AB

Bibliografia publikacji pracowników
Państwowej Szkoły Wyższej w Białej Podlaskiej

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


Zapytanie: LAST GLACIAL TERMINATION
Liczba odnalezionych rekordów: 1



Przejście do opcji zmiany formatu | Wyświetl/ukryj etykiety | Wyświetlenie wyników w wersji do druku | Pobranie pliku do edytora | Nowe wyszukiwanie
1/1
Nr opisu: naRychel Joanna Sokołowski Robert J. Sieradz Dominika Hrynowiecka Anna Mirosław-Grabowska Joanna Sienkiewicz Elwira^aoriginal-article^bOryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym1.900IF^a997000^b998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM^a009997.100^b009899.000^c009999.000^d009899.000202320232023Late Pleniglacial - Late Glacial climate oscillations detected in the organic lacustrine successi00000443510000000358AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGhttps://onlinelibrary.wiley.com/doi/10.1002/jqs.3477100^a0267-8179^bQ^e1099-1417^iX^jXY^kQ012470^a003^b003^c2022-11-08, 13:07^d2024-06-25, 14:14^e3219968932^f3024798825^aLate Pleniglacial - Late Glacial climate oscillations detected in the organic lacustrine succession at the Lipowo site, north-eastern Poland^aJournal of Quaternary Science^a2023^bVol. 38^cissue 2^dp. 186--207^a1099-1417^b1099-1417^a2022/2023^a10.1002/jqs.3477^aZbucki, Łukasz^cx^ablock melting^aThe profile of the Lipowo palaeolake (NE Poland) preserves a record of environmental and climate changes from the Last Glacial Termination (16.5k cal ka BP), stretching from the Oldest Dryas to the youngest Allerod warm oscillation. In this interdisciplinary study of the lacustrine succession at Lipowo, we used biological and geochemical indicators and multiproxy analyses to reconstruct environmental changes in the lake ecosystem, such as mollusc, zooplankton and vegetation development, trophic state, water temperature and water level. Four cold and four warm climate oscillations of different durations were identified on this basis: the Older Dryas climate deterioration and two short-term coolings within the Allerod Interstadial, separated by warm periods in the Bolling and Allerod. The covering of the lake series by diamicton deposits from the melting of dead-ice blocks is a particularly interesting and rare phenomenon for a postglacial area. The hydrological system of the catchment was generally closed, with a periodically opening and existing flow-through lake. Over the period of the lake's existence, vegetation changed in general from steppe tundra to forest with birch and pine. For most of this time, the palaeolake was mainly oligotrophic, with increased productivity and a higher trophic level only notable during the middle Bolling.^adead-ice^aLast Glacial Termination^apalaeoenvironment reconstruction^apermafrost^apollen analysis
Autorzy: , , .
Tytuł pracy:
Tytuł pracy w innym języku: NiskaSzymanekZbuckiCiołkoRogóż-Matyszczakoriginal-article997000009997.1000267-8179003Late Pleniglacial - Late Glacial climate oscillations detected in the organic lacustrine succession at the Lipowo site, north-eastern PolandJournal of Quaternary Science20231099-14172022/202310.1002/jqs.3477Zbucki, Łukaszblock meltingThe profile of the Lipowo palaeolake (NE Poland) preserves a record of environmental and climate changes from the Last Glacial Termination (16.5k cal ka BP), stretching from the Oldest Dryas to the youngest Allerod warm oscillation. In this interdisciplinary study of the lacustrine succession at Lipowo, we used biological and geochemical indicators and multiproxy analyses to reconstruct environmental changes in the lake ecosystem, such as mollusc, zooplankton and vegetation development, trophic state, water temperature and water level. Four cold and four warm climate oscillations of different durations were identified on this basis: the Older Dryas climate deterioration and two short-term coolings within the Allerod Interstadial, separated by warm periods in the Bolling and Allerod. The covering of the lake series by diamicton deposits from the melting of dead-ice blocks is a particularly interesting and rare phenomenon for a postglacial area. The hydrological system of the catchment was generally closed, with a periodically opening and existing flow-through lake. Over the period of the lake's existence, vegetation changed in general from steppe tundra to forest with birch and pine. For most of this time, the palaeolake was mainly oligotrophic, with increased productivity and a higher trophic level only notable during the middle Bolling.dead-iceLast Glacial Terminationpalaeoenvironment reconstructionpermafrostpollen analysis : Monika : Marcin : Łukasz Jan : Urszula : Anna : Oryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym1.900IF : 998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM : 009899.000 : Q : 003 : Vol. 38 : 1099-1417
Oznaczenie wydania: NiskaSzymanekZbucki
Charakterystyka formalna:
Słowa kluczowe ang.: ;

  Wyświetl ponownie stosując format:
Wyświetl/ukryj etykiety | Wyświetlenie wyników w wersji do druku | Pobranie pliku do edytora | Nowe wyszukiwanie | Biblioteka AB