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Bibliografia publikacji pracowników
Państwowej Szkoły Wyższej w Białej Podlaskiej

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


Zapytanie: SIERADZ DOMINIKA
Liczba odnalezionych rekordów: 3



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Autorzy: .
Tytuł pracy w innym języku: 0341-8162003Evolution of a kettle hole from the Late Saalian to the HoloceneCATENA20240341-81622024/202510.1016/j.catena.2024.108229Zbucki, ŁukaszxBiałe Błota lakeThe Białe Błota paleolake, situated in the northern Masovia, is a significant site, documenting the environmental processes occurring from the Late Saalian to the Holocene. A particular reconstruction of its evolution has been attained, based on lithological, geochemical, and palynological data, alongside radiocarbon dating. This multidimensional approach allowed the authors to construct a description of the vegetation, delineated by pollen zonation and its correlation with comparable Polish sites. The Białe Błota paleolake is a small reservoir filled with organic sediments accumulating during the Late Saalian, Eemian Interglacial, Vistulian, and the Holocene. These deposits represent two separate cycles of lake accumulation, each ending with by peat sedimentation. Starting from the Late Saalian, the onset of paleolake development coincides with the melting of dead ice blocks, initiating sedimentation marked by a transition from silty sand to detritus gyttja. The transition into the Eemian is manifested by an accumulation of detritus gyttja and the establishment of a birch-pine boreal forest, indicating a climate amelioration. The climatic optimum of the Eemian represents the peak of the forest development, marked by the spread of thermophilic trees and the dominance of oak woodlands. Accompanying shifts in the sediment geochemistry underline intensified organic productivity and changing nutrient dynamics within the paleolake ecosystem. During the post-optimum of the Eemian, the gradual transition from mixed broadleaved forests to pine-dominated landscapes coincides with climatic cooling and increasing humidity. In the Vistulian, the aeolian processes related to the periglacial conditions were activated. During the Late Glacial, a reactivation of the lake and further environmental changes reflecting climatic fluctuations and vegetation responses occur. The beginning of the Holocene is manife : Q : 003 : a case study from Białe Błota, northern Masovia, central Poland : Vol. 245 : 1872-6887
Tytuł czasopisma:
Oznaczenie wydania: 0341-8162003Evolution
Kopia niedostępna:
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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
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Nr opisu:
Autorzy: , Q 003 acetolyze resistant vegetative forms of freshwater dinoflagellate based on the Lake Młynek record form Northeastern Poland Vol. 37 Narodowe Centrum Nauki 003Unique finds in palynological spectraStudia Quaternaria20201641-55582020/202110.24425/sq.2020.133751Nitychoruk, Jerzyfreshwater dinoflagellateKorelacja faz osadnictwa pradziejowego i wczesnośredniowiecznego w Polsce północno-wschodniej z przemianami środowiska przyrodniczego w świetle badań osadów jeziornych (Correlation of prehistoric and early medieval settlement phases in northeast Poland with the changes of the natural environment in the light of lacus-trine sediments study)The freshwater dinoflagellate represent microfossils which are very rarely noted in lake deposits. In Late Holocene sediments of the Lake Młynek, the Iława Lakeland, northern Poland, we identified intense blooms of algae of the genus Palatinus. They occurred primarily in the period of strong human impact during expansion of the Monastic State of the Teutonic Order. The most amazing thing is that samples in which conventional palynological maceration has been used dinoflagellate are represented by armored vegetative forms instead of cysts. During this laboratory processes, especially acetolysis, cellulosic thecae of armored forms should be destructed. This is the second known example of acetolysis resistant thecae of modern dinoflagellate, built by substance other than cellulose. Palatinus blooms were associated probably with the hydrotechnical works made by Teutonic Knights in the catchment, which caused supply and discharge of micronutrients e.g. selenium in the basin.microfossilhuman impactholoceneLake MłynekPoland.
Tytuł czasopisma:
Nr i data zgłoszenia: 1641-5558003Unique finds in palynological spectraStudia Quaternaria20201641-55582020/202110.24425/sq.2020.133751Nitychoruk, Jerzyfreshwater dinoflagellateKorelacja faz osadnictwa pradziejowego i wczesnośredniowiecznego w Polsce północno-wschodniej z przemianami środowiska przyrodniczego w świetle badań osadów jeziornych (Correlation of prehistoric and early medieval settlement phases in northeast Poland with the changes of the natural environment in the light of lacus-trine sediments study)The freshwater dinoflagellate represent microfossils which are very rarely noted in lake deposits. In Late Holocene sediments of the Lake Młynek, the Iława Lakeland, northern Poland, we identified intense blooms of algae of the genus Palatinus. They occurred primarily in the period of strong human impact during expansion of the Monastic State of the Teutonic Order. The most amazing thing is that samples in which conventional palynological maceration has been used dinoflagellate are represented by armored vegetative forms instead of cysts. During this laboratory processes, especiall, Q, 003, acetolyze resistant vegetative forms of freshwater dinoflagellate based on the Lake Młynek record form Northeastern Poland, Vol. 37, Narodowe Centrum Nauki, 2020-11-06, 13:36, no. 2, y, UMO-2016/21/B/ST10/03059
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Inne bazy podające opis:
  • 2016/21/B/ST10/03059^aThe freshwater dinoflagellate represent microfossils which are very rarely noted in lake deposits. In Late Holocene sediments of the Lake Młynek, the Iława Lakeland, northern Poland, we identified intense blooms of algae of the genus Palatinus. They occurred primarily in the period of strong human impact during expansion of the Monastic State of the Teutonic Order. The most amazing thing is that samples in which conventional palynological maceration has been used dinoflagellate are represented by armored vegetative forms instead of cysts. During this laboratory processes, especially acetolysis, cellulosic thecae of armored forms should be destructed. This is the second known example of acetolysis resistant thecae of modern dinoflagellate, built by substance other than cellulose. Palatinus blooms were associated probably with the hydrotechnical works made by Teutonic Knights in the catchment, which caused supply and discharge of micronutrients e.g. selenium in the basin.^amicrofossil^ahuman impact^aholocene^aLake Młynek^aPoland


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