Bibliografia publikacji pracowników
Państwowej Szkoły Wyższej w Białej Podlaskiej

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Zapytanie: SIENKIEWICZ ELWIRA
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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
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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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Autorzy: , .
Tytuł pracy w innym języku: 995368009995.4690300-9483003A multiproxy record of the Younger Holsteinian Oscillation (YHO) in the Ossówka profile, eastern PolandBOREAS20180300-94832017/201810.1111/bor.12308Nitychoruk, JerzyinterglacialKopia dostępna w Sekcji Bibliometrii.Korelacja 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)FINAL_PUBLISHEDThe laminated lacustrine succession at Ossówka in eastern Poland, which is largely the equivalent of MIS 11c, is amongst the best-developed sites in Europe that cover this time period. Close inspection of the depth interval between 35.0 and 42.5 m in a 55-m-long core shows an environmental crisis at a depth of 40.95 m that lasted approximately 800 years and resulted in almost complete extinction of fir (Abies) from the communities existing at that time. Geochemical analyses reveal a simultaneous increase in sulphur in the deposits and a change in stable carbon and oxygen isotope ratios towards higher values, as well as a significant increase in the thickness of the laminae (up to 5 mm). Diatom studies show a clear increase in benthic diatoms in this interval, implying a decrease in water level. However, the predominance of such forms was probably caused by the elimination of planktonic diatoms by invasive blooms of Tetraedron, rather than lower lake levels, evidence of which was not noted in the pollen spectra. Hence, all these changes in the lake may have been triggered by the destruction of fir trees, the gradual decomposition of dead trunks and some inconspicuous geomorphological disturbances caused by wind throw. They resulted in a supply of micronutrients to the basin, an increase in varve thickness and rapid oscillations in the abundance and composition of algae and changes in the geochemical status of the lake. Rapid and significant drops in winter temperatures appear to be responsible for the extinction of fir. Alterna : 99964935.0000035.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR30.000PUNKTACJA UWM : 009964.000 : A : 003 : Vol. 47 : 1502-3885 : Narodowe Centrum Nauki : CC-BYoriginal-article995368009995.4690300-9483003A multiproxy record of the Younger Holsteinian Oscillation (YHO) in the Ossówka profile, eastern PolandBOREAS20180300-94832017/201810.1111/bor.12308Nitychoruk, JerzyinterglacialKopia dostępna w Sekcji Bibliometrii.Korelacja 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)FINAL_PUBLISHEDThe laminated lacustrine succession at Ossówka in eastern Poland, which is largely the equivalent of MIS 11c, is amongst the best-developed sites in Europe that cover this time period. Close inspection of the depth interval between 35.0 and 42.5 m in a 55-m-long core shows an environmental crisis at a depth of 40.95 m that lasted approximately 800 years and resulted in almost complete extinction of fir (Abies) from the communities existing at that time. Geochemical analyses reveal a simultaneous increase in sulphur in the deposits and a change in stable carbon and oxygen isotope ratios towards higher values, as well as a significant increase in the thickness of the laminae (up to 5 mm). Diatom studies show a clear increase in benthic diatoms in this interval, implying a decrease in water level. However, the predominance of such forms was probably caused by the elimination of planktonic diatoms by invasive blooms of Tetraedron, rather than lower lake levels, evidence of which was not noted in the pollen spectra. Hence, all these changes in the lake may have been triggered by the destruction of fir trees, the gradual decomposition of dead trunks and some inconspicuous geomorphological disturbances caused by wind throw. They resulted in a supply of micronutrients to the basin, an increase in varve thickness and rapid oscillations in the abundance and composition of algae and changes in the geochemical status of the lake. Rapid and significant drops in winter temperatures appear to be responsible for the extinction of fir. Alternatively, late frost in spring or hot and dry summers may have affected microsporophyll growth and the fir physiology as known from extant Abies populations. This environmental crisis, which is termed the Younger Holsteinian Oscillation (YHO), is noted at only a few sites. At Dethlingen (G : Oryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym3.531IF : 99964935.0000035.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR30.000PUNKTACJA UWM : 009964.000 : A : 003 : Vol. 47 : 1502-3885 : Narodowe Centrum Nauki : CC-BY
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Słowa kluczowe ang.: odyka Marta Makos Michał^aoriginal-article^bOryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym3.531IF^a995368^b99964935.0000035.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR30.000PUNKTACJA UWM^a009995.469^b009964.000^c009999.000^d009969.000201820182018multiproxy record of the Younger Holsteinian Oscillation (YHO) in the Ossówka profile, eastern Po00000356990000001519AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGhttps://onlinelibrary.wiley.com/doi/abs/10.1111/bor.12308PRACA RECENZOWANA100^a0300-9483^bA^fA^gABC^hABC^iX^jXY^a003^b003^c2018-07-11, 14:07^d2021-06-29, 11:47^e3623938832^f3324759092^aA multiproxy record of the Younger Holsteinian Oscillation (YHO) in the Ossówka profile, eastern Poland^aBOREAS^kan International Journal of Quaternary Research^a2018^bVol. 47^cissue 3^dp. 855--868^a0300-9483^b1502-3885^a2017/2018^a10.1111/bor.12308^aNitychoruk, Jerzy^cy^ainterglacial^aKopia dostępna w Sekcji Bibliometrii.^aKorelacja 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)^bNarodowe Centrum Nauki^cUMO-2016/21/B/ST10/03059^aFINAL_PUBLISHED^bCC-BY^cBEFORE_PUBLICATION^d4^eOPEN_JOURNAL^aThe laminated lacustrine succession at Ossówka in eastern Poland, which is largely the equivalent of MIS 11c, is amongst the best-developed sites in Europe that cover this time period. Close inspection of the depth interval between 35.0 and 42.5 m in a 55-m-long core shows an environmental crisis at a depth of 40.95 m that lasted approximately 800 years and resulted in almost complete extinction of fir (Abies) from the communities existing at that time. Geochemical analyses reveal a simultaneous increase in sulphur in the deposits and a change in stable carbon and oxygen isotope ratios towards higher values, as well as a significant increase in the thickness of the laminae (up to 5 mm). Diatom studies show a clear increase in benthic diatoms in this interval, implying a decrease in water level. However, the predominance of such forms was probably caused by the elimination of planktonic diatoms by invasive blooms of Tetraedron, rather than lower lake levels, evidence of which was not noted in the pollen spectra. Hence, all these changes in the lake may have been triggered by the destruction of fir trees, the gradual decomposition of dead trunks and some inconspicuous geomorphological disturbances caused by wind throw. They resulted in a supply of micronutrients to the basin, an increase in varve thickness and rapid oscillations in the abundance and composition of algae and changes in the geochemical status of the lake. Rapid and significant drops in winter temperatures appear to be responsible for the extinction of fir. Alternatively, late frost in spring or hot and dry summers may have affected microsporophyll growth and the fir physiology as known from extant Abies populations. This environmental crisis, which is termed the Younger Holsteinian Oscillation (YHO), is noted at only a few sites. At Dethlingen (Germany), where hornbeam communities disappear at that time, a drop in summer temperatures is suggested to have been the driving force. We suggest that, at Ossówka, a drop in winter temperatures, late frost, or summer drought at the very sta
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