TY - JOUR N2 - The Vistulian decline was a period of rapid environmental events. The authors correlated ages of the last Scandinavian Ice Sheet limits in northern Poland with ages of prominent events adapting the conditions of periglacial environment of Central Poland in response to the Late Vistulian climate warming. Ages from previous thematic geological and palaeogeographical studies were collected. The approach used indicates that despite methodological uncertainties and sometimes inconsistency of ages, it is especially helpful in timing of first warming signals (ca. 19–18 cal ka BP) and establishing of environmentally bipartite 3 millennia of the Oldest Dryas in the extraglacial zone. Abrupt warming at the onset of the Bølling-Allerød is well registered in biotic and abiotic archives available from Central Poland and remains in agreement with the large recession of the southern ice sheet margin. L1 - http://czasopisma.pan.pl/Content/110292/PDF/5_Dzieduszynska.pdf L2 - http://czasopisma.pan.pl/Content/110292 PY - 2019 IS - Iss. 2 EP - 145 DO - 10.24425/sq.2019.126385 KW - radiometric methods KW - 14C probability density function KW - extraglacial environment KW - last glacial phases KW - Late Pleistocene A1 - Dzieduszyńska, Danuta A. A1 - Forysiak, Jacek PB - Committee for Quaternary Research PAS PB - Institute of Geological Sciences PAS VL - vol. 36 DA - 2019.11.03 T1 - Chronostratigraphy of the late Vistulian in central Poland and the correlation with Vistulian glacial phases SP - 137 UR - http://czasopisma.pan.pl/dlibra/publication/edition/110292 T2 - Studia Quaternaria ER -