Krystyna Konecka-Betley

Abstract Transformations of the natural environment in the area surrounding and encompassing the Vistula River valley during the last 20 000 years BP should be discussed with regard to radiocarbon dating of the organic matter in the documented fossil soils. Part of the 14C dates from horizons A of pedosols in the valley have already been published, for the upper part of the valley by Balwierz & Nalepka [1992], and for the lower part - by Turkowska [1992]. Palynologic analysis was also made in many of the documented sites. The most important events in the history of the valley have been supplemented by radiocarbon dating by Starkel [2001]. This report presents 14C dates measured in the buried organic horizons of fossil soils in the Middle Vistula valley between Stężyca (Dęblin area) to Liszyno (Płock area). Most datings were made in the Kampinos Forest. For mineral-organic soils the dates lie between 1080 ± 90 Gd. 19S, Laski [Urbaniak-Biernacka 1973] and 12 160 ± 260 [Gd. 4391, Mariew [Konecka-Betley 1991]. In turn, the base of the oldest peat horizon in the Kampinos Forest supplied a date of 10 S90 ± 340 Gd. 2260, Wilków [Konecka-Betley et al. 1991].


2016 ◽  
Author(s):  
Nathan Stansell ◽  
◽  
Donald T. Rodbell ◽  
Joseph M. Licciardi ◽  
Mark B. Abbott ◽  
...  

2021 ◽  
pp. 1-16 ◽  
Author(s):  
Grzegorz Wierzbicki ◽  
Piotr Ostrowski ◽  
Piotr Bartold ◽  
Filip Bujakowski ◽  
Tomasz Falkowski ◽  
...  
Keyword(s):  

The Holocene ◽  
2021 ◽  
pp. 095968362110116
Author(s):  
Lucie Juřičková ◽  
Jakub Menšík ◽  
Jitka Horáčková ◽  
Vojen Ložek

The Alps are an important hotspot of species diversity and endemism, as well as a presumed glacial refugium of several species’ groups including land snails. The recent ranges of Alpine endemics are well known, but their fluctuations during the postglacial period mirroring local climate changes are understudied. By analysing five Late Glacial and Holocene mollusc successions from two areas in the southernmost part of the Bohemian Massif (Czech Republic) situated about 100 km north of the Alps, we reveal details of these fluctuations. The Alpine endemic rocky dweller Chilostoma achates had reached the southern part of the Bohemian Massif already in the Late Glacial and disappeared in the Mid-Holocene canopy forest optimum. On the contrary, the northern boundaries of Alpine canopy forest epigeic snails extended further north than today at the turn of the Middle and Late-Holocene, pointing to a more favourable forest microclimate. The earliest known occurrences of several temperate canopy forest central European species, especially Causa holosericea and Discus perspectivus, imply the role of different areas in the Alps as their glacial refugia.


2013 ◽  
Vol 53 (2) ◽  
pp. 191-233 ◽  
Author(s):  
Aleksandra Jurochnik ◽  
Dorota Nalepka

ABSTRACT Late Glacial (since Oldest Dryas) and Holocene (to Subatlantic) changes of vegetation at the Węgliny site (south-west Poland) are reconstructed based mainly on pollen analysis of five cores from the palaeobasin (anaerobic sediments). The chronology of the described events is based on palynological comparison with the Lubsza Plain environs, based on LPAZs from several published pollen diagrams on 14C data, and multiple cryptotephra levels determined in the Węgliny profiles. The Węgliny record integrates well into the north European Holocene and Late Glacial biostratigraphic framework. The Węgliny site is the next (fourth) locality in Poland where the Laacher See Tephra (LST) horizon within the Allerød chronozone was identified.


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