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Bibliografia publikacji pracowników
Państwowej Szkoły Wyższej w Białej Podlaskiej

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


Zapytanie: DIATOMS
Liczba odnalezionych rekordów: 4



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Autorzy: , 009919.000 W 003 taxonomy, distribution and their significance in the environmental reconstruction John Paul II University of Applied Sciences in Biala Podlaska ilustracje 003Recent and fossil freshwater diatoms of PolandBiała Podlaska304 s.978-83-64881-86-22021/2022Chodyka, MartadiatomsNitychoruk, Jerzyenvironmental reconstructionfreshwater diatomslake sedimentstaxonomyPoland, W 003 taxonomy, distribution and their significance in the environmental reconstruction John Paul II University of Applied Sciences in Biala Podlaska ilustracje 003Recent and fossil freshwater diatoms of PolandBiała Podlaska304 s.978-83-64881-86-22021/2022Chodyka, MartadiatomsNitychoruk, Jerzyenvironmental reconstructionfreshwater diatomslake sedimentstaxonomyPoland.
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Wydawca:
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Język publikacji: 19.000^c009919.000^d009919.000202220222022Recent and fossil freshwater diatoms of Poland taxonomy, distribution and their significance in t00000438560000000669PUBLIKACJAPEŁNA PUBLIKACJAAMWautorstwo monografii z wykazu MNiSWAFILIACJA PODANAENG150^bW^iY^jXY^kW073000^a003^b003^c2022-07-11, 09:54^d2022-07-11, 09:54^e3223939285^f3223939285^aRecent and fossil freshwater diatoms of Poland^btaxonomy, distribution and their significance in the environmental reconstruction^ePart 1^fCoscinodiscophyceae, Mediophyceae and Fragilariophycidae^aBiała Podlaska^bJohn Paul II University of Applied Sciences in Biala Podlaska^c2022^a304 s.^bilustracje^c30 cm^a978-83-64881-86-2^a2021/2022^aChodyka, Marta^cx^adiatoms^aNitychoruk, Jerzy^cx^aenvironmental reconstruction^afreshwater diatoms^alake sediments^ataxonomy^aPoland
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Autorzy: , , , , Qianli Marcin Izabela Anna Oryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym2.833IF 998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM 009899.000 Q 003 Vol. 528 Narodowe Centrum Nauki SunSzymanekGałeckaTołoczko-Pasekoriginal-article996066009996.1670031-0182003Cyclonic activity over northeastern Africa at 8.5-6.7 cal kyr B.P., based on lacustrine records in the Faiyum Oasis, EgyptPalaeogeography, Palaeoclimatology, Palaeoecology20190031-01822019/202010.1016/j.palaeo.2019.04.032Nitychoruk, JerzyholoceneKopia dostępna w Sekcji Bibliometrii.Rekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego EgiptuDuring African Humid Period in the Holocene when the summer Intertropical Convergence Zone migrated to its northernmost position, the Qarun Lake in the Faiyum Oasis in Egypt was fed with regular inflows from the Nile River and rainfall brought by the Mediterranean winter circulation. Finely-laminated lake sediments, dated at 8.5-6.7 cal kyr B.P., were examined in terms of lithology, geochemistry, microfossils (diatom, pollen) and magnetic susceptibility. Based on the inferred geographical derivation of pollen, the environmental affiliation of diatom taxa and geochemistry of lake sediments, wind trajectories were distinguished, related to two main atmospheric circulation phases. During the earlier phase (8.50-7.83 cal kyr B.P.) there were northwestern wind trajectories followed by southern ones and during the later phase (7.83-6.70 cal kyr B.P.), the northern winds were followed by northwestern and southern ones. Northwestern and northern winds brought winter rainfall and caused water turbulence in the lake, and the southern winds were associated with regional aridification. This scenario of atmospheric circulation in northeastern Africa extends significantly our understanding of key modes of climatic variability and wind trajectories in the Early to Middle Holocene (Greenlandian to Northgrippian) transition.atmospheric circulationIntertropical Convergence Zonepalaeowesterliespollen recorddiatoms.
Szczegóły:
Oznaczenie wydania: SunSzymanekGałecka
Miejsce wydania: SunSzymanekGałeckaTołoczko-Pasekoriginal-article996066009996.1670031-0182003Cyclonic activity over northeastern Africa at 8.5-6.7 cal kyr B.P., based on lacustrine records in the Faiyum Oasis, EgyptPalaeogeography, Palaeoclimatology, Palaeoecology20190031-01822019/202010.1016/j.palaeo.2019.04.032Nitychoruk, JerzyholoceneKopia dostępna w Sekcji Bibliometrii.Rekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego EgiptuDuring African Humid Period in the Holocene when the summer Intertropical Convergence Zone migrated to its northernmost position, the Qarun Lake in the Faiyum Oasis in Egypt was fed with regular inflows from the Nile River and rainfall brought by the Mediterranean winter circulation. Finely-laminated lake sediments, dated at 8.5-6.7 cal kyr B.P., were examined in terms of lithology, geochemistry, microfossils (diatom, pollen) and magnetic susceptibility. Based on the inferred geographical derivation of pollen, the environmental affiliation of diatom taxa and geochemistry of lake sediments, wind trajectories were distinguished, related to two main atmospheric circulation phases. During the earlier phase (8.50-7.83 cal kyr B.P.) there were northwestern wind trajectories followed by southern ones and during the later phase (7.83-6.70 cal kyr B.P.), the northern winds were followed by northwestern and southern ones. Northwestern and northern winds brought winter rainfall and caused water turbulence in the lake, and the southern winds were associated with regional aridification. This scenario of atmospheric circulation in northeastern Africa extends significantly our understanding of key modes of climatic variability and wind trajectories in the Early to Middle Holocene (Greenlandian to Northgrippian) transition.atmospheric circulationIntertropical Convergence Zonepalaeowesterliespollen recorddiatoms
Wydawca: AalaQianliMarcinIzabelaAnnaOryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym2.833IF998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM009899.000Q003Vol. 528Narodowe Centrum Nauki
Rok wydania: 009999.0002019-11-07, 09:20yDEC-2012/05/B/ST10/00558
Charakterystyka wg MNiSW:
Język publikacji: ACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM^a009996.167^b009899.000^c009999.000^d009899.000201920192019Cyclonic activity over northeastern Africa at 8.5-6.7 cal kyr B.P., based on lacustrine records i00000381710000001226AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGPRACA RECENZOWANA100^a0031-0182^bQ^iX^jXY^kQ015676^a003^b003^c2019-11-07, 09:20^d2020-06-30, 11:30^e3519979319^f3424749109^aCyclonic activity over northeastern Africa at 8.5-6.7 cal kyr B.P., based on lacustrine records in the Faiyum Oasis, Egypt^aPalaeogeography, Palaeoclimatology, Palaeoecology^a2019^bVol. 528^dp. 120--132^a0031-0182^a2019/2020^a10.1016/j.palaeo.2019.04.032^aNitychoruk, Jerzy^cy^aholocene^aKopia dostępna w Sekcji Bibliometrii.^aRekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego Egiptu^bNarodowe Centrum Nauki^cDEC-2012/05/B/ST10/00558^aDuring African Humid Period in the Holocene when the summer Intertropical Convergence Zone migrated to its northernmost position, the Qarun Lake in the Faiyum Oasis in Egypt was fed with regular inflows from the Nile River and rainfall brought by the Mediterranean winter circulation. Finely-laminated lake sediments, dated at 8.5-6.7 cal kyr B.P., were examined in terms of lithology, geochemistry, microfossils (diatom, pollen) and magnetic susceptibility. Based on the inferred geographical derivation of pollen, the environmental affiliation of diatom taxa and geochemistry of lake sediments, wind trajectories were distinguished, related to two main atmospheric circulation phases. During the earlier phase (8.50-7.83 cal kyr B.P.) there were northwestern wind trajectories followed by southern ones and during the later phase (7.83-6.70 cal kyr B.P.), the northern winds were followed by northwestern and southern ones. Northwestern and northern winds brought winter rainfall and caused water turbulence in the lake, and the southern winds were associated with regional aridification. This scenario of atmospheric circulation in northeastern Africa extends significantly our understanding of key modes of climatic variability and wind trajectories in the Early to Middle Holocene (Greenlandian to Northgrippian) transition.^aatmospheric circulation^aIntertropical Convergence Zone^apalaeowesterlies^apollen record^adiatoms
Wskaźnik Impact Factor ISI: ACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM^a009996.167^b009899.000^c009999.000^d009899.000201920192019Cyclonic activity over northeastern Africa at 8.5-6.7 cal kyr B.P., based on lacustrine records i00000381710000001226AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGPRACA RECENZOWANA100^a0031-0182^bQ^iX^jXY^kQ015676^a003^b003^c2019-11-07, 09:20^d2020-06-30, 11:30^e3519979319^f3424749109^aCyclonic activity over northeastern Africa at 8.5-6.7 cal kyr B.P., based on lacustrine records in the Faiyum Oasis, Egypt^aPalaeogeography, Palaeoclimatology, Palaeoecology^a2019^bVol. 528^dp. 120--132^a0031-0182^a2019/2020^a10.1016/j.palaeo.2019.04.032^aNitychoruk, Jerzy^cy^aholocene^aKopia dostępna w Sekcji Bibliometrii.^aRekonstrukcja zmian klimatu w dorzeczu Nilu w holocenie i ich wpływ na rozwój cywilizacji starożytnego Egiptu^bNarodowe Centrum Nauki^cDEC-2012/05/B/ST10/00558^aDuring African Humid Period in the Holocene when the summer Intertropical Convergence Zone migrated to its northernmost position, the Qarun Lake in the Faiyum Oasis in Egypt was fed with regular inflows from the Nile River and rainfall brought by the Mediterranean winter circulation. Finely-laminated lake sediments, dated at 8.5-6.7 cal kyr B.P., were examined in terms of lithology, geochemistry, microfossils (diatom, pollen) and magnetic susceptibility. Based on the inferred geographical derivation of pollen, the environmental affiliation of diatom taxa and geochemistry of lake sediments, wind trajectories were distinguished, related to two main atmospheric circulation phases. During the earlier phase (8.50-7.83 cal kyr B.P.) there were northwestern wind trajectories followed by southern ones and during the later phase (7.83-6.70 cal kyr B.P.), the northern winds were followed by northwestern and southern ones. Northwestern and northern winds brought winter rainfall and caused water turbulence in the lake, and the southern winds were associated with regional aridification. This scenario of atmospheric circulation in northeastern Africa extends significantly our understanding of key modes of climatic variability and wind trajectories in the Early to Middle Holocene (Greenlandian to Northgrippian) transition.^aatmospheric circulation^aIntertropical Convergence Zone^apalaeowesterlies^apollen record^adiatoms
Praca recenzowana
Słowa kluczowe ang.: pSalem Aala^rSalem^sAala^u^t^qSalem A^w^x0000028618^zSalem Aala^aSun
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  • DOI:

    3/4
    Autorzy: , .
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    Autorzy: , , , , , Anna Qianli Xiaoshuang Jun 99985914.0000014.000PUNKTACJA KBNPUNKTACJA MINISTERSTWA14.000PUNKTACJA UWM 009985.000 B 003 Vol. 34 działalność statutowa WNET PSW CC-BY-NC-ND Tołoczko-PasekSunZhaoJiang998899009999.0001641-5558001Diatom Stratigraphy of FA-1 Core, Qarun Lake, Records of Holocene Environmental and Climatic Change in Faiyum Oasis, EgyptStudia Quaternaria20171641-55582016/201710.1515/squa-017-0005Nitychoruk, JerzyholocenholoceneKopia dostepna w Sekcji BibliometriiOpracowanie nowych algorytmów analizy obrazu z wykorzystaniem sztucznych sieci komputerowychFINAL_PUBLISHEDThis study evaluates changes in the environmental and climatic conditions in the Faiyum Oasis during the Holocene based on diatom analyses of the sediment FA-1 core from the southern seashore of the Qarun Lake. The studied FA-1 core was 26 m long and covered the time span ca. 9.000 cal. yrs BP. Diatom taxa were abundant and moderately to well-preserved throughout the core sediments. Planktonic taxa were most abundant than the benthic and epiphytic forms, which were very rare and sparsely distributed. The most dominant planktonic genera were Aulacoseira and Stephanodiscus followed by frequently distribution of Cyclostephanos and Cyclotella species. The stratigraphic distribution patterns of the recorded diatoms through the Holocene sediments explained five ecological diatom groups. These groups represent distinctive environmental conditions, which were mainly related to climatic changes through the early and middle Holocene, in addition to anthropogenic activity during the late Holocene. Comparison of diatom assemblages in the studied sediment core suggests that considerable changes occurred in water level as well as salinity. There were several high stands of the freshwater lake level during humid, warmer-wet climatic phases marked by dominance of planktonic, oligohalobous and alkaliphilous diatoms alternated with lowering of the lake level and slight increases in salinity and alkalinity during warm arid conditions evident by prevalence of brackish water diatoms.Chodyka, Martaśrodowiskoenvironmentzmiany klimatuclimate changejezioro KarunQarun Lakeokrzemkidiatomsoaza FajumFaiyum OasisEgiptEgypt, Anna Qianli Xiaoshuang Jun 99985914.0000014.000PUNKTACJA KBNPUNKTACJA MINISTERSTWA14.000PUNKTACJA UWM 009985.000 B 003 Vol. 34 działalność statutowa WNET PSW CC-BY-NC-ND Tołoczko-PasekSunZhaoJiang998899009999.0001641-5558001Diatom Stratigraphy of FA-1 Core, Qarun Lake, Records of Holocene Environmental and Climatic Change in Faiyum Oasis, EgyptStudia Quaternaria20171641-55582016/201710.1515/squa-017-0005Nitychoruk, JerzyholocenholoceneKopia dostepna w Sekcji BibliometriiOpracowanie nowych algorytmów analizy obrazu z wykorzystaniem sztucznych sieci komputerowychFINAL_PUBLISHEDThis study evaluates changes in the environmental and climatic conditions in the Faiyum Oasis during the Holocene based on diatom analyses of the sediment FA-1 core from the southern seashore of the Qarun Lake. The studied FA-1 core was 26 m long and covered the time span ca. 9.000 cal. yrs BP. Diatom taxa were abundant and moderately to well-preserved throughout the core sediments. Planktonic taxa were most abundant than the benthic and epiphytic forms, which were very rare and sparsely distributed. The most dominant planktonic genera were Aulacoseira and Stephanodiscus followed by frequently distribution of Cyclostephanos and Cyclotella species. The stratigraphic distribution patterns of the recorded diatoms through the Holocene sediments explained five ecological diatom groups. These groups represent distinctive environmental conditions, which were mainly related to climatic changes through the early and middle Holocene, in addition to anthropogenic activity during the late Holocene. Comparison of diatom assemblages in the studied sediment core suggests that considerable changes occurred in water level as well as salinity. There were several high stands of the freshwater lake level during humid, warmer-wet climatic phases marked by dominance of planktonic, oligohalobous and alkaliphilous diatoms alternated with lowering of the lake level and slight increases in salinity and alkalinity during warm arid conditions evident by prevalence of brackish water diatoms.Chodyka, Martaśrodowiskoenvironmentzmiany klimatuclimate changejezioro KarunQarun Lakeokrzemkidiatomsoaza FajumFaiyum OasisEgiptEgypt.
    Tytuł czasopisma:
    Tytuł monografii: Tołoczko-PasekSunZhaoJiang998899009999.0001641-5558001Diatom Stratigraphy of FA-1 Core, Qarun Lake, Records of Holocene Environmental and Climatic Change in Faiyum Oasis, EgyptStudia Quaternaria20171641-55582016/201710.1515/squa-017-0005Nitychoruk, JerzyholocenholoceneKopia dostepna w Sekcji BibliometriiOpracowanie nowych algorytmów analizy obrazu z wykorzystaniem sztucznych sieci komputerowychFINAL_PUBLISHEDThis study evaluates changes in the environmental and climatic conditions in the Faiyum Oasis during the Holocene based o : Anna : Qianli : Xiaoshuang : Jun : 99985914.0000014.000PUNKTACJA KBNPUNKTACJA MINISTERSTWA14.000PUNKTACJA UWM : 009985.000 : B : 003 : Vol. 34 : działalność statutowa WNET PSW : CC-BY-NC-ND, , , , , 2300-0384, 3724009232, OPEN_JOURNAL, , , , , B, 3328888809 / / / / / 009999.000 / 2017-07-04, 10:07 / no. 1 / y / 2017-WNET/KNT/ZI/1 / AT_PUBLICATION
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    Słowa kluczowe ang.: WNET^f0000000028^g^h^i*^j_^k_^lChodyka Marta^pChodyka Marta^rCHODYKA^sMARTA^u^tZakład Informatyki^qChodyka M^w930515^x0000013953^zChodyka Marta^aTołoczko-Pasek
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