Late Weichselian and Holocene record of the paleoenvironmental changes in a small river valley in Central Poland

2016 ◽  
Vol 135 ◽  
pp. 24-40 ◽  
Author(s):  
Dominik Pawłowski ◽  
Ryszard K. Borówka ◽  
Grzegorz A. Kowalewski ◽  
Tomi P. Luoto ◽  
Krystyna Milecka ◽  
...  
2014 ◽  
Vol 324 ◽  
pp. 99-114 ◽  
Author(s):  
Danuta A. Dzieduszyńska ◽  
Piotr Kittel ◽  
Joanna Petera-Zganiacz ◽  
Stephen J. Brooks ◽  
Katarzyna Korzeń ◽  
...  

2011 ◽  
Vol 4 (1) ◽  
pp. 7-20
Author(s):  
Jacek Forysiak ◽  
Milena Obremska ◽  
Juliusz Twardy

Abstract Based on palaeobotanical analyses of organic deposits, as well as geomorphological and geological studies at four sites in various geomorphological locations in relation to tributaries of the Bzura River, the presence of traces of human activity, its intensiveness, and classification to cultural levels were analysed. A pattern of later and later settlement in areas remote from the axis of the Warsaw-Berlin streamway was observed along with the gradual introduction of settlement from river valley bottoms to watershed zones.


2015 ◽  
Vol 370 ◽  
pp. 12-28 ◽  
Author(s):  
Dominik Pawłowski ◽  
Krystyna Milecka ◽  
Piotr Kittel ◽  
Michał Woszczyk ◽  
Waldemar Spychalski

2014 ◽  
Vol 41 (4) ◽  
pp. 361-368 ◽  
Author(s):  
Danuta Dzieduszyńska ◽  
Joanna Petera-Zganiacz ◽  
Juliusz Twardy ◽  
Piotr Kittel ◽  
Piotr Moska ◽  
...  

AbstractResults of OSL dating and sedimentary studies from the profile of the low alluvial terrace of the middle Warta River are presented. The samples were dated using the single-aliquot regenera-tive method. Dating was used to establish a timing of the Weichselian Late Glacial events in the river valley environment. Stable conditions on the floodplain are expressed by the deposition of organic-rich series radiocarbon dated at 12 900-12 600 cal BP and 11 600-10 770 cal BP. Samples for OSL dating were collected from the mineral material deposited during the intensification of flood events during the Weichselian decline. The results obtained for the alluvia range from 12.78 ± 0.62 ka b2k to 14.33 ± 0.74 ka b2k. Sedimentological criteria allowed to distinguish between particular flood events. Overestimation of OSL ages is probably a result of rapidity of environmental changes in that time.


2020 ◽  
Vol 103 ◽  
pp. 102731
Author(s):  
Flávio Lima Lorente ◽  
Darciléa Ferreira Castro ◽  
Mariah Izar Francisquini ◽  
Luiz Carlos Ruiz Pessenda ◽  
Neuza Araújo Fontes ◽  
...  

2009 ◽  
Vol 207 (1-2) ◽  
pp. 26-41 ◽  
Author(s):  
Wojciech Wysota ◽  
Paweł Molewski ◽  
Robert J. Sokołowski

2012 ◽  
Vol 62 (4) ◽  
pp. 535-559 ◽  
Author(s):  
Norbert Keutgen ◽  
Zbigniew Remin ◽  
Ireneusz Walaszczyk

ABSTRACT Keutgen, N., Remin, Z. and Walaszczyk, I. 2012. Early representatives of the belemnite genus Belemnella (Cephalopoda) from the uppermost Campanian-Lower Maastrichtian of the Middle Vistula River section, central Poland. Acta Geologica Polonica, 62 (4), 535-559. Warszawa. Representatives of the belemnite genus Belemnella from the uppermost Campanian and lowermost Maastrichtian of the Middle Vistula River Valley section (central Poland) have been studied, using the species concept proposed by Schulz in 1979. Results have been compared to a recently proposed new interpretation of the genus Belemnella based on artificial neural networks, as put forward by Remin in 2007 and 2012. In the interval studied, four taxa have been recognised: Bln. longissima, Bln. inflata, Bln. obtusa and Bln. vistulensis, the last-named being a senior synonym of Bln. pseudobtusa. Three additional forms have been left in open nomenclature: Bln. cf. lanceolata , Bln. ex gr. lanceolata/inflata and Belemnella sp. Based on their documented vertical ranges, three Belemnella standard zones, as originally distinguished in the Kronsmoor section by Schulz (1979), northern Germany, have been defined, in ascending order: the Bln. lanceolata, Bln. vistulensis and Bln. obtusa zones. The bases of the lanceolata and obtusa zones in the Middle Vistula River Valley section can be directly correlated with the same zones at Kronsmoor, and appear to be isochronous within limits of stratigraphic resolution. The base of the vistulensis Zone (Bln. vistulensis according to the species concept of Schulz in 1979), however, is probably diachronous, being older in the Middle Vistula section. Although Schulz’s and Remin’s species concepts differ quite considerably, they do result in similar stratigraphic subdivisions of the Kronsmoor and Middle Vistula River sections.


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