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Bibliografia publikacji pracowników
Państwowej Szkoły Wyższej w Białej Podlaskiej

Baza tworzona przez Bibliotekę Akademii Bialskiej im. Jana Pawła II.


Zapytanie: SAALIAN
Liczba odnalezionych rekordów: 2



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Nr opisu: BLICATION^eOPEN_JOURNAL^aDue to the long sedimentation period (about 70 000 years) and the unique quality of the lake deposits represented by very long, monotonous layers of lacustrine chalk, the sequence at Ossówka is exceptional. We conducted highly-resolved pollen and isotope analysis of the 27-m-long, upper part of the sequence of the lake sediments covering the final stage of the Holsteinian and the early phases of the Saalian Complex (Marine Isotope Stages (MIS) 11-10). In the pollen profile three main forest interstadials (L PAZ O-3, O-5, O-7) and the intervening steppe - tundra stadials (L PAZ O-2, O-4, O-6, O-8) as well as numerous units of lower rank were identified. Interstadials were characterized mainly by the presence of well-established pine forest. Stadials in turn, represented steppe - tundra vegetation with very pronounced continental influences. Also, three clearly established phases of forest fires starting at the beginning of interstadials and gradually disappearing are interesting feature of the sequence. Fires of that scale are very rarely noted in the palynological spectra. The examined sequence is characterized by the high dynamics of changes in the post interglacial part of the profile. It provides, coupled with clear features of the Holsteinian succession and its duration, a reliable correlation with other terrestrial and marine archives.^alake deposits^apollen analysis^aSaalian
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Tytuł czasopisma:
Strony: FINAL_PUBLISHEDDue to the long sedimentation period (about 70 000 years) and the unique quality of the lake deposits represented by very long, monotonous layers of lacustrine chalk, the sequence at Ossówka is exceptional. We conducted highly-resolved pollen and isotope analysis of the 27-m-long, upper part of the sequence of the lake sediments covering the final stage of the Holsteinian and the early phases of the Saalian Complex (Marine Isotope Stages (MIS) 11-10). In the pollen profile three main forest interstadials (L PAZ O-3, O-5, O-7) and the intervening steppe - tundra stadials (L PAZ O-2, O-4, O-6, O-8) as well as numerous units of lower rank were identified. Interstadials were characterized mainly by the presence of well-established pine forest. Stadials in turn, represented steppe - tundra vegetation with very pronounced continental influences. Also, three clearly established phases of forest fires starting at the beginning of , OTHER, BEFORE_PUBLICATION
Charakterystyka merytoryczna:
Język publikacji: , (about 70 000 years) and the unique quality of the lake deposits represented by very long, monotonous layers of lacustrine chalk, the sequence at Ossówka is exceptional. We conducted highly-resolved pollen and isotope analysis of the 27-m-long, upper part of the sequence of the lake sediments covering the final stage of the Holsteinian and the early phases of the Saalian Complex (Marine Isotope Stages (MIS) 11-10). In the pollen profile three main forest interstadials (L PAZ O-3, O-5, O-7) and the intervening steppe - tundra stadials (L PAZ O-2, O-4, O-6, O-8) as well as numerous units of lower rank were identified. Interstadials were characterized mainly by the presence of well-established pine forest. Stadials in turn, represented steppe - tundra vegetation with very pronounced continental influences. Also, three clearly established phases of forest fires starting at the beginning of interstadials and gradually disappearing are interesting feature of the sequence. Fires of that scale are very rarely noted in the palynological spectra. The examined sequence is characterized by the high dynamics of changes in the post interglacial part of the profile. It provides, coupled with clear features of the Holsteinian succession and its duration, a reliable correlation with other terrestrial and marine archives.^alake deposits^apollen analysis^aSaalian
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Słowa kluczowe ang.: ing at the beginning of interstadials and gradually disappearing are interesting feature of the sequence. Fires of that scale are very rarely noted in the palynological spectra. The examined sequence is characterized by the high dynamics of changes in the post interglacial part of the profile. It provides, coupled with clear features of the Holsteinian succession and its duration, a reliable correlation with other terrestrial and marine archives.^alake deposits^apollen analysis^aSaalian
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Autorzy: , , , , , .
Tytuł czasopisma:
Uwagi: MajeckaPochocka-SzwarcRychelWoronkoZbuckiHradunovaHrychanikMamchykRylovaNowackiPielachoriginal-article996948009997.048
Tytuł pracy: HradunovaHrychanikMamchykRylovaNowackiPielachoriginal-article996948009997.0481040-6182003Revised limit of the saalian ice sheet in central EuropeQuaternary International20181040-61822017/201810.1016/j.quaint.2016.07.043Nitychoruk, Jerzyzlodowacenie WartySaalianKopia dostępna w Sekcji Bibliometrii.Model of geological structure, regional key horizons and Middle-Late Pleistocene climate in the southern part of the Polish-Belarusian cross-border areaFINAL_PUBLISHEDGeological investigations in the southern part of the Polish-Belarusian cross-border area were focused on correlation of main Middle Pleistocene stratigraphic units and on extent of the ice sheet of the Saalian Glaciation. Determination of regional stratotype horizons, establishing new key sites and sections of regional significance for Central Europe were based mostly on vegetation and paleoclimate changes recorded in glacial and interglacial lake deposits. Results of stratigraphical investigations abolished a predominant palaeogeographic image on ice sheet limits in this area. The Saalian maximum ice sheet limit was similar or even less extensive than during the subordinate Warta Stadial. Most of the area between the Middle Vistula in Poland and the Middle Dnieper in Belarus and the Ukraine was ice-free during this glaciation. On the other hand, immense glacial lobes during Saalian in the Middle Vistula and the Middle Dnieper valleys have not advanced presumably in the same time and were fed by ice moving from different parts of Scandinavia. Diversified Pleistocene tectonic uplifting in the area influenced much dynamics of the penultimate ice sheet in this part of Europe.Zbucki, Łukaszinterglacjał mazowieckiice sheet limitEuropa ŚrodkowaHolsteinian Interglacialruchy tektoniczneCentral EuropeDnieprneotectonic upliftingDnieper lobe : Aksana : Mikalai : Sergey : Tatyana : Łukasz : Monika : Oryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym1.952IF : 99969930.0000030.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR30.000PUNKTACJA UWM : 009969.000 : A : 003 : Vol. 478 : 1873-4553 : Narodowe Centrum Nauki : CC-BY-NC-ND, , , , , , , 3818839296, OTHER, , , , , , , 3524809101
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Praca recenzowana
Słowa kluczowe ang.: Zbucki Łukasz Jan^aHradunova
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